Warm tropical sea surface temperatures in the Late Cretaceous and Eocene epochs
By P. Pearson, P. Ditchfield, J. Singano, Katherine G. Harcourt-Brown, C. Nicholas, R. Olsson, N. Shackleton, M. Hall. Nature, 2001
746 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geology, Paleontology
View Paper: https://www.semanticscholar.org/paper/530519baaadc73759308273f2e18097fb5b8990d
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Citations in the corpus
- Planktonic foraminiferal response to the latest Maastrichtian abrupt warm event: a case study from South Atlantic DSDP Site 525A (2003, background): “Oxygen isotopes and paleotemperatures At DSDP Site 525A, planktonic foraminifera are well preserved (Plate I), but presence of secondary calcite growths within shells indicates bottom deep-sea diagenesis (Pearson et al., 2001).”
- Oligocene climate dynamics (2004, background): “This includes the ambient isotopic composition of seawater (dOsw) in which the foraminiferal calcite was precipitated (which is influenced by salinity and global ice volume), diagenetic modification [Schrag et al., 1992, 1995; Pearson et al., 2001], and the concentration of seawater carbonate”
- Possible atmospheric CO2 extremes of the Middle Cretaceous (late Albian-Turonian) (2002, background): “For low latitude planktonic foraminifera, addition of diagenetic calcite in equilibrium with either bottom water or shallow pore waters results in an increase in carbonate d18O and artificially low temperature estimates [Milliman, 1966; Schrag et al., 1995; Pearson et al., 2001].”
- Evolutionary radiation of the Jehol Biota: chronological and ecological perspectives (2006, background): “…volcanic eruptions (Ingle and Coffin 2004), increase of atmospheric CO2 and the greenhouse climate in the middle Cretaceous (Larson and Erba 1999; Wilson and Norris 2001; Pearson et al. 2001) and the Cretaceous Normal Superchron (CNS) that lasted for about 37Ma (120–83Ma, Gradstein et al. 1995).”