• Welcome to BirdForum, the internet's largest birding community with thousands of members from all over the world. The forums are dedicated to wild birds, birding, binoculars and equipment and all that goes with it.

    Please register for an account to take part in the discussions in the forum, post your pictures in the gallery and more.
ZEISS DTI thermal imaging cameras. For more discoveries at night, and during the day.

Vultur messii sp. nov. (2 Viewers)

Fred Ruhe

Well-known member
Netherlands
Federico J. Desgrange, Ricardo A, Bonini, Sergio M. Georgieff & Lucia M, Ibanez, 2023

A new fossil condor (Aves, Cathartiformes) from the Early Pliocene of Catamarca province, Argentina

Historical Biology: An International Journal of Paleobiology
doi:10.1080/08912963.2023.2288612

Abstract: https://www.tandfonline.com/doi/abs/10.1080/08912963.2023.2288612

Condors are New World vultures (Cathartiformes, Cathartidae) with broad wings and short tails. The fossil record of condors (Aves, Cathartiformes) in South America is scarce, and particularly in Argentina most of the remains assigned to condors have been debated. Here, we present a new fossil species of Cathartidae found in the Early Pliocene of Catamarca province, Argentina, that belongs to the extant genus Vultur. The new species, Vultur messii sp. nov. is considered to be the only valid fossil species of this iconic genus of birds. The presence of a fossil Vultur species, recovered from deposits older than 4.8 Ma, coincides with the rise of the pampean hills and the Andes, and the beginning of the regional aridification. The existence of incipient mountain chains may also indicate that the centre of origin of this genus is linked to the Andes mountain, which in turn indicates an earlier arrival and diversification of the condors in South America.

Enjoy,

Fred
 
Systematic palaeontology

Class Aves Linnaeus, 1758
Subclass Neognathae Pycraft, 1900
Order Cathartiformes Coues, 1884
Family Cathartidae Lafresnaye, 1839
Genus Vultur Linnaeus, 1758

Type species
Vultur gryphus
Linnaeus, 1758

Included species
Type species and V. messii sp. nov.

Vultur messii sp. nov.

Diagnosis

MCH 363 is assigned to genus Vultur (a genus that until the discovery of the new material was monotypic) based on the presence of a single foramen and a marked protuberance located medially to the crista trochanteris, an impressio lig. cruciati cranialis widely extended and a condylus lateralis that gradually transitions towards the diaphysis. It differs from Vultur gryphus in the following features: the presence of a much larger unique foramen, a caudal deep pit bounded cranially by the narrower facies articularis antitrochanterica, a markedly medially deflected crista trochanteris, a rounded and markedly large scar of origin of the m. gastrocnemius pars intermedia, an impressio ansae m. iliofibularis facing caudally, and a wide and shallow sulcus patellaris.

Holotype
MCH 363, right femur lacking part of the diaphysis.

Etymology
Honouring the Argentinean football player Lionel Andrés Messi, one of the best of our times, who, being captain and best player, together with an outstanding team won the FIFA World Cup in Qatar 2022.

Procedence
Andalhuala Formation (Late Miocene-Early Pliocene). S27°17’34.2’ W66°54’40.4’, San Fernando Norte, Belén Department, Catamarca province. The fossil comes from older deposits than 4.8 Ma, corresponding to the Early Pliocene.

Description
The caput femoris is stout, slightly constricted (not constricted in Vultur and Cathartes) with a marked and deep fovea lig. capitis. As in Vultur, the facies articularis acetabularis is poorly extended distally (not extended in Cathartes and Coragyps). The facies articularis antitrochanterica is narrow, bounding caudally a deep pit, absent in other cathartics (in Gymnogyps there is a long furrow, endowed with pneumatic foramina, laterally bounded by a marked, caudally directed tubercle absent in Vultur). Medial to the stout crista trochanteris (stouter in Gymnogyps), a large pneumatic foramen is placed (as is typical of Cathartidae). Having a unique foramen is also observed in Vultur gryphus, Breagyps clarki and Gymnogyps californianus, however this opening is much larger in the fossil species, and similar to Geronogyps and Breagyps. However, in Breagyps, the foramen is more proximally located, while in Geronogyps is more distally located, and in Gymnogyps, there is a deep furrow proximal to the foramen. Medially to this foramen, there is a marked curved ridge that bounds the foramen. This ridge is straighter in Vultur, Coragyps, and Cathartes. When viewed proximally, medially to the crista trochanteris, a marked protuberance is located, a feature observed only in Vultur among cathartids (this protuberance, although present is much less developed and barely noticeable in Gymnogyps). The crista trochanteris is markedly bended medially, similar to Breagyps and Geronogyps. The caudal angle between the lateral margin of the crista trochanteris and the caudal aspect of the facies articularis antitrochanterica is obtuse, and larger than that of Vultur (much smaller, and acute in Cathartes). The scar for the insertion of the m. iliotrochanteris caudalis is narrow and poorly marked (contrary to Vultur). The impressio obturatoriae has a marked oval shape. The scar of the insertion of the m. iliofemoralis internus has an oval shape, very similar to that of Vultur. The linea intermuscularis cranialis is poorly marked.
The distal area of the femur is more badly preserved, heavily crushed and lacking a portion of the condylus medialis. The fossa poplitea is deep and wide (shallow in Coragyps and Gymnogyps), with at least two noticeable large pneumatic foramina. This fossa is bounded laterally by the condylus lateralis, which when viewed laterally has a gradual transition towards the diaphysis as in Vultur (abrupt transition in Coragyps and Cathartes). The scar of origin of the m. gastrocnemius pars intermedia is rounded and large (smaller and oval in Vultur). The impression lig. cruciati cranialis is very wide and extended, as in Vultur (shallow and narrow in the smaller Cathartes and Coragyps). The tuberculum m. gastrocnemialis lateralis is low, large, with a heartshaped scar (oval in Vultur, rounded in Coragyps and Cathartes). The impressio ansae m. iliofibularis is small and oval, distally located in the aforementioned tuberculum, and faces caudally (caudolaterally in V. gryphus, laterally in Geronogyps and Breagyps). As in Vultur, the linea intermuscularis caudalis extends distally laterally on the shaft, bounding a scar located right proximally over the crista lateralis sulci patellaris (laterally located in Cathartes and Coragyps). This crista is stout and wide, bounding laterally a wide but shallow sulcus patellaris (narrow in Geronogyps and deeper in Vultur gryphus, in Gymnogyps it is wide and deep, and present a quadrangular contour when viewed distally). The impressio lig. collateralis lateralis is shallow. The fovea tendinis m. tibialis cranialis is shallow as in Cathartes (deep in Vultur). The sulcus intercondylaris is shallow (deep in Gymnogyps).

Fred


Figure 1. Holotype of Vultur messii sp. nov., MCH 363, right femur (A), compared with that of Vultur gryphus CIT-O 263 (B) in cranial, caudal, lateral, medial, proximal and distal views. Abbreviations: cl, condylus lateralis; ct, condylus medialis; faa, facies articularis antitrochanterica; flc, fovea lig. capitis; fp, fossa poplitea; ftc, fovea
tendinis m. tibialis cranialis; gi, scar of m. gastrocnemius pars intermedia; ial, impressio ansae m. iliofibularis; icl, impressio lig. collateralis lateralis; ifi, scar of m. iliofemoralis internus; ilcc, impressio lig. cruciatum cranialis; io, impressio obturatoriae; itc, scar of m. iliotrochanteris caudalis; p, caudal pit; pf, pneumatic foramen; sf, sulcus fibularis; si, sulcus intercondylaris; sp, sulcus patellaris; tf, trochanter femoris; tgl, tuberculum m. gastrocnemius lateralis. The black arrow points at the characteristic medial protuberance of Vultur.
Scale = 1 cm.`.
1701939327657.png
 

Users who are viewing this thread

Back
Top