首页> 外文期刊>Journal of foraminiferal research >LATE NEOGENE-QUATERNARY PLANKTIC FORAMINIFERAL BIOSTRATIGRAPHY AND BIOCHRONOLOGY FROM ODP SITE 807A, ONTONG JAVA PLATEAU, WESTERN EQUATORIAL PACIFIC
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LATE NEOGENE-QUATERNARY PLANKTIC FORAMINIFERAL BIOSTRATIGRAPHY AND BIOCHRONOLOGY FROM ODP SITE 807A, ONTONG JAVA PLATEAU, WESTERN EQUATORIAL PACIFIC

机译:晚期Neogene-Quationnary Planktic FainiferaRatigraphy和来自ODP Site 807a,Ontong Java Plateau,Western赤道太平洋的生物学

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摘要

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.
机译:来自海洋钻井计划(ODP)站点807a的晚间新生儿 - 四元段的生物数据和生物学研究,位于西赤道太平洋的Ontong Java高原,揭示了50个综合性传染率的事件,能够识别八个晚期新生儿生物氮杂,从Globorotaliosuifiotumida区间区间隔到Globorlatia truncatulinoides间隔区。从核心7和8中确定的晚期外科国的大型动物营业额(17次活动)在海底(MBSF)以下70到55米之间,跨越67万年(MYR)。这种值得注意的营业额可能是海洋环境转变的结果与印度太平洋海道的关闭,其次是北半球冰川。本研究为ODP站点807A提供了高分辨率的生物数据和生物学框架,这将有助于在西赤道太平洋过去600万年来各种古海洋变化的相关性和定时。

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