4.1 Article

First record of the brachiopod Lingulella waptaensis with pedicle from the Middle Cambrian Burgess Shale

Journal

ACTA ZOOLOGICA
Volume 91, Issue 2, Pages 150-162

Publisher

WILEY-BLACKWELL PUBLISHING, INC
DOI: 10.1111/j.1463-6395.2009.00394.x

Keywords

Brachiopoda; Lingulella; pedicle; Middle Cambrian; Burgess Shale

Funding

  1. Swedish Research Council
  2. Natural Sciences and Engineering Research Council of Canada

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Pettersson Stolk, S., Holmer, L. E. and Caron, J -B. 2010. First record of the brachiopod Lingulella waptaensis with pedicle from the Middle Cambrian Burgess Shale. -Acta Zoologica (Stockholm) 91: 150-162 The organophosphatic shells of linguloid brachiopods are a common component of normal Cambrian-Ordovician shelly assemblages. Preservation of linguloid soft-part anatomy, however, is extremely rare, and restricted to a few species in Lower Cambrian Konservat Lagerstatten. Such remarkable occurrences provide unique insights into the biology and ecology of early linguloids that are not available from the study of shells alone. Based on its shells, Lingulella waptaensis Walcott, was originally described in 1924 from the Middle Cambrian Burgess Shale but despite the widespread occurrence of soft-part preservation associated with fossils from the same levels, no preserved soft parts have been reported. Lingulella waptaensis is restudied herein based on 396 specimens collected by Royal Ontario Museum field parties from the Greater Phyllopod Bed (Walcott Quarry Shale Member, British Columbia). The new specimens, including three with exceptional preservation of the pedicle, were collected in situ in discrete obrution beds. Census counts show that L. waptaensis is rare but recurrent in the Greater Phyllopod Bed, suggesting that this species might have been generalist. The wrinkled pedicle protruded posteriorly between the valves, was composed of a central coelomic space, and was slender and flexible enough to be tightly folded, suggesting a thin chitinous cuticle and underlying muscular layers. The nearly circular shell and the long, slender and highly flexible pedicle suggest that L. waptaensis lived epifaunally, probably attached to the substrate. Vertical cross-sections of the shells show that L. waptaensis possessed a virgose secondary layer, which has previously only been known from Devonian to Recent members of the Family Lingulidae.

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