Tempo and scale of late Paleocene and early Eocene carbon isotope cycles: Implications for the origin of hyperthermals
The upper Paleocene and lower Eocene are marked by several prominent (> 1‰) carbon
isotope (δ13C) excursions (CIE) that coincide with transient global warmings, or thermal …
isotope (δ13C) excursions (CIE) that coincide with transient global warmings, or thermal …
Assessing offsets between the δ13C of sedimentary components and the global exogenic carbon pool across early Paleogene carbon cycle perturbations
A Sluijs, GR Dickens - Global Biogeochemical Cycles, 2012 - Wiley Online Library
Negative stable carbon isotope excursions (CIEs) across the Paleocene–Eocene thermal
maximum (PETM;∼ 56 Ma) range between 2‰ and 7‰, even after discounting sections …
maximum (PETM;∼ 56 Ma) range between 2‰ and 7‰, even after discounting sections …
Frequency, magnitude and character of hyperthermal events at the onset of the Early Eocene Climatic Optimum
Recent studies have shown that the Early Eocene Climatic Optimum (EECO) was preceded
by a series of short-lived global warming events, known as hyperthermals. Here we present …
by a series of short-lived global warming events, known as hyperthermals. Here we present …
Orbital climate forcing of δ13C excursions in the late Paleocene–early Eocene (chrons C24n–C25n)
High‐resolution stable carbon isotope records for upper Paleocene–lower Eocene sections
at Ocean Drilling Program Sites 1051 and 690 and Deep Sea Drilling Project Sites 550 and …
at Ocean Drilling Program Sites 1051 and 690 and Deep Sea Drilling Project Sites 550 and …
Persistence of carbon release events through the peak of early Eocene global warmth
Abstract The Early Eocene Climatic Optimum (53–50 million years ago) was preceded by
approximately six million years of progressive global warming. This warming was …
approximately six million years of progressive global warming. This warming was …
A high-resolution benthic stable-isotope record for the South Atlantic: Implications for orbital-scale changes in Late Paleocene–Early Eocene climate and carbon …
Abstract The Late Paleocene and Early Eocene were characterized by warm greenhouse
climates, punctuated by a series of rapid warming and ocean acidification events known as …
climates, punctuated by a series of rapid warming and ocean acidification events known as …
Terrestrial carbon isotope excursions and biotic change during Palaeogene hyperthermals
Pronounced transient global warming events between 60 and 50 million years ago have
been linked to rapid injection of isotopically-light carbon to the ocean–atmosphere system,. It …
been linked to rapid injection of isotopically-light carbon to the ocean–atmosphere system,. It …
North American continental margin records of the Paleocene‐Eocene thermal maximum: Implications for global carbon and hydrological cycling
The impacts of the Paleocene‐Eocene thermal maximum (PETM)(∼ 55 Ma), one of the most
rapid and extreme warming events in Earth history, are well characterized in open marine …
rapid and extreme warming events in Earth history, are well characterized in open marine …
Global extent of early Eocene hyperthermal events: A new Pacific benthic foraminiferal isotope record from Shatsky Rise (ODP Site 1209)
T Westerhold, U Röhl, B Donner… - Paleoceanography and …, 2018 - Wiley Online Library
Studying the dynamics of past global warming events during the late Paleocene to middle
Eocene informs our understanding of Earth's carbon cycle behavior under elevated …
Eocene informs our understanding of Earth's carbon cycle behavior under elevated …
Evidence for a rapid release of carbon at the Paleocene-Eocene thermal maximum
JD Wright, MF Schaller - Proceedings of the National …, 2013 - National Acad Sciences
The Paleocene/Eocene thermal maximum (PETM) and associated carbon isotope excursion
(CIE) are often touted as the best geologic analog for the current anthropogenic rise in …
(CIE) are often touted as the best geologic analog for the current anthropogenic rise in …
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- late paleocene early eocene
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- late paleocene δ13c excursions
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- late paleocene orbital climate
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