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The oldest known record of a ground sloth (Mammalia, Xenarthra, Folivora) from Hispaniola: evolutionary and paleobiogeographical implications
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Show full item recordAbstract: | [English] Sloths were among the most diverse groups of land vertebrates that inhabited the Greater Antilles until their extinction in the middle-late Holocene following the arrival of humans to the islands. Although the fossil record of the group is well known from Quaternary deposits in Cuba, Hispaniola, and Puerto Rico, remains from older units are scarce, limiting our understanding of their evolution and biogeographic history. Here we report the oldest known fossil ground sloth from Hispaniola, represented by an unassociated partial tibia and scapula that are recognized as a single taxon from the late Miocene-early Pliocene of the Dominican Republic. The combination of characters observed on the tibia suggests a close relationship with Megalocnus, otherwise only known from the Pleistocene–Holocene of Cuba. These fossils fill a temporal gap between those previously known from the early Miocene of Cuba and those from Pleistocene–Holocene deposits in the region and provide additional support for a continuous presence of the group in the Greater Antilles since the Oligocene. |
Author(s): | Viñola-López, Lázaro W.
Core Suárez, Elson E. Vélez-Juarbe, Jorge Almonte Milán, Juan N. Bloch, Jonathan I. |
Date: | 2021 |
Published: | Journal of Paleontology [ISSN: 1937-2337], 1-8. |
Citation: | Viñola-López, L. W., Core Suárez, E. E., Vélez-Juarbe, J., Almonte Milán, J. N. y Bloch, J. I. (2021). The oldest known record of a ground sloth (Mammalia, Xenarthra, Folivora) from Hispaniola: evolutionary and paleobiogeographical implications. Journal of Paleontology, 1-8. Recuperado de: |
URI: | https://bvearmb.do/handle/123456789/443
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Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of The Paleontological Society.
Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of The Paleontological Society.