Z-D Feng
Biographic Data
| ID | 6572562 |
|---|---|
| NAME | Z-D Feng |
| GIVEN NAMES | Z-D |
| FAMILY NAME | Feng |
| SIGNATURE | FENG Z |
| AFFILIATIONS | Chinese Academy of Sciences |
| VERIFIED | No |
| TOTAL WORKS | 11 |
| TOTAL CITATIONS | 1 |
| AUTHOR COUNT | 11 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1998 |
| LATEST PUBLICATION YEAR | 2015 |
| H-INDEX | 1 |
Climate changes and hydrological responses in the Tianshan Mountains and the northern Basins
Bioclimatic change of the past 2500 years within the Balkhash Basin, eastern Kazakhstan, Central Asia
Hydrological and ecological responses to climatic change and to land-use/land-cover changes in Central Asia
Geomorphological and sedimentological precautions in radiocarbon dating of eolian and lacustrine sequences in arid Asia
Holocene climate variations retrieved from Gun Nuur lake-sediment core in the northern Mongolian Plateau
Our pollen-based climate reconstruction shows that both temperature and moisture were low during the early Holocene from ~10,000 to ~8000 cal. a BP and gradually climbed from ~8000 to ~6000 cal. a BP. The last ~6000 years have been generally warm and wet with high-amplitude fluctuations. The high-moisture conditions for the past ~6000 years are not only corroborated by high arboreal pollen/non-arboreal (AP/NAP; trees and shrubs over herbs) pollen…
Stratigraphies and chronologies of late Quaternary loess–paleosol sequences in the core area of the central Asian arid zone
Holocene climatic and environmental changes in the arid and semi-arid areas of China: A review
This paper reviews recently published literature, most of which was published in Chinese, and searches for regional patterns of Holocene changes useful in depicting global patterns. The Holocene in the Xinjiang region can be divided into three stages: a warming and dry early stage (from 11 10 to 8-7 ka BP), a warm and wet middle stage (from 8-7 to 4.5-3 ka BP) and a fluctuating cool and dry late stage (since 4.5-3 ka BP). The Holocene in the nort…
Lacustrine and eolian records of Holocene climate changes in the Mongolian Plateau: Preliminary results
Chronological discord between the last interglacial paleosol (S1) and its parent material in the Chinese Loess Plateau
Gobi dynamics in the Northern Mongolian Plateau during the past 20,000+yr: Preliminary results
Last Glacial snowlines in the Tibetan Plateau: An argument against an extensive coalescing icesheet
Holocene climate variations retrieved from Gun Nuur lake-sediment core in the northern Mongolian Plateau
Our pollen-based climate reconstruction shows that both temperature and moisture were low during the early Holocene from ~10,000 to ~8000 cal. a BP and gradually climbed from ~8000 to ~6000 cal. a BP. The last ~6000 years have been generally warm and wet with high-amplitude fluctuations. The high-moisture conditions for the past ~6000 years are not only corroborated by high arboreal pollen/non-arboreal (AP/NAP; trees and shrubs over herbs) pollen…
Last Glacial snowlines in the Tibetan Plateau: An argument against an extensive coalescing icesheet
Gobi dynamics in the Northern Mongolian Plateau during the past 20,000+yr: Preliminary results
Chronological discord between the last interglacial paleosol (S1) and its parent material in the Chinese Loess Plateau
Lacustrine and eolian records of Holocene climate changes in the Mongolian Plateau: Preliminary results
Holocene climatic and environmental changes in the arid and semi-arid areas of China: A review
This paper reviews recently published literature, most of which was published in Chinese, and searches for regional patterns of Holocene changes useful in depicting global patterns. The Holocene in the Xinjiang region can be divided into three stages: a warming and dry early stage (from 11 10 to 8-7 ka BP), a warm and wet middle stage (from 8-7 to 4.5-3 ka BP) and a fluctuating cool and dry late stage (since 4.5-3 ka BP). The Holocene in the nort…
Stratigraphies and chronologies of late Quaternary loess–paleosol sequences in the core area of the central Asian arid zone
Bioclimatic change of the past 2500 years within the Balkhash Basin, eastern Kazakhstan, Central Asia
Hydrological and ecological responses to climatic change and to land-use/land-cover changes in Central Asia
Geomorphological and sedimentological precautions in radiocarbon dating of eolian and lacustrine sequences in arid Asia
Holocene climate variations retrieved from Gun Nuur lake-sediment core in the northern Mongolian Plateau
Our pollen-based climate reconstruction shows that both temperature and moisture were low during the early Holocene from ~10,000 to ~8000 cal. a BP and gradually climbed from ~8000 to ~6000 cal. a BP. The last ~6000 years have been generally warm and wet with high-amplitude fluctuations. The high-moisture conditions for the past ~6000 years are not only corroborated by high arboreal pollen/non-arboreal (AP/NAP; trees and shrubs over herbs) pollen…
Climate changes and hydrological responses in the Tianshan Mountains and the northern Basins
Geology (11 works) · Geography (10 works) · Physical geography (10 works) · Geology and Paleoclimatology Research (9 works) · Geomorphology (6 works) · Loess (6 works) · Paleontology (6 works) · Paleosol (6 works) · Climatology (5 works) · Geological formations and processes (5 works)