Biology:Alcione elainus

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Short description: Genus of pterosaur from the Late Cretaceous

Alcione elainus
Temporal range: Upper Maastrichtian
A. elainus FSAC-OB 2 holotype partial skeleton and FSAC-OB 217 metacarpal IV compressed.png
A, humerus of holotype; B, radius and ulna of holotype; C, sternum of holotype; D, referred metacarpal IV; E, metacarpal IV and scapulocoracoid of holotype; F, femur of holotype.
Scientific classification edit
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Order: Pterosauria
Suborder: Pterodactyloidea
Clade: Aponyctosauria
Genus: Alcione
Longrich et al., 2018
Species:
A. elainus
Binomial name
Alcione elainus
Longrich et al., 2018

Alcione is a genus of pterosaur from the Ouled Abdoun Basin of Morocco, dating back to the Maastrichtian stage of the Late Cretaceous period. Only one species, A. elainus, is known. This pterosaur lived in a marine environment alongside several other pterosaurs, including Simurghia and Barbaridactylus.

Discovery and naming

Locality and stratigraphy of the discovery site

All known specimens of Alcione were uncovered in a 3-year dig that unearthed about 200 pterosaur specimens. The type specimen, FSAC-OB 2, consists of a partial skeleton that preserves various elements, including the femur, humerus, scapulocoracoid, and sternum. Referred specimens include FSAC-OB 217, which consists of metacarpal IV, FSAC-OB 156, a mandible, and the more complete FSAC-OB 4. This specimen consists of the humerus, radius, ulna, a partial metacarpal IV, phalanx IV-1, scapulocoracoids, and synsacra.[1]

Alcione is named after Alcyone, who was transformed into a seabird, from Greek mythology. The specific name, A. elainus, comes from the Greek elaino, which means "to stray or wander."[1]

Description

Alcione was a small pterosaur, with a wingspan of 1.8–2.4 m (5.9–7.9 ft). Its limb proportions were relatively short compared to related pterosaurs. Its anatomy was relatively typical for the group. Its mandible was narrow and Y-shaped (from a dorsal view), and lacked teeth. Instead, it had sharp edges. The scapulocoracoid was fused in the type specimen, which suggests that it was mature. This bone was boomerang-shaped, a condition seen in many nyctosaurids, and to a lesser degree in pteranodontids.[1]

Classification

Size of Alcione (at top, just left of center) compared to other pterosaurs, birds, and a human

Below is a cladogram showing the results of a phylogenetic analysis first presented by Andres and colleagues in 2014, and updated with additional data by Longrich and colleagues in 2018. They found Alcione within the family Nyctosauridae.[2][1]

Ornithocheiroidea

Azhdarchoidea

Piksi barbarulna

 Pteranodontoidea 

Ornithocheiromorpha

 Pteranodontia 
Pteranodontidae

Pteranodon sternbergi

Pteranodon longiceps

Tethydraco regalis

Nyctosauridae

Alamodactylus byrdi

Volgadraco bogolubovi

Cretornis hlavaci

Alcione elainus

Simurghia robusta

Muzquizopteryx coahuilensis

Barbaridactylus grandis

Nyctosaurus lamegoi

Nyctosaurus nanus

Nyctosaurus gracilis

Mandible

In their phylogenetic analyses, Fernandes et al. (2022) recovered Alcione as the sister taxon to Epapatelo and Simurghia. These taxa, along with the Nyctosauridae, comprise the new clade, Aponyctosauria.[3]

Pteranodontia

Tethydraco

Pteranodon longiceps

Pteranodon sternbergi (Geosternbergia)

Alamodactylus

Volgadraco

Cretornis

Aponyctosauria

Epapatelo

Simurghia

Alcione

Nyctosauridae

Muzquizopteryx

Nyctosaurus lamegoi

Nyctosaurus grandis (Barbaridactylus)

Nyctosaurus nanus

Nyctosaurus gracilis

Paleobiology

Right humerus

The shorter wings of Alcione suggest that it was better adapted for rapid flapping during flight than other nyctosaurids. An alternative explanation is that this adaptation was to aid with underwater movement, as shortened wings are present in modern piscivorous birds.[1]

Paleoecology

Partial right wing

Alcione was discovered in upper Maastrichtian phosphates located in the Ouled Abdoun Basin of Northern Morocco. This geological formation does not belong to a formation. It is divided into couches, with Alcione being discovered in Couche III. This layer dates back to the latest Maastrichtian, about 1 million years before the extinction event at the end of the Cretaceous. Couche III represents the most diverse marine ecosystem known from the time.[1]

A large variety of marine life is known from the region, including sharks and bony fish, in addition to turtles, plesiosaurs, and mosasaurs. A few rare, fragmentary dinosaur fossils are known, including an abelisaur and a sauropod. Other pterosaurs in the formation were originally only represented by the azhdarchid Phosphatodraco mauritanicus. However, in addition to Alcione, more recent studies have revealed at least five more pterosaur species from this location, including Barbaridactylus, Simurghia, and Tethydraco.[1]

References

  1. 1.0 1.1 1.2 1.3 1.4 1.5 1.6 Longrich, Nicholas R.; Martill, David M.; Andres, Brian; Penny, David (2018). "Late Maastrichtian pterosaurs from North Africa and mass extinction of Pterosauria at the Cretaceous-Paleogene boundary". PLOS Biology 16 (3): e2001663. doi:10.1371/journal.pbio.2001663. PMID 29534059. 
  2. Andres, B.; Clark, J.; Xu, X. (2014). "The Earliest Pterodactyloid and the Origin of the Group". Current Biology 24 (9): 1011–6. doi:10.1016/j.cub.2014.03.030. PMID 24768054. https://www.cell.com/current-biology/pdfExtended/S0960-9822(14)00322-4. 
  3. Fernandes, Alexandra E.; Mateus, Octávio; Andres, Brian; Polcyn, Michael J.; Schulp, Anne S.; Gonçalves, António Olímpio; Jacobs, Louis L. (2022). "Pterosaurs from the Late Cretaceous of Angola". Diversity 14 (9): 741. doi:10.3390/d14090741. 

Wikidata ☰ Q50660755 entry