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Morphological Insights From Benthic Foraminifera for Environmental Conditions in the Baltic Sea During the Last Interglacial

Ni, Sha LU ; Muter, Dirk ; Charrieau, Laurie ; Pirzamanbein, Behnaz LU orcid ; Choquel, Constance LU ; Knudsen, Karen Luise ; Seidenkrantz, Marit-Solveig and Filipsson, Helena L. LU orcid (2025) In Paleoceanography and Paleoclimatology 40(3).
Abstract
Marine environments worldwide are increasingly threatened by warming, deoxygenation, and ocean acidification. These stressors can be recorded as alterations in foraminiferal geochemistry and morphology. We integrated morphological features with assemblage and geochemical records of benthic foraminifera from the Danish Straits at the entrance to the Baltic Sea, covering the Last Interglacial period (LIG, MIS5e), to assess potential indications of environmental changes. Using synchrotron radiation X-ray microcomputed tomography (SRµCT), we measured Elphidium clavatum in terms of diameter, height, surface area, volume, thickness, and number of pores. Pore patterns and wall thickness were evaluated simultaneously to assess both metabolic and... (More)
Marine environments worldwide are increasingly threatened by warming, deoxygenation, and ocean acidification. These stressors can be recorded as alterations in foraminiferal geochemistry and morphology. We integrated morphological features with assemblage and geochemical records of benthic foraminifera from the Danish Straits at the entrance to the Baltic Sea, covering the Last Interglacial period (LIG, MIS5e), to assess potential indications of environmental changes. Using synchrotron radiation X-ray microcomputed tomography (SRµCT), we measured Elphidium clavatum in terms of diameter, height, surface area, volume, thickness, and number of pores. Pore patterns and wall thickness were evaluated simultaneously to assess both metabolic and mechanical constraints under environmental changes. The proloculus (initial chamber) size may indicate the reproduction mode of foraminifera in response to environmental stress, including salinity and oxygen variations. We show that during the early-mid LIG, the physical resistance of E. clavatum against mechanical constraints remained relatively strong, characterized by high wall thickness and low porosity, coinciding with higher bottom water salinity and oxygen content. In the mid-late LIG, pore density and wall thickness decreased, while porosity and proloculus size increased, fueling metabolism and increasing survival rates. These traits reflect adaptation to an increasingly stressful environment with lower salinity and oxygen levels, as indicated by declining faunal diversity and increasing E. clavatum abundance. Our study demonstrates that benthic foraminiferal morphological features, including proloculus size, wall thickness, and pore patterns, serve as indicators for assessing stress levels and reconstructing bottom water conditions in brackish and potentially hypoxic environments during the LIG. (Less)
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author
; ; ; ; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
in
Paleoceanography and Paleoclimatology
volume
40
issue
3
article number
e2024PA005063
publisher
John Wiley & Sons Inc.
external identifiers
  • scopus:105000781110
ISSN
2572-4517
DOI
10.1029/2024PA005063
project
Tracing hypoxia during warm periods in the Baltic Sea region - using synchrotron X-ray spectroscopy and plasma analytical methods
Environmental changes in foraminiferal shell morphology revealed by synchrotron μCT
language
English
LU publication?
yes
id
aa1dd385-3fbd-4b45-8f42-8e49a657e73b
date added to LUP
2025-03-26 13:47:51
date last changed
2025-04-04 15:22:06
@article{aa1dd385-3fbd-4b45-8f42-8e49a657e73b,
  abstract     = {{Marine environments worldwide are increasingly threatened by warming, deoxygenation, and ocean acidification. These stressors can be recorded as alterations in foraminiferal geochemistry and morphology. We integrated morphological features with assemblage and geochemical records of benthic foraminifera from the Danish Straits at the entrance to the Baltic Sea, covering the Last Interglacial period (LIG, MIS5e), to assess potential indications of environmental changes. Using synchrotron radiation X-ray microcomputed tomography (SRµCT), we measured Elphidium clavatum in terms of diameter, height, surface area, volume, thickness, and number of pores. Pore patterns and wall thickness were evaluated simultaneously to assess both metabolic and mechanical constraints under environmental changes. The proloculus (initial chamber) size may indicate the reproduction mode of foraminifera in response to environmental stress, including salinity and oxygen variations. We show that during the early-mid LIG, the physical resistance of E. clavatum against mechanical constraints remained relatively strong, characterized by high wall thickness and low porosity, coinciding with higher bottom water salinity and oxygen content. In the mid-late LIG, pore density and wall thickness decreased, while porosity and proloculus size increased, fueling metabolism and increasing survival rates. These traits reflect adaptation to an increasingly stressful environment with lower salinity and oxygen levels, as indicated by declining faunal diversity and increasing E. clavatum abundance. Our study demonstrates that benthic foraminiferal morphological features, including proloculus size, wall thickness, and pore patterns, serve as indicators for assessing stress levels and reconstructing bottom water conditions in brackish and potentially hypoxic environments during the LIG.}},
  author       = {{Ni, Sha and Muter, Dirk and Charrieau, Laurie and Pirzamanbein, Behnaz and Choquel, Constance and Knudsen, Karen Luise and Seidenkrantz, Marit-Solveig and Filipsson, Helena L.}},
  issn         = {{2572-4517}},
  language     = {{eng}},
  month        = {{03}},
  number       = {{3}},
  publisher    = {{John Wiley & Sons Inc.}},
  series       = {{Paleoceanography and Paleoclimatology}},
  title        = {{Morphological Insights From Benthic Foraminifera for Environmental Conditions in the Baltic Sea During the Last Interglacial}},
  url          = {{http://dx.doi.org/10.1029/2024PA005063}},
  doi          = {{10.1029/2024PA005063}},
  volume       = {{40}},
  year         = {{2025}},
}