Page 68 - Carbonate Facies in Geologic History
P. 68

Use of Cycles in Chronostratigraphic Correlation                   55

                  It is  obvious that such chronostratigraphic correlation is essentially intraba-
               sinal, although certain thin, lithic units have been carried great distances across
               several tectonic provinces (see Wanless, 1972, on coals).
                  Arguments for the time stratigraphic use of these  cycle  boundaries and thin
               markers are mainly deductive and they should be tested wherever possible against
               as much detailed paleontology as is available. Shaw's system (1964)  of statistical
               treatment of sequence of faunal zones, related to a composite standard, offers  a
               hope of providing the kind of paleontology zonation needed for  this.  However,
               the requisite biostratigraphic detail with which to check our cyclic correlations is
               generally missing. For example: The Late Devonian beds  of the Williston Basin
               contain perhaps between 25-30 cycles, unusually regular and widespread. At best,
               our paleontologic zonation provides only a half dozen zones, whether based on
               goniatites, conodonts, or brachiopods, for these Frasnian and Fammenian beds
               (estimated time,  15-20 million years).  The same duration can  be  estimated for
               Late  Paleozoic  cycles  in  New  Mexico.  The  Late  Pennsylvanian  and  lowest
               Permian  of the  Sacramento Mountains, (narrow  east  shelf  of the  Oro  Grande
               basin) consist of approximately 50 cycles through beds in which the best fusulinid
               experts can at present find  only about 5 or 6 subdivisions of the zones  Triticites
               and  Schwagerina.  Time  involved  in  this  case  must  be  about  15  million  years.
               Estimated times  (Duff et aI.,  1967,  p.246) for  Late Paleozoic  cyclothems  range
               from 30000 to 300000 years each. Fischer (1964) and Zankl (1971) stated that the
               duration of the  300  Triassic Dachstein cyclothems  was  from  20000  to  100000
               years each, deposited within a period of 15 million years.
                  Therefore,  whereas  at  present  the  most  detailed  correlatable  paleontologic
               zones embrace about one to two million years or so (Hay, 1972), the sedimentary
               cycles discussed above were probably deposited in as little as 1/10 to 1/20 of this
               time!
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