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14C and Marine Reservoir Effect in Archaeological Samples from the Northeast Gulf of California

Published online by Cambridge University Press:  23 February 2016

David L Dettman ,
Douglas R Mitchell ,
Gary Huckleberry  and
Michael S Foster
David L Dettman
Affiliation:
Geosciences Department, University of Arizona, Gould-Simpson Building, Box 21077, Tucson, Arizona 85721, USA
Douglas R Mitchell
Affiliation:
Archaeological Consulting Services, Ltd., 424 W. Broadway Road, Tempe, Arizona 85282, USA
Gary Huckleberry
Affiliation:
Geoarchaeological Consultant, 3577 E. Nugget Canyon Place, Tucson, Arizona 85718, USA
Michael S Foster
Affiliation:
4505 E. Ute Street, Phoenix, Arizona 85044, USA
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Abstract

Previous studies of live-collected pre-weapons testing mollusk shells in the northern Gulf of California have demonstrated that the local radiocarbon reservoir effect (ΔR) is large and highly variable. To test the validity of this observation for paired charcoal and shell samples from archaeological contexts, we dated samples from four shell midden locations and six midden layers from the eastern shoreline of the Gulf of California near Puerto Peñasco, Sonora, Mexico. Dated charcoal samples were small twigs or brushy plants used to cook shellfish and the shells dated within each midden showed signs of burning. Ages range from approximately 5700 to 1900 cal BP. The offset between the modeled marine 14C age for calibrated ages of the middens and measured shell 14C age (ΔR) averaged 425 yr with a standard deviation of 115 yr.

Type
Articles
Information
Radiocarbon , Volume 57 , Issue 5 , 2015 , pp. 785 - 793
Copyright
Copyright © 2015 The Arizona Board of Regents on behalf of the University of Arizona 

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References

Argote, ML, Amador, A, Lavín, MF, Hunter, JR. 1995. Tidal dissipation and stratification in the Gulf of California. Journal of Geophysical Research 100(C8):16,103–18.CrossRefGoogle Scholar
Ascough, P, Cook, GT, Dugmore, AJ. 2005. Methodological approaches to determining the marine radiocarbon reservoir effect. Progress in Physical Geography 29(4):532–47.Google Scholar
Bischoff, JL, Niemitz, JW. 1980. Bathymetric Maps of the Gulf of California. U.S. Geological Survey Miscellaneous Investigation Series. Map I-11244.Google Scholar
Bradley, RJ. 1999. Shell exchange within the Southwest. In: Schaafsma, CR, Riley, CL, editors. The Casas Grandes World. Salt Lake City: University of Utah Press. p 213–28.Google Scholar
Brusca, RC. 2004. The Gulf of California–an overview. In: Brusca, RC, Kimrey, E, Moore, W, editors. A Seashore Guide to the Northern Gulf of California. Tucson: Arizona-Sonora Desert Museum. p 1–24.Google Scholar
Davis, O, Cutler, AH, Meldahl, KH, Palacios-Fest, M, Schreiber, JF, Lock, BE, Williams, LJ, Lancaster, N, Shaw, CA, Sinitiere, SM. 1990. Quaternary and environmental geology of the northeastern Gulf of California. In: Gehrels, G, Spencer, JE, editors. Geologic Excursions through the Sonoran Desert Region, Arizona and Sonora. Tucson: Arizona Geological Survey Special Paper 7. p 136–54.Google Scholar
Dettman, DL, Flessa, KW, Roopnarine, PD, Schöne, BR, Goodwin, DH. 2004. The use of oxygen isotope variation in the shells of estuarine mollusks as a quantitative record of seasonal and annual Colorado River discharge. Geochimica et Cosmochimica Acta 68(6):1253–63.CrossRefGoogle Scholar
Douglas, R, Gonzalez-Yajimovich, O, Ledesma-Vazquez, J, Staines-Urias, F. 2007. Climate forcing, primary production and the distribution of Holocene biogenic sediments in the Gulf of California. Quaternary Science Reviews 26(1–2):115–29.Google Scholar
Ezcurra, E, Felger, RC, Russell, AD, Equihua, M. 1988. Freshwater islands in a desert sand sea: the hydrology, flora, and phytogeography of the Gran Desierto oases of northwestern Mexico. Desert Plants 9(2):35–44.Google Scholar
Foster, MS, Mitchell, DR, Huckleberry, G, Dettman, DL. 2008. Observations on the archaeology, paleoenvironment, and geomorphology of the Puerto Peñasco area of northern Sonora, Mexico. Kiva 73(3):263–90.Google Scholar
Foster, MS, Mitchell, DR, Huckleberry, G, Dettman, DL, Adams, KR. 2012. Archaic period shell middens, sea-level fluctuations, and seasonality: archaeology along the northern Gulf of California littoral, Sonora, Mexico. American Antiquity 77(4):756–72.Google Scholar
Geib, PR. 2008. Age discrepancies with the radiocarbon dating of sagebrush (Artemisia tridentata Nutt.). Radiocarbon 50(3):347–57.CrossRefGoogle Scholar
Gifford, EW. 1946. Archaeology in the Punta Peñasco Region, Sonora. American Antiquity 11(4):215–21.Google Scholar
Goodfriend, GA, Flessa, KW. 1997. Radiocarbon reservoir ages in the Gulf of California: roles of upwelling and flow from the Colorado River. Radiocarbon 39(2):139–48.Google Scholar
Grimstead, DN, Pailes, MC, Dungan, KA, Dettman, DL, Martínez Tagüeña, N, Clark, AE. 2013. Identifying the origin of southwestern shell: a geochemical application to Mogollon Rim archaeomolluscs. American Antiquity 78(4):640–61.Google Scholar
Haury, EW. 1976. The Hohokam, Desert Farmers and Craftsmen. Excavations at Snaketown 1964–1965. Tucson: University of Arizona Press.CrossRefGoogle Scholar
Kowalewski, M, Avila Serrano, GE, Flessa, KW, Goodfriend, GA. 2000. Dead delta's former productivity: two trillion shells at the mouth of the Colorado River. Geology 28(12):1059–62.2.0.CO;2>CrossRefGoogle Scholar
Meldahl, KH, Cutler, AH. 1992. Neotectonics and taphonomy: Pleistocene molluscan shell accumulations in the northern Gulf of California. Palaios 7(2):187–97.Google Scholar
Mitchell, DR, Foster, MS. 2000. Shell middens along the Sea of Cortez, Puerto Peñasco, Sonora, Mexico. Journal of Field Archaeology 27(1):27–41.Google Scholar
Mitchell, DR, Huckleberry, G, Rowell, K, Dettman, DL. 2015. Coastal adaptations during the Archaic Period in the northern Sea of Cortez, Mexico. Journal of Island & Coastal Archaeology 10(1):28–51.Google Scholar
Ortleib, L. 1991. Quaternary vertical movements along the coasts of Baja California and Sonora. In: Dauphin, JP, Simoneit, BRT, editors. The Gulf and Peninsular Province of the Californias. Tulsa: American Association of Petroleum Geologists Memoir 47. p 447–80.Google Scholar
Reimer, PJ, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Buck, CE, Cheng, H, Edwards, RL, Friedrich, M, Grootes, PM, Guilderson, TP, Haflidason, H, Hajdas, I, Hatté, C, Heaton, TJ, Hoffmann, DL, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, Manning, SW, Niu, M, Reimer, RW, Richards, DA, Scott, EM, Southon, JR, Staff, RA, Turney, CSM, van der Plicht, J. 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55(4):1869–87.Google Scholar
Russell, N, Cook, GT, Ascough, PL, Scott, EM, Dugmore, AJ. 2011. Examining the inherent variability in ΔR: new methods of presenting ΔR values and implications for MRE studies. Radiocarbon 53(2):277–88.Google Scholar
Stuiver, M, Braziunas, TF. 1993. Modeling atmospheric 14C influences and 14C ages of marine samples to 10,000 BC. Radiocarbon 35(1):137–89.Google Scholar
Thompson, RW. 1968. Tidal flat sedimentation on the Colorado River Delta, northwestern Gulf of California. Geological Society of America Memoirs 107:1–133.Google Scholar