Strategies in times of crisis-insights into the benthic foraminiferal record of the Palaeocene-Eocene Thermal Maximum.

• Main Authors: Schmidt, Daniela N, Thomas, Ellen, Authier, Elisabeth, Saunders, David, Ridgwell, Andy
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2018
• Subjects: Imaging; Three-Dimensional; Ecosystem; Temperature; Population Density; Time Factors; Extinction; Biological; X-Ray Microtomography; Geological Phenomena; Foraminifera; Climate Change; Palaeocene–Eocene Thermal Maximum; benthic foraminifers; development; ocean drilling programme; µ-computed tomography; Palaeocene-Eocene; Thermal Maximum; mu-computed tomography; General Science & Technology; Indian; Pacific; Southern Ocean
• Online Access: https://escholarship.org/uc/item/6zn9r227

Climate change is predicted to alter temperature, carbonate chemistry and oxygen availability in the oceans, which will affect individuals, populations and ecosystems. We use the fossil record of benthic foraminifers to assess developmental impacts in response to environmental changes during the Palaeocene-Eocene Thermal Maximum (PETM). Using an unprecedented number of µ-computed tomography scans, we determine the size of the proloculus (first chamber), the number of chambers and the final size of two benthic foraminiferal species which survived the extinction at sites 690 (Atlantic sector, Southern Ocean, palaeodepth 1900 m), 1210 (central equatorial Pacific, palaeodepth 2100 m) and 1135 (Indian Ocean sector, Southern Ocean, palaeodepth 600-1000 m). The population at the shallowest site, 1135, does not show a clear response to the PETM, whereas those at the other sites record reductions in diameter or proloculus size. Temperature was similar at all sites, thus it is not likely to be the reason for differences between sites. At site 1210, small size coincided with higher chamber numbers during the peak event, and may have been caused by a combination of low carbonate ion concentrations and low food supply. Dwarfing at site 690 occurred at lower chamber numbers, and may have been caused by decreasing carbonate saturation at sufficient food levels to reproduce. Proloculus size varied strongly between sites and through time, suggesting a large influence of environment on both microspheric and megalospheric forms without clear bimodality. The effect of the environmental changes during the PETM was more pronounced at deeper sites, possibly implicating carbonate saturation.This article is part of a discussion meeting issue 'Hyperthermals: rapid and extreme global warming in our geological past'.