Enguo Sheng
Biographic Data
| ID | 5099263 |
|---|---|
| NAME | Enguo Sheng |
| GIVEN NAMES | Enguo |
| FAMILY NAME | Sheng |
| SIGNATURE | SHENG E |
| AFFILIATIONS | Chinese Academy of Sciences |
| ORCID | 0000-0001-8883-0858 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2013 |
| LATEST PUBLICATION YEAR | 2018 |
| H-INDEX | 0 |
Climate changes reconstructed from a glacial lake in High Central Asia over the past two millennia
Late Holocene Indian Summer Monsoon Variations Recorded at Lake Erhai, Southwestern China
In this study we report changes in Indian summer monsoon (ISM) intensity during the past ~ 3500 yr inferred from proxy indices at Lake Erhai, southwestern China. Both the pollen concentrations and other proxy indices, including sediment grain size, total organic carbon contents (TOC), and elemental contents (e.g., Fe, Al), clearly indicate a long term decreasing trend in ISM intensity over the late Holocene. During the period from approximately A…
Abrupt Holocene Indian Summer Monsoon failures
Knowledge of the millennial abrupt monsoon failures is critical to understanding the related causes. Here, we extracted proxy indices of Indian Summer Monsoon (ISM) intensity during the early to mid-Holocene, from peat deposits at Lake Xihu, in southwestern China. There are a series of abrupt, millennial-scale episodes of ISM weakening inferred from the Lake Xihu records, which are generally synchronous with those inferred from other archives ove…
Holocene peatland development along the eastern margin of the Tibetan Plateau
Knowledge of peatland initiation, accumulation, and decline or cessation is critical in understanding peatland development and the related carbon source/sink effect. In this study, we investigated the development of three peat profiles along the eastern margin of the Tibetan Plateau (ETP) and compared the results with those of our previous work along this transect. Our work showed that the initiation over the northern ETP is later and the slowdow…
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Holocene peatland development along the eastern margin of the Tibetan Plateau
Knowledge of peatland initiation, accumulation, and decline or cessation is critical in understanding peatland development and the related carbon source/sink effect. In this study, we investigated the development of three peat profiles along the eastern margin of the Tibetan Plateau (ETP) and compared the results with those of our previous work along this transect. Our work showed that the initiation over the northern ETP is later and the slowdow…
Late Holocene Indian Summer Monsoon Variations Recorded at Lake Erhai, Southwestern China
In this study we report changes in Indian summer monsoon (ISM) intensity during the past ~ 3500 yr inferred from proxy indices at Lake Erhai, southwestern China. Both the pollen concentrations and other proxy indices, including sediment grain size, total organic carbon contents (TOC), and elemental contents (e.g., Fe, Al), clearly indicate a long term decreasing trend in ISM intensity over the late Holocene. During the period from approximately A…
Abrupt Holocene Indian Summer Monsoon failures
Knowledge of the millennial abrupt monsoon failures is critical to understanding the related causes. Here, we extracted proxy indices of Indian Summer Monsoon (ISM) intensity during the early to mid-Holocene, from peat deposits at Lake Xihu, in southwestern China. There are a series of abrupt, millennial-scale episodes of ISM weakening inferred from the Lake Xihu records, which are generally synchronous with those inferred from other archives ove…
Climate changes reconstructed from a glacial lake in High Central Asia over the past two millennia
Climatology (4 works) · Geography (4 works) · Geology and Paleoclimatology Research (4 works) · Holocene (4 works) · Physical geography (4 works) · Arid (3 works) · Monsoon (3 works) · Archaeology and ancient environmental studies (2 works) · Coastal wetland ecosystem dynamics (2 works) · Ecology (2 works)