Groundwater sapping as the cause of irreversible desertification of Hunshandake Sandy Lands, Inner Mongolia, northern China

In the middle-to-late Holocene, Earth’s monsoonal regions experienced catastrophic precipitation decreases that produced green to desert state shifts. Resulting hydrologic regime change negatively impacted water availability and Neolithic cultures. Whereas mid-Holocene drying is commonly attributed...

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Detalles Bibliográficos
Publicado en:Proc Natl Acad Sci U S A
Autores principales: Yang, Xiaoping, Scuderi, Louis A., Wang, Xulong, Scuderi, Louis J., Zhang, Deguo, Li, Hongwei, Forman, Steven, Xu, Qinghai, Wang, Ruichang, Huang, Weiwen, Yang, Shixia
Formato: Artigo
Lenguaje:Inglês
Publicado: National Academy of Sciences 2015
Materias:
Physical Sciences
Acceso en línea:https://ncbi.nlm.nih.gov/pmc/articles/PMC4311860/
https://ncbi.nlm.nih.gov/pubmed/25561539
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1418090112
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