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A database of paleoceanographic sediment cores from the North Pacific, 1951–2016

机译:1951–2016年来自北太平洋的古海洋沉积岩心数据库

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We assessed sediment coring, data acquisition, and publications from the North Pacific (north of 30°?N) from 1951 to 2016. There are 2134 sediment cores collected by American, French, Japanese, Russian, and international research vessels across the North Pacific (including the Pacific subarctic gyre, Alaskan gyre, Japan margin, and California margin; 1391 cores), the Sea of Okhotsk (271 cores), the Bering Sea (123?cores), and the Sea of Japan (349 cores) reported here. All existing metadata associated with these sediment cores are documented here, including coring date, location, core number, cruise number, water depth, vessel metadata, and coring technology. North Pacific sediment core age models are built with isotope stratigraphy, radiocarbon dating, magnetostratigraphy, biostratigraphy, tephrochronology, %?opal, color, and lithological proxies. Here, we evaluate the iterative generation of each published age model and provide comprehensive documentation of the dating techniques used, along with sedimentation rates and age ranges. We categorized cores according to the availability of a?variety of proxy evidence, including biological (e.g., benthic and planktonic foraminifera assemblages), geochemical (e.g., major trace element concentrations), isotopic (e.g., bulk sediment nitrogen, oxygen, and carbon isotopes), and stratigraphic (e.g., preserved laminations) proxies. This database is a?unique resource to the paleoceanographic and paleoclimate communities and provides cohesive accessibility to sedimentary sequences, age model development, and proxies. The data set is publicly available through PANGAEA at https://doi.org/10.1594/PANGAEA.875998.
机译:我们评估了1951年至2016年北太平洋(北纬30°N以北)的沉积物取芯,数据采集和出版物。美国,法国,日本,俄罗斯和国际研究船在北太平洋收集了2134个沉积物岩心(包括太平洋亚弧环流,阿拉斯加环流,日本边缘和加利福尼亚边缘; 1391芯),鄂霍次克海(271芯),白令海(123芯)和日本海(349芯) 。与这些沉积物岩心相关的所有现有元数据都在此处记录,包括取心日期,位置,岩心编号,巡航编号,水深,船舶元数据和取心技术。北太平洋沉积物核心年龄模型是用同位素地层学,放射性碳测年,磁地层学,生物地层学,年代学,%岩石,颜色和岩性代理建立的。在这里,我们评估每个发布的年龄模型的迭代生成,并提供所用测年技术的全面文档,以及沉降速率和年龄范围。我们根据可用的各种替代证据对岩心进行分类,包括生物学的(例如底栖和浮游的有孔虫组合),地球化学的(例如主要微量元素浓度),同位素(例如大量的沉积氮,氧和碳同位素) )和地层(例如保留的叠片)代理。该数据库是古海洋和古气候社区的唯一资源,并为沉积序列,年龄模型的发展和代理提供了内聚的可访问性。该数据集可通过PANGEA在https://doi.org/10.1594/PANGAEA.875998上公开获得。

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