Zhuo Zheng
Datos Biográficos
| ID | 4455072 |
|---|---|
| NOMBRE | Zhuo Zheng |
| NOMBRES | Zhuo |
| APELLIDO | Zheng |
| FIRMA | ZHENG Z |
| AFILIACIONES | Sun Yat-sen University |
| ORCID | 0000-0003-1698-1440 |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 26 |
| TOTAL DE CITAS | 13 |
| TOTAL COMO AUTOR | 26 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 2000 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2026 |
| ÍNDICE H | 2 |
First successful purification of single-taxon fossil pollen from tropical peat sediments
Dynamic, high-resolution poverty measurement in data-scarce environments
Forest transformation and human impact in pearl river delta, south China, during the last 6000 cal yr BP
Regional land cover changes of the last 6,500 years in middle and southern subtropical China
Quantitative Land-Cover Reconstructions for China over the Past 6000 Years
Validation of relative pollen productivities for major tropical plant taxa
The environmental conditions of MIS5 in the northern South China Sea, revealed by n-alkanes indices and alkenones from a 39 m-long sediment sequence
Holocene fire and forest histories in relation to climate change and agriculture development in southeastern China
Pollen morphology of selected crop plants from southern China and testing pollen morphological data in an archaeobotanical study
A late Holocene record of vegetation and fire from the Amur Basin, far-eastern Russia
Holocene temperature and precipitation variability on the central Tibetan Plateau revealed by multiple palaeo-climatic proxy records from an alpine wetland sequence
This study has reconstructed the Holocene environmental history of central Tibetan Plateau, a transitional area between monsoon-dominated Asia and Westerlies-dominated Asia, to examine the interplay between the two circulation systems and effects of other potential mechanisms on the temporal variability of Holocene climatic conditions in the study area. Specifically, this study has produced a twin record of palaeo-hydrology and palaeo-temperature…
Pollen- and charcoal-based evidence for climatic and human impact on vegetation in the northern edge of Wuyi Mountains, China, during the last 8200 years
Pollen and charcoal records derived from the sediment core of Lantianyan (LTY) peat bog, Northern Wuyi Mountain chains, eastern subtropical China, provide valuable information of landscape evolution caused by both climatic variation and anthropogenic activities over the past 8200 years. Our results reveal fluvial and lacustrine deposition between c. 8200 and 5600 cal. yr BP. The high proportion of pollen from evergreen broadleaved forests (e.g. Q…
New evidence for Neolithic rice cultivation and Holocene environmental change in the Fuzhou Basin, southeast China
Peatland evolution and associated environmental changes in central China over the past 40,000 years
Central China has experienced stronger summer monsoon during warm periods such as Marine Isotope Stages (MIS) 1 and 3, and weaker summer monsoon during cool periods such as MIS 2. The evolution history of Dajiuhu subalpine peatland in central China can help investigate how the expansion and shrinkage of peatland were associated with monsoonal strength over the last glacial–interglacial cycle. Here we apply bulk organic carbon and molecular biomar…
Assessing the Importance of Climate Variables for the Spatial Distribution of Modern Pollen Data in China
To assess the importance of climate variables for the distribution of modern pollen data in China, we present a continental-scale dataset consisting of 1374 samples. Boosted regression trees and constrained ordination techniques are employed to quantify the importance of six climate variables (annual precipitation, PANN; actual/potential evapotranspiration ratio, Alpha; mean annual temperature, TANN; mean temperature of the warmest month, MTWA; m…
East Asian summer monsoon precipitation variability since the last deglaciation
The lack of a precisely-dated, unequivocal climate proxy from northern China, where precipitation variability is traditionally considered as an East Asian summer monsoon (EASM) indicator, impedes our understanding of the behaviour and dynamics of the EASM. Here we present a well-dated, pollen-based, ~20-yr-resolution quantitative precipitation reconstruction (derived using a transfer function) from an alpine lake in North China, which provides fo…
East Asian summer monsoon precipitation variations in China over the last 9500 years
To better understand the long-term changes of the East Asian summer monsoon precipitation ( P jja ), quantitative reconstructions and model simulations are needed. Here, we develop continental-scale pollen-based transfer functions for P jja with weighted averaging–partial least squares (WA-PLS) regression and a Bayesian multinomial regression method. We apply these transfer functions to a set of fossil pollen data from monsoonal China for quantit…
An examination of the fidelity of n-alkanes as a palaeoclimate proxy from sediments of Palaeolake Tianyang, South China
A stable mid-late Holocene monsoon climate of the central Tibetan Plateau indicated by a pollen record
Biomarker-based reconstructions of Holocene lake-level changes at Lake Gahai on the northeastern Tibetan Plateau
Holocene hydrological changes in regions dominated by the westerlies significantly differ from those by the Asian summer monsoon. The high-elevated northeastern Tibetan Plateau, located in between, is likely influenced by the interactions of both circulation systems. Here, we attempt to use biomarkers, n-alkanes and alkenones, to reconstruct Holocene lake-level changes at Lake Gahai in the Qaidam Basin. We choose a sediment core drilled at the la…
Vegetation changes during the past 40,000 years in Central China from a long fossil record
A palaeoenvironmental study of the Shiniusi archaeological sites in the Wujiang Drainage Area, upper Yangtze River, Chongqing region, China
Modern pollen assemblages from cultivated rice fields and rice pollen morphology
Pollen from a series of surface soil samples collected along a transect spanning southeast China was investigated to better understand palynological signals of ancient agriculture and other human activity. The transect surface samples consist of pairs taken inside and outside rice paddy fields. Pollen assemblages from these samples are valuable as modern analogs of human-altered environments and rice agriculture. Our measurements of Poaceae polle…
Palaeoenvironmental significance of grain-size distribution of river flood deposits
Palynological and satellite-based Modis observations of modern vegetational gradients in China
New evidence for Neolithic rice cultivation and Holocene environmental change in the Fuzhou Basin, southeast China
Pollen morphology of selected crop plants from southern China and testing pollen morphological data in an archaeobotanical study
Modern pollen assemblages from cultivated rice fields and rice pollen morphology
Pollen from a series of surface soil samples collected along a transect spanning southeast China was investigated to better understand palynological signals of ancient agriculture and other human activity. The transect surface samples consist of pairs taken inside and outside rice paddy fields. Pollen assemblages from these samples are valuable as modern analogs of human-altered environments and rice agriculture. Our measurements of Poaceae polle…
Forest transformation and human impact in pearl river delta, south China, during the last 6000 cal yr BP
Pollen- and charcoal-based evidence for climatic and human impact on vegetation in the northern edge of Wuyi Mountains, China, during the last 8200 years
Pollen and charcoal records derived from the sediment core of Lantianyan (LTY) peat bog, Northern Wuyi Mountain chains, eastern subtropical China, provide valuable information of landscape evolution caused by both climatic variation and anthropogenic activities over the past 8200 years. Our results reveal fluvial and lacustrine deposition between c. 8200 and 5600 cal. yr BP. The high proportion of pollen from evergreen broadleaved forests (e.g. Q…
Palaeoenvironmental significance of grain-size distribution of river flood deposits
Vegetation, Climate, and Sea Level in the Past 55,000 Years, Hanjiang Delta, Southeastern China
Pollen in Quaternary deposits from the subtropical Hanjiang Delta records three major phases in the local vegetation and climate history during the last 55,000 yr: (1) a prevalent cool-to-temperate and humid climate at ca. 24,000 14 C yr B.P. is indicated by abundant pollen of temperate trees including conifers; (2) between 20,000 and 15,000 14 C yr B.P., a cold, dry environment was associated with low sea level during the last glaciation, leadin…
Palynological and satellite-based Modis observations of modern vegetational gradients in China
A palaeoenvironmental study of the Shiniusi archaeological sites in the Wujiang Drainage Area, upper Yangtze River, Chongqing region, China
Modern pollen assemblages from cultivated rice fields and rice pollen morphology
Pollen from a series of surface soil samples collected along a transect spanning southeast China was investigated to better understand palynological signals of ancient agriculture and other human activity. The transect surface samples consist of pairs taken inside and outside rice paddy fields. Pollen assemblages from these samples are valuable as modern analogs of human-altered environments and rice agriculture. Our measurements of Poaceae polle…
Palaeoenvironmental significance of grain-size distribution of river flood deposits
Vegetation changes during the past 40,000 years in Central China from a long fossil record
An examination of the fidelity of n-alkanes as a palaeoclimate proxy from sediments of Palaeolake Tianyang, South China
A stable mid-late Holocene monsoon climate of the central Tibetan Plateau indicated by a pollen record
Biomarker-based reconstructions of Holocene lake-level changes at Lake Gahai on the northeastern Tibetan Plateau
Holocene hydrological changes in regions dominated by the westerlies significantly differ from those by the Asian summer monsoon. The high-elevated northeastern Tibetan Plateau, located in between, is likely influenced by the interactions of both circulation systems. Here, we attempt to use biomarkers, n-alkanes and alkenones, to reconstruct Holocene lake-level changes at Lake Gahai in the Qaidam Basin. We choose a sediment core drilled at the la…
Peatland evolution and associated environmental changes in central China over the past 40,000 years
Central China has experienced stronger summer monsoon during warm periods such as Marine Isotope Stages (MIS) 1 and 3, and weaker summer monsoon during cool periods such as MIS 2. The evolution history of Dajiuhu subalpine peatland in central China can help investigate how the expansion and shrinkage of peatland were associated with monsoonal strength over the last glacial–interglacial cycle. Here we apply bulk organic carbon and molecular biomar…
Assessing the Importance of Climate Variables for the Spatial Distribution of Modern Pollen Data in China
To assess the importance of climate variables for the distribution of modern pollen data in China, we present a continental-scale dataset consisting of 1374 samples. Boosted regression trees and constrained ordination techniques are employed to quantify the importance of six climate variables (annual precipitation, PANN; actual/potential evapotranspiration ratio, Alpha; mean annual temperature, TANN; mean temperature of the warmest month, MTWA; m…
East Asian summer monsoon precipitation variability since the last deglaciation
The lack of a precisely-dated, unequivocal climate proxy from northern China, where precipitation variability is traditionally considered as an East Asian summer monsoon (EASM) indicator, impedes our understanding of the behaviour and dynamics of the EASM. Here we present a well-dated, pollen-based, ~20-yr-resolution quantitative precipitation reconstruction (derived using a transfer function) from an alpine lake in North China, which provides fo…
East Asian summer monsoon precipitation variations in China over the last 9500 years
To better understand the long-term changes of the East Asian summer monsoon precipitation ( P jja ), quantitative reconstructions and model simulations are needed. Here, we develop continental-scale pollen-based transfer functions for P jja with weighted averaging–partial least squares (WA-PLS) regression and a Bayesian multinomial regression method. We apply these transfer functions to a set of fossil pollen data from monsoonal China for quantit…
Pollen- and charcoal-based evidence for climatic and human impact on vegetation in the northern edge of Wuyi Mountains, China, during the last 8200 years
Pollen and charcoal records derived from the sediment core of Lantianyan (LTY) peat bog, Northern Wuyi Mountain chains, eastern subtropical China, provide valuable information of landscape evolution caused by both climatic variation and anthropogenic activities over the past 8200 years. Our results reveal fluvial and lacustrine deposition between c. 8200 and 5600 cal. yr BP. The high proportion of pollen from evergreen broadleaved forests (e.g. Q…
New evidence for Neolithic rice cultivation and Holocene environmental change in the Fuzhou Basin, southeast China
A late Holocene record of vegetation and fire from the Amur Basin, far-eastern Russia
Holocene temperature and precipitation variability on the central Tibetan Plateau revealed by multiple palaeo-climatic proxy records from an alpine wetland sequence
This study has reconstructed the Holocene environmental history of central Tibetan Plateau, a transitional area between monsoon-dominated Asia and Westerlies-dominated Asia, to examine the interplay between the two circulation systems and effects of other potential mechanisms on the temporal variability of Holocene climatic conditions in the study area. Specifically, this study has produced a twin record of palaeo-hydrology and palaeo-temperature…
The environmental conditions of MIS5 in the northern South China Sea, revealed by n-alkanes indices and alkenones from a 39 m-long sediment sequence
Holocene fire and forest histories in relation to climate change and agriculture development in southeastern China
Pollen morphology of selected crop plants from southern China and testing pollen morphological data in an archaeobotanical study
Regional land cover changes of the last 6,500 years in middle and southern subtropical China
Quantitative Land-Cover Reconstructions for China over the Past 6000 Years
Validation of relative pollen productivities for major tropical plant taxa
Dynamic, high-resolution poverty measurement in data-scarce environments
Forest transformation and human impact in pearl river delta, south China, during the last 6000 cal yr BP
Geology and Paleoclimatology Research (24 obras) · Geography (20 obras) · Geology (16 obras) · Physical geography (16 obras) · Pollen (14 obras) · Ecology (13 obras) · Holocene (13 obras) · Biology (11 obras) · Archaeology (9 obras) · Archaeology and ancient environmental studies (9 obras)