Stable isotope ratios and geochemical composition of authigenic carbonates from ODP Sites 186-1150 and 186-1151
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2003
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| _version_ | 1867168560806100992 |
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| author | Ijiri, Akira Sakamoto, Tatsuhiko Tsunogai, Urumu Gamo, Toshitaka Saito, Saneatsu Suyehiro, Kiyoshi |
| author_facet | Ijiri, Akira Sakamoto, Tatsuhiko Tsunogai, Urumu Gamo, Toshitaka Saito, Saneatsu Suyehiro, Kiyoshi |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Several carbonaceous layers or fragments were recovered from sediments of Sites 1150 and 1151 on the deep-sea terrace of the Japan Trench during Leg 186. The X-ray diffraction analysis (XRD) data indicate that these are predominantly dolomitic. In this study, carbon and oxygen isotopes of these carbonates recovered at Sites 1150 and 1151 are presented. The oxygen isotope ratios of the dolomites analyzed range from +0.4 per mil to +4.1 per mil vs. Peedee formation belemnite (PDB) and those of calcites from +0.6 per mil to +2.8 per mil PDB. The isotopic composition of carbon varies from -7.0 per mil to +12.3 per mil PDB in dolomite and from -13.4 per mil to -24.1 per mil PDB in calcite. The wide range of carbon isotopic compositions indicates that the carbonate samples were formed by the decomposition of organic matter through reactions such as oxidation, sulfate reduction, and methane formation during diagenesis. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_783555 |
| institution | PANGAEA |
| language | en |
| publishDate | 2003 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Stable isotope ratios and geochemical composition of authigenic carbonates from ODP Sites 186-1150 and 186-1151 Ijiri, Akira Sakamoto, Tatsuhiko Tsunogai, Urumu Gamo, Toshitaka Saito, Saneatsu Suyehiro, Kiyoshi 186-1150A; 186-1150B; 186-1151A; DRILL; Drilling/drill rig; Joides Resolution; Leg186; North Pacific Ocean; Ocean Drilling Program; ODP Several carbonaceous layers or fragments were recovered from sediments of Sites 1150 and 1151 on the deep-sea terrace of the Japan Trench during Leg 186. The X-ray diffraction analysis (XRD) data indicate that these are predominantly dolomitic. In this study, carbon and oxygen isotopes of these carbonates recovered at Sites 1150 and 1151 are presented. The oxygen isotope ratios of the dolomites analyzed range from +0.4 per mil to +4.1 per mil vs. Peedee formation belemnite (PDB) and those of calcites from +0.6 per mil to +2.8 per mil PDB. The isotopic composition of carbon varies from -7.0 per mil to +12.3 per mil PDB in dolomite and from -13.4 per mil to -24.1 per mil PDB in calcite. The wide range of carbon isotopic compositions indicates that the carbonate samples were formed by the decomposition of organic matter through reactions such as oxidation, sulfate reduction, and methane formation during diagenesis. |
| title | Stable isotope ratios and geochemical composition of authigenic carbonates from ODP Sites 186-1150 and 186-1151 |
| topic | 186-1150A; 186-1150B; 186-1151A; DRILL; Drilling/drill rig; Joides Resolution; Leg186; North Pacific Ocean; Ocean Drilling Program; ODP |
| url | https://doi.org/10.1594/PANGAEA.783555 |