Late Neogene–Quaternary Planktic Foraminiferal Biostratigraphy and Biochronology from ODP Site 807A, Ontong Java Plateau, Western Equatorial Pacific

IF 0.9 4区 地球科学 Q4 PALEONTOLOGY Journal of Foraminiferal Research Pub Date : 2020-04-01 DOI:10.2113/gsjfr.50.2.111
Tushar Kaushik, A. Singh, D. K. Sinha
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引用次数: 3

Abstract

A biostratigraphic and biochronological study from the late Neogene–Quaternary section of Ocean Drilling Program (ODP) Site 807A, located on the Ontong Java Plateau, western equatorial Pacific, revealed 50 planktic foraminiferal events, enabling the identification of eight late Neogene–Quaternary biozones, from the Globorotalia plesiotumida Interval Zone to the Globorotalia truncatulinoides Interval Zone. A significant faunal turnover (17 events) from late Pliocene identified in cores 7 and 8, between 70 and 55 meters below seafloor (mbsf), and spanning 0.67 million years (Myr). This noteworthy turnover may be the result of a shift in oceanographic conditions pertaining to the closure of the Indo–Pacific Seaway, followed by the Northern Hemisphere Glaciation. This study provides a high resolution biostratigraphic and biochronological framework for ODP Site 807A that will aid in correlation and timing the various paleoceanographic changes over the last 6 million years in the western equatorial Pacific.
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西赤道太平洋Ontong爪哇高原ODP 807A遗址晚新近系-第四纪浮游有孔虫生物地层及生物年代学
位于赤道太平洋西部翁通爪哇高原的海洋钻探项目(ODP)807A场地晚第三纪-第四纪剖面的生物地层学和生物矿物学研究揭示了50个浮游有孔虫事件,从而确定了8个晚第三代-第四纪生物带,从蛇尾圆辐虫间隔带到截头圆辐虫区间带。在海底以下70至55米(mbsf)的7号和8号岩心中发现了上新世晚期的一次重大动物群更替(17次事件),跨度为67万年(Myr)。这一值得注意的更替可能是与印度洋-太平洋航道关闭有关的海洋学条件发生变化的结果,随后是北半球冰川作用。本研究为ODP站点807A提供了一个高分辨率的生物地层学和生物岩石学框架,这将有助于对比和确定赤道太平洋西部过去600万年中各种古海洋学变化的时间。
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来源期刊
Journal of Foraminiferal Research
Journal of Foraminiferal Research 地学-古生物学
CiteScore
2.10
自引率
9.10%
发文量
32
审稿时长
>12 weeks
期刊介绍: JFR publishes original papers of international interest dealing with the Foraminifera and allied groups of organisms. Review articles are encouraged.
期刊最新文献
2023 Cushman Foundation for Foraminiferal Research Award and Grant Recipients The Later Holocene Foraminifera of Liverpool Bay (Bae Lerpwl), British Isles: Morphospecies and Community Level Patterns Micro- to Macro-Scale Foraminiferal Distributions: The Contributions of Martin A. Buzas* Oceanic-Scale Species Diversity of Living Benthic Foraminifera: Insights into Neogene Diversity, Community Structure, Species Duration, and Biogeography Benthic Foraminiferal Response to the Aptian−Albian Carbon Cycle Perturbation in the Atlantic Ocean
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