Silicate weathering in anoxic marine sediments
International audience Two sediment cores retrieved at the northern slope of Sakhalin Island, Sea of Okhotsk, were analyzed for biogenic opal, organic carbon, carbonate, sulfur,major element concentrations, mineral contents, and dissolved substances including nutrients, sulfate, methane, major catio...
Published in: | Geochimica et Cosmochimica Acta |
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Online Access: | https://hal.science/hal-00336322 https://doi.org/10.1016/j.gca.2008.03.026 |
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ftunivlyon1:oai:HAL:hal-00336322v1 2023-06-11T04:15:44+02:00 Silicate weathering in anoxic marine sediments Wallmann, K. Aloisi, Giovanni Haeckel, M. Tishchenko, P. Pavlova, G. Greinert, J. Kutterolf, S. Eisenhauer, A. PaleoEnvironnements et PaleobioSphere (PEPS) Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) 2008 https://hal.science/hal-00336322 https://doi.org/10.1016/j.gca.2008.03.026 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gca.2008.03.026 hal-00336322 https://hal.science/hal-00336322 doi:10.1016/j.gca.2008.03.026 ISSN: 0016-7037 EISSN: 0016-7037 Geochimica et Cosmochimica Acta https://hal.science/hal-00336322 Geochimica et Cosmochimica Acta, 2008, 72 (12), pp.2895-2918. ⟨10.1016/j.gca.2008.03.026⟩ DISSOLVED ORGANIC-CARBON DEEP ARABIAN SEA ATMOSPHERIC CO2 OKHOTSK SEA SEAWATER COMPOSITION INTERSTITIAL WATERS CENOZOIC EVOLUTION SURFACE SEDIMENTS BOTTOM SEDIMENTS NORTHWESTERN SEA [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2008 ftunivlyon1 https://doi.org/10.1016/j.gca.2008.03.026 2023-05-30T22:46:13Z International audience Two sediment cores retrieved at the northern slope of Sakhalin Island, Sea of Okhotsk, were analyzed for biogenic opal, organic carbon, carbonate, sulfur,major element concentrations, mineral contents, and dissolved substances including nutrients, sulfate, methane, major cations, humic substances, and total alkalinity. Down-core trends in mineral abundance suggest that plagioclase feldspars and other reactive silicate phases (olivine, pyroxene, volcanic ash) are transformed into smectite in the methanogenic sediment sections. The element ratios Na/Al, Mg/Al, and Ca/Al in the solid phase decrease with sediment depth indicating a loss of mobile cations with depth and producing a significant down-core increase in the chemical index of alteration. Pore waters separated from the sediment cores are highly enriched in dissolved magnesium, total alkalinity, humic substances, and boron. The high contents of dissolved organic carbon in the deeper methanogenic sediment sections (50-150 mg dm(-3)) may promote the dissolution of silicate phases through complexation of Al3+ and other structure-building cations. A non-steady state transport-reaction model was developed and applied to evaluate the down-core trends observed in the solid and dissolved phases. Dissolved Mg and total alkalinity were used to track the in-situ rates of marine silicate weathering since thermodynamic equilibrium calculations showed that these tracers are not affected by ion exchange processes with sediment surfaces. The modeling showed that silicate weathering is limited to the deeper methanogenic sediment section whereas reverse weathering was the dominant process in the overlying surface sediments. Depth-integrated rates of marine silicate weathering in methanogenic sediments derived from the model (81.4-99.2 mmol CO2 m(-2) year(-1)) are lower than the marine weathering rates calculated from the solid phase data (198-245 mmol CO2 m(-2) year(-1)) suggesting a decrease in marine weathering over time. The production of CO2 ... Article in Journal/Newspaper okhotsk sea Sakhalin HAL Lyon 1 (University Claude Bernard Lyon 1) Okhotsk Geochimica et Cosmochimica Acta 72 12 2895 2918 |
institution |
Open Polar |
collection |
HAL Lyon 1 (University Claude Bernard Lyon 1) |
op_collection_id |
ftunivlyon1 |
language |
English |
topic |
DISSOLVED ORGANIC-CARBON DEEP ARABIAN SEA ATMOSPHERIC CO2 OKHOTSK SEA SEAWATER COMPOSITION INTERSTITIAL WATERS CENOZOIC EVOLUTION SURFACE SEDIMENTS BOTTOM SEDIMENTS NORTHWESTERN SEA [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
DISSOLVED ORGANIC-CARBON DEEP ARABIAN SEA ATMOSPHERIC CO2 OKHOTSK SEA SEAWATER COMPOSITION INTERSTITIAL WATERS CENOZOIC EVOLUTION SURFACE SEDIMENTS BOTTOM SEDIMENTS NORTHWESTERN SEA [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDE.MCG]Environmental Sciences/Global Changes Wallmann, K. Aloisi, Giovanni Haeckel, M. Tishchenko, P. Pavlova, G. Greinert, J. Kutterolf, S. Eisenhauer, A. Silicate weathering in anoxic marine sediments |
topic_facet |
DISSOLVED ORGANIC-CARBON DEEP ARABIAN SEA ATMOSPHERIC CO2 OKHOTSK SEA SEAWATER COMPOSITION INTERSTITIAL WATERS CENOZOIC EVOLUTION SURFACE SEDIMENTS BOTTOM SEDIMENTS NORTHWESTERN SEA [SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience Two sediment cores retrieved at the northern slope of Sakhalin Island, Sea of Okhotsk, were analyzed for biogenic opal, organic carbon, carbonate, sulfur,major element concentrations, mineral contents, and dissolved substances including nutrients, sulfate, methane, major cations, humic substances, and total alkalinity. Down-core trends in mineral abundance suggest that plagioclase feldspars and other reactive silicate phases (olivine, pyroxene, volcanic ash) are transformed into smectite in the methanogenic sediment sections. The element ratios Na/Al, Mg/Al, and Ca/Al in the solid phase decrease with sediment depth indicating a loss of mobile cations with depth and producing a significant down-core increase in the chemical index of alteration. Pore waters separated from the sediment cores are highly enriched in dissolved magnesium, total alkalinity, humic substances, and boron. The high contents of dissolved organic carbon in the deeper methanogenic sediment sections (50-150 mg dm(-3)) may promote the dissolution of silicate phases through complexation of Al3+ and other structure-building cations. A non-steady state transport-reaction model was developed and applied to evaluate the down-core trends observed in the solid and dissolved phases. Dissolved Mg and total alkalinity were used to track the in-situ rates of marine silicate weathering since thermodynamic equilibrium calculations showed that these tracers are not affected by ion exchange processes with sediment surfaces. The modeling showed that silicate weathering is limited to the deeper methanogenic sediment section whereas reverse weathering was the dominant process in the overlying surface sediments. Depth-integrated rates of marine silicate weathering in methanogenic sediments derived from the model (81.4-99.2 mmol CO2 m(-2) year(-1)) are lower than the marine weathering rates calculated from the solid phase data (198-245 mmol CO2 m(-2) year(-1)) suggesting a decrease in marine weathering over time. The production of CO2 ... |
author2 |
PaleoEnvironnements et PaleobioSphere (PEPS) Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Wallmann, K. Aloisi, Giovanni Haeckel, M. Tishchenko, P. Pavlova, G. Greinert, J. Kutterolf, S. Eisenhauer, A. |
author_facet |
Wallmann, K. Aloisi, Giovanni Haeckel, M. Tishchenko, P. Pavlova, G. Greinert, J. Kutterolf, S. Eisenhauer, A. |
author_sort |
Wallmann, K. |
title |
Silicate weathering in anoxic marine sediments |
title_short |
Silicate weathering in anoxic marine sediments |
title_full |
Silicate weathering in anoxic marine sediments |
title_fullStr |
Silicate weathering in anoxic marine sediments |
title_full_unstemmed |
Silicate weathering in anoxic marine sediments |
title_sort |
silicate weathering in anoxic marine sediments |
publisher |
HAL CCSD |
publishDate |
2008 |
url |
https://hal.science/hal-00336322 https://doi.org/10.1016/j.gca.2008.03.026 |
geographic |
Okhotsk |
geographic_facet |
Okhotsk |
genre |
okhotsk sea Sakhalin |
genre_facet |
okhotsk sea Sakhalin |
op_source |
ISSN: 0016-7037 EISSN: 0016-7037 Geochimica et Cosmochimica Acta https://hal.science/hal-00336322 Geochimica et Cosmochimica Acta, 2008, 72 (12), pp.2895-2918. ⟨10.1016/j.gca.2008.03.026⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gca.2008.03.026 hal-00336322 https://hal.science/hal-00336322 doi:10.1016/j.gca.2008.03.026 |
op_doi |
https://doi.org/10.1016/j.gca.2008.03.026 |
container_title |
Geochimica et Cosmochimica Acta |
container_volume |
72 |
container_issue |
12 |
container_start_page |
2895 |
op_container_end_page |
2918 |
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1768372809234382848 |