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Garganornis (meaning "Gargano bird") is an extinct genus of enormous flightless from the Late of , . The genus contains one species, G. ballmanni, named by Meijer in 2014. Its is thought to have been an adaptation to living in exposed, open areas with no terrestrial predators, and as a deterrent to the indigenous aerial predators like the and the giant .


Description
The of Garganornis is approximately 30% larger than that of the living in . Based on comparisons with the latter, it has been estimated that Garganornis had a weight in the range of , larger than any living . This suggests that it was likely flightless.

The preserved from the wings had quite a short and robust shaft, much shorter than any of the living large-bodied that are capable of flight. The carpometacarpus was also peculiarly flattened on its top end; and the trochlea carpalis (a bony articular process that drives wing extension and flexion) is reduced and weak in shape, limiting wrist movement—both likely adaptations to a flightless life.

In some specimens of Garganornis, there is a small bony knob on the top of the carpometacarpus that is similar to that of , , ducks, and other anseriforms; this was likely used for fighting, as in other members of the group.

Likewise short and robust was the of the foot. The processes known as the trochlea metatarsi II and IV, on the bottom portion of the tarsometatarsus, are more equal in length than most other anseriforms, with the exception of the Cape Barren goose, , and the giant, extinct . The of the toes are also relatively robust, and similar to other giant anseriforms; however, the impressions of ligaments on the bones are weaker and less defined.


Discovery and naming
The first remains of Garganornis were discovered from the Posticchia 5 fissure filling near the town of in , . These deposits are part of the faunal assemblage (named after an abundant rodent), which has been dated to 6–5.5 Ma in age. The holotype consists of a single partial left , catalogued as RGM 443307, which was described by Meijer in 2014.

Additional material was later described from Gargano by Pavia et al. in 2016, consisting of partial (DSTF-GA 49, NMA 504/1801), a single damaged tibiotarsus (DSTF-GA 77), partial (RGM 425554, RGM 425943), and various from the foot (MGPT-PU 135356, RGM 261535, RGM 261945). Additionally, some geologically earlier but morphologically comparable material was described from the Scontrone locality, which is close to the town of and has been dated to 9 Ma in age. This material consists of an almost complete tarsometatarsus, SCT 23; although it is temporally separated from the other material, the morphology and unusually large size of the bone suggests that it pertains to Garganornis.

The genus name Garganornis is derived from the general area of Gargano, in which the holotype fossils were discovered; the Greek suffix ornis means "bird". The species name honors Peter Ballmann, who first described the birds of the Gargano region.


Classification
Several characteristics of the allow Garganornis to be placed definitely in the order : the medial condyle is angled medially and bears a projection at its front end; and the canal of the extensor tendon is placed centrally over the intercondylar fossa. Features of the allow for a more specific assignment to the family : the extensor process is parallel to the trochlea carpalis and is not tilted towards the bottom; the is wide and unpointed; and a small knob is present above the caudal carpal .

Garganornis peculiarly shares a number of characteristics in the tibiotarsus with another group of large anseriforms, the . In particular, the intercondylar fossa is wide, the bottom opening of the extensor canal is circular (although it is placed more centrally relative to the condyles than in gastornithids), the extensor sulcus is relatively deep, and the pons supratendineus (a projection above the opening of the extensor canal) has a depression on its side. However, given that gastornithids and other fauna do not appear to have survived in—or even reached—this region, it is more likely that these shared traits are convergent adaptations to gigantic body sizes.


Paleoecology
Surveys conducted by P. Ballmann in the 1970s revealed a diverse bird fauna in the Gargano locality, consisting of 16 different taxa; later work established the presence of 10 additional distinct taxa (not including Garganornis), bringing the total to 26. These include the and an additional unnamed anatid; the giant and G.  murivorus, as well as an unnamed smaller ; the ; the , , "Strix" perpasta, another species referred to Strix, an additional species referred to Athene, and an unnamed taxon formerly referred to T.  sanctialbani; the Columba omnisanctorum; the swift Apus wetmorei; the and an unnamed taxon; a threskiornithid; a ; a ; two ; two ; a ; a ; and a . To date, Garganornis is the only bird that is found in both the Gargano and Scontrone localities; the lack of other Gargano birds in Scontrone is probably a result of .

Asides from birds, various mammals and reptiles are known from the Gargano and Scontrone localities. Most notably, the (including M.  magna, M.  parva, and M.  maiuscula) is very abundant; the genus lends its name to the entire local ecosystem, which has become known as the Mikrotia fauna. A second murid, sp., is also present. Other rodents include the giant , S.  daunius, and S.  lyrifer, along with the smaller species S.  deguili, S.  simplex, and S.  daamsi; and the , H.  nazarii, sp., and sp. The (hairy hedgehogs) , D.  minor, D.  intermedius, D.  brevirostris, D.  koenigswaldi, and D.  masinii were also giant, while their smaller relative is also present. Other mammals include the ; the and P.  imperialis; the deer-like ; and the otter . There is one reptile genus: a crocodile referred to .

Garganornis and the rest of the Mikrotia fauna has been dated to the stage of the Late . During the Miocene, the Gargano and Scontrone areas were part of an isolated archipelago that has been referred to as the Apulia-Abruzzi Palaeobioprovince. Small mammals, including the gymnure ancestors of Deinogalerix, probably reached these islands via rafting.

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