Evidência de evolução modular em pterossauro de cauda longa com um crânio pterodactiloide

terça-feira, fevereiro 02, 2010

Evidence for modular evolution in a long-tailed pterosaur with a pterodactyloid skull

Junchang Lü1,*, David M. Unwin2, Xingsheng Jin3, Yongqing Liu1 and Qiang Ji1

-Author Affiliations

1Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, People's Republic of China

2School of Museum Studies, University of Leicester, 19 University Road, Leicester LE1 7RF, UK

3Zhejiang Museum of Natural History, Hangzhou, Zhejiang 310012, People's Republic of China

*Author for correspondence (lujc2008@126.com).


Abstract

The fossil record is a unique source of evidence for important evolutionary phenomena such as transitions between major clades. Frustratingly, relevant fossils are still comparatively rare, most transitions have yet to be documented in detail and the mechanisms that underpin such events, typified by rapid large scale changes and for which microevolutionary processes seem insufficient, are still unclear. A new pterosaur (Mesozoic flying reptile) from the Middle Jurassic of China, Darwinopterus modularisgen. et sp. nov., provides the first insights into a prominent, but poorly understood transition between basal, predominantly long-tailed pterosaurs and the more derived, exclusively short-tailed pterodactyloids.Darwinopterus exhibits a remarkable ‘modular’ combination of characters: the skull and neck are typically pterodactyloid, exhibiting numerous derived character states, while the remainder of the skeleton is almost completely plesiomorphic and identical to that of basal pterosaurs. This pattern supports the idea that modules, tightly integrated complexes of characters with discrete, semi-independent and temporally persistent histories, were the principal focus of natural selection and played a leading role in evolutionary transitions.


evolution    Middle Jurassic   China   Pterosauria    Pterodactyloidea   Darwinopterus

Footnotes

Received September 3, 2009.
Accepted September 24, 2009.
© 2009 The Royal Society

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