Kelp carbon sink potential decreases with warming due to accelerating decomposition.

Cycling of organic carbon in the ocean has the potential to mitigate or exacerbate global climate change, but major questions remain about the environmental controls on organic carbon flux in the coastal zone. Here, we used a field experiment distributed across 28° of latitude, and the entire range...

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Main Authors: Karen Filbee-Dexter, Colette J Feehan, Dan A Smale, Kira A Krumhansl, Skye Augustine, Florian de Bettignies, Michael T Burrows, Jarrett E K Byrnes, Jillian Campbell, Dominique Davoult, Kenneth H Dunton, João N Franco, Ignacio Garrido, Sean P Grace, Kasper Hancke, Ladd E Johnson, Brenda Konar, Pippa J Moore, Kjell Magnus Norderhaug, Alasdair O'Dell, Morten F Pedersen, Anne K Salomon, Isabel Sousa-Pinto, Scott Tiegs, Dara Yiu, Thomas Wernberg
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2022-08-01
Series:PLoS Biology
Online Access:https://doi.org/10.1371/journal.pbio.3001702
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author Karen Filbee-Dexter
Colette J Feehan
Dan A Smale
Kira A Krumhansl
Skye Augustine
Florian de Bettignies
Michael T Burrows
Jarrett E K Byrnes
Jillian Campbell
Dominique Davoult
Kenneth H Dunton
João N Franco
Ignacio Garrido
Sean P Grace
Kasper Hancke
Ladd E Johnson
Brenda Konar
Pippa J Moore
Kjell Magnus Norderhaug
Alasdair O'Dell
Morten F Pedersen
Anne K Salomon
Isabel Sousa-Pinto
Scott Tiegs
Dara Yiu
Thomas Wernberg
author_facet Karen Filbee-Dexter
Colette J Feehan
Dan A Smale
Kira A Krumhansl
Skye Augustine
Florian de Bettignies
Michael T Burrows
Jarrett E K Byrnes
Jillian Campbell
Dominique Davoult
Kenneth H Dunton
João N Franco
Ignacio Garrido
Sean P Grace
Kasper Hancke
Ladd E Johnson
Brenda Konar
Pippa J Moore
Kjell Magnus Norderhaug
Alasdair O'Dell
Morten F Pedersen
Anne K Salomon
Isabel Sousa-Pinto
Scott Tiegs
Dara Yiu
Thomas Wernberg
author_sort Karen Filbee-Dexter
collection DOAJ
description Cycling of organic carbon in the ocean has the potential to mitigate or exacerbate global climate change, but major questions remain about the environmental controls on organic carbon flux in the coastal zone. Here, we used a field experiment distributed across 28° of latitude, and the entire range of 2 dominant kelp species in the northern hemisphere, to measure decomposition rates of kelp detritus on the seafloor in relation to local environmental factors. Detritus decomposition in both species were strongly related to ocean temperature and initial carbon content, with higher rates of biomass loss at lower latitudes with warmer temperatures. Our experiment showed slow overall decomposition and turnover of kelp detritus and modeling of coastal residence times at our study sites revealed that a significant portion of this production can remain intact long enough to reach deep marine sinks. The results suggest that decomposition of these kelp species could accelerate with ocean warming and that low-latitude kelp forests could experience the greatest increase in remineralization with a 9% to 42% reduced potential for transport to long-term ocean sinks under short-term (RCP4.5) and long-term (RCP8.5) warming scenarios. However, slow decomposition at high latitudes, where kelp abundance is predicted to expand, indicates potential for increasing kelp-carbon sinks in cooler (northern) regions. Our findings reveal an important latitudinal gradient in coastal ecosystem function that provides an improved capacity to predict the implications of ocean warming on carbon cycling. Broad-scale patterns in organic carbon decomposition revealed here can be used to identify hotspots of carbon sequestration potential and resolve relationships between carbon cycling processes and ocean climate at a global scale.
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spelling doaj.art-b48237f33d0942878a0913765ebf06762023-07-28T05:30:51ZengPublic Library of Science (PLoS)PLoS Biology1544-91731545-78852022-08-01208e300170210.1371/journal.pbio.3001702Kelp carbon sink potential decreases with warming due to accelerating decomposition.Karen Filbee-DexterColette J FeehanDan A SmaleKira A KrumhanslSkye AugustineFlorian de BettigniesMichael T BurrowsJarrett E K ByrnesJillian CampbellDominique DavoultKenneth H DuntonJoão N FrancoIgnacio GarridoSean P GraceKasper HanckeLadd E JohnsonBrenda KonarPippa J MooreKjell Magnus NorderhaugAlasdair O'DellMorten F PedersenAnne K SalomonIsabel Sousa-PintoScott TiegsDara YiuThomas WernbergCycling of organic carbon in the ocean has the potential to mitigate or exacerbate global climate change, but major questions remain about the environmental controls on organic carbon flux in the coastal zone. Here, we used a field experiment distributed across 28° of latitude, and the entire range of 2 dominant kelp species in the northern hemisphere, to measure decomposition rates of kelp detritus on the seafloor in relation to local environmental factors. Detritus decomposition in both species were strongly related to ocean temperature and initial carbon content, with higher rates of biomass loss at lower latitudes with warmer temperatures. Our experiment showed slow overall decomposition and turnover of kelp detritus and modeling of coastal residence times at our study sites revealed that a significant portion of this production can remain intact long enough to reach deep marine sinks. The results suggest that decomposition of these kelp species could accelerate with ocean warming and that low-latitude kelp forests could experience the greatest increase in remineralization with a 9% to 42% reduced potential for transport to long-term ocean sinks under short-term (RCP4.5) and long-term (RCP8.5) warming scenarios. However, slow decomposition at high latitudes, where kelp abundance is predicted to expand, indicates potential for increasing kelp-carbon sinks in cooler (northern) regions. Our findings reveal an important latitudinal gradient in coastal ecosystem function that provides an improved capacity to predict the implications of ocean warming on carbon cycling. Broad-scale patterns in organic carbon decomposition revealed here can be used to identify hotspots of carbon sequestration potential and resolve relationships between carbon cycling processes and ocean climate at a global scale.https://doi.org/10.1371/journal.pbio.3001702
spellingShingle Karen Filbee-Dexter
Colette J Feehan
Dan A Smale
Kira A Krumhansl
Skye Augustine
Florian de Bettignies
Michael T Burrows
Jarrett E K Byrnes
Jillian Campbell
Dominique Davoult
Kenneth H Dunton
João N Franco
Ignacio Garrido
Sean P Grace
Kasper Hancke
Ladd E Johnson
Brenda Konar
Pippa J Moore
Kjell Magnus Norderhaug
Alasdair O'Dell
Morten F Pedersen
Anne K Salomon
Isabel Sousa-Pinto
Scott Tiegs
Dara Yiu
Thomas Wernberg
Kelp carbon sink potential decreases with warming due to accelerating decomposition.
PLoS Biology
title Kelp carbon sink potential decreases with warming due to accelerating decomposition.
title_full Kelp carbon sink potential decreases with warming due to accelerating decomposition.
title_fullStr Kelp carbon sink potential decreases with warming due to accelerating decomposition.
title_full_unstemmed Kelp carbon sink potential decreases with warming due to accelerating decomposition.
title_short Kelp carbon sink potential decreases with warming due to accelerating decomposition.
title_sort kelp carbon sink potential decreases with warming due to accelerating decomposition
url https://doi.org/10.1371/journal.pbio.3001702
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