F H Chen
Dados Biográficos
| ID | 5216735 |
|---|---|
| NOME | F H Chen |
| PRENOMES | F H |
| SOBRENOME | Chen |
| ASSINATURA | CHEN F H |
| AFILIAÇÕES | Key Laboratory of Western China's Environmental Systems (Ministry of Education) Research School of Arid Environment and Climate Change Lanzhou University Lanzhou Gansu Province 730000 China |
| VERIFICADO | Não |
| TOTAL DE OBRAS | 4 |
| TOTAL DE CITAÇÕES | 11 |
| TOTAL COMO AUTOR | 4 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1991 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2014 |
| ÍNDICE H | 2 |
Stable Isotope Analysis of Human and Faunal Remains in the Western L oess P lateau, Approximately 2000 cal bc
During the second millennium bc , several significant changes were happening in prehistoric societies across E urasia. For instance, shifts in subsistence practice occurred in north‐western C hina, including the western L oess P lateau. However, the magnitude and nature of this dietary change are unclear and more detailed information and regional studies are needed in order to fully understand the reasons behind this change. In this study, palaeo…
Dry late-glacial and early Holocene climate in arid central Asia indicated by lithological and palynological evidence from Bosten Lake, China
Chronological discord between the last interglacial paleosol (S1) and its parent material in the Chinese Loess Plateau
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
Stable Isotope Analysis of Human and Faunal Remains in the Western L oess P lateau, Approximately 2000 cal bc
During the second millennium bc , several significant changes were happening in prehistoric societies across E urasia. For instance, shifts in subsistence practice occurred in north‐western C hina, including the western L oess P lateau. However, the magnitude and nature of this dietary change are unclear and more detailed information and regional studies are needed in order to fully understand the reasons behind this change. In this study, palaeo…
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
Chronological discord between the last interglacial paleosol (S1) and its parent material in the Chinese Loess Plateau
Dry late-glacial and early Holocene climate in arid central Asia indicated by lithological and palynological evidence from Bosten Lake, China
Stable Isotope Analysis of Human and Faunal Remains in the Western L oess P lateau, Approximately 2000 cal bc
During the second millennium bc , several significant changes were happening in prehistoric societies across E urasia. For instance, shifts in subsistence practice occurred in north‐western C hina, including the western L oess P lateau. However, the magnitude and nature of this dietary change are unclear and more detailed information and regional studies are needed in order to fully understand the reasons behind this change. In this study, palaeo…
Geography (4 obras) · Ecology (3 obras) · Geological formations and processes (3 obras) · Geology (3 obras) · Geology and Paleoclimatology Research (3 obras) · Paleontology (3 obras) · Physical geography (3 obras) · Pleistocene-Era Hominins and Archaeology (3 obras) · Archaeology (2 obras) · Climate change (2 obras)