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首页> 外文期刊>Deep-Sea Research >Bering Sea radiolarian biostratigraphy and paleoceanography at IODP Site U1341 during the last four million years
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Bering Sea radiolarian biostratigraphy and paleoceanography at IODP Site U1341 during the last four million years

机译:过去四百万年来IODP站点U1341的白令海放射虫生物地层学和古海洋学

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摘要

Radiolarian assemblages in sediment cores were investigated at the Integrated Ocean Drilling Program Site U1341 on Bowers Ridge in the southern Bering Sea. Radiolarian biozones at Site U1341 spanned the last 4 My from the youngest Amphimelissa setosa Zone (late Quaternary), via the Stylatractus universes Zone, the Eucyrtidium matuyamai Zone and a part of the Cycladophora sakaii Zone (middle to late Pliocene). The A. setosa Zone, newly proposed in this paper, is well correlated with the Botryostrobus aquilonaris Zone in the North Pacific Ocean. The bottom of the S. universus and top of the E. matuyamai Zones are emended in this paper by using the first common occurrence of A. setosa. Seventeen radiolarian datum points were identified at Site U1341 and tied to the geomagnetic and oxygen isotope stratigraphy. Radiolarian assemblages during the last 4 My showed a turnover from subarctic transitional species (Spongopyle osculosa and Larcopyle buetschlii) to subarctic species (Ceratospyris borealis) between 3.6 and 2.4 Ma, corresponding to the intensification of the Northern Hemisphere Glaciation (NHG). Recent polar species (A. setosa and Actinomma boreale) appeared abundantly after the Mid-Pleistocene Transition (MPT, 1.2-0.8 Ma). Repeated numbers of individual peaks of the abundances of Cycladophora davisiana, dwelling in cold and well-ventilated intermediate water, suggest intermediate to deep water formation in the Bering Sea during the last 1 My. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在白令海南部鲍尔斯里奇(Bowers Ridge)的海洋综合钻探计划站点U1341上研究了沉积物岩心中的放射虫组合。站点U1341上的放射虫生物区跨越最小的Amphimelissa setosa区(第四纪晚期),最后经过4 My,途经Stylatractus宇宙区,Eucyrtidium matuyamai区和Cycladophora sakaii区(上新世中期至晚期)。本文中新提出的A. setosa区与北太平洋的Botryostrobus aquilonaris区紧密相关。本文通过使用首次普遍出现的Set。A. setosa对S. universus的底部和E. matuyamai带的顶部进行了修改。在站点U1341上确定了17个放射虫基准点,并将其与地磁和氧同位素地层联系起来。最近4 My的放射虫组合显示了从弧下过渡物种(Spongopyle osculosa和Larcopyle buetschlii)到弧下物种(Ceratospyrisborealis)的翻转,介于3.6至2.4 Ma之间,这与北半球冰川(NHG)的加剧有关。在中更新世过渡(MPT,1.2-0.8 Ma)之后,最近的极地物种(A. setosa和放线放线菌)大量出现。居住在寒冷和通风良好的中间水域中的达斯达目环足莲的丰度的单个峰值的重复数目表明,在最后1 My期间,白令海的中间水形成了深水层。 (C)2015 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Deep-Sea Research》 |2016年第maraaap期|38-55|共18页
  • 作者单位

    Kyushu Univ, Grad Sch Sci, Dept Earth & Planetary Sci, Higashi Ku, 6-10-1 Hakozaki, Fukuoka 8128581, Japan|Marine Ecol Res Inst, Cent Lab, 300 Iwawada, Onjuku, Chiba 2995105, Japan;

    Kyushu Univ, Grad Sch Sci, Dept Earth & Planetary Sci, Higashi Ku, 6-10-1 Hakozaki, Fukuoka 8128581, Japan;

    Kyushu Univ, Grad Sch Sci, Dept Earth & Planetary Sci, Higashi Ku, 6-10-1 Hakozaki, Fukuoka 8128581, Japan|Hokusei Gakuen Univ, Atsubetsu Ku, 2-3-1 Oyachi, Sapporo, Hokkaido 0048631, Japan;

    Mie Univ, Fac Bioresources, 1577 Kurimamachiya Cho, Tsu, Mie 5148507, Japan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Radiolarians; Bering Sea; Biostratigraphy; Paleoceanography; Pliocene; Pleistocene; Integrated Ocean Drilling Program;

    机译:放射虫;白海;生物地层学;古海洋学;上新世;更新世;海洋综合钻探计划;

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