Unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminifera

Climate change is predicted to negatively impact calcification and change the structural integrity of biogenic carbonates, influencing their protective function. We assess the impacts of warming on the morphology and crystallography of Amphistegina lobifera, an abundant benthic foraminifera species...

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Main Authors: Danna Titelboim, Nikita J. Rothwell, Oliver T. Lord, Robert L. Harniman, Leanne A. Melbourne, Daniela N. Schmidt
Format: Article
Language:English
Published: The Royal Society 2024-04-01
Series:Royal Society Open Science
Subjects:
Online Access:https://royalsocietypublishing.org/doi/10.1098/rsos.231280
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author Danna Titelboim
Nikita J. Rothwell
Oliver T. Lord
Robert L. Harniman
Leanne A. Melbourne
Daniela N. Schmidt
author_facet Danna Titelboim
Nikita J. Rothwell
Oliver T. Lord
Robert L. Harniman
Leanne A. Melbourne
Daniela N. Schmidt
author_sort Danna Titelboim
collection DOAJ
description Climate change is predicted to negatively impact calcification and change the structural integrity of biogenic carbonates, influencing their protective function. We assess the impacts of warming on the morphology and crystallography of Amphistegina lobifera, an abundant benthic foraminifera species in shallow environments. Specimens from a thermally disturbed field area, mimicking future warming, are about 50% smaller compared with a control location. Differences in the position of the ν1 Raman mode of shells between the sites, which serves as a proxy for Mg content and calcification temperature, indicate that calcification is negatively impacted when temperatures are below the thermal range facilitating calcification. To test the impact of thermal stress on the Young's modulus of calcite which contributes to structural integrity, we quantify elasticity changes in large benthic foraminifera by applying atomic force microscopy to a different genus, Operculina ammonoides, cultured under optimal and high temperatures. Building on these observations of size and the sensitivity analysis for temperature-induced change in elasticity, we used finite element analysis to show that structural integrity is increased with reduced size and is largely insensitive to calcite elasticity. Our results indicate that warming-induced dwarfism creates shells that are more resistant to fracture because they are smaller.
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spelling doaj.art-96acb2cf7d1c4619b5fce15dcc527ecd2024-04-11T14:52:22ZengThe Royal SocietyRoyal Society Open Science2054-57032024-04-0111410.1098/rsos.231280Unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminiferaDanna Titelboim0Nikita J. Rothwell1Oliver T. Lord2Robert L. Harniman3Leanne A. Melbourne4Daniela N. Schmidt5School of Earth Sciences, University of Bristol , Bristol, UKSchool of Earth Sciences, University of Bristol , Bristol, UKSchool of Earth Sciences, University of Bristol , Bristol, UKSchool of Chemistry, University of Bristol , Bristol, UKSchool of Earth Sciences, University of Bristol , Bristol, UKSchool of Earth Sciences, University of Bristol , Bristol, UKClimate change is predicted to negatively impact calcification and change the structural integrity of biogenic carbonates, influencing their protective function. We assess the impacts of warming on the morphology and crystallography of Amphistegina lobifera, an abundant benthic foraminifera species in shallow environments. Specimens from a thermally disturbed field area, mimicking future warming, are about 50% smaller compared with a control location. Differences in the position of the ν1 Raman mode of shells between the sites, which serves as a proxy for Mg content and calcification temperature, indicate that calcification is negatively impacted when temperatures are below the thermal range facilitating calcification. To test the impact of thermal stress on the Young's modulus of calcite which contributes to structural integrity, we quantify elasticity changes in large benthic foraminifera by applying atomic force microscopy to a different genus, Operculina ammonoides, cultured under optimal and high temperatures. Building on these observations of size and the sensitivity analysis for temperature-induced change in elasticity, we used finite element analysis to show that structural integrity is increased with reduced size and is largely insensitive to calcite elasticity. Our results indicate that warming-induced dwarfism creates shells that are more resistant to fracture because they are smaller.https://royalsocietypublishing.org/doi/10.1098/rsos.231280ocean warmingthermal stresscalcificationstructural integritymorphological adaptation
spellingShingle Danna Titelboim
Nikita J. Rothwell
Oliver T. Lord
Robert L. Harniman
Leanne A. Melbourne
Daniela N. Schmidt
Unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminifera
Royal Society Open Science
ocean warming
thermal stress
calcification
structural integrity
morphological adaptation
title Unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminifera
title_full Unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminifera
title_fullStr Unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminifera
title_full_unstemmed Unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminifera
title_short Unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminifera
title_sort unexpected increase in structural integrity caused by thermally induced dwarfism in large benthic foraminifera
topic ocean warming
thermal stress
calcification
structural integrity
morphological adaptation
url https://royalsocietypublishing.org/doi/10.1098/rsos.231280
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