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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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Research works printed but not linked: 16
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Hensen, C., Zabel, M., Pfeifer, K., Schwenk, T., Kasten, S., Riedinger, N., Schulz, H. D., & Boëtius, A. (2003) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(03)00199-6 · Cited by 265
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“(e.g., Berner, 1982; Hedges, 1992; Emerson and Hedges, 1988; Premuzic et al., 1982; Smith and MacKenzie, 1987; Hedges and Keil, 1995; de Haas et al., 2002; Goni et al., 1997; Walsh, 1991).”
BackgroundStepwise oxygenation of the Paleozoic atmosphere
Krause, A. J., Mills, B. J. W., Zhang, S., Planavsky, N. J., Lenton, T. M., & Poulton, S. W. (2018) · Nature Communications · doi:10.1038/s41467-018-06383-y · Cited by 255
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Burke, A., Present, T. M., Paris, G., Rae, E. C. M., Sandilands, B. H., Gaillardet, J., Peucker‐Ehrenbrink, B., Fischer, W. W., McClelland, J. W., Spencer, R. G. M., et al. (2018) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2018.05.022 · Cited by 245
“Our estimate of the sulfide weathering flux from the weathering end-member decomposition (1.3 Tmol/y) is about twice as large as the commonly cited estimates of the global OWP flux (0.5–0.64 Tmol/y; Berner and Berner, 1996; Lerman et al., 2007), and is consistent with our estimate from an isotope mass balance discusse…”
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“[37] The averageOC accumulation rate (14.7 t C/km2/yr) in the ECS shelf is higher than the global mean value of 4.15 t C/km2/yr for shelves [Berner, 1982] (Table 3).”
BackgroundInfluentialOrganic carbon in shelf seas: sinks or sources, processes and products
de Haas, H., van Weering, T. C. E., & de Stigter, H. (2002) · Continental Shelf Research · doi:10.1016/s0278-4343(01)00093-0 · Cited by 238
“Early attempts to model the carbon cycle in the world oceans and seas were performed by Berner (1982) and Berner et al.”
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Aller, R. C., & Blair, N. E. (2006) · Continental Shelf Research · doi:10.1016/j.csr.2006.07.016 · Cited by 247
DeMaster, D. J. (2002) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/s0967-0645(02)00076-0 · Cited by 234
“5–1wt% of terrestrial organic carbon is buried with the detrital sediment on the continental margins (Berner, 1982), then most of the increase in the organic C contents above this threshold (equal to the x-axis intercept on Fig.”
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BackgroundSedimentary Diagenesis, Depositional Environments, and Benthic Fluxes
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BackgroundMicrobiological disproportionation of inorganic sulfur compounds
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Geochemistry of Fine-grained Sediments and Sedimentary Rocks
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“HCO3 - Ca2+ Na+ Mg2+ Cl- SO4 K+ A Meybeck (1979) Berner & Berner (1996) Mackenzie (1992)”
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Smith, S. V., & Mackenzie, F. T. (1987) · Global Biogeochemical Cycles · doi:10.1029/gb001i003p00187 · Cited by 200
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“At present, the combined OCfossil 206 re-burial flux in the Taiwanese and Himalayan source-to-sink systems is at least 0.8–1.2x106 tC 207 yr-1, accounting for >1% of the present day total organic carbon burial in marine sediments 208 (Berner, 1982; Schlünz and Schneider, 2000).”
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“This is an important question, since the flux and fate of river-derived material to the oceans play a key role in global environmental change (Bianchi and Allison, 2009), with up to 80% of global organic carbon being preserved in such marine deltaic deposits (Berner, 1982).”
BackgroundBlair, N. E., Leithold, E. L., & Aller, R. C. (2004) · Marine Chemistry · doi:10.1016/j.marchem.2004.06.023 · Cited by 195
Anaerobic mineralization in marine sediments from the Baltic Sea-North Sea transition
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“The highly reducing shelf sediments cover only 10 '10 of the ocean area but bury about 90 O/O of the organic carbon (Berner 1982).”
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“Organic carbon burial in marine sediments strongly depends on the supply of sediments (Berner, 1982), so, along with P regeneration, the increase in siliciclastic sediment supply to many shelf areas (Fig.”
BackgroundMolecular evidence for degradation and preservation of organic matter in the anoxic Black Sea Basin
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“Given the fact that there have been more studies on organic carbon preservation than on pyrite burial [Berner, 1982; Burdige, 2007; Hedges and Keil, 1995; Lin and Morse, 1991; Volkov and Rozanov, 1983], this approach should yield a more conclusive result than that obtained directly from global…”
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Middelburg, J. J. (2018) · Biogeosciences · doi:10.5194/bg-15-413-2018 · Cited by 194
“…accumulation rates are high in vegetated, coastal, deltaic, shelf and ocean-margin settings, the majority of organic matter burial occurs there, with organic carbon burial in deep-sea sediments accounting for < 5 % of the total buried matter (Berner, 1982; Duarte et al., 2005; Burdige, 2007).”
BackgroundEarly Diagenesis: Consequences for Applications of Molecular Biomarkers
Hedges, J. I., & Prahl, F. G. (1993) · Topics in geobiology · doi:10.1007/978-1-4615-2890-6_11 · Cited by 198
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Lasaga, A. C., Berner, R. A., & Garrels, R. M. (2011) · Geophysical monograph · doi:10.1029/gm032p0397 · Cited by 184
Self-citationThe global marine phosphorus cycle: sensitivity to oceanic circulation
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“Yet, in the modern ocean, up to 70–90% of burial of organic matter and reactive phosphorus takes place in nearshore environments and on the continental shelves (Berner, 1982; Ruttenberg, 1993; Howarth et al., 1995).”
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Ruttenberg, K. C. (1993) · Chemical Geology · doi:10.1016/0009-2541(93)90220-d · Cited by 182
Riedinger, N., Pfeifer, K., Kasten, S., Garming, J. F. L., Vogt, C., & Hensen, C. (2005) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2005.02.004 · Cited by 180
“Intermediate iron sulfides are metastable, but they can persist for a considerable period of time if hydrogen sulfide is entirely consumed (Berner, 1982; Kao et al., 2004).”
BackgroundSchlesinger, W. H. (2013) · Oxford Bibliographies in Ecology · doi:10.1093/obo/9780199830060-0111 · Cited by 175
Hu, L., Shi, X., Yu, Z., et al. (2012) · Marine Chemistry · doi:10.1016/j.marchem.2012.08.004 · Cited by 173
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“There is a net long-term burial of sulfide as pyrites of some 0.039 Pg S yr–1 (Berner 1982), corresponding to the production of 0.014 Pg C as carbon dioxide (2 mol carbon as CO2 per 1 mol sulfate reduced to sulfide).”
BackgroundInfluentialUranium isotopes distinguish two geochemically distinct stages during the later Cambrian SPICE event
Dahl, T. W., Boyle, R. A., Canfield, D. E., Connelly, J. N., Gill, B. C., Lenton, T. M., & Bizzarro, M. (2014) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2014.05.043 · Cited by 172
Litter in submarine canyons off the west coast of Portugal
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“Berner (1982) estimated a carbon deposition rate of 130 Mt/year in marine sediments, 80% of which was presumed to accumulate in deltaic and shelf sediments.”
BackgroundBiogeochemistry of Glacial Landscape Systems
Anderson, S. P. (2007) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.35.031306.140033 · Cited by 169
Dissolved Organic Carbon Cycling and Transformation
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“Today, some 70% of the total organic carbon removed from the global ocean-atmosphere-ter-restrial biosphere system is buried in the sediments of large tropical river deltas such as the Amazon and those in southeast Asia (Hedges and Keil, 1995; Berner, 1982).”
Great Salt Lake, and precursors, Utah: The last 30,000 years
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The isotopic composition of particulate organic carbon in mountain rivers of Taiwan
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“Present address: Department of Geography, Durham University, Science Laboratories, South Road, Durham, DH1 3LE, United Kingdom Email address: r.g.hilton@durham.ac.uk (Robert G. Hilton). efficiency can be high (Berner, 1982; Canfield, 1994; Hedges et al., 1999; Burdige, 2005;18 Galy et al., 2007a).”
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“Approximately, 85% of the carbon buried in continental margin environments occurs in river dominated ocean margin (RiOMar) systems (Berner, 1982; Hedges and Keil, 1995; McKee, 2003).”
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“The average C content of modern terriginous sediment rocks is 0.6% and the S content is 0.25% (Berner, 1982).”
BackgroundInfluentialBerner, R. A. (1989) · Global and Planetary Change · doi:10.1016/0921-8181(89)90018-0 · Cited by 159
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“A concern with this approach is that Fe is susceptible to rapid reduction and oxidation and its distribution can be affected by non-steady state chemical and physical processes associated with organic carbon input (diagenesis) (e.g. Berner, 1982, 1984).”
BackgroundStabilization of the coupled oxygen and phosphorus cycles by the evolution of bioturbation
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Clay mineral transformation as a major source for authigenic quartz in thermo-mature gas shale
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“…modern ocean, the burial of organic matter occurs predominantly in fine-grained siliciclastic sediments in deltaic, upper shelf, and slope settings where high rates of sedimentation, nutrient fluxes, and suspended loads of terrestrial organic matter are found (Berner 1982; Hedges and Keil 1995).”
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Variability and control of carbon consumption, export, and accumulation in marine communities
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“…usually amount to 90–95% of short-term refractory accumulation in open ocean sediments, whereas they only amount to 70–75% in coastal sediments (Berner 1982; Lein 1984), the differences in carbon preservation between oceanic phytoplankton and coastal macrophytic communities (i.e., marshes)…”
BackgroundWoulds, C., Cowie, G. L., Levin, L. A., Andersson, H. J., Middelburg, J. J., Vandewiele, S., Lamont, P. A., Larkin, K. E., GOODAY, A. J., Schumacher, S., et al. (2007) · Limnology and Oceanography · doi:10.4319/lo.2007.52.4.1698 · Cited by 153
“1698 Continental margin sediments are important sites for the accumulation and burial of organic matter (OM) (DeMaison and Moore 1980; Berner 1982).”
BackgroundLandfill CH4: Rates, fates, and role in global carbon cycle
Bogner, J., & Spokas, K. A. (1993) · Chemosphere · doi:10.1016/0045-6535(93)90432-5 · Cited by 154
Selective preservation of soil organic matter in oxidized marine sediments (Madeira Abyssal Plain)
Huguet, C., de Lange, G. J., Gustafsson, Ö., Middelburg, J. J., Damsté, J. S. S., & Schouten, S. (2008) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2008.09.021 · Cited by 157
Tomales bay metabolism: CNP stoichiometry and ecosystem heterotrophy at the land-sea interface
Smith, S. V., Hollibaugh, J. T., Dollar, S. J., & Vink, S. M. (1991) · Estuarine Coastal and Shelf Science · doi:10.1016/0272-7714(91)90055-g · Cited by 150
Controls on phosphorus concentration and accumulation in oceanic sediments
Filippelli, G. M. (1997) · Marine Geology · doi:10.1016/s0025-3227(96)00113-2 · Cited by 151
Bounding cross-shelf transport time and degradation in Siberian-Arctic land-ocean carbon transfer
Bröder, L., Tesi, T., Andersson, A., Semiletov, I., & Gustafsson, Ö. (2018) · Nature Communications · doi:10.1038/s41467-018-03192-1 · Cited by 149
Shi, Q., Leipe, T., Rueckert, P., et al. (2010) · Journal of Marine Systems · doi:10.1016/j.jmarsys.2010.02.003 · Cited by 149
Aller, R. C., Madrid, V. M., CHISTOSERDOV, A. Y., Aller, J. Y., & Heilbrun, C. (2010) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2010.05.008 · Cited by 150
A model of suboxic sedimentary diagenesis suitable for automatic tuning and gridded global domains
Archer, D. E., Morford, J. L., & Emerson, S. (2002) · Global Biogeochemical Cycles · doi:10.1029/2000gb001288 · Cited by 151
“[42] The gridded global domain presented above is limited to locations deeper than 1000 m, excluding shallow water sediments which are generally thought to comprise 80–90% of global carbon burial [Berner, 1982; Hedges and Keil, 1995].”
BackgroundEnhanced terrestrial carbon preservation promoted by reactive iron in deltaic sediments
Shields, M. R., Bianchi, T. S., Gélinas, Y., Allison, M. A., & Twilley, R. R. (2016) · Geophysical Research Letters · doi:10.1002/2015gl067388 · Cited by 151
“This plays a major role in atmospheric CO2 concentrations by providing a link between the short-term cycling of terrestrial and aquatic carbon and the long-term carbon cycle through burial and eventual incorporation into the rock cycle [Berner, 1982; Hedges and Keil, 1995; Burdige, 2005].”
BackgroundLenton, T. M. (2001) · Global Change Biology · doi:10.1046/j.1354-1013.2001.00429.x · Cited by 151
“About 0.3% of marine productivity (~1.3 3 1013 mol y±1) ã 2001 Blackwell Science Ltd, Global Change Biology, 7, 613±629 also reaches marine sediments (Berner 1982), and further oxidation occurs there.”
BackgroundInfluentialEffects of fuel and forest conservation on future levels of atmospheric carbon dioxide.
Walker, J. C., & Kasting, J. (1992) · Global and Planetary Change · doi:10.1016/0031-0182(92)90207-l · Cited by 188
“It is exactly balanced in our formulation by the precipitation of fresh organic carbon in shelf sediments (Berner, 1982), although short-term imbalances are possible in the real world.”
BackgroundJustić, D., Rabalais, N. N., & Turner, R. E. (2002) · Ecological Modelling · doi:10.1016/s0304-3800(01)00472-0 · Cited by 147
“We assume here that the above value also accounts for a large portion of anaerobic respiration, because most of the dissolved sulfide produced under anoxic conditions is re-oxidized by free dissolved oxygen (Berner, 1982).”
BackgroundAnthropogenic influences on riverine fluxes of dissolved inorganic carbon to the oceans
Raymond, P. A., & Hamilton, S. K. (2018) · Limnology and Oceanography Letters · doi:10.1002/lol2.10069 · Cited by 146
An evaluation of mobile mud dynamics in the Mississippi River deltaic region
Corbett, D. R., McKee, B. A., & Duncan, D. (2004) · Marine Geology · doi:10.1016/j.margeo.2004.05.028 · Cited by 144
“deltas and continental shelves are considered to be the main repositories of organic matter in marine sediments ( Berner, 1982, 1989; Hedges and Keil, 1995; Mayer et al., 1998).”
BackgroundWhat determines sedimentary C/S ratios?
Morse, J. W., & Berner, R. A. (1995) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(95)00024-t · Cited by 143
Self-citationDynamics of dissolved organic carbon in a coastal ecosystem
Zweifel, U. L., Wikner, J., Hagström, Å., et al. (1995) · Limnology and Oceanography · doi:10.4319/lo.1995.40.2.0299 · Cited by 143
Nature of particulate organic matter in the River Indus, Pakistan
Ittekkot, V., & Arain, R. (1986) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(86)90127-4 · Cited by 143
Mollenhauer, G., Inthorn, M., VOGT, T. M., Zabel, M., Damsté, J. S. S., & Eglinton, T. I. (2007) · Geochemistry Geophysics Geosystems · doi:10.1029/2007gc001603 · Cited by 148
“[2] Continental margins play an important role in the global carbon cycle as areas of high primary productivity [Carr, 2001], sites of organic matter burial [Berner, 1982; Reimers et al., 1992; Wollast, 1998], and locations where terrigenous material enters the oceans.”
BackgroundJørgensen, B. B. (1996) · Coastal and estuarine studies · doi:10.1029/ce052p0115 · Cited by 142
Stable isotopic characterization of organic carbon accumulation on the Amazon continental shelf
Showers, W., & Angle, D. G. (1986) · Continental Shelf Research · doi:10.1016/0278-4343(86)90062-2 · Cited by 142
Weijers, J. W. H., Schouten, S., Schefuß, E., Schneider, R. R., & Damsté, J. S. S. (2008) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2008.10.016 · Cited by 140
Fluxes of dissolved organic carbon from Chesapeake Bay sediments
Burdige, D. J., & Homstead, J. (1994) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(94)90095-7 · Cited by 140
Wortmann, U. G., Chernyavsky, B. M., Bernasconi, S. M., Brunner, B., Böttcher, M. E., & Swart, P. K. (2007) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2007.06.033 · Cited by 138
“E-mail address: uli.wortmann@utoronto.ca (U.G. Wortmann). nental-shelf sediments (Jørgensen, 1982), and is a fundamental process linking the geochemical cycles of carbon, sulfur, and oxygen (e.g., Berner, 1982; Schidlowski et al., 1983; Garrels and Lerman, 1984; Wortmann and Chernyavsky, 2007).”
BackgroundChen, C. A., Liu, K., & Macdonald, R. W. (2003) · Springer eBooks · doi:10.1007/978-3-642-55844-3_4 · Cited by 137
A critique of Phanerozoic climatic models involving changes in the CO2 content of the atmosphere
Boucot, A. J., & Gray, J. (2001) · Earth-Science Reviews · doi:10.1016/s0012-8252(01)00066-6 · Cited by 137
Chanton, J. P., Martens, C. S., & Goldhaber, M. B. (1987) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(87)90211-0 · Cited by 135
Hu, L., Shi, X., Guo, Z., et al. (2012) · Marine Geology · doi:10.1016/j.margeo.2012.10.008 · Cited by 135
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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