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

نویسندگان

چکیده

Abstract. The Pliocene-Recent is associated with many important climatic and paleoceanographic changes, which have shaped the biotic abiotic nature of modern world. closure Central American Seaway development intensification Northern Hemisphere ice sheets had profound global impacts on latitudinal vertical structure oceans, triggering extinction radiation marine groups. In particular, calcifying planktonic foraminifera, are highly sensitive to water column structure, exhibited a series extinctions as temperatures fell. By analyzing high-resolution (∼ 5 kyr) sedimentary records from Eastern Equatorial Pacific Ocean, complemented novel Triton dataset, we document changes in this microfossil group, within three species displayed isochronous co-extinction, cold-water affinity increased dominance meridional temperature gradients steepened. We suggest that these were terminal stages Seaway, where following sustained warmth mid-Pliocene Warm Period, bipolar sheet expansion initiated world cold- deep-dwelling became increasingly more successful. Such global-scale paleoecological macroevolutionary variations between Pliocene icehouse climate would significant deviations pre-industrial baselines future plankton communities anthropogenic forcing continues.

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ژورنال

عنوان ژورنال: Biogeosciences

سال: 2023

ISSN: ['1726-4189', '1726-4170']

DOI: https://doi.org/10.5194/bg-20-121-2023