High-resolution studies of the oldest cultivated soils in the southern Loess Plateau of China

Catena

Volumn 47, Issue 1, 2002, Pages 29-42

  Huang, Chun Chang ^a,b   Pang, Jiangli ^a   Huang, Ping ^a   Hou, Chunhong ^a   Han, Yuping ^a  

^a SHAANXI NORMAL UNIVERSITY   (China)

^b State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau   (China)

Author keywords

China; Cultivated soils; Dust accumulation; Holocene; Loess Plateau; Monsoonal change

Indexed keywords

ARABLE FARMING; DUST; EOLIAN DEPOSIT; HOLOCENE; LOESS; MONSOON; PEDOGENESIS;

CHINA;

CINNAMOMUM VERUM;

EID: 0036499626     PISSN: 03418162     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0341-8162(01)00169-2     Document Type: Article

References (18)

1. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during last 130,000 years
2. The deterioration of land resources and the change in human-earth relationships in the Weihe River Basin at about 3100 years BP
3. Diagnostic features and criteria of the heilusol (dark loessial soil) in the Loess Plateau
4. A regional aridity phase and its possible cultural impact during the Holocene Megathermal in the Guanzhong Basin, China
5. Chinese loess and the evolution of the East Asian monsoon
6. The environmental background of the dark loessial soil formation
7. Magnetic properties of modern soil and Quaternary loessic palaeosols: Palaeoclimatic implications
8. Complexity of Holocene climate as reconstructed from a Greenland ice core
9. Climatic variation and the major events in the Holocene in China
10. Advances in the studies of Chinese sand and dust storms
11. Analysis of dust rain in the historic times of China
12. Pedogenic evolution of the dark loessial soil in the eastern Gansu Province
13. Reappraisal of Chinese Loess Plateau stratigraphical sequences over the last 30,000 years: Precursors of an important Holocene monsoon climatic event