49 Paleontology and Stratigraphy I

Tuesday, 21 March 2017
8:00 AM - 12:00 PM
Monongahela, 17th Floor

DETERMINING ENVIRONMENTAL PARAMETERS USING FAUNAL GRADIENTS IN THE UPPER ORDOVICIAN (KATIAN; RICHMONDIAN) ROWLAND MEMBER OF THE WAYNESVILLE FORMATION, CINCINNATI ARCH

Paper number: 49-5
Program: Technical Sessions
Time: 9:20 AM – 9:40 AM

Authors

Abstract

Ancient marine benthic assemblages arrayed gradationally along environmental gradients, can be quantified to provide proxies of ecological parameters, especially those related to water depth. However, while it is commonly possible to determine the relative position of a given facies or fossil community, it is far more difficult to assign absolute depths in terms of meters below sea level. However, absolute depth estimates can be made using a variety of sedimentary structures including indicators of shoreline exposure, normal wave base, and storm wave base, as well as biologic evidence of light-related zones.

The Upper Ordovician (Katian) Rowland Member (Waynesville Formation) in northern Kentucky provides an excellent opportunity to quantify faunal gradients in relation to absolute depth because recent high-resolution correlations permit recognition of transects that range from peritidal to deeper subtidal (30-40 m based on microendoliths) within single small-scale cycles. The configuration of depth-related facies within this interval thus provides a unique opportunity to assign fossil assemblages to quantitatively defined depth zones along a gently dipping carbonate ramp. The abundance of carbonized dasyclad algae within the deeper organic-rich clay facies indicates relatively shallow water depths (< 15 m), while the Skolithos facies (with verdine?), which contains desiccation cracks, can be placed near the shoreline (~ 0 m).

The Rowland Member also displays well-defined biofacies, each representative of a distinct lithologic facies which can be assigned to depth intervals, including: (a) scavenging ostracods and infaunal filter feeders (e.g., Skolithos and lingulid brachiopods) in the shallowest shaly facies; 0-5 m; (b) abundant deposit feeding organisms, epibyssate bivalves, free-resting bryozoans, and non-calcified algae in the shallow subtidal "lagoonal" facies (5-10 m) (c) prolific herbivorous? gastropods in high energy shoal facies (10-15m); and (d) a higher diversity (10-15 species) of filter feeding epifaunal brachiopods and ramose bryozoans, in offshore areas (15-40 m). The distinct biofacies present within this depositional system provide a rich temporal and environmental framework in which to study ecological-evolutionary patterns.

Geological Society of America Abstracts with Programs. Vol. 49, No. 2

doi: 10.1130/abs/2017NE-291421

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