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  • Carbon isotopes; loess plateau; magnetic susceptibility; Miocene; occluded organic matter; paleosol; pedogenic carbonate; Pliocene  (1)
  • Chinese Loess Plateau; detrital rutile; detrital zircon; eolian sediment; Miocene; Pliocene; Provenance; Red Clay  (1)
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  • 1
    Publication Date: 2023-03-01
    Description: The data were collected for a joint detrital zircon and detrital rutile provenance study of the late Neogene aeolian Baode Red Clay, located on the northern part of the Chinese Loess Plateau. The data consist of detrital zircon U-Pb ages of the 4.04–2.64 Ma Baode Red Clay (four samples from the Pliocene Jingle Formation and one sample from the 2.64 Ma Transitional Unit), and detrital rutile trace element geochemistry of the 6.91–2.64 Ma Baode Red Clay (three samples from the Miocene Baode Formation, five samples from the Pliocene Jingle Formation, and one sample from the Transitional Unit) and 14 potential sedimentary source areas in Central-East Asia. The data were collected using Nu Plasma AttoM single collector ICP-MS (Nu Instruments Ltd., Wrexham, UK) connected to an Analyte Excite 193 ArF laser ablation system (Photon Machines, San Diego, USA) at the Geological Survey of Finland. The rutiles were analysed for Li, Mg, Al, Si, P, Ca, Sc, V, Cr, Mn, Fe, Co, Ni, Cu, Zn, Rb, Sr, Y, Zr, Nb, Mo, Sn, Sb, Ba, La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Hf, Ta, W, Pb, Th, and U. The grain size fractions of the analysed grains were mostly 30–90 μm for the Red Clay zircons and rutiles, and 20–500 μm for the potential source area rutiles.
    Keywords: Chinese Loess Plateau; detrital rutile; detrital zircon; eolian sediment; Miocene; Pliocene; Provenance; Red Clay
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-02-05
    Description: Pedogenic carbonate carbon isotope data, occluded organic matter carbon isotope data, and bulk magnetic susceptibility data are from the Jiaxian section of the Chinese Loess Plateau. Samples were collected from the field in July, 2017. Between 1 and 16 discrete pedogenic carbonate nodules were collected from 121 different depths over a 58-meter section. Separate bulk loess samples were collected every 10 cm for magnetic susceptibility analyses. 697 individual nodules were drilled and their carbonate δ13C values were measured at the University of Texas Stable Isotope Laboratory. Between 1 and 16 nodules were analyzed for each respective depth. When enough material was available (668 nodules), splits of the samples were acidified and rinsed before being analyzed for the δ13C values of occluded organic matter at the University of Texas Stable Isotope Laboratory. 17 and 109 replicate analyses are also included for carbonate and occluded organic matter, respectively. Magnetic susceptibility measurements were conducted at Nanjing University. Magnetic susceptibility data were used to correlate to previously published age models for the Jiaxian section that were based on paleomagnetic reversals.
    Keywords: Carbon isotopes; loess plateau; magnetic susceptibility; Miocene; occluded organic matter; paleosol; pedogenic carbonate; Pliocene
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Limitation Availability
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