III.—Notes on the Faunal Succession in the Carboniferous Limestone of Westmoreland and Neighbouring Portions of Lancashire and Yorkshire

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Abstract
In August last, at the meeting of the British Association at York, I gave a general account of the zonal succession of the Carboniferous Limestone as developed in Westmoreland and North Lancashire, and I instituted a comparison with beds of a similar age in the Ingleborough and North Pennine districts.

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