Marine oxygen production and open water supported an active nitrogen cycle during the Marinoan Snowball Earth
dc.contributor.author | Johnson, Benjamin W. | |
dc.contributor.author | Poulton, Simon W. | |
dc.contributor.author | Goldblatt, Colin | |
dc.date.accessioned | 2019-02-03T21:45:37Z | |
dc.date.available | 2019-02-03T21:45:37Z | |
dc.date.copyright | 2017 | en_US |
dc.date.issued | 2017 | |
dc.description.abstract | The Neoproterozoic Earth was punctuated by two low-latitude Snowball Earth glaciations. Models permit oceans with either total ice cover or substantial areas of open water. Total ice cover would make an anoxic ocean likely, and would be a formidable barrier to biologic survival. However, there are no direct data constraining either the redox state of the ocean or marine biological productivity during the glacials. Here we present iron-speciation, redox-sensitive trace element, and nitrogen isotope data from a Neoproterozoic (Marinoan) glacial episode. Iron-speciation indicates deeper waters were anoxic and Fe-rich, while trace element concentrations indicate surface waters were in contact with an oxygenated atmosphere. Furthermore, synglacial sedimentary nitrogen is isotopically heavier than the modern atmosphere, requiring a biologic cycle with nitrogen fixation, nitrification and denitrification. Our results indicate significant regions of open marine water and active biologic productivity throughout one of the harshest glaciations in Earth history. | en_US |
dc.description.reviewstatus | Reviewed | en_US |
dc.description.scholarlevel | Faculty | en_US |
dc.identifier.citation | Johnson, B. W.; Poulton, S. W.; & Goldblatt, C. (2017). Marine oxygen production and open water supported an active nitrogen cycle during the Marinoan Snowball Earth. Nature Communications, 8(1316). DOI: 10.1038/s41467-017-01453-z | en_US |
dc.identifier.uri | https://doi.org/10.1038/s41467-017-01453-z | |
dc.identifier.uri | http://hdl.handle.net/1828/10577 | |
dc.language.iso | en | en_US |
dc.publisher | Nature Communications | en_US |
dc.title | Marine oxygen production and open water supported an active nitrogen cycle during the Marinoan Snowball Earth | en_US |
dc.type | Article | en_US |