Abstract
Titanosauria is a clade of sauropod dinosaurs that includes species ranging from the largest known terrest-rial vertebrates to insular dwarfs no bigger than elephants. Although most sauropod dinosaurs exhibit highly vascularized fibrolamellar bone signaling rapid growth rates comparable to those of extant mammals, diminutive titanosaurs apparently exhibit histological traits consistent with reduced primary growth rates and/or truncated active growth to reach small adult body sizes. A better understanding of the evolution of titanosaur body size requires additional sampling of the 40+ known titanosaur species. The best-preserved and most complete titanosaur yet discovered is Rapetosaurus krausei from the Maastrichtian Maevarano Formation in Madagascar. Skeletal material from many individuals spanning a wide range of ontogeny, from neonates to very large body sizes, makes Rapetosaurus an ideal candidate for an analysis of growth. We analyzed Rapetosaurus histology using a growth series of 25 forelimb, hind limb, and girdle elements representing different ontogenetic stages, including samples from the largest Rapetosaurus known (femur length = 143 cm). Primary bone histology in Rapetosaurus is highly vascularized fibrolamellar tissue, such as is found in other sauropods and most sampled titanosaurs. Secondary remodeling begins early, as noted in other titanosaur taxa, and by mid-ontogeny is pervasive in most sampled elements. The largest known Rapetosaurus was still growing, whereas some small juveniles exhibit an unusual pattern of bone erosion and replacement in the context of peripheral lines of arrested growth that signal a temporary pause in bone apposition. We hypothesize that these signals may relate to the drought-stressed ecosystem inhabited by Rapetosaurus.
Citation for this article: Curry Rogers, K., and Z. Kulik. 2018. Osteohistology of Rapetosaurus krausei (Sauropoda: Titanosauria) from the Upper Cretaceous of Madagascar. Journal of Vertebrate Paleontology. DOI: 10.1080/02724634.2018.1493689.
ACKNOWLEDGMENTS
Members of the Mahajanga Basin Project collected the specimens described in this report between 1993 and 2010. L. Ballewske, D. Sorenson, and M. Whitney, all Macalester College alumni, contributed to preliminary data collection. J. Thole and K. Moffat provided microscopy and photography assistance. W. Simpson provided ready access to materials held in the Field Museum of Natural History collections. R. Rogers and M. D’Emic provided comments on earlier drafts of this paper. Thoughtful reviews by I. Cerda and E. Prondvai greatly improved the quality of the manuscript. Grants from the National Science Foundation (EAR-0955716, DEB-0822957, EAR-1664432, EAR-9418816, EAR-9706302, and EAR-0446488) and the National Geographic Society (8597-09) supported this work.