Iron Limitation Drives the Globally Extreme Fluorescence/Chlorophyll Ratios of the Southern Ocean

Abstract The ratio between fluorescence (F) and chlorophyll‐a (Chl)—where fluorescence is measured with a saturating fluorometer—is variable in the world's oceans, with the highest ratios and highest variability observed in the Southern Ocean. While species composition and Chl packaging per cel...

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Main Authors: Christina Schallenberg, Robert F. Strzepek, Sophie Bestley, Bozena Wojtasiewicz, Thomas W. Trull
Format: Article
Language:English
Published: Wiley 2022-06-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2021GL097616
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author Christina Schallenberg
Robert F. Strzepek
Sophie Bestley
Bozena Wojtasiewicz
Thomas W. Trull
author_facet Christina Schallenberg
Robert F. Strzepek
Sophie Bestley
Bozena Wojtasiewicz
Thomas W. Trull
author_sort Christina Schallenberg
collection DOAJ
description Abstract The ratio between fluorescence (F) and chlorophyll‐a (Chl)—where fluorescence is measured with a saturating fluorometer—is variable in the world's oceans, with the highest ratios and highest variability observed in the Southern Ocean. While species composition and Chl packaging per cell are strong drivers for the observed variability, additional factors, including iron limitation, have to this date not specifically been evaluated. Radiometers on biogeochemical (BGC)‐Argo floats allow for an independent estimate of Chl concentration that is based on the light attenuation coefficient, Kd. Making use of 4,000 radiometry profiles from BGC‐Argo floats in the Southern Ocean, we estimate Chl based on Kd and investigate the variability in F/Chl. Our analysis reveals a positive correlation between F/Chl and a proxy for iron limitation based on non‐photochemical quenching dynamics. The strong influence of iron limitation on F/Chl is further corroborated by data from Southern Ocean phytoplankton cultures.
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institution Kabale University
issn 0094-8276
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publishDate 2022-06-01
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series Geophysical Research Letters
spelling doaj-art-7f0bf97391b0442a84dfa1e21370b48f2025-01-22T14:38:16ZengWileyGeophysical Research Letters0094-82761944-80072022-06-014912n/an/a10.1029/2021GL097616Iron Limitation Drives the Globally Extreme Fluorescence/Chlorophyll Ratios of the Southern OceanChristina Schallenberg0Robert F. Strzepek1Sophie Bestley2Bozena Wojtasiewicz3Thomas W. Trull4Institute for Marine and Antarctic Studies University of Tasmania Hobart TAS AustraliaInstitute for Marine and Antarctic Studies University of Tasmania Hobart TAS AustraliaInstitute for Marine and Antarctic Studies University of Tasmania Hobart TAS AustraliaAustralian Antarctic Program Partnership Hobart TAS AustraliaOceans and Atmosphere CSIRO Hobart TAS AustraliaAbstract The ratio between fluorescence (F) and chlorophyll‐a (Chl)—where fluorescence is measured with a saturating fluorometer—is variable in the world's oceans, with the highest ratios and highest variability observed in the Southern Ocean. While species composition and Chl packaging per cell are strong drivers for the observed variability, additional factors, including iron limitation, have to this date not specifically been evaluated. Radiometers on biogeochemical (BGC)‐Argo floats allow for an independent estimate of Chl concentration that is based on the light attenuation coefficient, Kd. Making use of 4,000 radiometry profiles from BGC‐Argo floats in the Southern Ocean, we estimate Chl based on Kd and investigate the variability in F/Chl. Our analysis reveals a positive correlation between F/Chl and a proxy for iron limitation based on non‐photochemical quenching dynamics. The strong influence of iron limitation on F/Chl is further corroborated by data from Southern Ocean phytoplankton cultures.https://doi.org/10.1029/2021GL097616phytoplankton fluorescenceBGC‐ArgochlorophyllfluorometerSouthern Oceaniron limitation
spellingShingle Christina Schallenberg
Robert F. Strzepek
Sophie Bestley
Bozena Wojtasiewicz
Thomas W. Trull
Iron Limitation Drives the Globally Extreme Fluorescence/Chlorophyll Ratios of the Southern Ocean
Geophysical Research Letters
phytoplankton fluorescence
BGC‐Argo
chlorophyll
fluorometer
Southern Ocean
iron limitation
title Iron Limitation Drives the Globally Extreme Fluorescence/Chlorophyll Ratios of the Southern Ocean
title_full Iron Limitation Drives the Globally Extreme Fluorescence/Chlorophyll Ratios of the Southern Ocean
title_fullStr Iron Limitation Drives the Globally Extreme Fluorescence/Chlorophyll Ratios of the Southern Ocean
title_full_unstemmed Iron Limitation Drives the Globally Extreme Fluorescence/Chlorophyll Ratios of the Southern Ocean
title_short Iron Limitation Drives the Globally Extreme Fluorescence/Chlorophyll Ratios of the Southern Ocean
title_sort iron limitation drives the globally extreme fluorescence chlorophyll ratios of the southern ocean
topic phytoplankton fluorescence
BGC‐Argo
chlorophyll
fluorometer
Southern Ocean
iron limitation
url https://doi.org/10.1029/2021GL097616
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AT sophiebestley ironlimitationdrivesthegloballyextremefluorescencechlorophyllratiosofthesouthernocean
AT bozenawojtasiewicz ironlimitationdrivesthegloballyextremefluorescencechlorophyllratiosofthesouthernocean
AT thomaswtrull ironlimitationdrivesthegloballyextremefluorescencechlorophyllratiosofthesouthernocean