Skip to main content
Dryad

Data from: Palaeoscolecids from the Ludlow Series of Leintwardine, Herefordshire (UK) – the latest occurrence of palaeoscolecids in the fossil record

Data files

Apr 29, 2024 version files 1.81 GB
Apr 29, 2024 version files 1.81 GB

Abstract

The documentation of cuticular micro-ornament is vital for the taxonomic assignment of palaeoscolecids – vermiform lower Palaeozoic ecdysozoans interpreted as stem-group priapulans or early diverging panarthropods. This is due to the absence of the character-rich proboscis and tail hooks in palaeoscolecid material not from Burgess Shale-type Konservat-Lagerstätten. Here, the cuticular micro-ornamentation of palaeoscolecids from the upper Silurian (Ludlow) fauna of Leintwardine (Herefordshire, England), is described using scanning electron microscopy (SEM) and Reflectance Transformation Imaging (RTI). This material is taxonomically unstable as it was included in an effective wastebasket genus (Protoscolex) long before these imaging techniques were developed. This reveals the Leintwardine material is most closely comparable to a palaeoscolecid from the Darriwilian (Middle Ordovician) of the Builth-Llandrindod inlier, Powys, Wales, and is transferred accordingly to Radnorscolex Botting et al. as Radnorscolex latus Bather. The Leintwardine fauna represents the uppermost stratigraphic occurrence of palaeoscolecids, constrained to the Saetograptus leintwardinensis Zone (lower Ludfordian), and the comparatively sparse Silurian palaeoscolecid record is subsequently discussed. It is hypothesised palaeoscolecids may have become extinct during the mid-Ludfordian Lau Event, the onset of which is recorded in the biozone immediately above the Leintwardine fauna (Bohemograptus Zone). Finally, the British palaeoscolecid fauna is summarised, including a new record from the Dapingian (Middle Ordovician) of Carmarthenshire, South Wales.