Abstract
Lower Cambrian buildups in the subsurface of the Nepsko-Botuobinsky anteclise in southern Central Siberia were investigated with respect to the geometry of the reefs and their biotic and lithological composition. The buildups of the Osinsky horizon are characterized by an abundance of non-skeletal and skeletal algae (Epiphyton, Renalcis, Markovella et. al.) which acted as binders, encrusters and probably also as framebuilders. Archaeocyathids are important elements in the climax communities of some successions. The buildup rocks are limestones and dolomites (algal boundstones, archaeocyathid/algal boundstones, algal wackestones and mudstones). Coarsegrained reef detritus is missing.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
