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- W193600096 abstract "Microbialite units are commonly found within the Mesozoic–Tertiary carbonate succession of the Karst District of Slovenia and Italy. They record environmental conditions, which are linked with both local and global events. Local events are recorded by scattered occurrences and are mostly related to changes in the hydrodynamic regime of the platform and/or synsedimentary tectonics, which are responsible for rapid environmental changes. In addition, freshwater stromatolites indicate periodic continental influences. Global events are recorded by more or less continuous units of microbialite, which can be related to sea-level changes, as documented in the Turonian (regressive oncoid limestones) and the Maastrichtian, K/T boundary and basal Danian (peritidal limestones linked with Milankovichć cycles). In general, the microbialites provide evidence of environments where the higher order organic community declined and disappeared, after having tolerated a drastic variability. Below the microbialite units, the community was usually poorly diversified and composed of opportunistic taxa, such as small foraminifers (agglutinated forms, miliolids, discorbids and nonionids), thin-shelled gastropods and ostracods. The same or similar benthic taxa appeared again above the microbialite units indicating their ability to reestablish in the environment especially after peritidal conditions. Microbialite deposits are more evident and thicker in the Slovenia Karst District (Dolenja Vas and Sopada sections) than the Italian part (Padriciano sections)." @default.
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- W193600096 date "2011-01-01" @default.
- W193600096 modified "2023-09-27" @default.
- W193600096 title "Microbialites as Markers of Biotic and Abiotic Events in the Karst District, Slovenia and Italy" @default.
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- W193600096 doi "https://doi.org/10.1007/978-94-007-0397-1_11" @default.
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