Abstract Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major
palaeoceanographic phenomenon that took place during an interval of extreme global …

Abstract Oceanic Anoxic Event 2 (OAE 2), during the Cenomanian‐Turonian transition (∼
94 Ma), was the largest perturbation of the global carbon cycle in the mid‐Cretaceous and …

Planktonic foraminiferal population dynamics and benthic foraminiferal and radiolaria
distributions combined with δ 13 C and δ 18 O measurements of both bulk carbonate and …

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

Abstract The Plenus Cold Event (PCE) temporarily interrupted the supergreenhouse
conditions exacerbated during much of the Cenomanian–Turonian Oceanic Anoxic Event 2 …

The greenhouse world of the mid‐Cretaceous (~ 94 Ma) was punctuated by an episode of
abrupt climatic upheaval: Oceanic Anoxic Event 2. High‐resolution climate records reveal …

Widespread deposition of organic-rich shales during the Late Cretaceous Oceanic Anoxic
Event 2 (OAE 2, ca. 94 Ma) occurred during a period of significant global paleo …

The Late Cretaceous Epoch was characterized by major global perturbations in the carbon
cycle, the most prominent occurring near the Cenomanian–Turonian (CT) transition marked …

The Toarcian Oceanic Anoxic Event (T-OAE, c. 182 Ma) represents a major perturbation of
the carbon cycle marked by widespread black shale deposition. Consequently, the onset of …

Abstract The Cenomanian–Turonian Oceanic Anoxic Event (OAE2;~ 94.5 million years ago)
represents an episode of global-scale marine anoxia and biotic turnover, which corresponds …