Abstract

The strata of the Permotriassic Trappean Complex of Siberia (Ilimpeya River and Kapchan locality) are studied. The water-lava and water-tuff boundaries are shown to be promising for bacterial paleontological studies. The analysis of fossilized microbial communities shows that they vary depending on sedimentation conditions. This example is important for a better understanding of the prospects for the study of similar situations in the Archean and Proterozoic.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.