Glyptodontidae indet., 1839
publication ID |
https://dx.doi.org/10.3897/fr.27.e119967 |
publication LSID |
lsid:zoobank.org:pub:739CC1FF-7E28-4678-AD10-09E6412EB960 |
persistent identifier |
https://treatment.plazi.org/id/D9492CBB-DFCB-5DA2-A461-167100019493 |
treatment provided by |
by Pensoft |
scientific name |
Glyptodontidae indet. |
status |
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Fig. 6 View Figure 6
Referred material.
Two isolated osteoderms (AMU-CURS-1047 and -1360) were collected on the surface at the Cauca site (Fig. 1B View Figure 1 ).
Descriptions.
Both isolated osteoderms are from the shell. AMU-CURS-1047 has a Tl of 47 mm and is eroded on both the internal and external faces, which does not allow the identification of the ornamentation pattern (Fig. 6A1, A2 View Figure 6 ). AMU-CURS-1360 possibly corresponds to an osteoderm from the anterior lateral region of the shell and this has a Tl of 31 mm; it is also eroded on the inner face, and partially preserving the ornamentation of the outer face with a central figure of irregular polygonal shape, preserving some foramina that could belong to hair follicles and surrounded by a groove (Fig. 6B1, B2 View Figure 6 ).
Remarks.
The state of preservation of these two osteoderms does not allow a more precise taxonomic determination than Glyptodontidae , Glyptodontinae . However, these osteoderms could belong to the genus Glyptotherium , widely known in the Late Pleistocene of the Falcón State, especially at the sites of Muaco and Taima-Taima ( Carlini et al. 2008, 2022). A recent report suggests that these Glyptotherium -related armadillos had a broader distribution in what is now Venezuela during the Late Pleistocene, with reports including mountain areas above 1200 m altitude (see Jaimes et al. (2024b)).
Proboscidea Illiger, 1811
† Gomphotheriidae Hay, 1922
† Notiomastodon Cabrera, 1929
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