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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2022
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| Online-Zugang: | https://doi.org/10.1594/PANGAEA.947790 |
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| _version_ | 1867168217690013696 |
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| author | Nürnberg, Dirk |
| author_facet | Nürnberg, Dirk |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Proxy parameter of core M94-480 PC: Benthic and planktonic stable isotopes and coarse fraction of sediment core M94-480 PC. Isotope analyses were performed on the planktonic and benthic foraminiferal species Globigerinoides ruber (white) and Uvigerina peregrina, respectively. Sedimentological and logging data as well as the foraminiferal analyses were performed on piston core M94-480 PC, which was recovered from the northern Campeche Bank (Gulf of Mexico; 23°48.141'N 87°00.868'W) from 730 m water depth during R/V Meteor Cruise M94 in 2013 (https://doi.org/10.2312/cr_m94). Sampling and analytical studies were carried out from ~0.5 cm to 1215.5 cm core depth at 1-5 cm spatial resolution. The records cover the last ~360 kyrs. The stable carbon (δ13C; ‰ VPDB) and oxygen isotope (δ18O, ‰ VPDB) analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV Carbonate Preparation Device. The isotope data provide stratigraphical information. The coarse fraction percentages were derived from sieving. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_947790 |
| institution | PANGAEA |
| language | en |
| publishDate | 2022 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Benthic and planktonic stable isotopes and coarse fraction of sediment core M94-480 PC Nürnberg, Dirk AGE; DEPTH, sediment/rock; Globigerinoides ruber white, δ13C; Globigerinoides ruber white, δ18O; Grain size, sieving; Gulf of Mexico; Loop Current; M94; M94_480; Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV; Meteor (1986); Mid Pleistocene Transition; northern Campeche bank; northern hemisphere cooling; PC; Piston corer; planktic carbon isotopes; planktic oxygen isotopes; Size fraction > 0.063 mm, sand; Surface and Intermediate Water Variability in Yucatan Strait and the Gulf of Mexico; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O; YUCATAN_THROUGHFLOW Proxy parameter of core M94-480 PC: Benthic and planktonic stable isotopes and coarse fraction of sediment core M94-480 PC. Isotope analyses were performed on the planktonic and benthic foraminiferal species Globigerinoides ruber (white) and Uvigerina peregrina, respectively. Sedimentological and logging data as well as the foraminiferal analyses were performed on piston core M94-480 PC, which was recovered from the northern Campeche Bank (Gulf of Mexico; 23°48.141'N 87°00.868'W) from 730 m water depth during R/V Meteor Cruise M94 in 2013 (https://doi.org/10.2312/cr_m94). Sampling and analytical studies were carried out from ~0.5 cm to 1215.5 cm core depth at 1-5 cm spatial resolution. The records cover the last ~360 kyrs. The stable carbon (δ13C; ‰ VPDB) and oxygen isotope (δ18O, ‰ VPDB) analyses were performed on a Thermo Scientific MAT 253 mass spectrometer with an automated Kiel IV Carbonate Preparation Device. The isotope data provide stratigraphical information. The coarse fraction percentages were derived from sieving. |
| title | Benthic and planktonic stable isotopes and coarse fraction of sediment core M94-480 PC |
| topic | AGE; DEPTH, sediment/rock; Globigerinoides ruber white, δ13C; Globigerinoides ruber white, δ18O; Grain size, sieving; Gulf of Mexico; Loop Current; M94; M94_480; Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV; Meteor (1986); Mid Pleistocene Transition; northern Campeche bank; northern hemisphere cooling; PC; Piston corer; planktic carbon isotopes; planktic oxygen isotopes; Size fraction > 0.063 mm, sand; Surface and Intermediate Water Variability in Yucatan Strait and the Gulf of Mexico; Uvigerina peregrina, δ13C; Uvigerina peregrina, δ18O; YUCATAN_THROUGHFLOW |
| url | https://doi.org/10.1594/PANGAEA.947790 |