Taphonomy of fossil whales in the diatomaceous sediments of the Miocene/Pliocene Pisco Formation, Peru

Raul Esperante, Leonard Brand, Arthur Chadwick, Orlando Porna, Leonard R. Brand

Research output: Chapter in Book/Report/Conference proceedingChapter

Abstract

The Miocene/Pliocene Pisco Formation in Peru consists mostly of sandstones, siltstones, and tuffaceous beds in the lower units and diatomaceous mudstones in the upper units (Carvajal et af. 2000). Tuffaceous and diatomaceous sediments are rich in well-preserved fossil marine mammals (Esperante et af. 1999, 2000). Toothed whales (Suborder Odontoceti), baleen whales (Suborder Mysticeti), pinnipeds ofthe families Phocidae and Otariidae, dolphins, and shark teeth are the most abundant fossils, with sparse occurrences of other vertebrates, Invertebrates are rare, and are concentrated in a few beds. The purpose of this paper is to describe the general taphonomic features ofthe fossil whales of the Pisco Formation. Degree of articulation and preservation before burial, presence and absence of fauna associated with the whale bones, and the characteristics ofthe associated sediments are some ofthe features that will be addressed. These data will allow a more complete analysis of the paleoenvironment in which the whales died and were deposited,
Original languageAmerican English
Title of host publicationCurrent Topics on Taphonomy and Fossilization
StatePublished - 2002

Disciplines

  • Earth Sciences
  • Geology
  • Sedimentology

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