Current calcite (CaCO3) dissolution at the seafloor caused by anthropogenic CO2 (NCEI Accession 0176672)
This dataset consists of current CaCO3 dissolution at the seafloor caused by anthropogenic CO2 in the World Oceans. This dataset contains the main results from Sulpis et al. (PNAS, 2018). All the variables have a 1x1 degree resolution. It can be used to compute calcite dissolution at the seafloor fo...
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NOAA National Centers for Environmental Information
2018
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Online Access: | https://dx.doi.org/10.25921/kbqy-4v05 https://www.ncei.noaa.gov/archive/accession/0176672 |
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ftdatacite:10.25921/kbqy-4v05 2023-05-15T17:35:32+02:00 Current calcite (CaCO3) dissolution at the seafloor caused by anthropogenic CO2 (NCEI Accession 0176672) Sulpis, Olivier Boudreau, Bernard P. Mucci, Alfonso Jenkins, Chris Trossman, David S. Arbic, Brian K. Key, Robert M. 2018 https://dx.doi.org/10.25921/kbqy-4v05 https://www.ncei.noaa.gov/archive/accession/0176672 unknown NOAA National Centers for Environmental Information Dataset dataset 2018 ftdatacite https://doi.org/10.25921/kbqy-4v05 2022-02-09T12:36:08Z This dataset consists of current CaCO3 dissolution at the seafloor caused by anthropogenic CO2 in the World Oceans. This dataset contains the main results from Sulpis et al. (PNAS, 2018). All the variables have a 1x1 degree resolution. It can be used to compute calcite dissolution at the seafloor for changing bottom-water chemistry, calcite rain rates or current speeds, for instance. Oceanic uptake of anthropogenic CO2 leads to decreased pH, carbonate ion concentration, and saturation state with respect to CaCO3 minerals, causing increased dissolution of these minerals at the deep seafloor. This additional dissolution will figure prominently in the neutralization of man-made CO2. Yet, there has been no concerted assessment of the current extent of anthropogenic CaCO3 dissolution at the deep seafloor. Here, recent databases of bottom-water chemistry, benthic currents, and CaCO3 content of deep-sea sediments are combined with a new rate model to derive the global distribution of benthic calcite dissolution rates and obtain primary confirmation of an anthropogenic component. By comparing pre-industrial with present-day rates, we determine that significant anthropogenic dissolution now occurs in the western North Atlantic, amounting to 40-100% of the total seafloor dissolution at its most intense locations. At these locations, the calcite compensation depth has risen ~300 m. Increased benthic dissolution was also revealed at various hot spots in the southern extent of the Atlantic, Indian and Pacific Oceans. Our findings place constraints on future predictions of ocean acidification, are consequential to the fate of benthic calcifiers, and indicate that a by-product of human activities is currently altering the geological record of the deep sea. Dataset North Atlantic Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Pacific Indian |
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DataCite Metadata Store (German National Library of Science and Technology) |
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description |
This dataset consists of current CaCO3 dissolution at the seafloor caused by anthropogenic CO2 in the World Oceans. This dataset contains the main results from Sulpis et al. (PNAS, 2018). All the variables have a 1x1 degree resolution. It can be used to compute calcite dissolution at the seafloor for changing bottom-water chemistry, calcite rain rates or current speeds, for instance. Oceanic uptake of anthropogenic CO2 leads to decreased pH, carbonate ion concentration, and saturation state with respect to CaCO3 minerals, causing increased dissolution of these minerals at the deep seafloor. This additional dissolution will figure prominently in the neutralization of man-made CO2. Yet, there has been no concerted assessment of the current extent of anthropogenic CaCO3 dissolution at the deep seafloor. Here, recent databases of bottom-water chemistry, benthic currents, and CaCO3 content of deep-sea sediments are combined with a new rate model to derive the global distribution of benthic calcite dissolution rates and obtain primary confirmation of an anthropogenic component. By comparing pre-industrial with present-day rates, we determine that significant anthropogenic dissolution now occurs in the western North Atlantic, amounting to 40-100% of the total seafloor dissolution at its most intense locations. At these locations, the calcite compensation depth has risen ~300 m. Increased benthic dissolution was also revealed at various hot spots in the southern extent of the Atlantic, Indian and Pacific Oceans. Our findings place constraints on future predictions of ocean acidification, are consequential to the fate of benthic calcifiers, and indicate that a by-product of human activities is currently altering the geological record of the deep sea. |
format |
Dataset |
author |
Sulpis, Olivier Boudreau, Bernard P. Mucci, Alfonso Jenkins, Chris Trossman, David S. Arbic, Brian K. Key, Robert M. |
spellingShingle |
Sulpis, Olivier Boudreau, Bernard P. Mucci, Alfonso Jenkins, Chris Trossman, David S. Arbic, Brian K. Key, Robert M. Current calcite (CaCO3) dissolution at the seafloor caused by anthropogenic CO2 (NCEI Accession 0176672) |
author_facet |
Sulpis, Olivier Boudreau, Bernard P. Mucci, Alfonso Jenkins, Chris Trossman, David S. Arbic, Brian K. Key, Robert M. |
author_sort |
Sulpis, Olivier |
title |
Current calcite (CaCO3) dissolution at the seafloor caused by anthropogenic CO2 (NCEI Accession 0176672) |
title_short |
Current calcite (CaCO3) dissolution at the seafloor caused by anthropogenic CO2 (NCEI Accession 0176672) |
title_full |
Current calcite (CaCO3) dissolution at the seafloor caused by anthropogenic CO2 (NCEI Accession 0176672) |
title_fullStr |
Current calcite (CaCO3) dissolution at the seafloor caused by anthropogenic CO2 (NCEI Accession 0176672) |
title_full_unstemmed |
Current calcite (CaCO3) dissolution at the seafloor caused by anthropogenic CO2 (NCEI Accession 0176672) |
title_sort |
current calcite (caco3) dissolution at the seafloor caused by anthropogenic co2 (ncei accession 0176672) |
publisher |
NOAA National Centers for Environmental Information |
publishDate |
2018 |
url |
https://dx.doi.org/10.25921/kbqy-4v05 https://www.ncei.noaa.gov/archive/accession/0176672 |
geographic |
Pacific Indian |
geographic_facet |
Pacific Indian |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_doi |
https://doi.org/10.25921/kbqy-4v05 |
_version_ |
1766134731076796416 |