Maya Marine Subsistence: Isotopic Evidence from Marco Gonzalez and San Pedro, Belize

2009 ◽  
Vol 20 (1) ◽  
pp. 37-56 ◽  
Author(s):  
Jocelyn S. Williams ◽  
Christine D. White ◽  
Fred J. Longstaffe

AbstractThis article presents stable nitrogen and carbon isotopie analyses of diet at the Maya sites of Marco Gonzalez and San Pedro, Belize. This study, which provides important insight into social organization, trade, and subsistence economy for the Postclassic and Historic periods (ca. A.D. 900–1650), also expands our understanding of the distribution of stable carbon and nitrogen isotopes within coral reef food webs off coastal Belize. Marco Gonzalez and San Pedro represent the first documented ancient Maya populations whose diet consisted mostly of marine resources with a minimal reliance upon maize. Although these sites do not appear highly stratified, and there are no dietary differences between sexes or status, the inhabitants of Marco Gonzalez incorporated more mainland-terrestrial animals and maize into their diet than the people of San Pedro. This finding supports the postulated roles of these two settlements, where Marco Gonzalez had trade ties to the mainland site of Lamanai and San Pedro was a small fishing village.

1988 ◽  
Vol 53 (2) ◽  
pp. 320-336 ◽  
Author(s):  
William F. Keegan ◽  
Michael J. DeNiro

Previous studies have demonstrated that stable carbon- and nitrogen-isotope ratios of bone collagen can be used to distinguish marine and terrestrial components of prehistoric human diet. However, when this method was first applied to prehistoric Bahamians, their bone-collagen nitrogen-isotope ratios were found to be outside the ranges observed for other coastal populations that ate substantial quantities of marine foods. This study examines in detail the distributions of stable carbon and nitrogen isotopes in Bahamian food chains. Our results indicate that the unique isotopic signature in bone collagen of prehistoric Bahamians reflects the enrichment of 13C and the depletion of 15N in seagrass and coral-reef communities relative to other oceanic environments. The results also demonstrate that bone-collagen 13C/12C ratios can be used to distinguish marine from terrestrial contributions in the prehistoric Lucayan Taino diet, and that 15N/14N ratios serve to identify the use of certain marine food groups. This approach should prove useful for the study of consumption practices in other tropical coral-reef environments and as a method for evaluating theoretically predicted optimal diets.


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