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  • Dome C; Dome C, Antarctica; EDC; EDML; EDRILL; EPICA; EPICA-Campaigns; EPICA Dome C; EPICA drill; EPICA Dronning Maud Land, DML28C01_00; European Project for Ice Coring in Antarctica; ICEDRILL; Ice drill; Kohnen Station  (2)
  • 2,6,10,15,19-pentamethylicosane per unit sediment mass; Alkenone; 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; highly branched isoprenoid (HBI); Highly branched isoprenoids C20 per unit sediment mass; isotopes; n-alkane; n-Alkane C21, per unit sediment mass; n-Alkane C23, per unit sediment mass; n-Alkane C25, per unit sediment mass; n-Alkane C27, per unit sediment mass; n-Alkane C29, per unit sediment mass; n-Alkane C31, per unit sediment mass; n-Alkane C33, per unit sediment mass; n-Alkane C35, per unit sediment mass; n-alkene; n-Alkene C21:1 per unit sediment mass; n-Alkene C23:1 per unit sediment mass; n-Alkene C25:1 per unit sediment mass; n-Alkene C27:1 per unit sediment mass; Niederreiter Piston corer; NPC; Paleoclimate; Sediment core; Tibetan Plateau  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Dick, Dorothee; Wegner, Anna; Gabrielli, Paolo; Ruth, Urs; Barbante, Carlo; Kriews, Michael (2008): Rare earth elements determined in Antarctic ice by inductively coupled plasma-Time of flight, quadrupole and sector field-mass spectrometry: An inter-comparison study. Analytica Chimica Acta, 621(2), 140-147, https://doi.org/10.1016/j.aca.2008.05.026
    Publication Date: 2023-06-27
    Description: Inductively coupled plasma mass spectrometry (ICP-MS) is a suitable tool for multi-element analysis at low concentration levels. Rare earth element (REE) determinations in standard reference materials and small volumes of molten ice core samples from Antarctica have been performed with an ICP-time of flight-MS (ICP-TOF-MS) system. Recovery rates for REE in e.g. SPS-SW1 amounted to not, vert, similar ~103%, and the relative standard deviations were 3.4% for replicate analysis at REE concentrations in the lower ng/l range. Analyses of REE concentrations in Antarctic ice core samples showed that the ICP-TOF-MS technique meets the demands of restricted sample mass. The data obtained are in good agreement with ICP-Quadrupole-MS (ICP-Q-MS) and ICP-Sector Field-MS (ICP-SF-MS) results. The ICP-TOF-MS system determines accurately and precisely REE concentrations exceeding 5 ng/l while between 0.5 and 5 ng/l accuracy and precision are element dependent.
    Keywords: Dome C; Dome C, Antarctica; EDC; EDML; EDRILL; EPICA; EPICA-Campaigns; EPICA Dome C; EPICA drill; EPICA Dronning Maud Land, DML28C01_00; European Project for Ice Coring in Antarctica; ICEDRILL; Ice drill; Kohnen Station
    Type: Dataset
    Format: application/zip, 6 datasets
    Location Call Number Limitation Availability
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Ruth, Urs; Barbante, Carlo; Bigler, Matthias; Delmonte, Barbara; Fischer, Hubertus; Gabrielli, Paolo; Gaspari, Vania; Kaufmann, Patrik R; Lambert, Fabrice; Maggi, Valter; Marino, Federica; Petit, Jean Robert; Udisti, Roberto; Wagenbach, Dietmar; Wegner, Anna; Wolff, Eric William (2008): Proxies and measurement techniques for mineral dust in Antarctic ice cores. Environmental Science and Technology, 42(15), 5675-5681, https://doi.org/10.1021/es703078z
    Publication Date: 2023-11-28
    Description: To improve quantitative interpretation of ice core aeolian dust records a systematic methodical comparison has been made involving methods of water-insoluble particle counting (Coulter Counter and laser-sensing particle detector), soluble ions (ion chromatography, IC, and continuous flow analysis, CFA), elemental analysis (inductively coupled plasma mass spectroscopy, ICP-MS, at pH 1 and after full acid digestion), and water-insoluble elemental analysis (proton induced X-ray emission, PIXE). Ice core samples covering the last deglaciation have been used from the EPICA Dome C (EDC) and the EPICA Dronning Maud Land (EDML) ice cores. All methods correlate very well amongst each other. The ratios of glacial age concentrations to Holocene concentrations, which are typically a factor ~100, differ significantly between the methods, but differences are limited to a factor 〈 2 for most methods with insoluble particles showing the largest change. The recovery of ICP-MS measurements depends on the digestion method and is different for different elements and during different climatic periods. EDC and EDML samples have similar dust composition, which suggests a common dust source or a common mixture of sources for the two sites. The analysed samples further reveal a change of dust composition during the last deglaciation.
    Keywords: Dome C; Dome C, Antarctica; EDC; EDML; EDRILL; EPICA; EPICA-Campaigns; EPICA Dome C; EPICA drill; EPICA Dronning Maud Land, DML28C01_00; European Project for Ice Coring in Antarctica; ICEDRILL; Ice drill; Kohnen Station
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-06-12
    Description: Concentrations of aquatic (mid-chain n-alkenes, C20-HBIs) and terrestrial (long-chain n-alkanes) biomarker groups were analysed in core H7 from Hala Hu, China. The compounds were quantified relative to an internal standard (5α-androstane) using 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, a Restek DB-5 column (30 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) 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.
    Keywords: 2,6,10,15,19-pentamethylicosane per unit sediment mass; Alkenone; 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; highly branched isoprenoid (HBI); Highly branched isoprenoids C20 per unit sediment mass; isotopes; n-alkane; n-Alkane C21, per unit sediment mass; n-Alkane C23, per unit sediment mass; n-Alkane C25, per unit sediment mass; n-Alkane C27, per unit sediment mass; n-Alkane C29, per unit sediment mass; n-Alkane C31, per unit sediment mass; n-Alkane C33, per unit sediment mass; n-Alkane C35, per unit sediment mass; n-alkene; n-Alkene C21:1 per unit sediment mass; n-Alkene C23:1 per unit sediment mass; n-Alkene C25:1 per unit sediment mass; n-Alkene C27:1 per unit sediment mass; Niederreiter Piston corer; NPC; Paleoclimate; Sediment core; Tibetan Plateau
    Type: Dataset
    Format: text/tab-separated-values, 1615 data points
    Location Call Number Limitation Availability
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