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CP | Articles | Volume 15, issue 4
Clim. Past, 15, 1503–1536, 2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Paleoclimate data synthesis and analysis of associated uncertainty...

Clim. Past, 15, 1503–1536, 2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 08 Aug 2019

Research article | 08 Aug 2019

Pollen-based quantitative land-cover reconstruction for northern Asia covering the last 40 ka cal BP

Pollen-based quantitative land-cover reconstruction for northern Asia covering the last...
Xianyong Cao1,a, Fang Tian1, Furong Li2, Marie-José Gaillard2, Natalia Rudaya1,3,4, Qinghai Xu5, and Ulrike Herzschuh1,4,6 Xianyong Cao et al.
  • 1Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Research Unit Potsdam, Telegrafenberg A43, Potsdam 14473, Germany
  • 2Department of Biology and Environmental Science, Linnaeus University, Kalmar 39182, Sweden
  • 3Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences, pr. Akad. Lavrentieva 17, Novosibirsk 630090, Russia
  • 4Institute of Environmental Science and Geography, University of Potsdam, Karl-Liebknecht-Str. 24, 14476 Potsdam, Germany
  • 5College of Resources and Environment Science, Hebei Normal University, Shijiazhuang 050024, China
  • 6Institute of Biochemistry and Biology, University of Potsdam, Karl-Liebknecht-Str. 24, Potsdam 14476, Germany
  • apresent address: Key Laboratory of Alpine Ecology, CAS Center for Excellence in Tibetan Plateau Earth Sciences, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
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We collected the available relative pollen productivity estimates (PPEs) for 27 major pollen taxa from Eurasia and applied them to estimate plant abundances during the last 40 ka cal BP (calibrated thousand years before present) using pollen counts from 203 fossil pollen records in northern Asia (north of 40 N). These pollen records were organized into 42 site groups and regional mean plant abundances calculated using the REVEALS (Regional Estimates of Vegetation Abundance from Large Sites) model. Time-series clustering, constrained hierarchical clustering, and detrended canonical correspondence analysis were performed to investigate the regional pattern, time, and strength of vegetation changes, respectively. Reconstructed regional plant functional type (PFT) components for each site group are generally consistent with modern vegetation in that vegetation changes within the regions are characterized by minor changes in the abundance of PFTs rather than by an increase in new PFTs, particularly during the Holocene. We argue that pollen-based REVEALS estimates of plant abundances should be a more reliable reflection of the vegetation as pollen may overestimate the turnover, particularly when a high pollen producer invades areas dominated by low pollen producers. Comparisons with vegetation-independent climate records show that climate change is the primary factor driving land-cover changes at broad spatial and temporal scales. Vegetation changes in certain regions or periods, however, could not be explained by direct climate change, e.g. inland Siberia, where a sharp increase in evergreen conifer tree abundance occurred at ca. 7–8 ka cal BP despite an unchanging climate, potentially reflecting their response to complex climate–permafrost–fire–vegetation interactions and thus a possible long-term lagged climate response.

1 Introduction
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High northern latitudes such as northern Asia experience above-average temperature increases in times of past and recent global warming (Serreze et al., 2000; IPCC, 2007), known as polar amplification (Miller et al., 2010). Temperature rise is expected to promote vegetation change as the vegetation composition in these areas is assumed to be controlled mainly by temperature (J. Li et al., 2017; Tian et al., 2018). However, a more complex response can occur mainly because vegetation is not linearly related to temperature change (e.g. due to resilience, stable states, or time-lagged responses; Soja et al., 2007; Herzschuh et al., 2016) and/or vegetation is only indirectly limited by temperature while other temperature-related environmental drivers such as permafrost conditions are more influential (Tchebakova et al., 2005).

Such complex relationships between temperature and vegetation may help explain several contradictory findings of recent ecological change in northern Asia. For example, simulations of vegetation change in response to a warmer and drier climate indicate that steppe should expand in the present-day forest–steppe ecotone of southern Siberia (Tchebakova et al., 2009) but, contrarily, pine forest has increased during the past 74 years, probably because the warming temperature was mediated by improved local moisture conditions (Shestakova et al., 2017). In another example, evergreen conifers, which are assumed to be more susceptible to frost damage than Larix, expanded their distribution by 10 % during a period with cooler winters from 2001 to 2012, while the distribution of Larix forests decreased by 40 % on the West Siberian Plain as revealed by a remote sensing study (He et al., 2017). Additionally, some field studies and dynamic vegetation models infer a rapid response of the treeline to warming in northern Siberia (e.g. Moiseev, 2002; Soja et al., 2007; Kirdyanov et al., 2012), but combined model- and field-based investigations of larch stands in north-central Siberia reveal only a densification of tree stands, not an areal expansion (Kruse et al., 2016; Wieczorek et al., 2017).

These findings on recent vegetation dynamics that contradict a straightforward vegetation–temperature relationship may be better understood in the context of vegetation change over longer timescales. Synthesizing multi-record pollen data is the most suitable approach to investigate quantitatively the past vegetation change at broad spatial and long temporal scales. Broad spatial scale pollen-based land-cover reconstructions have been made for Europe (e.g. Mazier et al., 2012; Nielsen et al., 2012; Trondman et al., 2015) and temperate China (Li, 2016) for the Holocene. However, vegetation change studies in northern Asia are restricted to biome reconstructions (Tarasov et al., 1998, 2000; Bigelow et al., 2003; Binney et al., 2017; Tian et al., 2018), which do not reflect compositional change. Syntheses of pure pollen percentage data are not appropriate due to differences in pollen productivity, which may result in an overestimation of the strength of vegetation changes (Wang and Herzschuh, 2011). This might be particularly severe when strong pollen producers such as pine (Mazier et al., 2012) invade areas dominated by low pollen producers such as larch (Niemeyer et al., 2015). Marquer et al. (2014, 2017) also demonstrated the strength of pollen-based REVEALS (Regional Estimates of Vegetation Abundance from Large Sites) estimates of plant abundance in studies of Holocene vegetation change and plant diversity indices in Europe. Accordingly, syntheses of quantitative plant cover derived from the application of pollen productivity estimates (PPEs) to multiple pollen records (Trondman et al., 2015; Li, 2016) should be a better way to investigate Late Glacial and Holocene vegetation change in northern Asia.

In this study, we employ the taxonomically harmonized and temporally standardized fossil pollen datasets available from eastern continental Asia (Cao et al., 2013, 2015) and Siberia (Tian et al., 2018) covering the last 40 ka cal BP (henceforth abbreviated to ka). We compile all the available PPEs from Eurasia and use the mean estimate for each taxon. Finally, we quantitatively reconstruct plant cover using the REVEALS model (Sugita, 2007) for 27 major taxa at 18 key time slices. We reveal the nature, strength, and timing of vegetation change in northern Asia and its regional peculiarities, and discuss the driving factors of vegetation change.

2 Data and methods
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2.1 Fossil pollen data process

The fossil pollen records were obtained from the extended version of the fossil pollen dataset for eastern continental Asia containing 297 records (Cao et al., 2013, 2015) and the fossil pollen dataset for Siberia with 171 records (Tian et al., 2018). For the 468 pollen records, pollen names were harmonized to genus level for arboreal taxa and family level for herbaceous taxa, and age-depth models were re-established using the Bayesian age-depth modelling (further details are described in Cao et al., 2013). We selected 203 pollen records from lacustrine sediments (110 sites) and peat (93 sites) north of 40 N, with chronologies based on ≥3 dates and a <500-year-per-sample temporal resolution generally, following previous studies (Mazier et al., 2012; Nielsen et al., 2012; Fyfe et al., 2013; Trondman et al., 2015). Out of the 203 pollen records, 170 sites (83 from lakes, 87 from bogs) have original pollen counts, while in the other 33 sites only pollen percentages are available. Due to overall low site density, we decided to include these data. The pollen counts were back-calculated from percentages using the terrestrial pollen sum indicated in the original publications. Detailed information (including location, data quality, chronology reliability, and data source) on the selected sites is presented in Fig. A1 and Table A1 in the Appendix.

Table 1Selected time windows.

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We selected 18 key time slices for reconstruction (Table 1) to capture the general temporal patterns of vegetation change during the last 40 ka, i.e. 40, 25, 21, 18, 14, and 12 ka during the late Pleistocene and 1000-year resolution (500-year time windows around each millennium, i.e. 0.7–1.2, 1.7–2.2 ka, etc.) during the Holocene. For the 0 ka time slice, the ca. 150-year time window (<0.1 ka) was set to represent the modern vegetation. Since few pollen records have available samples at the 0 ka time slice, the 0.2 and 0.5 ka time slices covered a 250-year or 350-year time window (0.1–0.35 and 0.35–0.7 ka, respectively) to represent the recent vegetation, following the strategy and time windows implemented for Europe (Mazier et al., 2012; Trondman et al., 2015). For the last glacial period, even broader time windows were chosen to offset the sparsely available samples (Table 1). Pollen counts of all available samples within one time window were summed up to represent the total pollen count for each time slice. In this study, we selected 27 major pollen taxa (with available PPE, pollen productivity estimate, and values) that form dominant components in both modern vegetation communities and the fossil pollen spectra and reconstruct their abundances in the past vegetation (Table 2).

Table 2Fall speed (FS) of pollen grains and mean relative pollen productivity estimate (PPE) with standard error (SE) for the 27 selected taxa. Plant functional type (PFT) assignment is according to previous biome reconstructions (Tarasov et al., 1998, 2000; Bigelow et al., 2003; Ni et al., 2010).

a Eisenhut (1961); b Gregory (1973); c Li et al. (2017); d Broström et al. (2004); e Sugita et al. (1999); f Abraham and Kozáková (2012); g Broström (2002); h Xu et al. (2014); i Bunting et al. (2013).

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2.2 The REVEALS model setting

The REVEALS model assumes the PPEs of pollen taxa are constant variables over the target period and requires parameter inputs including sediment basin radius (m), fall speed of pollen grain (FS, m s−1), and PPE with standard error (SE; Sugita, 2007). The areas of the 110 lakes were obtained from descriptions in original publications and validated by measurements on Google Earth. Their basin radii were back-calculated from their areas assuming a circular shape. There are 83 large lakes (radius >390 m; following Sugita, 2007) in our dataset with a fairly even distribution across the study area (Figs. 1 and A1), which helps ensure the reliability of the regional vegetation estimations (Sugita, 2007; Mazier et al., 2012). Only 18 bogs have published descriptions about their size and it is infeasible to measure them on Google Earth because of unclear boundaries. A test run showed that using different bog radii (i.e. 5, 10, 20, 50, 100, 200, and 500 m) did not significantly affect the REVEALS estimates (Fig. A2), hence a standard (moderate size) radius of 100 m was set for all bogs.

We collected available PPEs for the 27 selected pollen taxa from 20 studies in Eurasia (Table A2). We calculated the mean PPE from all available PPE values, but excluded records with PPE  SE (Mazier et al., 2012). We included these PPEs for various species in the mean PPE calculation for their family or genus. For simplification, we did not evaluate the values or select PPE values following consistent criteria as was done in Europe (Mazier et al., 2012). Instead, we used the original values from the studies included in Mazier et al. (2012) and added new PPE values from Europe published since the synthesis by Mazier et al. (2012). SE of the mean PPE was estimated using the delta method (Stuart and Ord, 1994). Fall speeds for each of the 27 pollen taxa were retrieved from previous studies (Table 2).

The REVEALS model generally performs best with pollen records from large lakes, although multiple pollen records from small lakes and bogs (at least two sites) can also produce reliable results where large lakes are absent (Sugita, 2007; Trondman et al., 2016). Here, due to the sparse distribution of available sites, we divided the 203 sites into 42 site groups, based on criteria of geographic location, vegetation type (vegetation zone map modified from Tseplyayev, 1961; Dulamsuren et al., 2005; Hou, 2001), climate (based on modern precipitation and temperature contours), and permafrost (Brown et al., 1997) following the strategy of Li (2016); the pollen data within one site group should be of similar components and temporal patterns. To ensure the reliability of REVEALS estimates of plant cover, each group includes at least one large lake or two small sites (small lakes or bogs; Fig. 1; Table A3).

Figure 1Distribution of the 42 site groups together with the modern vegetation zones and permafrost extent in northern Asia. The vegetation-zone map modified from Tseplyayev (1961), Dulamsuren et al. (2005), and Hou (2001) includes the following. A: tundra, B: taiga forest, C: temperate mixed conifer–deciduous broadleaved forest, D: temperate steppe, E: semi-desert and desert; and F: warm-temperate deciduous forest.

The REVEALS model was run with a mean wind speed set to 3 m s−1 and neutral atmospheric conditions following Trondman et al. (2015), and the maximum distance of regional vegetation Zmax was set to 100 km. The lake and bog sites were reconstructed using the models of pollen dispersal and deposition for lakes (Sugita, 1993) and bogs (Prentice, 1985), respectively, in REVEALS version 5.0 (Shinya Sugita, unpublished data). The mean estimate of plant abundances from lakes and bogs was calculated for each of the 42 site groups, which includes both sediment types (using the computer program; Shinya Sugita, unpublished data). Finally, the 27 taxa were assigned to seven plant functional types (PFT; Table 1) following the PFT definitions for China and Siberia (Tarasov et al., 1998, 2000; Bigelow et al., 2003; Ni et al., 2010; Tian et al., 2018), with the restriction that each pollen taxon is attributed to only one PFT according to the strategy of Li (2016) (Table 2).

2.3 Numerical analyses of reconstruction

The abundance variations in the seven PFTs during the Holocene (time slices between 12 and 1 ka) from 36 site groups were used in a clustering analysis. Six site groups had to be excluded from the analysis due to poor coverage of time slices (G1, G5, G17, G19, G27, G42). For site groups with <3 missing time slices during the Holocene (G3, G16, G26, G32, G33, G35, G38, G39, G41), linear interpolation was employed to estimate the PFT abundances for the missing time slices. Time-series clustering for the three-way dataset was performed to generate a distance matrix among the site groups using the tsclust function in the dtwclust package (Sarda-Espinosa, 2018) in R 3.4.1 (R Core Team, 2017). The distance matrix was employed in hierarchical clustering (using the hclust function in R) to cluster the site groups. Constrained hierarchical clustering (using chclust function in rioja package version 0.9–15.1; Juggins, 2018) was used to determine the timing of primary vegetation changes (i.e. the first split) in each site group. A change was considered to be significant when the split passed the broken-stick test. The amount of PFT compositional change (turnover) through time during the period between 12 and 1 ka for the 36 site groups (time slices cover entire period) was estimated by detrended canonical correspondence analysis (DCCA) for each site group (ter Braak, 1986) using CANOCO 4.5 (ter Braak and Šmilauer, 2002).

3 Results
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3.1 Large-scale pattern

On a glacial–interglacial scale, marked temporal changes in the occurrence and abundance of PFTs are revealed, in particular the high cover of tree PFTs during the Holocene as opposed to the widespread open landscape during the glacial period. In contrast, vegetation changes in northern Asia within the Holocene are rather minor with only slight changes in PFT abundances. Cluster analyses of grouped vegetation records from the Holocene find five clusters (Fig. A3). Their spatial distribution is largely consistent with the distribution of modern vegetation types as characterized by certain PFTs. (1) Records from the forest–steppe ecotone (e.g. G12, G21; Fig. 2a) in north-central China and the Tianshan (the mentioned geographic locations are indicated in Fig. A4) have high tree PFTs during the middle Holocene. (2) Areas in southern and south-western Siberia and north-eastern China were covered by cool-temperate mixed forest or light taiga with a high diversity of trees throughout the Holocene (e.g. G2, G7, G14, G29; Fig. 2b). (3) The West Siberian Plain and south-eastern Siberia that are presently covered by open dark taiga forests (e.g. G8, G9, G33; Fig. 2c) had an even higher abundance of evergreen conifer trees during the middle Holocene than at present. (4) Larix formed light taiga forests in central Yakutia throughout the Holocene (e.g. G25, G26; Fig. 2d). (5) Northern Siberia, which is currently covered by tundra formed by boreal shrubs and herbs, had a higher share of tree PFTs during the middle Holocene (e.g. G28, G39; Fig. 2e).

The turnover in PFT composition is <0.7 SD units in almost all site groups, except G8 (0.88 SD), G9 (0.73 SD), and G24 (0.76 SD), indicating only slight vegetation change during the Holocene (Fig. 3). The three site groups with higher turnover show a distinct transition from light taiga to dark taiga in the middle Holocene (at ca. 8 ka). The significant primary vegetation changes (pass the broken-stick test) occur during different intervals in each site group. Overall, the middle Holocene (including 8.5, 7.5, 6.5, and 5.5 ka time slices) has the highest frequency of primary vegetation changes. Records from inland areas such as the West Siberian Plain, central Yakutia, and northern Mongolia are characterized by relatively many middle-Holocene splits. There are seven site groups whose primary vegetation changes during the early Holocene (including 11.5, 10.5, and 9.5 ka time slices), and most of them from the south-eastern coastal part of the study area. Only three site groups have late-Holocene primary vegetation changes (Fig. 3).

Figure 2Temporal changes in plant functional type (PFT) cover, as proportions, for the site groups from the warm temperate forest margin zone (a); cool-temperate mixed forest and taiga forest (b); dark taiga forest (c); light taiga forest and taiga–tundra ecotone (d); tundra and taiga–tundra ecotone (e). PFT I: evergreen conifer tree; PFT II: deciduous conifer tree; PFT III: boreal deciduous tree; PFT IV: temperate deciduous tree; PFT V: boreal shrub; PFT VI: arid-tolerant shrub and herb; and PFT VII: steppe and tundra forb.

3.2 Warm temperate forest margin zone in vicinity of Tianshan and north-central China (G6, G12, G13, G16, G21, G22)

Six site groups from the warm temperate forest–steppe transition zone (G6, G21, G22) and from the lowlands adjacent to mountainous forest in arid central Asia (G12, G13, G16) are clustered together (Fig. 3). Our results indicate that these areas, which are now dominated by arid-tolerant shrub and steppe species, had more arboreal species, mainly evergreen conifer tree taxa, in the middle Holocene (Fig. 2a). For example, north-central China (G21) has a marked mid-Holocene maximum in forest cover (7–4 ka; mean 51 %). However, certain peculiarities are noted: open landscape is reconstructed between 14 and 7 ka in northern Kazakhstan (G6), followed by an abundance of evergreen conifer trees and an increase in boreal deciduous trees that maintain high values (mean 30 %) after 7 ka. In the eastern branch of the Tianshan (G12), evergreen conifer trees are highly abundant from 10 to 7 ka and after 2 ka, while low abundance occurs from 14 to 11 ka and from 6 to 3 ka. In the Gobi desert near the Tianshan (G16) there was an even higher abundance of arid-tolerant species with no notable temporal trend in abundance of arboreal species. We assume that the high arboreal cover at site groups G13 and G22 at 14 and 12 ka originates from riverine transport and therefore exclude them from further analyses.

3.3 Cool-temperate mixed forest and taiga forest in southern and south-western Siberia and north-eastern China (G2, G7, G14, G15, G18, G29, G30, G31)

Eight site groups located in (or near) the temperate mixed conifer–deciduous broadleaved forest zone (G2, G29, G30, G31) and taiga–steppe transition zone (G7, G14, G15, G18) show similar PFT compositions and temporal evolutions. At these sites, evergreen conifer tree is the dominant PFT intermixed with other arboreal PFTs, such as deciduous conifers (Larix) in the Altai Mts. and northern Mongolia, and/or temperate deciduous trees in north-eastern China (Fig. 2b).

Evergreen conifer tree is the dominant PFT at 40, 25, and 21 ka in the southern part of north-eastern China (G29), Larix then becomes the dominant taxa at 14 and 12 ka, and temperate deciduous trees increase thereafter and maintain high cover between 11 and 3 ka. After 2 ka, evergreen conifer trees increase to 32 % on average while temperate deciduous trees decrease to 18 % on average. While arboreal abundance is lower in the northern part of north-eastern China (G30, G31) than in the southern part (G29), it shows a similar temporal pattern (Fig. 2b).

Figure 3Clustering results of the 36 site groups represented by the colour of the boxes, with the age of primary vegetation changes (middle row of each box; data in brackets mean the hierarchical clustering failed the broken-stick test) and the compositional change (turnover; lower row) during the Holocene.

Open landscape is revealed for the southern Ural region (G2) with high abundances of herbaceous species at 14 ka. The cover of Larix and evergreen conifer trees increases after 12 ka and maintains high values thereafter with no notable temporal trend (Fig. 2b).

In the taiga–steppe transition zone, Larix is the dominant arboreal taxon, particularly in the northern Altai Mts. and northern Mongolia (G15, G18). Open landscapes are inferred at 40, 21, and 12 ka on the southern West Siberian Plain (G7); cover of Larix increases at 11 ka and evergreen conifer trees increase from 9 ka and become the dominant forest taxon after 4 ka. The temporal pattern of evergreen conifer trees in the Altai Mts. (G14) is similar to the southern West Siberian Plain, although Larix maintains high abundances into the late Holocene. Relative to the Altai Mts., the abundance of evergreen conifer trees for all time windows are lower in the area north of the Altai Mts. and in northern Mongolia (G15, G18), but their temporal change patterns are consistent with those of the Altai Mts. (G14; Fig. 2b).

3.4 Dark taiga forest in western and south-eastern Siberia (G3, G4, G8, G9, G20, G32, G33, G34)

Site groups with dark taiga forest from western Siberia (G3, G4, G8, G9), the Baikal region (G20), and south-eastern Siberia (G32, G33, G34) form one cluster sharing similar PFT compositions dominated by evergreen conifer trees, with Larix and boreal broadleaved shrubs as the common woody taxa during the Holocene (Fig. 2c).

On the West Siberian Plain (G8, G9), high cover of Larix is reconstructed during the early Holocene as well as high woody cover since the middle Holocene formed by evergreen conifer trees and boreal shrubs. In the Ural region (G3, G4), evergreen conifer trees dominate the arboreal species throughout the Holocene. The absence of Larix in the early Holocene in this Ural region is a notable difference to the West Siberian Plain (Fig. 2c).

In the Baikal region (G20), a relatively closed landscape is revealed at 40 ka; openness then increases to >95 % at 25 and 21 ka. Since 14 ka, woody cover increases as shown by a notable rise in evergreen conifer trees from 14 to 8 ka and by increases of Larix after 7 ka (Fig. 2c).

In south-eastern Siberia (G32, G34), arboreal abundance is high in the early and late Holocene, but low in the middle Holocene. South of Sakhalin Island (G33), a closed landscape is revealed between 40 and 1 ka with >80 % woody cover. Evergreen conifer tree PFT has lower cover than boreal shrub PFT at 25 and 21 ka but increases in abundance around 14 ka rising to 83 % on average between 11 and 3 ka, and reduces thereafter (Fig. 2c).

3.5 Light taiga forest in north-western Siberia and central Yakutia (G10, G23, G24, G25, G26)

Plant composition of this cluster is dominated by Larix with high arboreal cover during the Holocene. Evergreen conifer trees are present at ca. 15 % cover between 11 and 2 ka, with high arboreal values (mean 73 %) during the Holocene in north-western Siberia (G10). In central Yakutia (G23, G24, G25), evergreen conifer trees increase markedly from ca. 8, 6, and 7 ka, respectively, and maintain high cover thereafter, with ca. 60 % arboreal cover throughout the Holocene. Evergreen conifer trees are almost absent in the taiga–tundra ecotone (G26; Fig. 2d).

3.6 Tundra on the Taymyr Peninsula and taiga–tundra ecotone in north-eastern Siberia (G11, G28, G35, G36, G37, G38, G39, G40, G41)

Plant compositions of this cluster are characterized by high abundances of boreal shrubs and tundra forbs. Larix is the only tree species on the Taymyr Peninsula (G11) and its abundance increases from 18 % at 14 ka to 60 % at 10 ka, and then decreases to 18 % at 5 ka. The landscape of the north Siberian coast (G28) is dominated by shrub tundra from 14 to 10 ka, then Larix increases sharply and maintains high values between 9 and 6 ka. After 5 ka, Larix reduces, and shrub tundra becomes the dominant landscape again (Fig. 2e).

In north-eastern Siberia, arboreal cover shows a decreasing trend from southerly site groups (G35, G36, G37; Fig. 2d) to northerly ones (G40, G38, G39, G41) following the increasing latitude. In the Olsky District, temporal patterns of vegetation changes in G37 are consistent with G36, with stable vegetation during the Holocene and increases in evergreen conifer tree abundance from ca. 9 ka. Arboreal composition on the southern Kamchatka Peninsula (G35) is dominated by boreal deciduous trees during the first stage of the Holocene, followed by rising abundances of Larix and evergreen conifer trees from 5 ka.

In north-eastern Siberia (G40, G38, G39, G41), the landscape is dominated by forb tundra with sparse shrubs between 40 and 21 ka; the cover of shrubs increases at 14 ka and arboreal cover (dominated by boreal deciduous trees) increases in the early Holocene (11 or 10 ka). Shrubs maintain a high abundance throughout the Holocene, while trees peak between 10 and 2 ka generally (Fig. 2e).

4 Discussion
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4.1 Land-cover changes and potential biases

The overall patterns of pollen-based REVEALS estimates of land cover are generally consistent with previous vegetation reconstructions. Although only a few site groups cover the period from 40 to 21 ka, a consistent vegetation signal indicates that relatively closed landscapes occurred in south-eastern Siberia, north-eastern China, and the Baikal region (Fig. 2), while most of Siberia was rather open, particularly around 21 ka (Fig. 2). These findings are consistent with previous pollen-based (Tarasov et al., 1998, 2000; Bigelow et al., 2003; Binney et al., 2017; Tian et al., 2018) and model-estimated biome reconstructions (Tian et al., 2018). During the late Pleistocene (40, 25, 21, 14 ka), steppe PFT abundance was high in central Yakutia and north-eastern Siberia (e.g. G25, G36, G37, G39, G40, G41), which may reflect the expansion of tundra–steppe, consistent with results from ancient sediment DNA which reveal abundant forb species during the period between 46 and 12.5 ka on the Taymyr Peninsula (Jørgensen et al., 2012). The tundra–steppe was replaced by light taiga in southern Siberia and by tundra in northern Siberia at the beginning of Holocene or the last deglaciation, which is consistent with ancient DNA results (forbs-dominated steppe-tundra; Willerslev et al., 2014).

During the Holocene, reconstructed land cover for each site group is generally consistent with their modern vegetation. The slight vegetation changes are represented by changes in PFT abundances rather than by changes in PFT presence or absence. Minor changes are also indicated in the cluster analysis, which shows that plant compositions and their temporal patterns are consistent among the site groups within the same modern vegetation zone (Fig. 3). PFT datasets from only 19 site groups pass the broken-stick test for clustering analysis, and most of them have only one significant vegetation change, further supporting the case that only slight changes occurred during the Holocene in northern Asia. In addition, the low total amount of PFT change (turnover) over the Holocene for most site groups supports the view of slight temporal changes in land cover.

Vegetation turnover on the Tibetan Plateau inferred from pollen percentages is documented to overestimate the strength of vegetation changes (Wang and Herzschuh, 2011). This matches with our results. In central Yakutia, the pollen percentage data indicate a strong vegetation change during the middle Holocene, represented by a sharp increase in Pinus pollen, but the strength of the vegetation change is overestimated because of the high PPE of Pinus. The PPE-corrected arboreal abundances in central Yakutia after ca. 7 ka with ca. 70 % Larix and ca. 10 % Pinus are consistent with modern light taiga (Katamura et al., 2009). Furthermore, the absence of Pinus macrofossils in central Yakutia throughout the Holocene (Binney et al., 2009) also suggests a restricted distribution of Pinus, possibly to sandy places such as river banks (Isaev et al., 2010).

Pollen-based turnover estimates from southern Norway range from 0.84 to 1.3 SD (mean 1.02 SD) for 10 Holocene pollen spectra (Birks, 2007), and from northern Europe from 0.01 (recent) to 0.99 (start of the Holocene) SD for three sites (N Sweden, NW and SE Finland) (Marquer et al., 2014). Moreover, the REVEALS-based turnover estimates (0.3–1) for northern Europe are significantly higher than the pollen-based one (0.2–0.8) from 11 to 5.5 kyr BP. The same is true for all other regions studied by Marquer et al. (2014) in north-western Europe, and the turnover estimates (pollen- and REVEALS-based) are generally higher at lower latitudes from southern Sweden down to Switzerland and eastwards to Britain and Ireland. These European values are higher than our REVEALS-based turnover estimates (from 0.37 to 0.88 SD, mean 0.66 SD; G3, G8, G9, G23, G24, G25, G36, G37) from a similar latitudinal range (Fig. 3). The fewer parameters used in the turnover calculations for northern Asia (PFTs) compared to Europe (pollen taxa) is a potential reason for the lower turnover obtained in this study. In addition, the PPE-based transformation from pollen percentages to plant abundances may reduce the strength of vegetation changes (Wang and Herzschuh, 2011). Aside from the methodological aspects, the lower turnover in northern Asia may, at least partly, originate from differences in the environmental history between northern Europe compared with northern Asia, i.e. glaciation followed by postglacial re-vegetation vs. non-glaciated areas with trees in refugia, respectively, and a maritime climate with temperature-limited vegetation distribution vs. a continental climate with temperature- and moisture-limited vegetation.

We consider the REVEALS-based regional vegetation-cover estimations in this study as generally reliable with reasonable standard errors (Fig. A5) thanks to the thorough selection of records with high-quality pollen data and reliable chronologies. In addition, the landscape reconstructions are generally consistent with previous syntheses of past vegetation change (e.g. Tian et al., 2018) and known global climate trends (Marcott et al., 2013), plus the clustering results of PFT abundance are consistent with modern spatial vegetation patterns. That said, this study faced two major methodological challenges, discussed below, that may reduce the reliability of the obtained quantitative land-cover reconstructions: (1) the low number of PPEs and their origin and (2) restrictions with respect to the number, distribution, and type of available sites.

Twenty PPE sets were used which mostly originate from Europe and temperate northern China. The available PPEs were estimated from various environmental and ecological settings, which might cause regional differences in each PPE. And PPEs of different species within one family or genus were included in our mean PPE calculation for the family or genus, ignoring the inter-species differences. Also, some taxa have few available PPEs with significant differences (such as Abies, Larix, Juglans, Brassicaceae), and their mean PPE could fail to represent their real pollen productivities. These aspects can cause uncertainty in the mean PPE to some extent. However, we believe that the compiled PPE sets can be used to extract major broad-scale and long-term vegetation patterns because the regional differences in the PPE for most taxa are small compared to the large between-taxa differences. The mean PPEs used in this REVEALS modelling (Table 2) are broadly consistent with those obtained from Europe (Mazier et al., 2012). In addition, although there are no PPEs for the core from the Siberia taiga forest, available studies on modern pollen composition support the weightings in the applied PPEs for major taxa in terms of pollen under- or over-representation of vegetation abundance. For example, modern pollen investigations in north-eastern Siberia revealed that pollen records from northern Larix forest often have less than 13 % Larix pollen, confirming the low pollen productivity of Larix relative to over-represented pollen taxa such as Betula and Alnus (Pisaric et al., 2001a; Klemm et al., 2016). Similarly, a study on modern pollen in southern Siberia (transitional area of steppe and taiga) finds that Artemisia, Betula, and Pinus are high pollen producers compared to Larix (Pelánková et al., 2008). Also, despite Larix being the most common tree in taiga forest in north-central Mongolia, the pollen abundance of Larix is generally lower than 3 % (Ma et al., 2008), implying its low pollen productivity.

In this study, we attempt to reconstruct past landscape changes at a regional scale. Pollen signals from large lakes are assumed to reflect regional vegetation patterns (e.g. Sugita et al., 2010; Trondman et al., 2015). If large lakes are absent in a region, multiple small-sized sites can be used, although error estimates are usually large (Sugita, 2007; Mazier et al., 2012; Trondman et al., 2016). In our study, 70 % of the time slices for the 42 site groups include pollen data from large lakes (i.e. radii >390 m), which supports the reliability of REVEALS reconstructions (Table A3). However, sites are unevenly distributed and occasionally sites from different areas were combined into one group (G2, G6, G34), which might produce a different vegetation-change signal because of the broad distribution of these sites (Fig. 1). In addition, the linear interpolation of pollen abundances for time windows with few pollen data might be another source of uncertainty, particularly for the late Pleistocene and its broad time windows (Table 1). Finally, pollen signals from certain sites and during certain periods may be of water-runoff origin rather than aerial origin violating the assumption of the REVEALS model that pollen is transported by wind.

4.2 Driving factors of vegetation changes

On a glacial–interglacial scale, pollen-based reconstructed land-cover changes in northern Asia are generally consistent with the global climate signal (e.g. sea-surface temperature: Pailler and Bard, 2002; ice-core: Andersen et al., 2004; solar insolation: Laskar et al., 2004; and cave deposits: Cheng et al., 2016; Fig. A6). For example, the relatively high arboreal cover at 40 ka (e.g. G20) corresponds with the warm MIS 3 record from the Baikal region (Swann et al., 2005). The open landscape at 25 and 21 ka (e.g. G25, G36) reflects the cold and dry last glacial maximum (e.g. Swann et al., 2010). Furthermore, the relatively high arboreal cover during the Holocene is consistent with the warm and wet climate (occurring in most site groups). The primary vegetation change in north-eastern China (G29, G30) occurs in the early Holocene (11.5 and 10.5 ka), caused by the rapid increase in abundance of temperate deciduous trees, which may reflect the warmer climate and enhanced summer monsoon known from that region at the beginning of the Holocene (Hong et al., 2009; Liu et al., 2014).

A sensitivity analysis of model-based biome estimation reveals that precipitation plays an important or even dominant role in controlling vegetation changes in arid central Asia (e.g. Tian et al., 2018). The climate of central Asia during the early Holocene is inferred to be quite dry and moisture increase occurs at ca. 8 ka revealed by a series of multi-proxy syntheses (Chen et al., 2008, 2016; Xie et al., 2018) and model-based estimations (Jin et al., 2012). In the taiga–steppe transition zone (south-eastern Siberia and north-central Asia, e.g. G6, G12, G14, G18), a relatively open landscape is reconstructed for the early Holocene and abundances of forest taxa increase after ca. 8 ka, which are consistent with the moisture evolution, and imply the importance of moisture in controlling vegetation changes. Our results support the prediction of an expansion of steppe in the present forest–steppe ecotone of southern Siberia in response to a warmer and drier climate in the future (Tchebakova et al., 2009). During the late Holocene, the decreases in forest cover in the forest–steppe ecotone of north-central China and central Asia are ascribed to the drying or cooling climate, respectively, by sensitivity analysis (Tian et al., 2018). Previous studies argued that the enhanced human impacts might be important factors for the reduction in forest cover (e.g. Ren, 2007); however, our study fails to determine its contribution on vegetation changes.

High abundances of Larix or boreal deciduous woody taxa (mostly shrubs) pollen occur in northern Siberia (e.g. G28, G38, G39, G40) during the middle Holocene, which is now covered by tundra. This is consistent with non-vegetation climate records of a mid-Holocene temperature maximum (e.g. Biskaborn et al., 2012; Nazarova et al., 2013). This result indicates that the boreal treeline in northern Siberia reacts sensitively to warming on millennial timescales, which contrasts with the observed lack of response on a decadal timescale (Wieczoreck et al., 2017). This may point to a highly non-linear vegetation–climate relationship in northern Siberia.

Our results indicate that climate change is the major factor driving land-cover change in northern Asia on a long temporal scale. However, climate change cannot fully explain the changes in arboreal taxa abundance for the West Siberian Plain (G8, G9) and sandy places in central Yakutia (G23, G24, G25). In addition to climate, changes in permafrost condition (Vandenberghe et al., 2014) and fire regime may have played a central role in vegetation change. Larix is the dominant arboreal taxon during the early Holocene (between ca. 12 and 8 ka), which is replaced by evergreen conifer trees, mostly pine and spruce at 8 or 7 ka. Larix can survive on permafrost with an active-layer depth of <40 cm (Osawa et al., 2010) and a high fire frequency, while pine trees can only grow on soil with >1.5 m of active-layer depth (Tzedakis and Bennett, 1995), and spruce is a fire avoider. Probably the compositional change of boreal trees was not in equilibrium with climate but rather driven by changes in the permafrost and fire characteristics that were themselves affected by forest composition, resulting in complex feedback mechanisms. This explanation would be in agreement with the finding by Herzschuh et al. (2016) that the boreal forest composition of nearby refugia during a glacial period influences the initial interglacial forest composition that is then only slowly replaced by a forest composition that is in equilibrium with climate.

Population changes in herbivores could also be an important factor for vegetation change at a regional scale during certain intervals (Zimov et al., 1995; Guthrie, 2006). As with our pollen-based land-cover reconstruction, a circumpolar ancient DNA meta-barcoding study confirms the replacement of steppe-like tundra by moist tundra with abundant woody plants at the Pleistocene–Holocene transition (Willerslev et al., 2014). According to Zimov et al. (1995, 2012), such a change cannot be explained by climate change alone, and thus a reduced density of herbivores is considered to be a major driving factor of steppe composition reduction, since a reduced number of herbivores is insufficient to maintain the open steppe landscapes and so causes a decrease in steppe area (Zimov et al., 1995; Guthrie, 2006). Our land-cover reconstruction fails to address the contribution of herbivores to vegetation changes, but the extinction of herbivorous megafauna would add to the complexity of the interactions among vegetation, climate, and permafrost.

5 Conclusions
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Regional vegetation based on pollen data has been estimated using the REVEALS model for northern Asia during the last 40 ka cal BP. Relatively closed land cover was replaced by open landscapes in northern Asia during the transition from MIS 3 to the last glacial maximum. Abundances of woody components increase again from the last deglaciation or early Holocene. Pollen-based REVEALS estimates of plant abundances should be a more reliable reflection of the vegetation as pollen may overestimate the turnover, and indicates that the vegetation was quite stable during the Holocene as only slight changes in the abundances of PFTs were recorded rather than mass expansion of new PFTs. From comparisons of our results with other data, we infer that climate change is likely the primary driving factor for vegetation changes on a glacial–interglacial scale. However, the extension of evergreen conifer trees since ca. 8–7 ka throughout Siberia could reflect vegetation–climate disequilibrium at a long-term scale caused by the interaction of climate, vegetation, fire, and permafrost, which could be a palaeo-analogue not only for the recent complex vegetation response to climate changes but also for the vegetation prediction in future.

Data availability
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Data availability. 

The used fossil pollen dataset with the re-established age-depth model for each pollen record have been made publicly available in PANGAEA (, Cao et al., 2019).

Appendix A
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Figure A1Distribution of the 203 fossil pollen sites together with the modern permafrost extent in northern Asia. The number of each site is used as its site ID in Table A1.

Figure A2Slight percentage changes for five major plant taxa reconstructed by the REVEALS model with different bog radii (5, 10, 20, 50, 100, 200, and 500 m).


Figure A3Cluster diagram of the site groups based on the plant functional type dataset.


Figure A4Map of the study area showing the geographic locations mentioned in the text.

Figure A5Selected examples of standard errors for seven plant functional type (PFT) reconstructions at site groups G21, G20, and G36 at 6 ka.


Figure A6Proxy-based climate reconstructions from the Northern Hemisphere and insolation variations during the last 40 ka cal BP discussed in the paper. NGRIP: the North Greenland Ice Core Project (Andersen et al., 2004); Sanbao cave (Cheng et al., 2016); Alkenone-derived sea-surface temperatures (SST) from deep-sea cores SU8118 and MD952042 (Pailler and Bard, 2002); solar insolation in July at 60 N (Laskar et al., 2004).


Table A1Metadata for all pollen records used in this study. For a list of original publications, see

LSC: liquid-scintillation counting; A: terrestrial plant macrofossil; B: non-terrestrial plant macrofossil; C: peat; D: pollen; U: unknown; E: total organic matter from silt; F: animal remains or shell; G: charcoal; H: CaCO3; I: tephra.

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Table A2Pollen productivity estimates (PPEs) with their standard errors (SEs) for 27 pollen taxa from 20 study areas. Estimates where SE  PPE were excluded from the calculation of mean PPE and are shown in italics.

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Table A3Number of pollen records from large lakes (≥390 m radius; represented by L), small lakes (<390 m radius; represented by S), and bogs (B) for each site group used to run REVEALS for each time slice. For example, site group G6 has 2 large lake records, 1 small lake record, and 2 bog records at 4 ka (represented by 2L1S2B).

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Author contributions
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Author contributions. 

XC and UH initiated and designed the study; XC and FT performed the land-cover reconstruction; FL and MJG were involved with the methods of the reconstruction; NR and QX contributed pollen data; XC wrote the preliminary version of the article, on which all co-authors commented.

Competing interests
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Competing interests. 

The authors declare that they have no conflict of interest.

Special issue statement
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Special issue statement. 

This article is part of the special issue “Paleoclimate data synthesis and analysis of associated uncertainty (BG/CP/ESSD inter-journal SI)”. It is not associated with a conference.

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The authors would like to express their gratitude to all the palynologists who, either directly or indirectly, contributed their pollen records and PPE results to our study. This research was supported by the German Research Foundation (DFG) and the PalMod project (BMBF). Furong Li and Marie-José Gaillard thank the Faculty of Health and Life Science of Linnaeus University (Kalmar, Sweden), the China-Swedish STINT Exchange Grant 2016–2018, and the Swedish Strategic Research Area on ModElling the Regional and Global Earth system (MERGE) for financial support. This study is a contribution to the Past Global Changes (PAGES) LandCover6k working group project.

Financial support
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Financial support. 

This research has been supported by the German Research Foundation (DFG) and the PalMod project (BMBF).

The article processing charges for this open-access
publication were covered by a Research
Centre of the Helmholtz Association.

Review statement
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Review statement. 

This paper was edited by Lukas Jonkers and reviewed by two anonymous referees.

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Abraham, V. and Kozáková, R.: Relative pollen productivity estimates in the modern agricultural landscape of Central Bohemia (Czech Republic), Rev. Palaeobot. Palyno., 179, 1–12, 2012. 

An, C., Tao, S., Zhao, J., Chen, F., Lv, Y., Dong, W., Li, H., Zhao, Y., Jin, M., and Wang, Z.: Late Quaternary (30.7–9.0 cal ka BP) vegetation history in Central Asia inferred from pollen records of Lake Balikun, northwest China, J. Paleolimnol., 49, 145–154, 2013. 

Andersen, K. K., Azuma, N., Barnola, J.-M., Bigler, M., Biscaye, P., Caillon, N., Chappellaz, J., Clausen, H. B., Dahl-Jensen, D., Fischer, H., Flückiger, J., Fritzsche, D., Fujii, Y., Goto-Azuma, K., Grenvold, K., Gundestrup, N. S., Hansson, M., Huber, C., Hvidberg, C. S., Johnsen, S. J., Jonsell, U., Jouzel, J., Kipfstuhl, S., Landais, A., Leuenberger, M., Lorrain, R., Masson–Delmotte, V., Miller, H., Motoyama, H., Narita, H., Popp, T., Rasmussen, S.O., Raynaud, D., Rothlisberger, R., Ruth, U., Samyn, D., Schwander, J., Shoji, H., Siggard-Andersen, M.-L., Steffensen, J. P., Stocker, T., Sveinbjörnsdóttir, A. E., Svensson, A., Takata, M., Tison, J.-L., Thorsteinsson, T., Watanabe, O., Wilhelms, F., and White, J. W. C.: High-resolution record of Northern Hemisphere climate extending into the last interglacial period, Nature, 431, 147–151, 2004. 

Anderson, P. M. and Lozhkin, A. V.: Late Quaternary vegetation of Chukotka (Northeast Russia), implications for Glacial and Holocene environments of Beringia, Quaternary Sci. Rev., 107, 112–128, 2015. 

Anderson, P. M., Belaya, B. V., Glushkova, O. Y., and Lozhkin, A. V.: New data about the vegetation history of northern Priokhot'ye during the Late Pleistocene and Holocene, in: Late Pleistocene and Holocene of Beringia, edited by: Gagiev, M. K., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 33–54, 1997 (in Russian). 

Anderson, P. M., Lozhkin, A. V., Belaya, B. V., and Stetsenko, T. V.: New data about the stratigraphy of late Quaternary deposits of northern Priokhot'ye, in: Environmental changes in Beringia during the Quaternary, edited by: Simakov, K. V., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 69–87, 1998 (in Russian). 

Anderson, P. M., Lozhkin, A. V., Solomatkina, T. B., and Brown, T. A.: Paleoclimatic implications of glacial and postglacial refugia for Pinus pumila in western Beringia, Quaternary Res., 73, 269–276, 2010. 

Andreev, A. A. and Klimanov, V. A.: Vegetation and climate history of central Yakutia during Holocene and late Pleistocene, in Formirovanie rel'efa, korrelyatnykh otlozhenii i rossypei severo-vostoka SSSR (Formation of deposits and placers on north-east of the USSR), Magadan, 26–51, 1989 (in Russian). 

Andreev, A. A. and Klimanov, V. A.: Vegetation History and climate changes in the interfluve of the Rivers Ungra and Yakokit (the southern Yakutia) in Holocene, Botanichesky Zhurnal (Botanical Journal), 76, 334–351, 1991. 

Andreev, A. A. and Klimanov, V. A.: Quantitative Holocene climatic reconstruction from Arctic Russia, J. Paleolimnol., 24, 81–91, 2000. 

Andreev, A. A., Klimanov, V. A., Sulerzhitskii, L. D., and Khotinskii, N. A.: Chronology of environmental changes in central Yakutia during the Holocene, in Paleoklimaty golotsena i pozdnelednikov'ya (Paleoclimates of Holocene and late glacial), Nauka, Moscow, 115–121, 1989 (in Russian). 

Andreev, A. A., Tarasov, P. E., Siegert, C., Ebel, T., Klimanov, V. A., Melles, M., Bobrov, A. A., Dereviagin, A. Y., Lubinski, D. J., and Hubberten, H.-W.: Late Pleistocene and Holocene vegetation and climate on the northern Taymyr Peninsula, Arctic Russia, Boreas, 32, 484–505, 2003. 

Andreev, A. A., Tarasov, P. E., Klimanov, V. A., Melles, M., Lisitsyna, O. M., and Hubberten, H.-W.: Vegetation and climate changes around the Lama Lake, Taymyr Peninsula, Russia during the Late Pleistocene and Holocene, Quaternary Int., 122, 69–84, 2004. 

Andreev, A. A., Tarasov, P. E., Ilyashuk, B. P., Ilyashuk, E. A., Cremer, H., Hermichen, W. D., Wischer, F., and Hubberten, H.-W.: Holocene environmental history recorded in Lake Lyadhej To sediments, Polar Urals, Russia, Palaeogeogr. Palaeocl., 223, 181–203, 2005. 

Andreev, A. A., Pierau, R., Kalugin, I. A., Daryin, A. V., Smolyaninova, L. G., and Diekmann, B.: Environmental changes in the northern Altai during the last millennium documented in Lake Teletskoye pollen record, Quaternary Res., 67, 394–399, 2007. 

Arkhipov, S. A. and Votakh, M. R.: Palynological characteristics and the absolute age of peat near the mouth of the Tom' River, in: Saks, V. N., The palynology of Siberia, Nauka, Moscow, 112–118, 1980 (in Russian). 

Baker, A. G., Zimny, M., Keczyński, N., Bhagwat, S. A., Willis, K. J., and Latałowa, M.: Pollen productivity estimates from old-growth forest strongly differ from those obtained in cultural landscapes: Evidence from the Biaowiea National Park, Poland, Holocene, 26, 80–92, 2016. 

Beer, R., Kaiser, F., Schmidt, K., Ammann, B., Carraro, G., Grisa, E., and Tinner, W.: Vegetation history of the walnut forest in Kyrgyzstan (Central Asia): natural or anthropogenic origin?, Quaternary Sci. Rev., 27, 621–632, 2008. 

Bezrukova, E. V., Belov, A. V., Abzaeva, A. A., Letunova, P. P., Orlova, L. A., Sokolova, L. P., Kulagina, N. V., and Fisher, E. E.: First High-Resolution Dated Records of Vegetation and Climate Changes on the Lake Baikal Northern Shore in the Middle–Late Holocene, Dokl. Earth Sci., 411, 1331–1335, 2006. 

Bezrukova, E. V., Tarasov, P. E., Solovieva, N., Krivonogov, S. K., and Riedel, F.: Last glacial–interglacial vegetation and environmental dynamics in southern Siberia: Chronology, forcing and feedbacks, Palaeogeogr. Palaeocl., 296, 185–198, 2010. 

Bezrukova, E. V., Belov, A. V., and Orlova, L. A.: Holocene vegetation and climate variability in North Pre-Baikal region, East Siberia, Russia, Quaternary Int., 237, 74–82, 2011. 

Bigelow, N. H., Brubaker, L. B., Edwards, M. E., Harrison, S. P., Prentice, I. C., Anderson, P. M., Andreev, A. A., Bartlein, P. J., Christensen, T. R., Cramer, W., Kaplan, J. O., Lozhkin, A. V., Matveyeva, N. V., Murray, D. F., McGuire, A. D., Razzhivin, V. Y., Ritchie, J. C., Smith, B., Walker, D. A., Gajewski, K., Wolf, V., Holmqvist, B. H., Igarashi, Y., Kremenetskii, K., Paus, A., Pisaric, M. F. J., and Volkova, V. S.: Climate change and arctic ecosystems: 1. Vegetation changes north of 55 N between the last glacial maximum, mid-Holocene, and present, J. Geophys. Res., 108, 8170,, 2003. 

Binney, H. A., Willis, K. J., Edwards, M. E., Bhagwat, S. A., Anderson, P. M., Andreev, A. A., Blaauw, M., Damblon, F., Haesaerts, P., Kienast, F., Kremenetski, K. V., Krivonogov, S. K., Lozhkin, A. V., MacDonald, G. M., Novenko, E. Y., Oksane, P., Sapelko, T. V., Väliranta, M., and Vazhenina, L.: The distribution of late-Quaternary woody taxa in northern Eurasia: evidence from a new macrofossil database, Quaternary Sci. Rev., 28, 2445–2464, 2009. 

Binney, H. A., Edwards, M. E., Macias-Fauria, M., Lozhkin, A., Anderson, P., Kaplan, J. O., Andreev, A. A., Bezrukova, E., Blyakharchuk, T., Jankovska, V., Khazina, I., Krivonogov, S., Kremenetski, K., Nield, J., Novenko, E., Ryabogina, N., Solovieva, N., Willis, K. J., and Zernitskaya, V.: Vegetation of Eurasia from the last glacial maximum to present: key biogeographic patterns, Quaternary Sci. Rev., 157, 80–97, 2017. 

Birks, H. J. B.: Estimating the amount of compositional change in late-Quaternary pollen-stratigraphical data, Veg. Hist. Archaeobot., 16, 197–202, 2007. 

Biskaborn, B. K., Herzschuh, U., Bolshiyanov, D., Savelieva, L., and Diekmann, B.: Environmental variability in northeastern Siberia during the last  13,300 yr inferred from lake diatoms and sediment-geochemical parameters, Palaeogeogr. Palaeocl., 329–330, 22–36, 2012. 

Biskaborn, B. K., Subetto, D. A., Savelieva, L. A., Vakhrameeva, P. S., Hansche, A., Herzschuh, U., Klemm, J., Heinecke, L., Pestryakova, L. A., Meyer, H., Kuhn, G., and Diekmann, B.: Late Quaternary vegetation and lake system dynamics in north-eastern Siberia: implications for seasonal climate variability, Quaternary Sci. Rev., 147, 406–421, 2016. 

Blyakharchuk, T. A.: Istorija rastitel'nosti yugo-vostoka Zapadnoi Sibiri v golotsene po dannym botanicheskogo I sporovo-pyl'tsevogo analiza torfa (The Holocene history of vegetation of south-eastern West Siberia by botanical and pollen analyses of peat deposits), PhD thesis, Tomsk State University, 1989. 

Blyakharchuk, T. A.: Four new pollen sections tracing the Holocene vegetational development of the southern part of the West Siberian Lowland, Holocene, 13, 715–731, 2003. 

Blyakharchuk, T. A., Wright, H. E., Borodavko, P. S., van der Knaap, W. O., and Ammann, B.: Late Glacial and Holocene vegetational changes on the Ulagan high-mountain plateau, Altai Mountains, southern Siberia, Palaeogeogr. Palaeocl., 209, 259–279, 2004. 

Blyakharchuk, T. A., Wright, H. E., Borodavko, P. S., van der Knaap, W. O., and Ammann, B.: Late Glacial and Holocene vegetational history of the Altai Mountains (southwestern Tuva Republic, Siberia), Palaeogeogr. Palaeocl., 245, 518–534, 2007. 

Borisova, O. K., Novenko, E. Y., Zelikson, E. M., and Kremenetski, K. V.: Lateglacial and Holocene vegetational and climatic changes in the southern taiga zone of West Siberia according to pollen records from Zhukovskoye peat mire, Quaternary Int., 237, 65–73, 2011. 

Broström, A.: Estimating source area of pollen and pollen productivity in the cultural landscapes of southern Sweden – developing a palynological tool for quantifying past plant cover, PhD thesis, Lund University, 2002. 

Broström, A., Sugita, S., and Gaillard, M.-J.: Pollen productivity estimates for the reconstruction of past vegetation cover in the cultural landscape of southern Sweden, Holocene, 14, 368–381, 2004. 

Brown, J., Ferrians Jr., O. J., Heginbottom, J. A., and Melnikov, E. S.: Circum-Arctic map of permafrost and ground-ice conditions. Washington, DC: U.S. Geological Survey in Cooperation with the Circum-Pacific Council for Energy and Mineral Resources, Circum-Pacific Map Series CP-45, scale 1 : 10 000 000, 1 sheet, 1997. 

Bunting, M. J., Armitage, R., Binney, H. A., and Waller, M.: Estimates of “relative pollen productivity” and “relevant source area of pollen” for major tree taxa in two Norfolk (UK) woodlands, Holocene, 15, 459–465, 2005. 

Bunting, M. J., Schofield, J. E., and Edwards, K. J.: Estimates of relative pollen productivity (RPP) for selected taxa from southern Greenland: A pragmatic solution, Rev. Palaeobot. Palyno., 190, 66–74, 2013. 

Cao, X., Ni, J., Herzschuh, U., Wang, Y., and Zhao, Y.: A late Quaternary pollen dataset in eastern continental Asia for vegetation and climate reconstructions: set-up and evaluation, Rev. Palaeobot. Palyno., 194, 21–37, 2013. 

Cao, X., Herzschuh, U., Ni, J., Zhao, Y., and Böhmer, T.: Spatial and temporal distributions of major tree taxa in eastern continental Asia during the last 22,000 years, Holocene, 25, 79–91, 2015. 

Cao, X., Tian, F., Andreev, A. A., Anderson, P. M., Lozhkin, A. V., Bezrukova, E. V., Ni, J., Rudaya, N. A., Stobbe, A., Wieczorek, M., and Herzschuh, U. A taxonomically harmonized and temporally standardized fossil pollen dataset from Siberia covering the last 40 ka, PANGAEA,, 2019. 

Chen, F., Yu, Z., Yang, M., Ito, E., Wang, S., Madsen, D. B., Huang, X., Zhao,Y., Sato, T., Birks, H. J. B., Boomer, I., Chen, J., An, C., and Wünnemann, B.: Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history, Quaternary Sci. Rev., 27, 351–364, 2008. 

Chen, F., Jia, J., Chen, J., Li, G., Zhang, X., Xie, H., Xia, D., Huang, W., and An, C.: A persistent Holocene wetting trend in arid central Asia, with wettest conditions in the late Holocene, revealed by multi-proxy analyses of loess-paleosol sequences in Xingjiang, China, Quaternary Sci. Rev., 146, 134–146, 2016. 

Cheng, H., Edwards, R. L., Sinha, A., Spötl, C., Yi, L., Chen, S., Kelly, M., Kathayat, G., Wang, X., Li, X., Kong, X., Wang, Y., Ning, Y., and Zhang, H.: The Asian monsoon over the past 640,000 years and ice age terminations, Nature, 534, 640–646, 2016. 

Demske, D., Heumann, G., Granoszewski, W., Nita, M., Mamakowa, K., Tarasov, P. E., and Oberhansli, H.: Late glacial and Holocene vegetation and regional climate variability evidenced in high-resolution pollen records from Lake Baikal, Global Planet. Change, 46, 255–279, 2005. 

Dirksen, V., Dirksen, O., Van Den Bogaard, C., and Diekmann, B.: Holocene pollen record from Lake Sokoch, interior Kamchatka (Russia), and its paleobotanical and paleoclimatic interpretation, Global Planet. Change, 58, 46–47, 2012. 

Dulamsuren, C., Welk, E., Jäger, E. J., Hauck, M., and Mühlenberg, M.: Range-habitat relationships of vascular plant species at the taiga forest-steppe borderline in the western Khentey Mountains, northern Mongolia, Flora, 200, 376–397, 2005. 

Eisenhut, G.: Untersuchung über die Morphologie und Ökologie der Pollenkörner heimischer und fremdländischer Waldbäume, Parey, Hamburg, 1961. 

Firsov, L. V., Levina, T. P., and Troitskii, S. L.: The Holocene climatic changes in northern Siberia, in: Climatic changes in arctic areas during the last ten thousand years, edited by: Vasari, V., Hyvarinen, H., and Hicks, S., Acta Universitatis Onlensis, Section A., Scientitae Rerum Naturalium Number 3, Geologica, University of Oula, Oula, 341–349, 1972. 

Firsov, L. V., Volkova, V. S., Levina, T. P., Nikolayeva, I. V., Orlova, L. A., Panychev, V. A., and Volkov, I. A.: The stratigraphy, geochronology, and standard spore-pollen diagram for Holocene peat, Gladkoye Bog, Novosibirsk, in: Problems of stratigraphy and paleogeography of the Pleistocene of Siberia, edited by: Arkhipov, S. A., Nauka, Novosibirsk, 96–107, 1982 (in Russian). 

Fyfe, R. M., Twiddle, C., Sugita, S., Gaillard, M.-J., Barratt, P., Caseldine, C. J., Dodson, J., Edwards, K. J., Farrell, M., Froyd, C., Grant, M. J., Huckerby, E., Innes, J. B., Shaw, H., and Waller, M.: The Holocene vegetation cover of Britain and Ireland: overcoming problems of scale and discerning patterns of openness, Quaternary Sci. Rev., 73, 132–148, 2013. 

Gregory, P. H.: The microbiology of the atmosphere, 2nd Edn., Leonard Hill, Aylesbury, 252 pp., 1973. 

Gunin, P. D., Vostokova, E. A., Dorofeyuk, N. I., Tarasov, P. E., and Black, C. C.: Vegetation Dynamics of Mongolia, Kluwer Academic Publishers, London, 1999. 

Guthrie, R. D.: New carbon dates link climatic change with human colonization and Pleistocene extinctions, Nature, 441, 207–209, 2006. 

He, Y., Huang, J., Shugart, H. H., Guan, X., Wang, B., and Yu, K.: Unexpected evergreen expansion in the Siberia forest under warming hiatus, J. Climate, 30, 5021–5037, 2017. 

Herzschuh, U., Tarasov, P., Wünnemann, B., and Hartmann, K.: Holocene vegetation and climate of the Alashan Plateau, NW China, reconstructed from Pollen data, Palaeogeogr. Palaeocl., 211, 1–17, 2004. 

Herzschuh, U., Birks, H. J. B., Laepple, T., Andreev, A., Melles, M., and Brigham-Grette, J.: Glacial legacies on interglacial vegetation at the Pliocene-Pleistocene transition in NE Asia, Nat. Commun., 7, 11967,, 2016. 

Hjelle, K. L. and Sugita, S.: Estimating pollen productivity and relevant source area of pollen using lake sediments in Norway: How does lake size variation affect the estimates?, Holocene, 22, 313–324, 2011. 

Hoff, U., Biskaborn, B. K., Dirksen, V. G., Dirksen, O. V., Kuhn, G., Meyer, H., Nazarova, L. B., Roth, A., and Diekmann, B.: Holocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts Lake, Global Planet. Change, 134, 101–117, 2015. 

Hong, B., Liu, C., Lin, Q., Yasuyuki, S., Leng, X., Wang, Y., Zhu, Y., and Hong, Y.: Temperature evolution from the δ18O record of Hani peat, Northeast China, in the last 14000 years, Sci. China Ser. D, 52, 952–964, 2009. 

Hou, X.: Vegetation Atlas of China, Science Press, Beijing, 2001. 

Hu, Y., Cao, X., Zhao, Z., Li, Y., Sun, Y., and Wang, H.: The palaeoenvironmental and palaeoclimatic reconstruction and the relation with the human activities during the Early and Middle Holocene in the upper Western Liao river region, Quaternary Sci., 36, 530–541, 2016 (in Chinese with English abstract). 

IPCC (Intergovernmental Panel on Climate Change): Climate change 2007: the physical science basis summary for policymakers, World Meteorological Organization, Geneva, Switzerland, 2007. 

Isaev, A. P., Protopopov, A. V., Protopopova, V. V., Egorova, A. A., Timofeyev, P. A., Nikolaev, A. N., Shurduk, I. F., Lytkina, L. P., Ermakov, N. B., Nikitina, N. V., Emova, A. P., Zakharova, V. I., Cherosov, M. M., Nikolin, E. G., Sosina, N. K., Troeva, E. I., Gogoleva, P. A., Kuznetsova, L. V., Pestryakov, B. N., Mironova, S. I., and Sleptsova, N. P.: Vegetation of Yakutia: Elements of Ecology and Plant Sociology, in: The Far North, edited by: Troeva, E. I., Isaev, A. P., Cherosov, M. M., and Karpov, N. S., Vol. 3, Springer Netherlands, Dordrecht, 143–260, 2010. 

Ivanov, V. F.: Quaternary deposits of the coast of eastern Chukotka, North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Vladivostok, 1986 (in Russian). 

Ivanov, V. F., Lozhkin, A. V., Kal'nichenko, S. S., Kyshtymov, A. I., Narkhinova, V. E., and Terekhova, V. E.: The late Pleistocene and Holocene of Chukchi Peninsula to the north of Kamchatka, in: Geology and useful minerals of northeast Asia, edited by: Goncharov, V. I., Far East Branch, USSR Academy of Sciences, Vladivostok, 33–42, 1984 (in Russian). 

Ji, M., Shen, J., Wu, J., and Wang, Y.: Paleovegetation and Paleoclimate Evolution of Past 27.7 cal ka BP Recorded by Pollen and Charcoal of Lake Xingkai, Northeastern China, Earth Surface Processes and Environmental Changes in East Asia, Springer, Japan, 81–94, 2015. 

Jiang, Q., Ji, J., Shen, J., Matsumoto, R., Tong, G., Qian, P., Ren, X., and Yan, D.: Holocene vegetational and climatic variation in westerly-dominated areas of Central Asia inferred from the Sayram Lake in northern Xinjiang, China, Science China Earth Sciences, 56, 339–353, 2013. 

Jiang, W. Y., Guo, Z. T., Sun, X. J., Wu, H. B., Chu, G. Q., Yuan, B. Y., Hatte, C., and Guiot, J.: Reconstruction of climate and vegetation changes of Lake Bayanchagan (Inner Mongolia): Holocene variability of the East Asian monsoon, Quaternary Res., 65, 411–420, 2006. 

Jin, L., Chen, F., Morrill, C., Otto-Bliesner, B. L., and Rosenbloom, N.: Causes of early Holocene desertification in arid central Asia, Clim. Dynam., 38, 1577–1591, 2012. 

Jørgensen, T., Haile, J., Möller, P., Andreev, A., Boessenkool, S., Rasmussen, M., Kienast, F., Coissac, E., Taberlet, P., Brochmann, C., Bigelow, N.H., Andersen, K., Orlando, L., Gilbert, M. T. P., and Willerslev, E.: A comparative study of ancient sedimentary DNA, pollen and macrofossils from permafrost sediments of northern Siberia reveals long-term vegetational stability, Mol. Ecol., 21, 1989–2003, 2012. 

Juggins, S.: rioja: Analysis of Quaternary Science Data, version 0.9-15.1, available at: (last access: 25 August 2017), 2018. 

Katamura, F., Fukuda, M., Bosikov, N. P., and Desyatkin, R. V.: Forest fires and vegetation during the Holocene in central Yakutia, eastern Siberia, J. Forest Res., 14, 30–36, 2009. 

Kats, S. V.: History of vegetation of western Siberia during the Holocene, Bulletin of commission for study the Quaternary, 13, 118–123, 1953 (in Russian). 

Khomutova, V. and Pushenko, M.: Evolution of lake ecosystem of Southern Ural (Russia) from palynological data, abstract of 14th Symposium “Palynologie & changements globaux”, Paris, 1995. 

Kirdyanov, A. V., Hagedorn, F., Knorre, A. A., Fedotova, E. V., Vaganov, E. A., Naurzbaev, M. M., Moiseev, P. A., and Rigling, A.: 20th century tree-line advance and vegetation changes along an altitudinal transect in the Putorana Mountains, northern Siberia, Boreas, 41, 56–67, 2012. 

Klemm, J., Herzschuh, U., and Pestryakova, L. A.: Vegetation, climate and lake changes over the last 7000 years at the boreal treeline in north-central Siberia, Quaternary Sci. Rev., 147, 422–434, 2016. 

Klimanov, V. A.: Methods for interpreting characteristics of past climate. Vestnik MGU, Geographic Series, 2, 92–98, 1976 (in Russian). 

Kong, Z. C. and Du, N. Q.: Vegetation and climate in North Shanxi Plateau from 7000 to 2300 aBP, in: Historic Climate Change in China, edited by: Zhang, P. Y., Shangdong Science and Tecnology Press, Jinan, 18–23, 1996. 

Korotky, A. M.: Paleographic conditions of the formation of Quaternary peats (south of Far East), in: Modern sedimentation and morpholithogenesis of the Far East, edited by: Pletnev, S. P. and Pushkar, V. S., Far Eastern Science Center, USSR Academy of Sciences, Vladivostok, 58–71, 1982 (in Russian). 

Korotky, A. M., Karaulova, L. P., and Troitskaya, T. S.: The Quaternary deposits of Primor'ye, Nauka, Novosibirsk, 1980 (in Russian). 

Korotky, A. M., Mokhova, L. M., and Pushkar, V. S.: The climate changes of the Holocene and landscape evolution of bald mountains of central Yam-Alin', in: Paleogeographic investigations in the Far East, edited by: Korotky, A. M. and Pushkar, V. S., Far Eastern Science Center of the USSR Academy of Sciences, Vladivostok, 5–22, 1985 (in Russian). 

Korotky, A. M., Pletnev, S. P., Pushkar, V. S., Grebennikova, T. A., Razzhigaeva, N. G., Sakhebgareeva, E. D., and Mokhova, L. M.: Evolution environment of south Far East (late Pleistocene and Holocene), Nauka, Moscow, 1988 (in Russian). 

Korotky, A. M., Grebennikova, T. A., Razzhigaeva, N. G., Volkov, V. G., Mokhova, L. M., Ganzey, L. A., and Bazarova, V. B.: Marine terraces of western Sakhalin Island, Catena, 30, 61–81, 1997. 

Kremenetskii, C. V., Tarasov, P. E., and Cherkinski, A. E.: Istoriva ostrovnykh borov Kazakhstana v golotsene (Holocene history of the Kazakhstan “island” pine forests), Botanicheski Zhurial (Botanical Journal), 79, 13–29, 1994. 

Kremenetski, C. V., Bottger, T., Junge, F. W., and Tarasov, A. G.: Late- and postglacial environment of the Buzuluk area, middle Volga region, Russia, Quaternary Sci. Rev., 18, 1185–1203, 1999. 

Krengel, M.: Discourse on history of vegetation and climate in Mongolia–palynological report of sediment core Bayan Nuur I (NW-Mongolia), in: State and dynamics of geosciences and human geography in Mongolia: extended abstracts of the international symposium (Berliner Geowissenschaftliche Abhandlungen), edited by: Walther, M., Janzen, J., Riedel, F., and Keupp, H., Selbstverlag Fachbereich Geowissenschaften, Free University of Berlin, Germany, 80–84, 2000. 

Kruse, S., Wieczorek, M., Jeltsch, F., and Herzschuh, U.: Treeline dynamics in Siberia under changing climates as inferred from an individual-based model for Larix, Ecol. Model., 338, 101–121, 2016. 

Laskar, J., Robutel, P., Joutel, F., Gastineau, M., Correia, A. C. M., and Levrard, B.: A long-term numerical solution for the insolation quantities of the Earth, Astron. Astrophys., 428, 261–285, 2004. 

Levina, T. P., Orlova, L. A., Panychev, V. A., and Ponomareva, E. A.: Radiochronometry and pollen stratigraphy of Holocene peat of Kayakskoye Zaimitschye (Barabinskaya forest-steppe), in: Regional geochronology of Siberia and the Far East, edited by: Nikolayeva, I. V., Nauka, Novosibirsk, 136–143, 1987 (in Russian). 

Li, C., Wu, Y., and Hou, X.: Holocene vegetation and climate in Northeast China revealed from Jingbo Lake sediment, Quaternary Int., 229, 67–73, 2011. 

Li, C. Y., Xu, Z. L., and Kong, Z. C.: A preliminary investigation on the Holocene vegetation changes from pollen analysis in the Gaoxigema section, Hunshandak Sand Land, Acta Phytoecologica Sinica, 27, 797–803, 2003 (in Chinese with English abstract). 

Li, F.: Pollen productivity estimates and pollen-based reconstructions of Holocene vegetation cover in northern and temperate China for climate modelling, PhD thesis, Linnaeus University, 2016. 

Li, F., Gaillard, M.-J., Sugita, S., Mazier, F., Xu, Q., Zhou, Z., Zhang, Y., Li, Y., and Laffly, D.: Relative pollen productivity estimates for major plant taxa of cultural landscapes in central eastern China, Veg. Hist. Archaeobot., 26, 587–605, 2017. 

Li, J., Fan, K., and Zhou, L.: Satellite observations of El Niño impacts on Eurasian spring vegetation greenness during the period 1982–2015, Remote Sens., 9, 628,, 2017. 

Li, R. Q., Zheng, L. M., and Zhu, G. R.: Lakes and Environmental Change in the Inner Mongolian Plateau, Beijing Normal University Press, Beijing, 121–135, 1990 (in Chinese). 

Li, W. Y. and Yan, S.: Quaternary spore and pollen research in Chaiwopu Basin, in: The Quaternary climo-environment changes and hydrogeological condition of Chaiwopu Basin in Xinjiang region, edited by: Shi, Y. F., Wen, Q. Z., and Qu, Y. G., China Ocean Press, Beijing, 1990. 

Li, Y., Nielsen, A. B., Zhao, X., Shan, L., Wang, S., Wu, J., and Zhou, L.: Pollen production estimates (PPEs) and fall speeds for major tree taxa and relevant source areas of pollen (RSAP) in Changbai Mountain, northeastern China, Revi. Palaeobot. Palyno., 216, 92–100, 2015. 

Li, Y. H., Yin, H. N., Zhang, Y., and Zhao, J.: Temperature drop at about 5000 aB.P.–4700 aB.P. in northeast of China and effect on archaeological culture, Yunnan Geographic Environment Research, 15, 12–18, 2003a. 

Li, Y. H., Yin, H. N., Zhang, X. Y., and Chen, Z. J.: The environment disaster events and the evolution of man-land relation in the west Liaoning during 5000 aBP, Journal of Glaciology and Geocryology, 25, 19–26, 2003b (in Chinese with English abstract). 

Li, Y. Y., Willis, K. J., Zhou, L. P., and Cui, H. T.: The impact of ancient civilization on the northeastern Chinese landscape: palaeoecological evidence from the Western Liaohe River Basin, Inner Mongolia, Holocene, 16, 1109–1121, 2006. 

Lin, M. C.: Spore-pollen analysis of Quaternary in Xinjiang Region, in: Quaternary Geology and Environment of Xinjinag Region, China, edited by: Wen, Q. Z., Agricultural Press of China, Beijing, 68–94, 1994 (in Chinese). 

Liu, X. Q., Herzschuh, U., Shen, J., Jiang, Q. F., and Xiao, X. Y.: Holocene environmental and climate changes inferred from Wulungu Lake in northern Xinjiang, China, Quaternary Res., 70, 412–425, 2008. 

Liu, Y. Y., Zhang, S. Q., Liu, J. Q., You, H. T., and Han, J. T.: Vegetation and environment history of Erlongwan Maar Lake during the late Pleistocene on pollen record, Acta Micropalaeontologica Sinica, 25, 274–280, 2008 (in Chinese with English abstract). 

Liu, Z., Wen, X., Brady, E. C., Otto-Bliesner, B., Yu, G., Lu, H., Cheng, H., Wang, Y., Zheng, W., Ding, Y., Edwards, R. L., Cheng, J., Liu, W., and Yang, H.: Chinese cave records and the East Asia Summer Monsoon, Quaternary Sci. Rev., 83, 115–128, 2014. 

López-García, P., López-Sáez, J. A., Chernykh, E. N., and Tarasov, P. E.: Late Holocene vegetation history and human activity shown by pollen analysis of Novienki peat bog (Kargaly region, Orenburg Oblast, Russia), Vege. Hist. Archaeobot., 12, 75–82, 2003. 

Lozhkin, A. V. and Anderson, P. M.: A late Quaternary pollen record from Elikchan 4 Lake, northeast Siberia, Geology of the Pacific Ocean, 14, 18–22, 1995. 

Lozhkin, A. and Anderson, P.: Late Quaternary lake records from the Anadyr Lowland, Central Chukotka (Russia), Quaternary Sci. Rev., 68, 1–16, 2013. 

Lozhkin, A. V. and Glushkova, O.Y.: New palynological assemblages and radiocarbon dates from the late Quaternary deposits of northern Priokhot'ye, in: Late Pleistocene and Holocene of Beringia, edited by: Gagiev, M. K., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 70–7, 1997 (in Russian). 

Lozhkin, A. V. and Vazhenina, L. N.: The characteristics of vegetational development from the Kolyma lowland in the early Holocene, in: Quaternary period of northeast Asia, edited by: Pokhialainen, V. P., North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan 135–144, 1987 (in Russian). 

Lozhkin, A. V., Pavlov, G. F., Ryabchun, V. K., Gorbachev, A. L., Zadal'skii, S. V., and Schubert, E. E.: A new mammoth discovery in Chukotka, Doklady Akademii Nauk, 302, 1440–1444, 1988 (in Russian). 

Lozhkin, A. V., Skorodumov, I. N., Meshkov, A. P., and Rovako, L. G.: Changed paleogeographic environments in the region of Glukhoye Lake (north coast of the Okhotsk Sea) during the Pleistocene-Holocene transition, Dokl. Akad. Nauk, 316, 184–188, 1990 (in Russian). 

Lozhkin, A. V., Anderson, P. M., Eisner, W. R., Ravako, L. G., Hopkins, D. M., Brubaker, L. B., Colinvaux, P. A., and Miller M. C.: Late Quaternary lacustrine pollen records from southwestern Beringia, Quaternary Res., 39, 314–324, 1993. 

Lozhkin, A. V., Anderson, P. M., Belaya, B. V., Glushkova, O. Y., and Kotova, L. N.: Particularities of vegetation evolution in the mountain regions of the Kolyma in the Subatlantic period of the Holocene, in: Quaternary climates and vegetation of western Beringia, edited by: Bychkov, Y. M., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 64–77, 1996a (in Russian). 

Lozhkin, A. V., Anderson, P. M., Belaya, B. V., Glushkova, O. Y., Kozhevinkova, M. V., and Kotova, L. N.: Palynological characteristics and radiocarbon dates of sediments from Elgennya Lake, Upper Kolyma, in: Quaternary climates and vegetation of western Beringia, edited by: Bychkov, Y. M., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 50–64, 1996b (in Russian). 

Lozhkin, A. V., Anderson, P. M., Brubaker, L. B., Kotov, A. N., Kotova, L. N., and Prokhorova, T. P.: The herb pollen zone from sediments of glacial lakes, in: Environmental changes in Beringia during the Quaternary, edited by: Simakov, K. V., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 96–111, 1998 (in Russian). 

Lozhkin, A. V., Anderson, P. M., Belaya, B. V., Glushkova, O. Y., and Stetsenko, T. V.: Vegetation change in northeast Siberia at the Pleistocene-Holocene boundary and during the Holocene, in: The Quaternary period of Beringia, edited by: Simakov, K. V., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 53–75, 2000 (in Russian). 

Lozhkin, A. V., Anderson, P. M., Vartanyan, S. L., Brown, T. A., Belaya, B. V., and Kotov, A. N.: Late Quaternary paleoenvironments and modern pollen data from Wrangel Island (northern Chukotka), Quaternary Sci. Rev., 20, 217–233, 2001. 

Ma, Y., Liu, K., Feng, Z., Sang, Y., Wang, W., and Sun, A.: A survey of modern pollen and vegetation along a south–north transect in Mongolia, J. Biogeogr., 35, 1512–1532, 2008. 

Marcott, S. A., Shakun, J. D., Clark, P. U., and Mix, A. C.: A reconstruction of regional and global temperature for the past 11,300 years, Science, 339, 1198–1201, 2013. 

Marquer, L., Gaillard, M. J., Sugita, S., Trondman, A. K., Mazier, F., Nielsen, A. B., Fyfe, R. M., Odgaard, B. V., Alenius, T., Birks, H. J. B, Bjune, A. E., Christiansen, J., Dodson, J., Edwards, K. J., Giesecke, T., Herzschuh, U., Kangur, M., Lorenz, S., Poska, A., Schult, M., and Seppä, H.: Holocene changes in vegetation composition in northern Europe: why quantitative pollen-based vegetation reconstructions matter, Quaternary Sci. Rev., 90, 199–216, 2014. 

Marquer, L., Gaillard, M.-J., Sugita, S., Poska, A., Trondman, A.-K., Mazier, F., Nielsen, A. B., Fyfe, R. M., Jönsson, A. M., Smith, B., Kaplan, J. O., Alenius, T., Birks, H. J. B., Bjune, A. E., Christiansen, J., Dodson, J., Edwards, K. J., Giesecke, T., Herzschuh, U., Kangur, M., Koff, T., Latałowa, M., Lechterbeck, J., Olofsson, J., and Seppä, H.: Quantifying the effects of land use and climate on Holocene vegetation in Europe, Quaternary Sci. Rev., 171, 20–37, 2017. 

Matthias, I., Nielsen, A. B., and Giesecke, T.: Evaluating the effect of flowering age and forest structure on pollen productivity estimates, Veg. Hist. Archaeobot., 21, 471–484, 2012. 

Mazier, F., Broström, A., Gaillard, M.-J., Sugita, S., Vittoz, P., and Buttler, A.: Pollen productivity estimates and relevant source area of pollen for selected plant taxa in a pasture woodland landscape of the Jura Mountains (Switzerland), Veg. Hist. Archaeobot., 17, 479–495, 2008. 

Mazier, F., Gaillard, M.-J., Kuneš, P., Trodmann, A.-K., and Broström, A.: Testing the effect of site selection and parameter setting on REVEALS-model estimates of plant abundance using the Czech Quaternary Palynological Database, Revi. Palaeobot. Palyno., 187, 38–49, 2012. 

Melles, M., Brigham-Grette, J., Minyuk, P. S., Nowaczyk, N. R., Wennrich, V., DeConto, R. M, Anderson, P. A., Andreev, A. A., Coletti, A., Cook, T. L., Haltia-Hovi, E., Kukkonen, M., Lozhkin, A. V., Rosén, P., Tarasov, P. E., Vogel, H., and Wagner, B.: 2.8 Million years of Arctic climate change from Lake El'gygytgyn, NE Russia, Science, 337, 315–320, 2012. 

Miller, G. H., Alley, R., Brigham-Grette, J., Fitzpatrick, J. J., Polyak, L., Serreze, M. C., and White, J. W. C.: Arctic amplification: can the past constrain the future?, Quaternary Sci. Rev., 29, 1779–1790, 2010. 

Moiseev, P. A.: Climate-change impacts on radial growth and formation of the age structure of highland larch forests in Kuznetsky Alatau, Russ. J. Ecol., 1, 10–16, 2002. 

Mokhova, L., Tarasov, P., Bazarova, V., and Klimin, M.: Quantitative biome reconstruction using modern and late Quaternary pollen data from the southern part of the Russian Far East, Quaternary Sci. Rev., 28, 2913–2926, 2009. 

Müller, S., Tarasov, P. E., Andreev, A. A., and Diekmann, B.: Late Glacial to Holocene environments in the present-day coldest region of the Northern Hemisphere inferred from a pollen record of Lake Billyakh, Verkhoyansk Mts, NE Siberia, Clim. Past, 5, 73–84,, 2009. 

Müller, S., Tarasov, P. E., Andreev, A. A., Tütken, T., Gartz, S., and Diekmann, B.: Late Quaternary vegetation and environments in the Verkhoyansk Mountains region (NE Asia) reconstructed from a 50-kyr fossil pollen record from Lake Billyakh, Quaternary Sci. Rev., 29, 2071–2086, 2010. 

Nazarova, L., Lüpfert, H., Subetto, D., Pestryakova, L., and Diekmann, B.: Holocene climate conditions in central Yakutia (Eastern Siberia) inferred from sediment composition and fossil chironomids of Lake Temje, Quaternary Int., 290–291, 264–274, 2013. 

Neishtadt, M. I. (Ed.): Holocene processes in western Siberia and associated problems, in: Studying and mastering the environment, USSR Academy of Sciences, Institute of Geography, Moscow, 90–99, 1976 (in Russian). 

Neustadt, M. I. and Zelikson, E. M.: Neue Angaben zur stratigraphie der Torfmoore Westsibiriens, Acta Agralia fennica, 123, 27–32, 1985. 

Ni, J., Yu, G., Harrison, S. P., and Prentice, I.C.: Palaeovegetation in China during the late Quaternary: biome reconstructions based on a global scheme of plant functional types, Palaeogeogr. Palaeocl., 289, 44–61, 2010. 

Nielsen, A. B., Giesecke, T., Theuerkauf, M., Feeser, I., Behre, K.-E., Beug, H.-J., Chen, S.-H., Christiansen, J., Dörfler, W., Endtmann, E., Jahns, S., de Klerk, P., Kühl, N., Latałowa, M., Odgaard, B. V., Rasmussen, P., Stockholm, J. R., Voigt, R., Wiethold, J., and Wolters, S.: Quantitative reconstructions of changes in regional openness in north-central Europe reveal new insights into old questions, Quaternary Sci. Rev., 47, 131–149, 2012. 

Niemeyer, B., Klemm, J., Pestryakova, J. A., and Herzschuh, U.: Relative pollen productivity estimates for common taxa of the northern Siberian Arctic, Rev. Palaeobot. Palyno., 221, 71–82, 2015. 

Oganesyan, A. S., Prokhorova, T. P., Trumpe, M. A., and Susekova, N. G.: Paleosols and peats of Wrangel Island, Pochvovedenie, 2, 15–28, 1993 (in Russian). 

Osawa, A., Zyryanova, O. A., Matsuura, Y., Kajimoto, T., and Wein, R. W.: Permafrost Ecosystems: Siberian Larch Forests, Springer, Dordrecht, 502, 2010. 

Pailler, D. and Bard, E.: High frequency paleoceanographic changes during the past 140,000 years recorded by the organic matter in sediments off the Iberian Margin, Palaeogeogr. Palaeocl., 181, 431–452, 2002. 

Panova, N.: Novye dannye po paleoekologii i istorii rastitelnosti yuzhnogo Yamala v golotsene (New data for paleoecology and vegetation history of southern Yamal during the Holocene), Chetvertichnyi period: metody issledovania, strat, 45–46, 1990. 

Panova, N.: Palinologicheskoe issledovanie Karasieozerskogo torfyanika na srednem Urale (Palynological study of Karasieozerskiy peatland on Middle Ural), in: Issledovanie lesov Urala, Materialy nauchnykh chteniy posvyaschennykh pamyati B, 28–31, 1997. 

Panova, N., Makovsky, V. I., and Erokhin, N. G.: Golotsenovaya dinamika rastitelnosti v raione Krasnoufimskoi stepi (Holocene dynamics of vegetation in Krasnoufimskaya forest-steppe area), Lesoobrazovatelnyi protses na Urale i v Zaurali, 80–93, 1996. 

Pelánková, B., Kuneš, P., Chytrý, M., Jankovská, V., Ermakov, N., and Svobodová-Svitavská, H.: The relationship of modern pollen spectra to vegetation and climate along a steppe-forest-tundra transition in southern Siberia, explored by decision trees, Holocene, 18, 1259–1271, 2008. 

Peteet, D. M., Andreev, A. A., Bardeen, W., and Mistretta, F.: Long-term Arctic peatland dynamics, vegetation and climate history of the Pur-Taz region, Western Siberia, Boreas, 27, 115–126, 1998. 

Pisaric, M. F. J., MacDonald, G. M., Cwynar, L. C., and Velichko, A. A.: Modern pollen and conifer stomates from north-central Siberian lake sediments: their use in interpreting late Quaternary fossil pollen assemblages, Arct. Antarct. Alp. Res., 33, 19–27, 2001a. 

Pisaric, M. F. J., MacDonald, G. M., Velichko, A. A., and Cwynar, L. C.: The Lateglacial and Postglacial vegetation history of the northwestern limits of Beringia, based on pollen, stomate and tree stump evidence, Quaternary Sci. Rev., 20, 235–245, 2001b. 

Poska, A., Meltsov, V., Sugita, S., and Vassiljev, J.: Relative pollen productivity estimates of major anemophilous taxa and relevant source area of pollen in a cultural landscape of the hemi-boreal forest zone (Estonia), Rev. Palaeobot. Palyno., 167, 30–39, 2011. 

Prentice, I. C.: Pollen representation, source area, and basin size: toward a unified theory of pollen analysis, Quaternary Res., 23, 76–86, 1985. 

Prokopenko, A. A., Khursevich, G. K., Bezrukova, E. V., Kuzmin, M. I., Boes, X., Williams, D. F., Fedenya, S. A., Kulagina, N. V., Letunova, P. P., and Abzaeva, A. A.: Paleoenvironmental proxy records from Lake Hovsgol, Mongolia, and a synthesis of Holocene climate change in the Lake Baikal watershed, Quaternary Res., 68, 2–17, 2007. 

Qiao, S. Y.: A preliminary study on Hani peat-mire in the west part of the Changbai Mountain, Scientia Geographica Sinica, 13, 279–287, 1993 (in Chinese with English abstract). 

Qiu, S. W., Jiang, P., Li, F. H., Xia, Y. M., and Wang, P. F.: Preliminary study on natural environmental evolution in Northeast China since Late Glacial, Acta Geographica Sinica, 36, 315–327, 1981 (in Chinese with English abstract). 

Räsänen, S., Suutari, H., and Nielsen, A. B.: A step further towards quantitative reconstruction of past vegetation in Fennoscandian boreal forests: Pollen productivity estimates for six dominant taxa, Rev. Palaeobot. Palyno., 146, 208–220, 2007. 

R Core Team: R: A Language and Environment for Statistical Computing, R Foundation for Statistical Computing, Vienna, 2017. 

Ren, G.: Changes in forest cover in China during the Holocene, Veg. Hist. Archaeobot., 16, 119–126, 2007. 

Ren, G. Y. and Zhang, L. S.: Late Holocene vegetation in Maili region, northeast China, as inferred from a high-resolution pollen record, Acta Bot. Sin., 39, 353–362, 1997. 

Rudaya, N., Tarasov, P., Dorofeyuk, N. I., Solovieva, N., Kalugin, I., Andreev, A. A., Darin, A., Diekmann, B., Riedel, F., Narantsetseg, T., and Wagner, M.: Holocene environments and climate in the Mongolian Altai reconstructed from the Hoton-Nur pollen and diatom records, Quaternary Sci. Rev., 28, 540–554, 2009. 

Rudaya, N., Nazarova, L., Nourgaliev, D., Palagushkina, O., Papin, D., and Frolova, L.: Mid-late Holocene environmental history of Kulunda, southern West Siberia: vegetation, climate and humans, Quaternary Sci. Rev., 48, 32–42, 2012. 

Sarda-Espinosa, A.: dtwclust: Time series clustering along with optimizations for the dynamic time warping distance, version 5.2.0, available at: (last access: 5 January 2018), 2018. 

Serreze, M. C., Walsh, J. E., Chapin III, F. S., Osterkamp, T., Dyurgerov, M., Romanovsky, V., Oechel, W. C., Morison, J., Zhang, T., and Barry, R. G.: Observational evidence of recent change in the northern high-latitude environment, Climatic Change, 46, 159–207, 2000. 

Shestakova, T. A., Voltas, J., Saurer, M., Siegwolf, R. T. W., and Kirdyanov, A. V.: Warming effects on Pinus sylvestris in the cold-dry Siberian forest-steppe: positive or negative balance of trade?, Forests, 8, 490,, 2017. 

Shichi, K., Takahara, H., Krivonogovc, S. K., Bezrukova, E. V., Kashiwaya, K., Takehara, A., and Nakamura, T.: Late Pleistocene and Holocene vegetation and climate records from Lake Kotokel, central Baikal region, Quaternary Int., 205, 98–110, 2009. 

Shilo, N. A.: Resolution: Interagency Stratigraphic meeting of Quaternary system of eastern USSR, North East Interdisciplinary Research Institute, Far East Branch, USSR Academy of Sciences, Magadan, 1987 (in Russian). 

Sjögren, P., van der Knaap, W. O., Huusko, A., and Leeuwen, J. F. N.: Pollen productivity, dispersal, and correction factors for major tree taxa in the Swiss Alps based on pollen-trap results, Rev. Palaeobot. Palyno., 152, 200–210, 2008. 

Soepboer, W., Sugita, S., Lotter, A. F., van Leeuwen, J. F. N., and van der Knaap, W. O.: Pollen productivity estimates for quantitative reconstruction of vegetation cover on the Swiss Plateau, Holocene, 17, 65–77, 2007. 

Soja, A. J., Tchebakova, N. M., French, N. H. F., Flannigan, M. D., Shugart, H. H., Stocks, B. J., Sukhinin, A. I., Parfenova, E. I., Chapin III, F. S., and Stackhouse Jr., P. W.: Climate-induced boreal forest change: predictions versus current observations, Global Planet. Change, 56, 274–296, 2007. 

Song, C. Q., Wang, B. Y., and Sun, X. J.: Implication of paleovegetational changes in Diaojiao Lake, Inner Mongolia, Acta Bot. Sin., 38, 568–575, 1996 (in Chinese with English abstract). 

Stebich, M., Rehfeld, K., Schlütz, F., Tarasov, P. E., Liu, J., and Mingram, J.: Holocene vegetation and climate dynamics of NE China based on the pollen record from Sihailongwan Maar Lake, Quaternary Sci. Rev., 124, 275–289, 2015. 

Stetsenko, T. V.: A pollen record from Holocene Lake deposits in the Malyk-Siena depression, upper Kolyma basin, in: Environmental changes in Beringia during the Quaternary edtied by: Simakov, K. V., North East Interdisciplinary Research Institute, Far East Branch, Russian Academy of Sciences, Magadan, 63–68, 1998 (in Russian). 

Stobbe, A., Gumnior, M., Roepke, A., and Schneider, H.: Palynological and sedimentological evidence from the Trans-Ural steppe (Russia) and its palaeoecological implications for the sudden emergence of Bronze Age sedentarism, Veg. Hist. Archaeobot., 24, 393–412, 2015. 

Stuart, A. and Ord, J. K.: Kendall's Advanced Theory of Statistic, Volume 1: Distribution Theory, Edward Arnold, London, 1994. 

Sugita, S.: A model of pollen source area for an entire lake surface, Quaternary Res., 39, 239–244, 1993. 

Sugita, S.: Theory of quantitative reconstruction of vegetation I: pollen from large sites REVEALS regional vegetation composition, Holocene, 17, 229–241, 2007. 

Sugita, S., Gaillard, M.-J., and Broström, A.: Landscape openness and pollen records: a simulation approach, Holocene, 9, 409–421, 1999. 

Sugita, S., Parshall, T., Calcote, R., and Walker, K.: Testing the landscape reconstruction algorithm for spatially explicit reconstruction of vegetation in northern Michigan and Wisconsin, Quaternary Res., 74, 289–300, 2010. 

Sun, A., Feng, Z., Ran, M., and Zhang, C.: Pollen-recorded bioclimatic variations of the last  22,600 years retrieved from Achit Nuur core in the western Mongolian Plateau, Quaternary Int., 311, 36–43, 2013. 

Sun, X. J., Du, N. Q., Weng, C. Y., Lin, R. F., and Wei, K. Q.: Paleovegetation and paleoenvironment of Manasi Lake, Xinjiang, N.W. China during the last 14 000 years, Quaternary Sci., 3, 239–248, 1994 (in Chinese with English abstract). 

Swann, G. E. A., Mackay, A. W., Leng, M. J., and Demory, F.: Climate change in Central Asia during MIS 3/2: a case study using biological responses from Lake Baikal, Global Planet. Change, 46, 235–253, 2005. 

Swann, G. E. A., Leng, M. J., Juschus, O., Melles, M., Brigham-Grette, J., and Sloane, H. J.: A combined oxygen and silicon diatom isotope record of Late Quaternary change in Lake El'gygytgyn, North East Siberia, Quaternary Sci. Rev., 29, 774–786, 2010. 

Tao, S. C., An, C. B., Chen, F. H., Tang, L. Y., Lv, Y. B., and Zheng, T. M.: Holocene vegetation changes interpreted from pollen records in Balikun Lake, Xinjiang, China, Acta Palaeontologica Sinica, 48, 194–199, 2009 (in Chinese with English abstract). 

Tarasov, P. E. and Kremenetskii, K. V.: Geochronology and stratigraphy of the Holocene lacustrine-bog deposits in northern and central Kazakhstan, Stratigr. Geo. Correl., 3, 73–80, 1995. 

Tarasov, P. E., Jolly, D., and Kaplan, J. O.: A continuous Late Glacial and Holocene record of vegetation changes in Kazakhstan, Palaeogeogr. Palaeocl., 136, 281–292, 1997. 

Tarasov, P. E., Webb, T., Andreev, A. A., Afanas'Eva, N. B., Berezina, N. A., Bezusko, L. G., Blyakharchuk, T. A., Bolikhovskaya, N. S., Cheddadi, R., Chernavskaya, M. M., Chernova, G. M., Dorofeyuk, N. I., Dirksen, V. G., Elina, G. A., Filimonova, L. V., Glebov, F. Z., Guiot, J., Gunova, V. S., Harrison, S. P., Jolly, D., Khomutova, V. I., Kvavadze, E. V., Osipova, I. M., Panova, N. K., Prentice, I. C., Saarse, L., Sevastyanov, D. V., Volkova, V. S., and Zernitskaya, V. P.: Present-day and mid-Holocene biomes reconstructed from pollen and plant macrofossil data from the Former Soviet Union and Mongolia, J. Biogeogr., 25, 1029–1053, 1998. 

Tarasov, P. E., Volkova, V. S., Webb, T., Guiot, J., Andreev, A. A., Bezusko, L. G., Bezusko, T. V., Bykova, G. V., Dorofeyuk, N. I., Kvavadze, E. V., Osipova, I. M., Panova, N. K., and Sevastyanov, D. V.: Last glacial maximum biomes reconstructed from pollen and plant macrofossil data from northern Eurasia, J. Biogeogr., 27, 609–620, 2000. 

Tarasov, P. E., Bezrukova, E. V., and Krivonogov, S. K.: Late Glacial and Holocene changes in vegetation cover and climate in southern Siberia derived from a 15 kyr long pollen record from Lake Kotokel, Clim. Past, 5, 285–295,, 2009. 

Tchebakova, N. M., Rehfeldt, G., and Parfenova, E. I.: Impacts of climate change on the distribution of Larix spp. and Pinus sylvestris and their climatypes in Siberia, Mitig. Adapt. Strat. Gl., 11, 861–882, 2005. 

Tchebakova, N. M., Parfenova, E., and Soja, A. J.: The effects of climate, permafrost and fire on vegetation change in Siberia in a changing climate, Environ. Res. Lett., 4, 045013,, 2009. 

ter Braak, C. J. F.: Canonical correspondence analysis: a new eigenvector technique for multivariate direct gradient analysis, Ecology, 67, 1167–1179, 1986. 

ter Braak, C. J. F. and Šmilauer, P.: CANOCO reference manual and CanoDraw for Windows user's guide: software for canonical community ordination (version 4.5), Microcomputer Power, 2002. 

Tian, F., Herzschuh, U., Dallmeyer, A., Xu, Q., Mischke, S., and Biskaborn, B. K.: High environmental variability in the monsoon-westerlies transition zone during the last 1200 years: lake sediment analyses from central Mongolia and supra-regional synthesis, Quaternary Sci. Rev., 73, 31–47, 2013. 

Tian, F., Cao, X., Dallmeyer, A., Lohmann, G., Zhang, X., Ni, J., Andreev, A. A., Anderson, P. M., Lozhkin, A. V., Bezrukova, E., Rudaya, N., Xu, Q., and Herzschuh, U.: Biome changes and their inferred climatic drivers in northern and eastern continental Asia at selected times since 40 cal ka BP, Veg. Hist. Archaeobot., 27, 365–379, 2018. 

Trondman, A.-K., Gaillard, M.-J., Mazier, F., Sugita, S., Fyfe, R. M., Nielsen, A. B., Twiddle, C., Barratt, P., Birks, H. J. B., Bjune, A. E., Björkman, L., Broström, A., Caseldine, C., David, R., Dodson, J., Dörfler, W., Fischer, E., van Geel, B., Giesecke, T., Hultberg, T., Kalnina, L., Kangur, M., van der Knaap, W.O., Koff, T., Kuneš, P., Lagerås, P., Latałowa, M., Lechterbeck, J., Leroyer, C., Leydet, M., Lindbladh, M., Marquer, L., Mitchell, F. J. G., Odgaard, B. V., Peglar, S. M., Persoon, T., Poska, A., Rösch, M., Seppä, H., Veski, S., and Wick, L.: Pollen-based quantitative reconstruction of Holocene regional vegetation cover (plant-functional types and land-cover types) in Europe suitable for climate modelling, Glob. Change Biol., 21, 676–697, 2015. 

Trondman, A.-K., Gaillard, M.-J., Sugita, S., Björkman, L., Greisamn, A., Hultberg, T., Lagerås, P., Lindbladh, M., and Mazier, F.: Are pollen records from small sites appropriate for REVEALS model-based quantitative reconstructions of past regional vegetation? An empirical test in southern Sweden, Veg. Hist. Archaeobot., 25, 131–151, 2016. 

Tseplyayev, V. P.: The forests of the U.S.S.R.: an economic characterisation, Lesa SSSR, Moscow, 1961. 

Tzedakis, P. C. and Bennett, K. D.: Interglacial vegetation succession: a view from southern Europe, Quaternary Sci. Rev., 14, 967–982, 1995. 

Vandenberghe, J., French, H. M., Gorbunov, A., Marchenko, S., Velichko, A. A., Jin, H., Cui, Z., Zhang, T., and Wan, X.: The Last Permafrost Maximum (LPM) map of the Northern Hemisphere: permafrost extent and mean annual air temperatures, 25–17 ka BP, Boreas, 43, 652–666, 2014. 

Velichko, A. A., Andreev, A. A., and Klimanov, V. A.: Paleoenvironmental changes in tundra and forest zones of the former USSR during late Pleistocene and Holocene, in: Environmental changes during the last 15 000, edited by: Velichko, A. A., 1, Geographical Institute, Russian Academy of Science, Moscow, 1994. 

Vipper, P. B.: Pollen profile CHERNOE, Chernoe Lake, Russia, Pangaea,, 2010. 

Volkov, I. A. and Arkhipov, S. A.: Quaternary deposits of the Novosibirsk Region, Joint Institute for Geology, Geophysics and Mineralogy, Siberia Branch, USSR Academy of Sciences, Novosibirsk, 1978 (in Russian). 

Volkova, V. S.: The Quaternary deposits of the lower Irtysh River and their biostratigraphic characteristics, Nauka, Novosibirsk, 1966 (in Russian). 

von Stedingk, H., Fyfe, R. M., and Allard, A.: Pollen productivity estimates from the forest–tundra ecotone in west-central Sweden: implications for vegetation reconstruction at the limits of the boreal forest, Holocene, 18, 323–332, 2008. 

Wang, B. Y., Song, C. Q., Cheng, Q. G., and Sun, X. J.: Palaeoclimate reconstruction by adopting the pollen-climate response surface model to analysis the Chasuqi deposition section, Acta Bot. Sin., 40, 1067–1074, 1998 (in Chinese with English abstract). 

Wang, H. Y., Liu, H. Y., Cui, H. T., and Abrahamsen, N.: Terminal Pleistocene/Holocene palaeoenvironmental changes revealed by mineral-magnetism measurements of lake sediments for Dali Nor area, southeastern Inner Mongolia Plateau, China, Palaeogeogr. Palaeocl., 170, 115–132, 2001. 

Wang, P. F. and Xia, Y. M.: Preliminary research of vegetational succession on the Songnen Plain since Late Pleistocene, Bulletin of Botanical Research, 8, 87–96, 1988 (in China with English abstract). 

Wang, W., Ma, Y. Z., Feng, Z. D., Narantsetseg, T., Liu, K. B., and Zhai, X. W.: A prolonged dry mid-Holocene climate revealed by pollen and diatom records from Lake Ugii Nuur in central Mongolia, Quaternary Int., 229, 74–83, 2011. 

Wang, W., Feng, Z., Ran, M., and Zhang, C.: Holocene climate and vegetation changes inferred from pollen records of Lake Aibi, northern Xinjiang, China: A potential contribution to understanding of Holocene climate pattern in East-central Asia, Quaternary Int., 311, 54–62, 2013. 

Wang, Y. and Herzschuh, U.: Reassessment of Holocene vegetation change on the upper Tibetan Plateau using the pollen-based REVEALS model, Rev. Palaeobot. Palyno., 168, 31–40, 2011. 

Wen, Q. Z. and Qiao, Y. L.: Preliminary probe of climatic sequence in the last 13 000 years in Xinjiang Region, Quaternary Sci., 4, 363–371, 1990 (in Chinese with English abstract). 

Wen, R. L., Xiao, J. L., Chang, Z. G., Zhai, D. Y., Xu, Q. H., Li, Y. C., and Itoh, S.: Holocene precipitation and temperature variations in the East Asian monsoonal margin from pollen data from Hulun Lake in northeastern Inner Mongolia, China, Boreas, 39, 262–272, 2010. 

Wieczorek, M., Kruse, S., Epp, L. S., Kolmogorov, A., Nikolaev, A. N., Heinrich, I., Jeltsch, F., Pestryakova, L. A., Zibulski, R., and Herzschuh, U.: Dissimilar responses of larch stands in northern Siberia to increasing temperatures – a field and simulation based study, Ecology, 98, 2343–2355, 2017. 

Willerslev, E., Davison, J., Moora, M., Zobel, M., Coissac, E., Edwards, M. E., Lorenzen, E. D., Vestergård, M., Gussarova, G., Haile, J., Craine, J., Gielly, L., Boessenkool, S., Epp, L. S., Pearman, P. B., Cheddadi, R., Murray, D., Bråthen, K. A., Yoccoz, N., Binney, H., Cruaud, C., Wincker, P., Goslar, T., Alsos, I. G., Bellemain, E., Brysting, A. K., Elven, R., Sønstebø, J. H., Murton, J., Sher, A., Rasmussen, M., Rønn, R., Mourier, T., Cooper, A., Austin, J., Möller, P., Froese, D., Zazula, G., Pompanon, F., Rioux, D., Niderkorn, V., Tikhonov, A., Savvinov, G., Roberts, R. G., MacPhee, R. D. E., Gilbert, M. T. P., Kjær, K. H., Orlando, L., Brochmann, C., and Taberlet, P.: Fifty thousand years of Arctic vegetation and megafaunal diet, Nature, 506, 47–51, 2014. 

Xia, Y. M.: Preliminary study on vegetational development and climatic changes in the Sanjiang Plain in the last 12 000 years, Scientia Geographica Sinica, 8, 240–249, 1988a (in China with English abstract). 

Xia, Y. M.: Preliminary study on pollen assemblage and palaeoenvironment of the Holocene peat in Northeast China, in: Studies on Chinese Bog, edited by: Huang, X. C., Science Press of China, Beijing, 65–72, 1988b (in China with English abstract). 

Xia, Y. M.: Study on record of spore-pollen in high moor peat and development and successive process of peat in Da and Xiao Hinggan Mountains, Scientia Geographica Sinica, 16, 337–344, 1996 (in China with English abstract). 

Xia, Y. M., Wang, P. F., Li, Q. S., and Jiang, G. W.: The preliminary study on climate change of the warm period of Holocene in the Northeast China, in: Research on the Past Life-Supporting Environment Change of China, edited by: Zhang, L. S., China Ocean Press, Beijing, 296–315, 1993 (in China with English abstract). 

Xiao, J. L., Xu, Q. H., Nakamura, T., Yang, X. L., Liang, W. D., and Inouchif, Y.: Holocene vegetation variation in the Daihai Lake region of north-central China: a direct indication of the Asian monsoon climatic history, Quaternary Sci. Rev., 23, 1669–1679, 2004. 

Xie, H., Zhang, H., Ma, J., Li, G., Wang, Q., Rao, Z., Huang, W., Huang, X., and Chen, F.: Trend of increasing Holocene summer precipitation in arid central Asia: Evidence from an organic carbon isotopic record from the LJW10 loess section in Xinjiang, NW China, Palaeogeogr. Palaeocl., 509, 24–32, 2018. 

Xu, Q., Cao, X., Tian, F., Zhang, S., Li, Y., Li, M., Liu, Y., and Liang, J.: Relative pollen productivities of typical steppe species in northern China and their potential in past vegetation reconstruction, Science China: Earth Sciences, 57, 1254–1266, 2014. 

Xu, Q. H., Wang, Z. H., Xu, Q. H., and Xia Y. M.: Pollen analysis of peat marsh in birch forest, the Changbai Mountains and the significance, Scientia Geographica Sinica, 14, 186–192, 1994 (in China with English abstract). 

Xu, Y. Q.: The assemblage of Holocene spore pollen and its environment in Bosten Lake area, Xinjiang, Arid Land Geography, 21, 43–49, 1998 (in Chinese with English abstract). 

Yan, F. H., Ye, Y. Y., and Mai, X. S.: The sporo-pollen assemblage in the Luo 4 drilling of Lop Lake in Uygur Autonomous Region of Xinjiang and its significance, Seismology and Geology, 5, 75–80, 1983 (in Chinese with English abstract). 

Yan, S., Mu, G. J., Xu, Y. Q., and Zhao, Z. H.: Quaternary environmental evolution of the Lop Nur region, China, Acta Geographica Sinica, 53, 332–340, 1998 (in Chinese with English abstract). 

Yan, S., Li, S. F., Kong, Z. C., Yang, Z. J., and Ni, J.: The pollen analyses and environmental changes of the Dongdaohaizi area in Urumqi, Xinjiang, Quaternary Sci., 24, 463–468, 2004 (in Chinese with English abstract). 

Yang, X. D., Wang, S. M., Xue, B., and Tong, G. B.: Vegetational development and environmental changes in Hulun Lake since Late Pleistocene, Acta Palaeontologica Sinica, 34, 647–656, 1995 (in Chinese with English abstract). 

Zhang, Y., Kong, Z. C., Yan, S., Yang, Z. J., and Ni, J.: “Medieval Warm Period” in Xinjiang: Rediscussion on paleoenvironment of the Sichanghu Profile in Gurbantunggut Desert, Quaternary Sci., 24, 701–708, 2004 (in Chinese with English abstract). 

Zhang, Y., Kong, Z. C., Ni, J., Yan, S., and Yang, Z. J.: Pollen record and environmental evolution of Caotanhu wetland in Xinjiang since 4550 cal. a BP, Chinese Sci. Bull., 53, 1049–1061, 2008. 

Zhang, Y. L. and Yang, Y. X.: The evolution of vegetation and climate on the basis of sporo-pollen assemblages since Mid-Holocene in the Tongjiang region, Heilongjiang, Scientia Geographica Sinica, 22, 426–429, 2002 (in Chinese with English abstract).  

Zimov, S. A., Chuprynin, V. I., Oreshko, A. P., Chapin III, F. S., Reynolds, J. F., and Chapin, M. C.: Steppe-tundra transition: an herbivore-driven biome shift at the end of the Pleistocene, Am. Nat., 146, 765–794, 1995. 

Zimov, S. A., Zimov, N. S., Tikhonov, A. N., and Chapin III, F. S.: Mammoth steppe: a high-productivity phenomenon, Quaternary Sci. Rev., 57, 26–45, 2012. 

Zudin, A. N. and Votakh, M. R.: The stratigraphy of Pliocene and Quaternary strata of Priobskogo Plateau, Nauka, Novosibirsk, 1977 (in Russian). 

Publications Copernicus
Short summary
The high-quality pollen records (collected from lakes and peat bogs) of the last 40 ka cal BP form north Asia are homogenized and the plant abundance signals are calibrated by the modern relative pollen productivity estimates. Calibrated plant abundances for each site are generally consistent with in situ modern vegetation, and vegetation changes within the regions are characterized by minor changes in the abundance of major taxa rather than by invasions of new taxa during the last 40 ka cal BP.
The high-quality pollen records (collected from lakes and peat bogs) of the last 40 ka cal BP...