Abstract

A trilobite fauna of Pterospathodus celloni Biozone age (late Llandovery) is described from a horizon near the top of the Odins Fjord Formation. The commonest trilobite is the phacopid Acernaspis sp., with which are associated the proetid Cyphoproetus? cf. C. alyo, the harpetid Scotoharpes?, a second phacopid (Ananaspis?), the encrinurid Briania and an undetermined encrinurid. The llilobile species compare closely with others already described from various localities in the mid-late Llandovery of Greenland and Canada. The overall composition of the trilobite fauna, however, contrast with that previously known from the Odins Fjord Formation; this may partly reflect the more offshore position of the Schley Fjord fauna on the Peary Land shelf. However, drowning of the shelf produced a possibly diachronous decrease in fauna! content and diversity as deepening and muddying progressed southwards over time. Thus, faunal contrasts may simply reflect sampling of different levels within this muddying-upwards succession.

Highlights

  • A trilobite fauna of Pterospatlwdus celloni Biozone age is described from a horizon near the top of the Odins Fjord Formation

  • The upper 30-40 m of the Odins Fjord Formation lime­ stones at this locality show a progressive facies change upwards, becoming darker, more argillaceous, thinly bed­ ded and nodular

  • The fossils were collected from the uppermost beds of the Odins Fjord Formation, some 2-3 m below the top

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Summary

Introduction

A trilobite fauna of Pterospatlwdus celloni Biozone age (late Llandovery) is described from a horizon near the top of the Odins Fjord Formation. The small collection of trilobites described here was obtained by R. R. Ineson in 1978 when they were engaged in the reconnaissance field mapping programme of the Peary Land region.

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