The DOI matches its Crossref record.
Burial of organic carbon and pyrite sulfur in the modern ocean; its geochemical and environmental significance.
Open accessOverview
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
The source backs part of the claim, not all of it — or backs it for a different population, condition or comparison.
In the citing paper
“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
Experimental — accuracy not yet measured
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Citations
Cites
The publisher hasn’t deposited this paper’s reference list.
Research works printed but not linked: 16
- Degens, E. T., and Mopper, K., 1976, Factors controlling the distribution and early diagenesis of organic material in marine sediments, in Riley, J. P., and Chester, R., eds., Chemical Oceanography, v. 6: New York, Academic Press, p. 58-113.
- - 1960, The Šea off Southern California: New York, John Wiley & Sons, 366 p. Emery, K. O., and Niino, H., 1963, Sediments of the Gulf of Thailand and adjacent continental shelf: Geol. Soc. America Bull., v. 74, p. 541-554.
- Freyer, H. D., 1979, Variations in the atmospheric CO2 content, in Bolin, B., Degens, E. T., Kempy, S., and Ketner, P., eds., I'he Global Cycle of Carbon: New York, John Wiley & Sons, p. 79-99.
- Garrels, R. M., and Perry, E. A., 1974, Cycling of carbon, sulfur and oxygen through geologic time, in Goldberg, E. D., ed., The Sea, v. 5: New York, Wiley-Interscience, p. 303-336.
- Goldhaber, M. B., ms, 1974, Equilibrium and dynamic aspects of the marine geochemistry of sulfur: Ph.D. thesis, Univ. California, Los Angeles, 399 p.
- Goldhaber, M. B., and Kaplan, I. R., 1974, The sulfur cycle, in Ġoldberg, E. D., ed., The Sea, v. 5: New York, Wiley-Interscience, p. 569-656.
- Hay, W. W., and Southam, J. R., 1977, Modulation of marine sedimentation by the continental shelves, in Andersen, N. R., and Malahoff, A., eds., The Fate of Fossil Fuel CO2 in the Oceans: New York, Plenum Press, p. 569-604.
- Heath, G. R., Moore, T. C., and Dauphin, J. P., 1977, Organic carbon in deep-sea sediments, in Andersen, N. R., and Malahoff, A., eds., The Fate of Fossil Fuel CO, in the Oceans: New York, Plenum Press, p. 605-625.
- Mackenzie, F. T., 1981, Global carbon cycle: some minor sinks for COg, in Carbon Dioxide Effects Research and Assessment Program Conf. 016, Flux of Organic Carbon by Rivers to the Ocean: Washington, D.C., U.S. Dept. Energy, p. 359-384.
- 1981, River transport of organic carbon to the oceans, in Carbon Dioxide Effects Research and Assessment Program Conf. Vol. 016, Flux of Organic Carbon by Rivers to the Ocean: Washington, D.C., U.S. Dept. Energy, p. 219-269.
- Milliman, J. D., 1974, Marine Carbonates: New York, Springer-Verlag, 375 p.
- Müller, P. J., and Mangini, A., 1980, Organic carbon decomposition rates in sediments of the Pacific manganese nodule belt dated by 2Th/31Pa: Earth Planetary Sci. Letters, v. 51, p. 94-114.
- Reeburgh, W. S., and Heggie, D. T., 1974, Depth distributions of gases in shallow water sediments, in Kaplan, I. R., ed., Naturai Gases in Marine Sediments: New York, Plenum Press, p. 27-45.
- Sweeney, R. E., ms, 1972, Pyritization during diagenesis of marine sediments: Ph.D. thesis, Univ. California, Los Angeles, 184 p.
- Volkov, I. I., Rosanov, A. G., Ivanov, M. V., Lein, A. Y., Grinenko, V. A., and Migdisov, A. A., 1982, Sulfur in the ocean, in The Global Biogeochemical Sulfur Cycle: S.C.O.P.E. publication in press.
- Wollast, R., and Billen, G., 1981, The fate of terrestrial organic carbon in the coastal area, in Carbon Dioxide Effects Research and Assessment Program Conf. Vol. 016, Flux of Organic Carbon by Rivers to the Oceans: Washington, D.C., U.S. Dept. Energy, p. 331-359.
Cited by
Sorted by citations
Items 201–300 of 1,000
Aller, R. C., & Blair, N. E. (2004) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2003.10.028 · Cited by 138
Sedimentary features and processes in the Nazaré and Setúbal submarine canyons, west Iberian margin
Arzola, R. G., Wynn, R. B., Lastras, G., Masson, D. G., & Weaver, P. P. E. (2008) · Marine Geology · doi:10.1016/j.margeo.2007.12.006 · Cited by 134
Rapid Variability of Seawater Chemistry Over the Past 130 Million Years
Wortmann, U. G., & Paytan, A. (2012) · Science · doi:10.1126/science.1220656 · Cited by 133
Hansen, K. W. (2003) · American Journal of Science · doi:10.2475/ajs.303.2.94 · Cited by 130
Aller, R. C., Heilbrun, C., Panzeca, C., Zhu, Z., & Baltzer, F. (2004) · Marine Geology · doi:10.1016/j.margeo.2004.04.027 · Cited by 134
Bolton, E. W., Berner, R. A., & Petsch, S. T. (2006) · American Journal of Science · doi:10.2475/08.2006.01 · Cited by 126
Self-citationThe impact of mobile demersal fishing on carbon storage in seabed sediments
Epstein, G., Middelburg, J. J., Hawkins, J. P., Norris, C. R., & Roberts, C. M. (2022) · Global Change Biology · doi:10.1111/gcb.16105 · Cited by 154
Goldsmith, S. T., Carey, A. E., Lyons, W. B., Kao, S.-J., Lee, T.-Y., & Chen, J. (2008) · Geology · doi:10.1130/g24624a.1 · Cited by 128
Demineralization of marine and freshwater sediments for CP/MAS 13C NMR analysis
Gélinas, Y., Baldock, J., & Hedges, J. I. (2001) · Organic Geochemistry · doi:10.1016/s0146-6380(01)00018-3 · Cited by 127
Wind-induced bottom sediment resuspension in a microtidal coastal environment
Booth, J. G., Miller, R. L., McKee, B. A., et al. (2000) · Continental Shelf Research · doi:10.1016/s0278-4343(00)00002-9 · Cited by 127
“Coastal sedimentary deposits are a focal site for the biogeochemical transformation of many elements and their study is critical in understanding oceanic elemental mass balances and residence times (Holland, 1978; Berner, 1982; Martin and Windom, 1991).”
BackgroundDirect Microbial Reduction and Subsequent Preservation of Uranium in Natural Near-Surface Sediment
Suzuki, Y., Kelly, S. D., Kemner, K., & Banfield, J. F. (2005) · Applied and Environmental Microbiology · doi:10.1128/aem.71.4.1790-1797.2005 · Cited by 126
“Although the salinity of the P4 water is obviously different from that of ocean water, the terminal electron-accepting processes and TOC content in P4 are similar to those in typical marine sediments (4).”
BackgroundRecent organic carbon sequestration in the shelf sediments of the Bohai Sea and Yellow Sea, China
Hu, L., Shi, X., Bai, Y., et al. (2015) · Journal of Marine Systems · doi:10.1016/j.jmarsys.2015.10.018 · Cited by 125
Riedinger, N., Brunner, B., Krastel, S., Arnold, G. L., Wehrmann, L. M., Formolo, M. J., Beck, A., Bates, S. M., Henkel, S., Kasten, S., et al. (2017) · Frontiers in Earth Science · doi:10.3389/feart.2017.00033 · Cited by 127
“In most continental margin sediments, pyrite is the most abundant iron sulfide species (e.g., Goldhaber and Kaplan, 1975; Cornwell and Morse, 1987; Morse and Cornwell, 1987) and a long-term sink for sulfur (Berner, 1982, 1989; Berner and Raiswell, 1983).”
BackgroundSedimentary processes on the Amazon continental shelf: past, present and future research
Nittrouer, C. A., & DeMaster, D. J. (1986) · Continental Shelf Research · doi:10.1016/0278-4343(86)90051-8 · Cited by 125
Hudson, R. J. M., Gherini, S. A., & Goldstein, R. A. (1994) · Global Biogeochemical Cycles · doi:10.1029/94gb01044 · Cited by 124
Sperling, E. A., & Stockey, R. G. (2018) · Integrative and Comparative Biology · doi:10.1093/icb/icy088 · Cited by 122
He, B., Dai, M., Huang, W., Liu, Q., Chen, H., & Xu, L. (2010) · Biogeosciences · doi:10.5194/bg-7-3343-2010 · Cited by 122
“1) Although there have been abundant researches that have attempted to tackle such questions related to the sources and fate of organic matter in coastal environments (Berner, 1982; Goni et al., 1997; Gordon and Goni, 2004; Hedges et al., 1986; Hedges and Parker, 1976; Kuwae et al., 2007; Ramaswamy et al., 2008), our…”
BackgroundGoldhaber, M. B. (2003) · Elsevier eBooks · doi:10.1016/b0-08-043751-6/07139-5 · Cited by 137
López‐Chicano, M., Bouamama, M., Vallejos, Á., et al. (2001) · Applied Geochemistry · doi:10.1016/s0883-2927(01)00012-9 · Cited by 123
Recent sediment transport and accumulation on the NW Iberian margin
van Weering, T. C. E., de Stigter, H., Boer, W., et al. (2002) · Progress In Oceanography · doi:10.1016/s0079-6611(02)00015-0 · Cited by 123
Goñi, M. A., Hatten, J. A., Wheatcroft, R. A., & Borgeld, J. C. (2013) · Journal of Geophysical Research Biogeosciences · doi:10.1002/jgrg.20024 · Cited by 120
“Because most organic matter burial occurs along continental and insular margins with significant sediment supply [e.g., Berner, 1982; Hedges, 1992], small mountainous rivers are likely to play an important role in this major long-term carbon sink [e.g., Dunne et al., 2007].”
BackgroundKeil, R. G., & Hedges, J. I. (1993) · Chemical Geology · doi:10.1016/0009-2541(93)90215-5 · Cited by 122
Jahnke, R. A., & Jahnke, D. B. (2000) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/s0967-0637(99)00118-1 · Cited by 121
“Eppley and Peterson, 1979; Antoine et al., 1996); relatively high e$ciency of vertical transport of organic matter (Lampitt and Antia, 1997; Lee et al., 1998); augmentation of vertical #uxes by lateral transport (Jahnke et al., 1990); high deposition and remineralization rates (Jahnke, 1996; Jahnke and Shimmield, 1995…”
BackgroundSulfur and iron speciation in surface sediments along the northwestern margin of the Black Sea
Wijsman, J. W. M., Middelburg, J. J., Herman, P. M. J., Böttcher, M. E., & Heip, C. H. R. (2001) · Marine Chemistry · doi:10.1016/s0304-4203(01)00019-6 · Cited by 122
“PII: S0304-4203 01 00019-6 and are important sites for the formation and burial Žof authigenic iron sulfides Berner, 1982; Jørgensen, .1982; Lin and Morse, 1991 .”
BackgroundTesi, T., Miserocchi, S., Goñi, M. A., et al. (2007) · Marine Chemistry · doi:10.1016/j.marchem.2007.01.005 · Cited by 122
“, 2005), which is buried in low energy regions with relative efficiency (Berner, 1982).”
BackgroundGlobal biogeochemical cycle of boron
Park, H., & Schlesinger, W. H. (2002) · Global Biogeochemical Cycles · doi:10.1029/2001gb001766 · Cited by 122
“If 0.157 1015 g C/yr represents the net incorporation of organic carbon into oceanic sediments [Berner, 1982], then the estimated boron deposition in organic sediments will be about 0.014 Tg B/yr.”
BackgroundInfluentialSubstantial iron sequestration during green-clay authigenesis in modern deep-sea sediments
Baldermann, A., Warr, L. N., Letofsky‐Papst, I., & Mavromatis, V. (2015) · Nature Geoscience · doi:10.1038/ngeo2542 · Cited by 124
Mercury Fluxes at the Ocean Margins
Cossa, D., Coquery, M., Gobeil, C., et al. (1996) · Springer eBooks · doi:10.1007/978-94-009-1780-4_11 · Cited by 120
Carbon pools and fluxes in the China Seas and adjacent oceans
Jiao, N., Liang, Y., Zhang, Y., Liu, J., Zhang, Y., Zhang, R., Zhao, M., Dai, M., Zhai, W., Gao, K., et al. (2018) · Science China Earth Sciences · doi:10.1007/s11430-018-9190-x · Cited by 121
Aller, R. C., Blair, N. E., & Brunskill, G. J. (2008) · Journal of Geophysical Research Atmospheres · doi:10.1029/2006jf000689 · Cited by 122
“[2] Deltaic systems are widely recognized as the major storage sites for inorganic sedimentary debris and organic carbon along continental boundaries [Berner, 1982; Hedges and Keil, 1995; Burdige, 2007].”
Leithold, E. L., & Hope, R. S. (1999) · Marine Geology · doi:10.1016/s0025-3227(98)00112-1 · Cited by 117
Nature of decadal-scale sediment accumulation on the western shelf of the Mississippi River delta
Corbett, D. R., McKee, B. A., & Allison, M. A. (2006) · Continental Shelf Research · doi:10.1016/j.csr.2006.07.012 · Cited by 116
Terrestrial feedback in atmospheric oxygen regulation by fire and phosphorus
Kump, L. R. (1988) · Nature · doi:10.1038/335152a0 · Cited by 115
Organic carbon burial in fjords: Terrestrial versus marine inputs
Cui, X., Bianchi, T. S., Savage, C., et al. (2016) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2016.07.003 · Cited by 115
“2), preservation efficiency of 80% is applied for long term OC burial (104–105 yrs), as suggested by Berner (1982), Hedges and Keil (1995) and Smith et al. (2015).”
BackgroundGoñi, M. A., Monacci, N., Gisewhite, R. A., Ogston, A. S., Crockett, J. S., & Nittrouer, C. A. (2006) · Estuarine Coastal and Shelf Science · doi:10.1016/j.ecss.2006.04.012 · Cited by 120
Stephens, M. P., Kadko, D., Smith, C. R., & Latasa, M. (1997) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(97)00358-x · Cited by 115
Mars Sedimentary Geology: Key Concepts and Outstanding Questions
Grotzinger, J., Beaty, D., Dromart, G., Gupta, S., Harris, M., Hurowitz, J., Kocurek, G., McLennan, S., Milliken, R., Ori, G., et al. (2011) · Astrobiology · doi:10.1089/ast.2010.0571 · Cited by 113
“…would be to seek evidence of sedimentary environments—the preferred geological setting for study—that may have elevated concentrations of biologically derived carbonaceous materials (Berner, 1982), as well as morphologic textures suggestive of former microbial processes (Cady et al., 2003).”
Organic carbon production, mineralisation and preservation on the Peruvian margin
Dale, A. W., Sommer, S., Lomnitz, U., Montès, I., Treude, T., Liebetrau, V., Gier, J., Hensen, C., Dengler, M., Stolpovsky, K., et al. (2015) · Biogeosciences · doi:10.5194/bg-12-1537-2015 · Cited by 116
“Burial of organic carbon represents a net removal of carbon dioxide from the atmosphere and a source of atmospheric oxygen (Berner, 1982).”
BackgroundImportance of tropical coastal environments
Nittrouer, C. A., Brunskill, G. J., & de Figueiredo, A. G., Jr. (1995) · Geo-Marine Letters · doi:10.1007/bf01204452 · Cited by 114
Mollenhauer, G., Schneider, R. R., Müller, P., et al. (2002) · Global Biogeochemical Cycles · doi:10.1029/2001gb001488 · Cited by 113
“The calculated budgets show that organic carbon accumulation in the Benguela area is larger compared to other ocean areas [cf. Berner, 1982] indicating that upwelling systems account for a significant fraction of global organic carbon burial.”
BackgroundResultCalvert, S. E., Thode, H. G., Yeung, D., & Karlin, R. E. (1996) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(96)00020-8 · Cited by 114
Cenozoic evolution of the sulfur cycle: Insight from oxygen isotopes in marine sulfate
Turchyn, A. V., & Schrag, D. P. (2005) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2005.11.007 · Cited by 113
“(c) Rough drawing of modern organic matter distribution (taken from [55,56]).”
BackgroundBiogeochemical response of tropical coastal systems to present and past environmental change
Jennerjahn, T. C. (2012) · Earth-Science Reviews · doi:10.1016/j.earscirev.2012.04.005 · Cited by 115
Climate regulates the erosional carbon export from the terrestrial biosphere
Hilton, R. G. (2016) · Geomorphology · doi:10.1016/j.geomorph.2016.03.028 · Cited by 118
“…by rivers and its delivery to 45 sedimentary environments acts as a major pathway of atmospheric CO2 drawdown and source of 46 atmospheric O2 (Berner, 1982; Derry and France-Lanord, 1996; France-Lanord and Derry, 1997) 47 together with marine organic carbon burial (Hayes et al., 1999;…”
BackgroundFernandes, M. B., & Sicre, M. (2000) · Organic Geochemistry · doi:10.1016/s0146-6380(00)00006-1 · Cited by 112
“%) calculated for world rivers by Berner (1982).”
BackgroundWatanabe, Y., Naraoka, H., Wronkiewicz, D. J., Condie, K. C., & Ohmoto, H. (1997) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(97)00164-6 · Cited by 111
Timescales of Oxygenation Following the Evolution of Oxygenic Photosynthesis
Ward, L. M., Kirschvink, J. L., & Fischer, W. W. (2015) · Origins of Life and Evolution of Biospheres · doi:10.1007/s11084-015-9460-3 · Cited by 112
“Burial of organic carbon is assumed to be a similar fraction of primary productivity to the modern, based on Berner (1982), of about 0.32 %.”
BackgroundInfluentialLate Archean euxinic conditions before the rise of atmospheric oxygen
Scott, C. T., Bekker, A., Reinhard, C. T., Schnetger, B., Krapež, B., Rumble, D., & Lyons, T. W. (2011) · Geology · doi:10.1130/g31571.1 · Cited by 109
Spatial distribution patterns of benthic microbial communities along the Pearl Estuary, China
Liu, J., Yang, H., Zhao, M., & Zhang, X. (2014) · Systematic and Applied Microbiology · doi:10.1016/j.syapm.2014.10.005 · Cited by 113
Trace sulfate in mid-Proterozoic carbonates and the sulfur isotope record of biospheric evolution
Gellatly, A. M., & Lyons, T. W. (2005) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2005.01.019 · Cited by 110
Li, X., Bianchi, T. S., Allison, M. A., et al. (2012) · Marine Chemistry · doi:10.1016/j.marchem.2012.10.001 · Cited by 109
Ittekkot, V. (1993) · Global and Planetary Change · doi:10.1016/0921-8181(93)90060-2 · Cited by 108
Wheatcroft, R. A., Goñ, M. A., Hatten, J. A., Pasternack, G. B., & Warrick, J. A. (2009) · Limnology and Oceanography · doi:10.4319/lo.2010.55.1.0161 · Cited by 108
“Sequestration of POC in marine sediments is a major longterm sink of CO2 and a net source of oxygen over millennial time scales (Berner 1982; Ludwig et al. 1998).”
BackgroundGardner, J. V., Dean, W. E., & Dartnell, P. (1997) · Paleoceanography · doi:10.1029/96pa03567 · Cited by 108
Hilton, R. G., Galy, Α., Hovius, N., Kao, S., Horng, M., & Chen, H. (2012) · Global Biogeochemical Cycles · doi:10.1029/2012gb004314 · Cited by 107
“[31] The erosion and export of POCnon-fossil by mountain rivers represents a lateral flux of recently fixed atmospheric CO2 and its fate is important for our understanding of the global carbon cycle [Berner, 1982; Hayes et al., 1999].”
BackgroundLarge-scale ocean deoxygenation during the Paleocene-Eocene Thermal Maximum
Yao, W., Paytan, A., & Wortmann, U. G. (2018) · Science · doi:10.1126/science.aar8658 · Cited by 105
Provenance, concentrations and nature of sedimentary organic nitrogen in the gulf of Maine
Mayer, L. M., Macko, S. A., & Cammen, L. M. (1988) · Marine Chemistry · doi:10.1016/0304-4203(88)90056-4 · Cited by 105
Kendall, M. M., Wardlaw, G. D., Tang, C. F., et al. (2006) · Applied and Environmental Microbiology · doi:10.1128/aem.01154-06 · Cited by 105
Seasonal variability and geochemical significance of organic matter in the River Ganges, Bangladesh
Ittekkot, V., Safiullah, S., Mycke, B., et al. (1985) · Nature · doi:10.1038/317800a0 · Cited by 103
Hu, Y., Feng, D., Liang, Q., Xia, Z., Chen, L., & Chen, D. (2015) · Deep Sea Research Part II Topical Studies in Oceanography · doi:10.1016/j.dsr2.2015.06.012 · Cited by 102
Rates and mechanisms of shoreface progradation and retreat downdrift of the Amazon river mouth
Allison, M. A., Nittrouer, C. A., & Faria, L. E. C. (1995) · Marine Geology · doi:10.1016/0025-3227(95)00020-y · Cited by 103
The potential storage of carbon caused by eutrophication of the biosphere
Peterson, B. J., & Melillo, J. M. (1985) · Tellus B · doi:10.3402/tellusb.v37i3.15006 · Cited by 127
Sediment texture, distribution and transport on the Ayeyarwady continental shelf, Andaman Sea
Rao, P. S., Ramaswamy, V., & Thwin, S. (2005) · Marine Geology · doi:10.1016/j.margeo.2005.02.016 · Cited by 102
Mayer, L. M., Schick, L. L., Allison, M. A., et al. (2007) · Marine Chemistry · doi:10.1016/j.marchem.2007.07.007 · Cited by 102
“Most burial of organic matter in the ocean occurs on continental shelves and upper slopes ( Berner, 1982; Hedges and Keil, 1995).”
BackgroundInfluentialSedimentary organic matter preservation: an assessment and speculative synthesis—a comment
Henrichs, S. M. (1995) · Marine Chemistry · doi:10.1016/0304-4203(95)00012-g · Cited by 102
Relationships between sulphur, organic carbon, and iron in the modern sediments of the Black Sea
Calvert, S. E., & Karlin, R. E. (1991) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(91)90367-e · Cited by 98
Global geochemical cycles of carbon, sulfur and oxygen
Walker, J. C. G. (1986) · Marine Geology · doi:10.1016/0025-3227(86)90093-9 · Cited by 98
“High concentrations of organic carbon in sediments generally correspond to high concentrations of sulfide 4 Z z cr" o z RECENT MARINE / SEDIMENTS )~/ {e g BERNER, 1982 / / xX x / x ATLANTIC x x AVERAGE x (BRUMSACK AND LEW) I i 2 SULFUR % Fig.9.”
BackgroundInfluentialTyson, R. V. (1996) · Geological Society London Special Publications · doi:10.1144/gsl.sp.1996.103.01.06 · Cited by 97
Giosan, L., Flood, R. D., & Aller, R. C. (2002) · Marine Geology · doi:10.1016/s0025-3227(02)00321-3 · Cited by 97
Terrestrial plant biopolymers in marine sediments
Gough, M. A., Fauzi, R., Mantoura, C., & Preston, M. R. (1993) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(93)90032-r · Cited by 96
“BERNER R. A. ( 1982) Burial of organic carbon and pyrite sulfur in the modern ocean: Its geochemical and environmental significance.”
BackgroundWard, N. D., Krusche, A. V., Sawakuchi, H. O., Brito, D. C., da Cunha, A. C., de Moura, J. M. S., da SILVA, R., Yager, P. L., Keil, R. G., & Richey, J. E. (2015) · Marine Chemistry · doi:10.1016/j.marchem.2015.06.013 · Cited by 103
Pyritization: a palaeoenvironmental and redox proxy reevaluated
Roychoudhury, A. N., Kostka, J. E., & Cappellen, P. V. (2003) · Estuarine Coastal and Shelf Science · doi:10.1016/s0272-7714(03)00058-1 · Cited by 98
“The notion of stability of pyrite, and the fact that most marine sediments and sedimentary rocks contain at least traces of pyrite (Berner, 1982), has resulted in the formation of pyrite being widely used as a proxy to identify a variety of redox controlled cyclic transitions and depositional…”
BackgroundInfluentialTerrigenous organic matter in sediments from the Fly River delta‐clinoform system (Papua New Guinea)
Goñi, M. A., Monacci, N., Gisewhite, R. A., Crockett, J. S., Nittrouer, C. A., Ogston, A. S., Alin, S. R., & Aalto, R. E. (2008) · Journal of Geophysical Research Atmospheres · doi:10.1029/2006jf000653 · Cited by 97
“Elevated inputs of recalcitrant organic matter (OM) and high mass accumulation rates make these systems some of the most significant sites of carbon burial in the present-day ocean [e.g., Berner, 1982; Hedges and Keil, 1995].”
Direct measurement of riverine particulate organic carbon age structure
Rosenheim, B. E., & Galy, V. (2012) · Geophysical Research Letters · doi:10.1029/2012gl052883 · Cited by 97
“…the ratio of recent OCbiosph to OCpetro transported to marine ecosystems and depositional centers by rivers, as well as changes in this ratio through time, are important in determining the accumulation of dioxygen (O2) and carbon dioxide (CO2) in the atmosphere over Earth’s history [Berner, 1982].”
BackgroundZhang, Y., Yao, P., Sun, C., Li, S., Shi, X., Zhang, X., & Liu, J. (2021) · Molecular Ecology · doi:10.1111/mec.15937 · Cited by 93
“Their metabolic activities profoundly impact the biogeochemical cycles of carbon, nitrogen and sulphur on a global scale (Berner, 1982; Nealson, 1997; Orcutt et al., 2011).”
BackgroundBralower, T. J., & Thierstein, H. R. (1987) · Geological Society London Special Publications · doi:10.1144/gsl.sp.1987.026.01.23 · Cited by 96
Anthropogenic disturbance keeps the coastal seafloor biogeochemistry in a transient state
van de Velde, S., Lancker, V. R. M. V., Hidalgo‐Martinez, S., Berelson, W. M., & Meysman, F. J. R. (2018) · Scientific Reports · doi:10.1038/s41598-018-23925-y · Cited by 112
Runoff-driven export of particulate organic carbon from soil in temperate forested uplands
Smith, J. C., Galy, Α., Hovius, N., et al. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.01.027 · Cited by 94
“It is particularly important to distinguish between carbon from fossil and non-fossil sources, because re-burial of fossil carbon has no effect on contemporary CO2 drawdown, while burial of nonfossil carbon bypasses the usual rapid oxidation pathway and sequesters carbon (Berner, 1982).”
BackgroundSato, H., Hayashi, K., Ogawa, Y., & Kawamura, K. (2012) · Marine Geology · doi:10.1016/j.margeo.2012.07.013 · Cited by 93
Watershed control on the carbon loading of marine sedimentary particles
Leithold, E. L., & Blair, N. E. (2001) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(01)00593-2 · Cited by 93
İnan, S., Yalçın, M. N., Guliev, I. S., Kuliev, K., & Feizullayev, A. A. (1997) · Marine and Petroleum Geology · doi:10.1016/s0264-8172(97)00058-5 · Cited by 93
Allison, M. A., Bianchi, T. S., McKee, B. A., et al. (2007) · Geophysical Research Letters · doi:10.1029/2006gl028362 · Cited by 93
“…to continental margins are also important loci for carbon production, remineralization and burial (continental margins are the site for 80–85% of global carbon burial [Berner, 1982; Hedges and Keil, 1997]), although their net effect on the global carbon budget remains unresolved [McKee, 2003].”
BackgroundMarchio, D., Savarese, M., Bovard, B. D., & Mitsch, W. J. (2016) · Forests · doi:10.3390/f7060116 · Cited by 94
“Early estimates of organic carbon burial in mangrove ecosystems suggest they account for 15% of the total organic carbon annually sequestered in marine sediments [17,18].”
BackgroundMississippi River subaqueous delta is entering a stage of retrogradation
Maloney, J. M., Bentley, S. J., Xu, K., et al. (2018) · Marine Geology · doi:10.1016/j.margeo.2018.03.001 · Cited by 92
“It is estimated that carbon burial on continental margins amounts to 80–85% of the global total (Berner, 1982; Hedges and Keil, 1997).”
BackgroundNutrient cycling in tropical and temperate coastal waters: Is latitude making a difference?
Lønborg, C., Müller, M., Butler, E. C. V., Jiang, S., Ooi, S. K., Trinh, D. H., Wong, P. Y., Ali, S. M., Chun, C., Wee, B. S., et al. (2021) · Estuarine Coastal and Shelf Science · doi:10.1016/j.ecss.2021.107571 · Cited by 92
“This contradicts the paradigm that coastal systems are the primary storage reservoirs for organic matter and most terrestrial weathering products (Berner, 1982).”
BackgroundDistribution and composition of organic matter in surface sediments of coastal Southeast Alaska
Walinsky, S. E., Prahl, F. G., Mix, A. C., Finney, B. P., Jaeger, J. M., & Rosen, G. P. (2009) · Continental Shelf Research · doi:10.1016/j.csr.2009.04.006 · Cited by 91
“Although small in area, continental margins account for 480% of the estimated 130 10 g of total organic carbon (TOC) buried globally each year in the marine environment (Berner, 1982). The quantity and quality of TOC buried in continental margin sediments varies widely. For example, Niggemann et al. (2007) studied two…”
BackgroundLim, Y. C., Lin, S., Yang, T. F., et al. (2011) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2011.04.004 · Cited by 92
Fluxes of amino acids and hexosamines to the deep Arabian Sea
Haake, B., Ittekkot, V., Ramaswamy, V., et al. (1992) · Marine Chemistry · doi:10.1016/0304-4203(92)90028-9 · Cited by 92
Glenn, C. R., & Arthur, M. A. (1985) · Chemical Geology · doi:10.1016/0009-2541(85)90057-9 · Cited by 92
Pelagic Sedimentation in Modern and Ancient Oceans
Hüneke, H., & Henrich, R. (2010) · Developments in sedimentology · doi:10.1016/b978-0-444-53000-4.00004-4 · Cited by 95
The potential storage of carbon caused by eutrophication of the biosphere
Peterson, B. J., & Melillo, J. M. (1985) · Tellus B · doi:10.1111/j.1600-0889.1985.tb00060.x · Cited by 91
Megathrust earthquake drives drastic organic carbon supply to the hadal trench.
Kioka, A., Schwestermann, T., Moernaut, J., Ikehara, K., Kanamatsu, T., McHugh, C. M., dos Santos Ferreira, C., Wiemer, G., Haghipour, N., Kopf, A. J., et al. (2019) · Scientific Reports · doi:10.1038/s41598-019-38834-x · Cited by 84
Kalaitzidis, S. P., Siavalas, G., SKARPELIS, N., Araujo, C. V., & Christanis, K. (2009) · International Journal of Coal Geology · doi:10.1016/j.coal.2009.06.005 · Cited by 90
Neogene burial of organic carbon in the global ocean
Li, Z., Zhang, Y., Torres, M. A., & Mills, B. J. W. (2023) · Nature · doi:10.1038/s41586-022-05413-6 · Cited by 94
Efficient preservation of young terrestrial organic carbon in sandy turbidity-current deposits
Hage, S., Galy, V., Cartigny, M., Açıkalın, S., Clare, M. A., Gröcke, D. R., Hilton, R. G., Hunt, J. E., Lintern, G., McGhee, C., et al. (2020) · Geology · doi:10.1130/g47320.1 · Cited by 85
Sampei, Y., Matsumoto, E., KAMEI, T., et al. (1997) · GEOCHEMICAL JOURNAL · doi:10.2343/geochemj.31.245 · Cited by 88
Cai, W., Wiebe, W. J., Wang, Y., et al. (2000) · Limnology and Oceanography · doi:10.4319/lo.2000.45.8.1743 · Cited by 88
“3C), which suggests significant anaerobic degradation (SO4 reduction) of organic matter (Berner 1982).”
BackgroundHydrological controls on marine chemistry in the Cryogenian Nanhua Basin (South China)
Cheng, M., Zhang, Z., Algeo, T. J., Liu, S., Liu, X., Wang, H., Chang, B., Jin, C., Pan, W., Cao, M., et al. (2021) · Earth-Science Reviews · doi:10.1016/j.earscirev.2021.103678 · Cited by 90
Aller, R. C., Hannides, A. K., Heilbrun, C., et al. (2004) · Continental Shelf Research · doi:10.1016/j.csr.2004.07.018 · Cited by 87
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
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review