Heavy mercury contamination at Maya sites reveals a deep historic legacy

Mercury is a toxic heavy metal. When leached into the natural environment, it accumulates and builds up through food chains, ultimately threatening human health and ecosystems.

In the last century, human activities have increased atmospheric mercury concentrations by 300-500% above natural levels.

However, in some parts of the world, humans have been modifying the mercury cycle for thousands of years. This anthropogenic (human-caused) mercury use has led to mercury entering places globally it wouldn’t otherwise be found, such as in lakes or soils in remote locations.

One region with an especially long (but poorly documented) history of mercury use is Mexico and Central America. Early Mesoamerican societies such as the Olmec had been mining and using mercury in southern Mexico as early as 2000 BCE.

This map of Mexico and Central America shows sites where liquid mercury has been found, known geological sources, and Maya sites with elevated soil mercury.This map of Mexico and Central America shows sites where liquid mercury has been found, known geological sources, and Maya sites with elevated soil mercury.

In our research, published in Frontiers in Environmental Science, we review the ways the Maya used mercury, the mystery of how they sourced it, and the environmental legacy of past mercury use.

Our present mercury problem has a deep legacy. Understanding its origins will also help us understand the trajectory of humanity’s fascination with, use of – and abuse of – this mercurial element.

Cultural and creative importance

Archaeologists have been finding mercury at archaeological sites in Mexico and Central America for more than a century.

The most common form reported is cinnabar (mercury sulfide, or HgS), a bright red mineral used extensively by the ancient Maya for decoration, craft, and ritual purposes such as burials and in tombs.

 The Maya used cinnabar in burials, identifiable by its distinct red colour. The Maya used cinnabar in burials, identifiable by its distinct red colour.

It has been far less common to find liquid (elemental) mercury. There are only seven occurrences of liquid mercury at Mesoamerican sites that we are aware of.

But it’s feasible there may have been many more – and that it’s simply invisible in today’s archaeological record. Liquid mercury from 1,000 or more years ago could have evaporated or oozed away into the environment through time.

Exceeding toxic levels

Most Maya settlements were great distances from known mercury sources located in Mexico and Honduras, and perhaps Guatemala and Belize. This means the production, trade, and use of mercury would have been highly valuable and logistically challenging – especially for managing toxic liquid mercury!

Over the past two decades, scientists working on Maya archaeological projects have tested artefacts, soils, and sediments for their chemical properties, including for mercury, to better understand past human activities.

They test soils and former Maya areas excavated from far below today’s ground surface, which tell us about mercury levels during the Maya’s time.

Rob Griffin sampling sediments for mercury near the bottom of the Corriental reservoir in Tikal, Guatemala.Rob Griffin sampling sediments for mercury near the bottom of the Corriental reservoir in Tikal, Guatemala.

Combined data from these tests show most Maya sites have some amount of mercury enrichment in buried soils. Specifically, seven out of ten sites were found to have mercury levels that equal or exceed modern benchmarks for environmental toxicity.

Locations with elevated mercury are typically areas the Maya occupied, including domestic patios, dating to the Late Classic (600-900 CE). Mercury also made its way into some drinking water sources including central reservoirs at Tikal.

While the appealing red cinnabar ore is the likely culprit of mercury pollution, the equally appealing and shimmering liquid mercury is another possible source of persistent pollution in some locations, such as Lamanai in modern-day Belize.

Mercury, also known as quicksilver, occurs naturally and is the only metallic element that stays liquid at room temperature.Mercury, also known as quicksilver, occurs naturally and is the only metallic element that stays liquid at room temperature.

At more complex sites, elevated mercury levels may be the result of both modern and ancient inputs. For example, it’s not clear if the mercury detected at the island Maya settlement of Marco Gonzalez (also in Belize) is from ancient or modern times.

Looming questions

Our work reveals a rich history of mercury use by the Maya and challenges the idea that pre-industrial societies didn’t have noteworthy impacts on their environments.

But there is much we still don’t know. Where and how did the Maya obtain mercury? Who mined it, traded it, and transported it by foot over hundreds of kilometres across present-day Central America?

Then there’s the question of whether the Maya were affected by mercury exposure. The next step will be for geochemists and archaeologists to track down the source of mercury at key sites and, if possible, scrutinise archaeological and human remains for signs of past mercury exposure.

We also need to find out what forms mercury takes in the environment today, so we can better understand where it came from, and provide guidance on what precautions (if any) need to be taken when working with legacy mercury.

Finding clues on early mercury use is crucial to understanding the interaction between legacy mercury and current mercury contamination in the environment today.

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By Duncan Cook / Associate Professor in Geography, Australian Catholic University

I am a geoscientist who conducts research on environmental histories of the Common Era. My work ranges from reconstructing environmental histories of the tropics in mainland southeast Asia and Central America, through to Australian and UK paleoenvironment reconstructions. I apply techniques from sedimentology, geochemistry, geomagnetism and geochronology to understand how ecosystems have responded to climate shifts and human actions over historic timescales. In doing so, my work seeks to better understanding the complex interactions between human, climate, and earth surface systems.

In 2013 I joined the National School of Arts at Australian Catholic University (ACU). I am based at the Brisbane campus of ACU, where I hold the positions of Associate Professor in Geography and Head of Discipline (Geography). I am also an adjunct research fellow of the Beach-Butzer Geoarchaeology Lab in the School of Geography and The Environment, University of Texas at Austin. Prior to joining ACU, I held research positions at the Smithsonian Institution, Georgetown University, the University of Glasgow, and The University of Sydney. I have also spent some time working outside of academia, as an Environmental Research Scientist with the Defence Technology Agency of the New Zealand Defence Force.

By Nicholas Dunning / Professor, University of Cincinnati

Nicholas P. Dunning is a Professor in the Department of Geography & GIS at the University of Cincinnati. He specializes in human-environment interactions with foci on paleoenvironmental reconstruction, ancient subsistence, and settlement patterns. He has been engaged in field work in the Maya Lowlands for about four decades, including the Puuc region, the Petexbatun, Tikal, and other Peten sites, northern Belize, and currently at Calakmul in southern Campeche, Mexico. Dunning has also worked in the West Indies, Chaco Canyon, and the eastern Mediterranean. When not digging in archaeological contexts, he tills a large organic garden.

By Sheryl Luzzadder-Beach / Centennial Professor of Geography and the Environment, The University of Texas at Austin College of Liberal Arts

PhD Geography University of Minnesota, 1990. Centennial Professor of Geography and the Environment at the University of Texas at Austin 2014- present; Chair, Geography and the Environment UT Austin 2014-2018; President, American Association of Geographers 2018-19, (Past President 2019-present); AAAS Fellow; AAG Fellow; Professor of Geography and Geoinformation Science, George Mason University 1993-2014; Associate Provost for General Education, George Mason University 2000-2003. Research areas include physical geography, hydrology and geomorphology, water chemistry, geoarchaeology, geostatistics, and gender, science and human rights, with field research in Mesoamerica, California, the Mediterranean and Near East, Peru, and Iceland.

By Simon Turner / Senior Research Fellow in Geography, UCL

Senior Research Fellow in Physical Geography and Environmental Change. Secretary of the Anthropocene Working Group. Research background in extracting stratigraphic records from wetlands and lakes using geochemical and paleolecological techniques

By Timothy Beach / Professor, The University of Texas at Austin College of Liberal Arts

Centennial Chair & Professor
Director, Soils & Geoarchaeology Labs
Geography and Environment, University of Texas at Austin
2022-23 Dumbarton Oaks Fellow, Washington, DC

(Source: theconversation.com; September 29, 2022; https://tinyurl.com/2wru68en)
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