Ocean community warming responses explained by thermal affinities and temperature gradients

As ocean temperatures rise, species distributions are tracking towards historically cooler regions in line with their thermal affinity1,2. However, different responses of species to warming and changed species interactions make predicting biodiversity redistribution and relative abundance a challeng...

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Published in:Nature Climate Change
Main Authors: Burrows, Michael T, Bates, Amanda E, Costello, Mark J, Edwards, Martin, Edgar, Graham J, Fox, Clive J, Halpern, Benjamin S, Hiddink, Jan G, Pinsky, Malin L, Batt, Ryan D, Molinos, Jorge Garcia, Payne, Benjamin L, Schoeman, D S, Stuart-Smith, Rick D, Poloczanska, Elvira S
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2019
Subjects:
Online Access:https://doi.org/10.1038/s41558-019-0631-5
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author Burrows, Michael T
Bates, Amanda E
Costello, Mark J
Edwards, Martin
Edgar, Graham J
Fox, Clive J
Halpern, Benjamin S
Hiddink, Jan G
Pinsky, Malin L
Batt, Ryan D
Molinos, Jorge Garcia
Payne, Benjamin L
Schoeman, D S
Stuart-Smith, Rick D
Poloczanska, Elvira S
author_facet Burrows, Michael T
Bates, Amanda E
Costello, Mark J
Edwards, Martin
Edgar, Graham J
Fox, Clive J
Halpern, Benjamin S
Hiddink, Jan G
Pinsky, Malin L
Batt, Ryan D
Molinos, Jorge Garcia
Payne, Benjamin L
Schoeman, D S
Stuart-Smith, Rick D
Poloczanska, Elvira S
author_sort Burrows, Michael T
collection University of the Sunshine Coast, Queensland, Australia: COAST Research Database
container_issue 12
container_start_page 959
container_title Nature Climate Change
container_volume 9
description As ocean temperatures rise, species distributions are tracking towards historically cooler regions in line with their thermal affinity1,2. However, different responses of species to warming and changed species interactions make predicting biodiversity redistribution and relative abundance a challenge3,4. Here, we use three decades of fish and plankton survey data to assess how warming changes the relative dominance of warm-affinity and cold-affinity species5,6. Regions with stable temperatures (for example, the Northeast Pacific and Gulf of Mexico) show little change in dominance structure, while areas with warming (for example, the North Atlantic) see strong shifts towards warm-water species dominance. Importantly, communities whose species pools had diverse thermal affinities and a narrower range of thermal tolerance showed greater sensitivity, as anticipated from simulations. The composition of fish communities changed less than expected in regions with strong temperature depth gradients. There, species track temperatures by moving deeper2,7, rather than horizontally, analogous to elevation shifts in land plants8. Temperature thus emerges as a fundamental driver for change in marine systems, with predictable restructuring of communities in the most rapidly warming areas using metrics based on species thermal affinities. The ready and predictable dominance shifts suggest a strong prognosis of resilience to climate change for these communities.
format Article in Journal/Newspaper
genre North Atlantic
genre_facet North Atlantic
geographic Pacific
geographic_facet Pacific
id ftunivscoast:usc:30064
institution Open Polar
language English
op_collection_id ftunivscoast
op_container_end_page 963
op_doi https://doi.org/10.1038/s41558-019-0631-5
op_relation usc:30064
URN:ISSN: 1758-678X
publishDate 2019
publisher Nature Publishing Group
record_format openpolar
spelling ftunivscoast:usc:30064 2025-01-16T23:41:38+00:00 Ocean community warming responses explained by thermal affinities and temperature gradients Burrows, Michael T Bates, Amanda E Costello, Mark J Edwards, Martin Edgar, Graham J Fox, Clive J Halpern, Benjamin S Hiddink, Jan G Pinsky, Malin L Batt, Ryan D Molinos, Jorge Garcia Payne, Benjamin L Schoeman, D S Stuart-Smith, Rick D Poloczanska, Elvira S 2019 https://doi.org/10.1038/s41558-019-0631-5 eng eng Nature Publishing Group usc:30064 URN:ISSN: 1758-678X FoR 0401 (Atmospheric Sciences) FoR 0406 (Physical Geography and Environmental Geoscience) FoR 0502 (Environmental Science and Management) Journal Article 2019 ftunivscoast https://doi.org/10.1038/s41558-019-0631-5 2019-12-16T23:25:37Z As ocean temperatures rise, species distributions are tracking towards historically cooler regions in line with their thermal affinity1,2. However, different responses of species to warming and changed species interactions make predicting biodiversity redistribution and relative abundance a challenge3,4. Here, we use three decades of fish and plankton survey data to assess how warming changes the relative dominance of warm-affinity and cold-affinity species5,6. Regions with stable temperatures (for example, the Northeast Pacific and Gulf of Mexico) show little change in dominance structure, while areas with warming (for example, the North Atlantic) see strong shifts towards warm-water species dominance. Importantly, communities whose species pools had diverse thermal affinities and a narrower range of thermal tolerance showed greater sensitivity, as anticipated from simulations. The composition of fish communities changed less than expected in regions with strong temperature depth gradients. There, species track temperatures by moving deeper2,7, rather than horizontally, analogous to elevation shifts in land plants8. Temperature thus emerges as a fundamental driver for change in marine systems, with predictable restructuring of communities in the most rapidly warming areas using metrics based on species thermal affinities. The ready and predictable dominance shifts suggest a strong prognosis of resilience to climate change for these communities. Article in Journal/Newspaper North Atlantic University of the Sunshine Coast, Queensland, Australia: COAST Research Database Pacific Nature Climate Change 9 12 959 963
spellingShingle FoR 0401 (Atmospheric Sciences)
FoR 0406 (Physical Geography and Environmental Geoscience)
FoR 0502 (Environmental Science and Management)
Burrows, Michael T
Bates, Amanda E
Costello, Mark J
Edwards, Martin
Edgar, Graham J
Fox, Clive J
Halpern, Benjamin S
Hiddink, Jan G
Pinsky, Malin L
Batt, Ryan D
Molinos, Jorge Garcia
Payne, Benjamin L
Schoeman, D S
Stuart-Smith, Rick D
Poloczanska, Elvira S
Ocean community warming responses explained by thermal affinities and temperature gradients
title Ocean community warming responses explained by thermal affinities and temperature gradients
title_full Ocean community warming responses explained by thermal affinities and temperature gradients
title_fullStr Ocean community warming responses explained by thermal affinities and temperature gradients
title_full_unstemmed Ocean community warming responses explained by thermal affinities and temperature gradients
title_short Ocean community warming responses explained by thermal affinities and temperature gradients
title_sort ocean community warming responses explained by thermal affinities and temperature gradients
topic FoR 0401 (Atmospheric Sciences)
FoR 0406 (Physical Geography and Environmental Geoscience)
FoR 0502 (Environmental Science and Management)
topic_facet FoR 0401 (Atmospheric Sciences)
FoR 0406 (Physical Geography and Environmental Geoscience)
FoR 0502 (Environmental Science and Management)
url https://doi.org/10.1038/s41558-019-0631-5