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Additional resources for Allotropy of Liquid Benzene

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Several species, including what is probably the youngest one, C. sp. aff. C. pompeckji (Madsen), occur in the northern Richardson Mountains, at localities in which their stratigraphic relations with other species cannot be determined in detail (Poulton, 1978). ) sp, in Bed I of the Salmon Cache Canyon section probably represents this interval, immediately below the Arctocephalites faunas which are the subject of this report. Extended discussion of the Cranocephalites faunas is beyond the scope of this report; further references to them are found in Meledina (1973) and Callomon (1975, 1985).

The subdivision of Cadoceras beds into only two zones (Meledina, 1977) suggests that they may be overly comprehensive. The assemblage of Cadoceras emilianzevi, C. subtenuicostatum, C. falsum (Meledina, 1977, p. 189, 190) and another associate C. , p. 192) is probably younger than those in the Salmon Cache Canyon section. , 1959). It is about the northeasternmost locality with Northwest European faunal character, narrowly separated from the Boreal areas by the Russian Platform. , 1959), indicating the correlation of the Boreal and Northwest European zones, in an area where they may intermix.

51; Meledina and Nal'nyaeva, 1972, p, 71) to characterize an interval between Arcticoceras :elow, and other Cadoceras species above. l, is therefore diminished and certainly these microconchs no longer are considered to ce reliable indicators of Callovian age. ~ rctocephntttes faunas discussed elsewhere in this report. _,eages is supported by the present study (Table 3). :odyense/henryi The general similarity of the Eurycephalites faunas .. '.. crassicostatum and X. saypoensis, which may be the -icroconch dimorph of the Western North American SJbfamily Eurycephalitinae.

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Allotropy of Liquid Benzene by Menzies A.W.C., Lacoss D.A.

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