Clumped and oxygen isotope data of dolomite veins from the Atlantis Massif, IODP Expedition 357
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2021
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| _version_ | 1867169146980007936 |
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| author | Ternieten, Lotta Früh-Green, Gretchen L Bernasconi, Stefano M |
| author_facet | Ternieten, Lotta Früh-Green, Gretchen L Bernasconi, Stefano M |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The clumped and oxygen isotopes of dolomite from serpentinized peridotites recovered during IODP Expedition 357 (October to December 2015) on the Atlantis Massif, Mid-Atlantic Ridge was examined to characterize carbon sources and the fate of dissolved organic (DOC) and inorganic carbon (DIC) in seawater during long-lived hydrothermal circulation and serpentinization. The measurements were performed at the ETH Zurich from 2017 to 2020 using a Kiel IV carbonate device interfaced with a ThermoFisher Scientific MAT253 isotope ratio mass spectrometer. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_935360 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Clumped and oxygen isotope data of dolomite veins from the Atlantis Massif, IODP Expedition 357 Ternieten, Lotta Früh-Green, Gretchen L Bernasconi, Stefano M 357-M0072B; 357-M0076B; 49-parameter, contamination index; Acid Temperature; AM-01A; AM-11A; Atlantis Massif; Carbon cycle; Clumped isotopes; Date/Time of event; Event label; Exp357; Identification; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; James Cook; Latitude of event; Longitude of event; Mass spectrometer MAT253; Radiocarbon ages; Run ID; Sample code/label; Sample ID; Sample method; Stable carbon and oxygen isotopes; Δ47; Δ47, error; Δ47, standard deviation; Δ48 offset; δ13C, dolomite; δ13C, dolomite, standard deviation; δ18O, dolomite; δ18O, dolomite, standard deviation; δ45; δ46; δ47; δ48; δ49 The clumped and oxygen isotopes of dolomite from serpentinized peridotites recovered during IODP Expedition 357 (October to December 2015) on the Atlantis Massif, Mid-Atlantic Ridge was examined to characterize carbon sources and the fate of dissolved organic (DOC) and inorganic carbon (DIC) in seawater during long-lived hydrothermal circulation and serpentinization. The measurements were performed at the ETH Zurich from 2017 to 2020 using a Kiel IV carbonate device interfaced with a ThermoFisher Scientific MAT253 isotope ratio mass spectrometer. |
| title | Clumped and oxygen isotope data of dolomite veins from the Atlantis Massif, IODP Expedition 357 |
| topic | 357-M0072B; 357-M0076B; 49-parameter, contamination index; Acid Temperature; AM-01A; AM-11A; Atlantis Massif; Carbon cycle; Clumped isotopes; Date/Time of event; Event label; Exp357; Identification; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; James Cook; Latitude of event; Longitude of event; Mass spectrometer MAT253; Radiocarbon ages; Run ID; Sample code/label; Sample ID; Sample method; Stable carbon and oxygen isotopes; Δ47; Δ47, error; Δ47, standard deviation; Δ48 offset; δ13C, dolomite; δ13C, dolomite, standard deviation; δ18O, dolomite; δ18O, dolomite, standard deviation; δ45; δ46; δ47; δ48; δ49 |
| url | https://doi.org/10.1594/PANGAEA.935360 |