Abstract All of the Big Five mass extinctions (BFMEs) of the Phanerozoic are postulated to
have been associated with eruptions of large igneous provinces (LIPs), although the role of …

Mercury (Hg) enrichments in ancient sediments have been used as a proxy of volcanism,
especially large igneous province (LIP) eruptions. However, considering the existence of …

This study investigates the mechanisms underlying the varied climate changes witnessed
during mass extinctions in the Phanerozoic Eon. Climate shifts during mass extinctions have …

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

Abstract The late Cretaceous-Danian (K-Pg) organic-rich sequence is a global archive that
witnessed abrupt paleo-condition changes during a high sea-level. In Egypt, this sequence …

An interglacial period existed between the Sturtian (ca. 720∼ 660 Ma) and the Marinoan
glacial period (ca. 650∼ 635 Ma) in the Cryogenian. It is manifested as the Mn-bearing …

Abstract The Late Permian was marked by a series of important geological events and
widespread organic‐rich black shale depositions, acting as important unconventional …

The Cretaceous provides us with an excellent case history of ocean-climate-biota system
perturbations. Such perturbations occurred several times during the Cretaceous, such as …

The geochemical record of the early Aptian and the transition to the Albian exposes the
presence of Hg/TOC anomalies, revealing the interference of LIPs in paleoenvironmental …

Abstract We find that Large Igneous Province (LIP) volcanism, mostly continental flood
basalts (CFBs), along with the largest extraterrestrial impacts show significant correlations …