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New Fossil Remains of Giraffids from the Lower Siwaliks of Punjab, Pakistan: Evolution, Systematics and Biogeography

Taxonomic study from a late Miocene Fossil locality Dhok Bun Ameer Khatoon, Lower Siwalik Hills of Pakistan has been conducted. New fossil remains belong to family Giraffidae which include right and left maxilla, isolated upper premolars and molars. After morphological and comparative analysis, the collection is attributed to Giraffokeryx punjabiensis and Giraffa priscilla. Size variation in dentition is taxonomically important for vertebrate evolutionary point of view and this is the main reason to conduct this study at this specific site

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The five digits of the giraffe metatarsal

Evolution has shaped the limbs of hoofed animals in specific ways. In artiodactyls, it is the common assumption that the metatarsal is composed of the fusion of digits III and IV, whereas the other three digits have been lost or are highly reduced. However, evidence from the fossil record and internal morphology of the metatarsal challenges these assumptions. Furthermore, only a few taxonomic groups have been analysed. In giraffes, we discovered that all five digits are present in the adult

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Siwalik Giraffidae (Mammalia, Artiodactyla): A review

The article is based on the published literature regarding the family Giraffidae, particularly about the extinct Siwalik species. The provided information is collected from the previous published articles, aiming to produce the basic information of the Siwalik giraffids. The distribution of the Siwalik giraffid species is also briefly discussed.

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Comparisons of Schansitherium tafeli with Samotherium boissieri (Giraffidae, Mammalia) from the Late Miocene of Gansu Province, China

We are describing and figuring for the first time skulls of Schansitherium tafeli, which are abundant in the Gansu area of China from the Late Miocene. They were animals about the size of Samotherium with shorter necks that had two pairs of ossicones that merge at the base, which is unlike Samotherium. The anterior ossicones consist of anterior lineations, which may represent growth lines. They were likely mixed feeders similar to Samotherium. Schansitherium is tentatively placed in a very close

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Key innovations in ruminant evolution: A paleontological perspective

Key innovations are newly acquired structures that permit the performance of a new function and open new adaptive zones, and are, therefore, of paramount significance for understanding the history of the Ruminantia, particularly its diversification through the Miocene. Here we review and discuss what is known about these evolutionary novelties, with special emphasis on the appearance and evolution of cranial appendages and highcrowned (or hypsodont) teeth. Cranial appendages probably favored the diversification of pecorans by being structures strongly related to

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The systematic position of Hoplitomerycidae (Ruminantia) revisited

Hoplitomeryx Leinders was originally described only on cranial characters. The type specimens were found during the 1970’s in karstic fissure fillings, most likely of Messinian age, in Gargano (Apulia, southeastern Italy), between Poggio Imperiale (418490300 N, 158210580 E) and Apricena (418470060 N, 158260410 E). During the 1990’s, Hoplitomeryx remains were also discovered in the lower Tortonian layered calcarenites near Scontrone (Abruzzo, central Italy; 41845015.550 N, 14802013.230 E). The skull fragments, teeth, and jawbones from both localities have been examined. The

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First comprehensive morphological analysis on the metapodials of Giraffidae

Giraffids are a group of relict pecoran ruminants with only two living taxa. During the Miocene, however, this group was much more diverse, with more than 20 different species showing a wide range of variability. In addition to many other parts of the skeleton this variability is also represented in their metapodials. We find inter-specific anatomical differences in the giraffid metapodials; each taxon evaluated possesses a unique combination of limb morphologies. The proximo-palmar/plantar metapodial surface provides useful characteristics and allows

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