Climate change and cultural response around 4000 cal yr B.P. in the western part of Chinese Loess Plateau

@article{An2005ClimateCA,
  title={Climate change and cultural response around 4000 cal yr B.P. in the western part of Chinese Loess Plateau},
  author={Cheng-bang An and Lingyu Tang and Loukas Barton and Fahu Chen},
  journal={Quaternary Research},
  year={2005},
  volume={63},
  pages={347 - 352}
}
New data suggest that dramatic environmental change in the Western Loess Plateau of China corresponded with substantial changes in human demography ca. 4000 cal yr B.P. These data demonstrate that a rapid climatic transition from wet to dry led to an ecologically devastated period between 4090 and 3600 cal yr B.P. The sudden reduction in the number of archaeological sites during this period, namely a reduction in the total number of sites and a contraction of the areal distribution of sites… 
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References

SHOWING 1-10 OF 49 REFERENCES
Environmental change and cultural response between 8000 and 4000 cal. yr BP in the western Loess Plateau, northwest China
Two ancient swamps in the western Loess Plateau, northwest China record the climate history between 8000 and 4000 cal. yr BP. Grain size, CaCO3, organic matter, mollusc fauna and pollen assemblages
Climate change at the 4.2 ka BP termination of the Indus valley civilization and Holocene south Asian monsoon variability
[1] Planktonic oxygen isotope ratios off the Indus delta reveal climate changes with a multi-centennial pacing during the last 6 ka, with the most prominent change recorded at 4.2 ka BP. Opposing
Human Occupations and Climate Change in the Puna de Atacama, Chile
TLDR
Faunal diversity was highest during the humid early Holocene of Atacama Desert, and the mid-Holocene collapse of human occupation is also recorded in cave deposits.
Evidence of a humid mid-Holocene in the western part of Chinese Loess Plateau
Field works show that the wetland/swamp layers were distributed ubiquitously in the western part of the Chinese Loess Plateau. Universality of the wetland/swampy layer and the consistency of the age
Late Holocene Climate and Cultural Changes in the Southwestern United States
TLDR
Columnar stalagmites in caves of the Guadalupe Mountains during the late Holocene record a 4000-year annually resolved climate history for the southwestern United States, with the exception of a slightly wetter interval from 440 to 290 years before the present.
Climate and the collapse of Maya civilization.
TLDR
A seasonally resolved record of titanium shows that the collapse of Maya civilization in the Terminal Classic Period occurred during an extended regional dry period, punctuated by more intense multiyear droughts centered at approximately 810, 860, and 910 A.D.
The Genesis and Collapse of Third Millennium North Mesopotamian Civilization
TLDR
Archaeological and soil-stratigraphic data define the origin, growth, and collapse of Subir, the third millennium rain-fed agriculture civilization of northern Mesopotamia on the Habur Plains of Syria and suggest that the impact of the abrupt climatic change was extensive.
Third Millennium BC Climatic Change and Old World Collapse
Around 4000 years ago the advanced urban civilizations of Egypt, Mesopotamia and India suddenly collapsed. Recent discoveries now strongly suggest that the collapse was linked to climate change. This
Kilimanjaro Ice Core Records: Evidence of Holocene Climate Change in Tropical Africa
TLDR
Variable deposition of F– and Na+during the African Humid Period suggests rapidly fluctuating lake levels between ∼11.7 and 4 ka, which is coincident with the “First Dark Age,” the period of the greatest historically recorded drought in tropical Africa.
Possible role of climate in the collapse of Classic Maya civilization
THE Maya civilization developed around 3,000 years ago in Mesoamerica, and after flourishing during the so-called Classic period, it collapsed around 750–900 AD1. It has been specula ted2–6 that
...
1
2
3
4
5
...