Excerpt from Proceedings and Transactions of the Nova Scotian Institute of Natural Science, Vol. 6: For 1883, 1884, 1885, 1886
There is, therefore, reason to suppose that the Hartley speci mens and our nullipore are analogous, as both have concretionary lamellar structure and attached spirorbes, and that the carboni ferous concretionary limestone is coralline or nullipore in origin.
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Quantità: 15 disponibili