Characteristics and genesis of microbial lumps in the Maozhuang Stage (Cambrian Series 2), Shandong Province, China

被引:19
|
作者
Yang RenChao [1 ,2 ]
Fan AiPing [1 ]
Han ZuoZhen [1 ]
Chi NaiJie [3 ]
Han Yu [4 ]
机构
[1] Shandong Univ Sci & Technol, Coll Geol Sci & Engn, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Peoples R China
[2] SINOPEC, Petr Explorat & Prod Res Inst, Beijing 100083, Peoples R China
[3] Shandong Prov Expt Inst Geol Sci, Jinan 250013, Peoples R China
[4] China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
Cambrian; Maozhuang Stage; microbe; microbial lump; carbonate; ENVIRONMENTAL SIGNIFICANCE; CARBONATE PLATFORMS; SWISS JURA; FACIES; CLASSIFICATION; LIMESTONES; MOUNTAINS; POSITION; ALBERTA; ONCOIDS;
D O I
10.1007/s11430-012-4539-4
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Microbial lumps have been found in the Maozhuang Stage (Cambrian Series 2) in the Liangcheng section, Shandong Province, China. Their macro- and micro-scale features distinguish them from other carbonate particles such as intraclasts and oncoids. Most lumps have a coarse sand to pebble size. They were mostly rounded during sedimentation or combined to form irregular shapes. A distinct boundary is present between the lumps and the surrounding cement of sparry calcite. The lumps contain either no core at all or several irregular "cores", without a distinct inner texture. They are composed mainly of calcified (micritized) microbes, most likely cyanobacteria. The microbes drilled holes in carbonate grains, after which lumps formed by micritization, cementation, and agglutination by an extracellular polymeric substance (EPS) in a high-energy shallow-marine, subtidal environment. As the lumps are directly related to microbes, they should be considered as microbialites.
引用
收藏
页码:494 / 503
页数:10
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