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- W4315695929 abstract "The late Westphalian – early Stephanian macrotloras of the Dobrudzha Coalfield show many similarities with the contemporaneous lowland assemblages from southern Britain and the Canadian Maritimes, but there are also present some taxa normall y associated with more upland basins such as Saar-Lorraine and Central Bohemia. This is in agreement with the Dobrudzha Coalfield occupying a marginal position on the Variscan Foreland, perhaps at higher altitudes than the more western coalfields. It has been possible to identify the main biozonal boundaries that were originally established in western Europe and eastern North America. The base of the Laveineopteris rarinervis Subzone occurs at coal m5 in the Makedonka Formation. The base of the Linopteris bunburii Zone (indicating the base of the Westphalian D Stage) is at coal n3 in the Krupen Formation. The Lobatopteris micromiltoni Subzone seems to be absent due to a nonsequence, but the Dicksonites plueckenetii Subzone is in the Gurkovo Formation. Evidence of the Odontopteris cantabrica Zone (indicating the Westphalian – Stephanian boundary) occurs at coal p7 in the upper Gurkovo Formation." @default.
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- W4315695929 date "2004-06-30" @default.
- W4315695929 modified "2023-10-01" @default.
- W4315695929 title "Review of the late Westphalian - early Stephanian macrofloras of the Dobrudzha Coalfield, Bulgaria" @default.
- W4315695929 doi "https://doi.org/10.52321/geolbalc.34.1-2.11" @default.
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