山东东营凹陷古近纪湖相藻礁群落结构及古生态特征

李国山; 王永标; 卢宗盛; 廖卫; 侯玮伟

doi:10.3799/dqkx.2011.110

Volume 36 Issue 6

Jun. 2011

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Article Navigation > Earth Science > 2011 > 36(6): 1044-1052

LI Guo-shan, WANG Yong-biao, LU Zong-sheng, LIAO Wei, HOU Wei-wei, 2011. Community Structure and Paleoecology of Paleogene Lacustrine Cladosiphonia Reefs in the Dongying Depression, Shandong Province, China. Earth Science, 36(6): 1044-1052. doi: 10.3799/dqkx.2011.110

Citation:

LI Guo-shan, WANG Yong-biao, LU Zong-sheng, LIAO Wei, HOU Wei-wei, 2011. Community Structure and Paleoecology of Paleogene Lacustrine Cladosiphonia Reefs in the Dongying Depression, Shandong Province, China. Earth Science, 36(6): 1044-1052. doi: 10.3799/dqkx.2011.110

Citation:

LI Guo-shan, WANG Yong-biao, LU Zong-sheng, LIAO Wei, HOU Wei-wei, 2011. Community Structure and Paleoecology of Paleogene Lacustrine Cladosiphonia Reefs in the Dongying Depression, Shandong Province, China. Earth Science, 36(6): 1044-1052. doi: 10.3799/dqkx.2011.110

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Community Structure and Paleoecology of Paleogene Lacustrine Cladosiphonia Reefs in the Dongying Depression, Shandong Province, China

doi: 10.3799/dqkx.2011.110

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2011-06-09
Available Online: 2021-11-10
Publish Date: 2011-06-15

Abstract

Abstract

Most fossil reefs found so far are preserved in marine sediments with high biodiversity of reef-building organisms and recognized as implication for shallow normal marine environment. However, lacustrine reefs are relatively scarce and usually constructed by low biodiversity but high abundance of reef associated fossils, implying specialized water conditions. The frame of Paleogene lacustrine reefs in Dongying depression of Shandong Province were constructed mainly by Cladosiphonia and bound by Cyanobacteria. Reef-dwelling organisms are of great abundance though only a few species are involved, such as ostracodes, micro-gastropods and spirorbis, which belong to euryhaline organisms. Large amount of fibrous calcite cement was formed as the product of early diagenesis around the Cladosiphonia, reinforcing the solidity of reef structure. Early diagenesis cement widely formed in the reef structure suggests high saturation of lacustrine chemistry for carbonate precipitation. Paleogene is a special stage in geologic history, during which different types of evaporates were deposited all over the world. Paleogene Cladosiphonia-build reefs in Dongying depression should have been formed under arid climate conditions. Cladosiphonia-build reefs undoubtedly facilitates the understanding of the palaeoecology of ancient lacustrine and the condition of paleoclimate, and is of great importance to the study of petroleum reservoir as well.
- reefs,
- Paleogene,
- Dongying depression,
- stratigraphy

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Community Structure and Paleoecology of Paleogene Lacustrine Cladosiphonia Reefs in the Dongying Depression, Shandong Province, China

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