Benthic foraminiferal assemblages and bottom water evolution off the Portuguese margin since the Middle Pleistocene
Guo, QM (郭启梅)1,2; Li, BH (李保华)1; Kim, JK3
2017-03
发表期刊Global and Planetary Change
ISSN0921-8181
卷号150页码:94-108
摘要

The upper 250 meter-long sediment core of Site U1391 (1085 m water depth) retrieved from the Portuguese margin in the Northeast Atlantic Ocean was adopted for the benthic foraminiferal analyses to disclose the variations in Mediterranean Outflow Water (MOW) intensity over the last similar to 0.9 Ma. Benthic foraminifera are abundant at this site and mainly composed of the hyaline forms (80%, such as Cibicidoides/Cibicides spp., Globobulimina spp., Bulimina spp., Uvigerina spp., Melonis spp., Sphaeroidina bulloides, Hoeglundina elegans, Gyroidinoides spp., Lenticulina spp. and Planulina ariminensis), while the agglutinated and porcelaneous forms have only 5% and 14.1% on average, respectively.

关键词Benthic Foraminifera Portuguese Margin Mediterranean Outflow Water Middle-late Pleistocene
DOI10.1016/j.gloplacha.2016.11.004
收录类别SCI
语种英语
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000397370100007
出版者ELSEVIER SCIENCE BV
文献类型期刊论文
条目标识符http://ir.nigpas.ac.cn/handle/332004/13697
专题中国科学院南京地质古生物研究所
中国科学院南京地质古生物研究所
其他
作者单位1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Jiangsu, Peoples R China;
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China;
3.Korean Inst Ocean Sci & Technol, Ansan 426744, South Korea;
4.Texas A&M Univ, IODP, College Stn, TX USA
第一作者单位中国科学院南京地质古生物研究所
推荐引用方式
GB/T 7714
Guo, QM ,Li, BH ,Kim, JK. Benthic foraminiferal assemblages and bottom water evolution off the Portuguese margin since the Middle Pleistocene[J]. Global and Planetary Change,2017,150:94-108.
APA Guo, QM ,Li, BH ,&Kim, JK.(2017).Benthic foraminiferal assemblages and bottom water evolution off the Portuguese margin since the Middle Pleistocene.Global and Planetary Change,150,94-108.
MLA Guo, QM ,et al."Benthic foraminiferal assemblages and bottom water evolution off the Portuguese margin since the Middle Pleistocene".Global and Planetary Change 150(2017):94-108.
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