Kansas Geological Survey
Open-file Report 2003-82
The bioclastic mudstone to wackestone facies is typically medium to dark gray in appearance with a micritic matrix. Diagnostic features include medium bedding (10-30 cm), abundant well-preserved whole-fossil marine bioclasts, and high-degree of bioturbation (Figure 2.10). Stylolites are commonly observed in the upper portion of the facies. Identified fossils include bryozoans, crinoids, brachiopods, mollusks, foraminifera, phyloid algae, and chaetetids. Thickness of the bioclastic-mudstone-to-wackestone facies ranges from 1 to 20 feet with an average of 12 feet (0.3 to 6 m; average of 4 m). Upper and lower contacts of the bioclastic-mudstone-to-wackestone facies with adjacent facies are gradational.
Bryozoans, brachiopods, phyloid algae, formainfera, chaetetids and crinoids indicate a normal salinity marine environment (Heckel, 1972). The presence of a micrite matrix is evidence of a low energy environment. Presence of well-preserved whole body fossils suggests a low-energy environment, probably below fair weather wave base. Disarticulation of bioclasts is due to bioturbation or storm activity. The combination of abundant and fragmented marine fauna, a micritic matrix, and texture suggests that the bioclastic-mudstone-to-wackestone facies was deposited in an open marine environment, probably below wave base. Historically, the bioclastic mudstone to wackestone facies would be interpreted as part of the “upper limestone” in the cyclothem model (Heckel, 1977).
|Figure 2.10 - Polished core section of bioclastic mudstone to wackestone facies with abundant whole fossil bioclasts. Note well persevation of bryozoans (A), chaetetes (B) and brachiopods (C). Sample 1 from 650' and sample 2 from 645' in the Hinthorn CW#1 well, 14-T32S-R16E, Montgomery County, Kansas|
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Last updated December 2003