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Douzhanopterus

From Wikipedia, the free encyclopedia
Genus of monofenestratan pterosaur from the Late Jurassic

Douzhanopterus
Temporal range:Oxfordian,160 Ma
Photograph of the type specimen ofDouzhanopterus (a) with closeups of the tail (b) and foot (c)
Scientific classificationEdit this classification
Kingdom:Animalia
Phylum:Chordata
Class:Reptilia
Order:Pterosauria
Clade:Pterodactyliformes
Genus:Douzhanopterus
Wanget al., 2017
Type species
Douzhanopterus zhengi
Wanget al., 2017

Douzhanopterus is an extinct genus ofmonofenestratanpterosaur from theLate Jurassic ofLiaoning,China. It contains a single species,D. zhengi, named by Wanget al. in 2017. In many respects, it represents atransitional form betweenbasal pterosaurs and the more specializedpterodactyloids; for instance, its tail is intermediate in length, still being about twice the length of thefemur but relatively shorter compared to that of the more basalWukongopteridae. Other intermediate traits include the relative lengths of theneck vertebrae and the retention of two, albeit reduced,phalanx bones in the fifth digit of the foot.Phylogenetically,Douzhanopterus is nested between the wukongopterids andPropterodactylus, which is similar toDouzhanopterus in many respects but approaches pterodactyloids more closely elsewhere.

Discovery and naming

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Theholotype specimen ofDouzhanopterus, a skeleton lacking the skull, is preserved on a plate and counterplate. The plate and counterplate are respectively catalogued as STM 19–35A and STM 19–35B, and they are stored at the Shandong Tianyu Museum of Nature inShandong,China. This specimen was purchased from a local farmer, who claimed that it had been excavated at Toudaoyingzi, Jiangchang inLiaoning province. However, the rock encasing the specimen is characteristic of sediments found at another locality within Liaoning, Linglongta. The latter belongs to the fossil-rich units of theTiaojishan Formation, which have been dated to 160.89 to 160.25 million years ago,[1] or theOxfordian stage of theJurassic period.[2]

In 2017, thetype and only speciesDouzhanopterus zhengi was named and described by Wang Xiaoli, Jiang Shunxing, Zhang Junqiang, Cheng Xin, Yu Xuefeng, Li Yameng, Wei Guangjin and Wang Xiaolin. The generic name combines the nameDòu-zhànshèng-fó (鬥戰勝佛, "Victorious Fighting Buddha"), which was given to the legendarySun Wukong when he attained the status ofBuddha, with the Latinised Greekpteron ("wing"). This is in reference to the animal occupying a more derived position relative to thewukongopterids. Thespecific name honours ProfessorZheng Xiaoting.[2]

Description

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Line drawing of the type specimen ofDouzhanopterus

Douzhanopterus was a relatively small pterosaur, with a wingspan of only 74 centimetres (29 in). The only known specimen represents an adult, judging by the degree of fusion in the hand bones,scapulocoracoid, and thetibia-fibula, as well as the fusion of the extensor tendon on the wing to the firstphalanx of the wing.[2][3][4]

Out of ninecervical vertebrae,[5] the last seven are definitely preserved, and theatlas andaxis may also be present. These vertebrae are long, generally about 2.5 to 3.5 times as long as they are wide. The vertebrae bear distinctcondyles for articulation with other vertebrae, and theneural spines are directed backwards and upwards; the ones near the middle also have prominentzygapophyses. Further along thevertebral column, there would have been 13dorsal vertebrae in total, followed by sixsacral vertebrae that form asacrum. These two types of vertebrae are similar, although the sideways-projecting transverse processes are more robust in the latter. In the tail were 22 caudal vertebrae, totalling to 83.86 mm (3.302 in) long, which is 173% the length of thehumerus. They increase in length from the first to the sixth but then become smaller after this point. Up until about the sixteenth caudal vertebra, the zygapophyses andchevrons are very long.[2]

Overall, thesternum is about as long as it is wide, with a forward-projecting front margin but a straight back margin. Thescapula is slender and long, being about 40% longer than thecoracoid; the coracoid itself does not bear any sort of expansion on its bottom surface. On the humerus, the deltopectoral crest is short and trapezoidal, and is placed at the top of the bone. A small crest is also present where the humerus articulates with theulna. Thepteroid, a bone unique to pterosaurs, is quite long, being about half as long as the ulna. In front of the pteroid, there is a smallsesamoid bone that is attached to the outer edge of thecarpals. The digits of the non-wing hand are somewhat long, being about 65% of humerus length and 53% of ulna length, and bear large claws. On the wing finger, the second phalanx is the longest, followed by the first and third, and then the fourth, which is still about 80% the length of the second.[2]

Fused entirely to the sacrum is thepelvic girdle. The portion of the pelvic girdle in front of thefemoral joint appears to consist of two unfused prepubes, which are longer than they are wide. Thefemur is slightly curved, and thefemoral head and neck form an angle of about 150° with the shaft. On the lower leg, the relatively straighttibia is about 180% the length of the femur; thefibula, which is about 45% the length of the tibia, is fused to it at both ends. Further below, the fivemetatarsals are rectangular. The second metatarsal is also the longest, followed again by the first and third, and then the fourth, with the third metatarsal being about 31% the length of the tibia. Unusually, the fifth digit of the foot still has two phalanges, the first straight and the second curved; the first is about 20% the length of the third metatarsal.[2]

Classification

[edit]

In 2017, Wanget al. assignedDouzhanopterus to theMonofenestrata.Douzhanopterus exhibits a number of characteristics that are intermediate between morebasal pterosaurs, including theWukongopteridae,[6][7][8][9] and the more derivedPterodactyloidea. In particular, the cervical vertebrae are generally longer; the tail is less than half of body length but still not particularly reduced; themetacarpals are moderately long compared to thehumerus andulna; and the fifth digit of the foot still bears twophalanges, although they are reduced with respect to basal pterosaurs but still larger than pterodactyloids. Its position in thephylogenetic tree recovered by Wanget al., the topology of which is partially reproduced below, is consistent with its intermediate condition.[2]

Monofenestrata

More derived thanDouzhanopterus is the "Painten pro-pterodactyloid", known from a juvenile specimen (later formally namedPropterodactylus[10]) from theKimmeridgian ofGermany.[11] They share a long fourth metacarpal, relatively reduced phalanges of the fifth digit on the foot, and a reduced but still relatively long tail with longzygapophyses andchevrons. However, several characteristics indicate thatDouzhanopterus is still more basal: thepteroid is larger relative to the ulna, thetibia is much longer than the femur, the tail is longer both absolutely (22 vertebrate and longer than the femur, as opposed to the 17 in the Painten specimen) and relative to the humerus, and the zygapophyses and chevrons are slightly longer.[11] These differences are probably not related to the young age of the Painten specimen, based on studies of unpublished juvenile monofenestratan specimens.[2]

References

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  1. ^Chu, Z.; He, H.; Ramezani, J.; Bowring, S.A.; Hu, D.; Zhang, L.; Zheng, S.; Wang, X.; Zhou, Z.; Deng, C.; Guo, J. (2016)."High-precision U-Pb geochronology of the Jurassic Yanliao Biota from Jianchang (western Liaoning Province, China): Age constraints on the rise of feathered dinosaurs and eutherian mammals".Geochemistry, Geophysics, Geosystems.17 (10):3983–3992.Bibcode:2016GGG....17.3983C.doi:10.1002/2016GC006529.
  2. ^abcdefghWang, X.; Jiang, S.; Zhang, J.; Cheng, X.; Yu, X.; Li, Y.; Wei, G.; Wang, X. (2017)."New evidence from China for the nature of the pterosaur evolutionary transition".Scientific Reports.7 (1) 42763.Bibcode:2017NatSR...742763W.doi:10.1038/srep42763.PMC 5311862.PMID 28202936.
  3. ^Bennett, S.C. (1993). "The Ontogeny ofPteranodon and Other Pterosaurs".Paleobiology.19 (1):92–106.Bibcode:1993Pbio...19...92B.doi:10.1017/S0094837300012331.JSTOR 2400773.
  4. ^Kellner, A.W.A. (2015)."Comments on Triassic pterosaurs with discussion about ontogeny and description of new taxa".Anais da Academia Brasileira de Ciências.87 (2):667–689.doi:10.1590/0001-3765201520150307.ISSN 1678-2690.PMID 26131631.
  5. ^Bennett, S.C. (2013). "A new specimen of the pterosaurScaphognathus crassirostris, with comments on constraint of cervical vertebrae number in pterosaurs".Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen.271 (3):327–348.doi:10.1127/0077-7749/2014/0392.
  6. ^Wang, X.; Kellner, A.W.A.; Jiang, S.; Meng, Xi (2009)."An unusual long-tailed pterosaur with elongated neck from western Liaoning of China".Anais da Academia Brasileira de Ciências.81 (4):793–812.doi:10.1590/S0001-37652009000400016.ISSN 1678-2690.PMID 19893903.
  7. ^Lu, J.; Unwin, D.M.; Jin, X.; Liu, Y.; Ji, Q. (2010)."Evidence for modular evolution in a long-tailed pterosaur with a pterodactyloid skull".Proceedings of the Royal Society B.277 (1680):383–389.doi:10.1098/rspb.2009.1603.PMC 2842655.PMID 19828548.
  8. ^Wang, X.; Kellner, A.W.A.; Jiang, S.; Cheng, X.; Meng, X.; Rodrigues, T. (2010)."New long-tailed pterosaurs (Wukongopteridae) from western Liaoning, China".Anais da Academia Brasileira de Ciências.82 (4):1045–1062.doi:10.1590/S0001-37652010000400024.ISSN 0001-3765.PMID 21152776.
  9. ^Lu, J.; Xu, L.; Chang, H.; Zhang, X. (2011). "A New Darwinopterid Pterosaur from the Middle Jurassic of Western Liaoning, Northeastern China and its Ecological Implications".Acta Geologica Sinica.85 (3):507–514.Bibcode:2011AcGlS..85..507L.doi:10.1111/j.1755-6724.2011.00444.x.
  10. ^Spindler, Frederik (2024-07-23)."A pterosaurian connecting link from the Late Jurassic of Germany".Palaeontologia Electronica.27 (2):1–27.doi:10.26879/1366.ISSN 1094-8074.
  11. ^abTischlinger, T.; Frey, E. (2013)."A new pterosaur with mosaic characters of basal and pterodactyloid pterosauria from the Upper Kimmeridgian of Painten (Upper Palatinate, Germany)".Archaeopteryx.31:1–13.
Avemetatarsalia
Pterosauria
    • see below↓
Preondactylia
Caviramidae?
Austriadraconidae
Raeticodactylidae
Eudimorphodontidae
Dimorphodontidae
Campylognathoididae
Rhamphorhynchidae
Scaphognathidae?
Pterodactylomorpha
    • see below↓
Campylognathoides liasicus

Scaphognathus crassirostris

Dorygnathus banthensis
Darwinoptera
Wukongopteridae
Anurognathidae
Pterodactyloidea
Lophocratia
    • see below↓
Jeholopterus ninchengensisKryptodrakon progenitor
Germanodactylidae
Gallodactylidae
Aurorazhdarchia
Aurorazhdarchidae
Ctenochasmatidae
Eupterodactyloidea
Ornithocheiroidea
    • see below↓
Pterodactylus antiquusPlataleorhynchus streptorophorodon
Dsungaripteridae
Thalassodromidae?
Tapejaridae
Dsungaripteromorpha?
Chaoyangopteridae
Azhdarchiformes
Alanqidae?
Azhdarchidae
Pteranodontoidea
    • see below↓
Bakonydraco galaczi

Tupandactylus imperator

Quetzalcoatlus
Pteranodontia
Pteranodontidae
Nyctosauromorpha
Aponyctosauria
Nyctosauridae
Lonchodectidae
Istiodactyliformes
Mimodactylidae
Istiodactylidae
Boreopteridae
Ornithocheiridae
Targaryendraconia?
Cimoliopteridae
Targaryendraconidae
Hamipteridae?
Anhangueridae
Pteranodon longiceps

Nyctosaurus gracilis

Ludodactylus sibbicki
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