A crocodylian trace from the Lance Formation (Upper Cretaceous) of Wyoming

Peter L Falkingham; Jesper Milàn; Philip L Manning

A crocodylian trace from the Lance Formation (Upper Cretaceous) of Wyoming

Peter L Falkingham, Jesper Milàn, Philip L Manning

Geologi

Abstract

A 1.5-m-long double sinusoidal trace from the Lance Formation of Wyoming, U.S.A, is attributed a crocodylian origin. The trace forms part of a diverse tracksite containing dinosaur and bird tracks. The double sinusoidal nature of the trace is suggested to have originated from the dual undulatory motion of body and tail. Other features such as scute and claw marks are comparable with modern crocodyle traces, even though clear footprints have not been identified. The trace therefore expands upon the already diverse dinosaurian ichnofauna of the Lance Formation to include crocodylians.

Originalsprog	Engelsk
Tidsskrift	New Mexico Museum of Natural History and Science. Bulletin
Vol/bind	51
Sider (fra-til)	171-174
Antal sider	4
ISSN	1524-4156
Status	Udgivet - 2010

Citationsformater

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title = "A crocodylian trace from the Lance Formation (Upper Cretaceous) of Wyoming",

abstract = "A 1.5-m-long double sinusoidal trace from the Lance Formation of Wyoming, U.S.A, is attributed a crocodylian origin. The trace forms part of a diverse tracksite containing dinosaur and bird tracks. The double sinusoidal nature of the trace is suggested to have originated from the dual undulatory motion of body and tail. Other features such as scute and claw marks are comparable with modern crocodyle traces, even though clear footprints have not been identified. The trace therefore expands upon the already diverse dinosaurian ichnofauna of the Lance Formation to include crocodylians.",

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journal = "New Mexico Museum of Natural History and Science. Bulletin",

issn = "1524-4156",

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TY - JOUR

T1 - A crocodylian trace from the Lance Formation (Upper Cretaceous) of Wyoming

AU - Falkingham, Peter L

AU - Milàn, Jesper

AU - Manning, Philip L

PY - 2010

Y1 - 2010

N2 - A 1.5-m-long double sinusoidal trace from the Lance Formation of Wyoming, U.S.A, is attributed a crocodylian origin. The trace forms part of a diverse tracksite containing dinosaur and bird tracks. The double sinusoidal nature of the trace is suggested to have originated from the dual undulatory motion of body and tail. Other features such as scute and claw marks are comparable with modern crocodyle traces, even though clear footprints have not been identified. The trace therefore expands upon the already diverse dinosaurian ichnofauna of the Lance Formation to include crocodylians.

AB - A 1.5-m-long double sinusoidal trace from the Lance Formation of Wyoming, U.S.A, is attributed a crocodylian origin. The trace forms part of a diverse tracksite containing dinosaur and bird tracks. The double sinusoidal nature of the trace is suggested to have originated from the dual undulatory motion of body and tail. Other features such as scute and claw marks are comparable with modern crocodyle traces, even though clear footprints have not been identified. The trace therefore expands upon the already diverse dinosaurian ichnofauna of the Lance Formation to include crocodylians.

M3 - Journal article

SN - 1524-4156

VL - 51

SP - 171

EP - 174

JO - New Mexico Museum of Natural History and Science. Bulletin

JF - New Mexico Museum of Natural History and Science. Bulletin

ER -