Organic carbon and calcium carbonate concentrations in bulk sediment of gravity core LV28-34-2
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
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PANGAEA
2025
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| _version_ | 1867169165907853312 |
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| author | Nürnberg, Dirk |
| author_facet | Nürnberg, Dirk |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Bound by the Asian continent to the northwest and north and the Kurile-Kamchatka-Island Arc to the east and southeast, the Sea of Okhotsk is the second largest marginal sea of the Pacific. In view of strengthened efforts of better understanding cool climate dynamics, the Sea of Okhotsk became an increasing focus of interest as it plays a key role for the modern hydrology of the NW Pacific, its high primary productivity, and its pronounced seasonality in sea ice coverage. We here provide proxydata from gravity core LV28-34-2. The ~9.6 m-long core was recovered from the Derugin Basin in the northern Sea of Okhotsk (53°51.971 N 146°47.499 E) from 1431 m water depth during R/V Lavrentiev Cruise LV28 in 1998 (doi:10.3289/GEOMAR_REP_82_1999). The proxyrecords cover the last ~150 kyrs at centennial resolution. We here provide concentrations of total organic carbon, calcium carbonate, and the calculated carbon/nitrogen ratios. Measurements were done on a Carlo Erba NA1500 CHN analyser at GEOMAR. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_976220 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Organic carbon and calcium carbonate concentrations in bulk sediment of gravity core LV28-34-2 Nürnberg, Dirk Akademik M.A. Lavrentyev; Calcium carbonate; Carbon, organic, total; Carbon/Nitrogen ratio; DEPTH, sediment/rock; Element analyser CNS, Carlo Erba NA1500; GC; glacial/interglacial; Gravity corer; KOMEX; KOMEX I; Kurile-Okhotsk Sea Marine Experiment; LV28; LV28-34-2; productivity; Sea of Okhotsk; sediment composition; Stable isotopes; the Sea of Okhotsk Bound by the Asian continent to the northwest and north and the Kurile-Kamchatka-Island Arc to the east and southeast, the Sea of Okhotsk is the second largest marginal sea of the Pacific. In view of strengthened efforts of better understanding cool climate dynamics, the Sea of Okhotsk became an increasing focus of interest as it plays a key role for the modern hydrology of the NW Pacific, its high primary productivity, and its pronounced seasonality in sea ice coverage. We here provide proxydata from gravity core LV28-34-2. The ~9.6 m-long core was recovered from the Derugin Basin in the northern Sea of Okhotsk (53°51.971 N 146°47.499 E) from 1431 m water depth during R/V Lavrentiev Cruise LV28 in 1998 (doi:10.3289/GEOMAR_REP_82_1999). The proxyrecords cover the last ~150 kyrs at centennial resolution. We here provide concentrations of total organic carbon, calcium carbonate, and the calculated carbon/nitrogen ratios. Measurements were done on a Carlo Erba NA1500 CHN analyser at GEOMAR. |
| title | Organic carbon and calcium carbonate concentrations in bulk sediment of gravity core LV28-34-2 |
| topic | Akademik M.A. Lavrentyev; Calcium carbonate; Carbon, organic, total; Carbon/Nitrogen ratio; DEPTH, sediment/rock; Element analyser CNS, Carlo Erba NA1500; GC; glacial/interglacial; Gravity corer; KOMEX; KOMEX I; Kurile-Okhotsk Sea Marine Experiment; LV28; LV28-34-2; productivity; Sea of Okhotsk; sediment composition; Stable isotopes; the Sea of Okhotsk |
| url | https://doi.org/10.1594/PANGAEA.976220 |