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Nature|April 28, 2012
Deposition of 1.88-billion-year-old iron formations as a consequence of rapid crustal growthBirger Rasmussen, Ian R Fletcher, Andrey Bekker, et al.Proceedings of the National Academy of Sciences of the United States of America|January 6, 2025
Reconciling Archean organic-rich mudrocks with low primary productivity before the Great Oxygenation EventNoam Lotem, Birger Rasmussen, Jian-Wei Zi, et al.Science Advances|January 5, 2022
Reexamination of 2.5-Ga "whiff" of oxygen interval points to anoxic ocean before GOESarah P Slotznick, Jena E Johnson, Birger Rasmussen, et al.Science Advances|April 7, 2023
Response to comment on "Reexamination of 2.5-Ga 'whiff' of oxygen interval points to anoxic ocean before GOE"Sarah P Slotznick, Jena E Johnson, Birger Rasmussen, et al.Proceedings of the National Academy of Sciences of the United States of America|November 2, 2022
Oceanic nutrient rise and the late Miocene inception of Pacific oxygen-deficient zonesXingchen Tony Wang, Yuwei Wang, Alexandra Auderset, et al.Pageof 2