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Mercury Contamination in Yucatán's Ancient Maya Water Sources Persisted for Centuries

Mercury Contamination in Yucatán's Ancient Maya Water Sources Persisted for Centuries Photo: НВ — Техно

Environmental Struggles of the Ancient Maya

Recent research reveals that ancient Maya communities on Mexico's Yucatán Peninsula faced significant mercury pollution in their water sources for centuries. Mercury levels detected in these bodies of water surpassed modern toxicity thresholds, posing risks to aquatic ecosystems and potentially causing long-term health issues for the inhabitants. This contamination is linked to the Maya's use of mercury-containing materials in their rituals and decorative arts.

Core sediment samples from Lake Cobá and the Kʼsach cenote in northern Yucatán showed mercury concentrations far exceeding current safety limits. Around 720 CE, mercury levels in the Kʼsach cenote peaked at approximately 18 micrograms per gram. Between 535 and 820 CE, the average mercury concentration there was 8.4 micrograms per gram. For context, modern toxicity guidelines identify 1.06 micrograms per gram as the probable effect threshold, while 2 micrograms per gram can cause severe harm to aquatic life.

Impact of Mercury Pollution on Local Ecosystems

Mercury levels in Lake Cobá began rising around 40 CE, reaching 2.3 micrograms per gram between 250 and 300 CE before gradually declining. At its height during the Classic and Early Postclassic periods, the Maya city of Cobá had an estimated population between 50,000 and 90,000. Mercury was highly valued in the region, utilized both as elemental mercury and in the form of cinnabar, a mercury sulfide mineral. Cinnabar served as a pigment in burial rituals and was used to decorate pottery and architecture, while elemental mercury has been found at various Maya archaeological sites.

This mercury contamination was localized rather than atmospheric, resulting from mercury imports into the Lake Cobá and Kʼsach cenote basins. During periods of high mercury pollution, ostracod and gastropod shells disappeared entirely from Lake Cobá sediments. Similarly, the Kʼsach cenote saw a decline in fossilized chironomid remains as mercury concentrations increased, indicating shifts in aquatic community composition. These water sources were vital for the ancient Maya, providing both drinking water and aquatic food resources.

In a related archaeological discovery, Mexico's National Institute of Anthropology and History (INAH) uncovered a 2,500-year-old astronomical complex in Puebla. This site, the Teteles de Ávila-Castillo complex in Sierra Norte de Puebla, represents the earliest known observatory of its kind outside the Maya region. It features a quadrangular courtyard flanked by two structures, with a western platform used to track the sun’s rising position throughout the year. Notably, this platform is roughly twice the size of a similar structure found at Uaxactún in northern Guatemala.

These findings highlight how environmental factors influenced ancient civilizations like the Maya and how their cultural activities impacted natural surroundings. Mercury pollution connected to ritualistic and artistic practices suggests complex social and economic systems within these communities. Furthermore, this research offers valuable insights into the historical links between environmental changes and public health in ancient populations.