Mammalian bone palaeohistology: a survey and new data with emphasis on island forms

KOLB, CH. ; SCHEYER. T.M.; VEITSCHEGGER, K. ; FORASIEPI, A.M.; AMSON, E.; VAN DER GEER, A.; VAN DEN HOEK OSTENDE, L.W.; HAYASHI, S.; SANCHEZ-VILLAGRA M.

PeerJ

PeerJ, Inc.

Lugar: San Francisco; Año: 2015 vol. 3 p. 1 - 44

The interest in mammalian palaeohistology has increased dramatically in the last two decades. Starting in 1849 via descriptive approaches, it has been demonstrated that bone tissue and vascularisation types correlate with several biological variables such as ontogenetic stage, growth rate, and ecology. Mammalian bone displays a large variety of bone tissues and vascularisation patterns reaching from lamellar or parallel-fibred to fibrolamellar or woven-fibred bone, depending on taxon and individual age. Here we systematically review the knowledge and methods on cynodont and mammalian bone microstructure as well as palaeohistology and discuss potential future research fields and techniques. We present new data on the bone microstructure of two extant marsupial species and of several extinct continental and island placental mammals. Extant marsupials display mainly parallel-fibred primary bone with radial and oblique but mainly longitudinal vascular canals. Three juvenile specimens of the dwarf island hippopotamid Hippopotamus minor from the Late Pleistocene of Cyprus show reticular to plexiform fibrolamellar bone. The island murid Mikrotia magna from the Late Miocene of Gargano, Italy displays parallelfibred primary bone with reticular vascularisation and strong remodelling in themiddle part of the cortex. Leithia sp., the dormouse from the Pleistocene of Sicily,is characterised by a primary bone cortex consisting of lamellar bone and a highamount of compact coarse cancellous bone. The bone cortex of the fossil continentallagomorph Prolagus oeningensis and three fossil species of insular Prolagus displaysmainly parallel-fibred primary bone and reticular, radial as well as longitudinal vascularisation. Typical for large mammals, secondary bone in the giant rhinocerotoid Paraceratherium sp. from the Late Oligocene of Turkey is represented by dense Haversianbone. The skeletochronological features of Sinomegaceros yabei, a large-sized deer from the Pleistocene of Japan closely related to Megaloceros, indicate a high growth rate. These examples and the synthesis of existing data show the potential of bone microstructure to reveal essential information on life history evolution. The bone tissue and the skeletochronological data of the sampled island species suggest the presence of various modes of bone histological modification and mammalian life history evolution on islands to depend on factors of island evolution such as island size, distance from mainland, climate, phylogeny, and time of evolution.