1
|
Bednaršek N, Pelletier G, Beck MW, Feely RA, Siegrist Z, Kiefer D, Davis J, Peabody B. Predictable patterns within the kelp forest can indirectly create temporary refugia from ocean acidification. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 945:174065. [PMID: 38897470 DOI: 10.1016/j.scitotenv.2024.174065] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/14/2023] [Revised: 06/04/2024] [Accepted: 06/15/2024] [Indexed: 06/21/2024]
Abstract
Kelps are recognized for providing many ecosystem services in coastal areas and considered in ocean acidification (OA) mitigation. However, assessing OA modification requires an understanding of the multiple parameters involved in carbonate chemistry, especially in highly dynamic systems. We studied the effects of sugar kelp (Saccharina latissima) on an experimental farm at the north end of Hood Canal, Washington-a low retentive coastal system. In this field mesocosm study, two oyster species (Magallana gigas, Ostrea lurida) were exposed at locations in the mid, edge, and outside the kelp array. The Hood Head Sugar Kelp Farm Model outputs were used to identify dominating factors in spatial and temporal kelp dynamics, while wavelet spectrum analyses helped in understanding predictability patterns. This was linked to the measured biological responses (dissolution, growth, isotopes) of the exposed organisms. Positioned in an area of high (sub)-diel tidal fluxes with low retention potential, there were no measurable alterations of the seawater pH at the study site, demonstrating that the kelp array could not induce a direct mitigating effect against OA. However, beneficial responses in calcifiers were still observed, which are linked to two causes: increased pH predictability and improved provisioning through kelp-derived particulate organic resource utilization and as such, kelp improved habitat suitability and indirectly created refugia against OA. This study can serve as an analogue for many coastal bay habitats where prevailing physical forcing drives chemical changes. Future macrophyte studies that investigate OA mitigating effects should focus also on the importance of predictability patterns, which can additionally improve the conditions for marine calcifiers and ecosystem services vulnerable to or compromised by OA, including aquaculture sustainability.
Collapse
Affiliation(s)
- Nina Bednaršek
- Cooperative Institute for Marine Resources Studies, Hatfield Marine Science Center, 2030 SE Marine Science Drive Newport, OR 97365, Oregon State University, USA; Institute Jožef Stefan, 1000 Ljubljana, Slovenia.
| | - Greg Pelletier
- Washington Department of Ecology, Olympia, 300 Desmond Dr SE, WA 98503,(Emeritus), USA
| | - Marcus W Beck
- Tampa Bay Estuary Program, St. Petersburg, FL 33701, USA
| | - Richard A Feely
- NOAA Pacific Marine Environmental Laboratory, Seattle, WA 98115, USA
| | - Zach Siegrist
- System Science Applications, Inc, Renton, Washington, USA
| | - Dale Kiefer
- University of Southern California, Los Angeles, CA 90089, USA
| | - Jonathan Davis
- Puget Sound Restoration Fund, Bainbridge Island, WA, 98110, USA
| | | |
Collapse
|
2
|
Shi Z, Zhao M, Wang K, Ma S, Luo H, Han Q, Shi Y. Acidification alleviates the inhibition of hyposaline stress on physiological performance of tropical seagrass Thalassia hemprichii. MARINE POLLUTION BULLETIN 2024; 205:116642. [PMID: 38941803 DOI: 10.1016/j.marpolbul.2024.116642] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/25/2023] [Revised: 03/03/2024] [Accepted: 06/19/2024] [Indexed: 06/30/2024]
Abstract
Since the Industrial Revolution, increasing atmospheric CO2 concentrations have had a substantial negative impact influence on coastal ecosystems because of direct effects including ocean acidification and indirect effects such as extreme rainfall events. Using a two-factor crossover indoor simulation experiment, this study examined the combined effects of acidification and hyposaline stress on Thalassia hemprichii. Seawater acidification increased the photosynthetic pigment content of T. hemprichii leaves and promoted seagrass growth rate. Hyposaline stress slowed down seagrass growth and had an impact on the osmotic potential and osmoregulatory substance content of seagrass leaves. Acidification and salinity reduction had significant interaction effects on the photosynthesis rate, photosynthetic pigment content, chlorophyll fluorescence parameters, and osmotic potential of T. hemprichii, but not on the growth rate. Overall, these findings have shown that the hyposaline stress inhibitory effect on the T. hemprichii physiological performance and growth may be reduced by acidification.
Collapse
Affiliation(s)
- Zhiqiang Shi
- Yazhou Bay Innovation Institute, Hainan Tropical Ocean University, Sanya 572022, China
| | - Muqiu Zhao
- Yazhou Bay Innovation Institute, Hainan Tropical Ocean University, Sanya 572022, China; Modern Marine Ranching Engineering Research Center of Hainan, Sanya 572022, China; Key Laboratory for Coastal Marine Eco-Environment Process and Carbon Sink of Hainan, Sanya 572022, China
| | - Kang Wang
- Yazhou Bay Innovation Institute, Hainan Tropical Ocean University, Sanya 572022, China
| | - Siyang Ma
- Yazhou Bay Innovation Institute, Hainan Tropical Ocean University, Sanya 572022, China
| | - Huijue Luo
- Yazhou Bay Innovation Institute, Hainan Tropical Ocean University, Sanya 572022, China
| | - Qiuying Han
- Yazhou Bay Innovation Institute, Hainan Tropical Ocean University, Sanya 572022, China; Modern Marine Ranching Engineering Research Center of Hainan, Sanya 572022, China; Key Laboratory for Coastal Marine Eco-Environment Process and Carbon Sink of Hainan, Sanya 572022, China
| | - Yunfeng Shi
- Yazhou Bay Innovation Institute, Hainan Tropical Ocean University, Sanya 572022, China; Modern Marine Ranching Engineering Research Center of Hainan, Sanya 572022, China; Key Laboratory for Coastal Marine Eco-Environment Process and Carbon Sink of Hainan, Sanya 572022, China.
| |
Collapse
|
3
|
Li Y, Zhang J, Zeng H, Zhang H. Ion association behaviors in the initial stage of calcium carbonate formation: An ab initio study. J Chem Phys 2024; 161:014503. [PMID: 38949280 DOI: 10.1063/5.0206841] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/04/2024] [Accepted: 06/12/2024] [Indexed: 07/02/2024] Open
Abstract
In this work, we performed static density functional theory calculations and ab initio metadynamics simulations to systematically investigate the association mechanisms and dynamic structures of four kinds of ion pairs that could be formed before the nucleation of CaCO3. For Ca2+-HCO3- and Ca2+-CO32- pairs, the arrangement of ligands around Ca2+ evolves between the six-coordinated octahedral structure and the seven-coordinated pentagonal bipyramidal structure. The formation of ion pairs follows an associative ligand substitution mechanism. Compared with HCO3-, CO32- exhibits a stronger affinity to Ca2+, leading to the formation of a more stable precursor phase in the prenucleation stage, which promotes the subsequent CaCO3 nucleation. In alkaline environments, excessive OH- ions decrease the coordination preference of Ca2+. In this case, the formation of Ca(OH)+-CO32- and Ca(OH)2-CO32- pairs favors the dissociative ligand substitution mechanism. The inhibiting effects of OH- ion on the CaCO3 association can be interpreted from two aspects, i.e., (1) OH- neutralizes positive charges on Ca2+, decreases the electrostatic interactions between Ca2+ and CO32-, and thus hinders the formation of the CaCO3 monomer, and (2) OH- decreases the capacity of Ca2+ for accommodating O, making it easier to separate Ca2+ and CO32- ions. Our findings on the ion association behaviors in the initial stage of CaCO3 formation not only help scientists evaluate the impact of ocean acidification on biomineralization but also provide theoretical support for the discovery and development of more effective approaches to manage undesirable scaling issues.
Collapse
Affiliation(s)
- Yue Li
- Department of Chemical and Materials Engineering, University of Alberta, Edmonton, Alberta T6G 1H9, Canada
| | - Jiarui Zhang
- Department of Chemical and Materials Engineering, University of Alberta, Edmonton, Alberta T6G 1H9, Canada
| | - Hongbo Zeng
- Department of Chemical and Materials Engineering, University of Alberta, Edmonton, Alberta T6G 1H9, Canada
| | - Hao Zhang
- Department of Chemical and Materials Engineering, University of Alberta, Edmonton, Alberta T6G 1H9, Canada
| |
Collapse
|
4
|
Khalil M, Stuhr M, Kunzmann A, Westphal H. Simultaneous ocean acidification and warming do not alter the lipid-associated biochemistry but induce enzyme activities in an asterinid starfish. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 932:173000. [PMID: 38719050 DOI: 10.1016/j.scitotenv.2024.173000] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/18/2023] [Revised: 04/30/2024] [Accepted: 05/03/2024] [Indexed: 05/13/2024]
Abstract
Ocean acidification and warming affect marine ecosystems from the molecular scale in organismal physiology to broad alterations of ecosystem functions. However, knowledge of their combined effects on tropical-subtropical intertidal species remains limited. Pushing the environmental range of marine species away from the optimum initiates stress impacting biochemical metabolic characteristics, with consequences on lipid-associated and enzyme biochemistry. This study investigates lipid-associated fatty acids (FAs) and enzyme activities involved in biomineralization of the tropical-subtropical starfish Aquilonastra yairi in response to projected near-future global change. The starfish were acclimatized to two temperature levels (27 °C, 32 °C) crossed with three pCO2 concentrations (455 μatm, 1052 μatm, 2066 μatm). Total lipid (ΣLC) and FAs composition were unaffected by combined elevated temperature and pCO2, but at elevated temperature, there was an increase in ΣLC, SFAs (saturated FAs) and PUFAs (polyunsaturated FAs), and a decrease in MUFAs (monounsaturated FAs). However, temperature was the sole factor to significantly alter SFAs composition. Positive parabolic responses of Ca-ATPase and Mg-ATPase enzyme activities were detected at 27 °C with elevated pCO2, while stable enzyme activities were observed at 32 °C with elevated pCO2. Our results indicate that the lipid-associated biochemistry of A. yairi is resilient and capable of coping with near-future ocean acidification and warming. However, the calcification-related enzymes Ca-ATPase and Mg-ATPase activity appear to be more sensitive to pCO2/pH changes, leading to vulnerability concerning the skeletal structure.
Collapse
Affiliation(s)
- Munawar Khalil
- Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany; Faculty of Geosciences, University of Bremen, Klagenfurter Str. 2-4, 28359 Bremen, Germany; Department of Marine Science, Faculty of Agriculture, Universitas Malikussaleh, Reuleut Main Campus, 24355 North Aceh, Indonesia.
| | - Marleen Stuhr
- Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany
| | - Andreas Kunzmann
- Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany
| | - Hildegard Westphal
- Leibniz Centre for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany; Faculty of Geosciences, University of Bremen, Klagenfurter Str. 2-4, 28359 Bremen, Germany
| |
Collapse
|
5
|
Hofmann Elizondo U, Vogt M, Bednaršek N, Münnich M, Gruber N. The impact of aragonite saturation variability on shelled pteropods: An attribution study in the California Current System. GLOBAL CHANGE BIOLOGY 2024; 30:e17345. [PMID: 38831686 DOI: 10.1111/gcb.17345] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/14/2023] [Revised: 04/22/2024] [Accepted: 04/25/2024] [Indexed: 06/05/2024]
Abstract
Observations from the California Current System (CalCS) indicate that the long-term trend in ocean acidification (OA) and the naturally occurring corrosive conditions for the CaCO3 mineral aragonite (saturation state Ω < 1) have a damaging effect on shelled pteropods, a keystone group of calcifying organisms in the CalCS. Concern is heightened by recent findings suggesting that shell formation and developmental progress are already impacted when Ω falls below 1.5. Here, we quantify the impact of low Ω conditions on pteropods using an individual-based model (IBM) with life-stage-specific mortality, growth, and behavior in a high-resolution regional hindcast simulation of the CalCS between 1984 and 2019. Special attention is paid to attributing this impact to different processes that lead to such low Ω conditions, namely natural variability, long-term trend, and extreme events. We find that much of the observed damage in the CalCS, and specifically >70% of the shell CaCO3 loss, is due to the pteropods' exposure to naturally occurring low Ω conditions as a result of their diel vertical migration (DVM). Over the hindcast period, their exposure to damaging waters (Ω < 1.5) increases from 9% to 49%, doubling their shell CaCO3 loss, and increasing their mortality by ~40%. Most of this increased exposure is due to the shoaling of low Ω waters driven by the long-term trend in OA. Extreme OA events amplify this increase by ~40%. Our approach can quantify the health of pteropod populations under shifting environmental conditions, and attribute changes in fitness or population structure to changes in the stressor landscape across hierarchical time scales.
Collapse
Affiliation(s)
- Urs Hofmann Elizondo
- Environmental Physics Group, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich, Zürich, Switzerland
| | - Meike Vogt
- Environmental Physics Group, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich, Zürich, Switzerland
| | - Nina Bednaršek
- Institute Jožef Stefan, Ljubljana, Slovenia
- Cooperative Institute for Marine Ecosystem and Resources Studies, Oregon State University, Corvallis, Oregon, USA
| | - Matthias Münnich
- Environmental Physics Group, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich, Zürich, Switzerland
| | - Nicolas Gruber
- Environmental Physics Group, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich, Zürich, Switzerland
| |
Collapse
|
6
|
Jiang J, Cao L, Jin X, Yu Z, Zhang H, Fu J, Jiang G. Response of ocean acidification to atmospheric carbon dioxide removal. J Environ Sci (China) 2024; 140:79-90. [PMID: 38331517 DOI: 10.1016/j.jes.2023.04.029] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/09/2023] [Revised: 04/22/2023] [Accepted: 04/22/2023] [Indexed: 02/10/2024]
Abstract
Artificial CO2 removal from the atmosphere (also referred to as negative CO2 emissions) has been proposed as a potential means to counteract anthropogenic climate change. Here we use an Earth system model to examine the response of ocean acidification to idealized atmospheric CO2 removal scenarios. In our simulations, atmospheric CO2 is assumed to increase at a rate of 1% per year to four times its pre-industrial value and then decreases to the pre-industrial level at a rate of 0.5%, 1%, 2% per year, respectively. Our results show that the annual mean state of surface ocean carbonate chemistry fields including hydrogen ion concentration ([H+]), pH and aragonite saturation state respond quickly to removal of atmospheric CO2. However, the change of seasonal cycle in carbonate chemistry lags behind the decline in atmospheric CO2. When CO2 returns to the pre-industrial level, over some parts of the ocean, relative to the pre-industrial state, the seasonal amplitude of carbonate chemistry fields is substantially larger. Simulation results also show that changes in deep ocean carbonate chemistry substantially lag behind atmospheric CO2 change. When CO2 returns to its pre-industrial value, the whole-ocean acidity measured by [H+] is 15%-18% larger than the pre-industrial level, depending on the rate of CO2 decrease. Our study demonstrates that even if atmospheric CO2 can be lowered in the future as a result of net negative CO2 emissions, the recovery of some aspects of ocean acidification would take decades to centuries, which would have important implications for the resilience of marine ecosystems.
Collapse
Affiliation(s)
- Jiu Jiang
- School of Environment, Hangzhou Institute for Advanced Study, University of Chinese Academy of Sciences, Hangzhou 310024, China; State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
| | - Long Cao
- Key Laboratory of Geoscience Big Data and Deep Resources of Zhejiang Province, School of Earth Sciences, Zhejiang University, Hangzhou 310058, China.
| | - Xiaoyu Jin
- Key Laboratory of Geoscience Big Data and Deep Resources of Zhejiang Province, School of Earth Sciences, Zhejiang University, Hangzhou 310058, China
| | - Zechen Yu
- School of Environment, Hangzhou Institute for Advanced Study, University of Chinese Academy of Sciences, Hangzhou 310024, China
| | - Han Zhang
- Zhejiang Climate Center, Hangzhou 310052, China
| | - Jianjie Fu
- School of Environment, Hangzhou Institute for Advanced Study, University of Chinese Academy of Sciences, Hangzhou 310024, China; State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.
| | - Guibin Jiang
- School of Environment, Hangzhou Institute for Advanced Study, University of Chinese Academy of Sciences, Hangzhou 310024, China; State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
| |
Collapse
|
7
|
Thangal SH, Muralisankar T, Mohan K, Santhanam P, Venmathi Maran BA. Biological and physiological responses of marine crabs to ocean acidification: A review. ENVIRONMENTAL RESEARCH 2024; 248:118238. [PMID: 38262516 DOI: 10.1016/j.envres.2024.118238] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/06/2023] [Revised: 01/02/2024] [Accepted: 01/17/2024] [Indexed: 01/25/2024]
Abstract
Marine crabs play an integral role in the food chain and scavenge the debris in the ecosystem. Gradual increases in global atmospheric carbon dioxide cause ocean acidification (OA) and global warming that leads to severe consequences for marine organisms including crabs. Also, OA combined with other stressors like temperature, hypoxia, and heavy metals causes more severe adverse effects in marine crabs. The present review was made holistic discussion of information from 111 articles, of which 37 peer-reviewed original research papers reported on the effect of OA experiments and its combination with other stressors like heavy metals, temperature, and hypoxia on growth, survival, molting, chitin quality, food indices, tissue biochemical constituents, hemocytes population, and biomarker enzymes of marine crabs. Nevertheless, the available reports are still in the infancy of marine crabs, hence, this review depicts the possible gaps and future research needs on the impact of OA on marine crabs.
Collapse
Affiliation(s)
- Said Hamid Thangal
- Aquatic Ecology Laboratory, Department of Zoology, Bharathiar University, Coimbatore-641046, Tamil Nadu, India
| | | | - Kannan Mohan
- PG and Research Department of Zoology, Sri Vasavi College, Erode, Tamil Nadu 638 316, India
| | - Perumal Santhanam
- Marine Planktonology& Aquaculture Laboratory, Department of Marine Science, Bharathidasan University, Tiruchirappalli- 620024, Tamil Nadu, India
| | - Balu Alagar Venmathi Maran
- Institute of Integrated Science and Technology, Nagasaki University, 1-14 Bunkyomachi, Nagasaki, 852-8521, Japan
| |
Collapse
|
8
|
Nussbaum R, Jeanneret S, Bakker E. Increasing the Sensitivity of pH Glass Electrodes with Constant Potential Coulometry at Zero Current. Anal Chem 2024; 96:6436-6443. [PMID: 38593052 PMCID: PMC11044110 DOI: 10.1021/acs.analchem.4c00592] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/30/2024] [Revised: 03/12/2024] [Accepted: 03/22/2024] [Indexed: 04/11/2024]
Abstract
It has recently become possible to increase the sensitivity of ion-selective electrodes (ISEs) by imposing a constant cell potential, allowing one to record current spikes with a capacitor placed in series in the circuit. The approach requires a transient current to pass through the measurement cell, which unfortunately may introduce measurement errors and additionally excludes the use of high-impedance indicator electrodes, such as pH glass electrodes. We present here an electronic circuit that overcomes these limitations, where the cell is measured at zero current in combination with a voltage follower, and the current spike and capacitor charging occur entirely within the instrument. The approach avoids the need for a counter electrode, and one may use any electrode useful in potentiometry regardless of its impedance. The characteristics of the circuit were found to approach ideality when evaluated with either an external potential source or an Ag/AgCl electrode. The current may be linearized and extrapolated to further reduce the measurement time. The circuit is further tested with the most common yet very challenging electrode, the pH glass electrode. A precision of 64 μpH was obtained for 0.01 pH change up to 0.05 from a reference solution. Similar pH changes were also measured reliably further away from the reference solution (0.5-0.55) and resulted in a precision of 377 μpH. The limitations of this experimental setup were explored by performing pH calibrations within the measuring range of the probe.
Collapse
Affiliation(s)
- Robin Nussbaum
- Department of Inorganic and
Analytical Chemistry, University of Geneva, CH-1211 Geneva, Switzerland
| | - Stéphane Jeanneret
- Department of Inorganic and
Analytical Chemistry, University of Geneva, CH-1211 Geneva, Switzerland
| | - Eric Bakker
- Department of Inorganic and
Analytical Chemistry, University of Geneva, CH-1211 Geneva, Switzerland
| |
Collapse
|
9
|
Melbourne LA, Goodkin NF. Using Museum collections to assess the impact of industrialization on mussel (Mytilus edulis) calcification. PLoS One 2024; 19:e0301874. [PMID: 38630684 PMCID: PMC11023280 DOI: 10.1371/journal.pone.0301874] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/14/2023] [Accepted: 03/22/2024] [Indexed: 04/19/2024] Open
Abstract
Mytilus edulis is a commercially and ecologically important species found along the east coast of the United States. Ecologically, M. edulis improves water quality through filtration feeding and provides habitat formation and coastal protection through reef formation. Like many marine calcifiers, ocean warming, and acidification are a growing threat to these organisms-impacting their morphology and function. Museum collections are useful in assessing long-term environmental impacts on organisms in a natural multi-stressor environment, where acclimation and adaptation can be considered. Using the American Museum of Natural History collections ranging from the early 1900s until now, we show that shell porosity changes through time. Shells collected today are significantly more porous than shells collected in the 1960s and, at some sites, than shells collected from the early 1900s. The disparity between porosity changes matches well with the warming that occurred over the last 130 years in the north Atlantic suggesting that warming is causing porosity changes. However, more work is required to discern local environmental impacts and to fully identify porosity drivers. Since, porosity is known to affect structural integrity, porosity increasing through time could have negative consequences for mussel reef structural integrity and hence habitat formation and storm defenses.
Collapse
Affiliation(s)
- Leanne A. Melbourne
- Department of Earth and Planetary Sciences, American Museum of Natural History, New York, New York, United States of America
| | - Nathalie F. Goodkin
- Department of Earth and Planetary Sciences, American Museum of Natural History, New York, New York, United States of America
| |
Collapse
|
10
|
Huang Y, Song X, Wang YP, Canadell JG, Luo Y, Ciais P, Chen A, Hong S, Wang Y, Tao F, Li W, Xu Y, Mirzaeitalarposhti R, Elbasiouny H, Savin I, Shchepashchenko D, Rossel RAV, Goll DS, Chang J, Houlton BZ, Wu H, Yang F, Feng X, Chen Y, Liu Y, Niu S, Zhang GL. Size, distribution, and vulnerability of the global soil inorganic carbon. Science 2024; 384:233-239. [PMID: 38603490 DOI: 10.1126/science.adi7918] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/17/2023] [Accepted: 03/07/2024] [Indexed: 04/13/2024]
Abstract
Global estimates of the size, distribution, and vulnerability of soil inorganic carbon (SIC) remain largely unquantified. By compiling 223,593 field-based measurements and developing machine-learning models, we report that global soils store 2305 ± 636 (±1 SD) billion tonnes of carbon as SIC over the top 2-meter depth. Under future scenarios, soil acidification associated with nitrogen additions to terrestrial ecosystems will reduce global SIC (0.3 meters) up to 23 billion tonnes of carbon over the next 30 years, with India and China being the most affected. Our synthesis of present-day land-water carbon inventories and inland-water carbonate chemistry reveals that at least 1.13 ± 0.33 billion tonnes of inorganic carbon is lost to inland-waters through soils annually, resulting in large but overlooked impacts on atmospheric and hydrospheric carbon dynamics.
Collapse
Affiliation(s)
- Yuanyuan Huang
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
- State Key Laboratory of Resources and Environmental Information System, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
| | - Xiaodong Song
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China
| | - Ying-Ping Wang
- CSIRO Environment, Private Bag 10, Clayton South VIC 3169, Australia
| | | | - Yiqi Luo
- Soil and Crop Sciences Section, School of Integrative Plant Science, Cornell University, Ithaca NY 14853, USA
| | - Philippe Ciais
- Laboratoire des Sciences du Climat et de l'Environnement, CEA/CNRS/UVSQ/Université Paris Saclay, Gif-sur-Yvette 91990, France
| | - Anping Chen
- Department of Biology and Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO 80523, USA
| | - Songbai Hong
- School of Urban Planning and Design, Shenzhen Graduate School, Peking University, Shenzhen 518055, China
| | - Yugang Wang
- State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, Xinjiang 830011, China
| | - Feng Tao
- Department of Ecology and Evolutionary Biology and Department of Global Development, Cornell University, Ithaca, New York 14853, USA
| | - Wei Li
- Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modelling, Institute for Global Change Studies, Tsinghua University, Beijing 100084, China
| | - Yiming Xu
- School of Grassland Science, Beijing Forestry University, Beijing 100083, China
| | - Reza Mirzaeitalarposhti
- Institute of Crop Science (340i), University of Hohenheim, Fruwirthstraße 20, 70599 Stuttgart, Germany
| | - Heba Elbasiouny
- Agriculture Faculty (Girls), Al-Azhar University, Cairo 11651, Egypt
| | - Igor Savin
- V.V. Dokuchaev Soil Science Institute, Moscow 119017, Russia
- Institute of Environmental Engineering of RUDN University, Moscow 117198, Russia
| | - Dmitry Shchepashchenko
- International Institute for Applied Systems Analysis (IIASA) Schlossplatz 1, 2361 Laxenburg, Austria
- Center for Forest Ecology and Productivity of the Russian Academy of Sciences, Moscow 117997, Russia
- Institute of Ecology and Geography, Siberian Federal University, 79 Svobodny Prospect, 660041 Krasnoyarsk, Russia
| | - Raphael A Viscarra Rossel
- Soil and Landscape Science School of Molecular and Life Sciences, Faculty of Science and Engineering, Curtin University, GPO Box U1987, Perth WA 6845, Australia
| | - Daniel S Goll
- Laboratoire des Sciences du Climat et de l'Environnement, CEA/CNRS/UVSQ/Université Paris Saclay, Gif-sur-Yvette 91990, France
| | - Jinfeng Chang
- International Institute for Applied Systems Analysis (IIASA) Schlossplatz 1, 2361 Laxenburg, Austria
- College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
| | - Benjamin Z Houlton
- Department of Ecology and Evolutionary Biology and Department of Global Development, Cornell University, Ithaca, New York 14853, USA
| | - Huayong Wu
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China
| | - Fei Yang
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China
| | - Xiaoming Feng
- Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
| | - Yongzhe Chen
- Department of Geography, The University of Hong Kong, Hong Kong 999077, China
| | - Yu Liu
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
| | - Shuli Niu
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
| | - Gan-Lin Zhang
- State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China
- College of Advanced Agronomy, University of Chinese Academy of Sciences, Beijing 100049, China
- Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
| |
Collapse
|
11
|
Fu X, Qin J, Ding C, Wei Y, Sun J. Effect of increased pCO 2 and temperature on the phytoplankton community in the coastal of Yellow Sea. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 918:170520. [PMID: 38309353 DOI: 10.1016/j.scitotenv.2024.170520] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/27/2023] [Revised: 01/23/2024] [Accepted: 01/26/2024] [Indexed: 02/05/2024]
Abstract
In order to study the dynamics of marine phytoplankton communities in response to anticipated in temperature and CO2, a shipboard continuous culture experiment (Ecostat) was conducted. The experiment involved simulations under current atmospheric CO2 concentrations (400 ppm) and projected year-2100 CO2 levels (1000 ppm), as well as varying temperature under present (22 °C) versus increased temperature (26 °C) in the Yellow Sea during the summer of 2020. The results showed that both the increased pCO2 and temperature had significant effects on microphytoplankton and picophytoplankton, with the warming effect proving to be more significant. The different responses of various species to acidification and warming and their coupling effect led to the changes in microphytoplankton and picophytoplankton community structure. Elevated temperature and greenhouse treatments promoted the growth of dominant diatoms and Synechococcus, such as Guinardia flaccida and Pseudo-nitzschia delicatissima. This phenomenons widened the ecological niche, and the changes in the growth patterns of dominant species consequently influenced the content of cellular elements. Mantel's analysis further demonstrated that both warming and greenhouse promoted the growth of diatoms and Synechococcus. Projections of marine phytoplankton community trends by the end of the century based on Growth Rate Ratio (GRR), indicated that not only would species with GRR < 1 decrease, but also numerous species with growth rates >1 at elevated pCO2 levels would be ousted from competition. This experiment demonstrates the need to investigate whether extended exposure to increased pCO2 and temperature over more extended time scales would similarly induce shifts in the biological and biogeochemical dynamics of the Yellow Sea.
Collapse
Affiliation(s)
- Xiaoting Fu
- College of Biotechnology, Tianjin University of Science and Technology, Tianjin 300457, China; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China; Research Centre for Indian Ocean Ecosystem, Tianjin University of Science and Technology, Tianjin 300457, China
| | - Jiahui Qin
- Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China; Research Centre for Indian Ocean Ecosystem, Tianjin University of Science and Technology, Tianjin 300457, China
| | - Changling Ding
- Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China; Research Centre for Indian Ocean Ecosystem, Tianjin University of Science and Technology, Tianjin 300457, China.
| | - Yuqiu Wei
- State Key Laboratory of Mariculture Biobreeding and Sustainable Goods, Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao, China
| | - Jun Sun
- Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China; College of Marine Science and Technology, China University of Geosciences (Wuhan), Wuhan 430074, PR China; Research Centre for Indian Ocean Ecosystem, Tianjin University of Science and Technology, Tianjin 300457, China.
| |
Collapse
|
12
|
Folkerts EJ, Oehlert AM, Heuer RM, Nixon S, Stieglitz JD, Grosell M. The role of marine fish-produced carbonates in the oceanic carbon cycle is determined by size, specific gravity, and dissolution rate. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 916:170044. [PMID: 38244625 DOI: 10.1016/j.scitotenv.2024.170044] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/22/2023] [Revised: 01/05/2024] [Accepted: 01/07/2024] [Indexed: 01/22/2024]
Abstract
Rising CO2 emissions have heightened the necessity for increased understanding of Earth's carbon cycle to predict future climates. The involvement of marine planktonic species in the global carbon cycle has been extensively studied, but contributions by marine fish remain poorly characterized. Marine teleost fishes produce carbonate minerals ('ichthyocarbonates') within the lumen of their intestines which are excreted at significant rates on a global scale. However, we have limited understanding of the fate of excreted ichthyocarbonate. We analyzed ichthyocarbonate produced by three different marine teleosts for mol%MgCO3 content, size, specific gravity, and dissolution rate to gain a better understanding of ichthyocarbonate fate. Based on the species examined here, we report that 75 % of ichthyocarbonates are ≤0.91 mm in diameter. Analyses indicate high Mg2+ content across species (22.3 to 32.3 % mol%MgCO3), consistent with previous findings. Furthermore, ichthyocarbonate specific gravity ranged from 1.23 to 1.33 g/cm3, and ichthyocarbonate dissolution rates varied among species as a function of aragonite saturation state. Ichthyocarbonate sinking rates and dissolution depth were estimated for the Atlantic, Pacific, and Indian ocean basins for the three species examined. In the North Atlantic, for example, ~33 % of examined ichthyocarbonates are expected to reach depths exceeding 200 m prior to complete dissolution. The remaining ~66 % of ichthyocarbonate is estimated to dissolve and contribute to shallow water alkalinity budgets. Considering fish biomass and ichthyocarbonate production rates, our results support that marine fishes are critical to the global carbon cycle, contributing to oceanic alkalinity budgets and thereby influencing the ability of the oceans to neutralize atmospheric CO2.
Collapse
Affiliation(s)
- Erik J Folkerts
- Department of Marine Biology and Ecology, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL 33149, United States of America.
| | - Amanda M Oehlert
- Department of Marine Geosciences, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL 33149, United States of America
| | - Rachael M Heuer
- Department of Marine Biology and Ecology, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL 33149, United States of America
| | - Sandy Nixon
- Department of Marine Biology and Ecology, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL 33149, United States of America
| | - John D Stieglitz
- Department of Marine Biology and Ecology, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL 33149, United States of America
| | - Martin Grosell
- Department of Marine Biology and Ecology, Rosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL 33149, United States of America
| |
Collapse
|
13
|
Yang M, Tan L, Batchelor-McAuley C, Compton RG. The solubility product controls the rate of calcite dissolution in pure water and seawater. Chem Sci 2024; 15:2464-2472. [PMID: 38362434 PMCID: PMC10866361 DOI: 10.1039/d3sc04063a] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/04/2023] [Accepted: 01/09/2024] [Indexed: 02/17/2024] Open
Abstract
Quantification of calcite dissolution underpins climate and oceanographic modelling. We report the factors controlling the rate at which individual crystals of calcite dissolved. Clear, generic criteria based on the change of calcite particle dimensions measured microscopically with time are established to indicate if dissolution occurs under kinetic or thermodynamic control. The dissolution of calcite crystals into water is unambiguously revealed to be under thermodynamic control such that the rate at which the crystal dissolved is controlled by the rate of diffusion of ions from a saturated surface layer adjacent to the calcite surface. As such the dissolution rate is controlled by the true stoichiometric solubility product which is inferred from the microscopic measurement as a function of the concentration of NaCl. Comparison with accepted literature values shows that the role of ion pairing at high ionic strengths as in seawater, specifically that of CaCO3 and other ion pairs, exerts a significant influence since these equilibria control the amount of dissolved calcium and carbonate ions in the later of solution immediately adjacent to the solid.
Collapse
Affiliation(s)
- Minjun Yang
- Physical and Theoretical Chemistry Laboratory, Department of Chemistry, University of Oxford South Parks Road Oxford UK
| | - Ling Tan
- Physical and Theoretical Chemistry Laboratory, Department of Chemistry, University of Oxford South Parks Road Oxford UK
| | | | - Richard G Compton
- Physical and Theoretical Chemistry Laboratory, Department of Chemistry, University of Oxford South Parks Road Oxford UK
| |
Collapse
|
14
|
Liu J, Li DW, He X, Liu R, Cheng H, Su C, Chen M, Wang Y, Zhao Z, Xu H, Cheng Z, Wang Z, Pedentchouk N, Lea-Smith DJ, Todd JD, Liu X, Zhao M, Zhang XH. A unique subseafloor microbiosphere in the Mariana Trench driven by episodic sedimentation. MARINE LIFE SCIENCE & TECHNOLOGY 2024; 6:168-181. [PMID: 38433963 PMCID: PMC10902237 DOI: 10.1007/s42995-023-00212-y] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 07/31/2023] [Accepted: 11/23/2023] [Indexed: 03/05/2024]
Abstract
Hadal trenches are characterized by enhanced and infrequent high-rate episodic sedimentation events that likely introduce not only labile organic carbon and key nutrients but also new microbes that significantly alter the subseafloor microbiosphere. Currently, the role of high-rate episodic sedimentation in controlling the composition of the hadal subseafloor microbiosphere is unknown. Here, analyses of carbon isotope composition in a ~ 750 cm long sediment core from the Challenger Deep revealed noncontinuous deposition, with anomalous 14C ages likely caused by seismically driven mass transport and the funneling effect of trench geomorphology. Microbial community composition and diverse enzyme activities in the upper ~ 27 cm differed from those at lower depths, probably due to sudden sediment deposition and differences in redox condition and organic matter availability. At lower depths, microbial population numbers, and composition remained relatively constant, except at some discrete depths with altered enzyme activity and microbial phyla abundance, possibly due to additional sudden sedimentation events of different magnitude. Evidence is provided of a unique role for high-rate episodic sedimentation events in controlling the subsurface microbiosphere in Earth's deepest ocean floor and highlight the need to perform thorough analysis over a large depth range to characterize hadal benthic populations. Such depositional processes are likely crucial in shaping deep-water geochemical environments and thereby the deep subseafloor biosphere. Supplementary Information The online version contains supplementary material available at 10.1007/s42995-023-00212-y.
Collapse
Affiliation(s)
- Jiwen Liu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, 266003 China
- Laboratory for Marine Ecology and Environmental Science, Laoshan Laboratory, Qingdao, 266237 China
- Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003 China
| | - Da-Wei Li
- Laboratory for Marine Ecology and Environmental Science, Laoshan Laboratory, Qingdao, 266237 China
- Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100 China
| | - Xinxin He
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, 266003 China
- Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003 China
| | - Ronghua Liu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, 266003 China
- Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003 China
| | - Haojin Cheng
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, 266003 China
- Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003 China
| | - Chenglong Su
- Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100 China
| | - Mengna Chen
- Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100 China
| | - Yonghong Wang
- Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education/College of Marine Geosciences, Ocean University of China, Qingdao, 266100 China
| | - Zhongsheng Zhao
- Key Laboratory of Physical Oceanography, Ministry of Education/Research Vessel Centre, Ocean University of China, Qingdao, 266100 China
| | - Hanyue Xu
- Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100 China
| | - Zhangyu Cheng
- Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100 China
| | - Zicheng Wang
- Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100 China
| | - Nikolai Pedentchouk
- School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ UK
| | - David J. Lea-Smith
- School of Biological Sciences, University of East Anglia, Norwich, NR4 7TJ UK
| | - Jonathan D. Todd
- School of Biological Sciences, University of East Anglia, Norwich, NR4 7TJ UK
| | - Xiaoshou Liu
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, 266003 China
- Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003 China
| | - Meixun Zhao
- Laboratory for Marine Ecology and Environmental Science, Laoshan Laboratory, Qingdao, 266237 China
- Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100 China
| | - Xiao-Hua Zhang
- Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, 266003 China
- Laboratory for Marine Ecology and Environmental Science, Laoshan Laboratory, Qingdao, 266237 China
- Institute of Evolution and Marine Biodiversity, Ocean University of China, Qingdao, 266003 China
| |
Collapse
|
15
|
Shetye S, Kurian S, Shenoy D, Gauns M, Pratihary A, Shirodkar G, Naik H, Fernandes M, Vidya P, Nandakumar K, Shaikh A. Contrasting patterns in pH variability in the Arabian Sea and Bay of Bengal. ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH INTERNATIONAL 2024; 31:15271-15288. [PMID: 38289549 DOI: 10.1007/s11356-024-31950-w] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/28/2023] [Accepted: 01/05/2024] [Indexed: 02/24/2024]
Abstract
Continuous understanding of the ongoing ocean acidification (OA) is essential for predicting the future impact of OA on marine ecosystems. Here we report the results of open ocean time-series measurements (19 cruises) of seawater pH in total hydrogen ion scale (pHT) and associated parameters in the Arabian Sea (AS) and the Bay of Bengal (BoB). During southwest monsoon (SWM), the pHT within the 30 to 100 m water column shows the maximum difference between the two basins with BoB pHT being lower (up to ~0.39 units) than AS which could be due to freshwater influx from rivers, mixed layer dynamics, and cold-core eddies. However, during Spring inter-monsoon (SIM), the pHT of BoB follows the trend of AS. A contrasting finding is that the lowest pHT occurs at 350 to 500 m in the BoB while it is ~1000 m in the AS. The pHT within the 150 to 1500 m layer of these two basins shows lower values by 0.03 (±0.02) in the BoB as compared to the AS. The possible reasons for the low pHT within the BoB oxygen minimum zone (OMZ) could be due to intrusion of western Pacific water in the BoB, freshwater influx from rivers, variations in OMZ of the two basins, higher temperature (~2°C) within the OMZ of the AS, and denitrification in the AS. The pHT in both the basins (500 to 1000 m) is lower than in the North Atlantic and higher than in the North Pacific waters; however, the pHT in the 200 to 500 m is lower in the BoB than in all these basins. This study highlights the under-saturation of calcium carbonate at very shallow depths (~ 100 m) in the BoB, indicating that the plankton in the BoB are facing a major risk from OA compared to the AS and need further investigation.
Collapse
Affiliation(s)
- Suhas Shetye
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India.
| | - Siby Kurian
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| | - Damodar Shenoy
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| | - Mangesh Gauns
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| | - Anil Pratihary
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| | - Gayatri Shirodkar
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| | - Hema Naik
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| | - Michelle Fernandes
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| | - Pottekkatt Vidya
- National Centre for Polar and Ocean Research (NCPOR), Ministry of Earth Sciences, Headland Sada, Goa, 403 804, India
| | - Kuniyil Nandakumar
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| | - Adnan Shaikh
- CSIR-National Institute of Oceanography, Dona Paula, Goa, 403 004, India
| |
Collapse
|
16
|
Azcárate-García T, Avila C, Figuerola B. Skeletal Mg content in common echinoderm species from Deception and Livingston Islands (South Shetland Islands, Antarctica) in the context of global change. MARINE POLLUTION BULLETIN 2024; 199:115956. [PMID: 38154175 DOI: 10.1016/j.marpolbul.2023.115956] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/14/2023] [Revised: 12/11/2023] [Accepted: 12/16/2023] [Indexed: 12/30/2023]
Abstract
Echinoderms with high levels of magnesium (Mg) in their skeletons may be especially sensitive to ocean acidification, as the solubility of calcite increases with its Mg content. However, other structural characteristics and environmental/biological factors may affect skeletal solubility. To better understand which factors can influence skeletal mineralogy, we analyzed the Mg content of Antarctic echinoderms from Deception Island, an active volcano with reduced pH and relatively warm water temperatures, and Livingston Island. We found significant interclass and inter- and intraspecific differences in the Mg content, with asteroids exhibiting the highest levels, followed by ophiuroids and echinoids. Specimens exposed to hydrothermal fluids showed lower Mg levels, which may indicate local environmental effects. These patterns suggest that environmental factors such as seawater Mg2+/Ca2+ ratio and temperature may influence the Mg content of some echinoderms and affect their susceptibility to future environmental changes.
Collapse
Affiliation(s)
- Tomás Azcárate-García
- Department of Marine Biology and Oceanography, Institute of Marine Sciences (ICM-CSIC), Passeig Maritim de la Barceloneta 37-49, Barcelona 08003, Catalonia, Spain; Department of Evolutionary Biology, Ecology and Environmental Sciences & Biodiversity Research Institute (IRBio), University of Barcelona, Av. Diagonal 643, Barcelona 08028, Catalonia, Spain.
| | - Conxita Avila
- Department of Evolutionary Biology, Ecology and Environmental Sciences & Biodiversity Research Institute (IRBio), University of Barcelona, Av. Diagonal 643, Barcelona 08028, Catalonia, Spain
| | - Blanca Figuerola
- Department of Marine Biology and Oceanography, Institute of Marine Sciences (ICM-CSIC), Passeig Maritim de la Barceloneta 37-49, Barcelona 08003, Catalonia, Spain.
| |
Collapse
|
17
|
Storto A, Yang C. Acceleration of the ocean warming from 1961 to 2022 unveiled by large-ensemble reanalyses. Nat Commun 2024; 15:545. [PMID: 38228601 PMCID: PMC10791650 DOI: 10.1038/s41467-024-44749-7] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/28/2023] [Accepted: 01/03/2024] [Indexed: 01/18/2024] Open
Abstract
Long-term changes in ocean heat content (OHC) represent a fundamental global warming indicator and are mostly caused by anthropogenic climate-altering gas emissions. OHC increases heavily threaten the marine environment, therefore, reconstructing OHC before the well-instrumented period (i.e., before the Argo floats deployment in the mid-2000s) is crucial to understanding the multi-decadal climate change in the ocean. Here, we shed light on ocean warming and its uncertainty for the 1961-2022 period through a large ensemble reanalysis system that spans the major sources of uncertainties. Results indicate a 62-year warming of 0.43 ± 0.08 W m-2, and a statistically significant acceleration rate equal to 0.15 ± 0.04 W m-2 dec-1, locally peaking at high latitudes. The 11.6% of the global ocean area reaches the maximum yearly OHC in 2022, almost doubling any previous year. At the regional scale, major OHC uncertainty is found in the Tropics; at the global scale, the uncertainty represents about 40% and 15% of the OHC variability, respectively before and after the mid-2000s. The uncertainty of regional trends is mostly affected by observation calibration (especially at high latitudes), and sea surface temperature data uncertainty (especially at low latitudes).
Collapse
Affiliation(s)
- Andrea Storto
- Institute of Marine Sciences (ISMAR), National Research Council (CNR), Rome, Italy.
| | - Chunxue Yang
- Institute of Marine Sciences (ISMAR), National Research Council (CNR), Rome, Italy
| |
Collapse
|
18
|
Guo C, Li L, Lin S, Lin X. Species-dependent effects of seawater acidification on alkaline phosphatase activity in dinoflagellates. JOURNAL OF PHYCOLOGY 2023; 59:1347-1352. [PMID: 37844083 DOI: 10.1111/jpy.13398] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/21/2023] [Revised: 05/29/2023] [Accepted: 09/05/2023] [Indexed: 10/18/2023]
Abstract
Increases of atmospheric CO2 cause ocean acidification (OA) and global warming, the latter of which can stratify the water column and impede nutrient supply from deep water. Phosphorus (P) is an essential nutrient for phytoplankton to grow. While dissolved inorganic phosphorus (DIP) is the preferred form of P, phytoplankton have evolved alkaline phosphatase (AP) to utilize dissolved organic phosphorus (DOP) when DIP is deficient. Although the function of AP is known to require pH > 7, how OA affects AP activity and hence the capacity of phytoplankton to utilize DOP is poorly understood. Here, we examined the effects of pH conditions (5.5-11) on AP activity from six species of dinoflagellates, an important group of marine phytoplankton. We observed a general pattern that AP activity declined sharply at pH 5.5, peaked between pH 7 and 8, and dropped at pH > 8. However, our data revealed remarkable interspecific variations in optimal pH and niche breadth of pH. Among the species examined, Fugacium kawagutii and Prorocentrum cordatum had an optimal pH at 8, and Alexandrium pacificum, Amphidinium carterae, Effrenium voratum, and Karenia mikimotoi showed an optimal pH of 7. However, whereas A. pacificum and K. mikimotoi had the broadest pH niche for AP (7-10) and F. kawagutii the second (8-10), Am. carterae, E. voratum, and P. cordatum exhibited a narrow pH range. The response of Am. carterae AP to pH changes was verified using purified AP heterologously expressed in Escherichia coli. These results in concert suggest OA will likely differentially impact the capacity of different phytoplankton species to utilize DOP in the projected more acidified and nutrient-limited future ocean.
Collapse
Affiliation(s)
- Chentao Guo
- State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Science, Xiamen University, Xiamen, Fujian, China
- Provincial Key Laboratory of Cultivation and High-Value Utilization of Marine Organisms, Fisheries Research Institute of Fujian Province, Xiamen, Fujian, China
| | - Ling Li
- State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Science, Xiamen University, Xiamen, Fujian, China
| | - Senjie Lin
- State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Science, Xiamen University, Xiamen, Fujian, China
- Laboratory of Marine Biology and Biotechnology, Qingdao National Laboratory of Marine Science and Technology, Qingdao, Shandong, China
- Department of Marine Sciences, University of Connecticut, Groton, Connecticut, USA
| | - Xin Lin
- State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Science, Xiamen University, Xiamen, Fujian, China
| |
Collapse
|
19
|
Tomasetti SJ, Doall MH, Hallinan BD, Kraemer JR, Gobler CJ. Oyster reefs' control of carbonate chemistry-Implications for oyster reef restoration in estuaries subject to coastal ocean acidification. GLOBAL CHANGE BIOLOGY 2023; 29:6572-6590. [PMID: 37777480 DOI: 10.1111/gcb.16960] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/14/2023] [Revised: 08/31/2023] [Accepted: 09/05/2023] [Indexed: 10/02/2023]
Abstract
Globally, oyster reef restoration is one of the most widely applied coastal restoration interventions. While reefs are focal points of processes tightly linked to the carbonate system such as shell formation and respiration, how these processes alter reef carbonate chemistry relative to the surrounding seawater is unclear. Moreover, coastal systems are increasingly impacted by coastal acidification, which may affect reef carbonate chemistry. Here, we characterized the growth of multiple constructed reefs as well as summer variations in pH and carbonate chemistry of reef-influenced seawater (in the middle of reefs) and ambient seawater (at locations ~50 m outside of reefs) to determine how reef chemistry was altered by the reef community and, in turn, impacts resident oysters. High frequency monitoring across three subtidal constructed reefs revealed reductions of daily mean and minimum pH (by 0.05-0.07 and 0.07-0.12 units, respectively) in seawater overlying reefs relative to ambient seawater (p < .0001). The proportion of pH measurements below 7.5, a threshold shown to negatively impact post-larval oysters, were 1.8×-5.2× higher in reef seawater relative to ambient seawater. Most reef seawater samples (83%) were reduced in total alkalinity relative to ambient seawater samples, suggesting community calcification was a key driver of modified carbonate chemistry. The net metabolic influence of the reef community resulted in reductions of CaCO3 saturation state in 78% of discrete samples, and juvenile oysters placed on reefs exhibited slower shell growth (p < .05) compared to oysters placed outside of reefs. While differences in survival were not detected, reef oysters may benefit from enhanced survival or recruitment at the cost of slowed growth rates. Nevertheless, subtidal restored reef communities modified seawater carbonate chemistry in ways that likely increased oyster vulnerability to acidification, suggesting that carbonate chemistry dynamics warrant consideration when determining site suitability for oyster restoration, particularly under continued climate change.
Collapse
Affiliation(s)
- Stephen J Tomasetti
- Department of Natural Sciences, University of Maryland Eastern Shore, Princess Anne, Maryland, USA
| | - Michael H Doall
- School of Marine and Atmospheric Sciences, Stony Brook University, Southampton, New York, USA
| | - Brendan D Hallinan
- School of Marine and Atmospheric Sciences, Stony Brook University, Southampton, New York, USA
| | - Jeffrey R Kraemer
- School of Marine and Atmospheric Sciences, Stony Brook University, Southampton, New York, USA
| | - Christopher J Gobler
- School of Marine and Atmospheric Sciences, Stony Brook University, Southampton, New York, USA
| |
Collapse
|
20
|
Park GH, Park S, Seok MW, Lee SE, Kim YI, Mo A, Ko YH, Kim H, Kim TW. Acidity in rainwater and airborne suspended particles in the southwestern coast of the East Sea (Sea of Japan): Their potential impact on seawater total alkalinity. MARINE POLLUTION BULLETIN 2023; 197:115742. [PMID: 37976590 DOI: 10.1016/j.marpolbul.2023.115742] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/06/2023] [Revised: 10/28/2023] [Accepted: 10/31/2023] [Indexed: 11/19/2023]
Abstract
Our understanding of the impact of atmospheric acid deposition on marine carbonate system remains limited, largely due to a lack of data regarding acidity present in atmospheric particles and precipitation. Previous research has relied on the electroneutrality-based ion balance method for indirect estimation of atmospheric acidity. In this study, atmospheric samples collected at a coastal site of South Korea were mixed with seawater to measure the change in seawater total alkalinity (ΔTAAPL) associated with atmospheric proton loading. For the precipitation samples, the measured ΔTAAPL and electroneutrality-based estimates showed a significant correlation. However, we did not observe similar results for the atmospheric particle samples. Furthermore, the decrease in oceanic TA due to ΔTAAPL was substantially smaller than that in dissolved inorganic carbon from concurrent nitrogen fertilization. Consequently, the adverse impact of acid deposition on ocean acidification or air-sea exchange of CO2 appears to be insignificant on a short-term scale.
Collapse
Affiliation(s)
- Geun-Ha Park
- Marine Environmental Research Department, Korea Institute of Ocean Science & Technology, Busan 49111, Republic of Korea
| | - Seunghee Park
- Division of Environmental Science and Ecological Engineering, Korea University, Seoul 02841, Republic of Korea
| | - Min-Woo Seok
- Division of Environmental Science and Ecological Engineering, Korea University, Seoul 02841, Republic of Korea
| | - Seon-Eun Lee
- Marine Environmental Research Department, Korea Institute of Ocean Science & Technology, Busan 49111, Republic of Korea
| | - Young-Il Kim
- East Sea Research Institute, Korea Institute of Ocean Science & Technology, Uljin 36315, Republic of Korea
| | - Ahra Mo
- Division of Environmental Science and Ecological Engineering, Korea University, Seoul 02841, Republic of Korea
| | - Young Ho Ko
- OJEong Resilience Institute, Korea University, Seoul 02841, Republic of Korea
| | - Haryun Kim
- East Sea Research Institute, Korea Institute of Ocean Science & Technology, Uljin 36315, Republic of Korea
| | - Tae-Wook Kim
- Division of Environmental Science and Ecological Engineering, Korea University, Seoul 02841, Republic of Korea; OJEong Resilience Institute, Korea University, Seoul 02841, Republic of Korea.
| |
Collapse
|
21
|
Xu X, Zhao H, Zang K, Zheng N, Huo C, Deng X, Wang J. Contrasting effects of temperature and biological processes on aragonite saturation state at the A4HDYD station in the North Yellow Sea. MARINE ENVIRONMENTAL RESEARCH 2023; 192:106187. [PMID: 37827965 DOI: 10.1016/j.marenvres.2023.106187] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/08/2023] [Revised: 08/31/2023] [Accepted: 09/15/2023] [Indexed: 10/14/2023]
Abstract
To explore the effects of seawater temperature and biological processes on aragonite saturation state (Ωarag), eight field surveys were conducted from December 2014 to November 2015 at A4HDYD station in the North Yellow Sea (NYS). Low regional yearly initial values of seawater Ωarag (1.26-1.76) were obtained in winter due to low seawater temperature. During spring to early autumn, surface-water Ωarag increased from 2.02 to 3.47 for the increasing seawater temperature and biological production, whereas bottom-water Ωarag remained as low as 1.44-1.79 due to low seawater temperature, net community respiration and the influence of the North Yellow Sea Cold Water Mass (NYSCWM). Following the collapse of stratification in late autumn, the seawater was well-mixed with an average Ωarag of 2.17. The annual cycle of seawater temperature dominated the seasonal variations of Ωarag, counteracted by biological production increasing Ωarag of 0.49 in surface water in March and strengthened by net community respiration decreasing Ωarag of 0.11-0.41 below the pycnocline during summer and autumn. It is, therefore, mid-to-high latitude coastal areas impacted by human activities are likely subject to ocean acidification due to the combined effects of low seawater temperature and net community respiration.
Collapse
Affiliation(s)
- Xuemei Xu
- State Environmental Protection Key Laboratory of Coastal Ecosystem, National Marine Environmental Monitoring Center, Dalian 116023, China
| | - Huade Zhao
- State Environmental Protection Key Laboratory of Coastal Ecosystem, National Marine Environmental Monitoring Center, Dalian 116023, China
| | - Kunpeng Zang
- College of Environment, Zhejiang University of Technology, Hangzhou 310014, China
| | - Nan Zheng
- State Environmental Protection Key Laboratory of Coastal Ecosystem, National Marine Environmental Monitoring Center, Dalian 116023, China
| | - Cheng Huo
- State Environmental Protection Key Laboratory of Coastal Ecosystem, National Marine Environmental Monitoring Center, Dalian 116023, China
| | - Xue Deng
- State Environmental Protection Key Laboratory of Coastal Ecosystem, National Marine Environmental Monitoring Center, Dalian 116023, China
| | - Juying Wang
- State Environmental Protection Key Laboratory of Coastal Ecosystem, National Marine Environmental Monitoring Center, Dalian 116023, China.
| |
Collapse
|
22
|
Zhang J, Yang Q, Yue W, Yang B, Zhou W, Chen L, Huang X, Zhang W, Dong J, Ling J. Seagrass Thalassia hemprichii and associated bacteria co-response to the synergistic stress of ocean warming and ocean acidification. ENVIRONMENTAL RESEARCH 2023; 236:116658. [PMID: 37454799 DOI: 10.1016/j.envres.2023.116658] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/11/2023] [Revised: 06/07/2023] [Accepted: 07/11/2023] [Indexed: 07/18/2023]
Abstract
Seagrass meadows play vital ecological roles in the marine ecosystem. Global climate change poses considerable threats to seagrass survival. However, it is unclear how seagrass and its associated bacteria will respond under future complex climate change scenarios. This study explored the effects of ocean warming (+2 °C) and ocean acidification (-0.4 units) on seagrass physiological indexes and bacterial communities (sediment and rhizosphere bacteria) of the seagrass Thalassia hemprichii during an experimental exposure of 30 days. Results demonstrated that the synergistic effect of ocean warming and ocean acidification differed from that of one single factor on seagrass and the associated bacterial community. The seagrass showed a weak resistance to ocean warming and ocean acidification, which manifested through the increase in the activity of typical oxidoreductase enzymes. Moreover, the synergistic effect of ocean warming and ocean acidification caused a significant decrease in seagrass's chlorophyll content. Although the bacterial community diversity exhibited higher resistance to ocean warming and ocean acidification, further bacterial functional analysis revealed the synergistic effect of ocean warming and ocean acidification led to significant increases in SOX-related genes abundance which potentially supported the seagrass in resisting climate stress by producing sulfates and oxidizing hydrogen sulfide. More stable bacterial communities were detected in the seagrass rhizosphere under combined ocean warming and ocean acidification. While for one single environmental stress, simpler networks were detected in the rhizosphere. In addition, the observed significant correlations between several modules of the bacterial community and the physiological indexes of the seagrass indicate the possible intimate interaction between seagrass and bacteria under ocean warming and ocean acidification. This study extends our understanding regarding the role of seagrass associated bacterial communities and sheds light on both the prediction and preservation of the seagrass meadow ecosystems in response to global climate change.
Collapse
Affiliation(s)
- Jian Zhang
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; Key Laboratory of Tropical Marine Biotechnology of Hainan Province, Sanya Institute of Ocean Eco-Environmental Engineering, Sanya, 572000, PR China; Guangdong Provincial Observation and Research Station for Coastal Upwelling Ecosystem, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Shantou, 515041, PR China; Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya, 572000, PR China
| | - Qingsong Yang
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; Key Laboratory of Tropical Marine Biotechnology of Hainan Province, Sanya Institute of Ocean Eco-Environmental Engineering, Sanya, 572000, PR China; Guangdong Provincial Observation and Research Station for Coastal Upwelling Ecosystem, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Shantou, 515041, PR China; Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya, 572000, PR China
| | - Weizhong Yue
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya, 572000, PR China
| | - Bing Yang
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; University of Chinese Academy of Sciences, Beijing, 100049, PR China
| | - Weiguo Zhou
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; Key Laboratory of Tropical Marine Biotechnology of Hainan Province, Sanya Institute of Ocean Eco-Environmental Engineering, Sanya, 572000, PR China; Guangdong Provincial Observation and Research Station for Coastal Upwelling Ecosystem, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Shantou, 515041, PR China; Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya, 572000, PR China
| | - Luxiang Chen
- College of Marine Sciences, South China Agricultural University, Guangzhou, Guangdong, 510642, PR China
| | - Xiaofang Huang
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; Key Laboratory of Tropical Marine Biotechnology of Hainan Province, Sanya Institute of Ocean Eco-Environmental Engineering, Sanya, 572000, PR China; Guangdong Provincial Observation and Research Station for Coastal Upwelling Ecosystem, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Shantou, 515041, PR China; University of Chinese Academy of Sciences, Beijing, 100049, PR China
| | - Wenqian Zhang
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; Key Laboratory of Tropical Marine Biotechnology of Hainan Province, Sanya Institute of Ocean Eco-Environmental Engineering, Sanya, 572000, PR China; Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya, 572000, PR China
| | - Junde Dong
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; Key Laboratory of Tropical Marine Biotechnology of Hainan Province, Sanya Institute of Ocean Eco-Environmental Engineering, Sanya, 572000, PR China; Guangdong Provincial Observation and Research Station for Coastal Upwelling Ecosystem, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Shantou, 515041, PR China; Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya, 572000, PR China.
| | - Juan Ling
- CAS Key Laboratory of Tropical Marine Bio-Resources and Ecology, Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, PR China; Key Laboratory of Tropical Marine Biotechnology of Hainan Province, Sanya Institute of Ocean Eco-Environmental Engineering, Sanya, 572000, PR China; Guangdong Provincial Observation and Research Station for Coastal Upwelling Ecosystem, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Shantou, 515041, PR China; Tropical Marine Biological Research Station in Hainan, Chinese Academy of Sciences, Sanya, 572000, PR China.
| |
Collapse
|
23
|
Chen WH, Armstrong E, Dillingham PW, Moratti SC, Ennis C, McGraw CM. Dual-Lifetime Referencing ( t-DLR) Optical Fiber Fluorescent pH Sensor for Microenvironments. SENSORS (BASEL, SWITZERLAND) 2023; 23:8865. [PMID: 37960564 PMCID: PMC10650387 DOI: 10.3390/s23218865] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/16/2023] [Revised: 10/24/2023] [Accepted: 10/27/2023] [Indexed: 11/15/2023]
Abstract
The pH behavior in the μm to cm thick diffusion boundary layer (DBL) surrounding many aquatic species is dependent on light-controlled metabolic activities. This DBL microenvironment exhibits different pH behavior to bulk seawater, which can reduce the exposure of calcifying species to ocean acidification conditions. A low-cost time-domain dual-lifetime referencing (t-DLR) interrogation system and an optical fiber fluorescent pH sensor were developed for pH measurements in the DBL interface. The pH sensor utilized dual-layer sol-gel coatings of pH-sensitive iminocoumarin and pH-insensitive Ru(dpp)3-PAN. The sensor has a dynamic range of 7.41 (±0.20) to 9.42 ± 0.23 pH units (95% CI, T = 20 °C, S = 35), a response time (t90) of 29 to 100 s, and minimal salinity dependency. The pH sensor has a precision of approximately 0.02 pHT units, which meets the Global Ocean Acidification Observing Network (GOA-ON) "weather" measurement quality guideline. The suitability of the t-DLR optical fiber pH sensor was demonstrated through real-time measurements in the DBL of green seaweed Ulva sp. This research highlights the practicability of optical fiber pH sensors by demonstrating real-time pH measurements of metabolic-induced pH changes.
Collapse
Affiliation(s)
- Wan-Har Chen
- Department of Chemistry, University of Otago, Dunedin 9054, New Zealand; (W.-H.C.); (S.C.M.); (C.E.)
| | - Evelyn Armstrong
- NIWA/University of Otago Centre for Oceanography, Department of Marine Science, University of Otago, Dunedin 9054, New Zealand;
| | - Peter W. Dillingham
- Department of Mathematics and Statistics, University of Otago, Dunedin 9054, New Zealand;
- Coastal People Southern Skies Centre of Research Excellence, University of Otago, Dunedin 9054, New Zealand
| | - Stephen C. Moratti
- Department of Chemistry, University of Otago, Dunedin 9054, New Zealand; (W.-H.C.); (S.C.M.); (C.E.)
| | - Courtney Ennis
- Department of Chemistry, University of Otago, Dunedin 9054, New Zealand; (W.-H.C.); (S.C.M.); (C.E.)
| | - Christina M. McGraw
- Department of Chemistry, University of Otago, Dunedin 9054, New Zealand; (W.-H.C.); (S.C.M.); (C.E.)
| |
Collapse
|
24
|
Korabik AR, Winquist T, Grosholz ED, Hollarsmith JA. Examining the reproductive success of bull kelp (Nereocystis luetkeana, Phaeophyceae, Laminariales) in climate change conditions. JOURNAL OF PHYCOLOGY 2023; 59:989-1004. [PMID: 37540062 DOI: 10.1111/jpy.13368] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/09/2023] [Revised: 05/23/2023] [Accepted: 05/29/2023] [Indexed: 08/05/2023]
Abstract
Climate change is affecting marine ecosystems in many ways, including raising temperatures and leading to ocean acidification. From 2014 to 2016, an extensive marine heat wave extended along the west coast of North America and had devastating effects on numerous species, including bull kelp (Nereocystis luetkeana). Bull kelp is an important foundation species in coastal ecosystems and can be affected by marine heat waves and ocean acidification; however, the impacts have not been investigated on sensitive early life stages. To determine the effects of changing temperatures and carbonate levels on Northern California's bull kelp populations, we collected sporophylls from mature bull kelp individuals in Point Arena, CA. At the Bodega Marine Laboratory, we released spores from field-collected bull kelp, and cultured microscopic gametophytes in a common garden experiment with a fully factorial design crossing modern conditions (11.63 ± 0.54°C and pH 7.93 ± 0.26) with observed extreme climate conditions (15.56 ± 0.83°C and 7.64 ± 0.32 pH). Our results indicated that both increased temperature and decreased pH influenced growth and egg production of bull kelp microscopic stages. Increased temperature resulted in decreased gametophyte survival and offspring production. In contrast, decreased pH had less of an effect but resulted in increased gametophyte survival and offspring production. Additionally, increased temperature significantly impacted reproductive timing by causing female gametophytes to produce offspring earlier than under ambient temperature conditions. Our findings can inform better predictions of the impacts of climate change on coastal ecosystems and provide key insights into environmental dynamics regulating the bull kelp lifecycle.
Collapse
Affiliation(s)
- Angela R Korabik
- Department of Environmental Science and Policy, University of California Davis, Davis, California, USA
| | - Tallulah Winquist
- Department of Biology, San Diego State University, San Diego, California, USA
| | - Edwin D Grosholz
- Department of Environmental Science and Policy, University of California Davis, Davis, California, USA
| | | |
Collapse
|
25
|
Cornwall CE, Comeau S, Donner SD, Perry C, Dunne J, van Hooidonk R, Ryan JS, Logan CA. Coral adaptive capacity insufficient to halt global transition of coral reefs into net erosion under climate change. GLOBAL CHANGE BIOLOGY 2023; 29:3010-3018. [PMID: 36943744 DOI: 10.1111/gcb.16647] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/21/2022] [Revised: 02/04/2023] [Accepted: 02/07/2023] [Indexed: 05/03/2023]
Abstract
Projecting the effects of climate change on net reef calcium carbonate production is critical to understanding the future impacts on ecosystem function, but prior estimates have not included corals' natural adaptive capacity to such change. Here we estimate how the ability of symbionts to evolve tolerance to heat stress, or for coral hosts to shuffle to favourable symbionts, and their combination, may influence responses to the combined impacts of ocean warming and acidification under three representative concentration pathway (RCP) emissions scenarios (RCP2.6, RCP4.5 and RCP8.5). We show that symbiont evolution and shuffling, both individually and when combined, favours persistent positive net reef calcium carbonate production. However, our projections of future net calcium carbonate production (NCCP) under climate change vary both spatially and by RCP. For example, 19%-35% of modelled coral reefs are still projected to have net positive NCCP by 2050 if symbionts can evolve increased thermal tolerance, depending on the RCP. Without symbiont adaptive capacity, the number of coral reefs with positive NCCP drops to 9%-13% by 2050. Accounting for both symbiont evolution and shuffling, we project median positive NCPP of coral reefs will still occur under low greenhouse emissions (RCP2.6) in the Indian Ocean, and even under moderate emissions (RCP4.5) in the Pacific Ocean. However, adaptive capacity will be insufficient to halt the transition of coral reefs globally into erosion by 2050 under severe emissions scenarios (RCP8.5).
Collapse
Affiliation(s)
- Christopher Edward Cornwall
- School of Biological Sciences and Coastal People Southern Skies, Victoria University of Wellington, Wellington, New Zealand
| | - Steeve Comeau
- Laboratoire d'Océanographie de Villefranche, CNRS-INSU, Sorbonne Université, Villefranche-sur-Mer, France
| | - Simon D Donner
- Institute of Resources, Environment and Sustainability / Department of Geography, University of British Columbia, Vancouver, British Columbia, Canada
| | - Chris Perry
- Geography, Faculty of Environment, Science and Economy, University of Exeter, Exeter, UK
| | - John Dunne
- NOAA/OAR Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey, USA
| | - Ruben van Hooidonk
- Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric and Earth Science, University of Miami, Miami, Florida, USA
- Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration, Miami, Florida, USA
| | - James S Ryan
- Department of Marine Science, California State University, Monterey Bay, California, USA
| | - Cheryl A Logan
- Department of Marine Science, California State University, Monterey Bay, California, USA
| |
Collapse
|
26
|
Huang Y, Fassbender A, Bushinsky S. Biogenic carbon pool production maintains the Southern Ocean carbon sink. Proc Natl Acad Sci U S A 2023; 120:e2217909120. [PMID: 37099629 PMCID: PMC10160987 DOI: 10.1073/pnas.2217909120] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/04/2022] [Accepted: 03/29/2023] [Indexed: 04/28/2023] Open
Abstract
Through biological activity, marine dissolved inorganic carbon (DIC) is transformed into different types of biogenic carbon available for export to the ocean interior, including particulate organic carbon (POC), dissolved organic carbon (DOC), and particulate inorganic carbon (PIC). Each biogenic carbon pool has a different export efficiency that impacts the vertical ocean carbon gradient and drives natural air-sea carbon dioxide gas (CO2) exchange. In the Southern Ocean (SO), which presently accounts for ~40% of the anthropogenic ocean carbon sink, it is unclear how the production of each biogenic carbon pool contributes to the contemporary air-sea CO2 exchange. Based on 107 independent observations of the seasonal cycle from 63 biogeochemical profiling floats, we provide the basin-scale estimate of distinct biogenic carbon pool production. We find significant meridional variability with enhanced POC production in the subantarctic and polar Antarctic sectors and enhanced DOC production in the subtropical and sea-ice-dominated sectors. PIC production peaks between 47°S and 57°S near the "great calcite belt." Relative to an abiotic SO, organic carbon production enhances CO2 uptake by 2.80 ± 0.28 Pg C y-1, while PIC production diminishes CO2 uptake by 0.27 ± 0.21 Pg C y-1. Without organic carbon production, the SO would be a CO2 source to the atmosphere. Our findings emphasize the importance of DOC and PIC production, in addition to the well-recognized role of POC production, in shaping the influence of carbon export on air-sea CO2 exchange.
Collapse
Affiliation(s)
- Yibin Huang
- Department of Ocean Sciences, University of California, Santa Cruz, CA95064
- National Oceanic and Atmospheric Administration, Pacific Marine Environmental Laboratory, Seattle, WA98115
| | - Andrea J. Fassbender
- Department of Ocean Sciences, University of California, Santa Cruz, CA95064
- National Oceanic and Atmospheric Administration, Pacific Marine Environmental Laboratory, Seattle, WA98115
| | - Seth M. Bushinsky
- Department of Oceanography, University of Hawaii at Mānoa, Honolulu, HA96822
| |
Collapse
|
27
|
Paredes-Molina FJ, Chaparro OR, Navarro JM, Cubillos VM, Montory JA, Pechenik JA. Embryonic encapsulated development of the gastropod Acanthina monodon is impacted by future environmental changes of temperature and pCO 2. MARINE ENVIRONMENTAL RESEARCH 2023; 187:105971. [PMID: 37004497 DOI: 10.1016/j.marenvres.2023.105971] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/25/2022] [Revised: 03/15/2023] [Accepted: 03/28/2023] [Indexed: 06/19/2023]
Abstract
Egg capsules of the gastropod Acanthina monodon were maintained during the entire period of encapsulated development at three temperatures (10, 15, 20 °C) and two pCO2 levels (400, 1200 μatm). Embryos per capsule, size at hatching, time to hatching, embryonic metabolic rates, and the resistance of juveniles to shell breakage were quantified. No embryos maintained at 20 °C developed to hatching. The combination of temperature and pCO2 levels had synergistic effects on hatching time and developmental success, antagonistic effects on number of hatchlings per capsule, resistance to juvenile shell cracking and metabolism, and additive effect on hatching size. Juveniles hatched significantly sooner at 15 °C, independent of the pCO2 level that they had been exposed to, while individuals hatched at significantly smaller sizes if they had been held under 15 °C/1200 μatm rather than at 10 °C/low pCO2. Embryos held at the higher pCO2 had a significantly greater percentage of abnormalities. For capsules maintained at low pCO2 and 15 °C, emerging juveniles had less resistance to shell breakage. Embryonic metabolism was significantly higher at 15 °C than at 10 °C, independent of pCO2 level. The lower metabolism occurred in embryos maintained at the higher pCO2 level. Thus, in this study, temperature was the factor that had the greatest effect on the encapsulated development of A. monodon, increasing the metabolism of the embryos and consequently accelerating development, which was expressed in a shorter intracapsular development time, but with smaller individuals at hatching and a lower resistance of their shells to breakage. On the other hand, the high pCO2 level suppressed metabolism, prolonged intracapsular development, and promoted more incomplete development of the embryos. However, the combination of the two factors can mitigate--to some extent--the adverse effects of both incomplete development and lower resistance to shell breakage.
Collapse
Affiliation(s)
- F J Paredes-Molina
- Instituto de Ciencias Marinas y Limnologicas, Universidad Austral de Chile, Valdivia, Chile.
| | - O R Chaparro
- Instituto de Ciencias Marinas y Limnologicas, Universidad Austral de Chile, Valdivia, Chile
| | - J M Navarro
- Instituto de Ciencias Marinas y Limnologicas, Universidad Austral de Chile, Valdivia, Chile; Centro FONDAP de Investigación de Ecosistemas Marinos de Altas Latitudes (IDEAL), Valdivia, Chile
| | - V M Cubillos
- Instituto de Ciencias Marinas y Limnologicas, Universidad Austral de Chile, Valdivia, Chile
| | - J A Montory
- Centro i∼mar, Universidad De Los Lagos, Casilla 557, Puerto Montt, Chile
| | - J A Pechenik
- Biology Department, Tufts University, Medford, MA, 02155, USA
| |
Collapse
|
28
|
Greatorex R, Knights AM. Differential effects of ocean acidification and warming on biological functioning of a predator and prey species may alter future trophic interactions. MARINE ENVIRONMENTAL RESEARCH 2023; 186:105903. [PMID: 36841179 DOI: 10.1016/j.marenvres.2023.105903] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/21/2022] [Revised: 01/19/2023] [Accepted: 01/29/2023] [Indexed: 06/18/2023]
Abstract
Independently, ocean warming (OW) and acidification (OA) from increased anthropogenic atmospheric carbon dioxide are argued to be two of the greatest threats to marine organisms. Increasingly, their interaction (ocean acidification and warming, OAW) is shown to have wide-ranging consequences to biological functioning, population and community structure, species interactions and ecosystem service provision. Here, using a multi-trophic experiment, we tested the effects of future OAW scenarios on two widespread intertidal species, the blue mussel Mytilus edulis and its predator Nucella lapillus. Results indicate negative consequences of OAW on the growth, feeding and metabolic rate of M. edulis and heightened predation risk. In contrast, Nucella growth and metabolism was unaffected and feeding increased under OAW but declined under OW suggesting OA may offset warming consequences. Should this differential response between the two species to OAW, and specifically greater physiological costs to the prey than its predator come to fruition in the nature, fundamental change in ecosystem structure and functioning could be expected as trophic interactions become disrupted.
Collapse
Affiliation(s)
- Rebecca Greatorex
- School of Biological and Marine Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK
| | - Antony M Knights
- School of Biological and Marine Sciences, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK.
| |
Collapse
|
29
|
Chen Y, Wang X, Sui Q, Chang G, Sun X, Zhu L, Chen B, Qu K, Xia B. Charge-dependent negative effects of polystyrene nanoplastics on Oryzias melastigma under ocean acidification conditions. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 865:161248. [PMID: 36587669 DOI: 10.1016/j.scitotenv.2022.161248] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/27/2022] [Revised: 12/22/2022] [Accepted: 12/24/2022] [Indexed: 06/17/2023]
Abstract
Marine nanoplastics (NPs) have attracted increasing global attentions because of their detrimental effects on marine environments. A co-existing major environmental concern is ocean acidification (OA). However, the effects of differentially charged NPs on marine organisms under OA conditions are poorly understood. We therefore investigated the effects of OA on the embryotoxicity of both positively and negatively charged polystyrene (PS) NPs to marine medaka (Oryzias melastigma). Positively charged PS-NH2 exhibited slighter aggregation under normal conditions and more aggregation under OA conditions than negatively charged PS-COOH. According to the integrated biomarker approach, OA reversed the toxicity of positively and negatively charged NPs towards embryos. Importantly, at environmental relevant concentrations, both types of PS-NPs could enter the embryos through chorionic pores and then transfer to the larvae. OA reversed the internalization of PS-NH2 and PS-COOH in O. melastigma. Overall, the reversed toxicity of PS-NH2 and PS-COOH associated with OA could be caused by the reversed bioavailability of NPs to O. melastigma, which was attributed to altered aggregation of the NPs in acidified seawater. This finding demonstrates the charge-dependent toxicity of NPs to marine fish and provides new insights into the potential hazard of NPs to marine environments under OA conditions that could be encountered in the near future.
Collapse
Affiliation(s)
- Yufei Chen
- Qingdao University of Science and Technology, Qingdao 266042, China; Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
| | - Xia Wang
- Qingdao University of Science and Technology, Qingdao 266042, China
| | - Qi Sui
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
| | - Guozhu Chang
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
| | - Xuemei Sun
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
| | - Lin Zhu
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
| | - Bijuan Chen
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
| | - Keming Qu
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
| | - Bin Xia
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China; Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China.
| |
Collapse
|
30
|
Jiang LQ, Kozyr A, Relph JM, Ronje EI, Kamb L, Burger E, Myer J, Nguyen L, Arzayus KM, Boyer T, Cross S, Garcia H, Hogan P, Larsen K, Parsons AR. The Ocean Carbon and Acidification Data System. Sci Data 2023; 10:136. [PMID: 36922515 PMCID: PMC10017681 DOI: 10.1038/s41597-023-02042-0] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/03/2022] [Accepted: 02/23/2023] [Indexed: 03/17/2023] Open
Abstract
The Ocean Carbon and Acidification Data System (OCADS) is a data management system at the National Oceanic and Atmospheric Administration (NOAA) National Centers for Environmental Information (NCEI). It manages a wide range of ocean carbon and acidification data, including chemical, physical, and biological observations collected from research vessels, ships of opportunity, and uncrewed platforms, as well as laboratory experiment results, and model outputs. Additionally, OCADS serves as a repository for related Global Ocean Observing System (GOOS) biogeochemistry Essential Ocean Variables (EOVs), e.g., oxygen, nutrients, transient tracers, and stable isotopes. OCADS endeavors to be one of the world's leading providers of ocean carbon and acidification data, information, products, and services. To provide the best data management services to the ocean carbon and acidification research community, OCADS prioritizes adopting a customer-centric approach and gathering knowledge and expertise from the research community to improve its data management practices. OCADS aims to make all ocean carbon and acidification data accessible via a single portal, and welcomes submissions from around the world: https://www.ncei.noaa.gov/products/ocean-carbon-acidification-data-system/.
Collapse
Affiliation(s)
- Li-Qing Jiang
- Cooperative Institute for Satellite Earth System Studies, Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland, 20740, USA.
- NOAA/NESDIS National Centers for Environmental Information, Silver Spring, Maryland, 20910, USA.
| | - Alex Kozyr
- Cooperative Institute for Satellite Earth System Studies, Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland, 20740, USA
- NOAA/NESDIS National Centers for Environmental Information, Silver Spring, Maryland, 20910, USA
| | - John M Relph
- NOAA/NESDIS National Centers for Environmental Information, Silver Spring, Maryland, 20910, USA
| | - Errol I Ronje
- NOAA/NESDIS National Centers for Environmental Information, Stennis Space Center, Mississippi, 39529, USA
| | - Linus Kamb
- NOAA/OAR Pacific Marine Environmental Laboratory, Seattle, Washington, 98115, USA
| | - Eugene Burger
- NOAA/OAR Pacific Marine Environmental Laboratory, Seattle, Washington, 98115, USA
| | - Jonathan Myer
- NOAA/NESDIS National Centers for Environmental Information, Asheville, North Carolina, 28801, USA
| | - Liem Nguyen
- Department of Computer Science, University of Maryland, College Park, Maryland, 20740, USA
| | - Krisa M Arzayus
- NOAA/NOS Integrated Ocean Observing System, Silver Spring, Maryland, 20910, USA
| | - Tim Boyer
- NOAA/NESDIS National Centers for Environmental Information, Silver Spring, Maryland, 20910, USA
| | - Scott Cross
- NOAA/NESDIS National Centers for Environmental Information, Charleston, South Carolina, 29412, USA
| | - Hernan Garcia
- NOAA/NESDIS National Centers for Environmental Information, Silver Spring, Maryland, 20910, USA
| | - Patrick Hogan
- NOAA/NESDIS National Centers for Environmental Information, Stennis Space Center, Mississippi, 39529, USA
| | - Kirsten Larsen
- NOAA/NESDIS National Centers for Environmental Information, Stennis Space Center, Mississippi, 39529, USA
| | - A Rost Parsons
- NOAA/NESDIS National Centers for Environmental Information, Stennis Space Center, Mississippi, 39529, USA
| |
Collapse
|
31
|
Zhang W, He L, Pan J, Zhou Y, Ge R, Li S, Shi Y, Chen X, Chu Y. Response of Juvenile Saccharina japonica to the Combined Stressors of Elevated pCO 2 and Excess Copper. PLANTS (BASEL, SWITZERLAND) 2023; 12:1140. [PMID: 36903998 PMCID: PMC10005686 DOI: 10.3390/plants12051140] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/03/2023] [Revised: 02/19/2023] [Accepted: 02/27/2023] [Indexed: 06/18/2023]
Abstract
Coastal macroalgae may be subjected to global and local environmental stressors, such as ocean acidification and heavy-metal pollution. We investigated the growth, photosynthetic characteristics, and biochemical compositions of juvenile sporophytes of Saccharina japonica cultivated at two pCO2 levels (400 and 1000 ppmv) and four copper concentrations (natural seawater, control; 0.2 μM, low level; 0.5 μM, medium level; and 1 μM, high level) to better understand how macroalgae respond to ongoing environmental changes. The results showed that the responses of juvenile S. japonica to copper concentrations depended on the pCO2 level. Under the 400 ppmv condition, medium and high copper concentrations significantly decreased the relative growth rate (RGR) and non-photochemical quenching (NPQ) but increased the relative electron transfer rate (rETR) and chlorophyll a (Chl a), chlorophyll c (Chl c), carotenoid (Car), and soluble carbohydrate contents. At 1000 ppmv, however, none of the parameters had significant differences between the different copper concentrations. Our data suggest that excess copper may inhibit the growth of juvenile sporophytes of S. japonica, but this negative effect could be alleviated by CO2-induced ocean acidification.
Collapse
Affiliation(s)
- Wenze Zhang
- College of Marine Sciences, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Key Laboratory of Marine Biotechnology of Fujian Province, Institute of Oceanology, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Department of Aquaculture and Aquatic Sciences, Kunsan National University, Gunsan 54150, Republic of Korea
| | - Lianghua He
- College of Marine Sciences, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Key Laboratory of Marine Biotechnology of Fujian Province, Institute of Oceanology, Fujian Agriculture and Forestry University, Fuzhou 350002, China
| | - Jiangqi Pan
- College of Marine Sciences, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Key Laboratory of Marine Biotechnology of Fujian Province, Institute of Oceanology, Fujian Agriculture and Forestry University, Fuzhou 350002, China
| | - Yuhong Zhou
- College of Marine Sciences, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Key Laboratory of Marine Biotechnology of Fujian Province, Institute of Oceanology, Fujian Agriculture and Forestry University, Fuzhou 350002, China
| | - Ruxiang Ge
- College of Marine Sciences, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Key Laboratory of Marine Biotechnology of Fujian Province, Institute of Oceanology, Fujian Agriculture and Forestry University, Fuzhou 350002, China
| | - Sufang Li
- Laboratoire Génie des Procédés et Matériaux (LGPM), CentraleSupélec, Université Paris-Saclay, 91190 Gif-sur-Yvette, France
| | - Yunyun Shi
- College of Marine Sciences, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Key Laboratory of Marine Biotechnology of Fujian Province, Institute of Oceanology, Fujian Agriculture and Forestry University, Fuzhou 350002, China
| | - Xinhua Chen
- College of Marine Sciences, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Key Laboratory of Marine Biotechnology of Fujian Province, Institute of Oceanology, Fujian Agriculture and Forestry University, Fuzhou 350002, China
| | - Yaoyao Chu
- College of Marine Sciences, Fujian Agriculture and Forestry University, Fuzhou 350002, China
- Key Laboratory of Marine Biotechnology of Fujian Province, Institute of Oceanology, Fujian Agriculture and Forestry University, Fuzhou 350002, China
| |
Collapse
|
32
|
Holcová K, Scheiner F. An experimental study on post-mortem dissolution and overgrowth processes affecting coccolith assemblages: A rapid and complex process. GEOBIOLOGY 2023; 21:193-209. [PMID: 36218003 DOI: 10.1111/gbi.12528] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/25/2022] [Revised: 09/10/2022] [Accepted: 09/19/2022] [Indexed: 06/16/2023]
Abstract
Coccolith dissolution together with post-mortem morphological features are immensely important phenomena that can affect assemblage compositions, complicate taxonomic identification as well as provide valuable palaeoenvironmental insights. This study summarizes the effects of pH oscillations on post-mortem coccolith morphologies and the abundances and compositions of calcareous nannoplankton assemblages in three distinct types of material-(i) Cretaceous chalk, (ii) Miocene marls, and (iii) late Holocene calcareous ooze. Two independent experimental runs within a semi-enclosed system setting were realized to observe assemblage alterations. One experiment was realized with the presence of bacteria and, in contrast, the second one inhibited their potential effect on the studied system. The pH was gradually decreased within the range of 8.3-6.4 using a reaction of CO2 with H2 O forming weak carbonic acid (H2 CO3 ), thereby affecting [ CO 3 2 - ]. Further, a subsequent overgrowth study was carried out during spontaneous degassing accompanied by a gradual pH rise. The experiment revealed that the process and intensity of coccolith corrosion and subsequent overgrowth build-ups are influenced by a plethora of different factors such as (i) pH and associated seawater chemistry, (ii) mineral composition of the sediment, (iii) the presence of coccoliths within a protective substrate (faecal pellets, pores, pits), and (iv) the presence/absence of bacteria. Nannoplankton assemblages with corroded coccoliths or with coccoliths with overgrowth build-ups showed that the observed relative abundances of taxa experienced alteration from the original compositions. Additionally, extreme pH oscillations may result in enhanced morphological changes that make coccoliths unidentifiable structures, and might even evoke the absence of coccoliths in the fossil record.
Collapse
Affiliation(s)
- Katarína Holcová
- Institute of Geology and Palaeontology, Charles University, Praha, Czech Republic
| | - Filip Scheiner
- Institute of Geology and Palaeontology, Charles University, Praha, Czech Republic
- Institute of Geology of the Czech Academy of Sciences, Praha, Czech Republic
| |
Collapse
|
33
|
Ziveri P, Gray WR, Anglada-Ortiz G, Manno C, Grelaud M, Incarbona A, Rae JWB, Subhas AV, Pallacks S, White A, Adkins JF, Berelson W. Pelagic calcium carbonate production and shallow dissolution in the North Pacific Ocean. Nat Commun 2023; 14:805. [PMID: 36808154 PMCID: PMC9941586 DOI: 10.1038/s41467-023-36177-w] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/23/2020] [Accepted: 01/18/2023] [Indexed: 02/22/2023] Open
Abstract
Planktonic calcifying organisms play a key role in regulating ocean carbonate chemistry and atmospheric CO2. Surprisingly, references to the absolute and relative contribution of these organisms to calcium carbonate production are lacking. Here we report quantification of pelagic calcium carbonate production in the North Pacific, providing new insights on the contribution of the three main planktonic calcifying groups. Our results show that coccolithophores dominate the living calcium carbonate (CaCO3) standing stock, with coccolithophore calcite comprising ~90% of total CaCO3 production, and pteropods and foraminifera playing a secondary role. We show that pelagic CaCO3 production is higher than the sinking flux of CaCO3 at 150 and 200 m at ocean stations ALOHA and PAPA, implying that a large portion of pelagic calcium carbonate is remineralised within the photic zone; this extensive shallow dissolution explains the apparent discrepancy between previous estimates of CaCO3 production derived from satellite observations/biogeochemical modeling versus estimates from shallow sediment traps. We suggest future changes in the CaCO3 cycle and its impact on atmospheric CO2 will largely depend on how the poorly-understood processes that determine whether CaCO3 is remineralised in the photic zone or exported to depth respond to anthropogenic warming and acidification.
Collapse
Affiliation(s)
- Patrizia Ziveri
- Universitat Autònoma de Barcelona, Institute of Environmental Science and Technology, Barcelona, Spain. .,Catalan Institution for Research and Advanced Studies (ICREA), Barcelona, Spain. .,Universitat Autònoma de Barcelona, BABVE Department, Barcelona, Spain.
| | - William Robert Gray
- Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Université Paris-Saclay, Gif-sur-Yvette, France. .,University of St Andrews, School of Earth and Environmental Sciences, St Andrews, United Kingdom.
| | - Griselda Anglada-Ortiz
- grid.7080.f0000 0001 2296 0625Universitat Autònoma de Barcelona, Institute of Environmental Science and Technology, Barcelona, Spain ,grid.10919.300000000122595234Centre for Arctic Gas Hydrate, Environment and Climate (CAGE), Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway
| | - Clara Manno
- grid.8682.40000000094781573British Antarctic Survey, Natural Environmental Research Council, Cambridge, United Kingdom
| | - Michael Grelaud
- grid.7080.f0000 0001 2296 0625Universitat Autònoma de Barcelona, Institute of Environmental Science and Technology, Barcelona, Spain
| | - Alessandro Incarbona
- grid.10776.370000 0004 1762 5517Università di Palermo, Dipartimento di Scienze della Terra e del Mare, Palermo, Italy
| | - James William Buchanan Rae
- grid.11914.3c0000 0001 0721 1626University of St Andrews, School of Earth and Environmental Sciences, St Andrews, United Kingdom
| | - Adam V. Subhas
- grid.56466.370000 0004 0504 7510Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA USA
| | - Sven Pallacks
- grid.7080.f0000 0001 2296 0625Universitat Autònoma de Barcelona, Institute of Environmental Science and Technology, Barcelona, Spain
| | - Angelicque White
- grid.410445.00000 0001 2188 0957School of Ocean and Earth Science and Technology, Department of Oceanography, University of Hawai’i at Manoa, Honolulu, USA
| | - Jess F. Adkins
- grid.20861.3d0000000107068890Department of Geology and Planetary Sciences, Linde Center for Global Environmental Science, California Institute of Technology, Pasadena, CA USA
| | - William Berelson
- grid.42505.360000 0001 2156 6853University of Southern California, Department of Earth Sciences, Los Angeles, CA USA
| |
Collapse
|
34
|
RNAi Silencing of the Biomineralization Gene Perlucin Impairs Oyster Ability to Cope with Ocean Acidification. Int J Mol Sci 2023; 24:ijms24043661. [PMID: 36835072 PMCID: PMC9961701 DOI: 10.3390/ijms24043661] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/23/2022] [Revised: 02/01/2023] [Accepted: 02/07/2023] [Indexed: 02/15/2023] Open
Abstract
Calcifying marine organisms, including the eastern oyster (Crassostrea virginica), are vulnerable to ocean acidification (OA) because it is more difficult to precipitate calcium carbonate (CaCO3). Previous investigations of the molecular mechanisms associated with resilience to OA in C. virginica demonstrated significant differences in single nucleotide polymorphism and gene expression profiles among oysters reared under ambient and OA conditions. Converged evidence generated by both of these approaches highlighted the role of genes related to biomineralization, including perlucins. Here, gene silencing via RNA interference (RNAi) was used to evaluate the protective role of a perlucin gene under OA stress. Larvae were exposed to short dicer-substrate small interfering RNA (DsiRNA-perlucin) to silence the target gene or to one of two control treatments (control DsiRNA or seawater) before cultivation under OA (pH ~7.3) or ambient (pH ~8.2) conditions. Two transfection experiments were performed in parallel, one during fertilization and one during early larval development (6 h post-fertilization), before larval viability, size, development, and shell mineralization were monitored. Silenced oysters under acidification stress were the smallest, had shell abnormalities, and had significantly reduced shell mineralization, thereby suggesting that perlucin significantly helps larvae mitigate the effects of OA.
Collapse
|
35
|
Schwaner C, Farhat S, Barbosa M, Boutet I, Tanguy A, Pales Espinosa E, Allam B. Molecular Features Associated with Resilience to Ocean Acidification in the Northern Quahog, Mercenaria mercenaria. MARINE BIOTECHNOLOGY (NEW YORK, N.Y.) 2023; 25:83-99. [PMID: 36417051 DOI: 10.1007/s10126-022-10183-3] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/29/2022] [Accepted: 11/08/2022] [Indexed: 06/16/2023]
Abstract
The increasing concentration of CO2 in the atmosphere and resulting flux into the oceans will further exacerbate acidification already threatening coastal marine ecosystems. The subsequent alterations in carbonate chemistry can have deleterious impacts on many economically and ecologically important species including the northern quahog (Mercenaria mercenaria). The accelerated pace of these changes requires an understanding of how or if species and populations will be able to acclimate or adapt to such swift environmental alterations. Thus far, studies have primarily focused on the physiological effects of ocean acidification (OA) on M. mercenaria, including reductions in growth and survival. However, the molecular mechanisms of resilience to OA in this species remains unclear. Clam gametes were fertilized under normal pCO2 and reared under acidified (pH ~ 7.5, pCO2 ~ 1200 ppm) or control (pH ~ 7.9, pCO2 ~ 600 ppm) conditions before sampled at 2 days (larvae), 32 days (postsets), 5 and 10 months (juveniles) and submitted to RNA and DNA sequencing to evaluate alterations in gene expression and genetic variations. Results showed significant shift in gene expression profiles among clams reared in acidified conditions as compared to their respective controls. At 10 months of exposure, significant shifts in allele frequency of single nucleotide polymorphisms (SNPs) were identified. Both approaches highlighted genes coding for proteins related to shell formation, bicarbonate transport, cytoskeleton, immunity/stress, and metabolism, illustrating the role these pathways play in resilience to OA.
Collapse
Affiliation(s)
- Caroline Schwaner
- School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY, 11790, USA
| | - Sarah Farhat
- School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY, 11790, USA
| | - Michelle Barbosa
- School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY, 11790, USA
| | - Isabelle Boutet
- Station Biologique de Roscoff, CNRS/Sorbonne Université, Place Georges Teissier, 29680, Roscoff, France
| | - Arnaud Tanguy
- Station Biologique de Roscoff, CNRS/Sorbonne Université, Place Georges Teissier, 29680, Roscoff, France
| | | | - Bassem Allam
- School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, NY, 11790, USA.
| |
Collapse
|
36
|
Acclimatization of a coral-dinoflagellate mutualism at a CO 2 vent. Commun Biol 2023; 6:66. [PMID: 36653505 PMCID: PMC9849335 DOI: 10.1038/s42003-022-04327-3] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/29/2022] [Accepted: 12/01/2022] [Indexed: 01/19/2023] Open
Abstract
Ocean acidification caused by shifts in ocean carbonate chemistry resulting from increased atmospheric CO2 concentrations is threatening many calcifying organisms, including corals. Here we assessed autotrophy vs heterotrophy shifts in the Mediterranean zooxanthellate scleractinian coral Balanophyllia europaea acclimatized to low pH/high pCO2 conditions at a CO2 vent off Panarea Island (Italy). Dinoflagellate endosymbiont densities were higher at lowest pH Sites where changes in the distribution of distinct haplotypes of a host-specific symbiont species, Philozoon balanophyllum, were observed. An increase in symbiont C/N ratios was observed at low pH, likely as a result of increased C fixation by higher symbiont cell densities. δ13C values of the symbionts and host tissue reached similar values at the lowest pH Site, suggesting an increased influence of autotrophy with increasing acidification. Host tissue δ15N values of 0‰ strongly suggest that diazotroph N2 fixation is occurring within the coral tissue/mucus at the low pH Sites, likely explaining the decrease in host tissue C/N ratios with acidification. Overall, our findings show an acclimatization of this coral-dinoflagellate mutualism through trophic adjustment and symbiont haplotype differences with increasing acidification, highlighting that some corals are capable of acclimatizing to ocean acidification predicted under end-of-century scenarios.
Collapse
|
37
|
Shen C, Testa JM, Herrmann M, Najjar RG. Decoupling of Estuarine Hypoxia and Acidification as Revealed by Historical Water Quality Data. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:780-789. [PMID: 36521075 DOI: 10.1021/acs.est.2c05949] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/17/2023]
Abstract
Hypoxia and acidification are commonly coupled in eutrophic aquatic environments because aerobic respiration is usually dominant in bottom waters and can lower dissolved oxygen (DO) and pH simultaneously. However, the degree of coupling, which can be weakened by non-aerobic respiration and CaCO3 cycling, has not been adequately assessed. In this study, we applied a box model to 20 years of water quality monitoring data to explore the relationship between hypoxia and acidification along the mainstem of Chesapeake Bay. In the early summer, dissolved inorganic carbon (DIC) production in mid-bay bottom waters was dominated by aerobic respiration, contributing to DO and pH declines. In contrast, late-summer DIC production was higher than that expected from aerobic respiration, suggesting potential buffering processes, such as calcium carbonate dissolution, which would elevate pH in hypoxic waters. These findings are consistent with contrasting seasonal relationships between riverine nitrogen (N) loads and hypoxic and acidified volumes. The N loads were associated with increased hypoxic and acidified volumes in June, but only increased hypoxic volumes in August, when acidified volume declines instead. Our study reveals that the magnitude of this decoupling varies interannually with watershed nutrient inputs, which has implications for the management of co-stressors in estuarine systems.
Collapse
Affiliation(s)
- Chunqi Shen
- College of Environmental Science and Engineering, Suzhou University of Science and Technology, Suzhou, Jiangsu215224, China
- Chesapeake Biological Laboratory, University of Maryland Center for Environmental Science, Solomons, Maryland20688, United States
| | - Jeremy M Testa
- Chesapeake Biological Laboratory, University of Maryland Center for Environmental Science, Solomons, Maryland20688, United States
| | - Maria Herrmann
- Department of Meteorology and Atmospheric Science, The Pennsylvania State University, University Park, Pennsylvania16802, United States
| | - Raymond G Najjar
- Department of Meteorology and Atmospheric Science, The Pennsylvania State University, University Park, Pennsylvania16802, United States
| |
Collapse
|
38
|
Henson HC, Holding JM, Meire L, Rysgaard S, Stedmon CA, Stuart-Lee A, Bendtsen J, Sejr M. Coastal freshening drives acidification state in Greenland fjords. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 855:158962. [PMID: 36170921 DOI: 10.1016/j.scitotenv.2022.158962] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/28/2022] [Accepted: 09/19/2022] [Indexed: 06/16/2023]
Abstract
Greenland's fjords and coastal waters are highly productive and sustain important fisheries. However, retreating glaciers and increasing meltwater are changing fjord circulation and biogeochemistry, which may threaten future productivity. The freshening of Greenland fjords caused by unprecedented melting of the Greenland Ice Sheet may alter carbonate chemistry in coastal waters, influencing CO2 uptake and causing biological consequences from acidification. However, few studies to date explore the current acidification state in Greenland coastal waters. Here we present the first-ever large-scale measurements of carbonate system parameters in 16 Greenlandic fjords and seek to identify the drivers of acidification state in these freshening ecosystems. Aragonite saturation state (Ω), a proxy for ocean acidification, was calculated from dissolved inorganic carbon (DIC) and total alkalinity from fjords along the east and west coast of Greenland spanning 68-75°N. Aragonite saturation was primarily >1 in the surface mixed layer. However, undersaturated-or corrosive--conditions (Ω < 1) were observed on both coasts (west: Ω = 0.28-3.11, east: Ω = 0.70-3.07), albeit at different depths. West Greenland fjords were largely corrosive at depth while undersaturation in East Greenland fjords was only observed in surface waters. This reflects a difference in the coastal boundary conditions and mechanisms driving acidification state. We suggest that advection of Sub Polar Mode Water and accumulation of DIC from organic matter decomposition drive corrosive conditions in the West, while freshwater alkalinity dilution drives acidification in the East. The presence of marine terminating glaciers also impacted local acidification states by influencing fjord circulation: upwelling driven by subglacial discharge brought corrosive bottom waters to shallower depths. Meanwhile, discharge from land terminating glaciers strengthened stratification and diluted alkalinity. Regardless of the drivers in each system, increasing freshwater discharge will likely lower carbonate saturation states and impact biotic and abiotic carbon uptake in the future.
Collapse
Affiliation(s)
| | - Johnna M Holding
- Arctic Research Centre, Aarhus University, Denmark; Department of Ecoscience, Aarhus University, Denmark
| | - Lorenz Meire
- Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research, Yerseke, the Netherlands; Greenland Climate Research Centre, Greenland Institute of Natural Resources, Nuuk, Greenland
| | | | - Colin A Stedmon
- National Institute of Aquatic Resources, Technical University of Denmark, Lyngby, Denmark
| | - Alice Stuart-Lee
- Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research, Yerseke, the Netherlands
| | - Jørgen Bendtsen
- Globe Institute, University of Copenhagen, Copenhagen, Denmark
| | - Mikael Sejr
- Arctic Research Centre, Aarhus University, Denmark; Department of Ecoscience, Aarhus University, Denmark
| |
Collapse
|
39
|
Xu D, Huang S, Fan X, Zhang X, Wang Y, Wang W, Beardall J, Brennan G, Ye N. Elevated CO 2 reduces copper accumulation and toxicity in the diatom Thalassiosira pseudonana. Front Microbiol 2023; 13:1113388. [PMID: 36687610 PMCID: PMC9853397 DOI: 10.3389/fmicb.2022.1113388] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/01/2022] [Accepted: 12/16/2022] [Indexed: 01/09/2023] Open
Abstract
The projected ocean acidification (OA) associated with increasing atmospheric CO2 alters seawater chemistry and hence the bio-toxicity of metal ions. However, it is still unclear how OA might affect the long-term resilience of globally important marine microalgae to anthropogenic metal stress. To explore the effect of increasing pCO2 on copper metabolism in the diatom Thalassiosira pseudonana (CCMP 1335), we employed an integrated eco-physiological, analytical chemistry, and transcriptomic approach to clarify the effect of increasing pCO2 on copper metabolism of Thalassiosira pseudonana across different temporal (short-term vs. long-term) and spatial (indoor laboratory experiments vs. outdoor mesocosms experiments) scales. We found that increasing pCO2 (1,000 and 2,000 μatm) promoted growth and photosynthesis, but decreased copper accumulation and alleviated its bio-toxicity to T. pseudonana. Transcriptomics results indicated that T. pseudonana altered the copper detoxification strategy under OA by decreasing copper uptake and enhancing copper-thiol complexation and copper efflux. Biochemical analysis further showed that the activities of the antioxidant enzymes glutathione peroxidase (GPX), catalase (CAT), and phytochelatin synthetase (PCS) were enhanced to mitigate oxidative damage of copper stress under elevated CO2. Our results provide a basis for a better understanding of the bioremediation capacity of marine primary producers, which may have profound effect on the security of seafood quality and marine ecosystem sustainability under further climate change.
Collapse
Affiliation(s)
- Dong Xu
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao, China,Function Laboratory for Marine Fisheries Science and Food Production Processes, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
| | - Shujie Huang
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao, China
| | - Xiao Fan
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao, China
| | - Xiaowen Zhang
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao, China
| | - Yitao Wang
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao, China
| | - Wei Wang
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao, China
| | - John Beardall
- School of Biological Sciences, Monash University, Clayton, VIC, Australia
| | - Georgina Brennan
- Institute of Marine Sciences, ICM-CSIC, Barcelona, Spain,*Correspondence: Georgina Brennan, ✉
| | - Naihao Ye
- Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao, China,Function Laboratory for Marine Fisheries Science and Food Production Processes, Qingdao National Laboratory for Marine Science and Technology, Qingdao, China,Naihao Ye, ✉
| |
Collapse
|
40
|
Mancuso A, Yam R, Prada F, Stagioni M, Goffredo S, Shemesh A. Oxygen and carbon isotope variations in Chamelea gallina shells: Environmental influences and vital effects. GEOBIOLOGY 2023; 21:119-132. [PMID: 36163640 PMCID: PMC10087952 DOI: 10.1111/gbi.12526] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 04/06/2022] [Revised: 07/19/2022] [Accepted: 09/01/2022] [Indexed: 06/16/2023]
Abstract
Stable isotopes in mollusc shells, together with variable growth rates and other geochemical properties, can register different environmental clues, including seawater temperature, salinity and primary productivity. However, the strict biological control over the construction of biominerals exerted by many calcifying organisms can constrain the use of these organisms for paleoenvironmental reconstructions. Biologically controlled calcification is responsible for the so called vital effects that cause a departure from isotopic equilibrium during shell formation, resulting in lower shell oxygen and carbon compared to the equilibrium value. We investigated shell oxygen and carbon isotopic composition of the bivalve Chamelea gallina in six sites along with a latitudinal gradient on the Adriatic Sea (NE Mediterranean Sea). Seawater δ18 O and δ13 CDIC varied from North to South, reflecting variations in seawater temperature, salinity, and chlorophyll concentration among sites. Shell δ18 O and δ13 C differed among sites and exhibited a wide range of values along with the ~400 km latitudinal gradient, away from isotopic equilibrium for both isotopes. These results hampered the utilization of this bivalve as a proxy for environmental reconstructions, in spite of C. gallina showing promise as a warm temperature proxy. Rigorous calibration studies with a precise insight of environment and shell growth are crucial prior to considering this bivalve as a reliable paleoclimatic archive.
Collapse
Affiliation(s)
- Arianna Mancuso
- Marine Science Group, Department of Biological, Geological and Environmental SciencesUniversity of BolognaBolognaItaly
- Fano Marine Center, The Inter‐Institute Center for Research on Marine BiodiversityResources and BiotechnologiesFanoItaly
| | - Ruth Yam
- Department of Earth and Planetary SciencesWeizmann Institute of ScienceRehovotIsrael
| | - Fiorella Prada
- Environmental Biophysics and Molecular Ecology Program, Department of Marine and Coastal Sciences, RutgersThe State University of New JerseyNew BrunswickNew JerseyUSA
| | - Marco Stagioni
- Marine Biology and Fisheries Lab, Dept. of Biological, Geological and Environmental SciencesUniversity of BolognaBolognaItaly
| | - Stefano Goffredo
- Marine Science Group, Department of Biological, Geological and Environmental SciencesUniversity of BolognaBolognaItaly
- Fano Marine Center, The Inter‐Institute Center for Research on Marine BiodiversityResources and BiotechnologiesFanoItaly
| | - Aldo Shemesh
- Department of Earth and Planetary SciencesWeizmann Institute of ScienceRehovotIsrael
| |
Collapse
|
41
|
Lustosa do Carmo TL, Moraes de Lima MC, de Vasconcelos Lima JL, Silva de Souza S, Val AL. Tissue distribution of appetite regulation genes and their expression in the Amazon fish Colossoma macropomum exposed to climate change scenario. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 854:158729. [PMID: 36116666 DOI: 10.1016/j.scitotenv.2022.158729] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/02/2022] [Revised: 08/24/2022] [Accepted: 09/09/2022] [Indexed: 06/15/2023]
Abstract
Climate change leads to an increase in water acidification and temperature, two environmental factors that can change fish appetite and metabolism, affecting fish population in both wild and aquaculture facilities. Therefore, our study tested if climate change affects gene expression levels of two appetite-regulating peptides - Neuropeptide Y (NPY) and Cholecystokinin (CCK) - in the brain of tambaqui, Colossoma macropomum. Additionally, we show the distribution of these genes throughout the body. Amino acid sequences of CCK and NPY of tambaqui showed high similarity with other Characiformes, with the closely related order Cypriniformes, and even with the more distantly related order Salmoniformes. High apparent levels of both peptides were expressed in all brain areas, while expression levels varied for peripheral tissues. NPY and CCK mRNA were detected in all peripheral tissues but cephalic kidney for CCK. As for the effects of climate change, we found that fish exposed to extreme climate scenario (800 ppm CO2 and 4.5 °C above current climate scenario) had higher expression levels of NPY and lower expression levels of CCK in the telencephalon. The extreme climate scenario also increased food intake, weight gain, and body length. These results suggest that the telencephalon is probably responsible for sensing the metabolic status of the organism and controlling feeding behavior through NPY, likely an orexigenic hormone, and CCK, which may act as an anorexigenic hormone. To our knowledge, this is the first study showing the effects of climate change on the endocrine regulation of appetite in an endemic and economically important fish from the Amazon. Our results can help us predict the impact of climate change on both wild and farmed fish populations, thus contributing to the elaboration of future policies regarding their conservation and sustainable use.
Collapse
Affiliation(s)
- Talita Laurie Lustosa do Carmo
- Laboratory of Ecophysiology and Molecular Evolution, National Institute for Amazonian Research, Manaus, Amazonas, Brazil.
| | - Mayara Cristina Moraes de Lima
- Laboratory of Ecophysiology and Molecular Evolution, National Institute for Amazonian Research, Manaus, Amazonas, Brazil
| | - José Luiz de Vasconcelos Lima
- Laboratory of Ecophysiology and Molecular Evolution, National Institute for Amazonian Research, Manaus, Amazonas, Brazil
| | - Samara Silva de Souza
- Laboratory of Ecophysiology and Molecular Evolution, National Institute for Amazonian Research, Manaus, Amazonas, Brazil
| | - Adalberto Luis Val
- Laboratory of Ecophysiology and Molecular Evolution, National Institute for Amazonian Research, Manaus, Amazonas, Brazil
| |
Collapse
|
42
|
Begum M, Masud MM, Alam L, Mokhtar MB, Amir AA. The impact of climate variables on marine fish production: an empirical evidence from Bangladesh based on autoregressive distributed lag (ARDL) approach. ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH INTERNATIONAL 2022; 29:87923-87937. [PMID: 35819668 DOI: 10.1007/s11356-022-21845-z] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/02/2021] [Accepted: 06/30/2022] [Indexed: 06/15/2023]
Abstract
Several studies have highlighted the significant impact of climate change on agriculture. However, there have been little empirical enquiries into the impact of climate change on marine fish production, particularly in Bangladesh. Hence, this study aims to investigate the impact of climate change on marine fish production in Bangladesh using data from 1961 to 2019. Data were obtained from the Food and Agriculture Organization, Bangladesh Meteorological Department, the World Development Indicators, and the National Oceanic and Atmospheric Administration. The autoregressive distributed lag (ARDL) model was used to describe the dynamic link between CO2 emissions, average temperature, Sea Surface Temperature (SST), rainfall, sunshine, wind and marine fish production. The ARDL approach to cointegration revealed that SST (β = 0.258), rainfall (β =0.297), and sunshine (β =0.663) significantly influence marine fish production at 1% and 10% levels in the short run and at 1% level in the long run. The results also found that average temperature has a significant negative impact on fish production in both short and long runs. On the other hand, CO2 emissions have a negative impact on marine fish production in the short run. Specifically, for every 1% rise in CO2 emissions, marine fish production will decline by 0.11%. The findings of this study suggest that policymakers formulate better policy frameworks for climate change adaptation and sustainable management of marine fisheries at the national level. Research and development in Bangladesh's fisheries sector should also focus on marine fish species that can resist high sea surface temperatures, CO2 emissions, and average temperatures.
Collapse
Affiliation(s)
- Mahfuza Begum
- The Institute for Environment and Development (LESTARI), The National University of Malaysia, Bangi, Selangor, Malaysia
| | - Muhammad Mehedi Masud
- Department of Development Studies, Faculty of Business and Economics, Universiti Malaya, 50603, Kuala Lumpur, Malaysia
| | - Lubna Alam
- The Institute for Environment and Development (LESTARI), The National University of Malaysia, Bangi, Selangor, Malaysia.
| | - Mazlin Bin Mokhtar
- The Institute for Environment and Development (LESTARI), The National University of Malaysia, Bangi, Selangor, Malaysia
| | - Ahmad Aldrie Amir
- The Institute for Environment and Development (LESTARI), The National University of Malaysia, Bangi, Selangor, Malaysia
| |
Collapse
|
43
|
Sanchez-Arcos C, Paris D, Mazzella V, Mutalipassi M, Costantini M, Buia MC, von Elert E, Cutignano A, Zupo V. Responses of the Macroalga Ulva prolifera Müller to Ocean Acidification Revealed by Complementary NMR- and MS-Based Omics Approaches. Mar Drugs 2022; 20:md20120743. [PMID: 36547890 PMCID: PMC9783899 DOI: 10.3390/md20120743] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/19/2022] [Revised: 11/21/2022] [Accepted: 11/23/2022] [Indexed: 11/29/2022] Open
Abstract
Ocean acidification (OA) is a dramatic perturbation of seawater environments due to increasing anthropogenic emissions of CO2. Several studies indicated that OA frequently induces marine biota stress and a reduction of biodiversity. Here, we adopted the macroalga Ulva prolifera as a model and applied a complementary multi-omics approach to investigate the metabolic profiles under normal and acidified conditions. Our results show that U. prolifera grows at higher rates in acidified environments. Consistently, we observed lower sucrose and phosphocreatine concentrations in response to a higher demand of energy for growth and a higher availability of essential amino acids, likely related to increased protein biosynthesis. In addition, pathways leading to signaling and deterrent compounds appeared perturbed. Finally, a remarkable shift was observed here for the first time in the fatty acid composition of triglycerides, with a decrease in the relative abundance of PUFAs towards an appreciable increase of palmitic acid, thus suggesting a remodeling in lipid biosynthesis. Overall, our studies revealed modulation of several biosynthetic pathways under OA conditions in which, besides the possible effects on the marine ecosystem, the metabolic changes of the alga should be taken into account considering its potential nutraceutical applications.
Collapse
Affiliation(s)
- Carlos Sanchez-Arcos
- Institute for Zoology, Cologne Biocenter University of Cologne, 50674 Köln, Germany
| | - Debora Paris
- Consiglio Nazionale delle Ricerche (CNR), Istituto di Chimica Biomolecolare (ICB), 80078 Pozzuoli, Italy
| | - Valerio Mazzella
- Department of Integrative Marine Ecology, Stazione Zoologica Anton Dohrn, Ischia Marine Center, 80077 Ischia, Italy
| | - Mirko Mutalipassi
- Department of Integrative Marine Ecology, Stazione Zoologica Anton Dohrn, Calabria Marine Centre, 87071 Amendolara, Italy
| | - Maria Costantini
- Department of Ecosustainable Marine Biotechnology, Stazione Zoologica Anton Dohrn, 80121 Napoli, Italy
| | - Maria Cristina Buia
- Department of Integrative Marine Ecology, Stazione Zoologica Anton Dohrn, Ischia Marine Center, 80077 Ischia, Italy
| | - Eric von Elert
- Institute for Zoology, Cologne Biocenter University of Cologne, 50674 Köln, Germany
| | - Adele Cutignano
- Consiglio Nazionale delle Ricerche (CNR), Istituto di Chimica Biomolecolare (ICB), 80078 Pozzuoli, Italy
- Department of Ecosustainable Marine Biotechnology, Stazione Zoologica Anton Dohrn, 80121 Napoli, Italy
- Correspondence: (A.C.); (V.Z.); Tel.: +39-081-8675313 (A.C.); +39-081-5833503 (V.Z.)
| | - Valerio Zupo
- Department of Ecosustainable Marine Biotechnology, Stazione Zoologica Anton Dohrn, 80077 Ischia, Italy
- Correspondence: (A.C.); (V.Z.); Tel.: +39-081-8675313 (A.C.); +39-081-5833503 (V.Z.)
| |
Collapse
|
44
|
Kekuewa SAH, Courtney TA, Cyronak T, Andersson AJ. Seasonal nearshore ocean acidification and deoxygenation in the Southern California Bight. Sci Rep 2022; 12:17969. [PMID: 36289268 PMCID: PMC9606271 DOI: 10.1038/s41598-022-21831-y] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/24/2022] [Accepted: 10/04/2022] [Indexed: 01/24/2023] Open
Abstract
The California Current System experiences seasonal ocean acidification and hypoxia (OAH) owing to wind-driven upwelling, but little is known about the intensity, frequency, and depth distribution of OAH in the shallow nearshore environment. Here we present observations of OAH and dissolved inorganic carbon and nutrient parameters based on monthly transects from March 2017 to September 2018 extending from the surf zone to the ~ 40 m depth contour in La Jolla, California. Biologically concerning OAH conditions were observed at depths as shallow as 10 m and as close as 700 m to the shoreline. Below 20 m depth, 8% of observations were undersaturated with respect to aragonite, 28% of observations had a pHT less than 7.85, and 19% of observations were below the sublethal oxygen threshold of 157 µmol kg-1. These observations raise important questions about the impacts of OAH on coastal organisms and ecosystems and how future intensified upwelling may exacerbate these conditions.
Collapse
Affiliation(s)
- Samuel A. H. Kekuewa
- grid.266100.30000 0001 2107 4242Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA USA
| | - Travis A. Courtney
- grid.267044.30000 0004 0398 9176Department of Marine Sciences, University of Puerto Rico Mayagüez, Mayagüez, PR USA
| | - Tyler Cyronak
- grid.261241.20000 0001 2168 8324Department of Marine and Environmental Sciences, Halmos College of Natural Sciences and Oceanography, Nova Southeastern University, Dania Beach, FL USA
| | - Andreas J. Andersson
- grid.266100.30000 0001 2107 4242Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA USA
| |
Collapse
|
45
|
Fan X, Batchelor-McAuley C, Yang M, Compton RG. Single Calcite Particle Dissolution Kinetics: Revealing the Influence of Mass Transport. ACS MEASUREMENT SCIENCE AU 2022; 2:422-429. [PMID: 36785660 PMCID: PMC9885995 DOI: 10.1021/acsmeasuresciau.2c00025] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Indexed: 06/18/2023]
Abstract
Calcite dissolution kinetics at the single particle scale are determined. It is demonstrated that at high undersaturation and in the absence of inhibitors the particulate mineral dissolution rate is controlled by a saturated calcite surface in local equilibrium with dissolved Ca2+ and CO3 2- coupled with rate determining diffusive transport of the ions away from the surface. Previous work is revisited and inconsistencies arising from the assumption of a surface-controlled reaction are highlighted. The data have implications for ocean modeling of climate change.
Collapse
Affiliation(s)
- Xinmeng Fan
- Physical
and Theoretical Chemistry Laboratory, Department of Chemistry, University of Oxford, South Parks Road, Oxford OX1 3QZ, Great Britain
| | - Christopher Batchelor-McAuley
- Physical
and Theoretical Chemistry Laboratory, Department of Chemistry, University of Oxford, South Parks Road, Oxford OX1 3QZ, Great Britain
| | - Minjun Yang
- Physical
and Theoretical Chemistry Laboratory, Department of Chemistry, University of Oxford, South Parks Road, Oxford OX1 3QZ, Great Britain
| | - Richard G. Compton
- Physical
and Theoretical Chemistry Laboratory, Department of Chemistry, University of Oxford, South Parks Road, Oxford OX1 3QZ, Great Britain
| |
Collapse
|
46
|
Bednaršek N, Carter BR, McCabe RM, Feely RA, Howard E, Chavez FP, Elliott M, Fisher JL, Jahncke J, Siegrist Z. Pelagic calcifiers face increased mortality and habitat loss with warming and ocean acidification. ECOLOGICAL APPLICATIONS : A PUBLICATION OF THE ECOLOGICAL SOCIETY OF AMERICA 2022; 32:e2674. [PMID: 35584131 PMCID: PMC9786838 DOI: 10.1002/eap.2674] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 02/23/2021] [Revised: 12/22/2021] [Accepted: 01/14/2022] [Indexed: 06/15/2023]
Abstract
Global change is impacting the oceans in an unprecedented way, and multiple lines of evidence suggest that species distributions are changing in space and time. There is increasing evidence that multiple environmental stressors act together to constrain species habitat more than expected from warming alone. Here, we conducted a comprehensive study of how temperature and aragonite saturation state act together to limit Limacina helicina, globally distributed pteropods that are ecologically important pelagic calcifiers and an indicator species for ocean change. We co-validated three different approaches to evaluate the impact of ocean warming and acidification (OWA) on the survival and distribution of this species in the California Current Ecosystem. First, we used colocated physical, chemical, and biological data from three large-scale west coast cruises and regional time series; second, we conducted multifactorial experimental incubations to evaluate how OWA impacts pteropod survival; and third, we validated the relationships we found against global distributions of pteropods and carbonate chemistry. OWA experimental work revealed mortality increases under OWA, while regional habitat suitability indices and global distributions of L. helicina suggest that a multi-stressor framework is essential for understanding pteropod distributions. In California Current Ecosystem habitats, where pteropods are living close to their thermal maximum already, additional warming and acidification through unabated fossil fuel emissions (RCP 8.5) are expected to dramatically reduce habitat suitability.
Collapse
Affiliation(s)
- Nina Bednaršek
- Marine Biological StationNational Institute for BiologyLjubljanaSlovenia
- Cooperative Institute for Marine Resources StudiesOregon State UniversityNewportOregonUSA
| | - Brendan R. Carter
- Cooperative Institute for Climate, Ocean, and Ecosystem StudiesUniversity of WashingtonSeattleWashingtonUSA
- NOAA Pacific Marine Environmental LaboratorySeattleWashingtonUSA
| | - Ryan M. McCabe
- Cooperative Institute for Climate, Ocean, and Ecosystem StudiesUniversity of WashingtonSeattleWashingtonUSA
- NOAA Pacific Marine Environmental LaboratorySeattleWashingtonUSA
| | - Richard A. Feely
- Cooperative Institute for Climate, Ocean, and Ecosystem StudiesUniversity of WashingtonSeattleWashingtonUSA
| | - Evan Howard
- Department of GeosciencesPrinceton UniversityPrincetonNew JerseyUSA
| | | | | | - Jennifer L. Fisher
- Cooperative Institute for Marine Resources StudiesOregon State UniversityNewportOregonUSA
| | - Jaime Jahncke
- Point Blue Conservation SciencePetalumaCaliforniaUSA
| | | |
Collapse
|
47
|
Danylchuk AJ, Griffin LP, Ahrens R, Allen MS, Boucek RE, Brownscombe JW, Casselberry GA, Danylchuk SC, Filous A, Goldberg TL, Perez AU, Rehage JS, Santos RO, Shenker J, Wilson JK, Adams AJ, Cooke SJ. Cascading effects of climate change on recreational marine flats fishes and fisheries. ENVIRONMENTAL BIOLOGY OF FISHES 2022; 106:381-416. [PMID: 36118617 PMCID: PMC9465673 DOI: 10.1007/s10641-022-01333-6] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 03/17/2022] [Accepted: 08/27/2022] [Indexed: 06/15/2023]
Abstract
Tropical and subtropical coastal flats are shallow regions of the marine environment at the intersection of land and sea. These regions provide myriad ecological goods and services, including recreational fisheries focused on flats-inhabiting fishes such as bonefish, tarpon, and permit. The cascading effects of climate change have the potential to negatively impact coastal flats around the globe and to reduce their ecological and economic value. In this paper, we consider how the combined effects of climate change, including extremes in temperature and precipitation regimes, sea level rise, and changes in nutrient dynamics, are causing rapid and potentially permanent changes to the structure and function of tropical and subtropical flats ecosystems. We then apply the available science on recreationally targeted fishes to reveal how these changes can cascade through layers of biological organization-from individuals, to populations, to communities-and ultimately impact the coastal systems that depend on them. We identify critical gaps in knowledge related to the extent and severity of these effects, and how such gaps influence the effectiveness of conservation, management, policy, and grassroots stewardship efforts.
Collapse
Affiliation(s)
- Andy J. Danylchuk
- Department of Environmental Conservation, University of Massachusetts Amherst, 160 Holdsworth Way, Amherst, MA 01003 USA
| | - Lucas P. Griffin
- Department of Environmental Conservation, University of Massachusetts Amherst, 160 Holdsworth Way, Amherst, MA 01003 USA
| | - Robert Ahrens
- Fisheries Research and Monitoring Division, NOAA Pacific Islands Fisheries Science Center, 1845 Wasp Blvd., Bldg 176, Honolulu, HI 96818 USA
| | - Micheal S. Allen
- Nature Coast Biological Station, School of Forest, Fisheries and Geomatics Sciences, The University of Florida, 552 First Street, Cedar Key, FL 32625 USA
| | - Ross E. Boucek
- Bonefish & Tarpon Trust, 2937 SW 27th Ave, Suite 203, Miami, FL 33133 USA
- Earth and Environment Department, Florida International University, Miami, FL 33199 USA
| | - Jacob W. Brownscombe
- Department of Biology, Carleton University, 1125 Colonel By Drive, Ottawa, ON K1S 5B6 Canada
| | - Grace A. Casselberry
- Department of Environmental Conservation, University of Massachusetts Amherst, 160 Holdsworth Way, Amherst, MA 01003 USA
| | - Sascha Clark Danylchuk
- Department of Environmental Conservation, University of Massachusetts Amherst, 160 Holdsworth Way, Amherst, MA 01003 USA
- Keep Fish Wet, 11 Kingman Road, Amherst, MA 01002 USA
| | - Alex Filous
- Department of Environmental Conservation, University of Massachusetts Amherst, 160 Holdsworth Way, Amherst, MA 01003 USA
| | - Tony L. Goldberg
- Department of Pathobiological Sciences, School of Veterinary Medicine, University of Wisconsin-Madison, 1656 Linden Drive, Madison, WI 53706 USA
| | - Addiel U. Perez
- Bonefish & Tarpon Trust, 2937 SW 27th Ave, Suite 203, Miami, FL 33133 USA
| | - Jennifer S. Rehage
- Earth and Environment Department, Florida International University, Miami, FL 33199 USA
| | - Rolando O. Santos
- Department of Biological Sciences, Florida International University, Miami, FL 33181 USA
| | - Jonathan Shenker
- Department of Ocean Engineering and Marine Sciences, Florida Institute of Technology, 150 West University Boulevard, Melbourne, FL 32904 USA
| | - JoEllen K. Wilson
- Bonefish & Tarpon Trust, 2937 SW 27th Ave, Suite 203, Miami, FL 33133 USA
| | - Aaron J. Adams
- Bonefish & Tarpon Trust, 2937 SW 27th Ave, Suite 203, Miami, FL 33133 USA
- Florida Atlantic University Harbor Branch Oceanographic Institute, 5600 US 1 North, Fort Pierce, FL 34946 USA
| | - Steven J. Cooke
- Department of Biology, Carleton University, 1125 Colonel By Drive, Ottawa, ON K1S 5B6 Canada
| |
Collapse
|
48
|
Leung JYS, Zhang S, Connell SD. Is Ocean Acidification Really a Threat to Marine Calcifiers? A Systematic Review and Meta-Analysis of 980+ Studies Spanning Two Decades. SMALL (WEINHEIM AN DER BERGSTRASSE, GERMANY) 2022; 18:e2107407. [PMID: 35934837 DOI: 10.1002/smll.202107407] [Citation(s) in RCA: 44] [Impact Index Per Article: 22.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/30/2021] [Revised: 06/24/2022] [Indexed: 06/15/2023]
Abstract
Ocean acidification is considered detrimental to marine calcifiers, but mounting contradictory evidence suggests a need to revisit this concept. This systematic review and meta-analysis aim to critically re-evaluate the prevailing paradigm of negative effects of ocean acidification on calcifiers. Based on 5153 observations from 985 studies, many calcifiers (e.g., echinoderms, crustaceans, and cephalopods) are found to be tolerant to near-future ocean acidification (pH ≈ 7.8 by the year 2100), but coccolithophores, calcifying algae, and corals appear to be sensitive. Calcifiers are generally more sensitive at the larval stage than adult stage. Over 70% of the observations in growth and calcification are non-negative, implying the acclimation capacity of many calcifiers to ocean acidification. This capacity can be mediated by phenotypic plasticity (e.g., physiological, mineralogical, structural, and molecular adjustments), transgenerational plasticity, increased food availability, or species interactions. The results suggest that the impacts of ocean acidification on calcifiers are less deleterious than initially thought as their adaptability has been underestimated. Therefore, in the forthcoming era of ocean acidification research, it is advocated that studying how marine organisms persist is as important as studying how they perish, and that future hypotheses and experimental designs are not constrained within the paradigm of negative effects.
Collapse
Affiliation(s)
- Jonathan Y S Leung
- Faculty of Materials and Energy, Southwest University, Chongqing, 400715, P. R. China
- Southern Seas Ecology Laboratories, School of Biological Sciences, The University of Adelaide, Adelaide, South Australia, 5005, Australia
| | - Sam Zhang
- Faculty of Materials and Energy, Southwest University, Chongqing, 400715, P. R. China
| | - Sean D Connell
- Southern Seas Ecology Laboratories, School of Biological Sciences, The University of Adelaide, Adelaide, South Australia, 5005, Australia
| |
Collapse
|
49
|
Toh EC, Liu KL, Tsai S, Lin C. Cryopreservation and Cryobanking of Cells from 100 Coral Species. Cells 2022; 11:cells11172668. [PMID: 36078076 PMCID: PMC9454506 DOI: 10.3390/cells11172668] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/06/2022] [Revised: 08/17/2022] [Accepted: 08/24/2022] [Indexed: 11/16/2022] Open
Abstract
When coral species become extinct, their genetic resources cannot be recovered. Coral cryobanks can be employed to preserve coral samples and thereby maintain the availability of the samples and increase their potential to be restocked. In this study, we developed a procedure to determine coral species-specific requirements for cryobank freezing through determining suitable cryoprotective agents (CPAs), CPA concentrations, equilibration times, holding durations, viability rates, and cell amounts for banked coral cells, and we established the first ever coral cell cryobank. Coral cells, including supporting and gland cells, epidermal nematocysts, Symbiodiniaceae and symbiotic endoderm cells (SEC) were found from the extracted protocol. Approximately half of the corals from the experimental corals consisted of spindle and cluster cells. Gastrodermal nematocysts were the least common. The overall concentration of Symbiodiniaceae in the coral cells was 8.6%. Freezing using DMSO as a CPA was suitable for approximately half of the corals, and for the other half of species, successful cell cryopreservation was achieved using MeOH and EG. EG and DMSO had similar suitabilities for Acanthastrea, Euphyllia, Favites, Lobophyllia, Pavona, Seriatopora, and Turbinaria, as did EG and MeOH for Acropora, Echinopyllia, and Sinularia and MeOH and DMSO for Platygyra after freezing. At least 14 straws from each species of coral were cryobanked in this study, totaling more than 1884 straws (0.5 mL) with an average concentration of 6.4 × 106 per mL. The results of this study may serve as a framework for cryobanks worldwide and contribute to the long-term conservation of coral reefs.
Collapse
Affiliation(s)
- En-Chun Toh
- Institute of Marine Biology, National Dong Hwa University, Pingtung 944401, Taiwan
| | - Kuan-Lin Liu
- Institute of Marine Biology, National Dong Hwa University, Pingtung 944401, Taiwan
| | - Sujune Tsai
- Department of Post Modern Agriculture, Mingdao University, Peetow, Changhua 52345, Taiwan
- Correspondence: (S.T.); (C.L.); Tel.: +886-925750025 (S.T.); +886-08-88825036 (C.L.)
| | - Chiahsin Lin
- Institute of Marine Biology, National Dong Hwa University, Pingtung 944401, Taiwan
- National Museum of Marine Biology & Aquarium, Checheng, Pingtung 944, Taiwan
- Correspondence: (S.T.); (C.L.); Tel.: +886-925750025 (S.T.); +886-08-88825036 (C.L.)
| |
Collapse
|
50
|
Ocean Warming Amplifies the Effects of Ocean Acidification on Skeletal Mineralogy and Microstructure in the Asterinid Starfish Aquilonastra yairi. JOURNAL OF MARINE SCIENCE AND ENGINEERING 2022. [DOI: 10.3390/jmse10081065] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 01/27/2023]
Abstract
Ocean acidification and ocean warming compromise the capacity of calcifying marine organisms to generate and maintain their skeletons. While many marine calcifying organisms precipitate low-Mg calcite or aragonite, the skeleton of echinoderms consists of more soluble Mg-calcite. To assess the impact of exposure to elevated temperature and increased pCO2 on the skeleton of echinoderms, in particular the mineralogy and microstructure, the starfish Aquilonastra yairi (Echinodermata: Asteroidea) was exposed for 90 days to simulated ocean warming (27 °C and 32 °C) and ocean acidification (455 µatm, 1052 µatm, 2066 µatm) conditions. The results indicate that temperature is the major factor controlling the skeletal Mg (Mg/Ca ratio and Mgnorm ratio), but not for skeletal Sr (Sr/Ca ratio and Srnorm ratio) and skeletal Ca (Canorm ratio) in A. yairi. Nevertheless, inter-individual variability in skeletal Sr and Ca ratios increased with higher temperature. Elevated pCO2 did not induce any statistically significant element alterations of the skeleton in all treatments over the incubation time, but increased pCO2 concentrations might possess an indirect effect on skeletal mineral ratio alteration. The influence of increased pCO2 was more relevant than that of increased temperature on skeletal microstructures. pCO2 as a sole stressor caused alterations on stereom structure and degradation on the skeletal structure of A. yairi, whereas temperature did not; however, skeletons exposed to elevated pCO2 and high temperature show a strongly altered skeleton structure compared to ambient temperature. These results indicate that ocean warming might exacerbate the skeletal maintaining mechanisms of the starfish in a high pCO2 environment and could potentially modify the morphology and functions of the starfish skeleton.
Collapse
|