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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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Huang, W., Yang, H., He, S., Zhao, B., & Cui, X. (2023) · Marine Chemistry · doi:10.1016/j.marchem.2023.104326 · Cited by 13
Ruban, A., Tesi, T., Ярощук, Е. И., Kosmach, D. A., Rudmin, M. A., Гершелис, Е. В., Dudarev, O., Mazurov, A. K., & Semiletov, I. (2023) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2023.106638 · Cited by 12
Miao, X., Oppo, D., Wei, J., Lin, Z.-Y., Liu, X.-T., Wu, T., Yu, X., Wu, K., & Li, J.-R. (2024) · Chemical Geology · doi:10.1016/j.chemgeo.2024.122262 · Cited by 11
Devereux, R., Lehrter, J. C., Cicchetti, G., Beddick, D. L., Yates, D. F., Jarvis, B. M., Aukamp, J., & Hoglund, M. D. (2019) · Biogeochemistry · doi:10.1007/s10533-019-00539-8 · Cited by 12
“Principally, deep water sediments have low OM deposition rates and hence low oxygen demand (Berner 1982) and, on the LCS, infrequent physical mixing from storms (Chen et al. 2005).”
BackgroundRatnayake, A. S. (2021) · Geo-Marine Letters · doi:10.1007/s00367-021-00710-x · Cited by 12
“TOC to TS relationship (C/S ratio) is an indicator of depositional processes such as sulfate reduction, Fe-S cycling, paleosalinity, and early diagenesis (e.g., Berner 1982, 1984; Meyers and Ishiwatari 1993; Sampei et al.”
BackgroundOzaki, K., Cole, D. B., Reinhard, C. T., & Tajika, E. (2022) · Geoscientific model development · doi:10.5194/gmd-15-7593-2022 · Cited by 14
“This is somewhat higher than previous estimates (Berner, 1982; Burdige, 2005; Muller-Karger et al., 2005), but given the rather large uncertainty we consider it defensible.”
ResultThe Holocene climatic optimum in Korea: Evidence from wetland records
Nahm, W., Kim, J. K., Kim, J. K., et al. (2013) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2013.02.033 · Cited by 12
Chen, K., Zhu, M., Yang, G., et al. (2014) · Marine Pollution Bulletin · doi:10.1016/j.marpolbul.2014.08.029 · Cited by 12
“Pyrite formation is commonly limited by the availability of labile organic matter (OM) in marine sediments (Berner, 1982; Burdige, 2006).”
BackgroundTrophic and tectonic limits to the global increase of marine invertebrate diversity
Cermeño, P., Benton, M. J., Paz, Ó., & Vérard, C. (2017) · Scientific Reports · doi:10.1038/s41598-017-16257-w · Cited by 12
Enhancement of cyanobacterial growth by riverine particulate material
Grimm, C., Martinez, R. E., Сергеевич, П. О., Benning, L. G., & Oelkers, É. H. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.06.012 · Cited by 12
“Burial of organic matter is required for the long-term 51 drawdown of CO2 via the ‘organic pathway’ because it prevents organic matter 52 decomposition and thus the return of CO2 to the atmosphere (Berner, 1982; Falkowski et al., 53 1998; Jeandel and Oelkers, 2015).”
BackgroundYang, J., Paytan, A., Yang, Y., Wei, S., Liu, B., Cui, H., Chen, Y., & Zhao, Y. (2020) · Journal of Marine Systems · doi:10.1016/j.jmarsys.2020.103415 · Cited by 12
Bioturbation has a limited effect on phosphorus burial in salt marsh sediments
van de Velde, S., James, R. K., Callebaut, I., Hidalgo‐Martinez, S., & Meysman, F. J. R. (2021) · Biogeosciences · doi:10.5194/bg-18-1451-2021 · Cited by 12
Laarkamp, K. L. (2000) · doi:10.1575/1912/4103 · Cited by 12
“Coastal sites are important in the total burial of organic material (Berner, 1982) and phosphorus (Ruttenberg, 1993; Ruttenberg & Berner, 1993) in oceanic sediments.”
BackgroundDiagenesis of sediments beneath the Ross Ice Shelf and their sedimentary history
Raiswell, R., & Tan, M. (1985) · Nature · doi:10.1038/315483a0 · Cited by 12
Sources of organic matter to surficial sediments from the Scotian Shelf and Slope, Canada
Pocklington, R., Leonard, J. D., & Crewe, N. F. (1991) · Continental Shelf Research · doi:10.1016/0278-4343(91)90091-j · Cited by 12
Johnston, D. T., & Fischer, W. W. (2012) · Wiley eBooks · doi:10.1002/9781118280874.ch14 · Cited by 12
“Exact values for these fluxes are challenging to pin down (e.g. Alt and Shanks, 2003; Strauss, 1999; Holser et al., 1979; Walker, 1986), but are generally of the same order as the inputs and yield a similar estimate of residence time (Berner 1982, McDuff and Edmond 1982, Paytan et al.”
ResultNN-TOC v1: global prediction of total organic carbon in marine sediments using deep neural networks
Parameswaran, N., González, E., Burwicz, E., Braack, M., & Wallmann, K. (2025) · Geoscientific model development · doi:10.5194/gmd-18-2521-2025 · Cited by 17
“3 are also consistent with the early work on TOC distributions by Berner (1982) and Emerson and Hedges (1988), showing low TOC values in the open oceans and elevated values for upwelling regions and the Arctic region.”
Shelf and slope sedimentation associated with large deltaic systems
Walsh, J. P., Corbett, D. R., Ogston, A. S., et al. (2013) · Cambridge University Press eBooks · doi:10.1017/cbo9781139136853.007 · Cited by 11
Acharya, S. S., & Panigrahi, M. K. (2016) · Continental Shelf Research · doi:10.1016/j.csr.2016.08.001 · Cited by 11
Dummann, W., Schröder-Adams, C. J., Hofmann, P., Rethemeyer, J., & Herrle, J. O. (2021) · Geosphere · doi:10.1130/ges02335.1 · Cited by 11
Huang, Y., Cheng, J., Wang, M., et al. (2022) · Frontiers in Earth Science · doi:10.3389/feart.2022.876913 · Cited by 11
“In the typically anoxic subseafloor marine sediments, the consumption of porewater sulfate is controlled by two microbially mediated processes: 1) organo clastic sulfate reduction (OSR) (Berner, 1982); and 2) anaerobic oxidation of methane (AOM) (Boetius et al., 2000).”
BackgroundInfluentialSediment Organic Carbon in Todos Santos Bay, Baja California, Mexico
Smith, S. V., Ibarra-Obando, S. E., Díaz‐Castañeda, V., et al. (2008) · Estuaries and Coasts · doi:10.1007/s12237-008-9054-7 · Cited by 11
“16 Gt year, about 27% higher than previously estimated by Berner (1982); these authors agree that about 95% of OC burial occurs on deltas, other shelf areas, and the upper slope. The burial represents about 40% of river OC delivery, with the difference between delivery and burial interpreted to represent an excess of…”
BackgroundInfluentialNot to be Sneezed at: Does Pollen from Forests of Exotic Pine Affect Deep Oceanic Trench Ecosystems?
Leduc, D., & Rowden, A. A. (2017) · Ecosystems · doi:10.1007/s10021-017-0146-8 · Cited by 11
Methane seep in the Shenhu area of the South China sea using geochemical and mineralogical features
Zhang, Q., Wu, D., Jin, G., Xu, X., Yang, C., & Liu, L. (2022) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2022.105829 · Cited by 11
Yang, S., Yang, Q., Liu, S., et al. (2015) · Acta Oceanologica Sinica · doi:10.1007/s13131-015-0723-7 · Cited by 11
“…author, E-mail: sunyao@ysfri.ac.cn duction, besides about 90% organic carbon buried in global ocean sediments concentrated in marginal sea and for inorganic carbon the percentage was over 50% (Berner, 1982; Hedges and Keil, 1995; Falkowski et al., 2000; Tesi et al., 2007; Song et al., 2011).”
BackgroundPetrology of the Desmoinesian Excello Black Shale of the Midcontinent Region of the United States
Ece, O. I. (1987) · Clays and Clay Minerals · doi:10.1346/ccmn.1987.0350403 · Cited by 11
Processes of Holocene ferromanganese-coated grains (oncolites) in the nearshore shelf of Cameroon
Giressè, P., Wiewióra, A., & Lacka, B. (1998) · Journal of Sedimentary Research · doi:10.2110/jsr.68.20 · Cited by 11
Analytical phosphorus fractionation of sediment trap material
Liebezeit, G. (1991) · Marine Chemistry · doi:10.1016/0304-4203(91)90057-4 · Cited by 11
Rasiq, K. T., Kurian, S., Karapurkar, S. G., & Naqvi, S. W. A. (2016) · Estuarine Coastal and Shelf Science · doi:10.1016/j.ecss.2016.04.013 · Cited by 11
“2 1-Introduction Oxygen Minimum Zones (OMZ) are important in terms of organic matter (OM) accumulation, preservation (Schulte et al., 2000) and burial as well as benthic solute fluxes (Berner, 1982; Walsh, 1991; Hedges and Keil, 1995; Woulds and Cowie, 2009).”
BackgroundPostglacial marine environmental changes in Maxwell Bay, King George Island, West Antarctica
Khim, B., & Yoon, H. I. (2003) · Polar Research · doi:10.3402/polar.v22i2.6464 · Cited by 11
“The limiting factor for pyrite formation under normal oxic seawater conditions is the amount of organic matter, which determines reducing conditions in the near-surface sediments (Berner 1982).”
BackgroundSulfur and organic carbon contents in sediment cores from the Tyro and Orca basins
Sheu, D.-D. (1987) · Marine Geology · doi:10.1016/0025-3227(87)90101-0 · Cited by 11
Mechanisms and ecological significance
McGlathery, K. J., Marino, R. M., & Howarth, R. W. (1994) · Cited by 11
Emeis, K., Morse, J. W., & Mays, L. L. (1991) · doi:10.2973/odp.proc.sr.117.155.1991 · Cited by 11
Early diagenetic processes in northwestern Black Sea sediments
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Measuring the Flow of Energy and Matter in Marine Benthic Animal Populations
van der Meer, J., Brey, T., Heip, C. H. R., et al. (2013) · doi:10.1002/9781118542392.ch8 · Cited by 11
Paleoenvironmental evolution during the Early Eocene Climate Optimum in the Chicxulub impact crater
Schaefer, B., Schwark, L., Böttcher, M. E., Smith, V., Coolen, M. J. L., & Grice, K. (2022) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2022.117589 · Cited by 12
Hossain, H. M. Z., Kawahata, H., Sampei, Y., Feakins, S. J., & Ratnayake, A. S. (2021) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2022.105769 · Cited by 10
Organic Carbon Sources in Surface Sediments on the Northern South China Sea
Lin, B., Liu, Z., Eglinton, T. I., et al. (2024) · Journal of Geophysical Research Biogeosciences · doi:10.1029/2023jg007909 · Cited by 10
“Organic carbon (OC) burial in marine sediments leads to CO 2 removal from the atmosphere and it is hence crucial to examine the controls on OC preservation in sediments (Berner, 1982).”
BackgroundYin, S., Hernández-Molina, F. J., Fan, W., & Li, J. (2024) · Geophysical Research Letters · doi:10.1029/2024gl109444 · Cited by 11
“About 0.1% of modern oceanic primary production is buried and preserved as organic carbon in marine sediments, which serve as a net sink for atmospheric CO 2 and a source for oxygen (O 2 ) (Arndt et al., 2013; Berner, 1982; Hedges & Keil, 1995).”
InfluentialLimited Organic Carbon Burial by the Rusty Carbon Sink in Swedish Fjord Sediments
Placitu, S., van de Velde, S., Hylén, A., Hall, P., Robertson, E. K., Eriksson, M., Leermakers, M., Mehta, N., & Bonneville, S. (2024) · Journal of Geophysical Research Biogeosciences · doi:10.1029/2024jg008277 · Cited by 11
“Organic carbon (OC) burial in marine sediments stores carbon over geological time scales (Eglinton, 2012; Jessen et al., 2017), thereby regulating carbon dioxide (CO 2 ) and oxygen (O 2 ) concentrations in the atmosphere and ultimately controlling Earth's climate (Berner, 1982).”
Esrafili-Dizaji, B., Hajikazemi, E., Dalvand, M., et al. (2020) · Facies · doi:10.1007/s10347-020-00608-7 · Cited by 10
“This process is probably related to sulphate reducing bacterial activity and occurs where sedimentation rates are low (Berner 1982).”
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Teske, A., Lizarralde, D., Höfig, T. W., et al. (2021) · Proceedings of the International Ocean Discovery Program. Expedition reports · doi:10.14379/iodp.proc.385.107.2021 · Cited by 10
“At Site U1550, TS and TOC contents are not correlated and show excess sulfur compared to the normal marine trend (Goldhaber and Kaplan, 1974; Berner, 1982), with an average TOC/TS value of 1.9.”
BackgroundInfluentialChen, W., Kemp, D. B., Newton, R. J., He, T., Huang, C., Cho, T., & Izumi, K. (2022) · Global and Planetary Change · doi:10.1016/j.gloplacha.2022.103884 · Cited by 10
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Glacial Cycles Influence Marine Methane Hydrate Formation
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“…an adequate methane supply, and the requirements of thermodynamic stability and methane abundance mean that marine hydrates are present in continental slope sediments, which are major sites of particulate organic carbon (POC) burial (Berner, 1982) and methanogenesis (Claypool & Kaplan, 1974).”
BackgroundWoulds, C., Middelburg, J. J., & Cowie, G. L. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2014.02.013 · Cited by 11
Prediction of sediment‐bound nutrient delivery from semi‐arid California watersheds
Gabet, E. J., Fierer, N., & Chadwick, O. A. (2005) · Journal of Geophysical Research Atmospheres · doi:10.1029/2005jg000032 · Cited by 10
“For example, eroded SOC that is oxidized quickly augments present atmospheric CO2 [Schlesinger and Melack, 1981], whereas SOC sequestered in offshore sedimentary deposits represents a net CO2 sink [ Berner, 1982 ].”
Sheng, Y., Sun, Q., Bottrell, S. H., et al. (2015) · Environmental Science Processes & Impacts · doi:10.1039/c5em00175g · Cited by 10
Fossil Lipids for Life-Detection: A Case Study from the Early Earth Record
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The Global Carbon Cycle and Climate Change
Schlesinger, W. H. (2005) · Advances in the economics of environmental resources · doi:10.1016/s1569-3740(05)05002-9 · Cited by 11
“1 Pg C/year (Berner, 1982).”
Carbon/sulphur/iron relationships in upwelling sediments
Morse, J. W., & Emeis, K. (1992) · Geological Society London Special Publications · doi:10.1144/gsl.sp.1992.064.01.16 · Cited by 10
Canfield, D. E., Kristensen, E. S., & Thamdrup, B. (2005) · Advances in marine biology · doi:10.1016/s0065-2881(05)48015-3 · Cited by 10
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Kong, F., Liu, X., Li, A., Dong, J., Wang, H., Zhuang, G., Zhang, Z., & Li, C. (2024) · Marine Geology · doi:10.1016/j.margeo.2024.107358 · Cited by 12
Yang, Y., Bendle, J., Pancost, R. D., et al. (2021) · Geophysical Research Letters · doi:10.1029/2020gl091853 · Cited by 9
“…cores that large quantities of sediments enriched in organic carbon are preserved in continental seas and basins along continental margins at low latitudes (Berner, 1982; Hedges & Keil, 1995), suggesting an important role in the global carbon cycle (e.g., Dai et al., 2013; K.-K. Liu et al., 2010).”
BackgroundResultEarly diagenetic processes in an iron-dominated marine depositional system
Figueroa, M. C., van de Velde, S., Gregory, D. D., Lemieux, S., Drake, J. L., Treude, T., Kemnitz, N., Berelson, W. M., Choumiline, K., Bates, S. M., et al. (2022) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2022.11.026 · Cited by 10
Using cuttings to extract geomechanical properties along lateral wells in unconventional reservoirs
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Simone, M., Schulz, K. G., Eyre, B. D., & Oakes, J. M. (2021) · Limnology and Oceanography · doi:10.1002/lno.11796 · Cited by 10
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“Marine sediments represent a major carbon reservoir on Earth.”
BackgroundAssessing the Potential of Mineral Carbonation with Industrial Alkalinity Sources in the U.S
Kirchofer, A., Brandt, A. R., Krevor, S. C. M., Prigiobbe, V., Becker, A., & Wilcox, J. L. (2013) · Energy Procedia · doi:10.1016/j.egypro.2013.06.510 · Cited by 9
Environmental changes at the inner sector of Ría de Muros (NW Spain) during Middle to Late Holocene
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Seasonal export of 234Th and POC in Daya Bay, northern South China Sea
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“Therefore, shell encrustation could occur because Fe may precipitate when it comes in contact with dissolved O2 and also when it comes in contact with S(2) pyritization (Berner, 1982).”
BackgroundThe Importance of Mineralization Processes in Surface Sediments at Continental Margins
Zabel, M., & Hensen, C. (2002) · Springer eBooks · doi:10.1007/978-3-662-05127-6_16 · Cited by 9
Booth, A. M., Buma, B. J., & Nagorski, S. A. (2023) · Journal of Geophysical Research Biogeosciences · doi:10.1029/2022jg007297 · Cited by 8
“millennial turnover times of soil C (Berner, 1982; Blair & Aller, 2012; Hedges & Keil, 1995; Hedges et al., 1997).”
BackgroundFeng, J., Li, N., Liang, J., Yang, S., Liang, Q., & Chen, D. (2023) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2023.106602 · Cited by 10
Sun, T., Yin, P., Cao, K., Duan, X., & Zhang, X. (2024) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2024.106863 · Cited by 8
Sedimentary diagenesis, depositional environments, and benthic fluxes
Aller, R. C., & Wehrmann, L. M. (2024) · Elsevier eBooks · doi:10.1016/b978-0-323-99762-1.00095-4 · Cited by 11
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“On the contrary, POC burial can be viewed either as a net sink of CO 2 at both short and long timescales (POC bio burial) or as having no impact on the carbon cycle (POC petro burial) (Berner, 1982; Clark et al., 2022; Galy, Beyssac, et al., 2008; Galy et al., 2015; Hilton and West, 2020).”
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Reconciling the impact of mobile bottom-contact fishing on marine organic carbon sequestration
Khedri, P., Gourgue, O., Depestele, J., Arndt, S., & van de Velde, S. (2025) · ICES Journal of Marine Science · doi:10.1093/icesjms/fsaf154 · Cited by 9
Yin, M., Duan, L., Song, J., Zhang, N., Li, X., Yuan, H., & Peng, Q. (2021) · Organic Geochemistry · doi:10.1016/j.orggeochem.2021.104268 · Cited by 8
Bioturbation and the δ56Fe signature of dissolved iron fluxes from marine sediments
van de Velde, S., Dale, A. W., & Arndt, S. (2023) · Royal Society Open Science · doi:10.1098/rsos.220010 · Cited by 8
“Sulfate concentrations could exert an important control on JDFe because the major benthic sink for iron in sediments is the precipitation and burial of pyrite [88].”
BackgroundOceanic redox conditions during the terminal Cambrian extinction event
Chen, X., Shields, G., Andersen, M. B., Qiu, C., Min, S.-Y., Shao, Q., & Ling, H. (2023) · Chemical Geology · doi:10.1016/j.chemgeo.2023.121456 · Cited by 8
“If we omit this sink, the euxinic organic C sink comprises only 5% of the total, whereas about half of organic C burial occurs in intermediate reducing settings (Berner, 1982).”
BackgroundMar’yash, A. A., Ходоренко, Н. Д., Звалинский, В. И., et al. (2015) · Geochemistry International · doi:10.1134/s0016702915080042 · Cited by 8
Arning, E. T., van Berk, W., & Schulz, H.-M. (2012) · Global Biogeochemical Cycles · doi:10.1029/2011gb004156 · Cited by 9
“[5] The early diagenetic carbon cycle in anoxic environments is complex and comprises of the interplay between solid, aqueous and gaseous carbon species, and many other elemental species (e.g., sulphur, calcium, and iron) [Berner, 1982].”
BackgroundOsterrieth, M., Borrelli, N. L., Álvarez, M. F., et al. (2016) · Environmental Earth Sciences · doi:10.1007/s12665-016-5506-8 · Cited by 8
“…in depositional environments is due to its stability (Raiswell and Berner 1985), allowing interpretations on the factors that control its formation and accumulation during early diagenesis, including availability of iron, sulfate, organic carbon and hydrodynamics (Berner 1970, 1982, 1984).”
BackgroundDistribution, sources and burial flux of sedimentary organic matter in the East China Sea
Wu, X., Wu, B., Jiang, M., et al. (2020) · Journal of Oceanology and Limnology · doi:10.1007/s00343-020-0037-2 · Cited by 8
“With the large riverine input, the intensifi ed human activity and the complex hydrodynamic process, the coastal area, as the vital sink and active interface, receives ~80% of organic carbon (OC) from the land-derived materials (Berner, 1982; Bianchi and Allison, 2009; Hu et al., 2012).”
BackgroundQu, Z., Thrush, S. F., & Lewis, N. (2021) · Ocean & Coastal Management · doi:10.1016/j.ocecoaman.2021.105951 · Cited by 8
Teske, A., Lizarralde, D., Höfig, T. W., et al. (2021) · Proceedings of the International Ocean Discovery Program. Expedition reports · doi:10.14379/iodp.proc.385.108.2021 · Cited by 8
The Origin of Earth's Mantle Nitrogen: Primordial or Early Biogeochemical Cycling?
Kurokawa, H., Laneuville, M., Li, Y., Zhang, N., Fujii, Y., Sakuraba, H., Houser, C., & Cleaves, H. J. (2022) · Geochemistry Geophysics Geosystems · doi:10.1029/2021gc010295 · Cited by 9
“We assumed the fraction of pelagic sediments, fpel, to be 0.038 (Berner, 1982; Stüeken, Kipp, Koehler, Schwieterman, et al., 2016).”
BackgroundInfluentialWang, X., Gao, J., Zhong, L., He, W., Jin, Z., Zhu, R., Liang, X., Liu, K., & Zhang, W. (2022) · Frontiers in Earth Science · doi:10.3389/feart.2022.918391 · Cited by 8
“Most studies show that geological events such as volcanism can accelerate the formation of organic-rich matter by changing the reducing properties of water column (Berner, 1982; Hedges, 1987; Hedges, 1992; Hedges and Keil, 1995; Cui et al., 2016).”
BackgroundWang, L., Liu, Y., Yang, C., Huang, H., Hou, M., Yang, C., & Yin, R. (2023) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2023.111634 · Cited by 8
Sun, X., Sun, X., Hu, L., et al. (2023) · Global Biogeochemical Cycles · doi:10.1029/2023gb007760 · Cited by 8
“To quantify the role of coastal zones in Hg sequestration in the ocean, we employed a compiled database of surface sediments and cores using two distinct methods from the literature (Berner, 1982; R. W. Smith et al., 2015; Zaferani et al., 2018) to provide a revised model of Hg burial in global coastal oceans.”
MethodAn introduction to the biogeochemistry of river-coastal systems
Bianchi, T. S., Bianchi, T. S., Allison, M. A., Bianchi, T. S., & Cai, W. (2013) · Cambridge University Press eBooks · doi:10.1017/cbo9781139136853.003 · Cited by 11
Koma, T., & Suzuki, Y. (1988) · Chemical Geology · doi:10.1016/0009-2541(88)90022-8 · Cited by 8
Clark, M. W., & McConchie, D. M. (2004) · Soil Research · doi:10.1071/sr03072 · Cited by 8
Wang, K., Shi, X., Qiao, S., et al. (2015) · Acta Oceanologica Sinica · doi:10.1007/s13131-015-0772-y · Cited by 8
Simulating biosignatures from pre-oxygen photosynthesizing life on TRAPPIST-1e
Eager-Nash, J. K., Daines, S. J., McDermott, J. W., Andrews, P., Grain, L. A., Bishop, J., Rogers, A. A., Smith, J. W. G., Khalek, C., Boxer, T. J., et al. (2024) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stae1142 · Cited by 11
Liu, M., Bai, Y., Jiang, L., et al. (2024) · CATENA · doi:10.1016/j.catena.2024.108611 · Cited by 7
Malinverno, A., Zitellini, N., Estes, E. R., et al. (2025) · Proceedings of the International Ocean Discovery Program. Expedition reports · doi:10.14379/iodp.proc.402.102.2025 · Cited by 7
Climate stabilization by alkalinity production from pyrite burial during oceanic anoxia
Fakhraee, M., Bauer, K. W., Planavsky, N. J., Reinhard, C. T., & Crowe, S. A. (2025) · Nature Geoscience · doi:10.1038/s41561-025-01698-0 · Cited by 7
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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