4.2 Article

An exceptional record of Cambrian trilobite moulting behaviour preserved in the Emu Bay Shale, South Australia

Journal

LETHAIA
Volume 51, Issue 4, Pages 473-492

Publisher

WILEY
DOI: 10.1111/let.12266

Keywords

Burgess Shale; Cambrian; ecdysis; Emu Bay Shale; Lagerstatten; moult configuration; trilobite

Categories

Funding

  1. Natural Environment Research Council doctoral training grant [NE/L002612/1]
  2. University of Adelaide
  3. Australian Research Council [FT130101329, LP0774959, DP120104251]
  4. Oxford University Museum of Natural History
  5. Palaeontological Association [PA-WA201401]
  6. Spanish Ministry of Science and Innovation [CGL2009-070073]
  7. Spanish Ministry of Economy and Competitivity [CGL2013-48877-P]
  8. National Geographic Society Research Exploration [8991-11]

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Trilobites dominate the Emu Bay Shale (EBS) assemblage (Cambrian Series 2, Stage 4, South Australia) in terms of numbers, with Estaingia bilobata Pocock being extremely abundant, and the larger Redlichia takooensis Lu , being common. Many specimens within the EBS represent complete moulted exoskeletons, which is unusual for Cambrian fossil deposits. The abundance of complete moults provides an excellent record that has allowed the recognition of various recurrent moult configurations for both species, enabling the inference of movement sequences required to produce such arrangements. Moult configurations of E.bilobata are characterized by slight displacement of the joined rostral plate and librigenae, often accompanied by detachment of the cranidium, suggesting ecdysis was achieved by anterior withdrawal via opening of the cephalic sutures. Moulting in R.takooensis often followed the same method, but configurations show greater displacement of cephalic sclerites, suggesting more vigorous movement by the animal during moulting. Both species also show rare examples of Salter's configuration, with the entire cephalon anteriorly inverted, and several other unusual configurations. These results indicate that moulting in trilobites was a more variable process than originally thought. In contrast, other Cambrian Konservat-Lagerstatten with an abundance of trilobites (e.g. Wheeler Shale, USA, and Mount Stephen Trilobite Beds, Canada) show larger numbers of axial shields' and isolated sclerites, often interpreted as disarticulated exuviae. This points to a higher level of disturbance from factors, such as animal activity, depositional processes or water movement, compared to that of the EBS, where quiescent conditions and intermittent seafloor anoxia contributed to an unparalleled trilobite moulting record.

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