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Large-scale culturing of the subpolar foraminifera Globigerina bulloides reveals tolerance to a large range of environmental parameters associated to different life-strategies and an extended lifespan

Large-scale culturing of the subpolar foraminifera Globigerina bulloides reveals tolerance to a large range of environmental parameters associated to different life-strategies and an extended lifespan
Large-scale culturing of the subpolar foraminifera Globigerina bulloides reveals tolerance to a large range of environmental parameters associated to different life-strategies and an extended lifespan
The subtropical to subpolar planktic foraminifera Globigerina bulloides is a calcifying marine protist, and one of the dominant foraminiferal species of the Nordic Seas. Previously, the relative abundance and shell geochemistry of fossil G. bulloides have been studied for palaeoceanographic reconstructions. There is however a lack of biological observations on the species and a poor understanding of its ecological tolerances, especially for high latitude genotypes. Here, we present observations from the first extensive culturing of G. bulloides under subpolar conditions, including the first low temperature (6–13°C) and variable salinity (30–38) experiments. Carbonate chemistry (pH and [CO32−]) was also manipulated. Experimental conditions were chosen to reflect a range of plausible past and future scenarios for the Nordic Seas. We found G. bulloides to be tolerant of environmental conditions well outside their optimal range (<10°C, salinity <33, pH <8). Observed life span was up to three months, which was attributed to a microalgal diet. Two alternative life strategies were employed, whereby individuals either experienced rapid growth and death, or a prolonged lifespan with minimal growth and death via slow decay. We posit this could help explain differences in geochemical signals recorded from different size fractions of fossil specimens used for palaeoceanographic reconstructions.
0142-7873
403-420
Sykes, Freya E.
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Meilland, Julie
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Westgård, Adele
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Chalk, Thomas B.
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Chierici, Melissa
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Foster, Gavin L.
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Ezat, Mohamed M.
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Dolan, John
c889133e-1e23-44a6-be78-7c819832e199
Sykes, Freya E.
9e036ab6-c4c6-4793-8067-9775bc00c819
Meilland, Julie
ef0c3ebf-8970-452e-9520-9995e090dcc0
Westgård, Adele
50b9f77a-0d49-40bf-8ab9-8b0ee4261781
Chalk, Thomas B.
0021bbe6-6ab1-4a30-8542-654d0f2d1a0a
Chierici, Melissa
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Foster, Gavin L.
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Ezat, Mohamed M.
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Dolan, John
c889133e-1e23-44a6-be78-7c819832e199

Sykes, Freya E., Meilland, Julie, Westgård, Adele, Chalk, Thomas B., Chierici, Melissa, Foster, Gavin L. and Ezat, Mohamed M. , Dolan, John (ed.) (2024) Large-scale culturing of the subpolar foraminifera Globigerina bulloides reveals tolerance to a large range of environmental parameters associated to different life-strategies and an extended lifespan. Journal of Plankton Research, 46 (4), 403-420. (doi:10.1093/plankt/fbae029).

Record type: Article

Abstract

The subtropical to subpolar planktic foraminifera Globigerina bulloides is a calcifying marine protist, and one of the dominant foraminiferal species of the Nordic Seas. Previously, the relative abundance and shell geochemistry of fossil G. bulloides have been studied for palaeoceanographic reconstructions. There is however a lack of biological observations on the species and a poor understanding of its ecological tolerances, especially for high latitude genotypes. Here, we present observations from the first extensive culturing of G. bulloides under subpolar conditions, including the first low temperature (6–13°C) and variable salinity (30–38) experiments. Carbonate chemistry (pH and [CO32−]) was also manipulated. Experimental conditions were chosen to reflect a range of plausible past and future scenarios for the Nordic Seas. We found G. bulloides to be tolerant of environmental conditions well outside their optimal range (<10°C, salinity <33, pH <8). Observed life span was up to three months, which was attributed to a microalgal diet. Two alternative life strategies were employed, whereby individuals either experienced rapid growth and death, or a prolonged lifespan with minimal growth and death via slow decay. We posit this could help explain differences in geochemical signals recorded from different size fractions of fossil specimens used for palaeoceanographic reconstructions.

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Accepted/In Press date: 15 May 2024
Published date: 7 June 2024

Identifiers

Local EPrints ID: 498187
URI: http://eprints.soton.ac.uk/id/eprint/498187
ISSN: 0142-7873
PURE UUID: 166ae96d-85a0-41f8-9192-e0c6f2891282
ORCID for Thomas B. Chalk: ORCID iD orcid.org/0000-0002-2880-3847
ORCID for Gavin L. Foster: ORCID iD orcid.org/0000-0003-3688-9668

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Date deposited: 12 Feb 2025 17:35
Last modified: 22 Aug 2025 02:18

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Contributors

Author: Freya E. Sykes
Author: Julie Meilland
Author: Adele Westgård
Author: Thomas B. Chalk ORCID iD
Author: Melissa Chierici
Author: Gavin L. Foster ORCID iD
Author: Mohamed M. Ezat
Editor: John Dolan

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