NIGPAS OpenIR  > 中国科学院南京地质古生物研究所
Sea surface environment inferred from planktonic foraminifera in the southern South China Sea since the last glacial period
Li, B.-H.(李保华); Wang, X.-Y.; Jian, Z.-M.; Wang, P.-X.
2009
Source PublicationPalaeoworld
ISSN1871-174X
Volume18Issue:1Pages:23-33
Language英语
Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/4763
Collection中国科学院南京地质古生物研究所
其他
Recommended Citation
GB/T 7714
Li, B.-H.,Wang, X.-Y.,Jian, Z.-M.,et al. Sea surface environment inferred from planktonic foraminifera in the southern South China Sea since the last glacial period[J]. Palaeoworld,2009,18(1):23-33.
APA Li, B.-H.,Wang, X.-Y.,Jian, Z.-M.,&Wang, P.-X..(2009).Sea surface environment inferred from planktonic foraminifera in the southern South China Sea since the last glacial period.Palaeoworld,18(1),23-33.
MLA Li, B.-H.,et al."Sea surface environment inferred from planktonic foraminifera in the southern South China Sea since the last glacial period".Palaeoworld 18.1(2009):23-33.
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