Abstract

The fauna of the Middle Devonian Red Hill I locality, Nevada, is unusual in the co-occurrence of a rich fish assemblage with a rich invertebrate one. Sponges are second in abundance of specimens and number of species only to the fishes and occur together with other invertebrates (conodonts, conulariids, dacryoconarid tentaculites, gastropods, bivalves, brachiopods, arthropods, and unidentifiable ammonoids and echinoderms). The invertebrates indicate a marine depositional paleoenvironment. The conodonts indicate a placement within the lower <i>disparalis</i> Zone, late Givetian. The fish assemblage is dominated by the antiarch <i>Asterolepis</i>. All the other fishes, acanthodians, actinopterygians and sarcopterygians, are less common. The closest biogeographic relationship of the fish fauna is with the Middle/Late Devonian fish fauna of the Baltic Region, followed by that of eastern Canada (Miguasha), Scotland and Iran. This distribution corresponds to the Devonian Euramerica faunal province with connection to eastern Gondwana (Iran and Australia). Localities with the same genera as Red Hill I are interpreted as marine with the exception of the Scottish localities. <i>Asterolepis</i> is the most widely distributed vertebrate genus, mostly marine, but it may be able to enter freshwater like <i>Eusthenopteron</i> if one accepts a freshwater depositional paleoenvironment for the Scottish localities. <br><br> doi:<a href="http://dx.doi.org/10.1002/mmng.201000001" target="_blank">10.1002/mmng.201000001</a>

Highlights

  • Red Hill I forms the northern end of the Northern Simpson Park Range, northwest of Eureka, Nevada

  • The locality was discovered by Michael Murphy from University of California, Riverside, California, in 1973

  • The Middle/Late Devonian boundary lies within the Red Hill Beds just above the fish beds

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Summary

Introduction

Red Hill I forms the northern end of the Northern Simpson Park Range, northwest of Eureka, Nevada. The Middle/Late Devonian boundary lies within the Red Hill Beds just above the fish beds. The placement of the Red Hill I fish beds into the earliest Late Devonian

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