4.7 Article

Pollen-based reconstruction of total land-cover change over the Holocene in the temperate steppe region of China: An attempt to quantify the cover of vegetation and bare ground in the past using a novel approach

期刊

CATENA
卷 214, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.catena.2022.106307

关键词

REVEALS; Modern analogue technique MAT; Pollen in surface soils; Pollen in surface lake sediments; MODIS vegetation data; Lake Daihai

资金

  1. National Natural Science Foundation of China [41630753, 41931181, U20A20116]
  2. NSFC-STINT [NSFC: 41611130050, STINT: CH2015-6227]
  3. Hebei Key Laboratory of Environmental Change and Ecological Construction and the Key Discipline Fund Project in Hebei province
  4. Swedish strategic research area MERGE (ModElling the Regional and Global Earth system)
  5. Faculty of Health and Life Science of Linnaeus University, Kalmar-Vaxjo, Sweden

向作者/读者索取更多资源

Fossil pollen data are essential for reconstructing ancient vegetation and land-cover changes. This study combines Sugita's REVEALS model and the Modern Analogue Technique (MAT) to estimate and reconstruct past actual vegetation cover using pollen data. The results are validated by comparing them with modern data.
Fossil pollen data are essential for reconstructing ancient vegetation and land-cover changes. Sugita's REVEALS model is the best method to estimate regional plant cover (in percentage cover) using pollen data from lakes. Such reconstructions imply that the sum of all plants' cover is 100%. However, land cover is not always represented by vegetation alone, the area of bare ground can be significant in many types of biomes, e.g., in alpine or steppe regions. Here we define total land cover as the sum of vegetation cover (VegC) and bare ground (BareC). In this study, we use the relationship between tree pollen percentages and both tree cover (TreeC) and VegC (=TreeC + herb cover (HerbC)) based on a dataset of modern pollen assemblages and related total land cover. This relationship is applied to estimate past actual vegetation cover (a-VegC) from fossil pollen percentages using the Modern Analogue Technique (MAT). The REVEALS (RV) model can then be applied to the same fossil pollen records to estimate regional cover of individual plant taxa (RV PlantC; e.g., RV PinusC, etc.), total tree cover (RV-TreeC) and total herb cover (RV-HerbC). These cover values can then be converted into RV aPlantC, RV a-TreeC and RV a-HerbC using the MAT-reconstructed a-VegC (e.g., RV PinusC x MAT a-VegC = RV aPinusC; RV-TreeC x MAT a-VegC = RV a-TreeC, etc.). The results of leave-one-out cross-validation indicates that the MAT reconstructions using the modern pollen assemblages provide values of a-TreeC, a-HerbC and BareC mostly very similar to the modern vegetation data. We further tested the method using pollen assemblages from lake surface sediments of 11 lakes and the results also suggest a good performance of MAT-based reconstruction. We then applied the proposed method (MAT-REVEALS) to four Holocene pollen records available from the study area to evaluate the feasibility of the strategy to reconstruct past actual plant cover. The results suggest that the method provides plausible estimates of vegetation cover for the sub-regions within the study area. The results from Lake Daihai over the last 10,000 years BP are interpreted and discussed in more details to evaluate the effects of possible departures from the approach assumptions.

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