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The geological record of ocean acidification
Ocean acidification may have severe consequences for marine ecosystems; however,
assessing its future impact is difficult because laboratory experiments and field observations …
assessing its future impact is difficult because laboratory experiments and field observations …
The Paleocene-Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future
During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of
petagrams of carbon were released into the ocean-atmosphere system with attendant …
petagrams of carbon were released into the ocean-atmosphere system with attendant …
[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
Abstract The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal,~ 56 million years
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
On the duration of the Paleocene‐Eocene thermal maximum (PETM)
The Paleocene‐Eocene thermal maximum (PETM) is one of the best known examples of a
transient climate perturbation, associated with a brief, but intense, interval of global warming …
transient climate perturbation, associated with a brief, but intense, interval of global warming …
Extreme warming of mid-latitude coastal ocean during the Paleocene-Eocene Thermal Maximum: Inferences from TEX86 and isotope data
Abstract Changes in sea surface temperature (SST) during the Paleocene-Eocene Thermal
Maximum (PETM) have been estimated primarily from oxygen isotope and Mg/Ca records …
Maximum (PETM) have been estimated primarily from oxygen isotope and Mg/Ca records …
Marine ecosystem responses to Cenozoic global change
The future impacts of anthropogenic global change on marine ecosystems are highly
uncertain, but insights can be gained from past intervals of high atmospheric carbon dioxide …
uncertain, but insights can be gained from past intervals of high atmospheric carbon dioxide …
Late Paleocene–early Eocene Tethyan carbonate platform evolution—a response to long-and short-term paleoclimatic change
C Scheibner, RP Speijer - Earth-science reviews, 2008 - Elsevier
The early Paleogene experienced the most pronounced long-term warming trend of the
Cenozoic, superimposed by transient warming events such as the Paleocene–Eocene …
Cenozoic, superimposed by transient warming events such as the Paleocene–Eocene …
The Palaeocene–Eocene Thermal Maximum super greenhouse: biotic and geochemical signatures, age models and mechanisms of global change
Abstract The Palaeocene–Eocene Thermal Maximum (PETM), a geologically brief episode
of global warming associated with the Palaeocene–Eocene boundary, has been studied …
of global warming associated with the Palaeocene–Eocene boundary, has been studied …
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 …
Eustatic variations during the Paleocene‐Eocene greenhouse world
We reconstruct eustatic variations during the latest Paleocene and earliest Eocene (∼ 58–
52 Ma). Dinoflagellate cysts, grain size fractions, and organic biomarkers in marine sections …
52 Ma). Dinoflagellate cysts, grain size fractions, and organic biomarkers in marine sections …