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Brachiopod giants from the Mississippian (Asbian) of western Ireland: Fossil bioarchives of seasonality and symbiosis and far-field harbingers of climate change

  • Lucia Angiolini
  • , Karem Azmy
  • , Enrico Cannaò
  • , Gaia Crippa
  • , Eamon Doyle
  • , Giovanna Della Porta
  • , John Murray
  • , Michael O'Connell
  • , Marco Viaretti
  • , David A.T. Harper
    • University of Milan
    • Memorial University of Newfoundland
    • Clare County Council
    • Botany and Plant Science and Martin Ryan Institute
    • Mainistir
    • Department of Earth Sciences
    • Durham University

    Research output: Contribution to a Journal (Peer & Non Peer)Articlepeer-review

    1 Citation (Scopus)

    Abstract

    Brachiopod species of Gigantoproductus have long fascinated researchers, not only because of their exceptional size and thick shell, but also as unparalleled bioarchives for palaeoecological and palaeoclimatic information. In this paper, we describe faunas containing Gigantoproductus semiglobosus from upper Visean (upper Asbian) successions in two regions of western Ireland, and report geochemical analyses that improve understanding of the palaeobiology of these brachiopods. The two regions are the Burren, where the Aillwee Member (Burren Formation) comprises thick-bedded cyclic bioclastic packstone to grainstone, interpreted as the deposits in predominantly shallow-water (subtidal) marine environments with episodic subaerial exposure, and the Aran Islands, where the Slievenaglasha Formation comprises cyclic crinoidal limestones with chert, deposited in slightly deeper water conditions. Shallowing upward fourth-order cycles in both regions have previously been interpreted as being under a glacioeustatic control. Reconstructed δ13Corg and δ15Norg of soft tissues of G. semiglobosus are respectively −29.0 to −30.1 ‰ (VPDB) and − 1.4 ‰ and + 6.1 ‰ (Air) and serve as proxies for identifying photosymbiotic relationships and a mixotroph lifestyle for this species. Well-preserved δ18Ocarb profiles record high seasonal variations (Δδ18O = 0.9 to 1.9 ‰ corresponding to a ΔT = 4 to 11 °C) for palaeoequatorial settings as a far-field proxy of the onset of sustained Gondwanan glaciation in the late Visean and provide evidence of warm tropics during the glaciation. The δ13Ccarb profiles are mostly controlled by local influences and changes in productivity. Our geochemical analyses of growth patterns, seasonal variation, diet and endosymbiosis in G. semiglobosus, sheds new light on the paradox of these unusual brachiopods, and provides a greater understanding of their massive size.

    Original languageEnglish
    Article number113418
    JournalPalaeogeography, Palaeoclimatology, Palaeoecology
    Volume683
    DOIs
    Publication statusPublished - 1 Feb 2026

    Keywords

    • Carbonate facies
    • Gigantoproductus
    • Isotopes
    • Late Palaeozoic climate
    • Western Ireland

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