Rapid plate reorganization may have influenced global climate during the Eocene; however,
its linkage remains poorly constrained, particularly during the middle Eocene. To elucidate …

During the mid-Cretaceous, the Earth experienced several environmental perturbations,
including an extremely warm climate and Oceanic Anoxic Events (OAEs). Submarine …

The late Paleozoic ice age (LPIA) was the longest-lived glaciation of the Phanerozoic, and
the demise of LPIA is the Earth's only recorded transition from an icehouse to a greenhouse …

Abstract Multiple short-term (< 10 5 years) global warming events (“hyperthermals”) occurred
throughout the early Eocene. Chemical weathering of continental silicate rocks is …

Large igneous provinces (LIPs) are proposed to have caused a number of episodes of
abrupt environmental change by increasing atmospheric CO2 levels, which were …

The geologic time scale for the Cenozoic Era has been notably improved over the last
decades by virtue of integrated stratigraphy, combining high-resolution astrochronologies …

Abstract The Paleocene-Eocene Thermal Maximum (PETM,∼ 56 Ma) was a major
hyperthermal event that has been linked to CO 2 release from the North Atlantic Igneous …

Abstract The Miocene Climatic Optimum represents one of the major warming events during
the Cenozoic and was accompanied by a positive stable carbon isotope excursion. Here, we …

An ice-free greenhouse interval (ca. 660∼ 650 Ma) occurred between the global Sturtian
(ca. 717 Ma∼ 660 Ma) and Marinoan glaciation (ca. 650 Ma∼ 635 Ma) during the …

Abstract The Cretaceous Period was marked by the formation of numerous large igneous
provinces (LIPs), several of which were associated with geologically rapid climate …