Regeneration of Desert Pavement and Varnish

1983 ◽  
pp. 225-243 ◽  
Author(s):  
Christopher D. Elvidge ◽  
Richard M. Iverson
Keyword(s):  
Desert Pavement

Desert pavement-coated surfaces in extreme deserts present the longest-lived landforms on Earth

2009 ◽  
Vol 121 (5-6) ◽  
pp. 688-697 ◽  
Author(s):  
A. Matmon ◽  
O. Simhai ◽  
R. Amit ◽  
I. Haviv ◽  
N. Porat ◽  
...  
Keyword(s):  
Desert Pavement ◽  
Coated Surfaces

Desert pavement development and landscape stability on the Eastern Libyan Plateau, Egypt

Geomorphology ◽  
2009 ◽  
Vol 107 (3-4) ◽  
pp. 178-194 ◽  
Author(s):  
Katherine A. Adelsberger ◽  
Jennifer R. Smith
Keyword(s):  
Desert Pavement

Desert Pavement Disturbance and Artifact Taphonomy: A Case Study from the Eastern Libyan Plateau, Egypt

2013 ◽  
Vol 28 (2) ◽  
pp. 112-130 ◽  
Author(s):  
Katherine A. Adelsberger ◽  
Jennifer R. Smith ◽  
Shannon P. McPherron ◽  
Harold L. Dibble ◽  
Deborah I. Olszewski ◽  
...  
Keyword(s):  
Desert Pavement

Analysis of a Well-Performing Desert Pavement

2009 ◽  
pp. 146-146-20
Author(s):  
P Sebaaly ◽  
V Thirmarayappa ◽  
J Epps ◽  
L Quilici
Keyword(s):  
Desert Pavement

scholarly journals The Upper Campanian – lower Maastrichtian cephalopod fauna of Botellos, Nuevo León: a key to understand faunal turnover across the Campanian–Maastrichtian boundary in NE Mexico

2017 ◽  
Vol 67 (1) ◽  
pp. 145-162 ◽  
Author(s):  
Christina Ifrim ◽  
Jacobo Edgar Lara De La Cerda ◽  
Victor Hugo Peña Ponce ◽  
Wolfgang Stinnesbeck
Keyword(s):  
North America ◽  
Nuevo Leon ◽  
Faunal Turnover ◽  
Desert Pavement ◽  
Nuevo León ◽  
Lower Maastrichtian ◽  
Upper Campanian

Abstract A new cephalopod collection from the Campanian-Maastrichtian boundary interval of NE Mexico, consisting of 1076 individuals assigned to 29 species and 22 genera is presented. This collection is a mix of ammonoids, one coleoid and one nautilid, which originate from at least three ammonoid biozones: The upper Campanian Exiteloceras jenneyi and Nostoceras (Nostoceras) hyatti zones, and the lower Maastrichtian Pachydiscus (Pachydiscus) neubergicus Zone. The age of the collection is thus middle late Campanian to late early Maastrichtian, and it closes a stratigraphic gap between faunas described formerly from this region. The specimens are nuclei collected from the desert pavement. The abundance of specimens allows for a comparison to other Campanian-Maastrichtian ammonoid records from Mexico, North America and Europe.

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