2018
DOI: 10.1017/rdc.2018.2
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Holocene Human Occupation of the Central Alaska Peninsula

Abstract: The Alaska Peninsula is a landscape defined by volcanic, tectonic, and glacial processes, and life throughout is conditioned on the interactions among them. During the middle Holocene (ca. 4100–3600 yr ago), intense caldera-forming eruptions of the Aniakchak and Veniaminof volcanoes changed the shape of the central portion of the Peninsula dramatically, and had significant and perhaps devastating impacts on both terrestrial and marine biota. Here we evaluate the severity of these impacts by tracking human sett… Show more

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Cited by 9 publications
(5 citation statements)
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“…Similarly, our goal is to understand the occupation on the Four Mountains within the context of the geologic events (volcanic eruptions and tsunamis), long-term ecosystem and climate fluctuations, and prehistoric subsistence strategies to look at how the IFM shaped resilience and vulnerability. Similar to the research by Barton et al (2018) in the central Alaska Peninsula, in this article, we focus on the occupation history evidenced by the stratigraphic and radiocarbon evidence to understand human resilience or vulnerability through time in the IFM in the face of volcanic eruptions (Okuno et al, 2017), site formation processes (Persico et al, 2018), climatic changes (research which is ongoing, but see Savinetsky et al [2010]), and tsunamis (see Griswold et al, 2018), among other environmental/human relationships.…”
Section: Introductionsupporting
confidence: 83%
See 1 more Smart Citation
“…Similarly, our goal is to understand the occupation on the Four Mountains within the context of the geologic events (volcanic eruptions and tsunamis), long-term ecosystem and climate fluctuations, and prehistoric subsistence strategies to look at how the IFM shaped resilience and vulnerability. Similar to the research by Barton et al (2018) in the central Alaska Peninsula, in this article, we focus on the occupation history evidenced by the stratigraphic and radiocarbon evidence to understand human resilience or vulnerability through time in the IFM in the face of volcanic eruptions (Okuno et al, 2017), site formation processes (Persico et al, 2018), climatic changes (research which is ongoing, but see Savinetsky et al [2010]), and tsunamis (see Griswold et al, 2018), among other environmental/human relationships.…”
Section: Introductionsupporting
confidence: 83%
“…The archaeological record of the IFM reveals the sustainability and resilience of the Unangax̂ people to environmental change during the four millennia prior to the arrival of Russians into the Aleutian chain. Tsunamis, earthquakes, and volcanic eruptions are known to affect other archaeological sites (see VanderHoek and Myron, 2004; Losey, 2005; Ludwin et al, 2005, 2007; Barton et al, 2018). We find no evidence that paleotsunamis affected either the Tana Aguna or the Ulyagan village in prehistory, and perhaps their location atop a cliff of unconsolidated sediment buffered villages from unusual waves.…”
Section: Discussionmentioning
confidence: 99%
“…Despite widespread interest and an extensive body of literature and observations on the subject, biologists and paleoecologists continue to discuss when salmon runs in this and other areas became stable and predictable (Barton et al, 2018; Finney et al, 2000; Finney et al, 2002; Finney et al, 2010; Gregory‐Eaves et al, 2003; Gregory‐Eaves et al, 2009; Milner et al, 2000; Milner & Bailey, 1989; Rogers et al, 2013). Archaeological data have contributed to understanding this development in Pacific Northwest salmon, providing a clear “no later than date” on the basis of when and where people first turned their attention to salmon.…”
Section: Archaeological Evidencementioning
confidence: 99%
“…The Sugpiaq (traditional Yupik name for the Alutiiq people indigenous to the Alaska Peninsula) likely began settling the Meshik River area around 1700 cal. YBP (Barton, Shirar, and Jordan, 2018). Migration to the Alaska Peninsula began thousands of years earlier, but geologic changes such as volcanic eruptions and sea-level change either delayed the occupation of the Meshik River drainage or buried evidence (Barton, Shirar, and Jordan, 2018).…”
Section: Introductionmentioning
confidence: 99%
“…YBP (Barton, Shirar, and Jordan, 2018). Migration to the Alaska Peninsula began thousands of years earlier, but geologic changes such as volcanic eruptions and sea-level change either delayed the occupation of the Meshik River drainage or buried evidence (Barton, Shirar, and Jordan, 2018). Because of the Aniakchak II eruption and the time required for terrestrial ecological recovery, the Sugpiaq harvested marine and nearshore resources and lived in semipermanent settlements near the coast (Barton, Shirar, and Jordan, 2018; Morseth, 2003).…”
Section: Introductionmentioning
confidence: 99%