SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 13 May 2009
Published in Soil Sci Soc Am J 73:1209-1220 (2009)
DOI: 10.2136/sssaj2008.0262
© 2009 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Google Scholar
Right arrow Articles by Sweetwood, R. V.
Right arrow Articles by Hixson, D.
PubMed
Right arrow Articles by Sweetwood, R. V.
Right arrow Articles by Hixson, D.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Sweetwood, R. V.
Right arrow Articles by Hixson, D.
Related Collections
Right arrow Soil History
Right arrow Soil Organic Matter
Right arrow Soil Geomorphology and Geography

PEDOLOGY

The Maya Footprint: Soil Resources of Chunchucmil, Yucatán, Mexico

Ryan V. Sweetwooda, Richard E. Terrya,*, Timothy Beachb, Bruce H. Dahlinc and David Hixsond

a Plant and Wildlife Sciences, Brigham Young Univ., Provo, UT 84062
b School of Foreign Service, 37th and O Streets, NW, Georgetown Univ., Washington, DC 20057
c Center for Environmental Studies, Shepherd Univ., Shepherdstown, WV 25443
d Dep. of Anthropology, Tulane Univ., New Orleans, LA 70118

* Corresponding author (richard_terry{at}byu.edu).

This study explored and characterized soil physical and chemical properties to determine how the ancient Maya of Chunchucmil, Yucatán, Mexico, fed themselves. Our objectives were to examine the soil resources and the areas of agricultural importance surrounding Chunchucmil and to search for evidence of agricultural intensification of soils by night soil and charcoal amendments. The C isotopic signature of ancient C4 crops was not detected, suggesting that either maize (Zea mays L.) was not extensively produced or that the mix of native C3 and C4 plants in the savanna hid the signature. There were no soil chemical or biomarker evidences of ancient agricultural intensification, suggesting that ancient agriculture was mainly based on shifting cultivation and arboriculture at Chunchucmil. Concentrations of black carbon, Ca, P, K, Mg, and organic C within urban and rural settlements were enhanced, but probably by incidental human activities. We estimate that the land requirement to sustain the population of Chunchucmil at its height would have been greater than the available resources based on traditional agricultural methods. We cannot ignore the possibilities of intensification techniques, like intensive weeding, watering, and organic fertilizers that would have left no or only modestly elevated major elements. But it is probable that the ancient Maya of Chunchucmil traded marine and estuary products from the Gulf Coast and other high-value trade items for imported agricultural products.

Abbreviations: AIRSAR, airborne synthetic aperture radar • BC, black carbon • EC, electrical conductivity • PREP, Pakbeh Regional Economy Program • SOM, soil organic matter







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2009 by the Soil Science Society of America.