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DISASTER MANAGEMENT
Rise and fall of agrarian states influenced by climate volatility
by Staff Writers
University Park PA (SPX) Oct 16, 2015


Comparing the climate record with organized agrarian state level societies in Mexico, Kennett and Marwan looked at the rise and falls of three states - Teotihuacan from 100 BCE to 650 CE, Toltec from 900 to 1150 CE and the Aztec Empire from 1400 to 1519.

Climate variability is one of the major forces in the rise and fall of agrarian states in Mexico and Peru, according to a team of researchers looking at both climate and archaeological records.

"We are arguing that the climate information in both areas is good enough to establish that climate is playing some role in the rise and fall of these city states," said Douglas Kennett, professor of environmental archaeology. "Now we need to further refine the archaeological data."

Kennett, working with Norbert Marwan, climatologist and statistician, Potsdam Institute for Climate Impact Research, Germany, looked at climate records for central Mexico gleaned from a stalagmite collected from Juxtlahuaca Cave in the state of Guerrero. They also looked at the climate record preserved in the Quelccaya ice cape in the Cordillera Vilcanota portion of the Peruvian Andes.

In both cases the climate records are based on oxygen isotope measurements on datable layers of ice or stalagmite cave deposition. These records show annual changes in rainfall and temperature for 2,000 years in Mexico and 1,800 years in Peru.

"There is a long tradition of archaeology in both central Mexico and the Peruvian highlands," said Kennett. "There are also new high resolution climate records available that have not yet been capitalized on by archaeologists."

The researchers note that some refinement in archaeological dating in some areas is still needed, but that the rise and fall of major polities is reasonably well known.

Comparing the climate record with organized agrarian state level societies in Mexico, Kennett and Marwan looked at the rise and falls of three states - Teotihuacan from 100 BCE to 650 CE, Toltec from 900 to 1150 CE and the Aztec Empire from 1400 to 1519.

"The fluorescence and expansion of Teotihuacan as a regional power between 100 and 400 CE occurred during an interval of persistent and stable rainfall," the researchers report today (Oct. 18) in Philosophical Transactions of the Royal Society A. Teotihuacan, during its heyday, influenced large portions of central Mexico.

The decline of Teotihuacan from 600 to 700 occurred during "some of the most volatile climate conditions evident in the Juxtlahuaca Cave climate record." This was followed by extended drought after 700 recognized by previous studies.

The decline of major states was typically followed by dispersal or decentralization of populations and power. Smaller, usually weaker cities arose in these regions, but were highly unstable and controlled little territory.

In the early 10th Century, Tula emerged as a major force in the central highlands. This corresponded to a wetter and more stable climate period than the 7th century. The researchers note that while there is some discussion as to the dating of the Tula civilization, "it appears that Tula was established during a relatively stable climatic interval and went into decline as climatic conditions became more volatile."

"While there is some support for the hypothesis that stable climatic conditions favored political centralization and that unstable climatic conditions contributed to sociopolitical instability and decentralization," said Kennett. "Additional chronological work is needed."

By the early 15th century, Tenochtitlan, now Mexico City, was one of the large cities vying for control of the Basin of Mexico. It eventually grew to a city of 200,000 people. The growth of the Aztec empire coincided with an extremely wet and stable climatic period. The empire fell under the conquistadors who arrived in 1519, so the potential societal effects of highly volatile climatic conditions during the 16th century are difficult to evaluate.

During each of these time periods urban populations developed agricultural methods that relied on the persistent availability of rainfall - irrigation. During the climate's unstable periods, evidence of population dispersal, destruction and warfare are evident in the archaeological record.

About 3,000 miles to the south, the situation in Peru looks very similar to Mexico. Three civilizations - Wari and Tiwanaku from 300 BCE to 1000 CE and Inka from 1438 to 1525 CE - emerged in the Andes. The Wari and Tiwanaku states developed side by side in the highlands covering the area from what is now northern Peru to northern Chile.

These civilizations developed sophisticated methods of intensive agriculture suitable for these high elevations. However, these methods were sensitive to changes in temperature and precipitation. States developed when the climate was warm, wet and stable. The climate became highly volatile and dry in 1000 CE when these states both went into decline.

Again from 1000 to 1300 CE the climate was highly volatile, populations dispersed, and smaller competing polities are evident throughout the highlands. As conditions stabilized the Inka Empire emerged and dominated the Andes from Ecuador to southern Chile by the end of the 15th century.

A complex combination of irrigation, cropping and other agricultural approaches along with an intricate network of regional capitals, rituals and military campaigns created this large empire. This time was also a stable climate period. Just as the Aztec empire fell, the Inka Empire fell to the Spanish conquistadors in 1533.

Both of these regions show the formation, decline and eventual reestablishment of states in a pattern that mirrors the stability and instability of climate conditions in each region. It appears that political fragmentation, sociopolitical instability and warfare occurred during the unstable climate periods, while the growth of strong, stable, successful states were favored during stable climatic intervals.

The researchers suggest that modeling the effects of future climate variations should focus on human response to transient short-term changes in addition to the traditional focus on long-term mean changes in climate.


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