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dc.contributor.authorStüeken, Eva E.
dc.contributor.authorGregory, Daniel D.
dc.contributor.authorMukherjee, Indrani
dc.contributor.authorMcGoldrick, Peter
dc.date.accessioned2022-04-25T23:43:16Z
dc.date.available2022-04-25T23:43:16Z
dc.date.issued2021-07-01
dc.identifier.citationStüeken , E E , Gregory , D D , Mukherjee , I & McGoldrick , P 2021 , ' Sedimentary exhalative venting of bioavailable nitrogen into the early ocean ' , Earth and Planetary Science Letters , vol. 565 , 116963 . https://doi.org/10.1016/j.epsl.2021.116963en
dc.identifier.issn0012-821X
dc.identifier.otherPURE: 273979863
dc.identifier.otherPURE UUID: 2c81cd7a-67a5-4752-a0ca-ab9b9afabd65
dc.identifier.otherRIS: urn:EA79ADE77284D38BA7172E8C0501391A
dc.identifier.otherORCID: /0000-0001-6861-2490/work/93161606
dc.identifier.otherScopus: 85105694445
dc.identifier.otherWOS: 000649176900015
dc.identifier.urihttps://hdl.handle.net/10023/25246
dc.descriptionEES acknowledges financial support from the School of Earth & Environmental Sciences, St Andrews. DDG acknowledges the support of NSERC for his Discovery grant (grant number 04834).en
dc.description.abstractOre deposits found in Proterozoic marine sedimentary basins supply much of the world's zinc. Many of the deposits formed contemporaneously with their host sediments when saline brines circulating from deeper in the basin reached the sea floor. Textural, geochemical and isotopic features of these SEDEX (‘sedimentary-exhalative’) deposits and their host sediments indicate that biologically active seeps, vents and brine pools were a feature of many ore-forming systems. In mineralised pockets of mid-Proterozoic basins, these ‘microbial oases’ were productive areas in an otherwise low productivity, anoxic, deep marine realm. Here we hypothesize that these metal-rich brines which circulated through organic matter-rich substrate also carried high levels of fixed nitrogen and stimulated distinct ecosystems at sites of mineralisation, or enhanced productivity more broadly in the basin. We tested this hypothesis with organic carbon and nitrogen analyses of samples of carbonaceous siltstone and shale from the 1.64 Ga Barney Creek Formation of northern Australia. The Barney Creek Formation hosts several SEDEX Zn systems, including one of the world's largest deposits at McArthur River Mine (the HYC deposit). Samples come from the mineralised edge of HYC and from correlated strata in drill cores at varying distances (1-60 km) from the deposit. The data reveal lower ratios of total organic carbon (TOC) to total nitrogen (TN) closer to the ore body. Strong correlations (r2>0.7) between TOC and TN and the absence of excess N in the samples suggest that most N was buried as bound to organic matter. Bioavailable N was thus probably more abundant closer to HYC, consistent with fixed nitrogen input by hydrothermal fluids. If correct, our data may suggest that such a hydrothermal nitrogen point source enabled microbes to develop lower C:N ratios in their biomass. A hydrothermal nitrogen source is also supported by a gradient in δ15N values from = +4‰ proximal to the vent to +7.5‰ in distal sites, which may point towards recycling of ammonium from the underlying Wollogorang Formation (1.73 Ga). This unit has previously been identified as a source of over-mature hydrocarbons to the ore-forming fluid. We speculate that, during the mid-Proterozoic, fixed nitrogen carried by SEDEX hydrothermal brines may have locally offset the lack of aerobic nutrient remineralization that characterized most of the anoxic Precambrian deep ocean and thus stimulated biological productivity in areas where the brines reached the sea floor, and, possibly, more broadly as spent brines mixed into the water column.
dc.language.isoeng
dc.relation.ispartofEarth and Planetary Science Lettersen
dc.rightsCopyright © 2021 Elsevier B.V. All rights reserved. This work has been made available online in accordance with publisher policies or with permission. Permission for further reuse of this content should be sought from the publisher or the rights holder. This is the author created accepted manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at https://doi.org/10.1016/j.epsl.2021.116963en
dc.subjectProterozoic lifeen
dc.subjectNitrogen cyclingen
dc.subjectSEDEX depositsen
dc.subjectG Geography (General)en
dc.subjectNDASen
dc.subjectSDG 14 - Life Below Wateren
dc.subjectACen
dc.subject.lccG1en
dc.titleSedimentary exhalative venting of bioavailable nitrogen into the early oceanen
dc.typeJournal articleen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews. School of Earth & Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews. St Andrews Centre for Exoplanet Scienceen
dc.identifier.doihttps://doi.org/10.1016/j.epsl.2021.116963
dc.description.statusPeer revieweden
dc.date.embargoedUntil2022-04-26


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