Neodymium isotopic composition and concentration in the Southwest Pacific Ocean

  • AMAKAWA HIROSHI
    High-precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University Atmosphere and Ocean Research Institute, The University of Tokyo
  • TAZOE HIROFUMI
    Institute of Radiation Emergency Medicine, Hirosaki University
  • GAMO TOSHITAKA
    Atmosphere and Ocean Research Institute, The University of Tokyo
  • OBATA HAJIME
    Atmosphere and Ocean Research Institute, The University of Tokyo
  • SANO YUJI
    Atmosphere and Ocean Research Institute, The University of Tokyo
  • SHEN CHUAN-CHOU
    High-precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University

書誌事項

公開日
2013
資源種別
journal article
DOI
  • 10.2343/geochemj.2.0260
公開者
一般社団法人日本地球化学会

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説明

We report two vertical profiles of the concentration and isotopic composition of neodymium (Nd) in seawater samples collected at 20°S and 30°S along a longitude of 170°W in the Southwest Pacific Ocean. At depths below 500 m, Nd isotopic composition values are less radiogenic than those obtained from the subtropical North Pacific. The minimum εNd values of -8.0 and -6.9 at depths of 800 to 1000 m correspond to Antarctic Intermediate Water (AAIW). The differences in εNd values between upper deep water (2000-3000 m) and lower deep water (>4000 m) seem to be associated with Upper and Lower Circumpolar Deep Waters (UCDW and LCDW, respectively). The radiogenic Nd supply to AAIW from the Society Islands is estimated to be 30 ± 22 tons Nd/yr, which is consistent with the estimates from previous studies conducted in the same location and the oceanic region close to the Hawaiian Islands. Our study demonstrates the uniqueness of Nd isotopic composition distributions in the Southwest Pacific Ocean. These results may be valuable for tracing present and past ocean circulation in this region.

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