Dinosaur footprints and other ichnofauna from the cretaceous Kem Kem beds of Morocco.

We describe an extensive ichnofossil assemblage from the likely Cenomanian-age 'lower' and 'upper' units of the 'Kem Kem beds' in southeastern Morocco. In the lower unit, trace fossils include narrow vertical burrows in cross-bedded sandstones and borings in dinosaur bo...

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Main Authors: Nizar Ibrahim, David J Varricchio, Paul C Sereno, Jeffery A Wilson, Didier B Dutheil, David M Martill, Lahssen Baidder, Samir Zouhri
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2014-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC3946209?pdf=render
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spelling doaj-96d39279d7914fddb64f3d4ed0f22fe82020-11-24T21:38:21ZengPublic Library of Science (PLoS)PLoS ONE1932-62032014-01-0196e9075110.1371/journal.pone.0090751Dinosaur footprints and other ichnofauna from the cretaceous Kem Kem beds of Morocco.Nizar IbrahimDavid J VarricchioPaul C SerenoJeffery A WilsonDidier B DutheilDavid M MartillLahssen BaidderSamir ZouhriWe describe an extensive ichnofossil assemblage from the likely Cenomanian-age 'lower' and 'upper' units of the 'Kem Kem beds' in southeastern Morocco. In the lower unit, trace fossils include narrow vertical burrows in cross-bedded sandstones and borings in dinosaur bone, with the latter identified as the insect ichnotaxon Cubiculum ornatus. In the upper unit, several horizons preserve abundant footprints from theropod dinosaurs. Sauropod and ornithischian footprints are much rarer, similar to the record for fossil bone and teeth in the Kem Kem assemblage. The upper unit also preserves a variety of invertebrate traces including Conichnus (the resting trace of a sea-anemone), Scolicia (a gastropod trace), Beaconites (a probable annelid burrow), and subvertical burrows likely created by crabs for residence and detrital feeding on a tidal flat. The ichnofossil assemblage from the Upper Cretaceous Kem Kem beds contributes evidence for a transition from predominantly terrestrial to marine deposition. Body fossil and ichnofossil records together provide a detailed view of faunal diversity and local conditions within a fluvial and deltaic depositional setting on the northwestern coast of Africa toward the end of the Cretaceous.http://europepmc.org/articles/PMC3946209?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Nizar Ibrahim
David J Varricchio
Paul C Sereno
Jeffery A Wilson
Didier B Dutheil
David M Martill
Lahssen Baidder
Samir Zouhri
spellingShingle Nizar Ibrahim
David J Varricchio
Paul C Sereno
Jeffery A Wilson
Didier B Dutheil
David M Martill
Lahssen Baidder
Samir Zouhri
Dinosaur footprints and other ichnofauna from the cretaceous Kem Kem beds of Morocco.
PLoS ONE
author_facet Nizar Ibrahim
David J Varricchio
Paul C Sereno
Jeffery A Wilson
Didier B Dutheil
David M Martill
Lahssen Baidder
Samir Zouhri
author_sort Nizar Ibrahim
title Dinosaur footprints and other ichnofauna from the cretaceous Kem Kem beds of Morocco.
title_short Dinosaur footprints and other ichnofauna from the cretaceous Kem Kem beds of Morocco.
title_full Dinosaur footprints and other ichnofauna from the cretaceous Kem Kem beds of Morocco.
title_fullStr Dinosaur footprints and other ichnofauna from the cretaceous Kem Kem beds of Morocco.
title_full_unstemmed Dinosaur footprints and other ichnofauna from the cretaceous Kem Kem beds of Morocco.
title_sort dinosaur footprints and other ichnofauna from the cretaceous kem kem beds of morocco.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2014-01-01
description We describe an extensive ichnofossil assemblage from the likely Cenomanian-age 'lower' and 'upper' units of the 'Kem Kem beds' in southeastern Morocco. In the lower unit, trace fossils include narrow vertical burrows in cross-bedded sandstones and borings in dinosaur bone, with the latter identified as the insect ichnotaxon Cubiculum ornatus. In the upper unit, several horizons preserve abundant footprints from theropod dinosaurs. Sauropod and ornithischian footprints are much rarer, similar to the record for fossil bone and teeth in the Kem Kem assemblage. The upper unit also preserves a variety of invertebrate traces including Conichnus (the resting trace of a sea-anemone), Scolicia (a gastropod trace), Beaconites (a probable annelid burrow), and subvertical burrows likely created by crabs for residence and detrital feeding on a tidal flat. The ichnofossil assemblage from the Upper Cretaceous Kem Kem beds contributes evidence for a transition from predominantly terrestrial to marine deposition. Body fossil and ichnofossil records together provide a detailed view of faunal diversity and local conditions within a fluvial and deltaic depositional setting on the northwestern coast of Africa toward the end of the Cretaceous.
url http://europepmc.org/articles/PMC3946209?pdf=render
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