Transitional fossil

The London specimen of Archaeopteryx, discovered only two years after the publication of On the Origin of Species

Transitional fossils (or missing links) are the fossilised remains of lifeforms that show features typical of two distinct groups. It may be a rare fossil, such as Archaeopteryx, which shows early features of a group which later becomes widespread.

The rarity of transitional forms is interesting. It suggests the new forms are not yet dominant in the ecology of their time, and their populations are relatively small. It follows that their fossils would be scarce. In the Solnhofen limestone where Archaeopteryx was found, there are more examples of pterosaurs of several genera than there are of the proto-bird.[1] In the Jurassic, the pterosaurs were dominant in the air.

Large numbers of different bird species are found in the famous Chinese lagerstatten deposits such as the Jehol biota. The Lower Cretaceous birds are clearly more bird-like, and the features they developed enabled them to invade habitat niches which had been the preserve of pterosaurs, or maybe were not previously exploited at all.

Pterosaur decline (if present) seems unrelated to bird diversity.[2] In fact, at least some bird niches were reclaimed by pterosaurs just before the KT event.[3]

  1. up to 29 species and nine genera of pterosaur have been found there. Bartell K.W., Swinburne N.H.M. and Conway-Morris S. 1990. Solnhofen: a study in Mesozoic palaeontology. Cambridge University Press. Transl. and revised from Bartel K.W. 1978. Ein Blick in die Erdgeschichte. Ott.
  2. Butler, Richard J.; Barrett, Paul M.; Nowbath, Stephen & Upchurch, Paul (2009). "Estimating the effects of sampling biases on pterosaur diversity patterns: implications for hypotheses of bird/pterosaur competitive replacement". Paleobiology. 35 (3): 432–46. doi:10.1666/0094-8373-35.3.432. S2CID 84324007.
  3. Longrich N.R.; Martill D.M.; Andres B. 2018. Late Maastrichtian pterosaurs from North Africa and mass extinction of Pterosauria at the Cretaceous-Paleogene boundary. PLOS Biology 16 (3): [1]

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