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 caused by continental weathering and influxes during the late Devonian Frasnian-Famennian bio-crisis and Annulata bio …
Oceanic anoxia is regarded as the major cause of the Late Devonian Frasnian–Famennian
(Fsingle bondF) bio-crisis and Annulata bio-event, and it is associated with continental …
(Fsingle bondF) bio-crisis and Annulata bio-event, and it is associated with continental …
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 …