Global warming, widespread oceanic anoxia and stagnation, and large perturbations of the global carbon cycle characterized the end-Permian to Middle Triassic interval. Nitrogen …
The marine calcium (Ca) cycle is controlled by rates of continental weathering, seawater pH, and carbonate deposition on the seafloor and is linked to atmospheric CO 2, climate …
Ammonoids are key fossil indexes for Triassic biochronology, as all Triassic stages and substages were initially defined on ammonoid faunas. In recent decades, the temporal …
Both the duration and severity of deep-water anoxic conditions across the Permian-Triassic mass extinction (PTME) are controversial. Panthalassa Ocean circulation models yield …
Y Du, H Song, J Tong, TJ Algeo, Z Li, H Song… - …, 2021 - pubs.geoscienceworld.org
The recovery of marine ecosystems in the aftermath of the Permian-Triassic mass extinction was accompanied by significant carbon-cycle perturbations, as reflected in large-amplitude …
Abstract The Cryogenian Angepena Formation (ca. 650 Ma) of South Australia records deposition in a peritidal environment equivalent to, and landward of the Balcanoona reef …
Marine sediments featuring special colors have always played an important role in disclosing regional or global environmental transitions and geological evolution. A deep …
The extinction of most heavy calcifiers, such as corals, calcareous algae and sponges, during the Permian-Triassic mass extinction (PTME) coincides with the sudden transition …
Marine red beds (MRBs), also known as oceanic red beds (ORBs), are reddish colored sediments deposited within the marine realm that have been stained during deposition …