Evaluating basinal and global repercussions of the initial rise of oxygen via geochemical constraints from the Paleoproterozoic Onega Basin, Fennoscandian Shield

Athena Eyster1, Michael J Tappa1, Sheila Abdul Rashid2, Aivo Lepland3, Alan D. Rooney4 and Ann Bauer1, (1)University of Wisconsin Madison, Department of Geoscience, Madison, United States, (2)The National University of Malaysia, Bangi, Malaysia, (3)Geological Survey of Norway, Trondheim, Norway, (4)Yale University, Department of Earth and Planetary Sciences, New Haven, CT, United States
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