Organic matter in upper Albian marine sediments in the High-Tatric units, central western Carpathians related to Oceanic Anoxic Event 1d—Geochemistry, microfacies and palynology
详细信息 查看全文
- 作者：Krzysztof Bąka ; sgbak@cyf-kr.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Monika Fabiańskab ; monika.fabianska@us.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Marta Bąkc ; martabak@agh.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Magdalena Misz-Kennanb ; magdalena.misz@us.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Magdalena Zielińskab ; magdalena.zielinska@us.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Paweł Dulembaa ; pdulemba@up.krakow.pl" class="auth_mail" title="E-mail the corresponding author ; Tomasz Bryndala ; tbryndal@up.krakow.pl" class="auth_mail" title="E-mail the corresponding author ; Beata Naglikc ; beata.naglik@op.pl" class="auth_mail" title="E-mail the corresponding author
- 关键词：Oceanic anoxic events ; Organic geochemistry ; Biomarkers ; Hemipelagic sediments ; Chemostratigraphy ; Tatra Mountains ; Carpathians
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：15 July 2016
- 年：2016
- 卷：454
- 期：Complete
- 页码：212-227
- 全文大小：3688 K
文摘
- •
Hemipelagic sediments of OAE1d contain mixed marine and land-derived organic matter.
- •
TOC content in the High-Tatric unit varies between 0.16–0.24.
- •
Organic matter input during OAE 1d was related to sea level rise.
- •
Late Albian climates changed during OAE 1d from arid to humid tropical.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |