Biodiversity of Early-Middle Ordovician acritarchs and sea level changes in South China
Yan, K (燕夔); Li, Jun (李军); Liu, JB
2005-10-01
发表期刊CHINESE SCIENCE BULLETIN
ISSN1001-6538
卷号50期号:20页码:2362-2368
摘要

As the primary producers, acritarchs represent the base of the food chain in the Paleozoic marine ecosystem which links with the evolution of acritarchs. Based on high precision quantitative research, much information about Paleozoic marine ecosystem is provided. A quantitative analysis of Early-Middle Ordovician acritarch diversity changes in the Meitan Formation, Honghuayuan section, Tongzi, Guizhou is made and the the acritarch diversity curves are compared with sea level curves. We found that acritarch diversity changes were related to sea level changes during the Early-Middle Ordovician. Whereas sea level rose, and acritarch diversity also increased. An inshore-offshore model of acritarchs best explains the relative abundance changes of some acritarch taxa in relation to sea level changes.

关键词Acritarchs Diversity Sea Level Changes Early-middle Ordovician South China
DOI10.1360/982005-165
语种英语
关键词[WOS]Microphytoplankton ; Diversity
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:000234331800018
出版者SCIENCE PRESS
文献类型期刊论文
条目标识符http://ir.nigpas.ac.cn/handle/332004/646
专题中国科学院南京地质古生物研究所
其他
通讯作者Li, Jun (李军)
作者单位1.Chinese Acad Sci, Nanjing Inst Geol & Paleontol, Nanjing 210008, Peoples R China
2.Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
3.Grad Univ, Chinese Acad Sci, Beijing 100049, Peoples R China
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Yan, K ,Li, Jun ,Liu, JB. Biodiversity of Early-Middle Ordovician acritarchs and sea level changes in South China[J]. CHINESE SCIENCE BULLETIN,2005,50(20):2362-2368.
APA Yan, K ,Li, Jun ,&Liu, JB.(2005).Biodiversity of Early-Middle Ordovician acritarchs and sea level changes in South China.CHINESE SCIENCE BULLETIN,50(20),2362-2368.
MLA Yan, K ,et al."Biodiversity of Early-Middle Ordovician acritarchs and sea level changes in South China".CHINESE SCIENCE BULLETIN 50.20(2005):2362-2368.
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