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Radiolaria occurrences of IODP Hole 386-M0082D

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PANGAEA2025-03-15 收录
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https://doi.pangaea.de/10.1594/PANGAEA.978996
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Results of radiolarian analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expedition took place between 2021-04-13 and 2021-06-01 onboard Japanese R/V Kaimei from and to Yokosuka, Japan, followed by an onshore phase onboard D/V Chikyu between 2022-02-14 – 2022-03-15. During the offshore phase, samples for radiolarian analyses were taken from the end of split cores at 2 m intervals. These were complemented during the onshore phase with samples from event layers identified from X-ray CT images. Samples in this dataset where categorized depending on their sedimentary regime by the following type key: E = event, H = hemipelagic, ? = unknown. Slides prepared from these samples were partially examined at 50× to 400× using a Zeiss Axio Imager.A1m POL-1 optical microscope on board Chikyu.

本数据集收录国际大洋发现计划(International Ocean Discovery Program, IODP)386航次(日本海沟古地震学)指定钻孔的放射虫分析成果。该航次包含两个作业阶段:海上作业阶段于2021年4月13日至2021年6月1日期间开展,搭载日本科考船"开南号"(R/V Kaimei)从日本横须贺出发并返航;陆上作业阶段则于2022年2月14日至2022年3月15日期间在"地球号"(D/V Chikyu)钻探船上完成。海上作业阶段中,放射虫分析样品以2米间隔取自劈开岩心的末端;陆上作业阶段补充采集了通过X射线计算机断层扫描(X-ray CT)图像识别得到的事件层样品。本数据集内的样品依据其沉积环境类型,通过以下分类标识进行区分:E代表事件沉积层,H代表半远洋沉积层,?代表沉积环境未知。由上述样品制备的显微薄片,部分在"地球号"船上使用蔡司(Zeiss)Axio Imager.A1m POL-1型光学显微镜,以50×至400×的放大倍率完成观测。
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