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all geography including DSDP/ODP Sites and Legs
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soils (1)
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Dasypodidae
Evidence for advanced carnivory in fossil armadillos (Mammalia: Xenarthra: Dasypodidae)
NEOICHNOLOGY OF ARMADILLOS: KEYS FOR THE PALEOECOLOGICAL AND BEHAVIORAL INTERPRETATION OF FOSSIL TETRAPOD BURROWS
ARMADILLO OSTEODERMS ALTERED BY DIGESTION AND HOW TAPHONOMY CAN HELP TAXONOMY
New records of Neogene Xenarthra (Mammalia) from eastern Puna (Argentina): diversity and biochronology
The teeth of the “toothless”: novelties and key innovations in the evolution of xenarthrans (Mammalia, Xenarthra)
Diet and habitat definitions for Mexican glyptodonts from Cedral (San Luis Potosí, México) based on stable isotope analysis
Function in the stunted forelimbs of Mononykus olecranus (Theropoda), a dinosaurian anteater
TAPHONOMIC ANALYSIS OF AN ASSEMBLAGE OF LAMA GUANICOE (ARTIODACTYLA, CAMELIDAE) FROM THE LATE HOLOCENE (PAMPEAN REGION, ARGENTINA)
Vertebral morphometrics in Varanus
Pleistocene mammals from Extinction Cave, Belize
Strangers in a strange land: Ecological dissimilarity to metatherian carnivores may partly explain early colonization of South America by Cyonasua- group procyonids
To replace or not to replace: the significance of reduced functional tooth replacement in marsupial and placental mammals
Ontogenetic mechanisms of size change: implications for the Lilliput effect and beyond
ENVIRONMENTAL INFLUENCE ON BURROW SYSTEM FEATURES OF A COLONIAL AND FOSSORIAL RODENT: IMPLICATIONS FOR INTERPRETING FOSSIL TETRAPOD BURROWS
Cranial anatomy of Microsyops annectens (Microsyopidae, Euarchonta, Mammalia) from the middle Eocene of Northwestern Wyoming
Aetosauria: a clade of armoured pseudosuchians from the Upper Triassic continental beds
Abstract Aetosauria is a clade of obligately quadrupedal, heavily armoured pseudosuchians known from Upper Triassic (late Carnian–Rhaetian) strata on every modern continent except Australia and Antarctica. As many as 22 genera and 26 species ranging from 1 to 6 m in length, and with a body mass ranging from less than 10 to more than 500 kg, are known. Aetosauroides scagliai was recently recovered as the most basal aetosaur, placed outside of Stagonolepididae (the last common ancestor of Desmatosuchus and Aetosaurus ). Interrelationships among the basal aetosaurs are not well understood but two clades with relatively apomorphic armour – the spinose Desmatosuchinae and the generally wide-bodied Typothoracisinae – are consistently recognized. Paramedian and lateral osteoderms are often distinctive at the generic level but variation within the carapace is not well understood in many taxa, warranting caution in assigning isolated osteoderms to specific taxa. The aetosaur skull and dentition varies across taxa, and there is increasing evidence that at least some aetosaurs relied on invertebrates and/or small vertebrates as a food source. Histological evidence indicates that, after an initial period of rapid growth, lines of arrested growth (LAGs) are common and later growth was relatively slow. The common and widespread Late Triassic ichnogenus Brachychirotherium probably represents the track of an aetosaur.