Arctic Observations Identify Phytoplankton Community Composition as Driver of Carbon Flux Attenuation

Abstract The attenuation coefficient b is one of the most common ways to describe how strong the carbon flux is attenuated throughout the water column. Therefore, b is an essential input variable in many carbon flux and climate models. Marsay et al. (2015, https://doi.org/10.1073/pnas.1415311112) pr...

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Main Authors: I. Wiedmann, E. Ceballos‐Romero, M. Villa‐Alfageme, A. H. H. Renner, C. Dybwad, H. van derJagt, C. Svensen, P. Assmy, J. M. Wiktor, A. Tatarek, M. Różańska‐Pluta, M. H. Iversen
Format: Article
Language:English
Published: Wiley 2020-07-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1029/2020GL087465
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author I. Wiedmann
E. Ceballos‐Romero
M. Villa‐Alfageme
A. H. H. Renner
C. Dybwad
H. van derJagt
C. Svensen
P. Assmy
J. M. Wiktor
A. Tatarek
M. Różańska‐Pluta
M. H. Iversen
author_facet I. Wiedmann
E. Ceballos‐Romero
M. Villa‐Alfageme
A. H. H. Renner
C. Dybwad
H. van derJagt
C. Svensen
P. Assmy
J. M. Wiktor
A. Tatarek
M. Różańska‐Pluta
M. H. Iversen
author_sort I. Wiedmann
collection DOAJ
description Abstract The attenuation coefficient b is one of the most common ways to describe how strong the carbon flux is attenuated throughout the water column. Therefore, b is an essential input variable in many carbon flux and climate models. Marsay et al. (2015, https://doi.org/10.1073/pnas.1415311112) proposed that the median surface water temperature (0–500 m) may be a predictor of b, but our observations from Arctic waters challenge this hypothesis. We found a highly variable attenuation coefficient (b = 0.43–1.84) in cold Arctic waters (<4.1 °C). Accordingly, we suggest that water temperature is not a globally valid predictor of the attenuation coefficient. We advocate instead that the phytoplankton composition and especially the relative abundance of diatoms can be used to parametrize the carbon flux attenuation in local and global carbon flux models.
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institution Kabale University
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publishDate 2020-07-01
publisher Wiley
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series Geophysical Research Letters
spelling doaj-art-d0fa124eabae43ddb818a801a0d32b072025-08-20T03:47:41ZengWileyGeophysical Research Letters0094-82761944-80072020-07-014714n/an/a10.1029/2020GL087465Arctic Observations Identify Phytoplankton Community Composition as Driver of Carbon Flux AttenuationI. Wiedmann0E. Ceballos‐Romero1M. Villa‐Alfageme2A. H. H. Renner3C. Dybwad4H. van derJagt5C. Svensen6P. Assmy7J. M. Wiktor8A. Tatarek9M. Różańska‐Pluta10M. H. Iversen11UiT The Arctic University of Norway Tromsø NorwayDepartamento de Física Aplicada II Universidad de Sevilla SpainDepartamento de Física Aplicada II Universidad de Sevilla SpainInstitute of Marine Research, Fram Centre Tromsø NorwayUiT The Arctic University of Norway Tromsø NorwayAlfred‐Wegener‐Institute, Helmholtz Center for Polar and Marine Research Bremerhaven GermanyUiT The Arctic University of Norway Tromsø NorwayNorwegian Polar Institute, Fram Centre Tromsø NorwayInstitute of Oceanology, Polish Academy of Sciences (IOPAN) Sopot PolandInstitute of Oceanology, Polish Academy of Sciences (IOPAN) Sopot PolandInstitute of Oceanology, Polish Academy of Sciences (IOPAN) Sopot PolandAlfred‐Wegener‐Institute, Helmholtz Center for Polar and Marine Research Bremerhaven GermanyAbstract The attenuation coefficient b is one of the most common ways to describe how strong the carbon flux is attenuated throughout the water column. Therefore, b is an essential input variable in many carbon flux and climate models. Marsay et al. (2015, https://doi.org/10.1073/pnas.1415311112) proposed that the median surface water temperature (0–500 m) may be a predictor of b, but our observations from Arctic waters challenge this hypothesis. We found a highly variable attenuation coefficient (b = 0.43–1.84) in cold Arctic waters (<4.1 °C). Accordingly, we suggest that water temperature is not a globally valid predictor of the attenuation coefficient. We advocate instead that the phytoplankton composition and especially the relative abundance of diatoms can be used to parametrize the carbon flux attenuation in local and global carbon flux models.https://doi.org/10.1029/2020GL087465biological carbon pumpcarbon flux attenuationdiatomscarbon exportMartin coefficient bsediment traps
spellingShingle I. Wiedmann
E. Ceballos‐Romero
M. Villa‐Alfageme
A. H. H. Renner
C. Dybwad
H. van derJagt
C. Svensen
P. Assmy
J. M. Wiktor
A. Tatarek
M. Różańska‐Pluta
M. H. Iversen
Arctic Observations Identify Phytoplankton Community Composition as Driver of Carbon Flux Attenuation
Geophysical Research Letters
biological carbon pump
carbon flux attenuation
diatoms
carbon export
Martin coefficient b
sediment traps
title Arctic Observations Identify Phytoplankton Community Composition as Driver of Carbon Flux Attenuation
title_full Arctic Observations Identify Phytoplankton Community Composition as Driver of Carbon Flux Attenuation
title_fullStr Arctic Observations Identify Phytoplankton Community Composition as Driver of Carbon Flux Attenuation
title_full_unstemmed Arctic Observations Identify Phytoplankton Community Composition as Driver of Carbon Flux Attenuation
title_short Arctic Observations Identify Phytoplankton Community Composition as Driver of Carbon Flux Attenuation
title_sort arctic observations identify phytoplankton community composition as driver of carbon flux attenuation
topic biological carbon pump
carbon flux attenuation
diatoms
carbon export
Martin coefficient b
sediment traps
url https://doi.org/10.1029/2020GL087465
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