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Ribeiro B, Lima C, Pereira SE, Peixoto R, Klautau M. Calcareous sponges can synthesize their skeleton under short-term ocean acidification. Sci Rep 2023; 13:6776. [PMID: 37185292 PMCID: PMC10130156 DOI: 10.1038/s41598-023-33611-3] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/01/2022] [Accepted: 04/15/2023] [Indexed: 05/17/2023] Open
Abstract
Calcifying organisms are considered as threatened by ocean acidification, because of their calcium carbonate skeleton. This study investigated if a calcareous sponge could synthesize its skeleton (i.e. spicules) under ocean-acidification conditions. Sponge cell aggregates that have the potential to develop into a functional sponge, called primmorphs, were submitted to a 5-day experiment, with two treatments: control (pH 8.1) and acidified conditions (pH 7.6). Primmorphs of the calcareous sponge Paraleucilla magna were able to synthesize a skeleton, even under low pH, and to develop into functional sponges. The spicules had the same shape in both conditions, although the spicules synthesized in low pH were slightly thinner than those in the control. These results suggest that P. magna may be able to survive near-future ocean-acidification conditions.
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Affiliation(s)
- Bárbara Ribeiro
- TaxoN Laboratory, Zoology Department, Biology Institute, Federal University of Rio de Janeiro, Rio de Janeiro, 21941-599, Brazil
| | - Carolina Lima
- TaxoN Laboratory, Zoology Department, Biology Institute, Federal University of Rio de Janeiro, Rio de Janeiro, 21941-599, Brazil
| | - Sara Emilly Pereira
- TaxoN Laboratory, Zoology Department, Biology Institute, Federal University of Rio de Janeiro, Rio de Janeiro, 21941-599, Brazil
| | - Raquel Peixoto
- Biological and Environmental Science and Engineering Division, Red Sea Research Center, King Abdullah University of Science and Technology, Thuwal, 23955-6900, Saudi Arabia
| | - Michelle Klautau
- TaxoN Laboratory, Zoology Department, Biology Institute, Federal University of Rio de Janeiro, Rio de Janeiro, 21941-599, Brazil.
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2
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Fordyce AJ, Knuefing L, Ainsworth TD, Beeching L, Turner M, Leggat W. Understanding decay in marine calcifiers: Micro‐CT analysis of skeletal structures provides insight into the impacts of a changing climate in marine ecosystems. Methods Ecol Evol 2020. [DOI: 10.1111/2041-210x.13439] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/20/2023]
Affiliation(s)
- Alexander J. Fordyce
- School of Environmental and Life Sciences University of Newcastle Ourimbah NSW Australia
| | - Lydia Knuefing
- Research School of Physics Australian National University Canberra ACT Australia
| | - Tracy D. Ainsworth
- School of Biological, Earth and Environmental Sciences University of New South Wales Sydney NSW Australia
| | - Levi Beeching
- National Laboratory for X‐ray Micro Computed Tomography Australian National University Canberra ACT Australia
| | - Michael Turner
- National Laboratory for X‐ray Micro Computed Tomography Australian National University Canberra ACT Australia
| | - William Leggat
- School of Environmental and Life Sciences University of Newcastle Ourimbah NSW Australia
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3
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Meng Y, Li C, Li H, Shih K, He C, Yao H, Thiyagarajan V. Recoverable impacts of ocean acidification on the tubeworm, Hydroides elegans: implication for biofouling in future coastal oceans. BIOFOULING 2019; 35:945-957. [PMID: 31687858 DOI: 10.1080/08927014.2019.1673376] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/19/2018] [Revised: 09/18/2019] [Accepted: 09/19/2019] [Indexed: 06/10/2023]
Abstract
Ocean uptake of anthropogenic CO2 causes ocean acidification (OA), which not only decreases the calcification rate, but also impairs the formation of calcareous shells or tubes in marine invertebrates such as the dominant biofouling tubeworm species, Hydroides elegans. This study examined the ability of tubeworms to resume normal tube calcification when returned to ambient pH 8.1 from a projected near-future OA level of pH 7.8. Tubeworms produced structurally impaired and mechanically weaker calcareous tubes at pH 7.8 compared to at pH 8.1, but were able to recover when the pH was restored to ambient levels. This suggests that tubeworms can physiologically recover from the impacts of OA on tube calcification, composition, density, hardness and stiffness when returned to optimal conditions. These results help understanding of the progression of biofouling communities dominated by tubeworms in future oceans with low pH induced by OA.
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Affiliation(s)
- Yuan Meng
- The Swire Institute of Marine Science and School of Biological Sciences, The University of Hong Kong, Hong Kong SAR, China
| | - Chaoyi Li
- The Swire Institute of Marine Science and School of Biological Sciences, The University of Hong Kong, Hong Kong SAR, China
| | - Hangkong Li
- Department of Civil Engineering, The University of Hong Kong, Hong Kong SAR, China
| | - Kaimin Shih
- Department of Civil Engineering, The University of Hong Kong, Hong Kong SAR, China
| | - Chong He
- Department of Mechanical Engineering, The Hong Kong Polytechnic University, Hong Kong SAR, China
| | - Haimin Yao
- Department of Mechanical Engineering, The Hong Kong Polytechnic University, Hong Kong SAR, China
| | - V Thiyagarajan
- The Swire Institute of Marine Science and School of Biological Sciences, The University of Hong Kong, Hong Kong SAR, China
- State Key Laboratory for Marine Pollution, Hong Kong SAR, China
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4
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Meng Y, Guo Z, Yao H, Yeung KWK, Thiyagarajan V. Calcium carbonate unit realignment under acidification: A potential compensatory mechanism in an edible estuarine oyster. MARINE POLLUTION BULLETIN 2019; 139:141-149. [PMID: 30686412 DOI: 10.1016/j.marpolbul.2018.12.030] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/24/2018] [Revised: 12/10/2018] [Accepted: 12/13/2018] [Indexed: 05/27/2023]
Abstract
Ocean acidification (OA) is well-known for impairing marine calcification; however, the end response of several essential species to this perturbation remains unknown. Decreased pH and saturation levels (Ω) of minerals under OA is projected to alter shell crystallography and thus to reduce shell mechanical properties. This study examined this hypothesis using a commercially important estuarine oyster Magallana hongkongensis. Although shell damage occurred on the outmost prismatic layer and the undying myostracum at decreased pH 7.6 and 7.3, the major foliated layer was relatively unharmed. Oysters maintained their shell hardness and stiffness through altered crystal unit orientation under pH 7.6 conditions. However, under the undersaturated conditions (ΩCal ~ 0.8) at pH 7.3, the realigned crystal units in foliated layer ultimately resulted in less stiff shells which indicated although estuarine oysters are mechanically resistant to unfavorable calcification conditions, extremely low pH condition is still a threat to this essential species.
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Affiliation(s)
- Yuan Meng
- The Swire Institute of Marine Sciences, School of Biological Sciences, The University of Hong Kong, Hong Kong Special Administrative Region, China
| | - Zhenbin Guo
- Department of Mechanical Engineering, The Hong Kong Polytechnic University, Hong Kong Special Administrative Region, China
| | - Haimin Yao
- Department of Mechanical Engineering, The Hong Kong Polytechnic University, Hong Kong Special Administrative Region, China
| | - Kelvin W K Yeung
- Department of Orthopaedics and Traumatology, Queen Mary Hospital, The University of Hong Kong, Hong Kong Special Administrative Region, China
| | - V Thiyagarajan
- The Swire Institute of Marine Sciences, School of Biological Sciences, The University of Hong Kong, Hong Kong Special Administrative Region, China; State Key Laboratory for Marine Pollution, Hong Kong Special Administrative Region, China.
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5
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Byrne M, Fitzer S. The impact of environmental acidification on the microstructure and mechanical integrity of marine invertebrate skeletons. CONSERVATION PHYSIOLOGY 2019; 7:coz062. [PMID: 31737270 PMCID: PMC6846232 DOI: 10.1093/conphys/coz062] [Citation(s) in RCA: 40] [Impact Index Per Article: 8.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/10/2019] [Revised: 06/25/2019] [Accepted: 07/25/2019] [Indexed: 05/20/2023]
Abstract
Ocean acidification (OA), from seawater uptake of anthropogenic CO2, has a suite of negative effects on the ability of marine invertebrates to produce and maintain their skeletons. Increased organism pCO2 causes hypercapnia, an energetically costly physiological stress. OA alters seawater carbonate chemistry, limiting the carbonate available to form the calcium carbonate (CaCO3) minerals used to build skeletons. The reduced saturation state of CaCO3 also causes corrosion of CaCO3 structures. Global change is also accelerating coastal acidification driven by land-run off (e.g. acid soil leachates, tannic acid). Building and maintaining marine biomaterials in the face of changing climate will depend on the balance between calcification and dissolution. Overall, in response to environmental acidification, many calcifiers produce less biomineral and so have smaller body size. Studies of skeleton development in echinoderms and molluscs across life stages show the stunting effect of OA. For corals, linear extension may be maintained, but at the expense of less dense biomineral. Conventional metrics used to quantify growth and calcification need to be augmented by characterisation of the changes to biomineral structure and mechanical integrity caused by environmental acidification. Scanning electron microscopy and microcomputed tomography of corals, tube worms and sea urchins exposed to experimental (laboratory) and natural (vents, coastal run off) acidification show a less dense biomineral with greater porosity and a larger void space. For bivalves, CaCO3 crystal deposition is more chaotic in response to both ocean and coastal acidification. Biomechanics tests reveal that these changes result in weaker, more fragile skeletons, compromising their vital protective roles. Vulnerabilities differ among taxa and depend on acidification level. Climate warming has the potential to ameliorate some of the negative effects of acidification but may also make matters worse. The integrative morphology-ecomechanics approach is key to understanding how marine biominerals will perform in the face of changing climate.
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Affiliation(s)
- Maria Byrne
- School of Medical Science and School of Life and Environmental Science, The University of Sydney, NSW 2006, Australia
- Corresponding author: School of Medical Science and School of Life and Environmental Science, The University of Sydney, NSW 2006, Australia.
| | - Susan Fitzer
- Institute of Aquaculture, University of Stirling, Stirling, FK9 4LA, UK
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Díaz-Castañeda V, Cox TE, Gazeau F, Fitzer S, Delille J, Alliouane S, Gattuso JP. Ocean acidification affects calcareous tube growth in adult stage and reared offspring of serpulid polychaetes. J Exp Biol 2019; 222:jeb.196543. [DOI: 10.1242/jeb.196543] [Citation(s) in RCA: 10] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/19/2018] [Accepted: 05/15/2019] [Indexed: 01/09/2023]
Abstract
The energetically costly transition from free-swimming larvae to benthic life stage and maintenance of a calcareous structure can make calcifying marine invertebrates vulnerable to ocean acidification. The first goal of this study was to evaluate the impacts of ocean acidification on calcified tube growth for two Serpulidae polychaete worms. Spirorbis sp. and Spirobranchus triqueter were collected at 11 m depth from the Northwest Mediterranean Sea and maintained for 30 and 90 d, at three mean pHT levels (total scale) of 8.1 (ambient), 7.7, and 7.4. Moderately decreased tube elongation rates were observed in both species at a pHT of 7.7 while severe reductions occurred at pHT 7.4. There was visual evidence of dissolution and tubes were more fragile at lower pH but, fragility was not attributed to changes in fracture toughness. Instead, it appeared to be due to the presence of larger alveoli covered in a thinner calcareous layer. The second objective of the study was to test for effects in offspring development of the species S. triqueter. Spawning was induced, and offspring were reared in the same pH conditions the parents experienced. Trochophore size was reduced at the lowest pH level but settlement success was similar across pH conditions. Post-settlement tube growth was most affected. At 38 d post-settlement, juvenile tubes at pHT of 7.7 and 7.4 were half the size of those at pHT 8.1. Results suggest future carbonate chemistry will negatively affect initiation and persistence of both biofouling and epiphytic polychaete tube worms.
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Affiliation(s)
- V. Díaz-Castañeda
- Centro de Investigación Científica y Educación Superior de Ensenada, Departmento de Ecología Marina. Carret. Tij. - Ensenada 3918, C.P. 22860 Ensenada, Baja California, México
| | - T. E. Cox
- University of New Orleans, Department of Biological Sciences 2000 Lakeshore Drive New Orleans, LA, 70148 USA
- Sorbonne Université, CNRS, Laboratoire d'Océanographie de Villefranche, 181 chemin du Lazaret, F-06230 Villefranche-sur-mer, France
| | - F. Gazeau
- Sorbonne Université, CNRS, Laboratoire d'Océanographie de Villefranche, 181 chemin du Lazaret, F-06230 Villefranche-sur-mer, France
| | - S. Fitzer
- Institute of Aquaculture, University of Stirling, FK9 4LA, Scotland, UK
| | - J. Delille
- Sorbonne Université, CNRS, Laboratoire d'Océanographie de Villefranche, 181 chemin du Lazaret, F-06230 Villefranche-sur-mer, France
| | - S. Alliouane
- Sorbonne Université, CNRS, Laboratoire d'Océanographie de Villefranche, 181 chemin du Lazaret, F-06230 Villefranche-sur-mer, France
| | - J.-P. Gattuso
- Sorbonne Université, CNRS, Laboratoire d'Océanographie de Villefranche, 181 chemin du Lazaret, F-06230 Villefranche-sur-mer, France
- Institute for Sustainable Development and International Relations, Sciences Po, 27 rue Saint Guillaume, F-75007 Paris, France
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Brown NEM, Milazzo M, Rastrick SPS, Hall-Spencer JM, Therriault TW, Harley CDG. Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. GLOBAL CHANGE BIOLOGY 2018; 24:e112-e127. [PMID: 28762601 DOI: 10.1111/gcb.13856] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/06/2017] [Accepted: 07/14/2017] [Indexed: 06/07/2023]
Abstract
Ocean acidification may have far-reaching consequences for marine community and ecosystem dynamics, but its full impacts remain poorly understood due to the difficulty of manipulating pCO2 at the ecosystem level to mimic realistic fluctuations that occur on a number of different timescales. It is especially unclear how quickly communities at various stages of development respond to intermediate-scale pCO2 change and, if high pCO2 is relieved mid-succession, whether past acidification effects persist, are reversed by alleviation of pCO2 stress, or are worsened by departures from prior high pCO2 conditions to which organisms had acclimatized. Here, we used reciprocal transplant experiments along a shallow water volcanic pCO2 gradient to assess the importance of the timing and duration of high pCO2 exposure (i.e., discrete events at different stages of successional development vs. continuous exposure) on patterns of colonization and succession in a benthic fouling community. We show that succession at the acidified site was initially delayed (less community change by 8 weeks) but then caught up over the next 4 weeks. These changes in succession led to homogenization of communities maintained in or transplanted to acidified conditions, and altered community structure in ways that reflected both short- and longer-term acidification history. These community shifts are likely a result of interspecific variability in response to increased pCO2 and changes in species interactions. High pCO2 altered biofilm development, allowing serpulids to do best at the acidified site by the end of the experiment, although early (pretransplant) negative effects of pCO2 on recruitment of these worms were still detectable. The ascidians Diplosoma sp. and Botryllus sp. settled later and were more tolerant to acidification. Overall, transient and persistent acidification-driven changes in the biofouling community, via both past and more recent exposure, could have important implications for ecosystem function and food web dynamics.
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Affiliation(s)
- Norah E M Brown
- Department of Zoology, University of British Columbia, Vancouver, BC, Canada
| | - Marco Milazzo
- DiSTeM, CoNISMa, University of Palermo, Palermo, Italy
| | - Samuel P S Rastrick
- Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, UK
- Institute of Marine Research, Bergen, Norway
| | - Jason M Hall-Spencer
- Marine Biology and Ecology Research Centre, University of Plymouth, Plymouth, UK
- Shimoda Marine Research Centre, Tsukuba University, Tsukuba, Japan
| | | | - Christopher D G Harley
- Department of Zoology, University of British Columbia, Vancouver, BC, Canada
- Institute for the Oceans and Fisheries, University of British Columbia, Vancouver, BC, Canada
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8
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Duquette A, McClintock JB, Amsler CD, Pérez-Huerta A, Milazzo M, Hall-Spencer JM. Effects of ocean acidification on the shells of four Mediterranean gastropod species near a CO 2 seep. MARINE POLLUTION BULLETIN 2017; 124:917-928. [PMID: 28823551 DOI: 10.1016/j.marpolbul.2017.08.007] [Citation(s) in RCA: 29] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/07/2016] [Revised: 08/02/2017] [Accepted: 08/04/2017] [Indexed: 06/07/2023]
Abstract
Marine CO2 seeps allow the study of the long-term effects of elevated pCO2 (ocean acidification) on marine invertebrate biomineralization. We investigated the effects of ocean acidification on shell composition and structure in four ecologically important species of Mediterranean gastropods (two limpets, a top-shell snail, and a whelk). Individuals were sampled from three sites near a volcanic CO2 seep off Vulcano Island, Italy. The three sites represented ambient (8.15pH), moderate (8.03pH) and low (7.73pH) seawater mean pH. Shell mineralogy, microstructure, and mechanical strength were examined in all four species. We found that the calcite/aragonite ratio could vary and increased significantly with reduced pH in shells of one of the two limpet species. Moreover, each of the four gastropods displayed reductions in either inner shell toughness or elasticity at the Low pH site. These results suggest that near-future ocean acidification could alter shell biomineralization and structure in these common gastropods.
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Affiliation(s)
- Ashley Duquette
- Department of Biology, University of Alabama at Birmingham, Birmingham, AL 35294, USA
| | - James B McClintock
- Department of Biology, University of Alabama at Birmingham, Birmingham, AL 35294, USA.
| | - Charles D Amsler
- Department of Biology, University of Alabama at Birmingham, Birmingham, AL 35294, USA
| | - Alberto Pérez-Huerta
- Department of Geological Sciences, University of Alabama, Tuscaloosa, AL 35487, USA
| | - Marco Milazzo
- Dipartimento di Scienze della Terra e del Mare, University of Palermo, 90123 Palermo, Italy
| | - Jason M Hall-Spencer
- Marine Biology and Ecology Research Centre, School of Marine Science and Engineering, Plymouth University, Plymouth, UK
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9
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Wang Z, Wang Y, Yan C. Simulating ocean acidification and CO2 leakages from carbon capture and storage to assess the effects of pH reduction on cladoceran Moina mongolica Daday and its progeny. CHEMOSPHERE 2016; 155:621-629. [PMID: 27160436 DOI: 10.1016/j.chemosphere.2016.04.086] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/20/2016] [Revised: 03/22/2016] [Accepted: 04/22/2016] [Indexed: 06/05/2023]
Abstract
In order to evaluate the effects of pH reduction in seawater as a result of increasing levels of atmospheric CO2, laboratory-scale experiments simulating the scenarios of ocean acidification (OA) and CO2 leakages of carbon capture and storage (CCS) were performed using the model organism Moina mongolica Daday. The LpH50s calculated in cladoceran toxicity tests showed that M. mongolica exhibited intermediate sensitivity to OA, which varied among species and with ontogeny, when compared with different phyla or classes of marine biota. Survival, reproduction and fecundity of parthenogenetic females were evaluated after 21-day exposures. Results showed that increased acidity significantly reduced the rate of reproduction of M. mongolica resulting in a decreased intrinsic rate of natural increase (rm) across the gradients of pH reduction. The analysis of macromolecule contents in neonates suggested that nutritional status in progeny from all broods were significantly reduced as seawater pH decreased, with increasing magnitude in latter broods, except the contents of protein from two former broods and lipids from the first brood. Our findings clearly showed that for this ecologically and economically important fish species, the negative effects of pH reduction on both "quantity" and "quality" of progeny may have far-reaching implications, providing direct evidence that OA could influence the energetic transfer of marine food web and ecosystem functions in acidified oceans in the future.
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Affiliation(s)
- Zaosheng Wang
- Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, 1799 Jimei Boulevard, Xiamen, 361021, People's Republic of China.
| | - Youshao Wang
- State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 510301, People's Republic of China
| | - Changzhou Yan
- Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, 1799 Jimei Boulevard, Xiamen, 361021, People's Republic of China
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10
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Li C, Meng Y, He C, Chan VBS, Yao H, Thiyagarajan V. Mechanical robustness of the calcareous tubeworm Hydroides elegans: warming mitigates the adverse effects of ocean acidification. BIOFOULING 2016; 32:191-204. [PMID: 26820060 DOI: 10.1080/08927014.2015.1129532] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/15/2015] [Accepted: 12/01/2015] [Indexed: 06/05/2023]
Abstract
Development of antifouling strategies requires knowledge of how fouling organisms would respond to climate change associated environmental stressors. Here, a calcareous tube built by the tubeworm, Hydroides elegans, was used as an example to evaluate the individual and interactive effects of ocean acidification (OA), warming and reduced salinity on the mechanical properties of a tube. Tubeworms produce a mechanically weaker tube with less resistance to simulated predator attack under OA (pH 7.8). Warming (29°C) increased tube volume, tube mineral density and the tube's resistance to a simulated predatory attack. A weakening effect by OA did not make the removal of tubeworms easier except for the earliest stage, in which warming had the least effect. Reduced salinity (27 psu) did not affect tubes. This study showed that both mechanical analysis and computational modeling can be integrated with biofouling research to provide insights into how fouling communities might develop in future ocean conditions.
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Affiliation(s)
- Chaoyi Li
- a The Swire Institute of Marine Sciences and School of Biological Sciences , The University of Hong Kong , Hong Kong SAR , China
| | - Yuan Meng
- a The Swire Institute of Marine Sciences and School of Biological Sciences , The University of Hong Kong , Hong Kong SAR , China
| | - Chong He
- b Department of Mechanical Engineering , The Hong Kong Polytechnic University , Hong Kong SAR , China
| | - Vera B S Chan
- c Department of Biological Sciences , University of Clemson , Clemson , SC , USA
| | - Haimin Yao
- b Department of Mechanical Engineering , The Hong Kong Polytechnic University , Hong Kong SAR , China
| | - V Thiyagarajan
- a The Swire Institute of Marine Sciences and School of Biological Sciences , The University of Hong Kong , Hong Kong SAR , China
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11
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Lane A, Campanati C, Dupont S, Thiyagarajan V. Trans-generational responses to low pH depend on parental gender in a calcifying tubeworm. Sci Rep 2015; 5:10847. [PMID: 26039184 PMCID: PMC4454138 DOI: 10.1038/srep10847] [Citation(s) in RCA: 23] [Impact Index Per Article: 2.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/03/2014] [Accepted: 04/24/2015] [Indexed: 11/25/2022] Open
Abstract
The uptake of anthropogenic CO2 emissions by oceans has started decreasing pH and carbonate ion concentrations of seawater, a process called ocean acidification (OA). Occurring over centuries and many generations, evolutionary adaptation and epigenetic transfer will change species responses to OA over time. Trans-generational responses, via genetic selection or trans-generational phenotypic plasticity, differ depending on species and exposure time as well as differences between individuals such as gender. Males and females differ in reproductive investment and egg producing females may have less energy available for OA stress responses. By crossing eggs and sperm from the calcareous tubeworm Hydroides elegans (Haswell, 1883) raised in ambient (8.1) and low (7.8) pH environments, we observed that paternal and maternal low pH experience had opposite and additive effects on offspring. For example, when compared to offspring with both parents from ambient pH, growth rates of offspring of fathers or mothers raised in low pH were higher or lower respectively, but there was no difference when both parents were from low pH. Gender differences may result in different selection pressures for each gender. This may result in overestimates of species tolerance and missed opportunities of potentially insightful comparisons between individuals of the same species.
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Affiliation(s)
- Ackley Lane
- The Swire Institute of Marine Science and School of Biological Sciences, The University of Hong Kong, Hong Kong SAR
| | - Camilla Campanati
- The Swire Institute of Marine Science and School of Biological Sciences, The University of Hong Kong, Hong Kong SAR
| | - Sam Dupont
- Department of Biological and Environmental Sciences, The Sven Lovén Centre for Marine Sciences - Kristineberg, University of Gothenburg, Fiskebäckskil, Sweden
| | - Vengatesen Thiyagarajan
- The Swire Institute of Marine Science and School of Biological Sciences, The University of Hong Kong, Hong Kong SAR
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