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Linking anoxia, biotic events, and basin evolution in the Late Devonian Illinois Basin, North America: A geochemical approach
Epeiric seas and their sedimentary deposits are vital for understanding the history of Earth's
oceans, but the lack of modern analogues and the frequent dominance of uniform mudrocks …
oceans, but the lack of modern analogues and the frequent dominance of uniform mudrocks …
Contrasting dynamics of marine bacterial-algal communities between the two main pulses of the Late Ordovician Mass Extinction
Understanding changes in bacterial-algal communities is vital for unraveling climato-
environmental factors linking ultimate triggers (eg, volcanic, bioevolutionary, and tectonic …
environmental factors linking ultimate triggers (eg, volcanic, bioevolutionary, and tectonic …
Oceanic euxinia and seafloor oxygenation linked to continental weathering and influxes during the Late Devonian Frasnian–Famennian bio-crisis and Annulata bio …
Oceanic anoxia is regarded as the immediate cause of the Late Devonian Frasnian–
Famennian (F–F) bio-crisis and Annulata bio-event. The oceanic anoxia has been linked to …
Famennian (F–F) bio-crisis and Annulata bio-event. The oceanic anoxia has been linked to …
Recognition of global carbon cycle perturbations in the Middle-Late Devonian New Albany Shale, south-central Indiana, USA: Deciphering local versus global …
Stable carbon isotope stratigraphy is an integral tool for identifying Devonian global events.
Carbon-cycle perturbations (excursions) tend to have geologically short durations that aid in …
Carbon-cycle perturbations (excursions) tend to have geologically short durations that aid in …