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- W2340413612 abstract "Because it occurs below the classic fossiliferous Cambrian of Caborca, the largely dolomitic Gamuza Complex of the Caborca region has been considered axiomatically as Precambrian and this also after one of us (L.R.) demonstrated that said Cambrian belongs in an allochtonous series, a Nevada nappe. In conformity with that axiom of the Precambrian âge of the Gamuza Complex, some body fossils that cannot be assigned even to the highest taxa with certainty and some trace fossils of its Clemente Formation, as well as the stromatolites of its dolomitic Gamuza and Papalote Formations were assigned a Precambrian âge, and the former were considered as an Ediacara fauna. At Cerro Clemente, an outcrop of the Caborca Formation, which underlies the Clemente Formation, furnished us with silicified skeleton fossils (Tabulata : i.e. Coelenterata Anthozoa ? Stromatoporoids : Coelenterata Hydrozoa?). Although they are poorly preserved, it can be excluded that they are either Precambrian or Cambrian. They may be either Paleozoic or, and very much more probably, Mesozoic. However, within the regional framework, a Paleozoic âge of the Gamuza Complex can be excluded on geological ground. It follows, therefore, that they suggest a Mesozoic, and finally, once the geological context is taken into account, a Triassic âge for the Gamuza Complex. Thus, the Gamuza Complex might be one of the fragments or slivers of the Tethyan, Alpine Upper Triassic, often with a Dachstein facies, which occur in several places of the northwestern American Cordillera, from the latitude of Hermosillo (Sonora) to Alaska." @default.
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- W2340413612 date "1998-01-01" @default.
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- W2340413612 title "Discovery of Phanerozoic fossils in the Gamuza Complex of Caborca, Sonora, Mexico" @default.
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