Abstract The Coniacian-Santonian (CS) was a time of differentiation in marine sedimentation, characterized by organic carbon (OC)-rich black shales and carbonates …
BT Huber, KG MacLeod, DK Watkins… - Global and Planetary …, 2018 - Elsevier
A compilation of foraminiferal stable isotope measurements from southern high latitude (SHL) deep-sea sites provides a novel perspective important for understanding Earth's …
ADC Du Vivier, D Selby, BB Sageman, I Jarvis… - Earth and Planetary …, 2014 - Elsevier
High-resolution osmium (Os) isotope stratigraphy across the Cenomanian–Turonian Boundary Interval from 6 sections for four transcontinental settings has produced a record of …
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 Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major palaeoceanographic phenomenon that took place during an interval of extreme global …
JD Scaife, M Ruhl, AJ Dickson… - Geochemistry …, 2017 - Wiley Online Library
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 …
Abstract The Cenomanian to Turonian boundary transition (ca. 95–93 Ma) represents one of the most profound global perturbations in the carbon cycle of the past 140 my This interval is …
Abstract Neodymium isotopic compositions (143 Nd/144 Nd or ε Nd) have been used as a tracer of water masses and lithogenic inputs to the ocean. To further evaluate the …
An analysis of orbitally influenced climate‐sensitive sedimentation is conducted across a meridional transect of the proto‐North Atlantic, to reconstruct the behavior of the carbon …