A transfer-function model developed from an extensive surface-pollen data set in northern China and its potential for palaeoclimate reconstructions
Bibliographic Data
| ID | 12265693 |
|---|---|
| Authors | Yuecong Li (0000-0002-9789-4367, Hebei Normal University), Qinghai Xu (0000-0003-2518-3520, Hebei Normal University, corresponding author), Jinsong Liu (0000-0003-0812-2099, Hebei Normal University), Xiaolan Yang (0000-0003-4189-0882, Hebei Institute of Geography, Shijiazhuang, 050011, PR China), Takeshi Nakagawa (0000-0001-5533-3169, Department of Geography, University of Newcastle, Newcastle upon Tyne NE17RU, UK) |
| Year | 2007 |
| Volume | 17 |
| Issue | 7 |
| Pages | 897-905 |
| Publication date | 2007-11-01 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | The Holocene (JOURNAL) |
| Journal identifiers | ISSN: 0959-6836 • E-ISSN: 1477-0911 |
| Publisher | SAGE Publishing (PUBLISHER • US) |
| DOI | 10.1177/0959683607082404 |
| OpenAlex | W2035788645 |
| Language | EN |
| Citations received | 10 |
| References cited | 22 |
A total of 237 surface soil pollen samples were collected from less disturbed zonal communities, and a new surface pollen data set has been established in northern China. Pollen—climate parameter transfer functions using weighted-averaging regression and calibration partial least squares (WA-PLS) model as a tool to reconstruct past climate changes from pollen data, were tested with this new surface pollen data set. The results of cross-validation showed that the method worked very well with precipitation ( R = 0.94, R 2 jack = 0.89, RMSEP jack = 69 mm, the safe dynamic range of the reconstruction was 40 mm~800 mm) and worked well with temperature ( T ann : R = 0.84, R 2 jack = 0.71, RMSEP jack = 2.0°C, the safe dynamic range of the reconstruction was −4°C~13°C; MT wa : R = 0.79, R 2 jack = 0.63, RMSEP jack = 2.5°C, and the safe dynamic range of the reconstruction was 8°C~26°C), indicating that the surface pollen data set and WA-PLS reconstruction technique in this paper have strong potential for palaeoclimatic reconstruction
Biology · Botany · Calibration · Data set · Geography · Meteorology · Partial least squares regression · Pollen · Precipitation · Range (aeronautics · Statistics · Environmental Science · Geology and Paleoclimatology Research · Landslides and related hazards · Materials Science · Mathematics · Tree-ring climate responses · Geology
Assessing the Importance of Climate Variables for the Spatial Distribution of Modern Pollen Data in China
Quantitative reconstruction of Holocene precipitation changes in southern Patagonia
Modern pollen–climate relationships and their application for pollen-based quantitative climate reconstruction of the mid-Holocene on the southern Korean Peninsula
Human impact, soil erosion, and vegetation response lags to climate change
Revisit the Medieval Warm Period and Little Ice Age in Proxy Records from Zemu Glacier Sediments, Eastern Himalaya
Vegetation and climate reconstructions on different time scales in China
East Asian summer monsoon precipitation variations in China over the last 9500 years
Late Holocene climate change and anthropogenic activities in north Xinjiang
A modern pollen–temperature calibration data set from Korea and quantitative temperature reconstructions for the Holocene
Pollen–vegetation–climate relationships in some desert and desert-steppe communities in northern China
Late- and Postglacial Climatic Change in the Northern Midwest, USA
Multidimensional scaling as a research tool in quaternary palynology
A Theory of Gradient Analysis
Detrended correspondence analysis
Weighted averaging partial least squares regression (WA-PLS)
Phytoliths as quantitative indicators for the reconstruction of past environmental conditions in China I
Correlation between climate events in the North Atlantic and China during the last glaciation
D.G. Frey and E.S. Deevey Review 1
A 140,000-year continental climate reconstruction from two European pollen records
Diatoms and pH reconstruction
Climate changes in northern China since the late Pleistocene and its response to global change
| Unique citing works | 10 |
|---|---|
| Citations per year | 0,59 |
| Citation span | 2009 - 2023 (15) |
| Citation velocity | historical |
| Highly cited | No |
| Citation types | Neutral: 8 |