Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion

Abstract ∼  5 kyr) sedimentary records from the Eastern Equatorial Pacific Ocean, complemented with global records from the novel Triton dataset, we document the biotic changes in this microfossil group, within which three species displayed isochronous co-extinction, and species with cold-water affinity increased in dominance as meridional temperature gradients steepened. We suggest that these changes were associated with the terminal stages of the closure of the Central American Seaway, where following the sustained warmth of the mid-Pliocene Warm Period, bipolar ice sheet expansion initiated a world in which cold- and deep-dwelling species became increasingly more successful. Such global-scale paleoecological and macroevolutionary variations between the Pliocene and the modern icehouse climate would suggest significant deviations from pre-industrial baselines within modern and future marine plankton communities as anthropogenic climate forcing continues.

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion ; volume:20 ; number:1 ; year:2023 ; pages:121-139 ; extent:19
Biogeosciences ; 20, Heft 1 (2023), 121-139 (gesamt 19)

Urheber
Woodhouse, Adam
Procter, Frances A.
Jackson, Sophie L.
Jamieson, Robert A.
Newton, Robert J.
Sexton, Philip F.
Aze, Tracy

DOI
10.5194/bg-20-121-2023
URN
urn:nbn:de:101:1-2023011204241952409163
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
15.08.2025, 07:32 MESZ

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Beteiligte

  • Woodhouse, Adam
  • Procter, Frances A.
  • Jackson, Sophie L.
  • Jamieson, Robert A.
  • Newton, Robert J.
  • Sexton, Philip F.
  • Aze, Tracy

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