The terrestrial mollusks as new indices of the Asian paleomonsoons in the Chinese loess plateau

Global and Planetary Change

Volumn 26, Issue 1-3, 2000, Pages 199-206

  Rousseau, Denis Didier ^a,b   Wu, Naiqin ^c   Guo, Zhengtang ^c  

^a INSTITUT DES SCIENCES DE L EVOLUTION   (France)

^b Department of Earth and Environmental Sciences   (United States)

^c INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

Author keywords

China; Last climatic cycle; Loess; Mollusks; Paleomonsoons

Indexed keywords

CHINA; CLIMATE CHANGE; LOESS; MONSOON; SEASONALITY;

BIOSTRATIGRAPHY; MOLLUSC; MONSOON; PALEOCLIMATE; PEDOGENESIS;

CHINA;

EID: 0033679554     PISSN: 09218181     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0921-8181(00)00086-2     Document Type: Article

References (19)

1. Magnetic susceptibility evidence of monsoon variation on the loess plateau of Central China during the last 130,000 years
2. Long-term variations of daily insolation and Quaternary climatic changes
3. Snail assemblages in loess strata and their environmental implication
4. A coupled environmental system formed at about 2.5 Ma in East Asia
5. Late Pleistocene chronology of loess deposition near Luochuan, China
6. High frequency pulses of East Asian monsoon climate in the last two glaciations: Link with the North Atlantic
7. Magnetostratigraphical dating of loess deposits in China
8. Late Pleistocene continental climate and oceanic variability recorded in northwest Pacific sediment
9. Loess stratigraphy in central China
10. Loess stratigraphy in central China
11. Magnetic susceptibility record of Chinese Loess
12. Monsoon variability over the past 150,000 years
13. Correlation between climate events m the North Atlantic and China during the last glaciation
14. Mollusques continentaux quaternaires de Bourgogne. Significations stratigraphiques et climatiques. Rapports avec d'autres faunes boreales de France
15. Climatic records from the Eustis loess section (Nebraska, USA) during the Late Pleistocene
16. Grain size of Quartz as an indicator of winter monsoon strength on the Loess Plateau of central China during the last 130,000 yr