The last horned armadillos: phylogeny and decline of Peltephilidae (Xenarthra, Cingulata)

Author:

Barasoain Daniel1ORCID,Croft Darin A.2ORCID,Zurita Alfredo E.1,Contreras Victor H.3,Tomassini Rodrigo L.4

Affiliation:

1. Laboratorio de Evolución de Vertebrados y Ambientes Cenozoicos, Centro de Ecología Aplicada del Litoral (UNNE‐CONICET) y Cátedra de Paleontología de Vertebrados, Facultad de Ciencias Exactas, Naturales y Agrimensura Universidad Nacional del Nordeste Corrientes RP5 3400 Argentina

2. Department of Anatomy Case Western Reserve University School of Medicine 10900 Euclid Ave Cleveland 44106‐4930 OH USA

3. Facultad de Ciencias Exactas, Físicas y Naturales, Instituto de Geología Dr Emiliano P. Aparicio, Departamentos Geología y Biología Universidad Nacional de San Juan Avenida Ignacio de La Rosa y Calle Meglioli, Rivadavia San Juan 5400 Argentina

4. INGEOSUR, Departamento de Geología Universidad Nacional del Sur (UNS‐CONICET) Avenida Alem 1253 Bahía Blanca 8000 Argentina

Abstract

AbstractPeltephilidae (Xenarthra, Cingulata) is an ancient lineage of medium–large‐sized ‘armadillos’ from South America, characterized by chisel‐shaped molariforms, a U‐shaped dental arcade, and cephalic osteoderms modified into hornlike structures. Although the biochron of the group extends from the early Eocene to the Late Miocene, the most abundant and complete records come from the Early Miocene of Patagonia. Remains from the Late Miocene are very scarce, and the last records of the group are from the Chasicoan Stage (Tortonian). The only taxon known from this interval is Epipeltephilus kanti from the Arroyo Chasicó Formation (9.23 ± 0.09 Ma; Buenos Aires Province, Argentina), a species previously represented only by a few isolated osteoderms. Here we report new remains assigned to E. kanti from the Late Miocene of Loma de Las Tapias Formation (c. 9.0–7.8 Ma; San Juan Province, Argentina), including a hemimandible and several fixed and mobile osteoderms. These new specimens constitute the youngest record of Peltephilidae. The inclusion of E. kanti within Epipeltephilus and the monophyly of the genera Peltephilus and Epipeltephilus are corroborated for the first time through a cladistic analysis. The decline and eventual disappearance of this ‘armadillo’ group in the Late Miocene is chronologically coincident with the replacement of subtropical/tropical environments by more open and arid ones and with the proliferation of other large armadillos such as Vetelia, Macrochorobates, and Macroeuphractus.

Publisher

Wiley

Subject

Paleontology

Reference121 articles.

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