Paleoenvironment and Human Occupation in the Maya Lowlands of the Usumacinta River, Southern Mexico. Issue 3 (5th April 2013)

• Record Type: Journal Article
• Authors: Solís‐Castillo, Berenice; Solleiro‐Rebolledo, Elizabeth; Sedov, Sergey; Liendo, Rodrigo; Ortiz‐Pérez, Mario; López‐Rivera, Sara; McNamee, Calla; Cyr, Howard; Wilson, Lucy
• Is Part Of: Geoarchaeology. Volume 28:Issue 3(2013:May/Jun.)
• Page Start: 268
• Page End: 288
• Publication Date: 2013-04-05
• Subjects: Archaeological geology -- Periodicals; 930.1028
• DOI: 10.1002/gea.21438
• Languages: English
• ISSNs: 0883-6353

Abstract

<abstract abstract-type="main"> <title> <x xml:space="preserve">Abstract</x> </title> <p>Paleosol sequences along the lowest terraces of the Usumacinta River in southern Mexico were used to reconstruct Holocene environmental changes and examine human–environmental interactions. Study sections were correlated through paleosol morphology, radiocarbon dating, and artifact seriation of Formative, Classic, and Postclassic ceramics. The oldest paleosols have gleyic features. Although they contain hard carbonate concretions dating to 5450–5380 cal. yr B.P., these Gleysols formed in the Late Pleistocene to Early Holocene. Carbonates were deposited later. The uppermost paleosols lack gleyic features, the oldest of which contains vertic features, dating to 2000–2700 cal. yr B.P., and contains abundant Formative period ceramics. The upper two paleosols are morphologically less developed and are strongly affected by human activities; radiocarbon ages and ceramic assemblages indicate that they belong to the Maya Classic and Postclassic periods. Stable carbon isotope values from the decalcified organic matter vary among paleosols of different ages and sites. δ<sup>13</sup>C values are highest (−16 to −20‰) in the Formative period paleosol. Although it is possible that maize cultivation could contribute to the isotopic signatures, we believe that the δ<sup>13</sup>C values indicate the dominance of drought‐resistant C4 and CAM vegetation due to their association with vertic soils. The Classic period paleosol has a slightly lower isotopic value (−20 to −22‰), while the Postclassic paleosol shows the lowest values (−22 to −23‰), suggesting reforestation of the floodplain. These results indicate that the Early Holocene paleosols formed in a humid climate similar to that of today, which transitions toward dryer conditions around 5500 cal. yr B.P. In the Late Holocene (approximately 3000 B.P.) an increase in seasonality occurs. This condition favored the formation of Vertisols, suitable for agriculture.</p> </abstract>