Mercury (Hg) is increasingly being used as a sedimentary tracer of Large Igneous Province (LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
Abstract The Cenomanian-Turonian Oceanic Anoxic Event 2 (OAE 2, ca. 94 Ma) is characterized by a marked positive carbon isotope excursion (CIE) recorded in global …
The middle Cretaceous was a period characterized by elevated sea-floor spreading rates, enhanced volcanism, high atmospheric CO 2 levels, warming temperatures, and the peak …
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 …
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 …
Abstract The latest Cenomanian to Santonian sedimentary record recovered at IODP Expedition 369 Site U1513 in the Mentelle Basin (SE Indian Ocean, paleolatitude 60° S at …
Earth history is punctuated by phases of extreme global stress of concurrent warming, ocean fertilisation and acidification that impacted biologic diversity and function. Under excess CO2 …
Abstract Paleoclimate during the Cenomanian-Turonian Oceanic Anoxic Event 2 (OAE 2, 94.5–93.9 Ma) was characterized by elevated atmospheric CO 2 concentrations and peak …