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The Initial Domestication of Cucurbita pepo in the Americas 10,000 Years Ago

Science
9 May 1997
Vol 276, Issue 5314
pp. 932-934

Abstract

Squash seeds, peduncles, and fruit rind fragments from Archaic period stratigraphic zones of Guilá Naquitz cave in Oaxaca, Mexico, are assigned to Cucurbita pepo on the basis of diagnostic morphological characters and identified as representing a domesticated plant on the basis of increased seed length and peduncle diameter, as well as changes in fruit shape and color, in comparison to wild Cucurbita gourds. Nine accelerator mass spectrometer radiocarbon dates on these specimens document the cultivation ofC. pepo by the inhabitants of Guilá Naquitz cave between 10,000 to 8000 calendar years ago (9000 to 7000 carbon-14 years before the present), which predates maize, beans, and other directly dated domesticates in the Americas by more than 4000 years.

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REFERENCES AND NOTES

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B. D. Smith, The Emergence of Agriculture (Scientific American Library, New York, 1995).
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P. K. Bretting, Ed., Econ. Bot. 44 (suppl.) (1990).
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B. D. Smith, Latin Am. Antiq., in press.
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D. S. Byers, Ed., The Prehistory of the Tehuacán Valley (Univ. of Texas Press, Austin, TX, 1967), vol. 1.
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K. V. Flannery, Ed., Guilá Naquitz (Academic Press, Orlando, FL, 1986).
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L. Kaplan, “Accelerator dates and the antiquity of Phaseolus,” paper presented at the annual meeting of the Society for Economic Botany, Miami, FL, 23 to 27 June 1993; “Phaseolus beans, accelerator dates in the Americas,” paper presented at the annual meeting of the Society for American Archaeology, Minneapolis, MN, 3 to 7 May 1995.
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T. Whitaker and H. Cutler, in (5), pp. 275–279.
10
The Guilá Naquitz cucurbit assemblage is now curated at the Laboratorio de Paleobotánica, Instituto Nacional de Antropologı́a e Historia (INAH), Mexico, Distrito Federal. The rind, seed, and peduncle specimens illustrated in the original analysis (9) are not present in the INAH collections. As a result, the rind and peduncle specimens illustrated in (9) are not included in this analysis. Seed measurements provided in (9), however, are included in Fig. 1.
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C. W. Cowan and B. D. Smith, J. Ethnobiol.13, 17 (1993).
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L. A. Newsom, S. D. Webb, J. S. Dunbar, ibid., p. 75.
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The as yet undated large peduncle from zone C (Fig. 1) may indicate an even earlier increase in fruit size, given that it is from the same provenience (E9) as the domesticated C. pepo seed that yielded an AMS radiocarbon date of 8910 14C years B.P. (Table 1 and Figs. 1 and 2C).
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D. Decker, Econ. Bot. 42, 4 (1988); D. Decker-Walters, T. W. Walters, C. W. Cowan, B. D. Smith, J. Ethnobiol. 13, 55 (1993).
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18
Figure 1 is by M. Bakry and Fig. 2 photographs are by C. Hansen. I thank INAH for permission to sample Guilá Naquitz specimens for AMS 14C dates; F. Sànchez, director of the Laboratorio de Paleobotánica, INAH, and J. L. Alvarado for their kind hospitality and their consultation on the analysis; J. L. Alvarado, D. Decker-Walters, K. Flannery, G. Fritz, L. Kaplan, L. Newsom, F. Sanchez, P. J. Watson, and M. Zeder for comments on the manuscript; and Y. Sugiura and C. Castillo, without whose assistance this research would not have been possible.

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Published In

Science
Volume 276 | Issue 5314
9 May 1997

Submission history

Received: 28 January 1997
Accepted: 4 March 1997
Published in print: 9 May 1997

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Authors

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Bruce D. Smith
Archaeobiology Program, Department of Anthropology, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560, USA.

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