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dc.contributor.author | Cartelle C. | |
dc.contributor.author | De Iuliis G. | |
dc.date.accessioned | 2025-02-01T02:53:24Z | |
dc.date.available | 2025-02-01T02:53:24Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=9327101 | |
dc.identifier.citation | Journal of Systematic Palaeontology, 2006, 4, 2, 199-209 | |
dc.identifier.issn | 1477-2019 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/47581 | |
dc.description.abstract | For most of the past 150 years the presence of only giant megatheriine ground sloths in the Pleistocene of Brazil has been recognised. However, it has recently been claimed that a dwarf Eremotherium species was present sympatrically with the large-sized giant ground sloth in northeastern and southeastern Brazil during the late Pleistocene and that the concept of a single Panamerican species was improbable. Based on analysis of the ontological sequence of skull suture closure and dental development of remains from a single locality, we demonstrate that the 'dwarf' species is based on the remains of immature individuals, at very early ontogenetic stages, of the large-sized species. Further, we reaffirm that the most parsimonious hypothesis is to consider all large-sized Eremotherium remains as belonging to a single species of Panamerican distribution. | |
dc.subject | MEGATHERIINAE | |
dc.subject | DWARF MEGATHERE | |
dc.subject | SYSTEMATICS | |
dc.subject | TAXONOMY | |
dc.subject | PALAEOBIOGEOGRAPHY | |
dc.subject | Pleistocene | |
dc.title | E | |
dc.type | Статья | |
dc.identifier.doi | 10.1017/S1477201905001781 | |
dc.subject.age | Cenozoic::Quaternary::Pleistocene | |
dc.subject.age | Кайнозой::Четвертичная::Плейстоцен |
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