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- W2008644805 abstract "The Devonian Tully clastic equivalents and associated rocks of east-central New York State were deposited in fluvial to offshore environments associated with the Catskill delta. These depositional environments have been well defined by Johnson and Johnson and Friedman. The compositional and textural immaturity of the sandstones (immature to submature graywacke) and nearly ubiquitous micro-cross-lamination indicate that rate of sediment supply exceeded rate of reworking. Four of the ichnofossils, including Arenicolites (“small form”), ?Teichichnus, Spirophyton, and large vertically oriented burrow-like structures of probable biological origin are found in narrow paleoenvironmental ranges, within alluvial, tidal, and nearshore facies. However, the other eleven trace fossils, including the most abundant types [Arenicolites (“large form”), arthropod traces (Diplichnites, Cruziana, ?Isopodichnus, Rusophycus), Bifungites, ?Chondrites, Skolithos (2 types), Zoophycos, large primarily intrastratally-produced burrows, and simple surficial trails ] occur in rocks deposited under diverse environmental conditions. Their distribution is not clearly related to environment or substrate texture. Factors contributing to the broad lateral distribution of most of the biogenic structures include: (1) the continual influx of sediment from the east, which may have excluded some forms and inhibited the development of stable, environmentally distinct ichnocoenoses, and (2) gradual changes in optimal behavioral patterns resulting from environmental transitions occurring over large geographic distances. The gradational nature of these changes may have exaggerated the broad environmental ranges of the trace-producing animals." @default.
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- W2008644805 date "1979-01-01" @default.
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- W2008644805 title "Paleoenvironmental distribution of trace fossils in the catskill deltaic complex, New York State" @default.
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- W2008644805 doi "https://doi.org/10.1016/0031-0182(79)90115-9" @default.
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