Evidence for a gradual rise of oxygen between 2.6 and 2.5 Ga from Mo isotopes and Re-PGE signatures in shales

Wille, M.; Kramers, J. D.; Nägler, T. F.; Beukes, N. J.; Schröder, S.; Meisel, Th.; Lacassie, J. P.; Voegelin, A. R. (2007). Evidence for a gradual rise of oxygen between 2.6 and 2.5 Ga from Mo isotopes and Re-PGE signatures in shales. Geochimica et cosmochimica acta, 71(10), pp. 2417-2434. New York, N.Y.: Elsevier Science 10.1016/j.gca.2007.02.019

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Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Institute of Geological Sciences

UniBE Contributor:

Wille, Martin Hermann, Kramers, Jan Dirk, Nägler, Frank Thomas, Vögelin, Andrea

Subjects:

500 Science > 550 Earth sciences & geology

ISSN:

0016-7037

Publisher:

Elsevier Science

Language:

English

Submitter:

Frank Thomas Nägler

Date Deposited:

04 Oct 2013 15:00

Last Modified:

02 Mar 2023 23:22

Publisher DOI:

10.1016/j.gca.2007.02.019

Web of Science ID:

000246699600001

BORIS DOI:

10.48350/25911

URI:

https://boris.unibe.ch/id/eprint/25911 (FactScience: 62271)

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