C Corradini, C Henderson, JE Barrick… - Newsletters on …, 2024 - iris.unimore.it
Conodonts are tooth-like elements of a primitive chordate and are generally abundant in many marine sedimentary rocks deposited from the late Cambrian to the latest Triassic. For …
M Leu, E Schneebeli-Hermann, Ø Hammer… - Lethaia, 2024 - idunn.no
The Smithian–Spathian transition (~ 249.2 Ma) is marked by profound environmental changes, carbon cycle perturbations, and the stepwise loss of nektonic biodiversity …
Anomalous mercury (Hg) contents recorded near the Permian‐Triassic boundary (PTB) are often linked to Siberian Traps Large Igneous Province (STLIP) volcanism and the Permian …
S Zhang, D Yuan, S Shen - Palaeogeography, Palaeoclimatology …, 2024 - Elsevier
Abstract The Guadalupian–Lopingian boundary (GLB) interval contains global-scale changes in biota and environment. The establishment of a uniform time scale and a robust …
Some 2.7 myr after the Permian–Triassic boundary mass extinction, a stepwise extinction of the nekton (ammonoids and conodonts) ended at the Smithian–Spathian boundary (SSB) …
Mercury (Hg) enrichment recorded in Smithian to Spathian (Olenekian) marine sedimentary successions has been used to link putative renewed Siberian Traps Large Igneous Province …
Vertebrate and invertebrate fossils from the Smithian (Early Triassic) to the Early-Middle Triassic boundary interval of Svalbard, Arctic Norway have been known for a long time, but …
Conodonts are for the first time described from the Grippia bonebed, lower part of the Vendomdalen Member, Vikinghøgda Formation, central Spitsbergen, Svalbard. They are …
Following the largest mass extinction of the Phanerozoic, the Early Triassic was characterized by a series of carbon cycle perturbations as revealed through multiple global …