A test of Bergmann’s rule in the Early Triassic: Latitude, body size, and sampling in Lystrosaurus

The ecogeographical rule known as Bergmann’s rule suggests that there is a positive relationship between body size and latitude when comparing closely related taxa. The underlying mechanism, or mechanisms, to explain this pattern vary as widely as the taxa that seem to follow it, which has led to skepticism over whether Bergmann’s rule should be considered a rule at all. Despite this, Bergmann’s rule is widespread among modern birds, mammals, beetles, and some amphibians, but far fewer extinct taxa have been subjected to tests of Bergmann’s rule. To test whether Bergmann’s rule is detected in extinct taxa, we compared body size proxies in Lystrosaurus recovered from Early Triassic-aged strata in Antarctica, South Africa, India, and China. Our results reveal that average body size is largest at mid-northern paleolatitudes (~45°N) instead of the highest southern paleolatitudes (~70°S). Additionally, maximum body size is consistent across northern and southern hemispheres, indicating that ..., We gathered cranial measurements from 482 Lystrosaurus skulls in order to compare body size proxies from Early Triassic specimens. Measurements were taken using Mitutoyo digital calipers (±0.02mm) at the following institutions: Burke Museum of Natural History and Culture, Washington, USA; American Museum of Natural History, New York, USA; Evolutionary Studies Institute, (formerly Bernard Price Institute for Paleontological Research), University of the Witwatersrand, Johannesburg, South Africa; The Field Museum of Natural History, Chicago, Illinois, USA;  Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China; National Museum, Bloemfontein, South Africa; Iziko, The South African Museum, Cape Town, South Africa. Measurement data were also compiled from a survey of the literature. , This Excel spreadsheet can be opened in spreadsheet applications that use the OpenDocument Spreadsheet format.