On Megatherium gallardoi Ameghino & Kraglievich (Xenarthra, Megatheriidae) and other megatheriines from the Ensenadan (Lower to Middle Pleistocene) of the Pampean region, Argentina

BRANDONI, D.; SOIBELZON E.; SCARANO A.

Geodiversitas

Año: 2008 vol. 30 p. 793 - 804

The Megatheriinae (Mammalia, Xenarthra, Megatheriidae) are recorded in Argentina from the middle Miocene to the early Holocene. Only the genus Megatherium Cuvier, comprising several species of controversial validity, is recognized for the Pleistocene of the Pampean region. Megatherium americanum Cuvier is the best studied species and occurs frequently in sediments assigned to the Lujanian Stage (Equus (Amerhippus) neogeus Biozone, ca. 0.13-0.08 My). On the other hand, Megatherium gallardoi C. Ameghino and Kraglievich and Megatherium silenum (Ameghino), both from Ensenadan sediments (Mesotherium cristatum Biozone) of Buenos Aires Province, have been considered by some authors as synonyms of Megatherium americanum. The main goal of this contribution is to complete the description of Megatherium gallardoi, clarify its taxonomic status, and establish its relationships with other megatheriines. The most remarkable features of Megatherium gallardoi are: premaxillae not fused to each other or to the maxillae; mandibular ramus relatively low; femur with lateral and medial diaphyseal margins markedly concave, diaphysis expanded transversely proximally and distally; medial reduction of the patellar trochlea; humerus and femur robust. Based on the anatomical and comparative analysis, we propose that 1) Megatherium gallardoi is a valid species; 2) specimen MACN Pv 5002 (type of Megatherium gallardoi) is an adult individual; 3) M. gallardoi is related to the clade formed by Megatherium americanum and Megatherium altiplanicum Saint-André and De Iuliis; 4) Megatherium silenum (the other Megatheriinae known for the Ensenadan Stage of Argentina) should be considered nomen vanum because it lacks diagnostic features and corresponds undoubtedly to a juvenile individual.