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In the Moscow basin both Ammonites of Virgatus-group and Aucellas are found, the rock being mainly of clayey material, such as would accumulate at a depth intermediate between that of the Greenland and Danish boulder-type. Much more evidence is needed before we have sufficient data to formulate a theory on this point. A quite different circumstance to be noted in connection with the East Greenland beds is that we have at present no evidence in this area of the existence of any deposits which wo...uld bridge over the gap between Callovian and Portlandian. They may still be discovered, but if we realise how near the coast-line must have been and the shallow nature of the deposits, it will not seem unlikely that some comparatively slight displacement may have converted the region into land for that space of time. The work that I have been doing now in translating Dr. Madsen's paper has recalled to my mind, over and over again, the time I spent in working out the Danish Jurassic boulders. Most of the conclusions I came to then, especially with regard to the Portlandian boulders, which interested me most, were em- bodied in the paper* published at the time, but a few have crystallised out since.
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