Articles | Volume 44, issue 1
https://doi.org/10.5194/jm-44-79-2025
https://doi.org/10.5194/jm-44-79-2025
Review article
 | 
20 Mar 2025
Review article |  | 20 Mar 2025

Recent benthic foraminifera communities offshore of Thwaites Glacier in the Amundsen Sea, Antarctica: implications for interpretations of fossil assemblages

Asmara A. Lehrmann, Rebecca L. Totten, Julia S. Wellner, Claus-Dieter Hillenbrand, Svetlana Radionovskaya, R. Michael Comas, Robert D. Larter, Alastair G. C. Graham, James D. Kirkham, Kelly A. Hogan, Victoria Fitzgerald, Rachel W. Clark, Becky Hopkins, Allison P. Lepp, Elaine Mawbey, Rosemary V. Smyth, Lauren E. Miller, James A. Smith, and Frank O. Nitsche

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Cited articles

Anderson, J. B.: Ecology and Distribution of Foraminifera in the Weddell Sea of Antarctica, Micropaleontology, 21, 69–96, https://doi.org/10.2307/1485156, 1975. 
Arrigo, K. R., Lowry, K. E., and van Dijken, G. L.: Annual changes in sea-ice and phytoplankton in polynyas of the Amundsen Sea, Antarctica, Deep-Sea Res. Pt. II, 71–76, 5–15, https://doi.org/10.1016/j.dsr2.2012.03.006, 2012. 
Arrigo, K. R., van Dijken, G. L., and Strong, A. L.: Environmental controls of marine productivity hot spots around Antarctica, J. Geophys. Res.-Oceans, 120, 5545–5565, https://doi.org/10.1002/2015JC010888, 2015. 
Balco, G., Brown, N., Nichols, K., Venturelli, R. A., Adams, J., Braddock, S., Campbell, S., Goehring, B., Johnson, J. S., Rood, D. H., Wilcken, K., Hall, B., and Woodward, J.: Reversible ice sheet thinning in the Amundsen Sea Embayment during the Late Holocene, The Cryosphere, 17, 1787–1801, https://doi.org/10.5194/tc-17-1787-2023, 2023. 
Balestra, B., Grunert, P., Ausin, B., Hodell, D., Flores, J.-A., Alvarez-Zarikian, C. A., Hernandez-Molina, F. J., Stow, D., Piller, W. E., and Paytan, A.: Coccolithophore and benthic foraminifera distribution patterns in the Gulf of Cadiz and Western Iberian Margin during Integrated Ocean Drilling Program (IODP) Expedition 339, J. Marine Syst., 170, 50–67, https://doi.org/10.1016/j.jmarsys.2017.01.005, 2017. 
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Short summary
Thwaites Glacier's retreat is driven by warm ocean water melting its ice shelf. Seafloor-dwelling marine protists, benthic foraminifera, reflect their environment. Here, ice margins, oceanography, and sea ice cover control live foraminiferal populations. Including dead foraminifera in the analyses shows the calcareous test preservation's role in the assemblage make-up. Understanding these modern communities helps interpret past glacial retreat controls through foraminifera in sediment records.

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