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H. C. Jenkyns | Semantic Scholar

Chemostratigraphy versus biostratigraphy: data from around the Cenomanian–Turonian boundary

A detailed isotopic profile is presented for a stratigraphically expanded Cenomanian–Turonian boundary section in Chalk facies exposed at Eastbourne, Sussex and compared with data from Pueblo,

Volume Index

Members Professor David B. Audretsch – Institute for Development Strategies, Indiana University, USA Professor Gordon Clark – School of Geography, University of Oxford, UK Professor Robert Dixon –

No evidence for a volcanic trigger for late Cambrian carbon-cycle perturbations

The early Paleozoic was marked by several carbon-cycle perturbations and associated carbon-isotope excursions (CIEs). Whether these CIEs are connected to significant (external) triggers, as is

Investigating the Behavior of Sedimentary Mercury (Hg) During Burial‐Related Thermal Maturation

Understanding the behavior of mercury (Hg) in organic‐rich sediments as they undergo thermal maturation is important, for example, because enrichment of Hg in sedimentary deposits has become a widely

Protracted carbon burial following the Early Jurassic Toarcian Oceanic Anoxic Event (Posidonia Shale, Lower Saxony Basin, Germany)

Lower Jurassic marine basins across the northwest European epicontinental shelf were commonly marked by deposition of organic-rich black shales. Organic-carbon burial was particularly widespread