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  • Online Resource  (3)
  • Frison, George C.  (3)
  • 1
    In: Geoarchaeology, Wiley, Vol. 20, No. 6 ( 2005-08), p. 627-649
    Abstract: Shallowly buried archaeological sites are particularly susceptible to surface and subsurface disturbance processes. Yet, because cultural deposition often operates on short time scales relative to geologic deposition, vertical artifact distributions can be used to clarify questions of site formation. In particular, patterns in artifact distributions that cannot be explained by occupation histories must be explained by natural processes that have affected sites. Buried only 10–50 cm beneath the ground surface for 10,450 14 C yr, the Folsom component at Barger Gulch Locality B (Middle Park, Colorado) exhibits many signs of post‐depositional disturbance. Through examination of variation in the vertical distribution of the artifact assemblage, we are able to establish that only a Folsom component is present. Using vertical artifact distributions, stratigraphy, and radiocarbon dating, we are able to reconstruct the series of events that have impacted the site. The Folsom occupation (˜10,450 14 C yr B.P.) was likely initially buried in a late‐Pleistocene eolian silt loam. Erosion brought the artifacts to rest on a deflation surface at some time prior to 9400 14 C yr B.P. A mollic epipedon formed in sediments that accumulated between 9400 and 7000 14 C yr B.P. Some time after 5200 14 C yr B.P., this soil was partially truncated, and artifacts that had previously dispersed upward created a secondary lag at its upper contact. This surface was buried again and artifact dispersal continued. © 2005 Wiley Periodicals, Inc.
    Type of Medium: Online Resource
    ISSN: 0883-6353 , 1520-6548
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2005
    detail.hit.zdb_id: 1479950-9
    SSG: 6,14
    SSG: 13
    Location Call Number Limitation Availability
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  • 2
    In: Geoarchaeology, Wiley, Vol. 20, No. 6 ( 2005-08), p. 599-625
    Abstract: Middle Park, a high‐altitude basin in the Southern Rocky Mountains of north‐central Colorado, contains at least 59 known Paleoindian localities. At Barger Gulch Locality B, an extensive Folsom assemblage (˜10,500 14 C yr B.P.) occurs within a buried soil. Radiocarbon ages of charcoal and soil organic matter, as well as stratigraphic positions of artifacts, indicate the soil is a composite of a truncated, latest‐Pleistocene soil and a younger mollic epipedon formed between ˜6000 and 5200 14 C yr B.P. and partially welded onto the older soil following erosion and truncation. Radiocarbon ages from an alluvial terrace adjacent to the excavation area indicate that erosion followed by aggradation occurred between ˜10,200 and 9700 14 C yr B.P., and that the erosion is likely related to truncation of the latest‐Pleistocene soil. Erosion along the main axis of Barger Gulch occurring between ˜10,000 and 9700 14 C yr B.P. was followed by rapid aggradation between ˜9700 and 9550 14 C yr B.P., which, along with the erosion at Locality B, coincides with the abrupt onset of monsoonal precipitation following cooling in the region ˜11,000–10,000 14 C yr B.P. during the Younger Dryas oscillation. Buried soils dated between ˜9500 and 8000 14 C yr B.P. indicate relative landscape stability and soil formation throughout Middle Park. Morphological characteristics displayed by early Holocene soils suggest pedogenesis under parkland vegetation in areas currently characterized by sagebrush steppe. The expansion of forest cover into lower elevations during the early Holocene may have resulted in lower productivity in regards to mammalian fauna, and may partly explain the abundance of early Paleoindian sites (˜11,000–10,000 14 C yr B.P., 76%) relative to late Paleoindian sites (˜10,000–8000 14 C yr B.P., 24%) documented in Middle Park. © 2005 Wiley Periodicals, Inc.
    Type of Medium: Online Resource
    ISSN: 0883-6353 , 1520-6548
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2005
    detail.hit.zdb_id: 1479950-9
    SSG: 6,14
    SSG: 13
    Location Call Number Limitation Availability
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  • 3
    In: American Antiquity, Cambridge University Press (CUP), Vol. 85, No. 3 ( 2020-07), p. 554-572
    Abstract: Los arqueólogos han sometido durante mucho tiempo a los sitios de caza y destazamiento de megafauna de Clovis al más alto nivel de escrutinio. En 1987, se encontró un mamut colombino ( Mammuthus columbi ) en asociación espacial con un pequeño conjunto de artefactos en el condado de Converse, Wyoming. Sin embargo, debido al pequeño conjunto de herramientas,la naturaleza limitada de las excavaciones y a las preguntas sobre la seguridad de la asociación entre los artefactos y los restos de mamuts, el sitio nunca se incluyó en los resúmenes de los sitios de caza y destazamiento de megafauna de Norteamérica. Aquí presentamos los resultados de cuatro temporadas de campo de nuevas excavaciones en el sitio La Prele Mammoth que confirman la presencia de una ocupación cultural asociada y basada en el contexto geológico, atributos de artefactos, distribuciones espaciales, análisis de residuos de proteínas y análisis microscópico de huellas de uso lítico. Este nuevo trabajo identificó una ocupación cultural más extensa que incluye la presencia de múltiples grupos de artefactos discretos en una proximidad espacial cercana a la cama de huesos de mamut. Este estudio confirma la presencia del segundo sitio de caza y destazamiento de mamuts de Clovis en Wyoming y muestra el valor de retornar a sitios de caza y destazamiento propuestos del Pleistoceno Terminal.
    Type of Medium: Online Resource
    ISSN: 0002-7316 , 2325-5064
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2020
    detail.hit.zdb_id: 2050689-2
    SSG: 7,26
    SSG: 6,14
    SSG: 6,33
    SSG: 6,11
    Location Call Number Limitation Availability
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