Bee burrows in the Late Cretaceous (Late Cenomanian) Dakota Formation, northeastern Arizona

David K Elliott, J. Dale Nations

Research output: Contribution to journalArticle

31 Citations (Scopus)

Abstract

Cretaceous burrows attributable to bees are the earliest known record of activity by those insects and are equivalent in age to, or possibly older than, the oldest known bee body fossil. The burrows consist of vertical shafts from which short lateral corridors and numerous brood cells open. They occur in a lenticular fluvial sandstone in the middle carbonaceous member of the Late Cretaceous (Late Cenomanian) Dakota Formation. A new ichnospecies, Celliforma dakotensis, is proposed for this trace fossil, which is distinguished from other members of the ichnogenus by the size of the brood cells and the nest architecture. The presence of these burrows is consistent with the environmental interpretation of this part of the Dakota Formation as representing an aggrading coastal plain.

Original languageEnglish (US)
Pages (from-to)243-253
Number of pages11
JournalIchnos
Volume5
Issue number4
StatePublished - 1996

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burrow
bee
Cretaceous
trace fossil
coastal plain
shaft
nest
sandstone
fossil
insect

Keywords

  • Bees
  • Dakota Formation
  • Ichnofossil
  • Late Cretaceous
  • Paleoenvironment

ASJC Scopus subject areas

  • Palaeontology

Cite this

Bee burrows in the Late Cretaceous (Late Cenomanian) Dakota Formation, northeastern Arizona. / Elliott, David K; Nations, J. Dale.

In: Ichnos, Vol. 5, No. 4, 1996, p. 243-253.

Research output: Contribution to journalArticle

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