Abstract Mercury (Hg) concentrations and Hg isotopes have been widely used to fingerprint geological volcanism. Mercury content, as a more accessible proxy, is more frequently used …
The Paleocene-Eocene Thermal Maximum (PETM) is recognized by a major negative carbon isotope (δ13C) excursion (CIE) signifying an injection of isotopically light carbon into …
P Xue, L Chang, E Thomas - Earth and Planetary Science Letters, 2023 - Elsevier
Reconstruction of oceanic redox conditions across the Palaeocene-Eocene Thermal Maximum (PETM,∼ 55.93 Ma) provides crucial information on potential PETM triggers and …
Abstract The Paleocene-Eocene Thermal Maximum (PETM;∼ 55.9 Ma) was a hyperthermal event associated with large carbon cycle perturbations, sustained global warming, and …
Among the predicted responses to ongoing climate warming is that coastal and inland areas may experience increasingly extreme weather, with potentially more droughts and floods …
Sedimentation on river floodplains is a complex process that involves overbank flooding, crevasse splaying, and river avulsion. The resulting floodplain stratigraphy often exhibits …
Paleocene-Eocene sedimentary archives record a series of global warming events called hyperthermals. These events occurred across a long-term increasing temperature trend and …
Abstract The Paleocene–Eocene thermal maximum (PETM;∼ 56 Ma) was a transient global warming event associated with a huge perturbation to the global carbon cycle. Changes in …
Early Eocene climates were globally warm, with ice-free conditions at both poles. Early Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate …