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Article: Geophilomorph centipedes from the Cretaceous amber of Burma

Publication: Palaeontology
Volume: 57
Part: 1
Publication Date: January 2014
Page(s): 97 110
Author(s): Lucio Bonato, Gregory D. Edgecombe and Alessandro Minelli
Addition Information

How to Cite

BONATO, L., EDGECOMBE, G. D., MINELLI, A. 2014. Geophilomorph centipedes from the Cretaceous amber of Burma. Palaeontology57, 1, 97–110, doi: 10.1111/pala.12051

Author Information

  • Lucio Bonato - Dipartimento di Biologia, Università degli Studi di Padova, Padova, Italy (email:
  • Gregory D. Edgecombe - Department of Earth Sciences, The Natural History Museum, London, UK (email:
  • Alessandro Minelli - Dipartimento di Biologia, Università degli Studi di Padova, Padova, Italy (email:

Publication History

  • Issue published online: 6 JAN 2014
  • Article first published online: 3 OCT 2013
  • Manuscript Accepted: 6 APR 2013
  • Manuscript Received: 14 FEB 2013

Online Version Hosted By

Wiley Online Library (Free Access)
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The only previously known Mesozoic fossils of the chilopod order Geophilomorpha are two species from the Late Jurassic and Late Cretaceous, both known from single specimens that cannot be assigned with precision to a family. Four specimens from the Late Cretaceous (earliest Cenomanian) amber of Burma include three that can be identified as conspecific, described here as Kachinophilus pereirai gen. nov. sp. nov. These specimens preserve greater morphological detail in comparison with other fossil geophilomorphs: the form and fine features of the head, the maxillary complex, the trunk sternites with associated glandular pores and the ultimate pair of legs defend the assignment of the species to the extant family Geophilidae, and most probably to a derived subgroup including well-known extant genera such as Ribautia Brölemann, 1909. Confocal laser scanning microscopy supplements examination under incident and transmitted light to document details of high taxonomic relevance in the head and the forcipular segment. The modern appearance of this species and its membership among deeply nested extant clades are consistent with molecular estimates that most of the diversity of crown-group Geophilomorpha originated before the Late Cretaceous.

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