4.1 Article

Late Devonian (Famennian) phacopid trilobites from western Xinjiang, Northwest China

Journal

PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS
Volume 103, Issue 2, Pages 327-340

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s12549-022-00547-x

Keywords

Trilobites; Phacopidae; lower Famennian; Hongguleleng Formation; Biodiversity; Taxonomy

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An early Famennian trilobite fauna from the lower member of the Hongguleleng Formation in northwestern China is described. The Hongguleleng Formation is a volcanic arc-related shallow marine shelf deposit, consisting of bioclastic argillaceous limestones, marls, and green calcareous shales. The studied material, although often poorly preserved, includes specimens of Clarksonops junggariensis gen. nov. sp. nov. and Houseops cf. olonbulagensis, which are the first known and described trilobites from lower Famennian deposits in northwestern China.
An early Famennian trilobite fauna represented by phacopids is recorded and illustrated from the lower member of the Hongguleleng Formation (crepida conodont Zone) near the Bulongguoer Reservoir in northwestern Xinjiang, northwestern China. In this area, the Hongguleleng Formation is rich in diverse faunas and exposes bioclastic argillaceous limestones and marls, intercalated with green calcareous shales of Famennian shallow marine shelf deposits formed in a volcanic arc-related setting. The studied material is most often incomplete, often poorly preserved as internal molds. Due to insufficient preservation of well-preserved cephala, additional material is required. However, among faunas, the Hongguleleng Formation contains specimens of Clarksonops junggariensis gen. nov. sp. nov., a so-far endemic taxon, which is the first known and described representatives of trilobites from lower Famennian deposits of northwestern China; and ?Houseops cf. olonbulagensis, a taxon encountered in western Mongolia. Their affinities with known other sighted species of the same age are discussed.

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