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Coccolith dissolution versus productivity changes during the Plio-Pleistocene (3.14–1.80 MA) in the South Atlantic (ODP site 1090)

  • Published:2022-10 Issue: Volume:603 Page:111184
  • ISSN:0031-0182
  • Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
  • language:en
  • Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Ballegeer Anne-Marie,Flores José A.,Sierro Francisco J.,Rigual-Hernández Andrés S.

Funder

Ministerio de Educación, Cultura y Deporte

Ministerio de Ciencia e Innovación

Gobierno de España Ministerio de Ciencia e Innovación

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference119 articles.

1. Late Paleogene calcareous nannoplankton evolution: a tale of climatic deterioration;Aubry,1992

2. Quantitative biochronology of Pliocene and early Pleistocene calcareous nannofossils from the Atlantic, Indian and Pacific oceans;Backman;Mar. Micropaleontol.,1983

3. Monitoring fluctuations of the Subtropical Front in the Tasman Sea between 3.45 and 2.45 Ma (ODP site 1172);Ballegeer;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2012

4. Diatom constraints on the position of the Antarctic Polar Front in the middle part of the Pliocene;Barron;Mar. Micropaleontol.,1996

5. Final closure of Panama and the onset of northern hemisphere glaciation;Bartoli;Earth Planet. Sci. Lett.,2005

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