Ancient Maya Secrets Unlocked

But the team also discovered evidence of erosion in upslope soils, suggesting that farming did spread to steeper, less suitable soils over time. And if Maya agriculture did cause substantial erosion, the soil loss could eventually have undercut the Maya’s ability to grow food, say the researchers.

The findings are just the latest example of how invisible artifacts in soil—something archeologists literally used to brush aside—can inform studies of past civilizations. That’s because artwork and buildings can crumble over time and jungles will eventually conceal ancient farm fields, but “the soil chemistry is still there,” Terry says.

He explains, for example, that most forest vegetation native to Tikal uses a photosynthetic pathway called C3, while maize uses a pathway called C4. The soil organic matter derived from these two pathways also differs, allowing researchers to make conclusions about the types of plants that were growing in the soils they test.

Thus, by analyzing soils in different areas of Tikal as well as looking at the layers that had formed in the soils, Terry and his collaborators were able to map the areas where ancient maize production occurred, including lowland “bajo” areas and possibly steeper slopes, as more food was needed.

Questions like this about past farming practices have always interested archeologists, Terry notes. But the tools of modern soil science are now enabling these scientists to ask increasingly sophisticated questions about how ancient peoples tried to sustain themselves—and whether their treatment of the land was a factor in cases where they failed.

“[These tools] open us up to thinking about the world in ways that we haven’t before,” Terry says. “We have changed the paradigm amongst the archaeologists.” 

The research appearing in SSSA-J was funded by grants from the National Science Foundation and Brigham Young University.

Read more in the latest issue of Soil Horizons, a publication of the Soil Science Society of America.

The full article is available for no charge for 30 days following the date of this summary. View the abstract athttps://www.soils.org/publications/sssaj/abstracts/0/0/sssaj2010.0224.

Contacts and sources:
Madeline Fisher
American Society of Agronomy