Study attributes Tibetan Empire collapse in 9th century to climate change

Historical reconstruction of the Tibetan Empire’s extent among surrounding empires at its peak ca. 800 CE [Credit: Chen et al. 2023]

The ‘abrupt’ climate change found by the researchers looks like a prelude to the Medieval Warm Period. Even without examining any technical details it’s clear from the data that the climate of the region did change. Interestingly, the aftermath of the period of change looks a lot like the Medieval Warm Period (see here, under ‘severe dry and warm’), which Wikipedia thinks ‘was a time of warm climate in the North Atlantic region that lasted from c. 950 to c. 1250’. The North Atlantic and Tibet are far apart, obviously.
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The Tibetan Empire was the world’s highest elevation empire, sitting over 4,000m above sea level, and thrived during 618 to 877 CE, says Phys.org.

Home to an estimated 10 million people, it spanned approximately 4.6 million km² across East and Central Asia, extending into northern India.

Considering the hostile conditions for populations to expand, including hypoxia where oxygen concentrations are 40% lower than at sea level, it is incredible that the empire flourished.

However, its collapse in the 9th century is not fully understood, with new research published in Quaternary Science Reviews aiming to untangle the role climate may have played in the end of a great civilization.

Zhitong Chen, from the Institute of Tibetan Plateau Research, China, and colleagues turned to the geological record of lake sediments (paleolimnology) to determine how the environment changed 12 centuries ago.

Xardai Co’s freshwater lake sediments preserve the remains of microscopic single-celled algae known as diatoms, with the research team noting a significant change from planktonic varieties (those drifting within a water body, generally nearer to the surface) to benthic forms (living near the lake floor). This is interpreted as representing a shift to drier conditions, therefore lowering lake levels.

There is a distinct pattern of high lake levels, suggesting warm and humid conditions prevailed during the rise and peak of the Tibetan Empire ca. 600-800 CE, before conditions intensified to severe drought, coinciding with the empire’s collapse ca. 800-877 CE.

Chen and collaborators link drought with the likelihood of crop failure leading to social unrest among the population, alongside religious and political challenges, thus consequently the empire’s demise.

The Tibetan Plateau is extremely sensitive to changes in climate due to its elevation, with temperature and precipitation fluctuations varying significantly from the average experienced across Earth. The study lake, Xardai Co, is typically ice covered today from November to April, but experiences local temperature shifts between –12.1°C and 14.1°C, as well as 71mm annual rainfall. These factors have important consequences on lake levels and therefore the organisms that live within them.
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The tipping point at 800 CE however sees a rapid increase in benthic diatoms Amphora pediculus and Amphora inariensis, while the aforementioned open water Lindavia radiosa and Lindavia ocellata declined. This diatom community persisted until 1300 CE, when lake levels began to rise once again during the Little Ice Age.

The data were matched against other paleo-environmental indicators from across the Tibetan Plateau and confirmed that these climate changes were persistent across the region, not solely localized to the study lake. This included precipitation records inferred from a second lake located 50km north of Xardai Co, Banggong Co, as well as temperature records from China.

Linking the climate changes to its impact upon the population of the time, agriculture and livestock farming were the dominant livelihoods, with crop production in the Yarlung Zangbo River valley and grazing on the Qangtang Plateau.

During empire expansion, the warmth and rain would have encouraged crop production and wild pasture for grazing animals, as well as raised the altitude at which they could be grown. Horses, goats and yaks are grazing animals and were important for the trade economy of Tibet.

Full article here.