Response of Antarctic (ODP Site 690) planktonic foraminifera to the Paleocene–Eocene thermal maximum: Faunal evidence for ocean/climate change
- 28 December 2002
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 17 (4) , 23-1-23-13
- https://doi.org/10.1029/2002pa000761
Abstract
No abstract availableKeywords
This publication has 54 references indexed in Scilit:
- Evidence of surface water oligotrophy during the Paleocene‐Eocene thermal maximum: Nannofossil assemblage data from Ocean Drilling Program Site 690, Maud Rise, Weddell SeaPaleoceanography and Paleoclimatology, 2002
- Termination of global warmth at the Palaeocene/Eocene boundary through productivity feedbackNature, 2000
- Increased terrestrial carbon storage across the Palaeocene–Eocene boundaryPalaeogeography, Palaeoclimatology, Palaeoecology, 2000
- Mechanisms of Climate Warming at the End of the PaleoceneScience, 1999
- High-resolution records of the late Paleocene thermal maximum and circum-Caribbean volcanism: Is there a causal link?Geology, 1997
- Late Paleocene to Eocene paleoceanography of the equatorial Pacific Ocean: Stable isotopes recorded at Ocean Drilling Program Site 865, Allison GuyotPaleoceanography and Paleoclimatology, 1995
- Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentrationNature, 1994
- Atlantic Eocene planktonic foraminiferal paleohydrographic indicators and stable isotope paleoceanographyPaleoceanography and Paleoclimatology, 1987
- Paleocene Planktonic Foraminiferal Biogeography and the Paleooceanography of the Atlantic OceanMicropaleontology, 1983
- Carbon Dioxide Excursions and the Deep-Sea Record: Aspects of the ProblemPublished by Springer Nature ,1977