Daily timescale dynamics of planktonic foraminifera shell-size distributions

Planktonic foraminifera (PF) shells comprise a significant fraction of the global oceanic carbonate flux and serve as a primary archive of the history of the oceans. Yet, a limited understanding of their life cycles dynamics and biological rhythms, hampers their application as palaeoceanographic pro...

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Main Authors: Natalie Chernihovsky, Adi Torfstein, Ahuva Almogi-Labin
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-05-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2023.1126398/full
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author Natalie Chernihovsky
Natalie Chernihovsky
Adi Torfstein
Adi Torfstein
Ahuva Almogi-Labin
author_facet Natalie Chernihovsky
Natalie Chernihovsky
Adi Torfstein
Adi Torfstein
Ahuva Almogi-Labin
author_sort Natalie Chernihovsky
collection DOAJ
description Planktonic foraminifera (PF) shells comprise a significant fraction of the global oceanic carbonate flux and serve as a primary archive of the history of the oceans. Yet, a limited understanding of their life cycles dynamics and biological rhythms, hampers their application as palaeoceanographic proxies. Here, we present the flux of ten PF species and their shell-size distributions at a daily timescale resolution in the Gulf of Aqaba (GOA), northern Red Sea. We report diameter measurements of ~13,500 shells, associated with ten PF species, retrieved using an automated time-series sediment trap deployed at a water depth of ~410 m (seafloor depth 610 m) throughout more than a full annual cycle between 2015 and 2016. Most of the PF species display a wide intraspecific shell-size distribution among adult PF, while six abundant species (G. ruber, G. rubescens + G. tenellus, G. glutinata, G. calida and G. siphonifera) display significantly smaller shell-sizes compared with corresponding specimens from sediment traps and seafloor sediments across other tropical, subtropical and upwelling regions. The results indicate that PF generation cycles can be classified according to three patterns: (1) Quiescent: minimal shell-size and extended life cycles due to unfavorable conditions and food scarcity when the water column is stratified and oligotrophic, (2) Transient: the gradual increase of Chlorophyll-a (Chl-a) concentrations and food availability enhance shorter life-cycles, although PF do not necessarily reach maximal shell-sizes, (3) Successive: PF fluxes and Chl-a concentrations are maximal, the generation time is extended and individuals might display growth to maximal shell-sizes.
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spelling doaj.art-9b31730e2af5470f87f8e1b362f9b3462023-05-18T08:11:54ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452023-05-011010.3389/fmars.2023.11263981126398Daily timescale dynamics of planktonic foraminifera shell-size distributionsNatalie Chernihovsky0Natalie Chernihovsky1Adi Torfstein2Adi Torfstein3Ahuva Almogi-Labin4The Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem, IsraelThe Interuniversity Institute for Marine Sciences, Eilat, IsraelThe Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, Jerusalem, IsraelThe Interuniversity Institute for Marine Sciences, Eilat, IsraelGeological Survey of Israel, Jerusalem, IsraelPlanktonic foraminifera (PF) shells comprise a significant fraction of the global oceanic carbonate flux and serve as a primary archive of the history of the oceans. Yet, a limited understanding of their life cycles dynamics and biological rhythms, hampers their application as palaeoceanographic proxies. Here, we present the flux of ten PF species and their shell-size distributions at a daily timescale resolution in the Gulf of Aqaba (GOA), northern Red Sea. We report diameter measurements of ~13,500 shells, associated with ten PF species, retrieved using an automated time-series sediment trap deployed at a water depth of ~410 m (seafloor depth 610 m) throughout more than a full annual cycle between 2015 and 2016. Most of the PF species display a wide intraspecific shell-size distribution among adult PF, while six abundant species (G. ruber, G. rubescens + G. tenellus, G. glutinata, G. calida and G. siphonifera) display significantly smaller shell-sizes compared with corresponding specimens from sediment traps and seafloor sediments across other tropical, subtropical and upwelling regions. The results indicate that PF generation cycles can be classified according to three patterns: (1) Quiescent: minimal shell-size and extended life cycles due to unfavorable conditions and food scarcity when the water column is stratified and oligotrophic, (2) Transient: the gradual increase of Chlorophyll-a (Chl-a) concentrations and food availability enhance shorter life-cycles, although PF do not necessarily reach maximal shell-sizes, (3) Successive: PF fluxes and Chl-a concentrations are maximal, the generation time is extended and individuals might display growth to maximal shell-sizes.https://www.frontiersin.org/articles/10.3389/fmars.2023.1126398/fullplanktonic foraminiferashell-size distributionlife cyclesbiological rhythmssediment trapsoligotrophic sea
spellingShingle Natalie Chernihovsky
Natalie Chernihovsky
Adi Torfstein
Adi Torfstein
Ahuva Almogi-Labin
Daily timescale dynamics of planktonic foraminifera shell-size distributions
Frontiers in Marine Science
planktonic foraminifera
shell-size distribution
life cycles
biological rhythms
sediment traps
oligotrophic sea
title Daily timescale dynamics of planktonic foraminifera shell-size distributions
title_full Daily timescale dynamics of planktonic foraminifera shell-size distributions
title_fullStr Daily timescale dynamics of planktonic foraminifera shell-size distributions
title_full_unstemmed Daily timescale dynamics of planktonic foraminifera shell-size distributions
title_short Daily timescale dynamics of planktonic foraminifera shell-size distributions
title_sort daily timescale dynamics of planktonic foraminifera shell size distributions
topic planktonic foraminifera
shell-size distribution
life cycles
biological rhythms
sediment traps
oligotrophic sea
url https://www.frontiersin.org/articles/10.3389/fmars.2023.1126398/full
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