Doctor of Philosophy, The Ohio State University, 2016, Geological Sciences
The Waukesha Lagerstatte in the Brandon Bridge Formation (Silurian: Llandovery Series, Telychian Stage) hosts a diverse, exceptionally preserved fauna. Similar to a number of other Silurian Lagerstatten in Laurentia, it was deposited on a warm, shallow-marine carbonate platform. The Waukesha Biota includes an interesting assemblage of organisms, some of which are characteristic of Silurian epeiric seas, others of which are expected but rare in the Silurian, and still others that could be considered “holdovers” of groups more characteristic of the Cambrian.
The Waukesha Lagerstatte hosts a diverse biota of metazoans that are mostly marine but also probably some terrestrial forms. Taxa include biomineralized trilobites, conulariids, Sphenothallus, and a variety of non-biomineralized or lightly skeletonized arthropods, lobopodians, `worms,' a cubozoan, chordates, and graptolites. Echinoderms, cephalopods, brachiopods, gastropods, bivalves, bryozoans, and corals, which are biomineralized and normally common in Silurian shelf lithofacies, are rare or unknown.
The Waukesha Lagerstatte substantially increases our understanding of the biota of Silurian carbonate platform ecosystems. Many of the taxa are represented by similar organisms in other less well-known Silurian Lagerstatten. The existence of the diverse Waukesha Biota is the result of specific taphonomic processes related to localized and atypical depositional conditions. Microbial processes contributed in important ways to exceptional preservation in this deposit.
Committee: Loren Babcock PhD (Advisor); William Ausich PhD (Committee Member); Hunter John PhD (Committee Member); Lower Steven PhD (Committee Member); Feldmann Rodney PhD (Other)
Subjects: Biology; Earth; Ecology; Geology; Microbiology; Paleontology