Stratigraphy, paleomagnetism, and cosmogenic-isotope burial ages of fossil-bearing strata within Riverbluff Cave, Greene County, Missouri.

Riverbluff Cave, in Greene County, Missouri, is a short single passage between the James River and its direct tributary, Ward Branch. Before stream incision the cave functioned as a spillway/piracy between the two streams during high-discharge events and accumulated a sequence of stratified fluvial...

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Publicado en:Quaternary Research Vol. 87; no. 3; pp. 516 - 529
Autores principales: Rovey, Charles W., Balco, Greg, Forir, Matt, Kean, William F.
Formato: Artículo
Publicado: Cambridge University Press May2017
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Acceso en línea:Ver este registro en EBSCOhost
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        atl: Stratigraphy, paleomagnetism, and cosmogenic-isotope burial ages of fossil-bearing strata within Riverbluff Cave, Greene County, Missouri.
      aug:
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          Rovey, Charles W.
          Balco, Greg
          Forir, Matt
          Kean, William F.
        affil:
          Department of Geography, Geology, and Planning, Missouri State University, 901 S. National, Springfield, Missouri 65897, USA
          Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, California 94709, USA
          Missouri Institute of Natural Science, 2327 W. Farm Road 190, Springfield, Missouri 65810, USA
          Department of Geosciences, University of Wisconsin-Milwaukee, P.O. Box 413, Milwaukee, Wisconsin 53201, USA
      su:
        Stratigraphic geology
        Paleomagnetism
        Cosmogenic nuclides
        Caves
        Sediment transport
        Missouri
      sug:
        subj:
          Missouri
          Stratigraphic geology
          Paleomagnetism
          Cosmogenic nuclides
          Caves
          Sediment transport
      keyword:
        Burial dating
        Mammoths
        Riverbluff Cave
      ab: Riverbluff Cave, in Greene County, Missouri, is a short single passage between the James River and its direct tributary, Ward Branch. Before stream incision the cave functioned as a spillway/piracy between the two streams during high-discharge events and accumulated a sequence of stratified fluvial sediments within the cave. Five cosmogenic-nuclide burial ages for these sediments range from 0.984 to 0.570 Ma. These ages are consistent with both the stratigraphic order of the samples and the inferred position of the Matuyama/Brunhes paleomagnetic boundary. These ages indicate that sandy channel-facies deposits derived from Ward Branch entrances began to accumulate within the cave as early as 0.984±0.065 Ma. This facies is capped by highly fossiliferous gravel beds dated at 0.658±0.065 Ma, which contain abundant mammoth bones (possibly <italic>Mammuthus trogontherii</italic>) and other vertebrates. The high concentration implies that this deposit may record some type of mass-mortality event. By 0.570±0.072 Ma, all Ward Branch entrances had been abandoned because of incision, and a laminated red clay derived from backflow from flooding along the James River capped the older channel sediments.
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    language: English
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