4.3 Article

A low diversity Sinuites gastropod community from the Floian, Early Ordovician , of South Wales

Journal

ACTA PALAEONTOLOGICA POLONICA
Volume 66, Issue 2, Pages 319-335

Publisher

INST PALEOBIOLOGII PAN
DOI: 10.4202/app.00854.2020

Keywords

Gastropoda; Onychochilidae; Tetgomva; biogeography; Floian; Arenig; Ordovician; Avalonia; UK

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This study describes a low diversity gastropod community dominated by Sinuites in the South Wales Llangynog Inlier, with an exceptionally diverse mollusc-dominated fauna and three new species described. The locality shows a high resemblance to contemporaneous high-latitude peri-Gondwana areas, with the presence of rare tergomyans and a significant addition to the global Floian record.
A low diversity Sinuites-dominated gastropod community is described from the Floian, Arenig Series, of the Llangynog Inlier, southwest of Carmarthen, South Wales. The abundant material comes from shallow-water siltstone and mudstone beds of the Bolahaul Member of the Ogof Hen Formation. The locality has an exceptionally diverse mollusc-dominated fauna (63.5% of the fauna), with gastropods constituting 6% and tergomyans 1% and echinoderms, arthropods and other fauna making up the rest. Except for one rare tergomyan mollusc, identified as Catrassonnella cf. vizcainoi, other tergomyans are described elsewhere. Nearly half of all gastropod specimens are represented by Sinuites ramseyensis. Three of the five taxa described are new: Mimospira llangynogensis sp. nov., Catalanispira prima sp. nov., and Ceratopea? moridunensis sp. nov. The assemblage compares best with those of contemporaneous high-latitude peri-Gondwana areas. Early Ordovician species of Catva.ssonnella are typically found in France, Iberia, Czech Republic, and Morocco, while species ofillimospira are found in Germany and Czech Republic, but also in Baltica where the main radiation took place later. Two of the oldest occurrences of Mimospira are from Avalonian Wales (Carmarthenshire and Anglesey). Catalanispira occurs later in Baltica and Laurentia in the late Middle and early Late Ordovician, when taxa from these areas start to appear in Wales and vice versa. The presence of Ceratopea?, a genus typical of Laurentia, is at odds with the biogeographic distribution of faunas at this time. Part of the observed distribution pattern may be explained by different latitudinal position and facies depths of Avalonia compared to Armorica, Bohemia, and Morocco. The species described herein are amongst the first Floian taxa of these groups formally described from this area and add significantly to the global Floian record.

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