Kansas Geological Survey
Open-file Report 2003-82
The pyritic black shale facies consists of micaceous dark gray to black shale. Diagnostic features include poorly developed irregular laminations (3 mm), and abundant pyritized wood and plant fragments (Figure 2.05). Angular pyrite concretions are approximately 0.25 inches in diameter (8 mm). Trace or body fossils were not observed in the pyritic black shale facies. Thickness of the pyritic shale facies ranges from 5 to 20 feet (1.5 to 6 m). Contacts with the overlying and underlying facies are gradational.
The abundance of pyrite concretions, pyritized plant material and poorly developed laminations suggest deposition from sediment fallout in a brackish water marginal marine environment. An abundance of pyrite nodules and associated plant fragments appears related to swamp or marsh environments (Ho and Coleman, 1969). No marine fossils were observed. The pyritic black shale facies is interpreted as being deposited in a brackish water, coastal marsh or swamp environment. Historically, the pyritic shale facies would be interpreted as part of the “outside shale” in the cyclothem model (Heckel, 1977).
|Figure 2.05 - Polished core section of the pyritic black shale facies. Note the development of irregular laminations (A) and angular pyrite concretions (B) of apporximately 0.25 inches in diameter (90 mm). The black appearance is due to a high organic content (i.e. carbonized wood fragments). Sample from 1,076' in the Hinthorn CW#1 well, 14-T32S-R16E, Montgomery County, Kansas|
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Last updated December 2003