In addition to research carried out on soils and sediments, there is a parallel field of research applying the same analytical techniques to the study of chemical residues in stuccoes. The most common material used to build floors in Mesoamerica after the Classic period was lime plaster. The study of residues in stuccoes becomes, therefore, a very promising study area. In last 25 years the Archaeological Prospection Laboratory at Mexico's National Autonomous University has developed a research strategy to study human activities based on ethnoarchaeological studies to interpret the distribution of chemical residues in archaeological floors. The most successful applications have been in lime-plastered surfaces; this article presents a brief review of these works. © 2007 Wiley Periodicals, Inc.
INTRODUCTIONThe application of chemical analysis to the study of archaeological floors is recent. It has been a consequence of the use of soil and sediment analysis in three different fields: agronomy, where chemical analysis is used to monitor plant health, fertility, and soil nutrients; geochemistry, where it is used as a mean to study geological evolution and locate mineral deposits of economic interest; and forensic science, where it is used to reconstruct crime scenes. Each of these fields followed a different path in developing these techniques. Arrhenius (1929) discovered the relationship between phosphate and archaeological remains while doing agronomic studies. From that moment on, geographers and archaeologists enthusiastically accepted the idea that phosphate was a good indicator of human settlement. As the history of phosphate analysis in archaeology shows (Mejía and Barba, 1988), it is no longer a mere adaptation of an agricultural technique but has become especially designed for field archaeology to demonstrate a close relationship to human activities. During its development, it has also served as an exploration tool, although this is not the field where its most promising applications are envisioned.Similarly, the chemical analysis of soils, sediments, and rocks has been used in geochemical prospection for the location, delimitation, and evaluation of ore deposits.