8 research outputs found
Mid- to late Cretaceous microbiostratigraphy, paleo-ecology and paleogeography of the Sergipe Basin, north eastern Brazil
2 volsAvailable from British Library Document Supply Centre- DSC:DX89285 / BLDSC - British Library Document Supply CentreSIGLEGBUnited Kingdo
Palaeoenvironmental turnover across the Palaeocene/Eocene boundary at the Stratotype section in Dababiya (Egypt) based on benthic foraminifera
The Maastrichtian‐Danian in the SW Zagros Fold‐Thrust Belt (S. Iran): An Integration of Planktonic Foraminiferal Biostratigraphy and Gamma‐Ray Spectrometry
Near-K/T age of clastic deposits from Texas to Brazil: impact, volcanism and/or sea-level lowstand?
Chemostratigraphy Across the Cretaceous-Paleogene (K-Pg) Boundary:Testing the Impact and Volcanism Hypotheses
Trochammina
The ecostratigraphic analysis of foraminiferal assemblages from Upper Pliensbachian to Lower Toarcian (Lower Jurassic) mudstones, siltstones and black shales from northern Siberia allows for a better understanding of the response to the benthic biotic crisis related to the Toarcian Oceanic Anoxic Event in a high latitude context. The assemblages were dominated by agglutinated taxa with extremely low diversity values and dominance of Trochammina. These features suggest that the foraminiferal assemblages were adapted to restricted conditions, where the main limiting factors were salinity and oxygen degree. The opportunist behaviour of Trochammina enabled this genus to survive and adapt to unfavourable conditions. Trochammina proliferated in relation to the sea-level fall and probable changes in salinity in the Arctic palaeobasin during the Margaritatus Chron and at the beginning of the Viligaensis Chron (Late Pliensbachian). Another Trochammina proliferation is associated with the initial development of the restricted oxygen conditions related to the Toarcian Oceanic Anoxic Event