The correlative significance of the Chitinozoa-bearing horizon in the Caradocian profiles of the Łeba region (NW Poland)

Teresa Podhalańska

Abstract


A rich Chitinozoa assemblage has been observed in five boreholes of the Łeba Elevation region (NW Poland) within the black mudstones bearing Lower Caradocian graptolites. These microfossils occur in a horizon of rather small thickness which, in a regional scale, may be . regarded as a correlative horizon within the monotonous deposits of the graptolite facies.


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