Filtering appendices on the branchial arches of Coelacanthus lepturns Agassiz

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Abstract
Recently, in describing the fauna of the passage-beds between the Dinantian and the Namurian, I pointed out, for the first time, the presence of some Conodonts1 in the Carboniferous of Belgium. Since the discovery of this first series of specimens, I have picked up several hundred Conodonts in various localities, included either in the passage-beds, or in the lower levels of the Namurian. It is to be expected that other localities may shortly be discovered.

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