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Palacios et al., 2009

Acritarchs from the MacLean Brook Formation, southeastern Cape Breton Island, Nova Scotia, Canada: New data on Middle Cambrian–Lower Furongian acritarch zonation

Palacios, T., Jensen, S., Barr, S. M., White, C. E.
DOI
DOI10.1016/j.palaeo.2008.12.006
Aasta2009
AjakiriPalaeogeography, Palaeoclimatology, Palaeoecology
Köide273
Number1-2
Leheküljed123-141
Tüüpartikkel ajakirjas
Keelinglise
Id48905

Abstrakt

We present here the results of a pilot study on Cambrian acritarchs from Cape Breton Island, Nova Scotia, based on a material from the MacLean Brook Formation in the Mira River Valley. An assemblage from the base of the formation contains 8 species including Eliasum llaniscumCristallinium dubium and Symplassosphaeridium cambriense, and correlates with a position close to the Paradoxides davidisP. forchhammeri Zone boundary. An assemblage from the upper part of the formation contains 16 species, of which 3 are new, including Cristallinium aciculatumPetaloferidium lacrimiferum n. sp., Pirea orbicularisStelliferidium pingiculumS. magnum n. sp., S. albanii n.sp, and Timofeevia microretis, correlated to the Olenus Zone. The upper assemblage is particularly noteworthy as it provides the first direct evidence for the Olenus Zone in the MacLean Brook Formation. Furthermore, it contains stratigraphically significant taxa known from sections on Baltica, and northern Gondwana but which have not been reported previously on Avalonia. The distinction between Stelliferidium and Timofeevia is discussed in part based on new data on Timofeevia lancarae from its type area in northern Spain. It is suggested that many reports of Furongian Timofeevia phosphoritica and T. lancarae are better referred to Stelliferidium.

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