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<a rel = "lightbox" href = "https://3c1703fe8d.site.internapcdn.net/newman/gfx/news/2019/5c7457e8d7dd1.jpg" title = "Cahokia Region and Horseshoe Lake Watershed, represented by a dotted black line The dark brown colors indicate a higher topography, mainly the slopes of the river, and the yellow, the Mississippi floodplain.The core sites are indicated by red stars.The Cahokia complex is approached by the large circle surrounding black rectangles indicating the position of some of the mounds The black dots indicate the location of other sites with mounds in the Horseshoe Lake watershed that were occupied at the same time as Cahokia [∼1000–1400 CE]. The elevation data of the base map is derived from the national altitude dataset. Credit: PNAS (2019). 10.1073 / pnas.1809400116 ">
Cahokia area and Horseshoe Lake watershed, represented by the black dotted line. The dark brown colors indicate a higher topography, mainly the river's cliffs, and the yellow, the Mississippi floodplain. The core sites are indicated by red stars. The Cahokia complex is approached by the large circle surrounding black rectangles indicating the position of some of the mounds on the site. The black dots indicate the location of other sites with mounds in the Horseshoe Lake watershed that were occupied at the same time as Cahokia. [∼1000–1400 CE]. The elevation data of the base map is derived from the national altitude dataset. Credit: PNAS (2019). 10.1073 / pnas.1809400116
A new study shows that climate change may have contributed to the decline of Cahokia, a famous prehistoric city near St. Louis. And it's about old human poop.
Posted today [Feb. 25, 2019] in the Proceedings of the National Academy of Sciences, the study establishes a direct link between changes in the size of the Cahokia population, as measured by a single fecal record, and environmental data showing signs of drought and floods.
"The way to rebuild the population usually involves archaeological data, which are distinct from the data being studied by climatologists," says lead author, AJ White, who has completed the work as a postgraduate student. at California State University in Long Beach. "One is about digging and excavating archaeological remains and the other about carrot lakes, and we are uniting these two factors by looking at both types of data from the same core of lakes."
Last year, White and a team of collaborators – including his former adviser Lora Stevens, professor of paleoclimatology and paleolimnology at California State University in Long Beach and the professor of anthropology at the University of Wisconsin-Madison – showed that they could detect human poop signatures. in lake carrot sediments collected in Horseshoe Lake, not far from the famous mounds of Cahokia.
These signatures, called fecal stanols, are molecules produced in the intestine during digestion and eliminated in the stool. When the inhabitants of Cahokia pooped on the mainland, part of it would have sunk into the lake. The more people lived and did their needs, more stanols were present in the lake sediments.
Because the sediments of a lake accumulate in layers, they allow scientists to capture snapshots of time throughout the history of an area through sediment cores. The deeper layers are formed earlier than the layers found above and all the material of a layer is about the same age.
White found that fecal stanol concentrations in Horseshoe Lake increased and decreased in the same manner as estimates of the Cahokia population based on more established archaeological methods.
Schroeder, a scholar from the Cahokia region, explains that the excavations of the houses of Cahokia and its surroundings show that the human occupation of the site has intensified around 600 AD and that 39, in 1100, the city of six square miles reached its peak of population. At the time, tens of thousands of people called him at home.
Archaeological evidence also shows that in 1200, the population of Cahokia was declining and the site was abandoned by Mississippians who built a mound around 1400.
Scientists have uncovered a number of explanations for its possible abandonment, including social and political unrest and environmental change.
For example, in 2015, Samuel Munoz, a former graduate student from UW-Madison and now a professor at Northeastern University, was the first to collect one of the Horseshoe Lake sediment cores. , which White had used in his study. the nearby Mississippi River was significantly flooded at approximately 11:50 am
White's latest study combines archaeological and environmental evidence.
"When we use this fecal stanol method, we can make these comparisons with environmental conditions that we have not been able to do so far," says White, who currently holds a doctorate. student at UC Berkeley.
Using the Munoz core and another White collected on Horseshoe Lake, the research team measured the relative amount of fecal stanols from humans present in the sediment layers. They compared these levels with stanol levels known to come from bacteria in the soil to establish a baseline concentration for each layer.
They examined the cores of lakes in search of floods and also looked for climate indicators to know if the weather conditions were relatively wet or dry. These indicators, the ratio of a heavy form of oxygen to a light form, can show changes in evaporation and precipitation. Stevens explains that when the water evaporates, the light form of oxygen goes with it, concentrating the heavy form.
The core of the lake showed that summer precipitation probably decreased around the beginning of Cahokia's decline. This could have affected people's ability to grow their maize, a staple crop.
Around 1150 archaeological records began to change in many ways, including the number and density of houses and the nature of artisanal production.
These are all indicators "of some kind of socio-political or economic stressors that have spurred a reorganization of some sort," she said. "When we see correlations with the climate, some archaeologists do not think climate is a factor, but it's hard to maintain this argument when evidence of significant climate change shows that people are facing new challenges. "
This is resonating today, she adds.
"Crops can be very resilient to climate change, but resilience does not necessarily mean there is no change, there may be cultural reorganization or decisions to move or migrate" says Schroeder. "We can see similar pressures today but fewer options to move."
For White, the study highlights the nuances and complications common to so many cultures and shows how environmental changes can contribute to the social changes already at stake.
Explore further:
Scientists can measure the evolution of the population with the help of chemicals found in the stool
More information:
A J. White el al., "Faecal stanols show a parallel correlation between floods and seasonal rainfall change and the decline of the population of Cahokia" PNAS (2019). www.pnas.org/cgi/doi/10.1073/pnas.1809400116
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