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Figure 1: Index maps showing location of the Carrizo Arroyo section in central New Mexico In contrast to the highly diverse earliest Pennsylvanian (Bashkirian) marine insect fossil-Lagerstätten of Ningxia, China, and Hagen-Vorhalle, Germany, Middle Pennsylvanian to Early Permian insect sites worldwide are dominated by fossils of cockroachoids [14]. Most of these sites are situated in the roof shales and interbeds of coal seams, such as Mazon Creek, Writhlington, Commentry, Wettin, Kuznetsk, etc. [5-8]. They mainly reflect the environments of wet coal forests of the Late Pennsylvanian and earliest Permian [9]. The earliest Permian Carrizo Arroyo site in New Mexico (Figure 1), investigated during the last decade, represents a new taphotype of arthropod Fossillagerstätten, which will be discussed here. The general depositional environment of this site is interpreted by Lucas & Krainer [10] as a coastal plain on a very shallow shelf during repeated transgressions and regressions, as evidenced by Abstract

Carrizo Arroyo, Central New Mexico - A New Late Paleozoic Taphotype of Arthropod Fossillagerstätte