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Cenozoic planktonic foraminifera biostratigraphy from the South Atlantic Transect (International Ocean Discovery Program Expedition 390/393)

南大西洋断面新生代浮游有孔虫生物地层学（国际海洋发现计划远征 390/393）

基本信息

批准号：
NE/X002187/1
负责人：
Bridget Wade
金额：
$ 3万
依托单位：
University College London
依托单位国家：
英国
项目类别：
Research Grant
财政年份：
2022
资助国家：
英国
起止时间：
2022 至无数据
项目状态：
已结题

来源：
https://gtr.ukri.org/projects?ref=NE%2FX002187%2F1
关键词：
Cenozoic planktonic foraminifera biostratigraphy South

项目摘要

Planktonic foraminifera are microscopic, single celled organisms which live in great abundance throughout the world oceans, being important part of the microplankton fauna. They make up their shells from calcium carbonate, which they obtain form the surrounding sea water. Evolution and extinction events of fossil planktonic foraminifera are extensively studied and used to assess the age of the deep-sea sediments and to correlate sedimentary rock units when building reservoir models for oil and gas exploration. Analysis of chemical composition of planktonic foraminifera shells, also provide scientists with paleoenvironmental information, which tells us about the past environments and help us to understand the nature of ancient climatic conditions on our planet.This particular study however, focuses predominantly on biostratigraphic analysis of the sedimentary cores, which will be recovered during the IODP Expedition 390/393 South Atlantic Transect. Shipboard biostratigraphy will allow us to date each sample and produce preliminary age-depth model for all drilled sites, which is a basis for any palaeoceanographic research. Additional observations of planktonic foraminifera abundances, assemblage composition and state of test preservation, will allow to assess the research potential of the collected sample material. This will aid other scientists working on these sedimentary cores, to plan their research projects more effectively, in accordance with the expected sample material quality. Post cruise study will focus on more detailed investigation of evolutionary events of stratigraphically important taxa. This will provide new age calibrations from the subtropical real, allowing to produce more robust age models in future palaeoceanographic studies.

浮游有孔虫是一种微小的单细胞生物，在世界海洋中大量存在，是微型浮游生物动物群的重要组成部分。它们从周围的海水中获取碳酸钙来形成外壳。浮游有孔虫化石的演化和灭绝事件被广泛研究，并用于评估深海沉积物的年龄，并在建立油气勘探储层模型时关联沉积岩单元。浮游有孔虫壳的化学成分分析，也为科学家提供了古环境信息，它告诉我们过去的环境，帮助我们了解我们星球上古代气候条件的本质。然而，这项特别的研究主要集中在沉积岩心的生物地层学分析上，这些岩心将在IODP远征390/393南大西洋样带期间恢复。船上的生物地层学将使我们能够确定每个样本的年代，并为所有钻探地点建立初步的年龄深度模型，这是任何古海洋学研究的基础。对浮游有孔虫丰度、组合组成和试验保存状态的进一步观察，将有助于评估所收集样品材料的研究潜力。这将有助于其他研究这些沉积岩心的科学家，根据预期的样品材料质量，更有效地规划他们的研究项目。巡航后的研究将集中于更详细地调查地层学上重要分类群的进化事件。这将提供亚热带真实的新时代校准，允许在未来的古海洋学研究中产生更可靠的年龄模型。

项目成果

期刊论文数量（2）

专著数量（0）

科研奖励数量（0）

会议论文数量（0）

专利数量（0）

South Atlantic Transect

南大西洋横断面

DOI：
发表时间：
2024
期刊：
Proceedings of the International Ocean Discovery Program Expedition reports
影响因子：
0
作者：
Coggon, R.M.;Teagle, D.A.H.;Sylvan, J.B.;Reece, J.;Estes, E.R.;Williams, T.J.;Christeson, G.L.
通讯作者：
Christeson, G.L.

Expedition 393 Preliminary Report: South Atlantic Transect 2