Cargando…
Different controls on the Hg spikes linked the two pulses of the Late Ordovician mass extinction in South China
The Late Ordovician mass extinction (LOME, ca. 445 Ma; Hirnantian stage) is the second most severe biological crisis of the entire Phanerozoic. The LOME has been subdivided into two pulses (intervals), at the beginning and the ending of the Hirnantian glaciation, the LOMEI-1 and LOMEI-2, respectivel...
Autores principales: | Qiu, Zhen, Wei, Hengye, Tian, Li, Corso, Jacopo Dal, Zhang, Jiaqiang, Zou, Caineng |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8956570/ https://www.ncbi.nlm.nih.gov/pubmed/35338189 http://dx.doi.org/10.1038/s41598-022-08941-3 |
Ejemplares similares
-
Phylogenetic Clustering of Origination and Extinction across the Late Ordovician Mass Extinction
por: Krug, Andrew Z., et al.
Publicado: (2015) -
Mercury spikes suggest volcanic driver of the Ordovician-Silurian mass extinction
por: Gong, Qing, et al.
Publicado: (2017) -
Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction
por: Kozik, Nevin P., et al.
Publicado: (2022) -
Large mass-independent sulphur isotope anomalies link stratospheric volcanism to the Late Ordovician mass extinction
por: Hu, Dongping, et al.
Publicado: (2020) -
Cascading trend of Early Paleozoic marine radiations paused by Late Ordovician extinctions
por: Rasmussen, Christian M. Ø., et al.
Publicado: (2019)