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The Black Forest (southwestern Germany) comprises two phyllite-bearing low-grade metasedimentary units, which are separated by the Central Schwarzwald Gneiss Complex. Both zones have been subjected to palynological investigation. In the north, the phyllites of the zone of Baden-Baden-Gaggenau, until now believed to be unfossiliferous, yielded a poorly preserved acritarch assemblage, indicating an...
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