Microfossils from the Liuchapo Formation: Possible oldest radiolarians from deep-water chert and phylogenetic analysis

Zhang, Yan; Feng, Qinglai; Nakamura, Yasuhide; Suzuki, Noritoshi

doi:10.1016/j.precamres.2021.106312

Cited by 9 publications

(1 citation statement)

References 67 publications

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“…Resolving the affinity of this taxon would require restudy of the type material and is beyond the scope of this study. Echidnina consists of tiny (210-300 µm diameter) globular spicular bodies (Bengtson, 1986) and is generally considered to be a radiolarian (e.g., Zhang et al, 2021). Thus, the family is primarily Devonian, with some examples from Ordovician and Carboniferous rocks.…”

Section: Systematic Palaeontologymentioning

confidence: 99%

Teganium (Porifera, Hexactinellida) from the Middle Ordovician Castle Bank fauna of Avalonia (Wales, UK)

Botting

Muir

2023

Palaeontol Electron

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The hexactinellid sponges Teganium and Teganiella are widespread in Ordovician, Devonian and Carboniferous strata in Laurentia, but have not previously been reported outside that palaeocontinent; some other members of the family Teganiidae are also restricted to Laurentia. The genus Teganiella in particular is considered to be a Laurentian endemic, with all species specialised for equatorial, shallow-water conditions. However, it is now clear that the diagnostic separation of Teganiella from Teganium was based on misunderstanding of the latter, and Teganiella should be considered a junior synonym. Based on this prior distribution, the discovery of two new species of Teganium (T. avalonensis sp. nov. and Teganium sp.) from the Middle Ordovician (Didymograptus murchisoni Biozone) of Castle Bank, Wales, is unexpected. These species are the oldest known and indicate diversification of the genus within a temperate microcontinent, prior to its appearance in Laurentia. The exceptional preservation of the new sponges also reveals detail of a complex body wall, supporting a more derived phylogenetic position within Hexactinellida (possibly affiliated to the Lyssacinosida) than previously recognised. The palaeobiogeography may suggest a relatively deep-water origin for the group (as for modern hexactinellids), which then became secondarily specialised for shallow-water environments within a Laurentian diversification.

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Section: Systematic Palaeontologymentioning

confidence: 99%