Concentrations of alkenones in Hala Hu sediment core H7
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| Autori principali: | , , , , , , , |
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2021
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| _version_ | 1867169439371231232 |
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| author | Aichner, Bernhard Callegaro, Alice van der Meer, Marcel T J Wünnemann, Bernd Yan, Dada Zhang, Yongzhan Barbante, Carlo Sachse, Dirk |
| author_facet | Aichner, Bernhard Callegaro, Alice van der Meer, Marcel T J Wünnemann, Bernd Yan, Dada Zhang, Yongzhan Barbante, Carlo Sachse, Dirk |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Concentrations of alkenones were analysed in core H7 from Hala Hu, China by means of an Agilent 7890A gas chromatography (GC) instrument, equipped with a mass selective detector (MSD; Agilent 5975C Series) and a flame ionization detector (FID; Agilent 7683B Series). For the GC, an Agilent VF-200ms column (60 m, inner diameter 0.25 mm, film thickness 0.25 μm) was used. The lake is located on the northern margin of the Tibetan Plateau (97.24 - 97.47°E, 38.12 - 38.25°N, 4078 m above sea level), along the modern marginal zone between the Asian Summer Monsoon (ASM) and westerlies influences. The core was drilled at the deepest point (65 m water depth) of the lake and extends from 212 to 636 cm sediment depth. According to the age-model (Yan et al., 2020) the covered time period is 7462 - 23610 cal yr BP. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_933821 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Concentrations of alkenones in Hala Hu sediment core H7 Aichner, Bernhard Callegaro, Alice van der Meer, Marcel T J Wünnemann, Bernd Yan, Dada Zhang, Yongzhan Barbante, Carlo Sachse, Dirk Alkenone; Alkenone, C37:2, per unit sediment mass; Alkenone, C37:3, per unit sediment mass; Alkenone, C37:4, per unit sediment mass; Alkenone, C38:2, per unit sediment mass; Alkenone, C38:3, per unit sediment mass; Alkenone, C38:4, per unit sediment mass; Alkenone, C39:2, per unit sediment mass; Alkenone, C39:3, per unit sediment mass; Alkenone, C39:4, per unit sediment mass; Biomarker; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; China; DEPTH, sediment/rock; Gas chromatography - mass spectrometry - flame ionization detector (GC/MS/FID) Agilent; H7; Hala_Hu_2010-H7; Hala Hu; isotopes; Niederreiter Piston corer; NPC; Paleoclimate; Sediment core; Tibetan Plateau Concentrations of alkenones were analysed in core H7 from Hala Hu, China by means of an Agilent 7890A gas chromatography (GC) instrument, equipped with a mass selective detector (MSD; Agilent 5975C Series) and a flame ionization detector (FID; Agilent 7683B Series). For the GC, an Agilent VF-200ms column (60 m, inner diameter 0.25 mm, film thickness 0.25 μm) was used. The lake is located on the northern margin of the Tibetan Plateau (97.24 - 97.47°E, 38.12 - 38.25°N, 4078 m above sea level), along the modern marginal zone between the Asian Summer Monsoon (ASM) and westerlies influences. The core was drilled at the deepest point (65 m water depth) of the lake and extends from 212 to 636 cm sediment depth. According to the age-model (Yan et al., 2020) the covered time period is 7462 - 23610 cal yr BP. |
| title | Concentrations of alkenones in Hala Hu sediment core H7 |
| topic | Alkenone; Alkenone, C37:2, per unit sediment mass; Alkenone, C37:3, per unit sediment mass; Alkenone, C37:4, per unit sediment mass; Alkenone, C38:2, per unit sediment mass; Alkenone, C38:3, per unit sediment mass; Alkenone, C38:4, per unit sediment mass; Alkenone, C39:2, per unit sediment mass; Alkenone, C39:3, per unit sediment mass; Alkenone, C39:4, per unit sediment mass; Biomarker; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; China; DEPTH, sediment/rock; Gas chromatography - mass spectrometry - flame ionization detector (GC/MS/FID) Agilent; H7; Hala_Hu_2010-H7; Hala Hu; isotopes; Niederreiter Piston corer; NPC; Paleoclimate; Sediment core; Tibetan Plateau |
| url | https://doi.org/10.1594/PANGAEA.933821 |