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Zhang S, Solan M, Tarhan L. Global distribution and environmental correlates of marine bioturbation. Curr Biol 2024; 34:2580-2593.e4. [PMID: 38781955 DOI: 10.1016/j.cub.2024.04.065] [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: 12/08/2023] [Revised: 03/27/2024] [Accepted: 04/29/2024] [Indexed: 05/25/2024]
Abstract
The activities of marine sediment-dwelling invertebrates play a fundamental role in mediating major biogeochemical cycles and have profoundly shaped the evolution of marine systems. Yet there remains a paucity of global marine data describing bioturbation intensities and mixed layer depths and interrogating how these vary with multiple environmental and ecological factors at a system scale. We applied an ensemble of tree-based machine learning techniques to resolve a global map and determine the environmental and ecological correlates most closely associated with bioturbation. We find that bioturbation intensity and the depth of the sediment mixed layer each reflect different associations with a consortium of environmental and ecological parameters, and that bioturbation intensities are much more readily predicted than sediment mixed layer depths from these correlates. Furthermore, we find that the bioturbation intensity, the depth of the sediment mixed layer, and their environmental and ecological correlates differ between shallow marine and open-ocean settings. Our findings provide new insights into the importance of potential drivers of ancient sediment mixing recorded by geologic archives. These results also highlight that climate change may, in the near future, drive shifts in bioturbation and reciprocal fundamental changes in benthic functioning.
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Affiliation(s)
- Shuang Zhang
- Department of Oceanography, Texas A&M University, 3146 TAMU, College Station, TX 77843, USA; Department of Earth and Planetary Sciences, Yale University, P.O. Box 208109, New Haven, CT 06520, USA.
| | - Martin Solan
- Ocean and Earth Science, National Oceanography Centre, Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK
| | - Lidya Tarhan
- Department of Earth and Planetary Sciences, Yale University, P.O. Box 208109, New Haven, CT 06520, USA.
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2
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Febvre C, Goldblatt C, El-Sabaawi R. Thermal performance of ecosystems: Modeling how physiological responses to temperature scale up in communities. J Theor Biol 2024; 585:111792. [PMID: 38513968 DOI: 10.1016/j.jtbi.2024.111792] [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: 10/11/2023] [Revised: 02/20/2024] [Accepted: 03/10/2024] [Indexed: 03/23/2024]
Abstract
Understanding how ecosystems respond to their environmental temperature is a major challenge. Thermodynamic constraints on species' metabolic rates are expected to affect ecosystem characteristics, but species interactions and interspecific variation in physiological thermal response curves (TRC) may obscure ecosystem-level responses to temperature. As a result, macroecological patterns related to temperature are still poorly understood. We investigate how physiological TRC scale up to ecosystem-level thermal responses by modifying the Tangled Nature (TaNa) model, a stochastic network model of ecology and evolution. We include new parameterizations that make reproduction, death, and mutation temperature-dependent. We find that ecosystem survival probability depends on how the minimum fitness required for species survival varies with temperature. The thermal response of ecosystem survival probability is the only ecosystem property that is sensitive to interspecific variation in TRC. Species richness scales up directly from the TRC of mutation rate, and average species population sizes are inversely related to mutation rate, with Species Abundance Distributions (SADs) exhibiting more rare species in warmer temperatures. Interactions between species are also inversely related to mutation, with positive interactions occurring more frequently in colder temperatures. The abundance of surviving ecosystems is not sensitive to temperature. This work helps clarify the specific relationships between physiological responses to temperature and ecosystem-level repercussions when species are interacting and adapting to their thermal environments.
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Affiliation(s)
- Camille Febvre
- School of Earth & Ocean Sciences, University of Victoria, 3600 Finnerty Road, Victoria, BC, Canada; Department of Biology, University of Victoria, 3600 Finnerty Road, Victoria, BC, Canada.
| | - Colin Goldblatt
- School of Earth & Ocean Sciences, University of Victoria, 3600 Finnerty Road, Victoria, BC, Canada
| | - Rana El-Sabaawi
- Department of Biology, University of Victoria, 3600 Finnerty Road, Victoria, BC, Canada
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3
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Wang Z, Fang C, Yang C, Zhang G, Sun D. Latitudinal gradient and influencing factors of deep-sea particle export along the Kyushu-Palau Ridge in the Philippine Sea. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 906:167460. [PMID: 37797769 DOI: 10.1016/j.scitotenv.2023.167460] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/12/2023] [Revised: 09/21/2023] [Accepted: 09/27/2023] [Indexed: 10/07/2023]
Abstract
The export of particulate organic matter (POM) to deep-sea is crucial for deep-sea ecosystems. However, in situ measurements of large-scale POM export flux are scarce in the tropical and subtropical western Pacific, leading to reliance on biogeochemical models or sediment trap data from a few stations. To address this gap, the underwater vision profiler was used to measure particulate density and to calculate particulate organic carbon (POC) fluxes along the Kyushu-Palau Ridge (KPR) in the Philippine Sea. The results revealed a significant latitudinal gradient of POC fluxes: 37 % of the POC output from 200 m depth was preserved to 2000 m in the Western Pacific Warm Pool and up to 51 % was preserved in the North Pacific Subtropical Gyre. The near-bottom POC fluxes north of 25°N (1.64 ± 0.80 mg m-2 d-1) were significantly higher than the average near-bottom value of the entire transect (0.60 ± 0.43 mg m-2 d-1). Multiple linear regression analysis showed that the chlorophyll concentration had a significant positive effect on the POC fluxes at all depths, except near the bottom, while local factors such as mesoscale eddies and the interaction effect between the topography and current velocity only had significant effects on the POC fluxes at depths of >2000 m. Particle size spectrum analysis revealed that particles ranging from 64 to 323 μm in size exerted a dominant influence on the increase in the POC fluxes in the near-bottom layers situated north of 25°N. These findings indicated that the spatial heterogeneity of POC fluxes in the western Pacific was governed not only by upper ocean primary productivity but also by mesoscale processes, current velocity, and topography. These results provided crucial fundamental information for cartography of the distribution and simulation of the dynamics of deep-sea organisms along the KPR in the Philippine Sea.
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Affiliation(s)
- Ziyu Wang
- Key Laboratory of Marine Ecosystem Dynamics, Second Institute of Oceanography, Ministry of Natural Resource, Hangzhou 310012, China
| | - Chen Fang
- College of Oceanography, Hohai University, Nanjing 210024, China
| | - Chenghao Yang
- State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Guoyin Zhang
- Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Dong Sun
- Key Laboratory of Marine Ecosystem Dynamics, Second Institute of Oceanography, Ministry of Natural Resource, Hangzhou 310012, China; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519000, China.
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4
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Beck KK, Nierste J, Schmidt-Grieb GM, Lüdtke E, Naab C, Held C, Nehrke G, Steinhoefel G, Laudien J, Richter C, Wall M. Ontogenetic differences in the response of the cold-water coral Caryophyllia huinayensis to ocean acidification, warming and food availability. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 900:165565. [PMID: 37495133 DOI: 10.1016/j.scitotenv.2023.165565] [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: 03/23/2023] [Revised: 07/03/2023] [Accepted: 07/14/2023] [Indexed: 07/28/2023]
Abstract
Cold-water corals (CWCs) are considered vulnerable to environmental changes. However, previous studies have focused on adult CWCs and mainly investigated the short-term effects of single stressors. So far, the effects of environmental changes on different CWC life stages are unknown, both for single and multiple stressors and over long time periods. Therefore, we conducted a six-month aquarium experiment with three life stages of Caryophyllia huinayensis to study their physiological response (survival, somatic growth, calcification and respiration) to the interactive effects of aragonite saturation (0.8 and 2.5), temperature (11 and 15 °C) and food availability (8 and 87 μg C L-1). The response clearly differed between life stages and measured traits. Elevated temperature and reduced feeding had the greatest effects, pushing the corals to their physiological limits. Highest mortality was observed in adult corals, while calcification rates decreased the most in juveniles. We observed a three-month delay in response, presumably because energy reserves declined, suggesting that short-term experiments overestimate coral resilience. Elevated summer temperatures and reduced food supply are likely to have the greatest impact on live CWCs in the future, leading to reduced coral growth and population shifts due to delayed juvenile maturation and high adult mortality.
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Affiliation(s)
- Kristina K Beck
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany; University of Bremen, Bremen, Germany.
| | - Jan Nierste
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany; University of Rostock, Rostock, Germany
| | | | - Esther Lüdtke
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
| | - Christoph Naab
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany; University of Augsburg, Augsburg, Germany
| | - Christoph Held
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
| | - Gernot Nehrke
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
| | - Grit Steinhoefel
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
| | - Jürgen Laudien
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
| | - Claudio Richter
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany; University of Bremen, Bremen, Germany
| | - Marlene Wall
- Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany; GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany
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5
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Clerc C, Aumont O, Bopp L. Filter-feeding gelatinous macrozooplankton response to climate change and implications for benthic food supply and global carbon cycle. GLOBAL CHANGE BIOLOGY 2023; 29:6383-6398. [PMID: 37751177 DOI: 10.1111/gcb.16942] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/20/2023] [Revised: 07/21/2023] [Accepted: 08/28/2023] [Indexed: 09/27/2023]
Abstract
It is often suggested that gelatinous zooplankton may benefit from anthropogenic pressures of all kinds and in particular from climate change. Large pelagic tunicates, for example, are likely to be favored over other types of macrozooplankton due to their filter-feeding mode, which gives them access to small preys thought to be less affected by climate change than larger preys. In this study, we provide model-based estimate of potential community changes in macrozooplankton composition and estimate for the first time their effects on benthic food supply and on the ocean carbon cycle under two 21st-century climate-change scenarios. Forced with output from an Earth System Model climate projections, our ocean biogeochemical model simulates a large reduction in macrozooplankton biomass in response to anthropogenic climate change, but shows that gelatinous macrozooplankton are less affected than nongelatinous macrozooplankton, with global biomass declines estimated at -2.8% and -3.5%, respectively, for every 1°C of warming. The inclusion of gelatinous macrozooplankon in our ocean biogeochemical model has a limited effect on anthropogenic carbon uptake in the 21st century, but impacts the projected decline in particulate organic matter fluxes in the deep ocean. In subtropical oligotrophic gyres, where gelatinous zooplankton dominate macrozooplankton, the decline in the amount of organic matter reaching the seafloor is reduced by a factor of 2 when gelatinous macrozooplankton are considered (-17.5% vs. -29.7% when gelatinous macrozooplankton are not considered, all for 2100 under RCP8.5). The shift to gelatinous macrozooplankton in the future ocean therefore buffers the decline in deep carbon fluxes and should be taken into account when assessing potential changes in deep carbon storage and the risks that deep ecosystems may face when confronted with a decline in their food source.
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Affiliation(s)
- Corentin Clerc
- LMD/IPSL, Ecole Normale Supérieure/Université PSL, CNRS, Ecole Polytechnique, Sorbonne Université, Paris, France
| | - Olivier Aumont
- LOCEAN/IPSL, IRD, CNRS, MNHN, Sorbonne Université, Paris, France
| | - Laurent Bopp
- LMD/IPSL, Ecole Normale Supérieure/Université PSL, CNRS, Ecole Polytechnique, Sorbonne Université, Paris, France
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6
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Maier SR, Brooke S, De Clippele LH, de Froe E, van der Kaaden AS, Kutti T, Mienis F, van Oevelen D. On the paradox of thriving cold-water coral reefs in the food-limited deep sea. Biol Rev Camb Philos Soc 2023; 98:1768-1795. [PMID: 37236916 DOI: 10.1111/brv.12976] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/21/2022] [Revised: 04/26/2023] [Accepted: 05/01/2023] [Indexed: 05/28/2023]
Abstract
The deep sea is amongst the most food-limited habitats on Earth, as only a small fraction (<4%) of the surface primary production is exported below 200 m water depth. Here, cold-water coral (CWC) reefs form oases of life: their biodiversity compares with tropical coral reefs, their biomass and metabolic activity exceed other deep-sea ecosystems by far. We critically assess the paradox of thriving CWC reefs in the food-limited deep sea, by reviewing the literature and open-access data on CWC habitats. This review shows firstly that CWCs typically occur in areas where the food supply is not constantly low, but undergoes pronounced temporal variation. High currents, downwelling and/or vertically migrating zooplankton temporally boost the export of surface organic matter to the seabed, creating 'feast' conditions, interspersed with 'famine' periods during the non-productive season. Secondly, CWCs, particularly the most common reef-builder Desmophyllum pertusum (formerly known as Lophelia pertusa), are well adapted to these fluctuations in food availability. Laboratory and in situ measurements revealed their dietary flexibility, tissue reserves, and temporal variation in growth and energy allocation. Thirdly, the high structural and functional diversity of CWC reefs increases resource retention: acting as giant filters and sustaining complex food webs with diverse recycling pathways, the reefs optimise resource gains over losses. Anthropogenic pressures, including climate change and ocean acidification, threaten this fragile equilibrium through decreased resource supply, increased energy costs, and dissolution of the calcium-carbonate reef framework. Based on this review, we suggest additional criteria to judge the health of CWC reefs and their chance to persist in the future.
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Affiliation(s)
- Sandra R Maier
- Greenland Climate Research Centre, Greenland Institute of Natural Resources, Kivioq 2, PO Box 570, Nuuk, 3900, Greenland
- Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research (NIOZ), Korringaweg 7, Yerseke, 4401 NT, The Netherlands
| | - Sandra Brooke
- Coastal & Marine Laboratory, Florida State University, 3618 Coastal Highway 98, St. Teresa, FL, 32327, USA
| | - Laurence H De Clippele
- Changing Oceans Research Group, School of GeoSciences, University of Edinburgh, Grant Institute, King's Buildings, Edinburgh, EH9 3FE, UK
| | - Evert de Froe
- Centre for Fisheries Ecosystem Research, Fisheries and Marine Institute at Memorial University of Newfoundland, 155 Ridge Rd, St. John's, NL A1C 5R3, Newfoundland and Labrador, Canada
- Department of Ocean Systems, Royal Netherlands Institute for Sea Research (NIOZ), PO Box 59, Den Burg (Texel), 1790 AB, The Netherlands
| | - Anna-Selma van der Kaaden
- Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research (NIOZ), Korringaweg 7, Yerseke, 4401 NT, The Netherlands
| | - Tina Kutti
- Institute of Marine Research (IMR), PO box 1870 Nordnes, Bergen, NO-5817, Norway
| | - Furu Mienis
- Department of Ocean Systems, Royal Netherlands Institute for Sea Research (NIOZ), PO Box 59, Den Burg (Texel), 1790 AB, The Netherlands
| | - Dick van Oevelen
- Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research (NIOZ), Korringaweg 7, Yerseke, 4401 NT, The Netherlands
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7
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Mercury isotopic evidence for the importance of particles as a source of mercury to marine organisms. Proc Natl Acad Sci U S A 2022; 119:e2208183119. [PMID: 36279440 PMCID: PMC9636975 DOI: 10.1073/pnas.2208183119] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/18/2022] Open
Abstract
The origin of methylmercury in pelagic fish remains unclear, with many unanswered questions regarding the production and degradation of this neurotoxin in the water column. We used mercury (Hg) stable isotope ratios of marine particles and biota to elucidate the cycling of methylmercury prior to incorporation into the marine food web. The Hg isotopic composition of particles, zooplankton, and fish reveals preferential methylation of Hg within small (< 53 µm) marine particles in the upper 400 m of the North Pacific Ocean. Mass-dependent Hg isotope ratios (δ
202
Hg) recorded in small particles overlap with previously estimated δ
202
Hg values for methylmercury sources to Pacific and Atlantic Ocean food webs. Particulate compound specific isotope analysis of amino acids (CSIA-AA) yield δ
15
N values that indicate more-significant microbial decomposition in small particles compared to larger particles. CSIA-AA and Hg isotope data also suggest that large particles (> 53 µm) collected in the equatorial ocean are distinct from small particles and resemble fecal pellets. Additional evidence for Hg methylation within small particles is provided by a statistical mixing model of even mass–independent (Δ
200
Hg and Δ
204
Hg) isotope values, which demonstrates that Hg within near-surface marine organisms (0–150 m) originates from a combination of rainfall and marine particles. In contrast, in meso- and upper bathypelagic organisms (200–1,400 m), the majority of Hg originates from marine particles with little input from wet deposition. The occurrence of methylation within marine particles is supported further by a correlation between Δ
200
Hg and Δ
199
Hg values, demonstrating greater overlap in the Hg isotopic composition of marine organisms with marine particles than with total gaseous Hg or wet deposition.
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8
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Martins I, Godinho A, Rakka M, Carreiro-Silva M. Beyond deep-sea mining sublethal effects: Delayed mortality from acute Cu exposure of the cold-water octocoral Viminella flagellum. MARINE POLLUTION BULLETIN 2022; 183:114051. [PMID: 36058176 DOI: 10.1016/j.marpolbul.2022.114051] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/14/2022] [Revised: 08/12/2022] [Accepted: 08/13/2022] [Indexed: 06/15/2023]
Abstract
The potential release of metals, especially copper (Cu) during mining of seafloor massive sulphides (SMS), represents a potential toxicological threat to cold-water coral (CWC) habitats. Herein, we evaluated for the first time the response of the whip coral Viminella flagellum to short-term acute Cu exposure. Nubbins of V. flagellum were exposed to Cu concentrations of 0 (control); 60; 150; 250; 450 and 600 μg/L for 96 h. After exposure, V. flagellum nubbins were transferred to a continuous flow-through aquarium and feed once a day for 3 weeks. No immediate mortality was detected during the short-term Cu exposure. However, a delayed mortality, which was concentration dependent was observed. The first signs of tissue loss occurred after 1 week of recovery in non-contaminated conditions in V. flagellum nubbins previously exposed to Cu concentrations of 60 and 150 μg/L followed by nubbins exposed to Cu concentrations of 250, 450 μg/L after 2 weeks and 600 μg/L after 3 weeks. A delayed mortality impact should be considered in future Cu tolerance experiments and scenarios of deep-sea mining exploitation.
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Affiliation(s)
- Inês Martins
- Institute of Marine Sciences - Okeanos, University of the Azores, Rua Professor Doutor Frederico Machado 4, 9901-862 Horta, Portugal; Instituto do Mar - IMAR, University of the Azores, Horta, Portugal.
| | - António Godinho
- Institute of Marine Sciences - Okeanos, University of the Azores, Rua Professor Doutor Frederico Machado 4, 9901-862 Horta, Portugal; Instituto do Mar - IMAR, University of the Azores, Horta, Portugal
| | - Maria Rakka
- Institute of Marine Sciences - Okeanos, University of the Azores, Rua Professor Doutor Frederico Machado 4, 9901-862 Horta, Portugal; Instituto do Mar - IMAR, University of the Azores, Horta, Portugal
| | - Marina Carreiro-Silva
- Institute of Marine Sciences - Okeanos, University of the Azores, Rua Professor Doutor Frederico Machado 4, 9901-862 Horta, Portugal; Instituto do Mar - IMAR, University of the Azores, Horta, Portugal
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9
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Lörz AN, Kaiser S, Oldeland J, Stolter C, Kürzel K, Brix S. Biogeography, diversity and environmental relationships of shelf and deep-sea benthic Amphipoda around Iceland. PeerJ 2021; 9:e11898. [PMID: 34447625 PMCID: PMC8364320 DOI: 10.7717/peerj.11898] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/30/2021] [Accepted: 07/13/2021] [Indexed: 11/24/2022] Open
Abstract
The waters around Iceland, bounding the Northern North Atlantic and the Nordic seas, are a region characterized by complex hydrography and seabed topography. This and the presence of the Greenland-Iceland-Faroe-Scotland ridge (GIFR) are likely to have a major impact on the diversity and distribution of the benthic fauna there. Biodiversity in this region is also under increasing threat from climate-induced changes, ocean warming and acidification in particular, affecting the marine realm. The aim of the present study was to investigate the biodiversity and distributional patterns of amphipod crustaceans in Icelandic waters and how it relates to environmental variables and depth. A comprehensive data set from the literature and recent expeditions was compiled constituting distributional records for 355 amphipod species across a major depth gradient (18–3,700 m). Using a 1° hexagonal grid to map amphipod distributions and a set of environmental factors (depth, pH, phytobiomass, velocity, dissolved oxygen, dissolved iron, salinity and temperature) we could identify four distinct amphipod assemblages: A Deep-North, Deep-South, and a Coastal cluster as well as one restricted to the GIFR. In addition to depth, salinity and temperature were the main parameters that determined the distribution of amphipods. Diversity differed greatly between the depth clusters and was significantly higher in coastal and GIFR assemblages compared to the deep-sea clusters north and south of the GIFR. A variety of factors and processes are likely to be responsible for the perceived biodiversity patterns, which, however, appear to vary according to region and depth. Low diversity of amphipod communities in the Nordic basins can be interpreted as a reflection of the prevailing harsh environmental conditions in combination with a barrier effect of the GIFR. By contrast, low diversity of the deep North Atlantic assemblages might be linked to the variable nature of the oceanographic environment in the region over multiple spatio-temporal scales. Overall, our study highlights the importance of amphipods as a constituent part of Icelandic benthos. The strong responses of amphipod communities to certain water mass variables raise the question of whether and how their distribution will change due to climate alteration, which should be a focus of future studies.
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Affiliation(s)
- Anne-Nina Lörz
- Institute for Marine Ecosystems and Fisheries Science, Universität Hamburg, Hamburg, Germany
| | - Stefanie Kaiser
- Faculty of Biology and Environmental Protection, Department of Invertebrate Zoology and Hydrobiology, University of Łódź, Lodz, Poland
| | | | - Caroline Stolter
- Department Biology, Zoological Institute, Universität Hamburg, Hamburg, Germany
| | | | - Saskia Brix
- Deutsches Zentrum für Marine Biodiversität, Senckenberg Nature Research Society, Hamburg, Germany
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Friedlander AM, Goodell W, Giddens J, Easton EE, Wagner D. Deep-sea biodiversity at the extremes of the Salas y Gómez and Nazca ridges with implications for conservation. PLoS One 2021; 16:e0253213. [PMID: 34191822 PMCID: PMC8244922 DOI: 10.1371/journal.pone.0253213] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/01/2021] [Accepted: 05/29/2021] [Indexed: 12/29/2022] Open
Abstract
The Salas y Gómez and Nazca ridges are underwater mountain chains that stretch across 2,900 km in the southeastern Pacific and are recognized for their high biodiversity value and unique ecological characteristics. Explorations of deep-water ecosystems have been limited in this region, and elsewhere globally. To characterize community composition of mesophotic and deep-sea demersal fauna at seamounts in the region, we conducted expeditions to Rapa Nui (RN) and Salas y Gómez (SyG) islands in 2011 and Desventuradas Islands in 2013. Remote autonomous baited-cameras were used to conduct stationary video surveys between 150-1,850 m at RN/SyG (N = 20) and 75-2,363 m at Desventuradas (N = 27). Individual organisms were identified to the lowest possible taxonomic level and relative abundance was quantified with the maximum number of individuals per frame. Deployments were attributed with associated environmental variables (temperature, salinity, dissolved oxygen, nitrate, silicate, phosphate, chlorophyll-a, seamount age, and bathymetric position index [BPI]). We identified 55 unique invertebrate taxa and 66 unique fish taxa. Faunal community structure was highly dissimilar between and within subregions both for invertebrate (p < 0.001) and fish taxa (p = 0.022). For fishes, dogfish sharks (Squalidae) accounted for the greatest dissimilarity between subregions (18.27%), with mean abundances of 2.26 ± 2.49 at Desventuradas, an order of magnitude greater than at RN/SyG (0.21 ± 0.54). Depth, seamount age, broad-scale BPI, and nitrate explained most of the variation in both invertebrate (R2 = 0.475) and fish (R2 = 0.419) assemblages. Slightly more than half the deployments at Desventuradas (N = 14) recorded vulnerable marine ecosystem taxa such as corals and sponges. Our study supports mounting evidence that the Salas y Gómez and Nazca ridges are areas of high biodiversity and high conservation value. While Chile and Peru have recently established or proposed marine protected areas in this region, the majority of these ridges lie outside of national jurisdictions and are under threat from overfishing, plastic pollution, climate change, and potential deep-sea mining. Given its intrinsic value, this region should be comprehensively protected using the best available conservation measures to ensure that the Salas y Gómez and Nazca ridges remain a globally unique biodiversity hotspot.
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Affiliation(s)
- Alan M. Friedlander
- Pristine Seas, National Geographic Society, Washington, DC, United States of America
- Hawaiʿi Institute of Marine Biology, University of Hawaiʿi, Kāneʻohe, Hawaiʿi, United States of America
| | - Whitney Goodell
- Pristine Seas, National Geographic Society, Washington, DC, United States of America
- Exploration Technology Lab, National Geographic Society, Washington, DC, United States of America
| | - Jonatha Giddens
- Exploration Technology Lab, National Geographic Society, Washington, DC, United States of America
| | - Erin E. Easton
- Ecology and Sustainable Management of Oceanic Islands, Universidad Católica del Norte, Coquimbo, Chile
- School of Earth, Environmental, and Marine Sciences, University of Texas Rio Grande Valley, Brownsville, Texas, United States of America
| | - Daniel Wagner
- Conservation International, Center for Oceans, Arlington, VA, United States of America
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11
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Microbial dysbiosis reflects disease resistance in diverse coral species. Commun Biol 2021; 4:679. [PMID: 34083722 PMCID: PMC8175568 DOI: 10.1038/s42003-021-02163-5] [Citation(s) in RCA: 22] [Impact Index Per Article: 7.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/16/2020] [Accepted: 04/28/2021] [Indexed: 01/28/2023] Open
Abstract
Disease outbreaks have caused significant declines of keystone coral species. While forecasting disease outbreaks based on environmental factors has progressed, we still lack a comparative understanding of susceptibility among coral species that would help predict disease impacts on coral communities. The present study compared the phenotypic and microbial responses of seven Caribbean coral species with diverse life-history strategies after exposure to white plague disease. Disease incidence and lesion progression rates were evaluated over a seven-day exposure. Coral microbiomes were sampled after lesion appearance or at the end of the experiment if no disease signs appeared. A spectrum of disease susceptibility was observed among the coral species that corresponded to microbial dysbiosis. This dysbiosis promotes greater disease susceptiblity in coral perhaps through different tolerant thresholds for change in the microbiome. The different disease susceptibility can affect coral’s ecological function and ultimately shape reef ecosystems. MacKnight et al. compared the phenotypic and microbial responses of seven Caribbean coral species with diverse life-history strategies after exposure to white plague disease. The different species exhibited a spectrum of disease susceptibility and associated mortality that corresponded with their tolerances to microbial change, indicating that coral disease and microbial dysbiosis may ultimately shape reef ecosystems.
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12
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Abstract
Recent assessment reports by the Intergovernmental Panel on Climate Change (IPCC) and the Intergovernmental Science-Policy Platform on Biodiversity and Ecosystem Services (IPBES) have highlighted the risks to humanity arising from the unsustainable use of natural resources. Thus far, land, freshwater, and ocean exploitation have been the chief causes of biodiversity loss. Climate change is projected to be a rapidly increasing additional driver for biodiversity loss. Since climate change and biodiversity loss impact human societies everywhere, bold solutions are required that integrate environmental and societal objectives. As yet, most existing international biodiversity targets have overlooked climate change impacts. At the same time, climate change mitigation measures themselves may harm biodiversity directly. The Convention on Biological Diversity’s post-2020 framework offers the important opportunity to address the interactions between climate change and biodiversity and revise biodiversity targets accordingly by better aligning these with the United Nations Framework Convention on Climate Change Paris Agreement and the Sustainable Development Goals. We identify the considerable number of existing and proposed post-2020 biodiversity targets that risk being severely compromised due to climate change, even if other barriers to their achievement were removed. Our analysis suggests that the next set of biodiversity targets explicitly addresses climate change-related risks since many aspirational goals will not be feasible under even lower-end projections of future warming. Adopting more flexible and dynamic approaches to conservation, rather than static goals, would allow us to respond flexibly to changes in habitats, genetic resources, species composition, and ecosystem functioning and leverage biodiversity’s capacity to contribute to climate change mitigation and adaptation.
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13
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Gutt J, Isla E, Xavier JC, Adams BJ, Ahn IY, Cheng CHC, Colesie C, Cummings VJ, di Prisco G, Griffiths H, Hawes I, Hogg I, McIntyre T, Meiners KM, Pearce DA, Peck L, Piepenburg D, Reisinger RR, Saba GK, Schloss IR, Signori CN, Smith CR, Vacchi M, Verde C, Wall DH. Antarctic ecosystems in transition - life between stresses and opportunities. Biol Rev Camb Philos Soc 2020; 96:798-821. [PMID: 33354897 DOI: 10.1111/brv.12679] [Citation(s) in RCA: 29] [Impact Index Per Article: 7.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/27/2020] [Revised: 12/08/2020] [Accepted: 12/10/2020] [Indexed: 12/23/2022]
Abstract
Important findings from the second decade of the 21st century on the impact of environmental change on biological processes in the Antarctic were synthesised by 26 international experts. Ten key messages emerged that have stakeholder-relevance and/or a high impact for the scientific community. They address (i) altered biogeochemical cycles, (ii) ocean acidification, (iii) climate change hotspots, (iv) unexpected dynamism in seabed-dwelling populations, (v) spatial range shifts, (vi) adaptation and thermal resilience, (vii) sea ice related biological fluctuations, (viii) pollution, (ix) endangered terrestrial endemism and (x) the discovery of unknown habitats. Most Antarctic biotas are exposed to multiple stresses and considered vulnerable to environmental change due to narrow tolerance ranges, rapid change, projected circumpolar impacts, low potential for timely genetic adaptation, and migration barriers. Important ecosystem functions, such as primary production and energy transfer between trophic levels, have already changed, and biodiversity patterns have shifted. A confidence assessment of the degree of 'scientific understanding' revealed an intermediate level for most of the more detailed sub-messages, indicating that process-oriented research has been successful in the past decade. Additional efforts are necessary, however, to achieve the level of robustness in scientific knowledge that is required to inform protection measures of the unique Antarctic terrestrial and marine ecosystems, and their contributions to global biodiversity and ecosystem services.
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Affiliation(s)
- Julian Gutt
- Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Columbusstr., Bremerhaven, 27568, Germany
| | - Enrique Isla
- Institute of Marine Sciences-CSIC, Passeig Maritim de la Barceloneta 37-49, Barcelona, 08003, Spain
| | - José C Xavier
- University of Coimbra, MARE - Marine and Environmental Sciences Centre, Faculty of Sciences and Technology, Coimbra, Portugal.,British Antarctic Survey, Natural Environmental Research Council, High Cross, Madingley Road, Cambridge, CB3 OET, U.K
| | - Byron J Adams
- Department of Biology and Monte L. Bean Museum, Brigham Young University, Provo, UT, U.S.A
| | - In-Young Ahn
- Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon, 21990, South Korea
| | - C-H Christina Cheng
- Department of Evolution, Ecology and Behavior, University of Illinois, Urbana, IL, U.S.A
| | - Claudia Colesie
- School of GeoSciences, University of Edinburgh, Alexander Crum Brown Road, Edinburgh, EH9 3FF, U.K
| | - Vonda J Cummings
- National Institute of Water and Atmosphere Research Ltd (NIWA), 301 Evans Bay Parade, Greta Point, Wellington, New Zealand
| | - Guido di Prisco
- Institute of Biosciences and BioResources (IBBR), National Research Council (CNR), Via Pietro Castellino 111, Naples, I-80131, Italy
| | - Huw Griffiths
- British Antarctic Survey, Natural Environmental Research Council, High Cross, Madingley Road, Cambridge, CB3 OET, U.K
| | - Ian Hawes
- Coastal Marine Field Station, University of Waikato, 58 Cross Road, Tauranga, 3100, New Zealand
| | - Ian Hogg
- School of Science, University of Waikato, Private Bag 3105, Hamilton, 3240, New Zealand.,Canadian High Antarctic Research Station, Polar Knowledge Canada, PO Box 2150, Cambridge Bay, NU, X0B 0C0, Canada
| | - Trevor McIntyre
- Department of Life and Consumer Sciences, University of South Africa, Private Bag X6, Florida, 1710, South Africa
| | - Klaus M Meiners
- Australian Antarctic Division, Department of Agriculture, Water and the Environment, and Australian Antarctic Program Partnership, University of Tasmania, 20 Castray Esplanade, Battery Point, TAS, 7004, Australia
| | - David A Pearce
- British Antarctic Survey, Natural Environmental Research Council, High Cross, Madingley Road, Cambridge, CB3 OET, U.K.,Department of Applied Sciences, Faculty of Health and Life Sciences, Northumbria University at Newcastle, Northumberland Road, Newcastle upon Tyne, NE1 8ST, U.K
| | - Lloyd Peck
- British Antarctic Survey, Natural Environmental Research Council, High Cross, Madingley Road, Cambridge, CB3 OET, U.K
| | - Dieter Piepenburg
- Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Columbusstr., Bremerhaven, 27568, Germany
| | - Ryan R Reisinger
- Centre d'Etudes Biologique de Chizé, UMR 7372 du Centre National de la Recherche Scientifique - La Rochelle Université, Villiers-en-Bois, 79360, France
| | - Grace K Saba
- Center for Ocean Observing Leadership, Department of Marine and Coastal Sciences, Rutgers University, 71 Dudley Rd., New Brunswick, NJ, 08901, U.S.A
| | - Irene R Schloss
- Instituto Antártico Argentino, Buenos Aires, Argentina.,Centro Austral de Investigaciones Científicas, Bernardo Houssay 200, Ushuaia, Tierra del Fuego, CP V9410CAB, Argentina.,Universidad Nacional de Tierra del Fuego, Ushuaia, Tierra del Fuego, CP V9410CAB, Argentina
| | - Camila N Signori
- Oceanographic Institute, University of São Paulo, Praça do Oceanográfico, 191, São Paulo, CEP: 05508-900, Brazil
| | - Craig R Smith
- Department of Oceanography, University of Hawaii at Manoa, 1000 Pope Road, Honolulu, HI, 96822, U.S.A
| | - Marino Vacchi
- Institute for the Study of the Anthropic Impacts and the Sustainability of the Marine Environment (IAS), National Research Council of Italy (CNR), Via de Marini 6, Genoa, 16149, Italy
| | - Cinzia Verde
- Institute of Biosciences and BioResources (IBBR), National Research Council (CNR), Via Pietro Castellino 111, Naples, I-80131, Italy
| | - Diana H Wall
- Department of Biology and School of Global Environmental Sustainability, Colorado State University, Fort Collins, CO, U.S.A
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14
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Levin LA, Wei C, Dunn DC, Amon DJ, Ashford OS, Cheung WWL, Colaço A, Dominguez‐Carrió C, Escobar EG, Harden‐Davies HR, Drazen JC, Ismail K, Jones DOB, Johnson DE, Le JT, Lejzerowicz F, Mitarai S, Morato T, Mulsow S, Snelgrove PVR, Sweetman AK, Yasuhara M. Climate change considerations are fundamental to management of deep-sea resource extraction. GLOBAL CHANGE BIOLOGY 2020; 26:4664-4678. [PMID: 32531093 PMCID: PMC7496832 DOI: 10.1111/gcb.15223] [Citation(s) in RCA: 17] [Impact Index Per Article: 4.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/10/2020] [Accepted: 05/12/2020] [Indexed: 05/19/2023]
Abstract
Climate change manifestation in the ocean, through warming, oxygen loss, increasing acidification, and changing particulate organic carbon flux (one metric of altered food supply), is projected to affect most deep-ocean ecosystems concomitantly with increasing direct human disturbance. Climate drivers will alter deep-sea biodiversity and associated ecosystem services, and may interact with disturbance from resource extraction activities or even climate geoengineering. We suggest that to ensure the effective management of increasing use of the deep ocean (e.g., for bottom fishing, oil and gas extraction, and deep-seabed mining), environmental management and developing regulations must consider climate change. Strategic planning, impact assessment and monitoring, spatial management, application of the precautionary approach, and full-cost accounting of extraction activities should embrace climate consciousness. Coupled climate and biological modeling approaches applied in the water and on the seafloor can help accomplish this goal. For example, Earth-System Model projections of climate-change parameters at the seafloor reveal heterogeneity in projected climate hazard and time of emergence (beyond natural variability) in regions targeted for deep-seabed mining. Models that combine climate-induced changes in ocean circulation with particle tracking predict altered transport of early life stages (larvae) under climate change. Habitat suitability models can help assess the consequences of altered larval dispersal, predict climate refugia, and identify vulnerable regions for multiple species under climate change. Engaging the deep observing community can support the necessary data provisioning to mainstream climate into the development of environmental management plans. To illustrate this approach, we focus on deep-seabed mining and the International Seabed Authority, whose mandates include regulation of all mineral-related activities in international waters and protecting the marine environment from the harmful effects of mining. However, achieving deep-ocean sustainability under the UN Sustainable Development Goals will require integration of climate consideration across all policy sectors.
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Affiliation(s)
- Lisa A. Levin
- Integrative Oceanography Division and Center for Marine Biodiversity and ConservationScripps Institution of OceanographyUniversity of California, San DiegoLa JollaCAUSA
| | - Chih‐Lin Wei
- Institute of OceanographyNational Taiwan UniversityTaipeiTaiwan
| | - Daniel C. Dunn
- School of Earth and Environmental SciencesUniversity of QueenslandSt LuciaQldAustralia
| | - Diva J. Amon
- Life Sciences DepartmentNatural History MuseumLondonUK
| | - Oliver S. Ashford
- Integrative Oceanography Division and Center for Marine Biodiversity and ConservationScripps Institution of OceanographyUniversity of California, San DiegoLa JollaCAUSA
| | - William W. L. Cheung
- Institute for the Oceans and FisheriesThe University of British ColumbiaVancouverBCCanada
| | - Ana Colaço
- IMARInstituto do Mar, and Instituto de Investigação em Ciências do Mar – Okeanos da Universidade dos AçoresHortaPortugal
| | - Carlos Dominguez‐Carrió
- IMARInstituto do Mar, and Instituto de Investigação em Ciências do Mar – Okeanos da Universidade dos AçoresHortaPortugal
| | - Elva G. Escobar
- Instituto de Ciencias del Mar y LimnologíaUniversidad Nacional Autónoma de MéxicoMexico CityMexico
| | - Harriet R. Harden‐Davies
- Australian National Centre for Ocean Resources and SecurityUniversity of WollongongWollongongNSWAustralia
| | - Jeffrey C. Drazen
- Department of OceanographyUniversity of Hawaii at ManoaHonoluluHIUSA
| | - Khaira Ismail
- Faculty of Science and Marine EnvironmentUniversiti Malaysia TerengganuKuala TerengganuMalaysia
| | - Daniel O. B. Jones
- Ocean Biogeochemistry and Ecosystems GroupNational Oceanography CentreSouthamptonUK
| | - David E. Johnson
- Global Ocean Biodiversity InitiativeSeascape Consultants Ltd.RomseyUK
| | - Jennifer T. Le
- Integrative Oceanography Division and Center for Marine Biodiversity and ConservationScripps Institution of OceanographyUniversity of California, San DiegoLa JollaCAUSA
| | - Franck Lejzerowicz
- Jacobs School of EngineeringUniversity of California San DiegoLa JollaCAUSA
| | - Satoshi Mitarai
- Marine Biophysics UnitOkinawa Institute of Science and Technology Graduate UniversityOkinawaJapan
| | - Telmo Morato
- IMARInstituto do Mar, and Instituto de Investigação em Ciências do Mar – Okeanos da Universidade dos AçoresHortaPortugal
| | - Sandor Mulsow
- Instituto Ciencias Marinas y LimnológicasUniversidad Austral de ChileValdiviaChile
| | - Paul V. R. Snelgrove
- Department of Ocean Sciences and Biology DepartmentMemorial University of NewfoundlandSt. John'sNLCanada
| | - Andrew K. Sweetman
- The Lyell Centre for Earth and Marine Science and TechnologyHeriot Watt UniversityEdinburghUK
| | - Moriaki Yasuhara
- School of Biological Sciences and Swire Institute of Marine ScienceThe University of Hong KongHong Kong SARChina
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15
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Stratmann T, van Oevelen D, Martínez Arbizu P, Wei CL, Liao JX, Cusson M, Scrosati RA, Archambault P, Snelgrove PVR, Ramey-Balci PA, Burd BJ, Kenchington E, Gilkinson K, Belley R, Soetaert K. The BenBioDen database, a global database for meio-, macro- and megabenthic biomass and densities. Sci Data 2020; 7:206. [PMID: 32601290 PMCID: PMC7324384 DOI: 10.1038/s41597-020-0551-2] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/25/2020] [Accepted: 06/05/2020] [Indexed: 11/30/2022] Open
Abstract
Benthic fauna refers to all fauna that live in or on the seafloor, which researchers typically divide into size classes meiobenthos (32/64 µm-0.5/1 mm), macrobenthos (250 µm-1 cm), and megabenthos (>1 cm). Benthic fauna play important roles in bioturbation activity, mineralization of organic matter, and in marine food webs. Evaluating their role in these ecosystem functions requires knowledge of their global distribution and biomass. We therefore established the BenBioDen database, the largest open-access database for marine benthic biomass and density data compiled so far. In total, it includes 11,792 georeferenced benthic biomass and 51,559 benthic density records from 384 and 600 studies, respectively. We selected all references following the procedure for systematic reviews and meta-analyses, and report biomass records as grams of wet mass, dry mass, or ash-free dry mass, or carbon per m2 and as abundance records as individuals per m2. This database provides a point of reference for future studies on the distribution and biomass of benthic fauna.
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Affiliation(s)
- Tanja Stratmann
- NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems, and Utrecht University, P.O. Box 140, 4400 AC, Yerseke, The Netherlands.
- Utrecht University, Department of Earth Sciences, Vening Meineszgebouw A, Princetonlaan 8a, 3584 CB, Utrecht, The Netherlands.
- HGF MPG Joint Research Group for Deep-Sea Ecology and Technology, Max Planck Institute for Marine Microbiology, Celsiusstr. 1, 28359, Bremen, Germany.
| | - Dick van Oevelen
- NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems, and Utrecht University, P.O. Box 140, 4400 AC, Yerseke, The Netherlands
| | - Pedro Martínez Arbizu
- German Centre for Marine Biodiversity, Senckenberg am Meer, Südstrand 44, 26382, Wilhelmshaven, Germany
| | - Chih-Lin Wei
- Institute of Oceanography, National Taiwan University, No. 1, Sec. 4, Roosevelt Road, Taipei, 105, Taiwan
| | - Jian-Xiang Liao
- Institute of Oceanography, National Taiwan University, No. 1, Sec. 4, Roosevelt Road, Taipei, 105, Taiwan
| | - Mathieu Cusson
- Département des sciences fondamentales et Québec-Océan, Université du Québec à Chicoutimi, Boulevard de l'Université, Chicoutimi, QC, G7H 2B1, Canada
| | - Ricardo A Scrosati
- Department of Biology, St. Francis Xavier University, 2320 Notre Dame Ave., Antigonish, NS, B2G 2W5, Canada
| | - Philippe Archambault
- ArcticNet & Québec-Océan/Takuvik, Université Laval, pavillon Alexandre-Vachon 1045, av. de la Médecine, Québec, QC, G1V 0A6, Canada
| | - Paul V R Snelgrove
- Department of Ocean Sciences and Biology, Memorial University of Newfoundland, Marine Lab Rd., St. John's, NL, A1C 5S7, Canada
| | | | - Brenda J Burd
- Institute of Ocean Sciences, Fisheries and Ocean Canada, P.O. Box 6000, Sidney, BC, V8L 5T5, Canada
| | - Ellen Kenchington
- Bedford Institute of Oceanography, Fisheries and Ocean Canada, P.O. Box 1006, 1 Challenger Dr., Dartmouth, NS, B2Y 4A2, Canada
| | - Kent Gilkinson
- Northwest Atlantic Fisheries Centre, Fisheries and Ocean Canada, 80 East White Hills, St. John's, NL, A1C 5 × 1, Canada
| | - Rénald Belley
- Maurice Lamontagne Institute, Fisheries and Oceans Canada, 850 Route de la Mer, Mont-Joli, QC, G5H 3Z4, Canada
| | - Karline Soetaert
- NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems, and Utrecht University, P.O. Box 140, 4400 AC, Yerseke, The Netherlands
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16
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Gooday AJ, Schoenle A, Dolan JR, Arndt H. Protist diversity and function in the dark ocean - Challenging the paradigms of deep-sea ecology with special emphasis on foraminiferans and naked protists. Eur J Protistol 2020; 75:125721. [PMID: 32575029 DOI: 10.1016/j.ejop.2020.125721] [Citation(s) in RCA: 25] [Impact Index Per Article: 6.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/31/2020] [Revised: 05/13/2020] [Accepted: 05/21/2020] [Indexed: 11/27/2022]
Abstract
The dark ocean and the underlying deep seafloor together represent the largest environment on this planet, comprising about 80% of the oceanic volume and covering more than two-thirds of the Earth's surface, as well as hosting a major part of the total biosphere. Emerging evidence suggests that these vast pelagic and benthic habitats play a major role in ocean biogeochemistry and represent an "untapped reservoir" of high genetic and metabolic microbial diversity. Due to its huge volume, the water column of the dark ocean is the largest reservoir of organic carbon in the biosphere and likely plays a major role in the global carbon budget. The dark ocean and the seafloor beneath it are also home to a largely enigmatic food web comprising little-known and sometimes spectacular organisms, mainly prokaryotes and protists. This review considers the globally important role of pelagic and benthic protists across all protistan size classes in the deep-sea realm, with a focus on their taxonomy, diversity, and physiological properties, including their role in deep microbial food webs. We argue that, given the important contribution that protists must make to deep-sea biodiversity and ecosystem processes, they should not be overlooked in biological studies of the deep ocean.
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Affiliation(s)
- Andrew J Gooday
- National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, UK; Life Sciences Department, Natural History Museum, Cromwell Road, London SW7 5BD, UK
| | - Alexandra Schoenle
- University of Cologne, Institute of Zoology, General Ecology, 50674 Cologne, Germany
| | - John R Dolan
- Sorbonne Université, CNRS UMR 7093, Laboratoroire d'Océanographie de Villefranche-sur-Mer, Villefranche-sur-Mer, France
| | - Hartmut Arndt
- University of Cologne, Institute of Zoology, General Ecology, 50674 Cologne, Germany.
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17
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Morato T, González-Irusta JM, Dominguez-Carrió C, Wei CL, Davies A, Sweetman AK, Taranto GH, Beazley L, García-Alegre A, Grehan A, Laffargue P, Murillo FJ, Sacau M, Vaz S, Kenchington E, Arnaud-Haond S, Callery O, Chimienti G, Cordes E, Egilsdottir H, Freiwald A, Gasbarro R, Gutiérrez-Zárate C, Gianni M, Gilkinson K, Wareham Hayes VE, Hebbeln D, Hedges K, Henry LA, Johnson D, Koen-Alonso M, Lirette C, Mastrototaro F, Menot L, Molodtsova T, Durán Muñoz P, Orejas C, Pennino MG, Puerta P, Ragnarsson SÁ, Ramiro-Sánchez B, Rice J, Rivera J, Roberts JM, Ross SW, Rueda JL, Sampaio Í, Snelgrove P, Stirling D, Treble MA, Urra J, Vad J, van Oevelen D, Watling L, Walkusz W, Wienberg C, Woillez M, Levin LA, Carreiro-Silva M. Climate-induced changes in the suitable habitat of cold-water corals and commercially important deep-sea fishes in the North Atlantic. GLOBAL CHANGE BIOLOGY 2020; 26:2181-2202. [PMID: 32077217 PMCID: PMC7154791 DOI: 10.1111/gcb.14996] [Citation(s) in RCA: 17] [Impact Index Per Article: 4.3] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/12/2019] [Revised: 12/17/2019] [Accepted: 01/06/2020] [Indexed: 05/16/2023]
Abstract
The deep sea plays a critical role in global climate regulation through uptake and storage of heat and carbon dioxide. However, this regulating service causes warming, acidification and deoxygenation of deep waters, leading to decreased food availability at the seafloor. These changes and their projections are likely to affect productivity, biodiversity and distributions of deep-sea fauna, thereby compromising key ecosystem services. Understanding how climate change can lead to shifts in deep-sea species distributions is critically important in developing management measures. We used environmental niche modelling along with the best available species occurrence data and environmental parameters to model habitat suitability for key cold-water coral and commercially important deep-sea fish species under present-day (1951-2000) environmental conditions and to project changes under severe, high emissions future (2081-2100) climate projections (RCP8.5 scenario) for the North Atlantic Ocean. Our models projected a decrease of 28%-100% in suitable habitat for cold-water corals and a shift in suitable habitat for deep-sea fishes of 2.0°-9.9° towards higher latitudes. The largest reductions in suitable habitat were projected for the scleractinian coral Lophelia pertusa and the octocoral Paragorgia arborea, with declines of at least 79% and 99% respectively. We projected the expansion of suitable habitat by 2100 only for the fishes Helicolenus dactylopterus and Sebastes mentella (20%-30%), mostly through northern latitudinal range expansion. Our results projected limited climate refugia locations in the North Atlantic by 2100 for scleractinian corals (30%-42% of present-day suitable habitat), even smaller refugia locations for the octocorals Acanella arbuscula and Acanthogorgia armata (6%-14%), and almost no refugia for P. arborea. Our results emphasize the need to understand how anticipated climate change will affect the distribution of deep-sea species including commercially important fishes and foundation species, and highlight the importance of identifying and preserving climate refugia for a range of area-based planning and management tools.
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Affiliation(s)
- Telmo Morato
- Okeanos Research Centre, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
- IMAR Instituto do Mar, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
| | - José-Manuel González-Irusta
- Okeanos Research Centre, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
- IMAR Instituto do Mar, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
| | - Carlos Dominguez-Carrió
- Okeanos Research Centre, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
- IMAR Instituto do Mar, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
| | - Chih-Lin Wei
- Institute of Oceanography, National Taiwan University, Taipei, Taiwan
| | - Andrew Davies
- Department of Biological Sciences, University of Rhode Island, Kingston, RI, USA
| | - Andrew K Sweetman
- Marine Benthic Ecology, Biogeochemistry and In situ Technology Research Group, The Lyell Centre for Earth and Marine Science and Technology, Heriot-Watt University, Edinburgh, UK
| | - Gerald H Taranto
- Okeanos Research Centre, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
- IMAR Instituto do Mar, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
| | - Lindsay Beazley
- Fisheries and Oceans Canada, Bedford Institute of Oceanography, Dartmouth, NS, Canada
| | - Ana García-Alegre
- Instituto Español de Oceanografía (IEO), Centro Oceanográfico de Vigo, Vigo, Pontevedra, Spain
| | | | | | | | - Mar Sacau
- Instituto Español de Oceanografía (IEO), Centro Oceanográfico de Vigo, Vigo, Pontevedra, Spain
| | - Sandrine Vaz
- MARBEC, University of Montpellier, IFREMER, CNRS, IRD, Sète, France
| | - Ellen Kenchington
- Fisheries and Oceans Canada, Bedford Institute of Oceanography, Dartmouth, NS, Canada
| | | | - Oisín Callery
- Earth and Ocean Sciences, NUI Galway, Galway, Ireland
| | - Giovanni Chimienti
- Department of Biology, University of Bari Aldo Moro, Bari, Italy
- CoNISMa, Rome, Italy
| | - Erik Cordes
- Department of Biology, Temple University, Philadelphia, PA, USA
| | | | - André Freiwald
- Marine Research Department, Senckenberg am Meer, Wilhelmshaven, Germany
| | - Ryan Gasbarro
- Department of Biology, Temple University, Philadelphia, PA, USA
| | - Cristina Gutiérrez-Zárate
- Okeanos Research Centre, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
- IMAR Instituto do Mar, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
| | | | - Kent Gilkinson
- Northwest Atlantic Fisheries Centre, Fisheries and Ocean Canada, St. John's, NL, Canada
| | - Vonda E Wareham Hayes
- Northwest Atlantic Fisheries Centre, Fisheries and Ocean Canada, St. John's, NL, Canada
| | - Dierk Hebbeln
- MARUM - Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
| | - Kevin Hedges
- Fisheries and Oceans Canada, Winnipeg, MB, Canada
| | - Lea-Anne Henry
- Changing Oceans Group, School of GeoSciences, Grant Institute, University of Edinburgh, Edinburgh, UK
| | | | - Mariano Koen-Alonso
- Northwest Atlantic Fisheries Centre, Fisheries and Ocean Canada, St. John's, NL, Canada
| | - Cam Lirette
- Fisheries and Oceans Canada, Bedford Institute of Oceanography, Dartmouth, NS, Canada
| | | | | | | | - Pablo Durán Muñoz
- Instituto Español de Oceanografía (IEO), Centro Oceanográfico de Vigo, Vigo, Pontevedra, Spain
| | - Covadonga Orejas
- Instituto Español de Oceanografía, Centro Oceanográfico de Baleares, Palma, Spain
| | - Maria Grazia Pennino
- Instituto Español de Oceanografía (IEO), Centro Oceanográfico de Vigo, Vigo, Pontevedra, Spain
| | - Patricia Puerta
- Instituto Español de Oceanografía, Centro Oceanográfico de Baleares, Palma, Spain
| | | | - Berta Ramiro-Sánchez
- Changing Oceans Group, School of GeoSciences, Grant Institute, University of Edinburgh, Edinburgh, UK
| | - Jake Rice
- Fisheries and Ocean Canada, Ottawa, ON, Canada
| | - Jesús Rivera
- Instituto Español de Oceanografía, Madrid, Spain
| | - J Murray Roberts
- Changing Oceans Group, School of GeoSciences, Grant Institute, University of Edinburgh, Edinburgh, UK
| | - Steve W Ross
- Center for Marine Science, University of North Carolina at Wilmington, Wilmington, NC, USA
| | - José L Rueda
- Instituto Español de Oceanografía, Centro Oceanográfico de Málaga, Málaga, Spain
| | - Íris Sampaio
- IMAR Instituto do Mar, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
- Marine Research Department, Senckenberg am Meer, Wilhelmshaven, Germany
| | - Paul Snelgrove
- Ocean Sciences Centre, Memorial University, St. John's, NL, Canada
| | - David Stirling
- Marine Laboratory, Marine Scotland Science, Aberdeen, UK
| | | | - Javier Urra
- Instituto Español de Oceanografía, Centro Oceanográfico de Málaga, Málaga, Spain
| | - Johanne Vad
- Changing Oceans Group, School of GeoSciences, Grant Institute, University of Edinburgh, Edinburgh, UK
| | - Dick van Oevelen
- Royal Netherlands Institute for Sea Research (NIOZ), Utrecht University, Yerseke, The Netherlands
| | - Les Watling
- Department of Biology, University of Hawai'i at Mānoa, Honolulu, HI, USA
| | | | - Claudia Wienberg
- MARUM - Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
| | | | - Lisa A Levin
- Center for Marine Biodiversity and Conservation and Integrative Oceanography Division, Scripps Institution of Oceanography, UC San Diego, La Jolla, CA, USA
| | - Marina Carreiro-Silva
- Okeanos Research Centre, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
- IMAR Instituto do Mar, Departamento de Oceanografia e Pesca, Universidade dos Açores, Horta, Portugal
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18
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Jansen J, Dunstan PK, Hill NA, Koubbi P, Melbourne-Thomas J, Causse R, Johnson CR. Integrated assessment of the spatial distribution and structural dynamics of deep benthic marine communities. ECOLOGICAL APPLICATIONS : A PUBLICATION OF THE ECOLOGICAL SOCIETY OF AMERICA 2020; 30:e02065. [PMID: 31872512 DOI: 10.1002/eap.2065] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/20/2018] [Revised: 08/15/2019] [Accepted: 11/11/2019] [Indexed: 06/10/2023]
Abstract
Characterizing the spatial distribution and variation of species communities and validating these characteristics with data from the field are key elements for an ecosystem-based approach to management. However, models of species distributions that yield community structure are usually not linked to models of community dynamics, constraining understanding and management of the ecosystem, particularly in data-poor regions. Here we use a qualitative network model to predict changes in Antarctic benthic community structure between major marine habitats characterized largely by seafloor depth and slope, and use multivariate mixture models of species distributions to validate the community dynamics. We then assess how future increases in primary production associated with anticipated loss of sea-ice may affect the ecosystem. Our study shows how both spatial and structural features of ecosystems in data-poor regions can be analyzed and possible futures assessed, with direct relevance for ecosystem-based management.
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Affiliation(s)
- Jan Jansen
- Institute for Marine and Antarctic Studies (IMAS), University of Tasmania, 20 Castray Esplanade, Battery Point, Hobart, Tasmania, 7004, Australia
| | | | - Nicole A Hill
- Institute for Marine and Antarctic Studies (IMAS), University of Tasmania, 20 Castray Esplanade, Battery Point, Hobart, Tasmania, 7004, Australia
| | - Philippe Koubbi
- UFR 918 Terre Environnement Biodiversité, Sorbonne Université, Paris, France
- Channel and North Sea Fisheries Research Unit, IFREMER, Boulogne-sur-Mer, France
| | | | - Romain Causse
- Unité Biologie des Organismes et Ecosystèmes Aquatiques (BOREA), Muséum National d'Histoire Naturelle, Sorbonne Université, Université de Caen Normandie, Université des Antilles, CNRS, IRD, Paris, France
| | - Craig R Johnson
- Institute for Marine and Antarctic Studies (IMAS), University of Tasmania, 20 Castray Esplanade, Battery Point, Hobart, Tasmania, 7004, Australia
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19
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Ashford OS, Kenny AJ, Barrio Froján CRS, Horton T, Rogers AD. Investigating the environmental drivers of deep-seafloor biodiversity: A case study of peracarid crustacean assemblages in the Northwest Atlantic Ocean. Ecol Evol 2019; 9:14167-14204. [PMID: 31938511 PMCID: PMC6953587 DOI: 10.1002/ece3.5852] [Citation(s) in RCA: 12] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/26/2019] [Revised: 10/11/2019] [Accepted: 11/01/2019] [Indexed: 11/14/2022] Open
Abstract
The deep-sea benthos covers over 90% of seafloor area and hosts a great diversity of species which contribute toward essential ecosystem services. Evidence suggests that deep-seafloor assemblages are structured predominantly by their physical environment, yet knowledge of assemblage/environment relationships is limited. Here, we utilized a very large dataset of Northwest Atlantic Ocean continental slope peracarid crustacean assemblages as a case study to investigate the environmental drivers of deep-seafloor macrofaunal biodiversity. We investigated biodiversity from a phylogenetic, functional, and taxonomic perspective, and found that a wide variety of environmental drivers, including food availability, physical disturbance (bottom trawling), current speed, sediment characteristics, topographic heterogeneity, and temperature (in order of relative importance), significantly influenced peracarid biodiversity. We also found deep-water peracarid assemblages to vary seasonally and interannually. Contrary to prevailing theory on the drivers of deep-seafloor diversity, we found high topographic heterogeneity (at the hundreds to thousands of meter scale) to negatively influence assemblage diversity, while broadscale sediment characteristics (i.e., percent sand content) were found to influence assemblages more than sediment particle-size diversity. However, our results support other paradigms of deep-seafloor biodiversity, including that assemblages may vary inter- and intra-annually, and how assemblages respond to changes in current speed. We found that bottom trawling negatively affects the evenness and diversity of deep-sea soft-sediment peracarid assemblages, but that predicted changes in ocean temperature as a result of climate change may not strongly influence continental slope biodiversity over human timescales, although it may alter deep-sea community biomass. Finally, we emphasize the value of analyzing multiple metrics of biodiversity and call for researchers to consider an expanded definition of biodiversity in future investigations of deep-ocean life.
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Affiliation(s)
- Oliver S. Ashford
- Department of ZoologyUniversity of OxfordOxfordUK
- Centre for the Environment, Fisheries and Aquaculture Science (Cefas)LowestoftUK
- Present address:
Scripps Institution of OceanographyLa JollaCAUSA
| | - Andrew J. Kenny
- Centre for the Environment, Fisheries and Aquaculture Science (Cefas)LowestoftUK
| | | | - Tammy Horton
- National Oceanography CentreUniversity of Southampton Waterfront CampusSouthamptonUK
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20
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Wang K, Zhang H, Han X, Qiu W. Sources and burial fluxes of sedimentary organic carbon in the northern Bering Sea and the northern Chukchi Sea in response to global warming. THE SCIENCE OF THE TOTAL ENVIRONMENT 2019; 679:97-105. [PMID: 31082605 DOI: 10.1016/j.scitotenv.2019.04.374] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/24/2019] [Revised: 04/17/2019] [Accepted: 04/25/2019] [Indexed: 06/09/2023]
Abstract
The Arctic and subarctic seas are the major CO2 sink areas on earth. In this study, the vertical variation characteristics of organic carbon, total nitrogen and their ratio (Corg/Nt), stable isotopes δ13C and δ15N, and BIT (branched and isoprenoid tetraether) index of GDGTs (glycerol dialkyl glycerol tetraethers) in combination with 210Pb-dating were used to analyze the changes in the marine and terrestrial sources of organic carbon in the northern Bering Sea (site 1), western Beaufort Sea slope (site 2) and northern Chukchi Sea (site 3). Organic carbon burial fluxes (OCBF) in the context of global warming were also explored at sites 1 and 3. The results showed that organic matter in these sediments were a mixed input of marine and terrestrial sources, and the BIT index and δ13C of site 2 suggested that the terrestrial soil organic matter was dominant. Based on a combination of 210Pb dating and Corg, the sedimentary OCBF at site 1 was 2.29-3.65 mg cm-2 y-1, and at site 3 was 0.00-0.41 mg cm-2 y-1. The temperature anomalies and sea ice changes in the Arctic in the past 100 years were compared with the burial fluxes of the terrestrial organic carbon. At site 1, the results indicated that fast melting of seasonal sea ice led to earlier arrival of ice algae bloom, enhanced zooplankton feeding and reduced carbon burial from 1947 to 2010, and the sudden increase in carbon burial after 2010 was attributed to an increase in primary productivity and terrestrial organic matter input due to an accelerated melting of sea ice. There was a smaller change in marine organic carbon content in site 3, but OCBF increased after a pre-1965 decrease, mainly controlled by terrestrial organic matter input associated with temperature rising and sea ice melting during recent decades.
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Affiliation(s)
- Kui Wang
- Key Laboratory of Marine Ecosystem and Biogeochemistry, State Oceanic Administration, Hangzhou 310012, China; Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Haisheng Zhang
- Key Laboratory of Marine Ecosystem and Biogeochemistry, State Oceanic Administration, Hangzhou 310012, China; Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Xibin Han
- Key Laboratory of Submarine Geosciences, State Oceanic Administration, Hangzhou 310012, China; Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Wenxian Qiu
- Guanghua Law School, Zhejiang University, Hangzhou 310008, China.
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21
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Vieira RP, Trueman CN, Readdy L, Kenny A, Pinnegar JK. Deep-water fisheries along the British Isles continental slopes: status, ecosystem effects and future perspectives. JOURNAL OF FISH BIOLOGY 2019; 94:981-992. [PMID: 30746699 DOI: 10.1111/jfb.13927] [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: 09/12/2018] [Accepted: 02/11/2019] [Indexed: 06/09/2023]
Abstract
In this paper, we revisit the state of deep-water fisheries to the west of the British Isles and aim to provide an overview on the key drivers behind community changes along continental margins. The deep-water fisheries to the west of the British Isles that extend from the shelf-slope break down to the lower slope and along banks and seamounts of the Rockall Basin, mainly target blue ling Molva dypterygia, roundnose grenadier Coryphaenoides rupestris, orange roughy Hoplostethus atlanticus, with by-catches of black scabbardfish Aphanopus carbo and tusk Brosme brosme. These fishing grounds experienced a long period of exhaustive exploitation until the early 2000s, but subsequently the implementation of management strategies has helped to relieve excessive fishing pressure. It is widely accepted that a better understanding of the long-term implications of disturbance is needed to understand patterns in deep-water communities and what sustainable use and exploitation of resources might look like in this context.
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Affiliation(s)
- Rui P Vieira
- Centre for Environment, Fisheries & Aquaculture Science, Lowestoft Laboratory, Lowestoft, UK
- School of Environmental Sciences, University of East Anglia, Norwich, UK
- Ocean and Earth Science, University of Southampton, Southampton, UK
| | - Clive N Trueman
- Ocean and Earth Science, University of Southampton, Southampton, UK
| | - Lisa Readdy
- Centre for Environment, Fisheries & Aquaculture Science, Lowestoft Laboratory, Lowestoft, UK
| | - Andrew Kenny
- Centre for Environment, Fisheries & Aquaculture Science, Lowestoft Laboratory, Lowestoft, UK
| | - John K Pinnegar
- Centre for Environment, Fisheries & Aquaculture Science, Lowestoft Laboratory, Lowestoft, UK
- School of Environmental Sciences, University of East Anglia, Norwich, UK
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22
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Cardeñosa D, Gollock MJ, Chapman DD. Development and application of a novel real‐time polymerase chain reaction assay to detect illegal trade of the European eel (
Anguilla anguilla
). CONSERVATION SCIENCE AND PRACTICE 2019. [DOI: 10.1111/csp2.39] [Citation(s) in RCA: 6] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/18/2022] Open
Affiliation(s)
- Diego Cardeñosa
- School of Marine and Atmospheric ScienceStony Brook University Stony Brook New York
- Fundación Colombia Azul Bogotá Colombia
| | | | - Demian D. Chapman
- Department of Biological SciencesFlorida International University Nebraska Florida
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23
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Hunter WR, Ogle N, O’Connor N. Warming affects predatory faunal impacts upon microbial carbon cycling. Funct Ecol 2019. [DOI: 10.1111/1365-2435.13304] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/27/2022]
Affiliation(s)
- William Ross Hunter
- Queen’s University Marine Laboratory, School of Biological Sciences Queen's University of Belfast Portaferry UK
| | - Neil Ogle
- Queen’s University Stable Isotope Facility, School of Natural and Built Environment Queen's University of Belfast Belfast UK
| | - Nessa O’Connor
- Queen’s University Marine Laboratory, School of Biological Sciences Queen's University of Belfast Portaferry UK
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24
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Molari M, Guilini K, Lins L, Ramette A, Vanreusel A. CO 2 leakage can cause loss of benthic biodiversity in submarine sands. MARINE ENVIRONMENTAL RESEARCH 2019; 144:213-229. [PMID: 30709637 DOI: 10.1016/j.marenvres.2019.01.006] [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: 08/20/2018] [Revised: 01/07/2019] [Accepted: 01/11/2019] [Indexed: 06/09/2023]
Abstract
One of the options to mitigate atmospheric CO2 increase is CO2 Capture and Storage in sub-seabed geological formations. Since predicting long-term storage security is difficult, different CO2 leakage scenarios and impacts on marine ecosystems require evaluation. Submarine CO2 vents may serve as natural analogues and allow studying the effects of CO2 leakage in a holistic approach. At the study site east of Basiluzzo Islet off Panarea Island (Italy), gas emissions (90-99% CO2) occur at moderate flows (80-120 L m-2 h-1). We investigated the effects of acidified porewater conditions (pHT range: 5.5-7.7) on the diversity of benthic bacteria and invertebrates by sampling natural sediments in three subsequent years and by performing a transplantation experiment with a duration of one year, respectively. Both multiple years and one year of exposure to acidified porewater conditions reduced the number of benthic bacterial operational taxonomic units and invertebrate species diversity by 30-80%. Reduced biodiversity at the vent sites increased the temporal variability in bacterial and nematode community biomass, abundance and composition. While the release from CO2 exposure resulted in a full recovery of nematode species diversity within one year, bacterial diversity remained affected. Overall our findings showed that seawater acidification, induced by seafloor CO2 emissions, was responsible for loss of diversity across different size-classes of benthic organisms, which reduced community stability with potential relapses on ecosystem resilience.
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Affiliation(s)
- Massimiliano Molari
- HGF-MPG Group for Deep Sea Ecology and Technology, Max Planck Institute for Marine Microbiology, Germany.
| | - Katja Guilini
- Marine Biology Research Group, Department of Biology, Ghent University, Krijgslaan 281/S8, 9000, Ghent, Belgium
| | - Lidia Lins
- Marine Biology Research Group, Department of Biology, Ghent University, Krijgslaan 281/S8, 9000, Ghent, Belgium
| | - Alban Ramette
- HGF-MPG Group for Deep Sea Ecology and Technology, Max Planck Institute for Marine Microbiology, Germany
| | - Ann Vanreusel
- Marine Biology Research Group, Department of Biology, Ghent University, Krijgslaan 281/S8, 9000, Ghent, Belgium
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25
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Ashford OS, Kenny AJ, Barrio Froján CRS, Bonsall MB, Horton T, Brandt A, Bird GJ, Gerken S, Rogers AD. Phylogenetic and functional evidence suggests that deep-ocean ecosystems are highly sensitive to environmental change and direct human disturbance. Proc Biol Sci 2018; 285:20180923. [PMID: 30068675 PMCID: PMC6111167 DOI: 10.1098/rspb.2018.0923] [Citation(s) in RCA: 22] [Impact Index Per Article: 3.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/25/2018] [Accepted: 07/09/2018] [Indexed: 11/12/2022] Open
Abstract
An understanding of the balance of interspecific competition and the physical environment in structuring organismal communities is crucial because those communities structured primarily by their physical environment typically exhibit greater sensitivity to environmental change than those structured predominantly by competitive interactions. Here, using detailed phylogenetic and functional information, we investigate this question in macrofaunal assemblages from Northwest Atlantic Ocean continental slopes, a high seas region projected to experience substantial environmental change through the current century. We demonstrate assemblages to be both phylogenetically and functionally under-dispersed, and thus conclude that the physical environment, not competition, may dominate in structuring deep-ocean communities. Further, we find temperature and bottom trawling intensity to be among the environmental factors significantly related to assemblage diversity. These results hint that deep-ocean communities are highly sensitive to their physical environment and vulnerable to environmental perturbation, including by direct disturbance through fishing, and indirectly through the changes brought about by climate change.
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Affiliation(s)
- Oliver S Ashford
- Department of Zoology, University of Oxford, Oxford OX1 3PS, UK
- Centre for the Environment, Fisheries and Aquaculture Science (Cefas), Pakefield Road, Lowestoft NR33 0HT, UK
| | - Andrew J Kenny
- Centre for the Environment, Fisheries and Aquaculture Science (Cefas), Pakefield Road, Lowestoft NR33 0HT, UK
| | | | | | - Tammy Horton
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton, SO14 3ZH, UK
| | - Angelika Brandt
- Department of Marine Zoology, Senckenberg Research Institute and Natural History Museum, Senckenberganlage 25, 60325 Frankfurt am Main, Germany
- FB 15 Biological Sciences, Institute for Ecology, Diversity and Evolution, Goethe University Frankfurt, Campus Riedberg, Max-von-Laue-Str. 13, 60438 Frankfurt am Main, Germany
| | - Graham J Bird
- 8 Shotover Grove, Waikanae, Kāpiti 5036, New Zealand
| | - Sarah Gerken
- Department of Biological Sciences, University of Alaska, Anchorage, AK 99508, USA
| | - Alex D Rogers
- Department of Zoology, University of Oxford, Oxford OX1 3PS, UK
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26
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Abstract
Seamounts are one of the major biomes of the global ocean. The last 25 years of research has seen considerable advances in the understanding of these ecosystems. The interactions between seamounts and steady and variable flows have now been characterised providing a better mechanistic understanding of processes influencing biology. Processes leading to upwelling, including Taylor column formation and tidal rectification, have now been defined as well as those leading to draw down of organic matter from the ocean surface to seamount summit and flanks. There is also an improved understanding of the interactions between seamounts, zooplankton and micronekton communities especially with respect to increased predation pressure in the vicinity of seamounts. Evidence has accumulated of the role of seamounts as hot spots for ocean predators including large pelagic fish, sharks, pinnipeds, cetaceans and seabirds. The complexity of benthic communities associated with seamounts is high and drivers of biodiversity are now being resolved. Claims of high endemism resulting from isolation of seamounts as islands of habitat and speciation have not been supported. However, for species characterised by low dispersal capability, such as some groups of benthic sessile or low-mobility invertebrates, low connectivity between seamount populations has been found with evidence of endemism at a local level. Threats to seamounts have increased in the last 25 years and include overfishing, destructive fishing, marine litter, direct and indirect impacts of climate change and potentially marine mining in the near future. Issues around these threats and their management are discussed.
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Affiliation(s)
- Alex D Rogers
- Department of Zoology, University of Oxford, Oxford, United Kingdom.
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27
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Climate change impacts on the biota and on vulnerable habitats of the deep Mediterranean Sea. RENDICONTI LINCEI-SCIENZE FISICHE E NATURALI 2018. [DOI: 10.1007/s12210-018-0725-4] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 10/28/2022]
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28
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Wollenburg JE, Katlein C, Nehrke G, Nöthig EM, Matthiessen J, Wolf-Gladrow DA, Nikolopoulos A, Gázquez-Sanchez F, Rossmann L, Assmy P, Babin M, Bruyant F, Beaulieu M, Dybwad C, Peeken I. Ballasting by cryogenic gypsum enhances carbon export in a Phaeocystis under-ice bloom. Sci Rep 2018; 8:7703. [PMID: 29769577 PMCID: PMC5956002 DOI: 10.1038/s41598-018-26016-0] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/01/2017] [Accepted: 04/27/2018] [Indexed: 11/30/2022] Open
Abstract
Mineral ballasting enhances carbon export from the surface to the deep ocean; however, little is known about the role of this process in the ice-covered Arctic Ocean. Here, we propose gypsum ballasting as a new mechanism that likely facilitated enhanced vertical carbon export from an under-ice phytoplankton bloom dominated by the haptophyte Phaeocystis. In the spring 2015 abundant gypsum crystals embedded in Phaeocystis aggregates were collected throughout the water column and on the sea floor at a depth below 2 km. Model predictions supported by isotopic signatures indicate that 2.7 g m−2 gypsum crystals were formed in sea ice at temperatures below −6.5 °C and released into the water column during sea ice melting. Our finding indicates that sea ice derived (cryogenic) gypsum is stable enough to survive export to the deep ocean and serves as an effective ballast mineral. Our findings also suggest a potentially important and previously unknown role of Phaeocystis in deep carbon export due to cryogenic gypsum ballasting. The rapidly changing Arctic sea ice regime might favour this gypsum gravity chute with potential consequences for carbon export and food partitioning between pelagic and benthic ecosystems.
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Affiliation(s)
- J E Wollenburg
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570, Bremerhaven, Germany.
| | - C Katlein
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570, Bremerhaven, Germany
| | - G Nehrke
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570, Bremerhaven, Germany
| | - E-M Nöthig
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570, Bremerhaven, Germany
| | - J Matthiessen
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570, Bremerhaven, Germany
| | - D A Wolf-Gladrow
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570, Bremerhaven, Germany
| | | | - F Gázquez-Sanchez
- Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge, CB2 3EQ, United Kingdom
| | - L Rossmann
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570, Bremerhaven, Germany
| | - P Assmy
- Norwegian Polar Institute, Fram Centre, 9296, Tromsø, Norway
| | - M Babin
- Takuvik Joint International Laboratory, Université Laval and CNRS, G1V 0A6, Québec, Canada
| | - F Bruyant
- Takuvik Joint International Laboratory, Université Laval and CNRS, G1V 0A6, Québec, Canada
| | - M Beaulieu
- Université de Sherbrooke, Department of Civil Engineering, QC J1K 2R1, Sherbrooke, Canada
| | - C Dybwad
- Department of Arctic and Marine Biology, Faculty of Biosciences, Fisheries and Economics, Universitetet i Tromsø - The Arctic University of Norway, N-9037, Tromsø, Norway
| | - I Peeken
- Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, D-27570, Bremerhaven, Germany
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29
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Brown A, Thatje S, Morris JP, Oliphant A, Morgan EA, Hauton C, Jones DOB, Pond DW. Metabolic costs imposed by hydrostatic pressure constrain bathymetric range in the lithodid crab Lithodes maja. ACTA ACUST UNITED AC 2018; 220:3916-3926. [PMID: 29093188 DOI: 10.1242/jeb.158543] [Citation(s) in RCA: 19] [Impact Index Per Article: 3.2] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/21/2017] [Accepted: 09/05/2017] [Indexed: 01/16/2023]
Abstract
The changing climate is shifting the distributions of marine species, yet the potential for shifts in depth distributions is virtually unexplored. Hydrostatic pressure is proposed to contribute to a physiological bottleneck constraining depth range extension in shallow-water taxa. However, bathymetric limitation by hydrostatic pressure remains undemonstrated, and the mechanism limiting hyperbaric tolerance remains hypothetical. Here, we assess the effects of hydrostatic pressure in the lithodid crab Lithodes maja (bathymetric range 4-790 m depth, approximately equivalent to 0.1 to 7.9 MPa hydrostatic pressure). Heart rate decreased with increasing hydrostatic pressure, and was significantly lower at ≥10.0 MPa than at 0.1 MPa. Oxygen consumption increased with increasing hydrostatic pressure to 12.5 MPa, before decreasing as hydrostatic pressure increased to 20.0 MPa; oxygen consumption was significantly higher at 7.5-17.5 MPa than at 0.1 MPa. Increases in expression of genes associated with neurotransmission, metabolism and stress were observed between 7.5 and 12.5 MPa. We suggest that hyperbaric tolerance in Lmaja may be oxygen-limited by hyperbaric effects on heart rate and metabolic rate, but that Lmaja's bathymetric range is limited by metabolic costs imposed by the effects of high hydrostatic pressure. These results advocate including hydrostatic pressure in a complex model of environmental tolerance, where energy limitation constrains biogeographic range, and facilitate the incorporation of hydrostatic pressure into the broader metabolic framework for ecology and evolution. Such an approach is crucial for accurately projecting biogeographic responses to changing climate, and for understanding the ecology and evolution of life at depth.
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Affiliation(s)
- Alastair Brown
- University of Southampton, Ocean and Earth Science, European Way, Southampton SO14 3ZH, UK
| | - Sven Thatje
- University of Southampton, Ocean and Earth Science, European Way, Southampton SO14 3ZH, UK
| | - James P Morris
- University of Southampton, Ocean and Earth Science, European Way, Southampton SO14 3ZH, UK
| | - Andrew Oliphant
- University of Southampton, Ocean and Earth Science, European Way, Southampton SO14 3ZH, UK
| | - Elizabeth A Morgan
- University of Southampton, Ocean and Earth Science, European Way, Southampton SO14 3ZH, UK
| | - Chris Hauton
- University of Southampton, Ocean and Earth Science, European Way, Southampton SO14 3ZH, UK
| | - Daniel O B Jones
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK
| | - David W Pond
- Scottish Association for Marine Science, Oban, Argyll PA37 1QA, UK
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30
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Jones MC, Cheung WWL. Using fuzzy logic to determine the vulnerability of marine species to climate change. GLOBAL CHANGE BIOLOGY 2018; 24:e719-e731. [PMID: 28948655 DOI: 10.1111/gcb.13869] [Citation(s) in RCA: 28] [Impact Index Per Article: 4.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/03/2017] [Accepted: 08/10/2017] [Indexed: 06/07/2023]
Abstract
Marine species are being impacted by climate change and ocean acidification, although their level of vulnerability varies due to differences in species' sensitivity, adaptive capacity and exposure to climate hazards. Due to limited data on the biological and ecological attributes of many marine species, as well as inherent uncertainties in the assessment process, climate change vulnerability assessments in the marine environment frequently focus on a limited number of taxa or geographic ranges. As climate change is already impacting marine biodiversity and fisheries, there is an urgent need to expand vulnerability assessment to cover a large number of species and areas. Here, we develop a modelling approach to synthesize data on species-specific estimates of exposure, and ecological and biological traits to undertake an assessment of vulnerability (sensitivity and adaptive capacity) and risk of impacts (combining exposure to hazards and vulnerability) of climate change (including ocean acidification) for global marine fishes and invertebrates. We use a fuzzy logic approach to accommodate the variability in data availability and uncertainties associated with inferring vulnerability levels from climate projections and species' traits. Applying the approach to estimate the relative vulnerability and risk of impacts of climate change in 1074 exploited marine species globally, we estimated their index of vulnerability and risk of impacts to be on average 52 ± 19 SD and 66 ± 11 SD, scaling from 1 to 100, with 100 being the most vulnerable and highest risk, respectively, under the 'business-as-usual' greenhouse gas emission scenario (Representative Concentration Pathway 8.5). We identified 157 species to be highly vulnerable while 294 species are identified as being at high risk of impacts. Species that are most vulnerable tend to be large-bodied endemic species. This study suggests that the fuzzy logic framework can help estimate climate vulnerabilities and risks of exploited marine species using publicly and readily available information.
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Affiliation(s)
- Miranda C Jones
- Changing Ocean Research Unit, Institute for the Oceans and Fisheries, University of British Columbia, Vancouver, BC, Canada
| | - William W L Cheung
- Changing Ocean Research Unit, Institute for the Oceans and Fisheries, University of British Columbia, Vancouver, BC, Canada
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31
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Danovaro R, Corinaldesi C, Dell'Anno A, Rastelli E. Potential impact of global climate change on benthic deep-sea microbes. FEMS Microbiol Lett 2018; 364:4553516. [PMID: 29045616 DOI: 10.1093/femsle/fnx214] [Citation(s) in RCA: 44] [Impact Index Per Article: 7.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/05/2017] [Accepted: 10/12/2017] [Indexed: 11/12/2022] Open
Abstract
Benthic deep-sea environments are the largest ecosystem on Earth, covering ∼65% of the Earth surface. Microbes inhabiting this huge biome at all water depths represent the most abundant biological components and a relevant portion of the biomass of the biosphere, and play a crucial role in global biogeochemical cycles. Increasing evidence suggests that global climate changes are affecting also deep-sea ecosystems, both directly (causing shifts in bottom-water temperature, oxygen concentration and pH) and indirectly (through changes in surface oceans' productivity and in the consequent export of organic matter to the seafloor). However, the responses of the benthic deep-sea biota to such shifts remain largely unknown. This applies particularly to deep-sea microbes, which include bacteria, archaea, microeukaryotes and their viruses. Understanding the potential impacts of global change on the benthic deep-sea microbial assemblages and the consequences on the functioning of the ocean interior is a priority to better forecast the potential consequences at global scale. Here we explore the potential changes in the benthic deep-sea microbiology expected in the coming decades using case studies on specific systems used as test models.
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Affiliation(s)
- Roberto Danovaro
- Department of Life and Environmental Sciences, Polytechnic University of Marche, 60131 Ancona, Italy.,Stazione Zoologica Anton Dohrn, Villa Comunale, 80121 Naples, Italy
| | - Cinzia Corinaldesi
- Department of Sciences and Engineering of Materials, Environment and Urbanistics, Polytechnic University of Marche, 60131 Ancona, Italy
| | - Antonio Dell'Anno
- Department of Life and Environmental Sciences, Polytechnic University of Marche, 60131 Ancona, Italy
| | - Eugenio Rastelli
- Department of Life and Environmental Sciences, Polytechnic University of Marche, 60131 Ancona, Italy.,Stazione Zoologica Anton Dohrn, Villa Comunale, 80121 Naples, Italy
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32
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Brown A, Thatje S, Hauton C. The Effects of Temperature and Hydrostatic Pressure on Metal Toxicity: Insights into Toxicity in the Deep Sea. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2017; 51:10222-10231. [PMID: 28708382 DOI: 10.1021/acs.est.7b02988] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/07/2023]
Abstract
Mineral prospecting in the deep sea is increasing, promoting concern regarding potential ecotoxicological impacts on deep-sea fauna. Technological difficulties in assessing toxicity in deep-sea species has promoted interest in developing shallow-water ecotoxicological proxy species. However, it is unclear how the low temperature and high hydrostatic pressure prevalent in the deep sea affect toxicity, and whether adaptation to deep-sea environmental conditions moderates any effects of these factors. To address these uncertainties we assessed the effects of temperature and hydrostatic pressure on lethal and sublethal (respiration rate, antioxidant enzyme activity) toxicity in acute (96 h) copper and cadmium exposures, using the shallow-water ecophysiological model organism Palaemon varians. Low temperature reduced toxicity in both metals, but reduced cadmium toxicity significantly more. In contrast, elevated hydrostatic pressure increased copper toxicity, but did not affect cadmium toxicity. The synergistic interaction between copper and cadmium was not affected by low temperature, but high hydrostatic pressure significantly enhanced the synergism. Differential environmental effects on toxicity suggest different mechanisms of action for copper and cadmium, and highlight that mechanistic understanding of toxicity is fundamental to predicting environmental effects on toxicity. Although results infer that sensitivity to toxicants differs across biogeographic ranges, shallow-water species may be suitable ecotoxicological proxies for deep-sea species, dependent on adaptation to habitats with similar environmental variability.
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Affiliation(s)
- Alastair Brown
- University of Southampton, Ocean and Earth Science, National Oceanography Centre Southampton, European Way, Southampton, SO14 3ZH, U.K
| | - Sven Thatje
- University of Southampton, Ocean and Earth Science, National Oceanography Centre Southampton, European Way, Southampton, SO14 3ZH, U.K
| | - Chris Hauton
- University of Southampton, Ocean and Earth Science, National Oceanography Centre Southampton, European Way, Southampton, SO14 3ZH, U.K
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Yool A, Martin AP, Anderson TR, Bett BJ, Jones DOB, Ruhl HA. Big in the benthos: Future change of seafloor community biomass in a global, body size-resolved model. GLOBAL CHANGE BIOLOGY 2017; 23:3554-3566. [PMID: 28317324 DOI: 10.1111/gcb.13680] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/03/2016] [Revised: 02/24/2017] [Accepted: 02/24/2017] [Indexed: 05/16/2023]
Abstract
Deep-water benthic communities in the ocean are almost wholly dependent on near-surface pelagic ecosystems for their supply of energy and material resources. Primary production in sunlit surface waters is channelled through complex food webs that extensively recycle organic material, but lose a fraction as particulate organic carbon (POC) that sinks into the ocean interior. This exported production is further rarefied by microbial breakdown in the abyssal ocean, but a residual ultimately drives diverse assemblages of seafloor heterotrophs. Advances have led to an understanding of the importance of size (body mass) in structuring these communities. Here we force a size-resolved benthic biomass model, BORIS, using seafloor POC flux from a coupled ocean-biogeochemistry model, NEMO-MEDUSA, to investigate global patterns in benthic biomass. BORIS resolves 16 size classes of metazoans, successively doubling in mass from approximately 1 μg to 28 mg. Simulations find a wide range of seasonal responses to differing patterns of POC forcing, with both a decline in seasonal variability, and an increase in peak lag times with increasing body size. However, the dominant factor for modelled benthic communities is the integrated magnitude of POC reaching the seafloor rather than its seasonal pattern. Scenarios of POC forcing under climate change and ocean acidification are then applied to investigate how benthic communities may change under different future conditions. Against a backdrop of falling surface primary production (-6.1%), and driven by changes in pelagic remineralization with depth, results show that while benthic communities in shallow seas generally show higher biomass in a warmed world (+3.2%), deep-sea communities experience a substantial decline (-32%) under a high greenhouse gas emissions scenario. Our results underscore the importance for benthic ecology of reducing uncertainty in the magnitude and seasonality of seafloor POC fluxes, as well as the importance of studying a broader range of seafloor environments for future model development.
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Affiliation(s)
- Andrew Yool
- National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, UK
| | - Adrian P Martin
- National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, UK
| | - Thomas R Anderson
- National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, UK
| | - Brian J Bett
- National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, UK
| | - Daniel O B Jones
- National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, UK
| | - Henry A Ruhl
- National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, UK
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Baussant T, Nilsen M, Ravagnan E, Westerlund S, Ramanand S. Physiological responses and lipid storage of the coral Lophelia pertusa at varying food density. JOURNAL OF TOXICOLOGY AND ENVIRONMENTAL HEALTH. PART A 2017; 80:266-284. [PMID: 28569653 DOI: 10.1080/15287394.2017.1297274] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/07/2023]
Abstract
Despite the importance of the cold-water coral Lophelia pertusa to deep-sea reef ecosystem functioning, current knowledge of key physiological responses to available food resources is scarce. Scenarios with varying food density may help to understand how corals deal with seasonal variations in the dark ocean and might be used to study consequences of anthropogenic activities potentially affecting food availability. Thus, the physiological responses of L. pertusa to varying food (Artemia salina nauplii) concentration, ranging from 20% to 300% of carbon equivalent turned over by basal coral respiration, were investigated. A starvation group was also included. Measurements of respiration, growth, mucus production, and energy reserves (storage fatty acids) were performed at several time intervals over 26 weeks. In general, data showed a stronger effect of experimental time on measured responses, but no significant influence of food density treatment. In starved corals, respiration rate declined to 52% of initial respiration, while skeleton growth rate was maintained at the same rate as Artemia-fed corals throughout the investigation. Mucus production measured as the sum of dissolved organic carbon (DOC) and particulate organic carbon (POC) was also similar across food treatments, but POC production exceeded that of DOC at the highest food density. No marked effect was observed on storage fatty acids. These results confirm that L. pertusa is highly resilient to environmental conditions with suboptimal food densities over a time scale of months. Regulation of several physiological processes, including respiration and mucus production, possibly in combination with an opportunistic feeding strategy, contributed to this tolerance to maintain viable corals. Thus, it appears that L. pertusa is well adapted to life in the deep sea.
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Affiliation(s)
- Thierry Baussant
- a Department of Environment , International Research Institute of Stavanger , Randaberg , Norway
| | - Marianne Nilsen
- a Department of Environment , International Research Institute of Stavanger , Randaberg , Norway
- b Department of Research and Development , Western Norway University of Applied Sciences (HVL), Campus Sogndal , Sogndal , Norway
| | - Elisa Ravagnan
- a Department of Environment , International Research Institute of Stavanger , Randaberg , Norway
| | - Stig Westerlund
- a Department of Environment , International Research Institute of Stavanger , Randaberg , Norway
| | - Sreerekha Ramanand
- a Department of Environment , International Research Institute of Stavanger , Randaberg , Norway
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35
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Mattern T, Meyer S, Ellenberg U, Houston DM, Darby JT, Young M, van Heezik Y, Seddon PJ. Quantifying climate change impacts emphasises the importance of managing regional threats in the endangered Yellow-eyed penguin. PeerJ 2017; 5:e3272. [PMID: 28533952 PMCID: PMC5436559 DOI: 10.7717/peerj.3272] [Citation(s) in RCA: 24] [Impact Index Per Article: 3.4] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/09/2017] [Accepted: 03/28/2017] [Indexed: 11/20/2022] Open
Abstract
Climate change is a global issue with effects that are difficult to manage at a regional scale. Yet more often than not climate factors are just some of multiple stressors affecting species on a population level. Non-climatic factors—especially those of anthropogenic origins—may play equally important roles with regard to impacts on species and are often more feasible to address. Here we assess the influence of climate change on population trends of the endangered Yellow-eyed penguin (Megadyptes antipodes) over the last 30 years, using a Bayesian model. Sea surface temperature (SST) proved to be the dominating factor influencing survival of both adult birds and fledglings. Increasing SST since the mid-1990s was accompanied by a reduction in survival rates and population decline. The population model showed that 33% of the variation in population numbers could be explained by SST alone, significantly increasing pressure on the penguin population. Consequently, the population becomes less resilient to non-climate related impacts, such as fisheries interactions, habitat degradation and human disturbance. However, the extent of the contribution of these factors to declining population trends is extremely difficult to assess principally due to the absence of quantifiable data, creating a discussion bias towards climate variables, and effectively distracting from non-climate factors that can be managed on a regional scale to ensure the viability of the population.
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Affiliation(s)
- Thomas Mattern
- Department of Zoology, University of Otago, Dunedin, New Zealand
| | - Stefan Meyer
- Department of Zoology, University of Otago, Dunedin, New Zealand
| | - Ursula Ellenberg
- Department of Ecology, Environment and Evolution, La Trobe University, Melbourne, Australia
| | - David M Houston
- Science and Policy Group, Department of Conservation, Auckland, New Zealand
| | | | - Melanie Young
- Department of Zoology, University of Otago, Dunedin, New Zealand
| | | | - Philip J Seddon
- Department of Zoology, University of Otago, Dunedin, New Zealand
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36
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Keil R. Anthropogenic Forcing of Carbonate and Organic Carbon Preservation in Marine Sediments. ANNUAL REVIEW OF MARINE SCIENCE 2017; 9:151-172. [PMID: 27814028 DOI: 10.1146/annurev-marine-010816-060724] [Citation(s) in RCA: 20] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/16/2023]
Abstract
Carbon preservation in marine sediments, supplemented by that in large lakes, is the primary mechanism that moves carbon from the active surficial carbon cycle to the slower geologic carbon cycle. Preservation rates are low relative to the rates at which carbon moves between surface pools, which has led to the preservation term largely being ignored when evaluating anthropogenic forcing of the global carbon cycle. However, a variety of anthropogenic drivers-including ocean warming, deoxygenation, and acidification, as well as human-induced changes in sediment delivery to the ocean and mixing and irrigation of continental margin sediments-all work to decrease the already small carbon preservation term. These drivers affect the cycling of both carbonate and organic carbon in the ocean. The overall effect of anthropogenic forcing in the modern ocean is to decrease delivery of carbon to sediments, increase sedimentary dissolution and remineralization, and subsequently decrease overall carbon preservation.
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Affiliation(s)
- Richard Keil
- School of Oceanography, University of Washington, Seattle, Washington 98195-5351;
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37
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Drazen JC, Sutton TT. Dining in the Deep: The Feeding Ecology of Deep-Sea Fishes. ANNUAL REVIEW OF MARINE SCIENCE 2017; 9:337-366. [PMID: 27814034 DOI: 10.1146/annurev-marine-010816-060543] [Citation(s) in RCA: 48] [Impact Index Per Article: 6.9] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/06/2023]
Abstract
Deep-sea fishes inhabit ∼75% of the biosphere and are a critical part of deep-sea food webs. Diet analysis and more recent trophic biomarker approaches, such as stable isotopes and fatty-acid profiles, have enabled the description of feeding guilds and an increased recognition of the vertical connectivity in food webs in a whole-water-column sense, including benthic-pelagic coupling. Ecosystem modeling requires data on feeding rates; the available estimates indicate that deep-sea fishes have lower per-individual feeding rates than coastal and epipelagic fishes, but the overall predation impact may be high. A limited number of studies have measured the vertical flux of carbon by mesopelagic fishes, which appears to be substantial. Anthropogenic activities are altering deep-sea ecosystems and their services, which are mediated by trophic interactions. We also summarize outstanding data gaps.
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Affiliation(s)
- Jeffrey C Drazen
- Department of Oceanography, University of Hawaii at Manoa, Honolulu, Hawaii 96822;
| | - Tracey T Sutton
- Halmos College of Natural Sciences and Oceanography, Nova Southeastern University, Dania Beach, Florida 33004;
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38
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Soetaert K, Mohn C, Rengstorf A, Grehan A, van Oevelen D. Ecosystem engineering creates a direct nutritional link between 600-m deep cold-water coral mounds and surface productivity. Sci Rep 2016; 6:35057. [PMID: 27725742 PMCID: PMC5057138 DOI: 10.1038/srep35057] [Citation(s) in RCA: 8] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/05/2016] [Accepted: 09/20/2016] [Indexed: 11/09/2022] Open
Abstract
Cold-water corals (CWCs) form large mounds on the seafloor that are hotspots of biodiversity in the deep sea, but it remains enigmatic how CWCs can thrive in this food-limited environment. Here, we infer from model simulations that the interaction between tidal currents and CWC-formed mounds induces downwelling events of surface water that brings organic matter to 600-m deep CWCs. This positive feedback between CWC growth on carbonate mounds and enhanced food supply is essential for their sustenance in the deep sea and represents an example of ecosystem engineering of unparalleled magnitude. This ’topographically-enhanced carbon pump’ leaks organic matter that settles at greater depths. The ubiquitous presence of biogenic and geological topographies along ocean margins suggests that carbon sequestration through this pump is of global importance. These results indicate that enhanced stratification and lower surface productivity, both expected consequences of climate change, may negatively impact the energy balance of CWCs.
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Affiliation(s)
- Karline Soetaert
- NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems, and Utrecht University, Yerseke, The Netherlands
| | | | | | | | - Dick van Oevelen
- NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems, and Utrecht University, Yerseke, The Netherlands
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39
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Morris KJ, Bett BJ, Durden JM, Benoist NMA, Huvenne VAI, Jones DOB, Robert K, Ichino MC, Wolff GA, Ruhl HA. Landscape-scale spatial heterogeneity in phytodetrital cover and megafauna biomass in the abyss links to modest topographic variation. Sci Rep 2016; 6:34080. [PMID: 27681937 PMCID: PMC5040962 DOI: 10.1038/srep34080] [Citation(s) in RCA: 37] [Impact Index Per Article: 4.6] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/12/2016] [Accepted: 09/07/2016] [Indexed: 11/09/2022] Open
Abstract
Sinking particulate organic matter (POM, phytodetritus) is the principal limiting resource for deep-sea life. However, little is known about spatial variation in POM supply to the abyssal seafloor, which is frequently assumed to be homogenous. In reality, the abyss has a highly complex landscape with millions of hills and mountains. Here, we show a significant increase in seabed POM % cover (by ~1.05 times), and a large significant increase in megafauna biomass (by ~2.5 times), on abyssal hill terrain in comparison to the surrounding plain. These differences are substantially greater than predicted by current models linking water depth to POM supply or benthic biomass. Our observed variations in POM % cover (phytodetritus), megafauna biomass, sediment total organic carbon and total nitrogen, sedimentology, and benthic boundary layer turbidity, all appear to be consistent with topographically enhanced current speeds driving these enhancements. The effects are detectable with bathymetric elevations of only 10 s of metres above the surrounding plain. These results imply considerable unquantified heterogeneity in global ecology.
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Affiliation(s)
- Kirsty J Morris
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK
| | - Brian J Bett
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK
| | - Jennifer M Durden
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK.,Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, European Way, Southampton SO14 3ZH, UK
| | - Noelie M A Benoist
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK.,Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, European Way, Southampton SO14 3ZH, UK
| | - Veerle A I Huvenne
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK
| | - Daniel O B Jones
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK
| | - Katleen Robert
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK.,Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, European Way, Southampton SO14 3ZH, UK
| | - Matteo C Ichino
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK.,Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, European Way, Southampton SO14 3ZH, UK
| | - George A Wolff
- School of Environmental Sciences, University of Liverpool L69 3BX, UK
| | - Henry A Ruhl
- National Oceanography Centre, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK
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40
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Smith KL, Huffard CL, Sherman AD, Ruhl HA. Decadal Change in Sediment Community Oxygen Consumption in the Abyssal Northeast Pacific. AQUATIC GEOCHEMISTRY 2016; 22:401-417. [PMID: 32355451 PMCID: PMC7175715 DOI: 10.1007/s10498-016-9293-3] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 01/21/2016] [Accepted: 04/30/2016] [Indexed: 06/11/2023]
Abstract
Long time-series studies are critical to assessing impacts of climate change on the marine carbon cycle. A 27-year time-series study in the abyssal northeast Pacific (Sta. M, 4000 m depth) has provided the first concurrent measurements of sinking particulate organic carbon supply (POC flux) and remineralization by the benthic community. Sediment community oxygen consumption (SCOC), an estimate of organic carbon remineralization, was measured in situ over daily to interannual periods with four different instruments. Daily averages of SCOC ranged from a low of 5.0 mg C m-2 day-1 in February 1991 to a high of 31.0 mg C m-2 day-1 in June 2012. POC flux estimated from sediment trap collections at 600 and 50 m above bottom ranged from 0.3 mg C m-2 day-1 in October 2013 to 32.0 mg C m-2 day-1 in June 2011. Monthly averages of SCOC and POC flux correlated significantly with no time lag. Over the long time series, yearly average POC flux accounted for 63 % of the estimated carbon demand of the benthic community. Long time-series studies of sediment community processes, particularly SCOC, have shown similar fluctuations with the flux of POC reaching the abyssal seafloor. SCOC quickly responds to changes in food supply and tracks POC flux. Yet, SCOC consistently exceeds POC flux as measured by sediment traps alone. The shortfall of ~37 % could be explained by sediment trap sampling artifacts over decadal scales including undersampling of large sinking particles. High-resolution measurements of SCOC are critical to developing a realistic carbon cycle model for the open ocean. Such input is essential to evaluate the impact of climate change on the oceanic carbon cycle, and the long-term influences on the sedimentation record.
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Affiliation(s)
- K. L. Smith
- Monterey Bay Aquarium Research Institute, Moss Landing, CA USA
| | - C. L. Huffard
- Monterey Bay Aquarium Research Institute, Moss Landing, CA USA
| | - A. D. Sherman
- Monterey Bay Aquarium Research Institute, Moss Landing, CA USA
| | - H. A. Ruhl
- National Oceanography Centre, Southampton, UK
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41
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Provan F, Nilsen MM, Larssen E, Uleberg KE, Sydnes MO, Lyng E, Øysæd KB, Baussant T. An evaluation of coral lophelia pertusa mucus as an analytical matrix for environmental monitoring: A preliminary proteomic study. JOURNAL OF TOXICOLOGY AND ENVIRONMENTAL HEALTH. PART A 2016; 79:647-657. [PMID: 27484144 DOI: 10.1080/15287394.2016.1210494] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/06/2023]
Abstract
For the environmental monitoring of coral, mucus appears to be an appropriate biological matrix due to its array of functions in coral biology and the non-intrusive manner in which it can be collected. The aim of the present study was to evaluate the feasibility of using mucus of the stony coral Lophelia pertusa (L. pertusa) as an analytical matrix for discovery of biomarkers used for environmental monitoring. More specifically, to assess whether a mass-spectrometry-based proteomic approach can be applied to characterize the protein composition of coral mucus and changes related to petroleum discharges at the seafloor. Surface-enhanced laser desorption/ionization-time of flight mass spectrometry (SELDI-TOF MS) screening analyses of orange and white L. pertusa showed that the mucosal protein composition varies significantly with color phenotype, a pattern not reported prior to this study. Hence, to reduce variability from phenotype difference, L. pertusa white individuals only were selected to characterize in more detail the basal protein composition in mucus using liquid chromatography, mass spectrometry, mass spectrometry (LC-MS/MS). In total, 297 proteins were identified in L. pertusa mucus of unexposed coral individuals. Individuals exposed to drill cuttings in the range 2 to 12 mg/L showed modifications in coral mucus protein composition compared to unexposed corals. Although the results were somewhat inconsistent between individuals and require further validation in both the lab and the field, this study demonstrated preliminary encouraging results for discovery of protein markers in coral mucus that might provide more comprehensive insight into potential consequences attributed to anthropogenic stressors and may be used in future monitoring of coral health.
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Affiliation(s)
- Fiona Provan
- a International Research Institute of Stavanger (IRIS), Biomiljø , Randaberg , Norway
| | - Mari Mæland Nilsen
- a International Research Institute of Stavanger (IRIS), Biomiljø , Randaberg , Norway
| | - Eivind Larssen
- a International Research Institute of Stavanger (IRIS), Biomiljø , Randaberg , Norway
| | - Kai-Erik Uleberg
- a International Research Institute of Stavanger (IRIS), Biomiljø , Randaberg , Norway
| | - Magne O Sydnes
- a International Research Institute of Stavanger (IRIS), Biomiljø , Randaberg , Norway
- b Faculty of Science and Technology, Department of Mathematics and Natural Science , University of Stavanger , Stavanger , Norway
| | - Emily Lyng
- a International Research Institute of Stavanger (IRIS), Biomiljø , Randaberg , Norway
| | - Kjell Birger Øysæd
- a International Research Institute of Stavanger (IRIS), Biomiljø , Randaberg , Norway
| | - Thierry Baussant
- a International Research Institute of Stavanger (IRIS), Biomiljø , Randaberg , Norway
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42
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Abstract
The deep ocean absorbs vast amounts of heat and carbon dioxide, providing a critical buffer to climate change but exposing vulnerable ecosystems to combined stresses of warming, ocean acidification, deoxygenation, and altered food inputs. Resulting changes may threaten biodiversity and compromise key ocean services that maintain a healthy planet and human livelihoods. There exist large gaps in understanding of the physical and ecological feedbacks that will occur. Explicit recognition of deep-ocean climate mitigation and inclusion in adaptation planning by the United Nations Framework Convention on Climate Change (UNFCCC) could help to expand deep-ocean research and observation and to protect the integrity and functions of deep-ocean ecosystems.
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Affiliation(s)
- Lisa A Levin
- Center for Marine Biodiversity and Conservation, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093-0218, USA.
| | - Nadine Le Bris
- Sorbonne Universités, UPMC Univ. Paris 6, CNRS, Laboratoire d'Ecogéochimie des Environnements Benthiques, Observatoire Océanologique, 66650 Banyuls-sur-Mer, France
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Gutt J, Alvaro MC, Barco A, Böhmer A, Bracher A, David B, De Ridder C, Dorschel B, Eléaume M, Janussen D, Kersken D, López-González PJ, Martínez-Baraldés I, Schröder M, Segelken-Voigt A, Teixidó N. Macroepibenthic communities at the tip of the Antarctic Peninsula, an ecological survey at different spatial scales. Polar Biol 2015. [DOI: 10.1007/s00300-015-1797-6] [Citation(s) in RCA: 8] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/22/2022]
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van der Grient JMA, Rogers AD. Body Size Versus Depth: Regional and Taxonomical Variation in Deep-Sea Meio- and Macrofaunal Organisms. ADVANCES IN MARINE BIOLOGY 2015; 71:71-108. [PMID: 26320616 DOI: 10.1016/bs.amb.2015.07.002] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/04/2023]
Abstract
Body size (weight per individual) is an important concept in ecology. It has been studied in the deep sea where a decrease in size with increasing depth has often been found. This has been explained as an adaptation to food limitation where size reduction results in a lowered metabolic rate and a decreased energetic requirement. However, observations vary, with some studies showing an increase in size with depth, and some finding no depth correlation at all. Here, we collected data from peer-reviewed studies on macro- and meiofaunal abundance and biomass, creating two datasets allowing statistical comparison of factors expected to influence body size in meio- and macrofaunal organisms. Our analyses examined the influence of region, taxonomic group and sampling method on the body size of meiofauna and macrofauna in the deep sea with increasing depth, and the resulting models are presented. At the global scale, meio- and macrofaunal communities show a decrease in body size with increasing depth as expected with the food limitation hypothesis. However, at the regional scale there were differences in trends of body size with depth, either showing a decrease (e.g. southwest Pacific Ocean; meio- and macrofauna) or increase (e.g. Gulf of Mexico; meiofauna only) compared to a global mean. Taxonomic groups also showed differences in body size trends compared to total community average (e.g. Crustacea and Bivalvia). Care must be taken when conducting these studies, as our analyses indicated that sampling method exerts a significant influence on research results. It is possible that differences in physiology, lifestyle and life history characteristics result in different responses to an increase in depth and/or decrease in food availability. This will have implications in the future as food supply to the deep sea changes as a result of climate change (e.g. increased ocean stratification at low to mid latitudes and reduced sea ice duration at high latitudes).
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Affiliation(s)
| | - Alex D Rogers
- Department of Zoology, University of Oxford, Oxford, United Kingdom
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Gutt J, Bertler N, Bracegirdle TJ, Buschmann A, Comiso J, Hosie G, Isla E, Schloss IR, Smith CR, Tournadre J, Xavier JC. The Southern Ocean ecosystem under multiple climate change stresses--an integrated circumpolar assessment. GLOBAL CHANGE BIOLOGY 2015; 21:1434-53. [PMID: 25369312 DOI: 10.1111/gcb.12794] [Citation(s) in RCA: 77] [Impact Index Per Article: 8.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/05/2014] [Accepted: 10/13/2014] [Indexed: 05/26/2023]
Abstract
A quantitative assessment of observed and projected environmental changes in the Southern Ocean (SO) with a potential impact on the marine ecosystem shows: (i) large proportions of the SO are and will be affected by one or more climate change processes; areas projected to be affected in the future are larger than areas that are already under environmental stress, (ii) areas affected by changes in sea-ice in the past and likely in the future are much larger than areas affected by ocean warming. The smallest areas (<1% area of the SO) are affected by glacier retreat and warming in the deeper euphotic layer. In the future, decrease in the sea-ice is expected to be widespread. Changes in iceberg impact resulting from further collapse of ice-shelves can potentially affect large parts of shelf and ephemerally in the off-shore regions. However, aragonite undersaturation (acidification) might become one of the biggest problems for the Antarctic marine ecosystem by affecting almost the entire SO. Direct and indirect impacts of various environmental changes to the three major habitats, sea-ice, pelagic and benthos and their biota are complex. The areas affected by environmental stressors range from 33% of the SO for a single stressor, 11% for two and 2% for three, to <1% for four and five overlapping factors. In the future, areas expected to be affected by 2 and 3 overlapping factors are equally large, including potential iceberg changes, and together cover almost 86% of the SO ecosystem.
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Affiliation(s)
- Julian Gutt
- Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Alten Hafen 26, Bremerhaven, D - 27568, Germany
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Trueman CN, Johnston G, O'Hea B, MacKenzie KM. Trophic interactions of fish communities at midwater depths enhance long-term carbon storage and benthic production on continental slopes. Proc Biol Sci 2015; 281:rspb.2014.0669. [PMID: 24898373 DOI: 10.1098/rspb.2014.0669] [Citation(s) in RCA: 89] [Impact Index Per Article: 9.9] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/12/2022] Open
Abstract
Biological transfer of nutrients and materials between linked ecosystems influences global carbon budgets and ecosystem structure and function. Identifying the organisms or functional groups that are responsible for nutrient transfer, and quantifying their influence on ecosystem structure and carbon capture is an essential step for informed management of ecosystems in physically distant, but ecologically linked areas. Here, we combine natural abundance stable isotope tracers and survey data to show that mid-water and bentho-pelagic-feeding demersal fishes play an important role in the ocean carbon cycle, bypassing the detrital particle flux and transferring carbon to deep long-term storage. Global peaks in biomass and diversity of fishes at mid-slope depths are explained by competitive release of the demersal fish predators of mid-water organisms, which in turn support benthic fish production. Over 50% of the biomass of the demersal fish community at depths between 500 and 1800 m is supported by biological rather than detrital nutrient flux processes, and we estimate that bentho-pelagic fishes from the UK-Irish continental slope capture and store a volume of carbon equivalent to over 1 million tonnes of CO2 every year.
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Affiliation(s)
- C N Trueman
- Ocean and Earth Science, National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK
| | - G Johnston
- Marine Institute, Rinville, Oranmore, Co. Galway, Republic of Ireland
| | - B O'Hea
- Marine Institute, Rinville, Oranmore, Co. Galway, Republic of Ireland
| | - K M MacKenzie
- Ocean and Earth Science, National Oceanography Centre, Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK
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Lefort S, Aumont O, Bopp L, Arsouze T, Gehlen M, Maury O. Spatial and body-size dependent response of marine pelagic communities to projected global climate change. GLOBAL CHANGE BIOLOGY 2015; 21:154-64. [PMID: 25044507 DOI: 10.1111/gcb.12679] [Citation(s) in RCA: 40] [Impact Index Per Article: 4.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/09/2014] [Revised: 06/30/2014] [Accepted: 07/02/2014] [Indexed: 05/24/2023]
Abstract
Temperature, oxygen, and food availability directly affect marine life. Climate models project a global warming of the ocean's surface (~+3 °C), a de-oxygenation of the ocean's interior (~-3%) and a decrease in total marine net primary production (~-8%) under the 'business as usual' climate change scenario (RCP8.5). We estimated the effects of these changes on biological communities using a coupled biogeochemical (PISCES)--ecosystems (APECOSM) model forced by the physical outputs of the last generation of the IPSL-CM Earth System Model. The APECOSM model is a size-structured bio-energetic model that simulates the 3D dynamical distributions of three interactive pelagic communities (epipelagic, mesopelagic, and migratory) under the effects of multiple environmental factors. The PISCES-APECOSM model ran from 1850 to 2100 under historical forcing followed by RCP8.5. Our RCP8.5 simulation highlights significant changes in the spatial distribution, biomass, and maximum body-size of the simulated pelagic communities. Biomass and maximum body-size increase at high latitude over the course of the century, reflecting the capacity of marine organisms to respond to new suitable environment. At low- and midlatitude, biomass and maximum body-size strongly decrease. In those regions, large organisms cannot maintain their high metabolic needs because of limited and declining food availability. This resource reduction enhances the competition and modifies the biomass distribution among and within the three communities: the proportion of small organisms increases in the three communities and the migrant community that initially comprised a higher proportion of small organisms is favored. The greater resilience of small body-size organisms resides in their capacity to fulfill their metabolic needs under reduced energy supply and is further favored by the release of predation pressure due to the decline of large organisms. These results suggest that small body-size organisms might be more resilient to climate change than large ones.
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Affiliation(s)
- Stelly Lefort
- Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL CNRS/CEA/UVSQ), Orme des Merisiers, Point Courrier 132, Bât. 712, Gif-sur-Yvette Cedex, 91191, France
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How can we identify and communicate the ecological value of deep-sea ecosystem services? PLoS One 2014; 9:e100646. [PMID: 25055119 PMCID: PMC4108315 DOI: 10.1371/journal.pone.0100646] [Citation(s) in RCA: 28] [Impact Index Per Article: 2.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/20/2014] [Accepted: 05/28/2014] [Indexed: 12/02/2022] Open
Abstract
Submarine canyons are considered biodiversity hotspots which have been identified for their important roles in connecting the deep sea with shallower waters. To date, a huge gap exists between the high importance that scientists associate with deep-sea ecosystem services and the communication of this knowledge to decision makers and to the wider public, who remain largely ignorant of the importance of these services. The connectivity and complexity of marine ecosystems makes knowledge transfer very challenging, and new communication tools are necessary to increase understanding of ecological values beyond the science community. We show how the Ecosystem Principles Approach, a method that explains the importance of ocean processes via easily understandable ecological principles, might overcome this challenge for deep-sea ecosystem services. Scientists were asked to help develop a list of clear and concise ecosystem principles for the functioning of submarine canyons through a Delphi process to facilitate future transfers of ecological knowledge. These ecosystem principles describe ecosystem processes, link such processes to ecosystem services, and provide spatial and temporal information on the connectivity between deep and shallow waters. They also elucidate unique characteristics of submarine canyons. Our Ecosystem Principles Approach was successful in integrating ecological information into the ecosystem services assessment process. It therefore has a high potential to be the next step towards a wider implementation of ecological values in marine planning. We believe that successful communication of ecological knowledge is the key to a wider public support for ocean conservation, and that this endeavour has to be driven by scientists in their own interest as major deep-sea stakeholders.
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