Published online by Cambridge University Press: 23 September 2025
We report a new stratigraphic section in the Argentine Precordillera (Zanja Honda, west of Pachimoco, San Juan Province), recording the Silurian-Devonian transition. It corresponds to particular siliciclastics of the uppermost 75 m of the Los Espejos Formation (LEF) exhibiting coquines at the base, noduliferous dark siltstones above, then greenish-brown sandstones, and subsequently, a reddish, massive, fine-grained sandstone interval. The overlying shaly lower interval of the Talacasto Formation records the homalonotid trilobite Burmeisteria notica (Clarke, 1913a), indicating the Lochkovian-Pragian interval. Brachiopods and trilobites of the basal coquinites are typical of the upper Silurian of the LEF elsewhere. However, Slovinograptus Urbanek, 1997, the youngest graptolite from southwestern Gondwana, indicates the Silurian-Devonian transition in the basal coquine. The dalmanitid Pachimocaspis pachimocensis new genus new species comes from this and other undoubted Silurian underlying coquinites. The brachiopod and trilobite associations disappear in the overlying dark nodular siltstone interval, replaced by an earliest Lochkovian Orthostrophia meridionalis Benedetto in Benedetto et al., 1992 brachiopod association and a monospecific Pachimocaspis pachimocensis n. gen. n. sp. Thus, we recognize a neat faunal turnover around the Silurian-Devonian boundary as in other southern South American localities. We refer to Pachimocaspis pachimocensis n. gen. n. sp. pygidia from the Silurian-Devonian of Bolivia and the lowest Pragian of the Talacasto Formation from Las Aguaditas locality in the Precordillera Basin. Pachimocaspis pachimocensis n. gen. n. sp. lacks the typical pygidial dalmanitid morphology, exhibiting instead a subelliptical shape with no caudal spine. Also, thoracic pleural tips are variably blunt along the thorax in contrast with the evenly spinose dalmanitid morphology. The morphology of this taxon challenges its systematic position in regarding Silurian-Devonian subfamilies from high paleolatitudes, resembling instead extra-Gondwanic, early Silurian synphoriines.
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Handling Editor: Thomas Hegna