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  1. 広島大学の刊行物
  2. Journal of science of the Hiroshima University. Series C, Earth and planetary sciences
  3. 11巻2号

Tide-induced reworking of planktonic foraminifers on the outer shelf and slope off the Miyako Island, southern Ryukyus, Japan: Preliminary results

https://doi.org/10.15027/53169
https://doi.org/10.15027/53169
7f331ed7-b86f-4338-b9c7-3d5ee0e49260
名前 / ファイル ライセンス アクション
JSHUCE_11-2_239.pdf JSHUCE_11-2_239.pdf (2.7 MB)
Item type デフォルトアイテムタイプ_(フル)(1)
公開日 2023-03-18
タイトル
タイトル Tide-induced reworking of planktonic foraminifers on the outer shelf and slope off the Miyako Island, southern Ryukyus, Japan: Preliminary results
言語 en
作成者 SAKAI, Saburo

× SAKAI, Saburo

en SAKAI, Saburo

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KANO, Akihiro

× KANO, Akihiro

en KANO, Akihiro

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OHTSUKA, Susumu

× OHTSUKA, Susumu

en OHTSUKA, Susumu

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NAKAGUCHI, Kazumitsu

× NAKAGUCHI, Kazumitsu

en NAKAGUCHI, Kazumitsu

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Go, Akio

× Go, Akio

en Go, Akio

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
内容記述
内容記述 Significance of sediment reworking to a shallower environment is preliminarily discussed by occurrences and oxygen isotopes of planktonic foraminifer (Globolotalia inflata) tests collected from the sea bottom sediments on the insular shelf to slope, off the Miyako Islands, southern Ryukyus, Japan. The isotopic data and comparison with the present water temperature-depth profile indicate that vertical distribution of G. inflata with size of 300-355µm ranges from 135 to 250m (average 160m). Strong tidal currents between the East China Sea and the Pacific Ocean developed in the study area may induce the transpotation of sediment particles to a shallower environment. This is demonstrated by the occurrences of this species in sediment deposited in depth shallower than inhabiting depth. The analyzed tests were not altered by long-time contact with bottom water because they preserve surface structures and a narrow range of oxygen isotopic composition. Shortly after G. inflata died and settled on sea bottom, the tests were commonly transported to the shallower environment by the upwelling, which may result from strong tidal currents and the topographic feature of the Ryukyu Island Arc.
言語 en
出版者
出版者 Hiroshima University
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.15027/53169
ID登録タイプ JaLC
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 0075-4374
収録物識別子
収録物識別子タイプ NCID
収録物識別子 AA11095875
開始ページ
開始ページ 239
書誌情報 Journal of science of the Hiroshima University. Series C, Earth and planetary sciences
Journal of science of the Hiroshima University. Series C, Earth and planetary sciences

巻 11, 号 2, p. 239-246, 発行日 2003-08-25
旧ID 53169
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