Extreme global warmth and an abrupt negative carbon isotope excursion during the
Paleocene–Eocene Thermal Maximum (PETM) have been attributed to a massive release of …

The late Paleocene thermal maximum (LPTM) is associated with a brief, but intense, interval
of global warming and a massive perturbation of the global carbon cycle. We have …

Enormous amounts of 13 C-depleted carbon rapidly entered the exogenic carbon cycle
during the onset of the Paleocene-Eocene thermal maximum (PETM), as attested to by a …

The massive perturbation to global climate and the carbon cycle during the
Paleocene/Eocene Thermal Maximum (PETM)(approx. 55.5 Ma) may have been forced by a …

Much of the North Atlantic region experienced hundreds of metres of transient uplift during
the latest Paleocene. Regional uplift should cause dissociation of gas hydrates stored in …

Dramatic warming and upheaval of the carbon system at the end of the Paleocene Epoch
have been linked to massive dissociation of sedimentary methane hydrate. However, testing …

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 …

A continuous age model for the brief climate excursion at the Paleocene–Eocene boundary
has been constructed by assuming a constant flux of extraterrestrial 3He (3HeET) to the …

Isotopic records across the “Latest Paleocene Thermal Maximum “(LPTM) indicate that
bottom water temperature increased by more than 4° C during a brief time interval (< 104 …

During the Paleocene‐Eocene Thermal Maximum (PETM,∼ 55 Ma), marine and terrestrial
carbon isotope values exhibit a negative shift of at least 2.5‰, indicative of massive …