Ocean redox structure across the Late Neoproterozoic Oxygenation Event: A nitrogen isotope perspective

• Published in: Earth and Planetary Science Letters
• Main Authors: Ader, Magali, Sansjofre, Pierre, Halverson, Galen, Busigny, Vincent, Trindade, Ricardo I. F., Kunzmann, Marcus, Nogueira, Afonso C. R.
• Other Authors: Institut de Physique du Globe de Paris (IPGP), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS), Domaines Océaniques (LDO), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS), Instituto de Astronomia, Geofísica e Ciências Atmosféricas São Paulo (IAG), Universidade de São Paulo (USP), Department of Earth and Planetary Sciences/Geotop, McGill University = Université McGill Montréal, Canada, Faculdade de Geologia, Federal University of Para - Universidade Federal do Para Belem - Brésil
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2014
• Subjects: ocean oxygenation; nitrogen biogeochemical cycle; Nitrogen isotopes; Neoproterozoic; paleoceanography; [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry; [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography; Canada; Svalbard
• Online Access: https://hal.archives-ouvertes.fr/hal-01388690; https://hal.archives-ouvertes.fr/hal-01388690/document; https://hal.archives-ouvertes.fr/hal-01388690/file/Ader%20et%20al%202014.pdf; https://doi.org/10.1016/j.epsl.2014.03.042

International audience The end of the Neoproterozoic Era (1000 to 541 Ma) is widely believed to have seen the transition from a dominantly anoxic to an oxygenated deep ocean. This purported redox transition appears to be closely linked temporally with metazoan radiation and extraordinary perturbations to the global carbon cycle. However, the geochemical record of this transition is not straightforward, and individual data sets have been variably interpreted to indicate full oxygenation by the early Ediacaran Period (635 to 541 Ma) and deep ocean anoxia persevering as late as the early Cambrian. Because any change in marine redox structure would have profoundly impacted nitrogen nutrient cycling in the global ocean, the N isotope signature of sedimentary rocks (δ15Nsed) should reflect the Neoproterozoic deep-ocean redox transition. We present new N isotope data from Amazonia, northwest Canada, northeast Svalbard, and South China that span the Cryogenian glaciations (∼750 to 580 Ma). These and previously published data reveal a Nisotope distribution that closely resembles modern marine sediments, with a mode in δ15N close to +4 and range from −4 to +11. No apparent change is seen between the Cryogenian and Ediacarian. Data from earlier Proterozoic samples show a similar distribution, but shifted slightly towards more negative δ15N values and with a wider range. The most parsimonious explanation for the similarity of these Nisotopedistribution is that as in the modern ocean, nitrate (and hence O2) was stable in most of the middle–late Neoproterozoic ocean, and possibly much of Proterozoic Eon. However, nitrate would likely have been depleted in partially restricted basins and oxygen minimum zones (OMZs), which may have been more widespread than in the modern ocean.