Do bacterial and fungal communities assemble differently during primary succession?

High‐throughput sequencing technologies are now allowing us to study patterns of community assembly for diverse microbial assemblages across environmental gradients and during succession. Here we discuss potential explanations for similarities and differences in bacterial and fungal community assembly patterns along a soil chronosequence in the foreland of a receding glacier. Although the data are not entirely conclusive, they do indicate that successional trajectories for bacteria and fungi may be quite different. Recent empirical and theoretical studies indicate that smaller microbes (like most bacteria) are less likely to be dispersal limited than are larger microbes – which could result in a more deterministic community assembly pattern for bacteria during primary succession. Many bacteria are also better adapted (than are fungi) to life in barren, early‐successional sediments in that some can fix nitrogen and carbon from the atmosphere – traits not possessed by any fungi. Other differences between bacteria and fungi are discussed, but it is apparent from this and other recent studies of microbial succession that we are a long way from understanding the mechanistic underpinnings of microbial community assembly during ecosystem succession. We especially need a better understanding of global and regional patterns of microbial dispersal and what environmental factors control the development of microbial communities in complex natural systems.     

天山一号冰川前沿生态系统真菌群落结构演替及分布格局

【目的】分析真菌群落结构和多样性随着一号冰川退缩前沿年代序列的变化,揭示真菌群落的演替轨迹及环境因子对群落组成的影响。【方法】采用宏基因组学研究方法,结合生物信息学和统计学分析技术,对取自一号冰川末端表面冰尘,底部和前沿14个样品进行总DNA的提取,ITS基因的扩增并使用Illumina Miseq平台测序,通过相关生物地理化学特性综合分析在不同年代序列下真菌群落结构及其演替规律。【结果】经测序,筛选和质控分析获得185103条rawreads,占78.3%的非单序列在97%的相似度聚类分析共得到300个操作分类单元(OTU),共划分为6个门:子囊菌门(Ascomycota,52.7%)、担子菌门(Basidiomycota,16.9%)、壶菌门(Chytridiomycota,15.1%)、接合菌门(Zygomycota,2.4%)和球囊菌门(Glomeromycota,1.2%)。从演替初期到后期阶段虽然子囊菌的序列数逐渐下降而担子菌出现缓慢上升趋势,但子囊菌随着土壤年代序列的增加始终为优势类群,壶菌在冰川底部和前沿基层普遍存在且丰度仅次于子囊菌和担子菌。我们在缺乏植被的最新退缩基层发现依靠自养型宿主存活的活体营养菌,如Taphrinomycetes、Urediniomycetes和Ustilaginomycetes。从冰川底部和前沿基层检测到丰度较高的酵母菌,而粪生真菌(coprophilous fungi)仅仅出现在冰川前沿基层,共23个操作分类单元。球囊菌仅在前沿部分样品中存在,有着十分狭小的生态位分布。【结论】一号冰川前沿随着年代序列的增加真菌群落存在明显的演替轨迹和多样性的显著变化,不同生态位真菌类群组成的相似性较低且都存在明显的指示性真菌类群。     

Succession of terrestrial macrofungi along a deglaciation gradient at Glacier Blåisen, South Norway

A survey of terrestrial macrofungi along a deglaciation gradient from the glacier forefront to the established vegetation has been performed. The study was accomplished along a transect from Lake Finsevann to Glacier Blåisen, South Norway. Fortysix 6 m × 6 m plots divided into 9 subplots were positioned along this transect. The frequency of fruit bodies of each species in each plot was given on a 0–9 scale reflecting their occurrence in the subplots. Biotic and abiotic environmental variables for the plots were also recorded. The numerical methods used include principal component analysis (PCA), detrended correspondence analysis (DCA), and canonical correspondence analysis (CCA). Totally 99 species of macrofungi were recorded; 80.8 % of the species belonged to the Basidiomycota and 19.2 % to the Ascomycota. About one third of the species was only found once. In general, the species richness was highest on the glacier forefront, lowest in the most established vegetation. The proportion of species of Ascomycota was highest close to the glacier front. The main gradient in the data set was shown related to the primary ecological succession following the retreat of glaciers. The second gradient was possibly related to fine scale variation due to local moisture, microtopography, and secondary distribution. Of the variation in composition of species, 3 % can be ascribed to abiotic variance, 10 % to vascular plant variance, and 16 % to the combination of the abiotic and vascular plant component of variation. The results are discussed in the light of the time since deglaciation and the influence of certain biotic and abiotic environmental factors.     

Co-invading ectomycorrhizal fungal succession in pine-invaded mountain grasslands

Ectomycorrhizal (EM) fungal communities that associate with invading pines (Pinus spp.) are expected to be poor in species diversity. However, long-term successional trajectories and the persistence of dispersal limitations of EM fungi in the exotic range are not well understood. We sampled the roots and surrounding soil of Pinus elliottii and P. taeda trees invading mountain grasslands of Argentina. We also sampled the EM fungal spore bank in grassland soil near (∼150 m) and far (∼850 m) from the original pine plantations. We found 86 different co-invasive EM fungal OTUs. Differential dispersal capacities among EM fungi were detected in the spore bank of grassland soil, but not under mature pines. After thirty years of invasion, the age, but not the degree of spatial isolation of pine individuals affected the EM fungal composition. We showed how EM fungal succession occurs during pine invasions, which may have clear consequences for ecosystem functioning of co-invaded sites.     

Heterotrophic microbial communities use ancient carbon following glacial retreat

When glaciers retreat they expose barren substrates that become colonized by organisms, beginning the process of primary succession. Recent studies reveal that heterotrophic microbial communities occur in newly exposed glacial substrates before autotrophic succession begins. This raises questions about how heterotrophic microbial communities function in the absence of carbon inputs from autotrophs. We measured patterns of soil organic matter development and changes in microbial community composition and carbon use along a 150-year chronosequence of a retreating glacier in the Austrian Alps. We found that soil microbial communities of recently deglaciated terrain differed markedly from those of later successional stages, being of lower biomass and higher abundance of bacteria relative to fungi. Moreover, we found that these initial microbial communities used ancient and recalcitrant carbon as an energy source, along with modern carbon. Only after more than 50 years of organic matter accumulation did the soil microbial community change to one supported primarily by modern carbon, most likely from recent plant production. Our findings suggest the existence of an initial stage of heterotrophic microbial community development that precedes autotrophic community assembly and is sustained, in part, by ancient carbon.     

Effects of an introduced mustard,Thlaspi arvense,on soil fungal communities in subalpine meadows

The subalpine meadows of the Rocky Mountains, USA, are at the advancing front of global change; however, little is known about the sensitivities of high-elevation soil fungal communities to ongoing ecological changes. Soil fungi are sensitive to abiotic and biotic environmental stressors, including climate change, soil disturbance, and the presence of introduced, non-native plants. Invasive plants in the Brassicaceae (mustard family) are known to alter fungal community structure, suppress arbuscular mycorrhizal fungi, and change their relationship with native plant hosts in forest ecosystems, but these phenomena have not been studied in the subalpine zone where non-native mustard plants are becoming established. Here, we investigated whether the presence of the introduced mustard plant, Thlaspi arvense, is associated with distinct properties of the whole fungal and arbuscular mycorrhizal fungal communities in subalpine meadow ecosystems. We observed clear differences in the composition, relative abundance of core taxa, and mean taxon relatedness of soil fungal communities in plots with T. arvense relative to those with only native vegetation. A suite of novel fungi were associated with T. arvense, and overall patterns of AMF phylogenetic diversity were drastically reduced in association with its presence. Our results suggest that T. arvense introduction impacts the soil fungal community, with potential implications for native plant communities and soil nutrient cycling in high elevation meadows of the Rocky Mountains.     

Effects of natural vegetative restoration on soil fungal and bacterial communities in bare patches of the southern Taihang Mountains

Understanding the distribution and composition of soil microbes in bare patches is a critical step to improving ecological remediation. The effects of different vegetative restoration types on soil microbes within semi‐arid bare patches remain unclear. Here, we evaluated the distribution of soil fungi and bacteria among different ecological restoration types at the southern Taihang Mountains. Analysis of variance showed that the chemical properties of soil with vegetation cover have higher nutrient quality than those of the exposed soil. The results also suggested that vegetative restoration significantly improved the diversity and the richness of the soil fungal and bacterial communities. Sequencing results showed that Ascomycota and Basidiomycota were the main soil fungal communities, whereas Proteobacteria, Acidobacteria, and Actinobacteria were the main soil bacterial communities. There were significant relationships between the contents of moisture, organic matter and organic carbon and the soil fungal/bacterial communities. Venn and network diagrams indicated that the vegetative restoration types largely influenced the soil fungi and weakly influenced the soil bacteria in the bare patches. This study discusses the importance of vegetative restoration in the ecological remediation of bare patches. These findings provide effective references for soil restorative measures, water conservation, and bare‐spot reduction at the southern Taihang Mountains in future.     

典型农田退耕后土壤真菌与细菌群落的演替

土壤真菌和细菌作为地下生态系统的重要组成部分,其群落的恢复状况是评价农田退耕还林生态效益的重要指标。以云南省维西县典型退耕还林农田为对象,利用高通量测序等方法比较了不同退耕年限的农田土壤中真菌和细菌群落随植被演替的变化特征。结果发现,农田撂荒后土壤细菌多样性先显著降低后缓慢上升,真菌多样性变化不明显;地上部植被由草本经灌丛再向林地演替的过程中,土壤真菌的群落组成随植被变化呈现明显的改变,主要体现在粪壳菌纲(Sordariomycetes)所占比例的减少(由30%减至10%左右)和伞菌纲(Agaricomycetes)所占比例的增加(由5%以下增至20%以上);而细菌的群落组成无明显变化。聚类分析的结果显示,真菌的群落组成变化与植物群落的演替规律更为同步。不同演替阶段的退耕农田土壤真菌和细菌群落均明显区别于未经扰动的天然林,表明人为扰动对土壤微生物群落的影响可能在较长时间内持续存在。研究揭示了云南典型农田退耕后地下土壤真菌和细菌群落随植被演替的变化特征,为全面评价该地区退耕还林的生态效益提供了数据支撑。     

我国寒温带至亚热带森林多孔菌区系和多样性比较

多孔菌是木材腐朽菌的重要类群, 具有重要的生态功能和经济价值。本文比较分析了我国寒温带至亚热带的阿尔泰山脉、秦岭山脉和南岭山脉的多孔菌物种、生态习性和区系特征。经调查, 在三个山脉共发现多孔菌8目29科107属287种, 其中阿尔泰山、秦岭和南岭分别为84种、132种、160种, 优势科均为多孔菌科和锈革孔菌科。三个山脉的共有属和共有种分别为25个和14个。区系地理分析发现, 阿尔泰山脉和秦岭山脉以世界广布成分和北温带成分为主, 南岭山脉以世界广布和泛热带成分为主。在寄主选择性方面, 阿尔泰山脉的多孔菌偏好生长在裸子植物上, 其比例高于被子植物, 而秦岭和南岭则相反。在腐朽类型方面, 从寒温带至亚热带白腐真菌物种数量呈现逐渐上升的趋势, 而褐腐真菌数量逐渐下降。通过比较分析3个不同气候带的多孔菌物种多样性、寄主偏好性和引起的腐朽类型, 发现气候和植被类型是影响多孔菌区系组成的主要因素。     

Contrasting primary successional trajectories of fungi and bacteria in retreating glacier soils

Early community assembly of soil microbial communities is essential for pedogenesis and development of organic legacies. We examined fungal and bacterial successions along a well‐established temperate glacier forefront chronosequence representing ~70 years of deglaciation to determine community assembly. As microbial communities may be heavily structured by establishing vegetation, we included nonvegetated soils as well as soils from underneath four plant species with differing mycorrhizal ecologies (Abies lasiocarpa, ectomycorrhizal; Luetkea pectinata, arbuscular mycorrhizal; Phyllodoce empetriformis, ericoid mycorrhizal; Saxifraga ferruginea, nonmycorrhizal). Our main objectives were to contrast fungal and bacterial successional dynamics and community assembly as well as to decouple the effects of plant establishment and time since deglaciation on microbial trajectories using high‐throughput sequencing. Our data indicate that distance from glacier terminus has large effects on biomass accumulation, community membership, and distribution for both fungi and bacteria. Surprisingly, presence of plants rather than their identity was more important in structuring bacterial communities along the chronosequence and played only a very minor role in structuring the fungal communities. Further, our analyses suggest that bacterial communities may converge during assembly supporting determinism, whereas fungal communities show no such patterns. Although fungal communities provided little evidence of convergence in community structure, many taxa were nonrandomly distributed across the glacier foreland; similar taxon‐level responses were observed in bacterial communities. Overall, our data highlight differing drivers for fungal and bacterial trajectories during early primary succession in recently deglaciated soils.     

Mycorrhiza-plant colonization patterns on a subalpine glacier forefront as a model system of primary succession

Lyman glacier in the North Cascades Mountains of Washington has a subalpine forefront characterized by a well-developed terminal moraine, inconspicuous successional moraines, fluting, and outwash. These deposits were depleted of symbiotic fungi when first exposed but colonized by them over time after exposure. Four major groups of plant species in this system are (1) mycorrhiza-independent or facultative mycotrophic, (2) dependent on arbuscular mycorrhizae (AM) (3) dependent on ericoid mycorrhiza (ERM) or ectomycorrhizae (EM), and (4) colonized by dark-septate (DS) endophytes. We hypothesized that availability of mycorrhizal propagules was related to the success of mycorrhiza-dependent plants in colonizing new substrates in naturally evolved ecosystems. To test this hypothesis roots samples of 66 plant species were examined for mycorrhizal colonization. The plants were sampled from communities at increasing distances from the glacier terminus to compare the newest communities with successively older ones. Long established, secondary successional dry meadow communities adjacent to the glacier forefront, and nearby high alpine communities were sampled for comparison. DS were common on most plant species on the forefront. Nonmycorrhizal plants predominated in the earlier successional sites, whereas the proportion of mycorrhizal plants generally increased with age of community. AM were present, mostly at low levels, and nearly absent in two sites of the forefront. ERM were present in all species of Ericaceae sampled, and EM in all species of Pinaceae and Salicaceae. Roots of plants in the long established meadow and heath communities adjacent to the forefront and the high alpine community all had one or another of the colonization types, with DS and AM predominating.     

Do forest soil microbes have the potential to resist plant invasion? A case study in Dinghushan Biosphere Reserve (South China)

Successful invaders must overcome biotic resistance, which is defined as the reduction in invasion success caused by the resident community. Soil microbes are an important source of community resistance to plant invasions, and understanding their role in this process requires urgent investigation. Therefore, three forest communities along successional stages and four exotic invasive plant species were selected to test the role of soil microbes of three forest communities in resisting the exotic invasive plant. Our results showed that soil microbes from a monsoon evergreen broadleaf forest (MEBF) (late-successional stage) had the greatest resistance to the invasive plants. Only the invasive species Ipomoea triloba was not sensitive to the three successional forest soils. Mycorrhizal fungi in early successional forest Pinus massonina forest (PMF) or mid-successional forest pine-broadleaf mixed forest (PBMF) soil promoted the growth of Mikania micrantha and Eupatorium catarium, but mycorrhizal fungi in MEBF soil had no significant effects on their growth. Pathogens plus other non-mycorrhizal microbes in MEBF soil inhibited the growth of M. micrantha and E. catarium significantly, and only inhibited root growth of E. catarium when compared with those with mycorrhizal fungi addition. The study suggest that soil mycorrhizal fungi of early-mid-successional forests benefit invasive species M. micrantha and E. catarium, while soil pathogens of late-successional forest may play an important role in resisting M. micrantha and E. catarium. The benefit and resistance of the soil microbes are dependent on invasive species and related to forest succession. The study gives a possible clue to control invasive plants by regulating soil microbes of forest community to resist plant invasion.     

冰川前缘土壤微生物原生演替的生态特征——以乌鲁木齐河源1号冰川为例

为了解冰川前缘土壤微生物在原生演替过程中的生态特征及其影响因素,用空间距离代替时间序列,以乌鲁木齐河源1号冰川终碛堤为起点,沿6个不同演替时期(0,4,15,31,43a和对照)的样带采集土样,以冰川附近发育良好的土壤为对照,测定土壤酶活性、微生物氮矿化与脱氨作用以及微生物生物量。结果表明,土壤脲酶、蛋白酶、酸性磷酸酶、芳基硫酸酯酶、蔗糖酶活性、微生物氮矿化及脱氨作用随演替时间而增加,微生物生物量碳和氮变化呈波动状,趋势不明显。相关分析表明,土壤有机质与酶活、微生物生物量存在极显著正相关(P0.01)。1号冰川前缘微生物多样性指数随着演替时间持续增加,但目前仍未达稳定状态。     

Vertical distribution of the soil microbiota along a successional gradient in a glacier forefield

Spatial patterns of microbial communities have been extensively surveyed in well‐developed soils, but few studies investigated the vertical distribution of micro‐organisms in newly developed soils after glacier retreat. We used 454‐pyrosequencing to assess whether bacterial and fungal community structures differed between stages of soil development (SSD) characterized by an increasing vegetation cover from barren (vegetation cover: 0%/age: 10 years), sparsely vegetated (13%/60 years), transient (60%/80 years) to vegetated (95%/110 years) and depths (surface, 5 and 20 cm) along the Damma glacier forefield (Switzerland). The SSD significantly influenced the bacterial and fungal communities. Based on indicator species analyses, metabolically versatile bacteria (e.g. Geobacter) and psychrophilic yeasts (e.g. Mrakia) characterized the barren soils. Vegetated soils with higher C, N and root biomass consisted of bacteria able to degrade complex organic compounds (e.g. Candidatus Solibacter), lignocellulolytic Ascomycota (e.g. Geoglossum) and ectomycorrhizal Basidiomycota (e.g. Laccaria). Soil depth only influenced bacterial and fungal communities in barren and sparsely vegetated soils. These changes were partly due to more silt and higher soil moisture in the surface. In both soil ages, the surface was characterized by OTUs affiliated to Phormidium and Sphingobacteriales. In lower depths, however, bacterial and fungal communities differed between SSD. Lower depths of sparsely vegetated soils consisted of OTUs affiliated to Acidobacteria and Geoglossum, whereas depths of barren soils were characterized by OTUs related to Gemmatimonadetes. Overall, plant establishment drives the soil microbiota along the successional gradient but does not influence the vertical distribution of microbiota in recently deglaciated soils.     

大兴安岭森林火烧后不同演替阶段土壤细菌多样性动态

【目的】研究我国最大的林区之一——大兴安岭森林火烧后不同演替阶段土壤细菌多样性动态,为天然林保护工程对于生物多样性的影响增添新的认识。【方法】以空间替代时间的方法分析大兴安岭森林演替对于土壤细菌多样性动态的影响。大兴安岭森林火烧后典型的自然演替序列为火烧迹地(LG-BA)、灌丛(SHR)、白桦林(BP)、白桦落叶松混交林(BP-LG)、落叶松林(LG-OM)。在演替序列的每个典型样地上采集0-10 cm土样,采用Illumina Mi Seq高通量测序技术测定土壤细菌群落组成及其多样性。【结果】细菌操作分类单位(OTU)数量从少到多的顺序为火烧迹地落叶松白桦混交林灌丛落叶松林白桦林。随着森林演替,多样性指数Simpson先增高后降低;Shannon指数先增加后减少再增加;OTU的丰度变化比较平缓,表明物种变化较小。在各演替阶段中,土壤细菌种类主要有变形菌门(Proteobacteria)、酸杆菌门(Acidobacteria)、放线菌门(Actinobacteria)和浮霉菌门(Planctomycetes),4个门的种类含量随演替顺序都呈现先增加后减少的趋势。主成分分析表明不同演替阶段土壤细菌群落存在一定的差异性。冗余分析表明有机质(SOM)、全氮(TN)、全磷(TP)和p H对于土壤细菌群落变化有影响。【结论】随着森林演替,大兴安岭地区土壤细菌种类和生物多样性会发生变化,其变化与土壤化学成分和p H有关。     

Fungal colonization of shrub willow roots at the forefront of a receding glacier

Shrub willows (Salix spp.) form associations with arbuscular mycorrhizal (AM), ectomycorrhizal (EM) and dark septate endophytic (DSE) fungi. Willow root colonization by these three types of fungi was studied on a deglaciated forefront of Lyman Glacier, Washington, USA. Root colonization was low; less than 1% of the root length was colonized by AM and 25.6% by DSE. EM colonized 25% of the root tips and 19.4% of the root length. AM and DSE colonization were not related to distance from the present glacier terminus or to canopy cover. EM colonization increased with distance from the glacier terminus based on gridline intercept data but not on root tip frequency data. Availability of propagules in the substrate was low, but numbers of propagules increased with distance from the glacier terminus. The EM communities were dominated by three ascomycetes showing affinity to Sordariaceae in BLAST analyses. Other frequent taxa on the glacier forefront included species of Cortinariaceae, Pezizaceae, Russulaceae, Thelephoraceae and Tricholomataceae. When occurrence of individual taxa was used as a response variable to canopy cover, distance from the glacier terminus, and their interaction, four different fungal guilds were identified: 1) fungi that did not respond to these environmental variables; 2) fungi that occurred mainly in intercanopy areas and decreased with distance from the glacier terminus; 3) fungi that were insensitive to canopy cover but increased with distance from the glacier terminus; 4) fungi that occurred mainly under willow canopies and increased with distance from the glacier terminus. We suggest that fungal colonization is mainly limited by fungal propagule availability. Environmental conditions may also limit successful establishment of plant-fungus associations. We propose that the four EM guilds partly explain successional dynamics. The initial EM community comprises fungi that tolerate low organic matter and nitrogen environment (first and second guilds above). During later community development, these fungi are replaced by those that benefit from an increased organic matter and nitrogen environment (third and fourth guilds above).     

Soil Microbial Communities of Eastern Antarctica

Investigation of microbial communities of Antarctica soils is a very important field of research that expands our knowledge of microbial participation in primary soil formation and specific features of their communities in extreme habitats, and it is of considerable interest in directed search of for microorganisms as potential biotechnological objects. The results of long-term (2012–2017) complex studies on soil microbial communities of the Russian East Antarctica polar stations at Shirmakher oasis (Novolazarevskaya station), the Larsemann Hills (Progress station), and the Tala Hills (Molodezhnaya station) are presented in this review. The assessment of biomass of soil microorganisms by the methods of direct microscopy has been carried out for the first time for this region. The general amount of microbial biomass is small; the fungi dominate (77–99%). The unique features of Antarctic soils are the high content and morphological diversity of small forms of microorganisms: fungi are presented by mainly single-celled structures (small spores and yeasts), while bacteria by ultrafine (filtering) forms. At the same time, microorganisms can significantly contribute to such important ecological functions of soil as the emission of greenhouse gases, especially during the warm season with the stable positive temperatures of the soil. This should be considered during creation of models and forecasts of global warming. The use of various isolation techniques for the analysis of the soil microbial population, together with the succession approach, significantly expand the information about taxonomic diversity of cultivated fungi and bacteria in Antarctica soils.     

内蒙古草原典型植物对土壤微生物群落的影响

为了分析内蒙古草原不同植物物种对土壤微生物群落的影响, 采用实时荧光定量PCR (real-time PCR)以及末端限制性片段长度多态性分析(terminal restriction fragment length polymorphism, T-RFLP)等分子生物学技术, 测定了退化-恢复样地上几种典型植物的根际土壤和非根际土壤中细菌和真菌的数量及群落结构。结果表明, 不同植物物种对根际和非根际细菌及根际真菌数量均有显著影响。根际土壤中的细菌和真菌数量普遍高于非根际土壤, 尤其以真菌更为明显。对T-RFLP数据进行多响应置换过程(multi-response permutation procedures, MRPP)分析和主成分分析(principal component analysis, PCA), 结果表明, 大多数物种的根际细菌及真菌的群落结构与非根际有明显差异, 并且所有物种的真菌群落可以按根际和非根际明显分为两大类群。此外, 细菌和真菌群落结构在一定程度上存在按物种聚类的现象, 以细菌较为明显。这些结果揭示了不同植物对土壤微生物群落的影响特征, 对理解内蒙古草原地区退化及恢复过程中植被演替引起的土壤性质和功能的变化有一定的帮助。     

The influence of late pleistocene mountain glaciations on the genetic differentiation of long-tailed ground squirrel (<Emphasis Type="Italic">Urocitellus undulatus</Emphasis>)

Long-tailed ground squirrel (Urocitellus undulatus) is a polytypic species with a wide distribution from the Tien Shan to the Amur River region. Previously, considerable genetic differentiation between eastern and western populations of this species was demonstrated. Moreover, the greatest differences were observed in the western part of the range located in Central Asia, the region that was subjected to repeated glaciations in the past and represents one of the centers of the ground squirrel secondary diversification. The analysis of polymorphism of the mitochondrial DNA control region was carried out on long-tailed ground squirrels living in the northern part of Central Asia, on the territory of the Altai Mountains (45 individuals from 23 localities). The presence of two genetically differentiated (7.7% differences) and geographically separated lineages (western and eastern) was revealed. The data obtained disprove the hypothesis on unidirectional, from west to east, colonization of the Altai Mountains after the end of the last glacial maximum and show the two pathways of the ground squirrel colonization of the Altai, from both western and eastern refugia.