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Naranbulagornis khun gen. et sp. nov. (1 Viewer)

Fred Ruhe

Well-known member
Netherlands
Nikita V. Zelenkov, 2019

A swan-sized anseriform bird from the late Paleocene of Mongolia

Journal of Vertebrate Paleontology. Online edition: e1531879

Abstract: https://www.tandfonline.com/doi/abs/10.1080/02724634.2018.1531879?journalCode=ujvp20

The early evolutionary history of waterfowl (Anseriformes) is poorly understood. Aside from the morphologically aberrant Presbyornithidae, the only other known early Paleogene anseriform taxon is Anatalavis oxfordi from the early Eocene of England. Here, I describe two bones from the late Paleocene of southern Mongolia (localities Naran-Bulag and Tsagaan-Khushuu), which belong to a very large swan-sized swimming waterfowl (Anseriformes) and are described as Naranbulagornis khun, gen. et sp. nov. This is the first non-presbyornithid anseriform bird found in the early Paleogene (Paleocene through early Eocene) of Asia and one of the few currently known Paleocene birds from Central Asia. It is also the largest volant bird from the Paleogene of Asia. Naranbulagornis khun documents a mosaic of autapomorphic and plesiomorphic features that are otherwise present in modern Anhimidae, Anseranatidae, and Anatidae, indicating a greater morphological diversity of early Cenozoic anseriforms than previously thought. The new taxon is morphologically closer to Anatoidea than to Presbyornithidae and represents the earliest global evidence of a spatial coexistence between presbyornithids and other basal waterfowl during the early Paleogene.

Enjoy,

Fred
 
SYSTEMATIC PALEONTOLOGY

Order ANSERIFORMES Wagler, 1831
Family INCERTAE SEDIS
NARANBULAGORNIS KHUN, gen. et sp. nov.

Etymology—The genus name (masculine gender) refers to the locality, meaning ‘bird from sunshine spring,’ and the specific epithet means ‘swan’ in Mongolian.

Holotype—PIN 3102/74, proximal right carpometacarpus.

Type Locality and Horizon—Naran-Bulag, southern Mongolia; fluvial phase of the Naran Member, whitish layers of the second phase of the channel (see Badamgarav and Reshetov, 1985); latest Paleocene (Gashatan ALMA).

Referred Material—PIN 3104/1089, distal fragment of the left femur; locality Tsagaan-Khushuu, Mongolia; Naran Member; latest Paleocene (Gashatan ALMA).

Fred
 

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