Impacts of resource fluctuations and recurrent tsunamis on the occupational history of Čḯxwicən, a Salishan village on the southern shore of the Strait of Juan de Fuca, Washington State, U.S.A. (February 2019)

• Record Type: Journal Article
• Authors: Hutchinson, Ian; Butler, Virginia L.; Campbell, Sarah K.; Sterling, Sarah L.; Etnier, Michael A.; Bovy, Kristine M.
• Is Part Of: Journal of archaeological science. Volume 23(2019)
• Page Start: 1131
• Page End: 1142
• Publication Date: 2019-02
• Subjects: Pacific Northwest -- Čḯxwicən -- Radiocarbon -- Palaeodemography -- Summed probability density function -- Null model -- Marine resources -- Herring -- Palaeoclimate -- Cascadia -- Earthquakes -- Tsunamis; Archaeology -- Periodicals; Archaeology -- Research -- Periodicals; 930.1
• DOI: 10.1016/j.jasrep.2018.04.001
• Languages: English
• ISSNs: 2352-409X

Abstract

Abstract: A summed probability density function (spdf), generated from the catalog of 101 radiocarbon ages on wood and charcoal from the Čḯx w icən archaeological site (Washington State, USA), serves as a proxy for the site's occupational history over the last 2500 years. Significant differences between spdfs derived from a null model of population growth (a bootstrapped logistic equation) and the observed index suggest relatively less cultural activity at Čḯx w icən between about 1950–1750 cal BP, 1150–950 cal BP, and 650 to 550 cal BP; and increased activity between about 1350–1250 cal BP and 550–500 cal BP. Peaks in the Čḯx w icən spdf are closely echoed by those derived from English Camp and Cama Beach, the other intensively dated archaeological sites in the region, from about 1600 to 650 cal BP. The fluctuations at all three sites in that period appear to be predominantly associated with the availability of marine resources, as shown by a statistically significant correlation between the Čḯx w icən spdf and the abundance of fish remains in late Holocene sediments in Saanich Inlet, a fjord on the southeast coast of Vancouver Island. A dramatic fall in the Čḯx w icən spdf after 1250 cal BP, and the presence of sandy deposits in the village midden may reflect the impact of a tsunami triggered by earthquake "U" at the neighboring Cascadia plate boundary. Other tsunamis from this source over the last 2500 years apparently had more modest effects on activity levels at Čḯx w icən. Highlights: A summed probability density function (spdf) encapsulates the occupational history of Čxwicn over the last 2500 years. The observed spdf differs significantly from spdfs derived from a bootstrapped model of logistic population growth. Two other well-dated sites in the region exhibit temporal patterns of occupation that are similar to that at Čḯx w icən. Fluctuations in the observed spdf are highly correlated with the abundance of fish bones in a local marine sediment core. A decline in activity at Čḯx w icən shortly after 1250 cal BP likely reflects the impact of a local tsunami.