Environmental Controls of Size Distribution of Modern Planktonic Foraminifera in the Tropical Indian Ocean

Abstract Paleoceanographic studies often rely on abundance changes in microfossil species, with little consideration for characteristics such as organism size, which may also be related to environmental changes. Using a tropical Indian Ocean (TIO) core‐top data set, we test the Optimum size‐hypothes...

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Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Michael B. Adebayo, Clara T. Bolton, Ross Marchant, Franck Bassinot, Sandrine Conrod, Thibault deGaridel‐Thoron
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2022GC010586
https://doaj.org/article/6bc734eab0b34ecf80f1b7c541d923a8
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spelling ftdoajarticles:oai:doaj.org/article:6bc734eab0b34ecf80f1b7c541d923a8 2023-12-03T10:29:13+01:00 Environmental Controls of Size Distribution of Modern Planktonic Foraminifera in the Tropical Indian Ocean Michael B. Adebayo Clara T. Bolton Ross Marchant Franck Bassinot Sandrine Conrod Thibault deGaridel‐Thoron 2023-04-01T00:00:00Z https://doi.org/10.1029/2022GC010586 https://doaj.org/article/6bc734eab0b34ecf80f1b7c541d923a8 EN eng Wiley https://doi.org/10.1029/2022GC010586 https://doaj.org/toc/1525-2027 1525-2027 doi:10.1029/2022GC010586 https://doaj.org/article/6bc734eab0b34ecf80f1b7c541d923a8 Geochemistry, Geophysics, Geosystems, Vol 24, Iss 4, Pp n/a-n/a (2023) planktonic foraminifera size automated analysis optimum size‐hypothesis environmental controls sea surface temperature carbonate ion concentration Geophysics. Cosmic physics QC801-809 Geology QE1-996.5 article 2023 ftdoajarticles https://doi.org/10.1029/2022GC010586 2023-11-05T01:35:59Z Abstract Paleoceanographic studies often rely on abundance changes in microfossil species, with little consideration for characteristics such as organism size, which may also be related to environmental changes. Using a tropical Indian Ocean (TIO) core‐top data set, we test the Optimum size‐hypothesis (OSH), investigating whether relative abundance or environmental variables are better descriptors of planktonic foraminifera species' optimum conditions. We also investigate the environmental drivers of whole‐assemblage planktonic foraminiferal test size variation in the TIO. We use an automated imaging and sorting system (MiSo) to identify planktonic foraminiferal species, analyze their morphology, and quantify fragmentation rate using machine learning techniques. Machine model accuracy is confirmed by comparison with human classifiers (97% accuracy). Data for 33 environmental parameters were extracted from modern databases and, through exploratory factor analysis and regression models, we explore relationships between planktonic foraminiferal size and oceanographic parameters in the TIO. Results show that the size frequency distribution of most planktonic foraminifera species is unimodal, with some larger species showing multimodal distributions. Assemblage size95/5 (95th percentile size) increases with increasing species diversity, and this is attributed to vertical niche separation induced by thermal stratification. Our test for the OSH reveals that relative abundance is not a good predictor of species' optima and within‐species size95/5 response to environmental parameters is species‐specific, with parameters related to carbonate ion concentration, temperature, and salinity being primary drivers. At the species and assemblage levels, our analyses indicate that carbonate ion concentration and temperature play important roles in determining size trends in TIO planktonic foraminifera. Article in Journal/Newspaper Planktonic foraminifera Directory of Open Access Journals: DOAJ Articles Indian Geochemistry, Geophysics, Geosystems 24 4
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic planktonic foraminifera size
automated analysis
optimum size‐hypothesis
environmental controls
sea surface temperature
carbonate ion concentration
Geophysics. Cosmic physics
QC801-809
Geology
QE1-996.5
spellingShingle planktonic foraminifera size
automated analysis
optimum size‐hypothesis
environmental controls
sea surface temperature
carbonate ion concentration
Geophysics. Cosmic physics
QC801-809
Geology
QE1-996.5
Michael B. Adebayo
Clara T. Bolton
Ross Marchant
Franck Bassinot
Sandrine Conrod
Thibault deGaridel‐Thoron
Environmental Controls of Size Distribution of Modern Planktonic Foraminifera in the Tropical Indian Ocean
topic_facet planktonic foraminifera size
automated analysis
optimum size‐hypothesis
environmental controls
sea surface temperature
carbonate ion concentration
Geophysics. Cosmic physics
QC801-809
Geology
QE1-996.5
description Abstract Paleoceanographic studies often rely on abundance changes in microfossil species, with little consideration for characteristics such as organism size, which may also be related to environmental changes. Using a tropical Indian Ocean (TIO) core‐top data set, we test the Optimum size‐hypothesis (OSH), investigating whether relative abundance or environmental variables are better descriptors of planktonic foraminifera species' optimum conditions. We also investigate the environmental drivers of whole‐assemblage planktonic foraminiferal test size variation in the TIO. We use an automated imaging and sorting system (MiSo) to identify planktonic foraminiferal species, analyze their morphology, and quantify fragmentation rate using machine learning techniques. Machine model accuracy is confirmed by comparison with human classifiers (97% accuracy). Data for 33 environmental parameters were extracted from modern databases and, through exploratory factor analysis and regression models, we explore relationships between planktonic foraminiferal size and oceanographic parameters in the TIO. Results show that the size frequency distribution of most planktonic foraminifera species is unimodal, with some larger species showing multimodal distributions. Assemblage size95/5 (95th percentile size) increases with increasing species diversity, and this is attributed to vertical niche separation induced by thermal stratification. Our test for the OSH reveals that relative abundance is not a good predictor of species' optima and within‐species size95/5 response to environmental parameters is species‐specific, with parameters related to carbonate ion concentration, temperature, and salinity being primary drivers. At the species and assemblage levels, our analyses indicate that carbonate ion concentration and temperature play important roles in determining size trends in TIO planktonic foraminifera.
format Article in Journal/Newspaper
author Michael B. Adebayo
Clara T. Bolton
Ross Marchant
Franck Bassinot
Sandrine Conrod
Thibault deGaridel‐Thoron
author_facet Michael B. Adebayo
Clara T. Bolton
Ross Marchant
Franck Bassinot
Sandrine Conrod
Thibault deGaridel‐Thoron
author_sort Michael B. Adebayo
title Environmental Controls of Size Distribution of Modern Planktonic Foraminifera in the Tropical Indian Ocean
title_short Environmental Controls of Size Distribution of Modern Planktonic Foraminifera in the Tropical Indian Ocean
title_full Environmental Controls of Size Distribution of Modern Planktonic Foraminifera in the Tropical Indian Ocean
title_fullStr Environmental Controls of Size Distribution of Modern Planktonic Foraminifera in the Tropical Indian Ocean
title_full_unstemmed Environmental Controls of Size Distribution of Modern Planktonic Foraminifera in the Tropical Indian Ocean
title_sort environmental controls of size distribution of modern planktonic foraminifera in the tropical indian ocean
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2022GC010586
https://doaj.org/article/6bc734eab0b34ecf80f1b7c541d923a8
geographic Indian
geographic_facet Indian
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source Geochemistry, Geophysics, Geosystems, Vol 24, Iss 4, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2022GC010586
https://doaj.org/toc/1525-2027
1525-2027
doi:10.1029/2022GC010586
https://doaj.org/article/6bc734eab0b34ecf80f1b7c541d923a8
op_doi https://doi.org/10.1029/2022GC010586
container_title Geochemistry, Geophysics, Geosystems
container_volume 24
container_issue 4
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