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1990
At the Cenomanian/Turonian boundary in the Outer Carpathian basin the sedimentation of black and green Radiolarian shales was replaced by deposition of variegated shales reflecting a distinct change in sedimentary conditions from anaerobic to aeorobic. Sedimentation of the Turonian to Lower Senonian variegated shales preceded uplift of the intrabasinal
Ewa Malata, Nestor Oszczypko
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At the Cenomanian/Turonian boundary in the Outer Carpathian basin the sedimentation of black and green Radiolarian shales was replaced by deposition of variegated shales reflecting a distinct change in sedimentary conditions from anaerobic to aeorobic. Sedimentation of the Turonian to Lower Senonian variegated shales preceded uplift of the intrabasinal
Ewa Malata, Nestor Oszczypko
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Cretaceous Research, 1992
A relatively poorly diversified trace fossil assemblage from thin- and medium-bedded flysch of the Inoceramian beds in the Polish Outer Carpathians is dominated by postdepositional r-selected Chondrites, Planolites and Helminthoida. Predepositional K-selected forms are very rare.
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A relatively poorly diversified trace fossil assemblage from thin- and medium-bedded flysch of the Inoceramian beds in the Polish Outer Carpathians is dominated by postdepositional r-selected Chondrites, Planolites and Helminthoida. Predepositional K-selected forms are very rare.
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