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Burial of organic carbon and pyrite sulfur in the modern ocean; its geochemical and environmental significance.
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“Moreover, on longer geological time scales, the deposition, burial and subduction of OC within marine sediment in plate subduction margins can play a pivotal role in the long-term carbon cycle, influencing atmospheric CO2 amounts over millions of years (Berner, 1982; Burdige, 2007; Clift, 2017).”
From Event Stratigraphy in a Hadal Oceanic Trench: The Japan Trench as Sedimentary Archive Recording Recurrent Giant Subduction Zone Earthquakes and Their Role in Organic Carbon Export to the Deep Sea (2019) · cites this paper as Berner, 1982
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“This transfer constitutes a geological carbon sink if the buried organic carbon is recently assimilated plant or soil organic carbon (OCbios) (Berner, 1982; Derry & France-Lanord, 1997; Galy et al., 2007; Hilton et al., 2008).”
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BackgroundInfluentialEstimating the upper limit of Proterozoic petrographic organic carbon recycling
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“…carbon (OC) in soils and sedimentary depocenters can remove carbon from the atmosphere over timescales of centuries to millennia (Hilton and West, 2020; Galy et al., 2015; Blair and Aller, 2012; Battin et al., 2009; Hayes et al., 1999; Stallard, 1998; France-Lanord and Derry, 1997; Berner, 1982).”
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Sedimentary conditions drive modern pyrite burial flux to exceed oxidation
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“To our knowledge, this represents the first independent pyrite burial flux estimate that does not rely on OC burial scaling factors 32 , global mass-balance box models 37 or the assumption of sulfur-cycle steady state 3,6 .”
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“Over geological timescales, the burial of biospheric OC acts as a carbon sink, consuming atmospheric CO 2 (Berner, 1982; France‐Lanord & Derry, 1997), whereas the exposure of carbonaceous rocks leads to the oxidation of petrogenic OC, functioning as a carbon source (Berner, 2004; Hilton & West,…”
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“The fluvial export and deposition of recently fixed POCbiosphere (such as from litter and surface soils) in the sedimentary basins are an important mechanism of atmospheric CO2 drawdown over millennial timescales (Berner, 1982; France-Lanord and Derry, 1997; Hilton and West, 2020).”
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“The TOC, TN, and TS contents of the sediments are known as useful proxies for the reconstruction of the depositional environment (e.g. Berner, 1982; Sampei et al., in Lützow-Holm Bay (Yasuhara et al., 2007).”
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Rao, P. S., Mascarenhas, A., Paropkari, A. L., et al. (1994) · Marine Geology · doi:10.1016/0025-3227(94)90017-5 · Cited by 4
“A linear relationship exists between organic carbon and sulfide sulfur in normal marine sediments with the regression line passing through the origin (Goldhaber and Kaplan, 1974; Berner, 1982), whereas the regression line for anoxic sediments”
BackgroundInfluentialPyritized ooids from the Arabian Sea Basin
Rao, P. S., Rao, C. M., & Reddy, N. P. C. (1988) · Deep Sea Research Part A Oceanographic Research Papers · doi:10.1016/0198-0149(88)90012-x · Cited by 4
Advances in marine chemistry 1979–1982
Jenkins, W. J., & Edmond, J. M. (1983) · Reviews of Geophysics · doi:10.1029/rg021i005p01233 · Cited by 4
Sediment fluxes and carbon budgets in Loch Creran, western Scotland
Loh, P. S., Reeves, A. D., Miller, A. E. J., et al. (2010) · Geological Society London Special Publications · doi:10.1144/sp344.10 · Cited by 4
“According to Berner (1982), a total of 126 1012 g a21 OC is deposited in deltaic shelf sediments.”
BackgroundHewaidy, A. G. A., Mandur, M. M. M., Farouk, S., et al. (2019) · Arabian Journal of Geosciences · doi:10.1007/s12517-019-4485-y · Cited by 4
“Although they receive high terrigenous organic matter alongside the high clastic supply, most prodeltaic and submarine fans have TOC% values less than 1% (Demaison and Moore 1980; Berner 1982; Tyson 1995).”
BackgroundExamination of the 2011 Mississippi River Flood Deposit on the Louisiana Continental Shelf
Young, D. R. (2014) · The Scholarship East Carolina University's Institutional Repository (East Carolina University) · Cited by 4
Chen, Z., Xun, L., Xia, Y., et al. (2025) · mBio · doi:10.1128/mbio.01722-25 · Cited by 3
“However, over 80% sulfide is eventually reoxidized back to sulfate, while less than 20% is ultimately buried as metal sulfides, e.g., FeS, FeS 2 , or sulfurized organic matter (3, 4).”
Song, Q., Wang, J., Algeo, T. J., Xu, L., Chen, C., Wang, Z., cheng, C., Geng, K., & Li, Q. (2026) · Frontiers in Marine Science · doi:10.3389/fmars.2026.1771442 · Cited by 4
Rosentreter, J. A., & Eyre, B. D. (2025) · Global Biogeochemical Cycles · doi:10.1029/2024gb008134 · Cited by 3
“TAlk production through pyrite formation was also estimated based on mangrove carbon burial rates and the ratio between sedimentary organic carbon and sulfur (C/S ratio) in mangrove sediments (Berner, 1982, 1984; Hu & Cai, 2011; Krumins et al., 2013).”
El-Ezz, A. R. A., Abdou, A. A., & Temraz, M. G. (2012) · Petroleum Science and Technology · doi:10.1080/10916466.2010.499404 · Cited by 3
“Moreover, the dominant occurrence of the framboids, particularly the clustered forms in organic-rich shales, tends to indicate a biogenic origin as a consequence of the bacterial reduction of seawater sulfate (Berner, 1982).”
BackgroundYou, O.-R., Mok, J., Kim, S.-H., Choi, D.-L., & Hyun, J. (2010) · Ocean and Polar Research · doi:10.4217/opr.2010.32.3.299 · Cited by 3
“유기물 분해에 의해 생성된 무기물은 다시 수층으로 재순환(recycling)하게 되고, 분해 가 이루어지지 않은 일부 유기물은 퇴적물 내에 묻히거나 (buried) 외해로 이동된다(Berner 1982; Wollast 1991).”
Ismail, S., Schulz, H.-M., Wilkes, H., et al. (2010) · Geological Society London Petroleum Geology Conference series · doi:10.1144/0070811 · Cited by 3
Arning, E. T., Häußler, S., van Berk, W., & Schulz, H.-M. (2016) · Computers & Geosciences · doi:10.1016/j.cageo.2016.04.004 · Cited by 3
Source and composition of organic matter and its role in designing sediment microbial communities
Vincent, S. G. T., Jennerjahn, T. C., & Ramasamy, K. (2021) · Elsevier eBooks · doi:10.1016/b978-0-12-815165-5.00001-7 · Cited by 5
Middle Archean continent formation by crustal delamination
Zegers, T. E., & van Keken, P. E. (2001) · Geology · doi:10.1130/0091-7613(2001)029
Metadata
- Authors
- Berner, R. A.
- Corresponding author
- Berner, R. A.
- Venue
- American Journal of Science
- Publisher
- American Journal of Science (AJS)
- Published
- 1982-04-01
- Volume
- 282
- Issue
- 4
- Pages
- 451-473
- ISSN
- 0002-9599 (ISSN-L)
- OpenAlex
- W2049621326
- Cited by
- 1,200
- References
- 0
- Citations by year
- 2026: 35 · 2025: 53 · 2024: 66 · 2023: 53 · 2022: 62 · 2021: 57 · 2020: 54 · 2019: 37 · 2018: 43 · 2017: 40 · 2016: 47 · 2015: 43 · 2014: 20 · 2013: 42 · 2012: 34
- FWCI
- 14.34
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- American Journal of Science (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Plankton and Biogeochemistry
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- organic carbon burial, pyrite sulfur, marine sediment, marine geochemistry, marine environment, sulfur cycling
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