No single dating technique can offer absolute certainty. The most robust chronologies emerge from the cross-validation of complementary methods — radiocarbon, thermoluminescence, OSL, dendrochronology, and ESR. This integrated strategy is now the international standard for high-level Pre-Columbian expertise.
Guillaume Bresso systematically applies this multidisciplinary framework to deliver assessments of exceptional scientific reliability.
Choosing the Right Method: Radiocarbon, TL, or OSL?
The choice of dating method is strategic and depends on the material and research question. Below is a comparative overview:
| Method |
Material |
Measurable Period |
Average Precision |
Main Limitations |
| Radiocarbon (C14) |
Organic matter |
Up to ~50,000 years |
±20 to ±200 years |
Sensitive to contamination; inapplicable to minerals |
| Thermoluminescence (TL) |
Ceramics, terracotta |
300 to 500,000 years |
±10% |
Partially destructive |
| OSL |
Sediments, quartz/feldspar |
1,000 to 700,000 years |
±5% to ±15% |
Requires strict light-protected sampling |
Combining these methods on Pre-Columbian material yields the most reliable and defensible chronologies.