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Watanabe, Yoshio; Matsumoto, Ryo; Lu, Hailong (2000): Geochemical composition of sediments from ODP Site 164-997, Blake Ridge [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.803967, Supplement to: Watanabe, Y et al. (2000): Data Report: Trace element geochemistry of the Blake Ridge sediments at Site 997. In: Paull, CK; Matsumoto, R; Wallace, PJ; Dillon, WP (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 164, 1-13, https://doi.org/10.2973/odp.proc.sr.164.223.2000

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Abstract:
Twenty-two trace elements in 355 sediment samples from Site 997 on the Blake Ridge were examined by inductively coupled plasma-optical emission spectrometry and inductively coupled plasma-mass spectrometry, for respective fractions of acid-soluble and insoluble compositions. Downhole profiles of these elements exhibit complicated fluctuations throughout late Miocene to Pleistocene, principally due to the variations in the acid-soluble fraction. Noncarbonate composition is given from the acid-insoluble residues, which permits us to recognize secular feature of selected element variance for four intervals. These intervals (I: 0-183 mbsf; II: 183- 440 mbsf; III: 440-618 mbsf; and IV: 618-750 mbsf) are interpreted to have originated from changes in the suite of sediments of particular sources and chemical composition, sedimentation rate, dilution of biogenic carbonate abundance, and possibly the current system that controlled deposition and reworking of the terrigenous materials.
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Coverage:
Median Latitude: 31.843167 * Median Longitude: -75.468567 * South-bound Latitude: 31.843100 * West-bound Longitude: -75.468600 * North-bound Latitude: 31.843300 * East-bound Longitude: -75.468500
Date/Time Start: 1995-12-06T12:35:00 * Date/Time End: 1995-12-17T07:25:00
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3 datasets

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