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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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Glover AG, Gooday AJ, Bailey DM, Billett DSM, Chevaldonné P, Colaço A, Copley J, Cuvelier D, Desbruyères D, Kalogeropoulou V, Klages M, Lampadariou N, Lejeusne C, Mestre NC, Paterson GLJ, Perez T, Ruhl H, Sarrazin J, Soltwedel T, Soto EH, Thatje S, Tselepides A, Van Gaever S, Vanreusel A. Temporal change in deep-sea benthic ecosystems: a review of the evidence from recent time-series studies. ADVANCES IN MARINE BIOLOGY 2010; 58:1-95. [PMID: 20959156 DOI: 10.1016/b978-0-12-381015-1.00001-0] [Citation(s) in RCA: 30] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/19/2023]
Abstract
Societal concerns over the potential impacts of recent global change have prompted renewed interest in the long-term ecological monitoring of large ecosystems. The deep sea is the largest ecosystem on the planet, the least accessible, and perhaps the least understood. Nevertheless, deep-sea data collected over the last few decades are now being synthesised with a view to both measuring global change and predicting the future impacts of further rises in atmospheric carbon dioxide concentrations. For many years, it was assumed by many that the deep sea is a stable habitat, buffered from short-term changes in the atmosphere or upper ocean. However, recent studies suggest that deep-seafloor ecosystems may respond relatively quickly to seasonal, inter-annual and decadal-scale shifts in upper-ocean variables. In this review, we assess the evidence for these long-term (i.e. inter-annual to decadal-scale) changes both in biologically driven, sedimented, deep-sea ecosystems (e.g. abyssal plains) and in chemosynthetic ecosystems that are partially geologically driven, such as hydrothermal vents and cold seeps. We have identified 11 deep-sea sedimented ecosystems for which published analyses of long-term biological data exist. At three of these, we have found evidence for a progressive trend that could be potentially linked to recent climate change, although the evidence is not conclusive. At the other sites, we have concluded that the changes were either not significant, or were stochastically variable without being clearly linked to climate change or climate variability indices. For chemosynthetic ecosystems, we have identified 14 sites for which there are some published long-term data. Data for temporal changes at chemosynthetic ecosystems are scarce, with few sites being subjected to repeated visits. However, the limited evidence from hydrothermal vents suggests that at fast-spreading centres such as the East Pacific Rise, vent communities are impacted on decadal scales by stochastic events such as volcanic eruptions, with associated fauna showing complex patterns of community succession. For the slow-spreading centres such as the Mid-Atlantic Ridge, vent sites appear to be stable over the time periods measured, with no discernable long-term trend. At cold seeps, inferences based on spatial studies in the Gulf of Mexico, and data on organism longevity, suggest that these sites are stable over many hundreds of years. However, at the Haakon Mosby mud volcano, a large, well-studied seep in the Barents Sea, periodic mud slides associated with gas and fluid venting may disrupt benthic communities, leading to successional sequences over time. For chemosynthetic ecosystems of biogenic origin (e.g. whale-falls), it is likely that the longevity of the habitat depends mainly on the size of the carcass and the ecological setting, with large remains persisting as a distinct seafloor habitat for up to 100 years. Studies of shallow-water analogs of deep-sea ecosystems such as marine caves may also yield insights into temporal processes. Although it is obvious from the geological record that past climate change has impacted deep-sea faunas, the evidence that recent climate change or climate variability has altered deep-sea benthic communities is extremely limited. This mainly reflects the lack of remote sensing of this vast seafloor habitat. Current and future advances in deep-ocean benthic science involve new remote observing technologies that combine a high temporal resolution (e.g. cabled observatories) with spatial capabilities (e.g. autonomous vehicles undertaking image surveys of the seabed).
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Affiliation(s)
- A G Glover
- Zoology Department, The Natural History Museum, London, United Kingdom
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