TIMING OF MORPHOLOGICAL CHANGE IN GASTROPODS DURING THE MID-PALEOZOIC PRECURSOR TO THE MESOZOIC MARINE REVOLUTION
Examining the diversity of pleurotomariinid gastropods through the Paleozoic reveals a rapid decline in the mid-Devonian, corresponding to the Frasnian-Famennian extinction. Pleurotomariinid gastropods through the Paleozoic manifest an overall increase in percent genera with potentially anti-predatory morphologies, particularly presence of nodes, from the Lower Devonian through the Lower Permian (Spearman's Ranked Correlation, r = 0.94, p < 0.001). While the diversity of pleurotomariinids declined in the Pennsylvanian, noded genera continued to increase in number. Pleurotomariinids with cords diversify from the lower to mid-Devonian while the overall diversity of pleurotomariinids rapidly declines. Average sphericity of pleurotomariinid genera also increases through the Paleozoic while the variance in sphericity decreases. This pattern could either be the result of selective pressures driving pleurotomariinids to more predator-resistant morphologies (spheres resist point-loading), or the result of functional constraints on pleurotomariniid morphology. These exploratory results need to be further examined through geographical analysis and predation traces.