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Authigenic Carbonate and the History of the Global Carbon Cycle
Open accessAbstract
The Third Way: Because organic carbon contains a larger fraction of the light isotope 12 C than inorganic carbonate, variations in the carbon isotopic record of sedimentary rocks are thought to represent changes in the amount of organic carbon buried as sediments (and thus removed from the rest of the carbon cycle). Schrag et al. (p. 540 ; see the Perspective by Canfield and Kump ) suggest that historically a third component was important: authigenic carbonate. Authigenic carbonate is not produced in any appreciable quantity today, but was much more abundant when the level of atmospheric oxygen was low.
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“Periods of low atmospheric oxygen and widespread marine anoxia in past climates have been favorable for the formation of abiotic authigenic carbonates in marine sediment pore fluids, representing a significant carbon sink54.”
From Acceleration of dolomitization by zinc in saline waters (2019) · cites this paper as [54]
In the citing paper
“These processes can alter carbonate δ 13 C and δ 18 O, as well as the trace element compositions (e.g., Schrag et al., 2013;Swart and Kennedy, 2012), limiting their use for paleoenvironmental proxies.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Schrag et al., 2013
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“…encompassing carbonate production and associated processes at various scales, from local precipitation to global sedimentation (Schlager, 2000; Schrag et al., 2013; Reijmer, 2021)—is therefore essential for comprehending the dynamics of the carbon cycle and its implications for climate…”
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“…and in recent models variously attributed to non-steady state behaviour, disconnections from open ocean DIC (dissolved inorganic carbon), methane release and diagenesis (Bjerrum & Canfield, 2011; Busch et al., 2022; Derry, 2010; Fike et al., 2006; Knauth & Kennedy, 2009; Schrag et al., 2013).”
A potentially New Early Ediacaran Glaciation
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“…flux of methane hydrates from an anox‐ ic ocean (Bjerrum and Canfield, 2011), authigenic/diagenetic carbonates (Xiao et al., 2020; Zhou et al., 2016; Schrag et al., 2013), and dynamic/episodic marine shelf oxygenation associ‐ ated with amalgamation of the Gondwana continents (Li et al., 2018)…”
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Biogeochemical Consequences of the Sedimentary Subseafloor Biosphere
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“Conversely, negative carbon isotope excursions could be explained by a decrease in the burial flux of authigenic carbonate or by the incorporation of authigenic carbonate within carbonate shelf sediments (Schrag et al., 2013).”
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Lithium isotopes trace silicate weathering-driven authigenic carbonate formation in marine sediments
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“Authigenic carbonates are carbonate minerals that precipitated in situ from solution, either at the sediment-water interface or within sediment pore water 1 .”
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“…interpreted to reflect oxidation of exposed continental shelf sediments rich in fossil organic matter and/or oxidation of oceanic methane hydrate (e.g. Kaufman et al. 2007), or to reflect a contribution from authigenic carbonates produced in sediments during early diagenesis (Schrag et al. 2013).”
BackgroundIsotopic Tracers of Nonclassical Crystallization
Lammers, L. N., & Koishi, A. (2021) · ACS symposium series · doi:10.1021/bk-2021-1383.ch007 · Cited by 3
A refined recycled carbonatite model for the δ13C negative anomaly in the upper Doushantuo Formation
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“The homogeneous micrite microfacies is interpreted as authigenic precipitation of carbonate in a subaqueous subenvironment (Schrag et al., 2013).”
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“Biological carbonate production in the oceans is an important contributor to the global marine carbonate factory and biogeo-chemical cycles (Schrag et al., 2013; Gilbert et al., 2022).”
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Hagen, C. (2024) · Geochemistry Geophysics Geosystems · doi:10.1029/2024gc011718 · Cited by 3
“Following the Shuram CIE, CIP values transition to ∼ 0‰ by the Precambrian–Cambrian boundary (Figure 1).”
InfluentialIsotopically anomalous organic carbon in the aftermath of the Marinoan snowball Earth
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“…the conditions of diagenesis and catagenesis in the areas of their formation, thereby allowing reconstruction of the features of the past bio-geochemical processes, which makes it relevant to study in detail the mechanisms of their formation (Lein, 2004; Schrag et al., 2013; Phillips et al., 2018).”
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“( 20 17 ); da ta of th e M K se ct io n ar e fr om th is st ud y. diagenetic fluid modification, and authigenic carbonate formation (e.g., Knauth and Kennedy, 2009; Derry, 2010; Schrag et al., 2013).”
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“…or thermogenic carbon release, variations in the burial flux of organic carbon, unstable carbonate saturation state due to ocean acidification or elevated alkalinity, and/or authi-genic carbonate precipitation (Payne et al., 2004; Payne & Kump, 2007; Meyer et al., 2011; Schrag et al., 2013).”
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“As a result, many authors have interpreted extreme negative anomalies as diagenetic artefacts, biased sampling of authigenic cements or as purely regional phenomena (Bristow & Kennedy, 2008; Derry, 2010; Grotzinger & Fike, 2011; Schrag et al., 2013; Li et al., 2017; Shi et al., 2018).”
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The Carbon Isotope Record and Earth Surface Oxygenation
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“Mechanisms to explain a positive excursion of δ 13C imply increase in organic carbon burial rates (changes in chemistry of ocean or methanogenesis) or more acidic weathering conditions with increase in biological productivity (Schrag et al., 2013).”
Background埃迪卡拉纪Shuram碳同位素负偏事件有机碳<?Pub _newline?>氧化假说的定量模型评估
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Metadata
- Authors
- Schrag, D. P., Higgins, J. A., Macdonald, F. A., & Johnston, D. T.
- Affiliations
- Harvard University (US)
- Princeton University (US)
- Venue
- Science
- Published
- 2013-02
- Volume
- 339
- Issue
- 6119
- Pages
- 540-543
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2114839168
- Semantic Scholar
- 271d01ca5514443dcc869aa77013e96976d7ffd6
- Cited by
- 532
- References
- 37
- Citations by year
- 2026: 28 · 2025: 48 · 2024: 53 · 2023: 44 · 2022: 45 · 2021: 47 · 2020: 39 · 2019: 44 · 2018: 30 · 2017: 36 · 2016: 40 · 2015: 40 · 2014: 18 · 2013: 19
- FWCI
- 26.42
- Type
- journal article
- Language
- en
- Open access
- green
- nrs.harvard.edu
- Licence
- cc-by
- Locations
- Science (publishedVersion)
- PubMed (publishedVersion)
- Digital Access to Scholarship at Harvard (DASH) (Harvard University) (submittedVersion, cc-by)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- authigenic carbonates, carbon cycle, carbon isotopes, early diagenesis, atmospheric oxygen, ocean anoxia, Proterozoic, Paleozoic, Triassic, carbon isotope excursion
- MeSH terms
- Anaerobiosis, Atmosphere, Carbon Isotopes, Carbonates, Methane, Oxidation-Reduction, Oxygen, Geologic Sediments, Carbon Cycle
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