• Stone and mammoth ivory tool production in Tanana Valley, Alaska

    From Primum Sapienti@invalide@invalid.invalid to sci.anthropology.paleo on Sun Dec 28 23:15:57 2025
    From Newsgroup: sci.anthropology.paleo


    https://www.sciencedirect.com/science/article/pii/S1040618225004306

    Stone and mammoth ivory tool production,
    circulation, and human dispersals in the
    middle Tanana Valley, Alaska: Implications
    for the Pleistocene peopling of the Americas

    Abstract
    In the middle Tanana Valley of central Alaska,
    the Holzman archaeological site is located
    along Shaw Creek's west bank. For the last
    three decades, the Tanana Valley has been the
    focus of intense Late Pleistocene archaeological
    and geological investigations into the
    interaction between the First Alaskans and Ice
    Age megafauna, particularly woolly mammoth.
    Archaeological excavations at the Holzman site
    have uncovered expedient tools on local quartz
    with well-preserved hearths, avifauna, and
    megafauna. Evidence for cooking and ivory tool
    manufacture dated to 14,000 years ago (14 ka)
    in component 5b (C5b) has been demonstrated rCo
    making Holzman among the earliest sites in the
    Americas. In the 13.7 ka C5a, an extensive
    workshop event left abundant local quartz
    artifacts behind, the by-product of mammoth
    ivory reduction and manufacture of ivory blanks
    or preforms, and the earliest known ivory rod
    tools in the Americas. The Holzman site
    contributes new information to a growing
    archaeological record of the middle Tanana
    Valley during the Late Glacial period. Based on
    current evidence, the confluence of Shaw Creek
    with the Tanana River was especially active
    during the initial arrival of Indigenous people.
    The subsequent selection of local quartz, cherts,
    and siltstone occurred with a particular focus on
    the harvest of woolly mammoth ivory. The evidence
    suggests a late southern migration by ancestral
    Clovis people south of the continental ice sheets
    into the mid-continental North America sometime
    between 14-13 ka.
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