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The trace fossil Gyrophyllites in deep-sea siliciclastic deposits of the Istebna Formation (Upper Cretaceous-Palaeocene) of the Carpathians : an example of biologically controlled distribution 119

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The trace fossil Gyrophyllites in deep-sea siliciclastic deposits of the Istebna Formation (Upper Cretaceous-Palaeocene) of the Carpathians : an example of biologically controlled distribution 0 1 5 1 1 1 1

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