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Identification of Maize Pollen: Reply to Eubanks

Published online by Cambridge University Press:  20 January 2017

Miriam L. Fearn
Affiliation:
Department of Geology and Geography, University of South Alabama, Mobile, AL 36688
Kam-Biu Liu
Affiliation:
Department of Geography and Anthropology, Louisiana State University, Baton Rouge, LA 70803

Abstract

Eubanks bases her identification of the fossil pollen grain from Alabama as Tripsacum primarily on her calculated spinule density. To make those calculations, she used only our published photograph, and she assumed a grain expansion of 35 percent. She ignores the fact that the spinule density of the fossil pollen grain is actually the same as that of similarly treated Zea mays pollen. While there is always the possibility of a misidentification or of long-distance transport, the most likely interpretation remains that the 3500 B.P. pollen grain is Zea mays and that it represents limited cultivation of ancient corn in southern Alabama.

Eubanks identifica el grano fosilifero de polen de Alabama como Tripsacum principalmente en base a cálcules de la densidad de espinas. Ella realizeó los cálcules unicamente en base a nuestra fotografia publicada presumiendo una expansión de 35 por ciento. No tiene en cuenta que la densidad de espinas en el grano fosilifero de polen es en realidad igual al polen de Zea mays sujeto al mismo tratamiento. No se pueden descartar las posibilidades de identificación equivocada о el deplazamiento de larga distancia pero la interpretaciín más probable es que el grano de polen de 3500 B. P. es Zea mays y que revela el cultivo limitado del maíz antiguo en el sur de Alabama.

Type
Comments
Copyright
Copyright © Society for American Archaeology 1997

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References

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