期刊
BULLETIN OF GEOSCIENCES
卷 85, 期 4, 页码 585-602出版社
CZECH GEOLOGICAL SURVEY
DOI: 10.3140/bull.geosci.1206
关键词
calcispheres; peloids; micritization; lime mud; Prague Basin; Devonian
资金
- Grant Agency of the Academy of Science [KJB 307020602]
- Czech-American Cooperation Program [Kontakt ME08011]
- Czech Geological Survey [3325, 3333, 323000]
- Palaeontological Association
Several types of peloids are present in the Lower and Middle Devonian limestones of the Prague Basin (uppermost part of the Trebotov Limestone of the Daleje-Trebotov Formation and Chotec Formation, uppermost Emsian-Eifelian) and are interpreted as being of calcispheral, echinoderm, and/or calcimicrobial origin. Possible mechanisms of peloid formation, the mode of life of calcispheres and their role in the accumulation of Paleozoic lime mud are discussed. Mass occurrences of peloids and calcispheres are characteristic features of the Chotec Formation (Eifelian, costatus-kockelianus conodont zones). It is concluded that specific environmental conditions, such as a higher nutrient load, existed during the sedimentation of this unit, probably in response to the Basal Chotec event.
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