Repository logo
Home
Research Outputs
Collections
Statistics
Shared Repository Homepage
  1. Home
  2. Cultural Heritage Shared Repository Service
  3. National Museum Scotland
  4. Conference Item
  5. Brachiopods from the Ordovician of southern Belgium (Avalonia): the end of a terra incognita

Brachiopods from the Ordovician of southern Belgium (Avalonia): the end of a terra incognita

Resource type
Abstract
Creator (person)
Mottequin, Bernard
Candela, Yves
ORCIDORCID logo
Abstract
Contrary to the well-exposed Devonian–Carboniferous rock sequence, the thick siliciclastic Cambrian–Silurian succession of Belgium is poor in macrofossils and, more especially, in brachiopods. These rocks mostly crop out in the Brabant and the Stavelot–Venn massifs, and in the Condroz Inlier. Occurrences of Ordovician brachiopods have been reported since the second half of the 19th century in the Brabant Massif but, until recently, only those from the Ashgill Fosses Formation (Condroz Inlier) have been properly taxonomically studied (Sheehan 1987). In the Early Ordovician, Belgium was located in high southern latitudes (it was part of Avalonia, a terrane with a Gondwanan origin), offshore from high latitude Gondwana (Amazonia–North-West Africa). During the Ordovician, Avalonia rifted from Gondwana and drifted northward, eventually docking Baltica in the Katian forming a block that collided with Laurentia in the Silurian and closing the Iapetus Ocean. The ongoing revision of the historical collections of the Royal Belgian Institute of Natural Sciences, complemented with newly collected specimens, has enables us to document the development of brachiopod faunas in this part of Avalonia from the Tremadocian. Early and Middle Ordovician brachiopod faunas are characterized by poor preservation leading to tentative identifications, low diversity and low to medium abundance assemblages, dominated by linguliformean taxa (Candela et al. 2021; Candela & Mottequin 2022, in press), from assemblages rooted in the Furongian (Popov et al. 2013). Middle to Late Ordovician brachiopod assemblages (e.g., Oxhe and Fosses formations) are characterized by a distinct shift towards rhynchonelliformean-dominated faunas that show stronger affinities with palaeo-equatorial faunas (Laurentia, Baltica), than with Early Ordovician peri-Gondwanan and Gondwanan faunas.
Event title
4th International Congres of Stratigraphy
Publisher
International Congres on Stratigraphy
Official URL
https://strati2023.sciencesconf.org/464561/document
Related URL
https://www.nms.ac.uk/collections-research/collections-departments/natural-sciences/meet-the-team/dr-yves-candela/
Rights statement
In Copyright
Keywords
Ordovician
Belgium
Avalonia
brachiopods
Additional information
Full text of abstract available via the official URL
Managed by the British Library and supported by the AHRC

Built with DSpace-CRIS software - Extension maintained and optimized by 4Science

  • Cookie settings
  • End User Agreement
  • About
  • Contact
  • Help
Repository logo COAR Notify