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| China's Hunshandake Sandy Lands [Credit: Steve Forman] |
Their research findings appear in the January 2015 issue of the Proceedings of the National Academy of Sciences and are available online.
“With our unique scientific capabilities, we are able to assert with confidence that a quick change in climate drastically changed precipitation in this area, although, further study needs to be conducted to understand why this change occurred,” Forman said.
Between 2001 and 2014, the researchers investigated sediment sections throughout the Hunshandake and were able to determine that a sudden and irreversible shift in the monsoon system led to the abrupt drying of the Hunshandake resulting in complications for the population.
“This disruption of the water flow significantly impacted human activities in the region and limited water availability. The consequences of a rapid climatic shift on the Hunshandake herding and agricultural cultures were likely catastrophic,” Forman said.
He said these climatic changes and drying of the Hunshandake continue to adversely impact the current population today. The Hunshandake remains arid and even with massive rehabilitation efforts will unlikely regrow dense vegetation.
“This study has far-reaching implications for understanding how populations respond and adapt to drastic climate change,” Forman said.
Forman is the director of the Geoluminescence Dating Research Lab in the department of geology.
Author: Tonya B. Lewis | Source: Baylor University [February 17, 2015]






