Synchronizing rock clocks in the late Cambrian
The Cambrian is the most poorly dated period of the past 541 million years. Here, the authors present a new astronomical time scale, allowing for a first assessment, in numerical time, of the evolution of major biotic and abiotic changes that characterized the late Cambrian Earth.
Main Authors: | Zhengfu Zhao, Nicolas R. Thibault, Tais W. Dahl, Niels H. Schovsbo, Aske L. Sørensen, Christian M. Ø. Rasmussen, Arne T. Nielsen |
---|---|
Format: | Article |
Language: | English |
Published: |
Nature Portfolio
2022-04-01
|
Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-022-29651-4 |
Similar Items
-
Sedimentological studies in the late Precambrian and lower Cambrian rocks of east Finnmark
by: Banks, N
Published: (1971) -
No evidence for a volcanic trigger for late Cambrian carbon-cycle perturbations
by: Frieling, J, et al.
Published: (2023) -
Late pre-cambrian glaciation in Scotland /
by: 348525 Spencer, Anthony Mansell
Published: (1971) -
Geochemical characteristics of Cambrian bitumen and Cambrian-Ordovician source rocks in the Keping area, NW Tarim Basin
by: Shijing Xu, et al.
Published: (2023-12-01) -
Review of Survey activities 2010: Shale gas investigations in Denmark: Lower Palaozoic shales on Bornholm
by: Klitten, Kurt, et al.
Published: (2011-07-01)