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- W1489415468 abstract "We appreciate Khomentovsky's review of his views on Cambriancorrelations across the Siberian Platform but do not find his argumentscompelling. Indeed, his Comment emphasizes the need for correlationaltools beyond those offered by small shelly fossils (SSFs). In Siberia, therecord of Nemakit-Daldynian and SSP's is largely cumulative,with interpreted zonal boundaries based on first appearances rather than extinctions.In consequence, published zonal schemes are relatively insensitiveto hiatuses within sections. They are sensitive to the environmental andtaphonomic factors that govern local stratigraphic ranges of SSP taxa, andthat is one reason why the three principal groups of Russian stratigraphersworking on Proterozoic-Cambrian beds differ on intraplatform correlations(Khomentovsky and Karlova, 1993; Repina and Rozanov, 1992; Missarzhevsky,1989). A second reason for the discrepancy is a misapprehension,repeated here by Khomentovsky, that stage boundaries are defined bya particular set of fossils rather than a boundary point in a stratotype section.We did not choose any subset of basal Tommotian SSFs as diagnostic forthe initial stage boundary; we noted only that all principal taxa of the N. sunnaginicuszone were present when the first rocks above the boundary pointaccumulated in the stratotype region." @default.
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- W1489415468 date "1996-09-01" @default.
- W1489415468 modified "2023-09-23" @default.
- W1489415468 title "Sizing up the sub-Tommotian unconformity in Siberia: Reply" @default.
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