Document Type
Thesis
Abstract
The Solite Quarry, located in the Triassic Danville Basin, is a Lagerstitte comprised of microlaminated shales that preserve an exceptional record of late Triassic insect diversity. Present in rocks from the 3 cm-thick “insect layer” are two-dimensional carbonized remains of members of an unidentified nepomorphan family. Because of the nature of their two-dimensional preservation, potential analyses are limited. This is further complicated by the fact that much of the thorax is obscured by the legs in most specimens. The goal of my research is to utilize eigenshape analysis on high-resolution photos of these insects to determine which modern nepomorphan family they are most similar to in shape and size. To accomplish this, I used TpsDig2 to collect 100 equallyspaced x, y coordinates around the six proximal leg elements of 172 unidentified Solite nepomorphans from the Virginia Museum of Natural History paleontology collections. | selected specimens that were preserved in the same orientation and with the same level of taphonomic detail. I then outlined the analogous parts of approximately 30 specimens each from four different modern nepomorphan families: Notonectidae, Corixidae, Belostomatidae, and Naucoridae. Each outline was subjected to a standard eigenshape analysis, standardizing for body size, rotation, and translation. Results from the modern families were compared to the fossil material to determine the degree of morphological similarity. Preliminary results suggest the preserved part of the insects in question is most similar in morphology to Belostomatidae. Understanding the relationship these insects have to modern nepomorphans will help us to better understand the significance of Solite with regard to the evolutionary development of the infraorder.
Date Awarded
2016
Department
Geology
Advisor 1
Rowan Lockwood
Recommended Citation
Turk, Katherine A., "Eigenshape Analysis as a Tool for Family-level Identification of Nepomorphans from the Solite Lagerstätte (Triassic, Virginia)" (2016). Geology Senior Theses. William & Mary. Paper 382.
https://scholarworks.wm.edu/geologyseniors/382