Aquila sp.
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publication ID |
https://doi.org/10.11646/zootaxa.5627.2.5 |
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publication LSID |
lsid:zoobank.org:pub:9FE03BE3-E444-43AF-B003-C340D14B7A71 |
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DOI |
https://doi.org/10.5281/zenodo.15345283 |
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persistent identifier |
https://treatment.plazi.org/id/D36487CD-FFF3-FFC1-6493-D5FB11A1F898 |
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treatment provided by |
Plazi |
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scientific name |
Aquila sp. |
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Aquila sp. indet.
Location and age: Beremend 38; Lower Pliocene (MN16).
Material: 1 distal left tarsometatarsus fragment ( Figure 2 View FIGURE 2 /1) and a drawing of it ( Figure 2 View FIGURE 2 /2).
Dimensions (mm): E—7.7, F—19.2, G—10.7.
Description: Typical eagle tarsometatarsus distal epiphysis. The size range of the fossil is between that of Aquila heliaca and Haliaeetus albicilla . The only aquiline known to have lived in the Carpathian Basin during the Neogene is Aquila chrysaetos , which is known from Villány ( MN 16) ( Jánossy 1977, 1979a).
Comparative material: Aquila heliaca (68.4.1); Hieraaetus fasciatus (2010.295.1); Hieraaetus pennatus (2010.296.1).
This material is not catalogued, it belongs to the Chapel of Reconciliation in Beremend and will be catalogued in the collection there.
| MN |
Museu Nacional, Universidade Federal do Rio de Janeiro |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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