Articles | Volume 20, issue 1
https://doi.org/10.5194/bg-20-121-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-20-121-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Jan 2023
Research article |
| 09 Jan 2023
| 09 Jan 2023
Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion
Adam Woodhouse
CORRESPONDING AUTHOR
School of Earth and Environment, University of Leeds, Leeds, LS2 9JT,
UK
University of Texas Institute for Geophysics, University of Texas at
Austin, Austin, TX, 78758, USA
Frances A. Procter
School of Earth and Environment, University of Leeds, Leeds, LS2 9JT,
UK
Sophie L. Jackson
School of Earth and Environment, University of Leeds, Leeds, LS2 9JT,
UK
Robert A. Jamieson
School of Earth and Environment, University of Leeds, Leeds, LS2 9JT,
UK
Robert J. Newton
School of Earth and Environment, University of Leeds, Leeds, LS2 9JT,
UK
Philip F. Sexton
School of Environment, Earth and Ecosystem Sciences, Open University,
Walton Hall, Kents Hill, Milton Keynes, MK7 6AA, UK
Tracy Aze
School of Earth and Environment, University of Leeds, Leeds, LS2 9JT,
UK
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Short summary
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This study uses novel techniques to look at the microstructure of planktonic foraminifera (single-celled marine organisms) fossils, to further our understanding of how they form their hard exterior shells and how the microstructure and chemistry of these shells can change as a result of processes that occur after deposition on the seafloor. Understanding these processes is of critical importance for using planktonic foraminifera for robust climate and environmental reconstructions of the past.
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Short summary
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Short summary
This study looked into the regional and global response of planktonic foraminifera to the climate over the last 5 million years, when the Earth cooled significantly. These single celled organisms exhibit the best fossil record available to science. We document an abundance switch from warm water to cold water species as the Earth cooled. Moreover, a closer analysis of certain species may indicate higher fossil diversity than previously thought, which has implications for evolutionary studies.
This study looked into the regional and global response of planktonic foraminifera to the...
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