Abstract

[Pufahl et al. (2010)][1] question the interpretation of data in [Poulton et al. (2004)][2], showing a transition from ferruginous to euxinic conditions on the continental shelf of a major ocean basin at ca. 1840 Ma. In contrast with [Poulton et al. (2004)][2] and also [Johnston et al. (2006)][3],

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.