A Unitary Association-based Conodont Biozonation of the Smithian-Spathian Boundary (Early Triassic) and Associated Biotic Crisis from South China
Overview
Overview
Authors
Authors
Affiliations
Affiliations
Soon will be listed here.
Abstract
Supplementary Information: The online version contains supplementary material available at 10.1186/s13358-022-00259-x.
References
1.
Payne J, Lehrmann D, Wei J, Orchard M, Schrag D, Knoll A
. Large perturbations of the carbon cycle during recovery from the end-permian extinction. Science. 2004; 305(5683):506-9.
DOI: 10.1126/science.1097023.
View
2.
Stanley S
. Evidence from ammonoids and conodonts for multiple Early Triassic mass extinctions. Proc Natl Acad Sci U S A. 2009; 106(36):15264-7.
PMC: 2741239.
DOI: 10.1073/pnas.0907992106.
View
3.
Goudemand N, Romano C, Brayard A, Hochuli P, Bucher H
. Comment on "Lethally hot temperatures during the Early Triassic greenhouse". Science. 2013; 339(6123):1033.
DOI: 10.1126/science.1232924.
View
4.
Hochuli P, Sanson-Barrera A, Schneebeli-Hermann E, Bucher H
. Severest crisis overlooked-Worst disruption of terrestrial environments postdates the Permian-Triassic mass extinction. Sci Rep. 2016; 6:28372.
PMC: 4920029.
DOI: 10.1038/srep28372.
View
5.
Brayard A, Escarguel G, Bucher H, Monnet C, Bruhwiler T, Goudemand N
. Good genes and good luck: ammonoid diversity and the end-Permian mass extinction. Science. 2009; 325(5944):1118-21.
DOI: 10.1126/science.1174638.
View