Biomass Turnover Rates in Metabolically Active and Inactive Marine Calanoid Copepods

Lipid-storing copepods are fundamental to the functioning of marine ecosystems, transferring energy from primary producers to higher trophic levels and sequestering atmospheric carbon (C) in the deep ocean. Quantifying trophic transfer and biogeochemical cycling by copepods requires improved underst...

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Main Authors: Daniel J. Mayor, Kathryn B. Cook, Barry Thornton, Florence Atherden, Geraint A. Tarling, Thomas R. Anderson
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-06-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.907290/full
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author Daniel J. Mayor
Kathryn B. Cook
Barry Thornton
Florence Atherden
Geraint A. Tarling
Thomas R. Anderson
author_facet Daniel J. Mayor
Kathryn B. Cook
Barry Thornton
Florence Atherden
Geraint A. Tarling
Thomas R. Anderson
author_sort Daniel J. Mayor
collection DOAJ
description Lipid-storing copepods are fundamental to the functioning of marine ecosystems, transferring energy from primary producers to higher trophic levels and sequestering atmospheric carbon (C) in the deep ocean. Quantifying trophic transfer and biogeochemical cycling by copepods requires improved understanding of copepod metabolic rates in both surface waters and during lipid-fueled metabolism over winter. Here we present new biomass turnover rates of C and nitrogen (N) in Calanoides acutus, Calanoides natalis, Calanus glacialis and Calanus hyperboreus alongside published data for Calanus finmarchicus and Calanus pacificus. Turnover rates in metabolically active animals, normalised to 10°C, ranged between 0.007 – 0.105 d-1 and 0.004 – 0.065 d-1 for C and N, respectively. Turnover rates of C were typically faster than those for N, supporting the understanding that non-protein C, e.g. lipid, is catabolised faster than protein. Re-analysis of published data indicates that inactive, overwintering C. finmarchicus turn over wax ester lipids at a rate of 0.0016 d-1. These and other basal rate data will facilitate the mechanistic representation of copepod physiology in global biogeochemical models, thereby reducing uncertainties in our predictions of future ocean ecosystem functioning and C sequestration.
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spelling doaj.art-360fbe6bd24d4c9281316373b378b5442022-12-22T00:27:07ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452022-06-01910.3389/fmars.2022.907290907290Biomass Turnover Rates in Metabolically Active and Inactive Marine Calanoid CopepodsDaniel J. Mayor0Kathryn B. Cook1Barry Thornton2Florence Atherden3Geraint A. Tarling4Thomas R. Anderson5National Oceanography Centre, Southampton, United KingdomNational Oceanography Centre, Southampton, United KingdomJames Hutton Institute, Aberdeen, United KingdomNational Oceanography Centre, Southampton, United KingdomBritish Antarctic Survey, Cambridge, United KingdomNational Oceanography Centre, Southampton, United KingdomLipid-storing copepods are fundamental to the functioning of marine ecosystems, transferring energy from primary producers to higher trophic levels and sequestering atmospheric carbon (C) in the deep ocean. Quantifying trophic transfer and biogeochemical cycling by copepods requires improved understanding of copepod metabolic rates in both surface waters and during lipid-fueled metabolism over winter. Here we present new biomass turnover rates of C and nitrogen (N) in Calanoides acutus, Calanoides natalis, Calanus glacialis and Calanus hyperboreus alongside published data for Calanus finmarchicus and Calanus pacificus. Turnover rates in metabolically active animals, normalised to 10°C, ranged between 0.007 – 0.105 d-1 and 0.004 – 0.065 d-1 for C and N, respectively. Turnover rates of C were typically faster than those for N, supporting the understanding that non-protein C, e.g. lipid, is catabolised faster than protein. Re-analysis of published data indicates that inactive, overwintering C. finmarchicus turn over wax ester lipids at a rate of 0.0016 d-1. These and other basal rate data will facilitate the mechanistic representation of copepod physiology in global biogeochemical models, thereby reducing uncertainties in our predictions of future ocean ecosystem functioning and C sequestration.https://www.frontiersin.org/articles/10.3389/fmars.2022.907290/fulllipid turnoverprotein turnoverbasal metabolismdiapauseecosystem modelphysiology
spellingShingle Daniel J. Mayor
Kathryn B. Cook
Barry Thornton
Florence Atherden
Geraint A. Tarling
Thomas R. Anderson
Biomass Turnover Rates in Metabolically Active and Inactive Marine Calanoid Copepods
Frontiers in Marine Science
lipid turnover
protein turnover
basal metabolism
diapause
ecosystem model
physiology
title Biomass Turnover Rates in Metabolically Active and Inactive Marine Calanoid Copepods
title_full Biomass Turnover Rates in Metabolically Active and Inactive Marine Calanoid Copepods
title_fullStr Biomass Turnover Rates in Metabolically Active and Inactive Marine Calanoid Copepods
title_full_unstemmed Biomass Turnover Rates in Metabolically Active and Inactive Marine Calanoid Copepods
title_short Biomass Turnover Rates in Metabolically Active and Inactive Marine Calanoid Copepods
title_sort biomass turnover rates in metabolically active and inactive marine calanoid copepods
topic lipid turnover
protein turnover
basal metabolism
diapause
ecosystem model
physiology
url https://www.frontiersin.org/articles/10.3389/fmars.2022.907290/full
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