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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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Wang, J., Hilton, R. G., Jin, Z., Zhang, F., Densmore, A. L., Gröcke, D. R., Xu, X., Li, G., & West, A. J. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.02.031 · Cited by 43
“Over geological timescales, erosion and burial of POCbiosphere is an important CO2 sink (Berner, 1982; France-Lanord and Derry, 1997), while oxidation of POCpetro will release CO2 into the atmosphere (Petsch et al., 2000; Bouchez et al., 2010; Hilton et al., 2014; Hemingway et al., 2018).”
BackgroundAkam, S. A., Coffin, R. B., Abdulla, H. A. N., & Lyons, T. W. (2020) · Frontiers in Marine Science · doi:10.3389/fmars.2020.00206 · Cited by 42
“(Berner, 1982; Jørgensen, 1982; Jørgensen and Nelson, 2004; Zopfi et al., 2004; Wasmund et al., 2017).”
Chen, G., Chang, X., Gang, W., Wang, N., Zhang, P., Cao, Q., & Xu, J. (2020) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2020.104587 · Cited by 41
The Geologic History of the Carbon Cycle
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Thomson, J., Jarvis, I., Green, D. R. H., & Green, D. (1998) · doi:10.2973/odp.proc.sr.157.130.1998 · Cited by 41
Dissolved organic phosphorus in the Mississippi River plume during spring and fall 2002
Rinker, K. R., & Powell, R. T. (2006) · Marine Chemistry · doi:10.1016/j.marchem.2005.09.013 · Cited by 40
“Within the global oceanic carbon cycle, a disproportionately large amount of fixed carbon is being buried in coastal waters (Berner, 1982; Hedges and Keil, 1995) and while much of this carbon may be of terrigenous origin, a large amount is autochthonous (Trefry et al., 1994; Hedges and Keil, 1995).”
BackgroundCui, X., Bianchi, T. S., Hutchings, J., et al. (2016) · Journal of Geophysical Research Biogeosciences · doi:10.1002/2015jg003225 · Cited by 40
“Continental shelves bury over 90% of OC in the ocean and represent the largest sink of terrestrial (OCterr) and marine (OCmari) OC in the global ocean [Berner, 1982; Hedges, 1992; Hedges and Keil, 1995; Bianchi, 2011].”
BackgroundFate of Organic Carbon Burial in Modern Sediment Within Yangtze River Estuary
Sun, X., Fan, D., Liao, H., & Tian, Y. (2019) · Journal of Geophysical Research Biogeosciences · doi:10.1029/2019jg005379 · Cited by 41
“The estimated OCARs in cores C6 and D2 were 3.50–4.67 g C cm−2 year −1 (4.29 ± 0.41 g C cm−2 year−1) and 3.94–5.58 g C cm−2 year−1 (4.39 ± 0.47 g C cm−2 year−1), respectively (Figure S4), which is comparable to the average global OCAR in shelf sediments (4.15 g C cm−2 year−1; Berner, 1982).”
ResultInfluentialMenges, J., Hovius, N., Andermann, C., Lupker, M., Haghipour, N., Märki, L., & Sachse, D. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.07.003 · Cited by 40
Smedberg, E., Mörth, C., Swaney, D. P., & Humborg, C. (2006) · Global Biogeochemical Cycles · doi:10.1029/2005gb002567 · Cited by 40
“[2] Silicon (Si) may play a crucial role in carbon (C) sequestration patterns on land over geological timescales [Berner, 1982 1992; Schwartzman and Volk, 1989].”
BackgroundSulphur Isotopes and Microbial Sulphur Cycling in Sediments
Bottrell, S. H., & Raiswell, R. (2000) · Springer eBooks · doi:10.1007/978-3-662-04036-2_12 · Cited by 40
du Châtelet, E. A., Bout‐Roumazeilles, V., Coccioni, R., et al. (2012) · Marine Geology · doi:10.1016/j.margeo.2012.10.013 · Cited by 39
Wallmann, K., Schneider, B., & Sarnthein, M. (2016) · Climate of the past · doi:10.5194/cp-12-339-2016 · Cited by 44
“These include bulk sedimentation rate (Berner, 1982), surface area of sediment particles (Mayer et al., 2004), oxygen exposure time (Hartnett et al., 1998), and the resuspension and down-slope transport of shelf POC promoting POC burial at the upper slope (Walsh et al., 1981; Dale et al., 2015).”
BackgroundWitts, J. D., Newton, R. J., Mills, B. J. W., Wignall, P. B., Bottrell, S. H., Hall, J. L. O., Francis, J. E., & Crame, J. A. (2018) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.02.037 · Cited by 41
“…of the tight coupling apparent in marine sediments between the burial of isotopically depleted organiccarbon and pyrite-sulfur, any increase in pyrite burial, indicated by a significant positive shift in the sulfur isotope record, should be mirrored by an increase in carbon burial (Berner, 1982).”
BackgroundSulfur cycling in the Yellow River and the sulfate flux to the ocean
Zhang, D., Zhao, Z., Peng, Y., Fan, B., Zhang, L., Li, J., & Chen, A. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.119451 · Cited by 40
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“An estimated 80–85% of carbon burial is currently occurring on continental margins, mainly off river-dominated coasts (Berner, 1982; Hedges and Keil, 1995).”
The Global Sulphur Cycle and Its Links to Plant Environment
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“ocean area (Berner 1982), the production and accumulation rates of BSi in these margins are significantly higher than in the open ocean (Nelson et al.”
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“This is partially due to the variability of the particulate organic carbon (POC) fluxes from continents to oceans, which have a major role in the regulation of atmospheric C regardless of the timescale (Berner, 1982, Sarmiento and Gruber, 2006).”
BackgroundWhere’s the Carbon: Exploring the Spatial Heterogeneity of Sedimentary Carbon in Mid-Latitude Fjords
Smeaton, C., & Austin, W. E. N. (2019) · Frontiers in Earth Science · doi:10.3389/feart.2019.00269 · Cited by 37
“…systems it is estimated that globally the muddy sediments bury between 57 and 107 tonnes OC km−2 yr−1 which far exceeds all other marine environments (Berner, 1982; Hedges et al., 1997; Smith et al., 2015) with the upper range being similar to the OC rich intertidal environments (Duarte et al.,…”
BackgroundInfluentialOrigin and Diagenesis of Clay Minerals in the Monterey Formation, Santa Maria Basin Area, California
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The Recycling of Biogenic Material at the Seafloor
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“We can make some useful generalizations from the results of these studies (Boudreau, 1994). First, the depth of the “mixed layer”—the depth zone over which bioturbation is present—is fairly constant throughout the ocean at 10 ^ 5 cm. Second, the bioturbation mixing coefficient varies widely, with values ranging from ,…”
ResultInfluentialZhu, C. W., Wagner, T., Pan, J., & Pancost, R. D. (2011) · Geochemistry Geophysics Geosystems · doi:10.1029/2011gc003506 · Cited by 43
“[2] Burial of organic matter in marine sediments is thought to represent the second largest sink of atmospheric CO2, thereby directly contributing to climatic regulation over geological timescales [ Berner, 1982, 1990 ].”
BackgroundMethane fluxes to the atmosphere from deepwater hydrocarbon seeps in the northern Gulf of Mexico
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“As a result, on Earth, >90% of organic C is buried on continental margins (Berner 1989, 1982; Burdige 2005).”
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“Burial of organic carbon in the sediments is estimated to be between 126 and 160 Mt C yr-1 (Berner, 1982; Hedges and Keil, 1995; Baumgart et al., 2010; Bourgoin and Tremblay, 2010).”
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Erosion of modern terrestrial organic matter as a major component of sediments in fjords
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“They account for 90% of Holocene organic carbon (OC) burial in the global ocean, despite occupying less than 10% of ocean surface area [Berner, 1982; Hedges, 1992; Hedges and Keil, 1995].”
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Ocean life cycles and the atmospheric CO2 content
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Introducing GloRiSe – a global database on river sediment composition
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“Riverine suspended sediment fluxes of organic carbon (Berner, 1982; Hilton and West, 2020), phosphorous (Berner, 1999; Froelich et al.”
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“In this study, although C/S ratios in the fluvial sediment (mean 35.08) are consistent with freshwater sediment (Berner 1984: 18.75–93.75), the marine sediment values are exceptionally high (more than an order of magnitude above typical values quoted by Berner 1982).”
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“Introduction Marine sediments represent the largest reservoir of organic carbon on earth and organic matter (OM) burial in marine sediments plays a key-role in the carbon cycle (Berner, 1982).”
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“However, evidence suggests that the bulk of the reactive carbon is mineralized at an early stage of diagenesis, leading to asymptotic carbon concentrations close to the sea floor (Berner, 1982).”
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“Under natural hydrodynamic processes, OC can accumulate and add to the long-term store within marine sediments (Berner, 1982; Hedges and Keil, 1995).”
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“Sedimentary rocks harbor large reservoirs of N, attributable primarily to burial of organic matter in marine sediments (Berner 1982 ).”
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“In bioturbated sediments, both acids (H2CO3, HNO3, H2S, H2SO4) and enhanced pCO2 required for calcium carbonate dissolution are produced by oxidation of organic carbon, by sulfate reduction, denitri®cation from microbial metabolism, and by oxidation of solid sul®des formed during earlier sulfate reductions (Aller, 198…”
BackgroundPrecambrian evolution of the climate system
Walker, J. C. G. (1990) · Global and Planetary Change · doi:10.1016/0921-8181(90)90005-w · Cited by 32
“Instead it is preserved in sediments, principally on the continental shelves and slopes (Berner, 1982), to become a constituent of a long-lived geological reservoir of reduced organic carbon or kerogen.”
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“The sequestration of terrestrial particulate organic carbon (OC) in marine sediments can lead to a drawdown of atmospheric CO2 and thus form a long-term control on carbon dioxide and oxygen levels in Earth’s atmosphere (Berner, 1982; Burdige, 2007; Hilton & West, 2020).”
BackgroundInfluentialKhosronejad, A., Limaye, A. B. S., Zhang, Z., et al. (2023) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2022ms003257 · Cited by 31
“stacking and connectivity of subsurface fluid reservoirs (Gibling, 2006), and influencing global geochemical cycles (Berner, 1982).”
BackgroundInfluentialImpact of Hurricane Katrina (2005) on shelf organic carbon burial and deltaic evolution
Allison, M. A., Dellapenna, T. M., Gordon, E. S., Mitra, S., & Petsch, S. T. (2010) · Geophysical Research Letters · doi:10.1029/2010gl044547 · Cited by 32
“[3] Rivers supply as much as 1 Gt total carbon to the world’s oceans, and as much as 85% of the carbon burial in continental margins takes place on these river‐dominated shelves [Berner, 1982; Bianchi and Allison, 2009].”
BackgroundHuang, K.-M., & Lin, S. (1995) · GEOCHEMICAL JOURNAL · doi:10.2343/geochemj.29.301 · Cited by 31
Schultz, R. B. (2004) · Chemical Geology · doi:10.1016/j.chemgeo.2003.12.011 · Cited by 31
“Thus, the limiting factor in pyrite formation in euxinic sediments is not the Corg content (as in normal marine settings), but the quantity of detrital reactive Fe present (Leventhal, 1983; Berner, 1982).”
BackgroundRushdi, A. I., Al-Shaikh, I. M., El‐Mubarak, A. H., et al. (2017) · Marine Pollution Bulletin · doi:10.1016/j.marpolbul.2017.07.014 · Cited by 31
Hanken, N., Uchman, A., Nielsen, J. K., Olaussen, S., Eggebø, T., & Steinsland, R. (2016) · Ichnos/Ichnos : an international journal for plant and animal traces · doi:10.1080/10420940.2016.1199427 · Cited by 31
“The reducing conditions are established due to the decay of the organic matter and the restricted renewal of oxidative agents (e.g., Goldhaber and Kaplan, 1974; Berner, 1982, 1984, 1985; Shen and Buick, 2004).”
BackgroundInfluentialRiboulleau, A., Spina, A., Vecoli, M., Riquier, L., Quijada, M., Tribovillard, N., & Averbuch, O. (2018) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2018.02.004 · Cited by 30
“The dotted line corresponds to the 1045 relationship observed in “normal marine” shales (Berner, 1982; Berner and Raiswell, 1983).”
BackgroundOcean acidification and hypoxia alter organic carbon fluxes in marine soft sediments
Ravaglioli, C., Bulleri, F., Rühl, S., McCoy, S. J., Findlay, H. S., Widdicombe, S., & Queirós, A. M. (2019) · Global Change Biology · doi:10.1111/gcb.14806 · Cited by 32
“Marine sediments are key for the accumulation and burial of or‐ ganic matter (Berner, 1982; Smith, Bianchi, Allison, Savage, & Galy, 2015).”
BackgroundBoitsov, S., Klungsøyr, J., & Jensen, H. K. B. (2020) · Chemosphere · doi:10.1016/j.chemosphere.2020.126344 · Cited by 30
Sedimentary organic matter preservation: an assessment and speculative synthesis—a comment
Berner, R. A. (1995) · Marine Chemistry · doi:10.1016/0304-4203(95)00010-o · Cited by 30
Self-citationDissolved organic carbon (DOC) fluxes of deep-sea sediments from the Arabian Sea and NE Atlantic
Lahajnar, N., Rixen, T., Gaye, B., Schäfer, P., & Ittekkot, V. (2005) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/j.dsr2.2005.05.006 · Cited by 31
Qiao, J., Bao, H., Huang, D., Li, D., Lee, T., Huang, J., & Kao, S.-J. (2019) · Biogeochemistry · doi:10.1007/s10533-019-00629-7 · Cited by 30
“Riverine transport is the major pathway for the transfer of terrigenous particulate organic carbon (POC) to the ocean (Berner 1982).”
BackgroundEarly diagenesis and trace element accumulation in North American Arctic margin sediments.
Kuzyk, Z., Gobeil, C., Goñi, M., & Macdonald, R. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2016.12.015 · Cited by 28
“…burial in continental margin sediments represent the major sink 57 terms in the oceanic budgets of a number of redox-sensitive trace elements, including Mo, U, and 58 Cd (Berner, 1982; Dunk et al., 2002; McManus et al., 2006; Raiswell et al., 2006; Rosenthal et 59 al., 1995a; Scott et al., 2008).”
BackgroundXi, Z., Tang, S., Lash, G. G., Zhang, B., & Lin, D. (2020) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2020.110173 · Cited by 29
Die Wind-getriebene ?biologische Pumpe? und der Kohlenstoffentzug im Ozean
Haake, B., & Ittekkot, V. (1990) · Die Naturwissenschaften · doi:10.1007/bf01131777 · Cited by 29
Organic Matter in the Contemporary Ocean
Eglinton, T. I., & Repeta, D. J. (2003) · Treatise on Geochemistry · doi:10.1016/b0-08-043751-6/06155-7 · Cited by 29
Measuring the Flow of Energy and Matter in Marine Benthic Animal Populations
van der Meer, J., Heip, C. H. R., Herman, P. M. J., Moens, T., & van Oevelen, D. (2005) · doi:10.1002/9780470995129.ch8 · Cited by 29
Baker, M. L., Hage, S., Talling, P. J., Açıkalın, S., Hilton, R. G., Haghipour, N., Ruffell, S. C., Pope, E., Jacinto, R. S., Clare, M. A., et al. (2024) · Geology · doi:10.1130/g51976.1 · Cited by 34
Jiménez‐Arias, J. L., Morris, E., Rubio-de-Ingles, M.-J., Peralta, G., García‐Robledo, E., Corzo, A., & Papaspyrou, S. (2020) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2020.138205 · Cited by 33
Evaluation of Sedimentary Organic Carbon Reactivity and Burial in the Eastern China Marginal Seas
Guo, J., Yuan, H., Song, J., Li, X., Duan, L., Li, N., & Wang, Y. (2021) · Journal of Geophysical Research Oceans · doi:10.1029/2021jc017207 · Cited by 26
Teske, A., Lizarralde, D., Höfig, T. W., et al. (2021) · Proceedings of the International Ocean Discovery Program. Expedition reports · doi:10.14379/iodp.proc.385.102.2021 · Cited by 28
von Ahn, C. M. E., Scholten, J. C., Malik, C., Feldens, P., Liu, B., Dellwig, O., Jenner, A.-K., Papenmeier, S., Schmiedinger, I., Zeller, M. A., et al. (2021) · Frontiers in Environmental Science · doi:10.3389/fenvs.2021.642346 · Cited by 29
“The composition of sediments investigated in the WB is typical for silty/muddy deposits along the North-German coastline FIGURE 8 | Covariations of TS versus TOC including the relationship suggested for Holocene siliciclastic sediments (Berner, 1982).”
BackgroundInfluentialZhao, H., Ling, K., Qin, S., Lei, M., & Wen, H. (2023) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2023.105409 · Cited by 27
Reduced inorganic sulfur in the sediments of the Yellow Sea and East China Sea
Kang, X., Liu, S., & Zhang, G. (2014) · Acta Oceanologica Sinica · doi:10.1007/s13131-014-0499-1 · Cited by 28
Ku, T. C. W., Kay, J., Browne, E., Martini, A. M., Peters, S. C., & Chen, M. D. (2007) · Marine Geology · doi:10.1016/j.margeo.2007.12.001 · Cited by 28
“…normal marine sediments causes increasing organic carbon burial rates to correspond with increasing sulfate reduction rates and pyrite burial rates and results in relatively constant Corg/Spy weight ratios of 2.8±0.8 (Berner, 1982; Berner and Canfield, 1989; Lin and Morse, 1991; Lin et al., 2002).”
BackgroundMethodInfluentialBiogeochemical applications of compound-specific radiocarbon analysis
Pearson, A. (1999) · doi:10.1575/1912/4083 · Cited by 28
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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