Global reductions in seafloor biomass in response to climate change

Seafloor organisms are vital for healthy marine ecosystems, contributing to elemental cycling, benthic remineralization, and ultimately sequestration of carbon. Deep-sea life is primarily reliant on the export flux of particulate organic carbon from the surface ocean for food, but most ocean biogeoc...

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Published in:Global Change Biology
Main Authors: Jones, DOB, Yool, A, Wei, C, Henson, SA, Ruhl, HA, Watson, RA, Gehlen, M
Format: Article in Journal/Newspaper
Language:English
Published: Blackwell Publishing Ltd 2013
Subjects:
Online Access:https://doi.org/10.1111/gcb.12480
http://www.ncbi.nlm.nih.gov/pubmed/24382828
http://ecite.utas.edu.au/96093
id ftunivtasecite:oai:ecite.utas.edu.au:96093
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spelling ftunivtasecite:oai:ecite.utas.edu.au:96093 2023-05-15T17:41:37+02:00 Global reductions in seafloor biomass in response to climate change Jones, DOB Yool, A Wei, C Henson, SA Ruhl, HA Watson, RA Gehlen, M 2013 https://doi.org/10.1111/gcb.12480 http://www.ncbi.nlm.nih.gov/pubmed/24382828 http://ecite.utas.edu.au/96093 en eng Blackwell Publishing Ltd http://dx.doi.org/10.1111/gcb.12480 Jones, DOB and Yool, A and Wei, C and Henson, SA and Ruhl, HA and Watson, RA and Gehlen, M, Global reductions in seafloor biomass in response to climate change, Global Change Biology, 20, (6) pp. 1861-1872. ISSN 1354-1013 (2013) [Refereed Article] http://www.ncbi.nlm.nih.gov/pubmed/24382828 http://ecite.utas.edu.au/96093 Agricultural and Veterinary Sciences Fisheries Sciences Aquatic Ecosystem Studies and Stock Assessment Refereed Article PeerReviewed 2013 ftunivtasecite https://doi.org/10.1111/gcb.12480 2019-12-13T21:58:23Z Seafloor organisms are vital for healthy marine ecosystems, contributing to elemental cycling, benthic remineralization, and ultimately sequestration of carbon. Deep-sea life is primarily reliant on the export flux of particulate organic carbon from the surface ocean for food, but most ocean biogeochemistry models predict global decreases in export flux resulting from 21st century anthropogenically induced warming. Here we show that decadal-to-century scale changes in carbon export associated with climate change lead to an estimated 5.2% decrease in future (20912100) global open ocean benthic biomass under RCP8.5 (reduction of 5.2 Mt C) compared with contemporary conditions (20062015). Our projections use multi-model mean export flux estimates from eight fully coupled earth system models, which contributed to the Coupled Model Intercomparison Project Phase 5, that have been forced by high and low representative concentration pathways (RCP8.5 and 4.5, respectively). These export flux estimates are used in conjunction with published empirical relationships to predict changes in benthic biomass. The polar oceans and some upwelling areas may experience increases in benthic biomass, but most other regions show decreases, with up to 38% reductions in parts of the northeast Atlantic. Our analysis projects a future ocean with smaller sized infaunal benthos, potentially reducing energy transfer rates though benthic multicellular food webs. More than 80% of potential deep-water biodiversity hotspots known around the world, including canyons, seamounts, and cold-water coral reefs, are projected to experience negative changes in biomass. These major reductions in biomass may lead to widespread change in benthic ecosystems and the functions and services they provide. Article in Journal/Newspaper Northeast Atlantic eCite UTAS (University of Tasmania) Global Change Biology 20 6 1861 1872
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Agricultural and Veterinary Sciences
Fisheries Sciences
Aquatic Ecosystem Studies and Stock Assessment
spellingShingle Agricultural and Veterinary Sciences
Fisheries Sciences
Aquatic Ecosystem Studies and Stock Assessment
Jones, DOB
Yool, A
Wei, C
Henson, SA
Ruhl, HA
Watson, RA
Gehlen, M
Global reductions in seafloor biomass in response to climate change
topic_facet Agricultural and Veterinary Sciences
Fisheries Sciences
Aquatic Ecosystem Studies and Stock Assessment
description Seafloor organisms are vital for healthy marine ecosystems, contributing to elemental cycling, benthic remineralization, and ultimately sequestration of carbon. Deep-sea life is primarily reliant on the export flux of particulate organic carbon from the surface ocean for food, but most ocean biogeochemistry models predict global decreases in export flux resulting from 21st century anthropogenically induced warming. Here we show that decadal-to-century scale changes in carbon export associated with climate change lead to an estimated 5.2% decrease in future (20912100) global open ocean benthic biomass under RCP8.5 (reduction of 5.2 Mt C) compared with contemporary conditions (20062015). Our projections use multi-model mean export flux estimates from eight fully coupled earth system models, which contributed to the Coupled Model Intercomparison Project Phase 5, that have been forced by high and low representative concentration pathways (RCP8.5 and 4.5, respectively). These export flux estimates are used in conjunction with published empirical relationships to predict changes in benthic biomass. The polar oceans and some upwelling areas may experience increases in benthic biomass, but most other regions show decreases, with up to 38% reductions in parts of the northeast Atlantic. Our analysis projects a future ocean with smaller sized infaunal benthos, potentially reducing energy transfer rates though benthic multicellular food webs. More than 80% of potential deep-water biodiversity hotspots known around the world, including canyons, seamounts, and cold-water coral reefs, are projected to experience negative changes in biomass. These major reductions in biomass may lead to widespread change in benthic ecosystems and the functions and services they provide.
format Article in Journal/Newspaper
author Jones, DOB
Yool, A
Wei, C
Henson, SA
Ruhl, HA
Watson, RA
Gehlen, M
author_facet Jones, DOB
Yool, A
Wei, C
Henson, SA
Ruhl, HA
Watson, RA
Gehlen, M
author_sort Jones, DOB
title Global reductions in seafloor biomass in response to climate change
title_short Global reductions in seafloor biomass in response to climate change
title_full Global reductions in seafloor biomass in response to climate change
title_fullStr Global reductions in seafloor biomass in response to climate change
title_full_unstemmed Global reductions in seafloor biomass in response to climate change
title_sort global reductions in seafloor biomass in response to climate change
publisher Blackwell Publishing Ltd
publishDate 2013
url https://doi.org/10.1111/gcb.12480
http://www.ncbi.nlm.nih.gov/pubmed/24382828
http://ecite.utas.edu.au/96093
genre Northeast Atlantic
genre_facet Northeast Atlantic
op_relation http://dx.doi.org/10.1111/gcb.12480
Jones, DOB and Yool, A and Wei, C and Henson, SA and Ruhl, HA and Watson, RA and Gehlen, M, Global reductions in seafloor biomass in response to climate change, Global Change Biology, 20, (6) pp. 1861-1872. ISSN 1354-1013 (2013) [Refereed Article]
http://www.ncbi.nlm.nih.gov/pubmed/24382828
http://ecite.utas.edu.au/96093
op_doi https://doi.org/10.1111/gcb.12480
container_title Global Change Biology
container_volume 20
container_issue 6
container_start_page 1861
op_container_end_page 1872
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