Abstract

AbstractConodonts are an extinct group of early vertebrates. Articulated fossils of their feeding apparatus (‘natural assemblages’) are rare, and preserved soft tissues vanishingly so. Here, a primitive conodont with preserved soft tissues is redescribed from the Waukesha Lagerstätte of Wisconsin, USA. Although the feeding apparatus of derived prioniodontid conodonts is well understood, together with the homologies between taxa, the same is not true of more primitive conodonts that have apparatuses composed entirely of coniform elements. The new data provide insights into the long‐term problem of determining homology across different types of conodont feeding apparatus. The Waukesha Panderodus preserves an almost complete apparatus, consisting of two parallel rows of elements that occluded across the sagittal plane. A pair of M elements lies at the rostral end of the apparatus, with four pairs of S elements located immediately caudal to them. Three pairs of P elements are identified at the caudal end of the apparatus, for the first time in a primitive conodont with coniform elements. A symmetrical S0 element is located on the midline between the M–S and P suites and provides the key for establishing homology with more derived ramiform–pectiniform apparatuses. The exceptional preservation reveals cartilaginous supports for the elements that inserted into their basal cavities. The trunk of the animal is poorly preserved but was dorsoventrally flattened in life with transverse myomeres containing muscle fibrils. Overall, the specimen shows that Panderodus was a macrophagous feeder and provides an insight into the functional anatomy of early vertebrate predation.

Highlights

  • MATERIAL AND METHODMore organic-rich, argillaceous, dolostones (Wendruff et al 2020); the Panderodus specimen is preserved in the former lithology

  • T H E fossil record of vertebrates currently extends back to the early Cambrian and the initial diversification of bilaterian animal groups

  • The rostral feeding apparatus is composed of 17 coniform elements, with eight dextral– sinistral pairs in opposition across the sagittal plane of the animal and an additional symmetrical S0 element that sat on the midline

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Summary

MATERIAL AND METHOD

More organic-rich, argillaceous, dolostones (Wendruff et al 2020); the Panderodus specimen is preserved in the former lithology. The anatomy present in the Waukesha specimen cannot be explained entirely by preservation at a late stage of decay, most conspicuously the absence of the large pair of lobate structures interpreted as eyes that are so clearly associated with better preserved conodont taxa (Briggs et al 1983; Gabbott et al 1995), and some natural assemblages of feeding apparatuses in which no other soft tissues are present (Aldridge et al 2013). These are concentrated at the lateral margins of the body trace where the remains of arcuate myomeres begin to diverge, and along the midline of the body where the opposing myomeres meet; the latter may represent the filling of voids left by the decay of axial structures

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