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Isotopic Evidence for an Aerobic Nitrogen Cycle in the Latest Archean
Abstract
The nitrogen cycle provides essential nutrients to the biosphere, but its antiquity in modern form is unclear. In a drill core though homogeneous organic-rich shale in the 2.5-billion-year-old Mount McRae Shale, Australia, nitrogen isotope values vary from +1.0 to +7.5 per mil (per thousand) and back to +2.5 per thousand over approximately 30 meters. These changes evidently record a transient departure from a largely anaerobic to an aerobic nitrogen cycle complete with nitrification and denitrification. Complementary molybdenum abundance and sulfur isotopic values suggest that nitrification occurred in response to a small increase in surface-ocean oxygenation. These data imply that nitrifying and denitrifying microbes had already evolved by the late Archean and were present before oxygen first began to accumulate in the atmosphere.
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“The whiff is recorded by spikes in Mo and Re concentrations, elevated nitrogen isotope values, and iron speciation data (Anbar et al., 2007; Reinhard et al., 2009; Garvin et al., 2009);”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Garvin et al., 2009
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Marine C, S and N biogeochemical processes in the redox-stratified early Cambrian Yangtze ocean
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BackgroundPossible nitrogen fertilization of the early Earth Ocean by microbial continental ecosystems
Thomazo, C., Couradeau, E., & García‐Pichel, F. (2018) · Nature Communications · doi:10.1038/s41467-018-04995-y · Cited by 44
Ammonium availability in the Late Archaean nitrogen cycle
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“N values reported by Garvin et al. (2009) for the 2.5 Ga Mount McRae Shale, the Kimberley Shale OC concentrations (127 to 1430 ppm) are than 10 to 100 times less than those reported for the Mount McRae Shale (~18,000 to 161,000 ppm).”
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“…appearances of nitrite/nitrate-dependent metabolisms are captured by the sedimentary nitrogen isotope record in late Mesoarchean soils at 3.2 Ga (Homann et al. 2018) and in Neoarchean shallow-marine settings at 2.7 and 2.5 Ga (Garvin et al. 2009; Godfrey and Falkowski 2009; Koehler et al. 2018).”
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“…by ferruginous conditions (Holland, 2002; Canfield, 2004), possibly punctuated by occasional sulfidic intervals in the Neoarchean (Anbar et al., 2007; Garvin et al., 2009; Reinhard et al., 2009); the early atmosphere was reducing with abundant carbon dioxide and methane but essentially devoid of…”
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“, 2007), on N isotope ratios (Garvin et al., 2009), and on Se isotope ratios (Stüeken et al.”
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“…Tesdal et al., 2013) and have been widely used to interpret positive δ15N values in the geological record (Ader et al., 2014; Algeo et al., 2014; Garvin et al., 2009; Godfrey & Falkowski, 2009; Kipp et al., 2018; Koehler et al., 2017; Luo et al., 2018; Stüeken, 2013; Wang et al., 2013; Wang,…”
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“Aerobic degradation of organic matter would result in 15N-enrichment of up to 4‰ (Gaye-Haake et al. 2005; Möbius et al. 2010), while anaerobic degradation of organic matter depletes 15N by 2‰ (Freudenthal et al. 2001; Möbius et al. 2010).”
BackgroundSchad, M., Konhauser, K. O., Sánchez‐Baracaldo, P., Kappler, A. A., & Bryce, C. C. (2019) · Free Radical Biology and Medicine · doi:10.1016/j.freeradbiomed.2019.07.014 · Cited by 28
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“McRae Shale, suggesting the presence of O2 in ancient shallow waters (Garvin et al., 2009).”
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“The strongly fractionating metabolism commonly considered for the moderately positive δ 15 N values recorded from 2.5 Ga onwards is non-quantitative denitrification 16,17,19,20 , which—in the modern ocean— occurs in dysoxic parts of the water column.”
InfluentialRodrigues, P. D. O. C., Hinnov, L. A., & Franco, D. R. (2019) · Precambrian Research · doi:10.1016/j.precamres.2019.04.007 · Cited by 24
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“The rise of oceanic oxidants preceding the Great Oxidation Event (GOE) might have initiated nitrification/ denitrification during the Neoarchean, when positive δ15N values have been observed (Garvin et al., 2009; Godfrey & Falkowski, 2009; Stüeken et al., 2015; Thomazo et al., 2011), paving the way towards an aerobic…”
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Early Life Record from Nitrogen Isotopes
Pinti, D., & Hashizume, K. (2011) · Springer eBooks · doi:10.1007/978-90-481-8794-2_8 · Cited by 19
“For a complete treatment on the subject, please refer to the reviews of Galloway (2003) , Brandes et al. (2007) and Sigman et al. (2009).”
MethodNitrogen isotope evidence for stepwise oxygenation of the ocean during the Great Oxidation Event
Chen, C., Busigny, V., Ader, M., Thomazo, C., Chaduteau, C., & Philippot, P. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.07.011 · Cited by 24
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Delarue, F., Robert, F., Sugitani, K., Tartèse, R., Duhamel, R., & Derenne, S. (2018) · Geochemical Perspectives Letters · doi:10.7185/geochemlet.1816 · Cited by 21
“The late Archean era (2.8 to 2.5 Ga) is characterised by the occurrence of positive OM δ15N values (up to ca. +5 ‰) presumably reflecting a rise in the abundance of oxidised N species (Beaumont and Robert, 1999; Garvin et al., 2009; Godfrey and Falkowski, 2009).”
BackgroundInfluentialAnaerobic nitrogen cycling on a Neoarchaean ocean margin
Mettam, C., Zerkle, A. L., Claire, M. W., Prave, A. R., Poulton, S. W., & Junium, C. K. (2019) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2019.115800 · Cited by 20
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“Accompanying theMo enrichment is a positive excursion in nitrogen isotope ratios (δ15 N) suggestive of local aerobic nitrogen cycling (Garvin et al., 2009), which implicates an expansion of oxygenated surface waters following the pulse of oxidative weathering.”
BackgroundOrganic Geochemical Signatures of Early Life on Earth
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“…of NH4+ to N Frontiers in Microbiology | www.frontiersin.org 2 September 2016 | Volume 7 | Article 1526 oxyanions by O2 in surface environments to support continued subsurface N2 synthesis via denitrification and anammox (Fennel et al., 2005; Garvin et al., 2009; Godfrey and Falkowski, 2009).”
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Luo, G., Zhu, X., Wang, S., Zhang, S., & Jiao, C. (2022) · Science China Earth Sciences · doi:10.1007/s11430-021-9934-y · Cited by 20
“…the carbonate associated Cr may not record the isotope information of seawater Cr6+, which probably can explain the discrepancy of the temporal variations in δ53Cr reconstructed based on carbonate rocks and BIF, respectively (Planavsky et al., 2014b; Cole et al., 2016; Gilleaudeau et al., 2016).”
BackgroundPhanerozoic radiation of ammonia oxidizing bacteria
Ward, L. M., Johnston, D. T., & Shih, P. M. (2021) · Scientific Reports · doi:10.1038/s41598-021-81718-2 · Cited by 19
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Fakhraee, M., Tarhan, L. G., Reinhard, C. T., Crowe, S. A., Lyons, T. W., & Planavsky, N. J. (2023) · Earth-Science Reviews · doi:10.1016/j.earscirev.2023.104398 · Cited by 20
“…multiple independent lines of evidence (e.g., redox-sensitive elements such as Mn, Fe, and Mo) for oxygen production, some of which are similarly characterized by a lack of evidence for extensive alteration (Czaja et al., 2012; Garvin et al., 2009; Kendall et al., 2010; Ostrander et al., 2019).”
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“This N2 fixation isotope record contradicts the possibility of existing water-column partial denitrification and/or anammox of marginal marine basins connected to the open ocean (δ(15)N values traditionally > +3‰; e.g., Ader et al., 2016; Garvin et al., 2009; Gilleaudeau et al., 2020; Stüeken et al., 2016), but is in…”
BackgroundEarth: Atmospheric Evolution of a Habitable Planet
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Shale Heavy Metal Isotope Records of Low Environmental O2 Between Two Archean Oxidation Events
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“Heavy N isotope values again support a local aerobic N cycle (up to δ(15)N = 7.5‰; Garvin et al., 2009), and even heavier Se and Mo isotope compositions imply more pronounced removal of lighter-mass isotopes in mildly oxygenated settings on the continental shelf (up to δ(82)Se = 1.”
BackgroundInfluentialSelf-citationRasmussen, B., Zi, J., & Muhling, J. R. (2023) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2023.117997 · Cited by 16
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“…to terrestrial environments for over a billion years (Ren et al. 2019) and the sedimentary geochemical records are derived from shallow oceans (Garvin et al. 2009; Pufahl and Hiatt 2012; Zerkle et al. 2017; Kipp et al. 2018), transportation of nitrite from the land to the ocean would be…”
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Self-citation16 Good Golly, Why Moly? THE STABLE ISOTOPE GEOCHEMISTRY OF MOLYBDENUM
Kendall, B., Dahl, T. W., & Anbar, A. D. (2017) · De Gruyter eBooks · doi:10.1515/9783110545630-017 · Cited by 16
“McRae Shale in drillcore ABDP-9 (Hamersley Basin) has been intensively 1124 studied at high stratigraphic resolution using a diverse range of elemental and isotopic (S, Mo, U, 1125 N, Se, Os) redox proxies (Anbar et al., 2007; Kaufman et al., 2007; Garvin et al., 2009; Reinhard 1126 et al., 2009; Duan et al., 2010; Ke…”
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Volcanic fertilization of Late Triassic lacustrine algal blooms
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Metadata
- Authors
- Garvin, J., Buick, R., Anbar, A. D., Arnold, G. L., & Kaufman, A. J.
- Affiliations
- University of Washington (US)
- Corresponding author
- Buick, Roger
- Venue
- Science
- Published
- 2009-02-20
- Volume
- 323
- Issue
- 5917
- Pages
- 1045-1048
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2000496027
- Cited by
- 260
- References
- 23
- Citations by year
- 2026: 6 · 2025: 21 · 2024: 14 · 2023: 11 · 2022: 18 · 2021: 18 · 2020: 13 · 2019: 14 · 2018: 20 · 2017: 17 · 2016: 8 · 2015: 11 · 2014: 12 · 2013: 23 · 2012: 18
- FWCI
- 13.73
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Science (publishedVersion)
- PubMed (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- nitrogen cycling, Archean, nitrogen isotopes, nitrification, denitrification, molybdenum, sulfur isotopes, ocean oxygenation, organic-rich shale, rock core
- MeSH terms
- Aerobiosis, Quaternary Ammonium Compounds, Anaerobiosis, Archaea, Australia, Bacteria, Biological Evolution, Nitrates, Nitrites, Nitrogen, Nitrogen Fixation, Nitrogen Isotopes, Oceans and Seas, Oxidation-Reduction, Oxygen, Time, Geologic Sediments
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