How Unusual Was the Paleocene‐Eocene Thermal Maximum?
Abstract The Paleocene‐Eocene Thermal Maximum (PETM) was an extreme fluctuation of Earth's climate and a potential analog for future unmitigated anthropogenic climate change, but whose cause is debated. We show that fluctuations in Cenozoic benthic foraminiferal δ13 ${\delta }^{13}$C and δ18 ${\delta }^{18}$O follow a Laplace distribution. We present a
B. B. Cael, G. L. Foster
wiley +1 more source
Oligocene deep ocean oxygen isotope variations primarily driven by temperature. [PDF]
Boscolo-Galazzo F +9 more
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Abstract The existence of missing geomagnetic reversals has been proposed, with potential for new magnetostratigraphic age controls. We estimate geomagnetic reversal frequency from 0 to 155 Ma using adaptive‐bandwidth kernel density estimation (AKDE) to evaluate data sparseness and to assess how reversal frequency changes when recently identified ...
Yutaka Yoshimura +10 more
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Eccentricity rhythms in the Oligocene-Miocene carbon cycle regulated by weathering and carbonate burial. [PDF]
Liu F +6 more
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From trace to trace maker: Oligocene-Miocene coprolites of southern Poland and their potential producers. [PDF]
Brachaniec T +8 more
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Life history of a new Paraceratheriid from the Early Oligocene of Northwest China. [PDF]
Lu X, Deng T.
europepmc +1 more source
24 million years of pollination interaction between European linden flowers and bumble bees. [PDF]
Geier C +9 more
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Paleodistribution of Cercidiphyllaceae and Future Habitat Prediction for <i>Cercidiphyllum japonicum</i> Under Climate Change. [PDF]
Mao P +6 more
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The importance of past rifting in large igneous province development. [PDF]
Kounoudis R +7 more
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