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

Ader, Magali; Sansjofre, Pierre; Halverson, Galen P.; Busigny, Vincent; Trindade, Ricardo I.F.; Kunzmann, Marcus; Nogueira, Afonso C.R.

doi:10.1016/j.epsl.2014.03.042

Cited by 180Paleontology and Stratigraphy of FossilsGeological and Geochemical AnalysisGeology and Paleoclimatology Research

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

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Ader, Magali, Sansjofre, Pierre, Halverson, Galen P., Busigny, Vincent, Trindade, Ricardo I.F., Kunzmann, Marcus, Nogueira, Afonso C.R.·2014·Earth and Planetary Science Letters

DOI 10.1016/j.epsl.2014.03.042

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Spatial variation of δ15N values appears inconsistent with widespread N cycling in the late-Neoproterozoic ocean.
“Spatial variation of δ15N values appears inconsistent with widespread N cycling in late-Neoproterozoic ocean25, 26.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [26]
Section 5.2 interprets the late-Neoproterozoic δ15N distribution as evidence for a nitrogen cycle similar to the modern ocean’s, with nitrate stable throughout most of the ocean. The Conclusions likewise say the global nitrogen cycle operated similarly to today’s. The paper argues against a globally redox-stratified ocean, not against widespread nitrogen cycling. (LLM, conf=0.88)
Checked by a reasoning model — may be wrong.
Experimental — accuracy not yet measured
The low δ15N values in the Nangao section originated from primary producers utilizing 15N-depleted NH4+, consistent with oceanic redox structure associated with OAEs.
“Rather, such low values have originated from primary producers utilizing 15N-depleted NH4 +, a process consistent with what is known of oceanic redox structure associated with the OAEs26, 28.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [26]
Section 1.2 (page unavailable) says that ammonium assimilation by primary producers under a shallow redox transition zone can produce negative δ15N values, as proposed for OAE2. Section 5.2 (page unavailable) also links low δ15N values during OAEs to redox stratification. The paper does not examine the Nangao section or establish that its producers used 15N-depleted NH4+, so it supports the proposed mechanism, not that site-specific conclusion. (LLM, conf=0.86)
Experimental — accuracy not yet measured
Assimilation of N2 into organic matter by N-fixation is accompanied by fractionation of as much as −4‰.
“Assimilation of N2 into organic matter by N-fixation is accompanied by fractionation of as much as −4‰26.”
From Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation (2017) · cites this paper as [26]

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[93]93. Sansofre, P., 2011. L'environnement post-marinoen (ca. 635 ma) : une étude multi-proxy de la plateforme carbonatée du Groupe d'Araras (Mato Grosso, Brésil). PhD thesis, Université Paris- Diderot, pp 287.

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“…produced by green or purple sulfur bacteria participating in ammonia assimilation with a large fractionation (Ohkouchi et al., 2005; Pennock et al., 1996) when upwelling currents were vigorous enough for some ammonia to reach the surface water before being converted to N2 (Ader et al., 2014) (Fig.”
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Authors: Ader, M., Sansjofre, P., Halverson, G. P., Busigny, V., Trindade, R. I. F., Kunzmann, M., & Nogueira, A. C. R.
Affiliations: Institut de physique du globe de Paris (FR)
Geotop (CA)
ORCID: Ader, Magali
Sansjofre, Pierre
Halverson, Galen P.
Busigny, Vincent
Trindade, Ricardo I.F.
Kunzmann, Marcus
Nogueira, Afonso C.R.
Venue: Earth and Planetary Science Letters
Publisher: Elsevier BV
Published: 2014-06
Volume: 396
Pages: 1-13
ISSN: 0012-821X (ISSN-L)
DOI: 10.1016/j.epsl.2014.03.042
OpenAlex: W1977990865
Cited by: 180
References: 158
Citations by year: 2026: 11 · 2025: 18 · 2024: 28 · 2023: 11 · 2022: 15 · 2021: 20 · 2020: 12 · 2019: 15 · 2018: 13 · 2017: 12 · 2016: 10 · 2015: 13 · 2014: 1
FWCI: 8.77
Type: journal article
Language: en
Open access: green
hal.science
Licence: other-oa
www.elsevier.com/tdm/userlicense/1.0/ (tdm)
www.elsevier.com/legal/tdmrep-license (tdm)
Locations: Earth and Planetary Science Letters (publishedVersion)
HAL (submittedVersion, other-oa)
Adelaide Research & Scholarship (AR&S) (University of Adelaide) (submittedVersion)
Funders: Conselho Nacional de Desenvolvimento Científico e Tecnológico
Fundação de Amparo à Pesquisa do Estado de São Paulo
American Chemical Society Petroleum Research Fund
Topics: Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
Keywords: nitrogen isotopes, ocean anoxia, atmospheric oxygenation, paleoceanography, Neoproterozoic

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

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