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Soil-Moisture Conditions Indicated by Field-Layer Plants Help Identify

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Soil-Moisture Conditions Indicated by Field-Layer Plants Help Identify Ecological Indicators 57 (2015) 196–207 Contents lists available at ScienceDirect Ecological Indicators jo urnal homepage: www.elsevier.com/locate/ecolind Soil-moisture conditions indicated by field-layer plants help identify vulnerable forests in the forest-steppe of semi-arid Southern Siberia a,∗ b,1 a c Oleg A. Anenkhonov , Andrey Yu. Korolyuk , Denis V. Sandanov , Hongyan Liu , d e Andrei A. Zverev , Dali Guo a Institute of General and Experimental Biology, Siberian Branch of Russian Academy of Sciences, Sakh’yanovoi str., 6, 670047 Ulan-Ude, Russian Federation b Central Siberian Botanical Garden, Siberian Branch of Russian Academy of Science, Zolotodolinskaya str., 101, 630090 Novosibirsk, Russian Federation c College of Urban and Environmental Sciences, Peking University, Beijing 100871, China d Tomsk State University, Lenina str., 36, 634050 Tomsk, Russian Federation e Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China a r t i c l e i n f o a b s t r a c t Article history: High variability in soil-moisture conditions is typical for semi-arid forest-steppe ecosystems where pre- Received 21 March 2014 cipitation varies greatly over time. Plant species that inhabit these environments integrate responses to Received in revised form 3 April 2015 broadly fluctuating wetness conditions. Indirect assessment of contrasting habitat wetness based on plant Accepted 8 April 2015 indicator values, species frequency, and species coverage was carried out in two sites representing the larch (Larix sibirica) and pine (Pinus sylvestris) forest-steppe communities. For the larch forest-steppe, we Keywords: found that plant community composition and spatial structure depended strongly on wetness. In addi- Forest-steppe tion, we found that the vegetation was clearly differentiated into forest stands and steppe communities, Plant indicator values depending on the slope aspect. There was also a strong correlation between dissimilarities of species Habitat wetness composition and differences in habitat wetness revealed in the larch forest-steppe. In contrast, soil prop- Plant distribution patterns Semi-arid vegetation erties, such as gravel and stone content were found to be a key factor in the spatial distribution of plant Pine forest species composition in the pine-forest-steppe communities. Indirect assessment of moisture conditions Larch forest in the forest-steppe habitats, based on the field-layer plant species, was found to be preferable for indicat- Forest vulnerability ing soil water deficits in the forest. Furthermore, as long-term observational data is often lacking, indirect Climate change assessment of the forest-steppe vegetation provides an opportunity to identify vulnerable forests at the Southern Siberia marginal distribution. Based on indirect assessments of soil-moisture conditions, and taking into account differences in potential drought resistance between larch and pine forests, we concluded that increasing aridity will cause the replacement of Siberian larch by Scots pine in the South Siberian forest-steppe landscape. Consequently, in the future it is likely that forest-steppe typological diversity will decrease, and the semi-arid landscape may become more monotonous. © 2015 Elsevier Ltd. All rights reserved. 1. Introduction analytical methods. Synoptic data from precipitation gauges can provide a general overview of soil-moisture differentiation among High variability in soil-moisture conditions, depending on various ecosystems. These assessments provide information of a weather fluctuations, is a well-known phenomenon. Significant coarse and relative nature, but are often insufficient for determin- variability is typical for semi-arid ecosystems where precipitation ing vegetation community patterns, in addition to forests suffering varies greatly in spatial and temporal distribution in comparison from water deficit. with humid and arid territories. For this reason, determining wet- An integrated response to broadly fluctuating wetness con- ness gradients requires long-term monitoring studies and specific ditions can be deduced from the plant species inhabiting such environments (Zonneveld, 1983; Diekmann, 2003). In the early 1950s, German ecologist Heinz Ellenberg and Russian geobotanist ∗ Corresponding author. Tel.: +7 9021675098; fax: +7 3012 433034. Leontyi G. Ramensky independently developed indicator systems E-mail addresses: [email protected] (O.A. Anenkhonov), [email protected] for vascular plants. The first edition of the indicator values, devel- (A.Yu. Korolyuk), [email protected] (D.V. Sandanov), oped by Ramensky et al. (1956), covered the European portion of [email protected] (H. Liu), [email protected] (A.A. Zverev), [email protected] the former USSR. The name given by the author for this indica- (D. Guo). 1 tor system was “standard ecological scale”. L.N. Sobolev and V.D. Fax: +7 383 3301986. http://dx.doi.org/10.1016/j.ecolind.2015.04.012 1470-160X/© 2015 Elsevier Ltd. All rights reserved. O.A. Anenkhonov et al. / Ecological Indicators 57 (2015) 196–207 197 Utekhin (1982), along with R.P. McIntosh (1983) described Ramen- topic, as climate warming and drought-caused alterations in the sky’s approach in English. composition of forest species can drive vegetation-type conver- As the data on plant ecology and geography were extended, veg- sions, promote new plant-community assemblages, resetting or etation of other regions was included in the “standard ecological shifting successional trajectories (Anderegg et al., 2013). Besides, scale”. These areas included Siberia (Tsatsenkin et al., 1974, 1978; semi-arid forests have global importance because of substantial Korolyuk, 2006) and the Russian Far East (Komarova et al., 2003). carbon sequestration and subsequent cooling effects (Rotenberg Ellenberg (1974) published a list of indicator values for vascular and Yakir, 2010). At the same time, forests are critically important plants occurring in central Europe based on preliminary studies for environmental monitoring in semi-arid regions, which support from the early 1950s. The latest edition was sufficiently expanded approximately 36% of the world’s human population and highly and included values for bryophytes and lichens (Ellenberg et al., diverse flora and fauna (Millennium Ecosystem Assessment, 2005; 1991). There is also a well known alternative list of indicator val- Carpenter et al., 2009). There are, however, no observational studies ues proposed for Switzerland (Landolt, 1977; Landolt et al., 2010). addressing the effects of changes in habitat wetness on the commu- Although researchers independently developed plant indicator val- nity diversity and structure within the forest-steppe ecosystems. ues, in general, the approaches were quite similar. Moreover, there is a lack of data necessary to assess current wet- The indirect assessment method and characterization of habi- ness conditions and probable future habitat deterioration under tat wetness based on indicator values of plants combine intensive increasing aridity. long-term procedures and single measurements. Plant species Due to some tree species succumbing more readily than oth- composition reflects the wetness conditions to which the com- ers (e.g. Mueller et al., 2005), reliable approaches to exploring the munities are exposed over time, and therefore, plant communities resilience of different tree species to habitat moisture shortage are can integrate a longer time period through the later application needed. It remains unclear what kind of forest stands are the most of plant and community indicator values. Evaluation of the plant vulnerable under a decreasing soil water supply and increasing indicator values and weighted averages has been found to be pos- climate aridity. This presents a barrier to predictions on prob- sible for the indirect assessment of long-term community exposure able climate-forced vegetation dynamics and/or transformations patterns. For example, several researchers have found correlations of forest-steppe ecosystems. Thus, we hypothesized that wetness between assessments based on indicator values and direct environ- condition indicated by ground plant species determines forest dis- mental traits measurement (e.g., Diekmann, 1995; Diekmann and tribution in the forest-steppe ecotone and it is possible to identify Dupre, 1997; Diekmann and Falkengren-Grerup, 1998; Ertsen et al., the forest patches facing the greatest water deficit. To enable a 1998; Dzwonko, 2001). In addition, Kopecky´ and Ciˇ zkovaˇ (2010) better understanding of how Siberian forest-steppe communities reported that the Topographic Wetness Index (TWI), computed depend on soil moisture dynamics and to pave the road for a better from an analysis of the contributing upslope area, was correlated protection of these ecosystems during future climate changes we with habitat wetness estimates based on Ellenberg’s (1974) indi- investigated the following: (1) does the wetness condition indi- cator values. Thereafter, Moeslund et al. (2013) found a correlation cated by understorey plant species determine forest distribution between TWI and the Ellenberg indicator values (moisture) cal- in the forest-steppe ecotone? (2) If yes, is it possible to use this culated for relevés in lowland region (in Denmark). Thus, there information to identify the forest patches facing the greatest water is evidence that plants integrate conditions to which they are deficit? exposed over time, and assessments based on the
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