Sea change in sediments

David J. Des Marais ()
Additional contact information
David J. Des Marais: Exobiology Branch and the NASA Astrobiology Institute, MS 239-4, NASA Ames Research Center

Nature, 2005, vol. 437, issue 7060, 826-827

Abstract: Earth's oxygen levels increased slowly over a long and ill-defined transitional period around two billion years ago. A microbial ‘footprint’ from this era provides biological evidence to complement existing geological data.

Date: 2005
References: Add references at CitEc
Citations:

Downloads: (external link)
https://www.nature.com/articles/437826b Abstract (text/html)
Access to the full text of the articles in this series is restricted.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:437:y:2005:i:7060:d:10.1038_437826b

Ordering information: This journal article can be ordered from
https://www.nature.com/

DOI: 10.1038/437826b

Access Statistics for this article

Nature is currently edited by Magdalena Skipper

More articles in Nature from Nature
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().