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4S ULAF HOLTEDAHL. [sea ARCT. EXP. FHA)!
I tuel very much inrlineil to believe that these fossils were collected Iron) a locality very near to the place where the plzocuvfauna was ob- tuineil, since they have been mixed into one collection. Should this he rorreut. “e have here an indication (it relatively small thicknesses for the lower part ul the Devonian — with highest Silurian if we regard the [limou- tnnna ul Niagaran age— or perhaps fur a complete absence of several horizons [rum 3 rorrespumling period. In the Goose Fjord region, 3— 4000 feet at seililnenl, perhaps more, come between the base of the Series B and the high Devonian.
