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Paleoceanographic reconstructions of the South-Western Atlantic for the Middle and Late Pleistocene based on benthic foraminifer assemblages

Abstract

Benthic foraminiferal assemblages were investigated in the sediment core AI-3321 (30°56.85’ S, 38°02.45’ W, 2969 m water depth, 293 cm length), retrieved from the western slope of the Rio Grande Rise in the western South Atlantic. Six intervals reflecting the changes in relative abundance of indicative species during the last three glacial-interglacial cycles are defined based on cluster analysis. Intervals VI and I are characterized by the dominance of Globocassidulina subglobosa, which indicates well-aerated conditions and enhanced hydrodynamic activity of the deep water bathing the seafloor. The high relative abundance of Epistominella exigua points to stressful conditions for benthic foraminiferal faunas with variable (pulsed) food supply to the bottom during Intervals V and III. Slight enhancement of sea surface bioproductivity is proposed for Intervals IV and II based on the high percentages of Alabaminella weddellensis.

About the Authors

L. A. Kuleshova
Shirshov Institute of Oceanology, Russian Academy of Sciences; I. Kant Baltic University
Russian Federation

Junior Research Fellow ShIO; master student I. Kant BU



E. A. Ovsepyan
Shirshov Institute of Oceanology, Russian Academy of Sciences
Russian Federation

Research Scientist, Ph.D. in Geology



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Review

For citations:


Kuleshova L.A., Ovsepyan E.A. Paleoceanographic reconstructions of the South-Western Atlantic for the Middle and Late Pleistocene based on benthic foraminifer assemblages. Vestnik Moskovskogo universiteta. Seriya 5, Geografiya. 2019;(3):72-82. (In Russ.)

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