The Geology of Minnesota volume 31

Cover The Geology of Minnesota volume 31
The Geology of Minnesota volume 31
Geological And Natural History Survey of Minnesota
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They also resemble, perhaps even more, the trifid surface spicules ("Gabel-Anker'') of many lithistid sponges. The horizontal rays in the latter often are bifurcate close to the centre, so that even the duplex character of these rays in Anomalospongia is in a measure simulated. (See fig. \b and c. ) I am not prepared to decide definitely that these resemblances are or are not indica- tive of I'elationship. It seemed desirable, however, to mention the facts, since they illustrate the sense of th...e preceding paragraph.
As already indicated, it is my belief that the uncertain Amphispongia is related to A nomalospongia indeed, that the two might well be united in one family. That genus was proposed by Salter* for certain free, compressed, elongate-elliptical masses, rounded at both ends, and rarely more than 50 mm. Long by 18 mm. Wide, which *Mem. Gcol. Sur. Gt, Britain. 32. Scotland, p. 135, 1S61.
74 THE PALEONTOLOGY OF MINNESOTA.
LAnomalospongla occur in Silurian strata near Edinburg, Scotland.


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