THE SIGNIFICANCE OF EROSIONAL FEATURES FOUND IN THE MIDDLE DEVONIAN GENESEO SHALE
Petrographic and small-scale sedimentary features were examined in a core and in thin sections for the entire Geneseo succession, in order to arrive at an improved understanding of mudstone facies and paleodepositional environment. The lower Geneseo is a banded black shale, representing more rapid deposition and surficial mixing by benthos (“cryptobioturbation”). The middle Geneseo exhibits multiple dark gray-black shale cycles, bounded by erosional surfaces often marked by a thin lag. These, interpreted as parasequences, probably reflect fluctuations in sea-level. Dark gray muds display thin silt lags and laminae at the base, and an increase in macroscopic bioturbation and homogenization upwards, grading into the pyritic black muds that exhibit lamination, erosional silt lags and “cryptobioturbation”. These cycles decrease in thickness upsection and grade into dark gray shales with scours, wave and current ripples, and macroscopically visible bioturbation. The upper Geneseo is marked by the Lodi Limestone, a thin silty carbonate concretionary unit that represents sediment starved conditions.
The Geneseo shale succession reflects the interplay between sediment supply and accommodation during a forced transgression, sequestering sediments further onshore and giving rise to an increase in offshore bottom current reworking and erosion. Erosional features and small scale sedimentary structures in the base of parasequences suggest an increase in sediment exposure and reworking (amalgamation) due to sediment starvation, and also is consistent with lower preservation potential of bioturbation features in basal portions of parasequences.