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| Main Authors: | , , , |
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| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
2023
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| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.959922 |
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| _version_ | 1867171038490525696 |
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| author | Zabel, Matthias Kölling, Martin Bohrmann, Gerhard Behrendt, Nele |
| author_facet | Zabel, Matthias Kölling, Martin Bohrmann, Gerhard Behrendt, Nele |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The samples are retrieved from sediment core GeoB24310-1 (Napoli MV; 0-280 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_959922 |
| institution | PANGAEA |
| language | en |
| publishDate | 2023 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24310-1 Zabel, Matthias Kölling, Martin Bohrmann, Gerhard Behrendt, Nele 18O; Cavity ring-down spectroscopy (CRDS), Picarro Inc., L21301i; Center for Marine Environmental Sciences; ClusterOceanFloor; dD; DEPTH, sediment/rock; GC; GeoB24310-1; GPF 19-2-007H; Gravity corer; MARUM; Mediterranean Ridge accretionary complex; Mediterranean Sea; mud volcano; Napoli MV; Olimpi mud volcano field; pore water; R/V SONNE; SO278; SO278_10-1; Sonne_2; The Ocean Floor - Earth's Uncharted Interface; water isotopes; δ18O, porewater; δ18O, porewater, standard deviation; δ Deuterium; δ Deuterium, standard deviation The samples are retrieved from sediment core GeoB24310-1 (Napoli MV; 0-280 cm) in the Olimpi mud volcano field, located south of Crete at the Mediterranean Ridge accretionary complex. Hydrogen (δD) and oxygen (δ18O) isotopes were analysed in the sediment geochemistry laboratory at MARUM using a Picarro 2130i CRD System. Approximately 2 mL of the onboard extracted pore water was used per measurement. The results are an average of at least three injections, while a total of 9 injections of 7 µL each have been analysed per sample. Results are reported in delta notation (‰) relative to V-SMOW2 -SLAP2 with nominal standard (std) deviation of 0.03 for δ18O and 0.3 for δD. Actual std deviation is between 0.02 and 0.29 for δ18O and between 0.04 and 1.68 for δD. |
| title | Stable oxygen and hydrogen isotopic composition of pore water (δ18O; δD) of sediment core GeoB24310-1 |
| topic | 18O; Cavity ring-down spectroscopy (CRDS), Picarro Inc., L21301i; Center for Marine Environmental Sciences; ClusterOceanFloor; dD; DEPTH, sediment/rock; GC; GeoB24310-1; GPF 19-2-007H; Gravity corer; MARUM; Mediterranean Ridge accretionary complex; Mediterranean Sea; mud volcano; Napoli MV; Olimpi mud volcano field; pore water; R/V SONNE; SO278; SO278_10-1; Sonne_2; The Ocean Floor - Earth's Uncharted Interface; water isotopes; δ18O, porewater; δ18O, porewater, standard deviation; δ Deuterium; δ Deuterium, standard deviation |
| url | https://doi.org/10.1594/PANGAEA.959922 |