Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution
In this study, the ‘dead carbon proportion’ (DCP) calculated from combined U-Th and radiocarbon analyses was used to explore the carbon isotope systematics in Corchia Cave (Italy) speleothems, using the example of stalagmite CC26 which grew during the last ∼12 ka. The DCP values in CC26 are among th...
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ftusouthflorida:oai:digitalcommons.usf.edu:kip_articles-8223 2023-12-10T09:47:37+01:00 Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution Bajo, Petra Borsato, Andrea Drysdale, Russell Hua, Quan 2017-01-01T08:00:00Z https://digitalcommons.usf.edu/kip_articles/7223 https://doi.org/10.1016/j.gca.2017.04.038 unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/kip_articles/7223 doi:10.1016/j.gca.2017.04.038 https://doi.org/10.1016/j.gca.2017.04.038 KIP Articles text 2017 ftusouthflorida https://doi.org/10.1016/j.gca.2017.04.038 2023-11-12T17:28:19Z In this study, the ‘dead carbon proportion’ (DCP) calculated from combined U-Th and radiocarbon analyses was used to explore the carbon isotope systematics in Corchia Cave (Italy) speleothems, using the example of stalagmite CC26 which grew during the last ∼12 ka. The DCP values in CC26 are among the highest ever recorded in a stalagmite, spanning the range 44.8–68.8%. A combination of almost closed-system conditions and sulphuric acid dissolution (SAD) are proposed as major drivers in producing such a high DCP with minor contribution from old organic matter from the deep vadose zone. The long-term decrease in both DCP and δ13C most likely reflects post-glacial soil recovery above the cave, with a progressive increase of soil CO2 contribution to the total dissolved inorganic carbon (DIC). Pronounced millennial-scale shifts in DCP and relatively small coeval but antipathetic changes in δ13C are modulated by the effects of hydrological variability on open and closed-system dissolution, SAD and prior calcite precipitation. Hence, the DCP in Corchia Cave speleothems represents an additional proxy for rainfall amount. Text Carbonic acid University of South Florida St. Petersburg: Digital USFSP Geochimica et Cosmochimica Acta 210 208 227 |
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Open Polar |
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University of South Florida St. Petersburg: Digital USFSP |
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ftusouthflorida |
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description |
In this study, the ‘dead carbon proportion’ (DCP) calculated from combined U-Th and radiocarbon analyses was used to explore the carbon isotope systematics in Corchia Cave (Italy) speleothems, using the example of stalagmite CC26 which grew during the last ∼12 ka. The DCP values in CC26 are among the highest ever recorded in a stalagmite, spanning the range 44.8–68.8%. A combination of almost closed-system conditions and sulphuric acid dissolution (SAD) are proposed as major drivers in producing such a high DCP with minor contribution from old organic matter from the deep vadose zone. The long-term decrease in both DCP and δ13C most likely reflects post-glacial soil recovery above the cave, with a progressive increase of soil CO2 contribution to the total dissolved inorganic carbon (DIC). Pronounced millennial-scale shifts in DCP and relatively small coeval but antipathetic changes in δ13C are modulated by the effects of hydrological variability on open and closed-system dissolution, SAD and prior calcite precipitation. Hence, the DCP in Corchia Cave speleothems represents an additional proxy for rainfall amount. |
format |
Text |
author |
Bajo, Petra Borsato, Andrea Drysdale, Russell Hua, Quan |
spellingShingle |
Bajo, Petra Borsato, Andrea Drysdale, Russell Hua, Quan Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution |
author_facet |
Bajo, Petra Borsato, Andrea Drysdale, Russell Hua, Quan |
author_sort |
Bajo, Petra |
title |
Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution |
title_short |
Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution |
title_full |
Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution |
title_fullStr |
Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution |
title_full_unstemmed |
Stalagmite carbon isotopes and dead carbon proportion (DCP) in a near-closed-system situation: An interplay between sulphuric and carbonic acid dissolution |
title_sort |
stalagmite carbon isotopes and dead carbon proportion (dcp) in a near-closed-system situation: an interplay between sulphuric and carbonic acid dissolution |
publisher |
Digital Commons @ University of South Florida |
publishDate |
2017 |
url |
https://digitalcommons.usf.edu/kip_articles/7223 https://doi.org/10.1016/j.gca.2017.04.038 |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_source |
KIP Articles |
op_relation |
https://digitalcommons.usf.edu/kip_articles/7223 doi:10.1016/j.gca.2017.04.038 https://doi.org/10.1016/j.gca.2017.04.038 |
op_doi |
https://doi.org/10.1016/j.gca.2017.04.038 |
container_title |
Geochimica et Cosmochimica Acta |
container_volume |
210 |
container_start_page |
208 |
op_container_end_page |
227 |
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1784891300740333568 |