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

The Aptian was characterized by dramatic tectonic, oceanographic, climatic and biotic
changes and its record is punctuated by Oceanic Anoxic Events (OAEs). The timing and …

Large igneous province (LIP) volcanism has been proposed as a key trigger of several
major climate and environmental perturbations during the Phanerozoic Aeon. Large-scale …

Abstract The Aptian–Albian boundary is marked by one of the major oceanic perturbations
during the Cretaceous, called Oceanic Anoxic Event (OAE) 1b. Extensive volcanic episodes …

Abstract While the Cretaceous Normal Polarity Superchron has documented instances of
brief reversed polarity intervals, the absence of accurate age determinations for such abrupt …

Abstract The upper Aptian-lower Albian stratigraphic interval documents important
perturbations in the carbon cycle associated with the Oceanic Anoxic Event 1b (OAE 1b) …

An integrated study of multiple geochemical proxies (δ 13 C carb, δ 13 C org, TOC, HI,
CaCO 3, trace elements/Al ratios) of the late Aptian–early Albian oceanic anoxic event …

The early to mid-Aptian was punctuated by episodic phases of organic-carbon burial in
various oceanographic settings, which are possibly related to massive volcanism associated …

Abstract The Barremian and Aptian were times of global plate reconfiguration and profound
changes in the ocean–climate system, culminating in the worldwide deposition of lower …

Abstract The Early Cretaceous Aptian–Albian boundary (AAB) interval (∼ 113 Ma) was
marked by severe environmental perturbations, including Oceanic Anoxic Event (OAE) 1b …