
doi: 10.1007/bf01820641
Archaeocythan limestones of the Lower Cambrian Nebida Fm. (SW-Sardinia) form bioherms (lower Nebida Fm. = Matoppa Mbr.) as well as biostromes (upper Nebida Fm. = Punta Manna Mbr.). In both cases algae are the main rock forming organisms; they act as sediment binding and sediment baffling organisms and thus are responsible for the growth of these carbonates.
550.geology, Article
550.geology, Article
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