| _version_ | 1867172333790167040 |
|---|---|
| author | Ishiwatari, Ryoshi Yamada, Keita Houtatsu, M Naraoka, Hiroshi |
| author_facet | Ishiwatari, Ryoshi Yamada, Keita Houtatsu, M Naraoka, Hiroshi |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The organic and isotopic geochemical study of two sediment cores (KH-79-3, L-3, and KH-79-3, C-3) from the Oki Ridge in the Japan Sea has revealed that total organic carbon (TOC) mass accumulation rates are extremely high in the 12-11 ka (calendar age) interval and TOC in the sections in the 24-17 ka interval is depleted in 13C by 3.5 per mil relative to Holocene sediments. Alkenone sea surface temperature (SST) shows a decrease from 18° to 14°C from 17.5 to 11.6 ka and a sharp increase from 14° to 19°C from 11.6 to 11.1 ka. The SST changes are associated with the inflow of cold seawater with the vertical water mixing and the inflowof warm Tsushima Current into the Japan Sea. The d13C values for both 24-methylcholesta-5,22-dien-3?-ol (diatom marker) and dinosterol (dinoflagellate marker), are at their minimum from 24 to 17 ka, while those for long-chain alkenones are not. The theoretical considerations on d13C for biomarkers suggest low photosynthetic carbon demand of diatoms and dinoflagellates from 24 to 17 ka. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_856814 |
| institution | PANGAEA |
| language | en |
| publishDate | 1999 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Bulk geochemistry of sediment cores KH-79-3_L3 and KH-79-3_C3 Ishiwatari, Ryoshi Yamada, Keita Houtatsu, M Naraoka, Hiroshi AGE; Carbon, organic, total; Carbon/Nitrogen ratio; Comment; DEPTH, sediment/rock; Event label; GC; Gravity corer; KH-79-3_C3; KH-79-3_L3; L3; Oki Ridge; δ13C, organic carbon The organic and isotopic geochemical study of two sediment cores (KH-79-3, L-3, and KH-79-3, C-3) from the Oki Ridge in the Japan Sea has revealed that total organic carbon (TOC) mass accumulation rates are extremely high in the 12-11 ka (calendar age) interval and TOC in the sections in the 24-17 ka interval is depleted in 13C by 3.5 per mil relative to Holocene sediments. Alkenone sea surface temperature (SST) shows a decrease from 18° to 14°C from 17.5 to 11.6 ka and a sharp increase from 14° to 19°C from 11.6 to 11.1 ka. The SST changes are associated with the inflow of cold seawater with the vertical water mixing and the inflowof warm Tsushima Current into the Japan Sea. The d13C values for both 24-methylcholesta-5,22-dien-3?-ol (diatom marker) and dinosterol (dinoflagellate marker), are at their minimum from 24 to 17 ka, while those for long-chain alkenones are not. The theoretical considerations on d13C for biomarkers suggest low photosynthetic carbon demand of diatoms and dinoflagellates from 24 to 17 ka. |
| title | (Table 1) Bulk geochemistry of sediment cores KH-79-3_L3 and KH-79-3_C3 |
| topic | AGE; Carbon, organic, total; Carbon/Nitrogen ratio; Comment; DEPTH, sediment/rock; Event label; GC; Gravity corer; KH-79-3_C3; KH-79-3_L3; L3; Oki Ridge; δ13C, organic carbon |
| url | https://doi.org/10.1594/PANGAEA.856814 |