Microbial Diversity in High Arsenic Groundwater in Hetao Basin of Inner Mongolia,China

The microbial diversity and community structure in twenty-one groundwater samples from high arsenic shallow aquifers of Hetao Basin, Inner Mongolia, China was investigated with an integrated approach including polymerase chain reaction (PCR)-denaturing gradient gel electrophoresis (DGGE) and 16S rRNA gene phylogenetic analyses. A total of 25 bacterial and 32 archaeal DGGE bands were exercised for sequencing. Phylogenetic analyses showed that the bacterial DGGE bands were dominated by Proteobacteria, and the archaeal bands were dominated by Thaumarchaeota and Euryarchaeota. Based on arsenic concentrations, three samples (corresponding to low, medium, and high level of arsenic, respectively) were selected for construction of 16S rRNA gene clone libraries. A total of 912 (468 and 444 for bacteria and archaea, respectively) 16S rRNA gene clone sequences were obtained and subjected to phylogenetic analyses. The results showed that bacterial communities of these samples were dominated by Acinetobacter, Pseudomonas, Massilia, Dietzia, Planococcus, Brevundimonas, Aquabacterium and Geobacter, and archaeal communities by Nitrosophaera, Thermoprotei and Methanosaeta. The relative abundance of major groups varied as a function of changes in groundwater geochemistry. Acinetobacter, Brevundimonas, Geobacter, Thermoprotei and Methanosaeta dominated in high arsenic samples with high concentrations of methane and Fe(II), and low concentrations of SO^2? ₄ and NO^? ₃, while Pseudomonas and Nitrosophaera were abundant in low arsenic groundwater. These results imply that microbes play an important role in arsenic mobilization in the shallow aquifers of Hetao Basin, Inner Mongolia.     

Bacterial Diversity and Community Structure in High Arsenic Aquifers in Hetao Plain of Inner Mongolia,China

The bacterial diversity and community structure of high arsenic (As) aquifers was investigated using an integrated approach adopting both geochemistry and molecular biology (polymerase chain reaction (PCR)-denaturing gradient gel electrophoresis (DGGE) and 16S rRNA gene clone library analyses). Nine borehole sediments and one groundwater sample from the living place of a villager (affected by arseniasis) and 12 sediments from a control borehole in Hetao Plain were investigated. The As concentrations ranged from 33.6 to 77.6 mg/kg in high As borehole sediments and 1.5 to 5.8 mg/kg in those samples from the control. The As concentration in the groundwater was 744.8 μg/L. Ratios between As(III) and total As in high As sediments increased gradually with depth and ranged from 0.02 to 0.34. Similarly, the Fe(II)/total Fe presented the same increasing trend with depth. The correlation between TOC contents and total As was positive. High concentrations of total As, S, Fe and TOC were found in clay and low in sand samples. Phylogenetic analysis showed significantly different bacterial communities among high As sediments, control sediments and the high As groundwater. Both DGGE and 16S rRNA gene clone library results showed that the high As sediments were dominated by Thiobacillus, Pseudomonas, Brevundimonas, and Hydrogenophaga, with Thiobacillus being distinctly dominant (63.5%). Whereas the low As sediments were dominated by some other genera including Psychrobacter, Massilia and Desulfotalea. The bacterial populations in the high As groundwater mainly included Pseudomonas, Acinetobacter and Aquabacterium. These results improve our understanding of the bacterial diversity in high As aquifers in Hetao Plain and suggest how specific bacterial populations help mediate the mobilization of As into high As groundwaters.     

Abundance and Diversity of Sulfate-Reducing Bacteria in High Arsenic Shallow Aquifers

The abundance, diversity, and relative distribution of sulfate-reducing bacteria (SRB) in high arsenic (As) groundwater aquifers of Hangjinhouqi County in the Hetao Basin, Inner Mongolia was investigated using denaturing gradient gel electrophoresis (DGGE) and quantitative polymerase chain reaction (qPCR) analysis of dsrB genes (encoding dissimilatory sulfite reductase beta-subunit). DGGE results revealed that SRB populations were diverse, but were mainly composed of Desulfotomaculum, Desulfobulbus, Desulfosarcina, and Desulfobacca. The abundance of Desulfobulbus was positively correlated with the ratio of Fe(II)/Fe(III). Although qPCR results showed that the dsrB gene abundance in groundwater samples ranged from below detection to 4.9 × 10⁶ copies/L, and the highest percentage of dsrB gene copies to bacterial 16S rRNA gene copies was 2.1%. Geochemical analyses showed that As(III) content and the ratio of Fe(II) to Fe(III) increased with total As, while sulfate concentrations decreased. Interestingly, the dsrB gene abundance was positively correlated with As concentrations. These results indicate that sulfate reduction occurs simultaneously with As and Fe reduction, and might result in increased As release and mobilization when As is not incorporated into iron sulfides. This study improves our understanding of SRB and As cycling in high As groundwater systems.     

Arsenic contamination of groundwater and prevalence of arsenical dermatosis in the Hetao plain area,Inner Mongolia,China

The present study determined cardiac chamber-specific alterations of the expression of the atrial and brain natriuretic peptide (ANP and BNP) genes with a small increase in age beyond adulthood and with systemic hypertension of intermediate duration. The expression distributions of these genes was determined using in situ hybridization in the right and left atria (RA and LA), and the right and left ventricles (RV and LV) in Wistar Kyoto rats (WKY) and age-matched Spontaneously Hypertensive rats (SHR) at ages 6 months (adult) and 8 months (advanced-age beyond adulthood).In all rat groups, both genes were expressed (ANP > BNP) in the LA and LV, and were not expressed in the RA and RV. The genes were expressed in the LA in all rat groups; the ANP, but not the BNP, expression increased with advancing age and with superimposed hypertension. They were expressed in the LV of the advanced-age WKY, adult and advanced-age SHR, but not in the adult WKY. The ANP mRNA labeling in the LA was diffuse and interspersed with dense accumulations, whereas BNP labeling was diffuse. The labeling of both genes in the form of sparse clusters was seen in the LV of the advanced-age SHR. Our study showed that ANP and BNP expression in left heart chambers increased with a small increase in age, with hypertension of intermediate duration, and with modest left ventricular hypertrophy. The chamber-specific expression distribution could be due to special groups of cardiac cells, or to local chamber-specific factors.     

Microbial Biogeography of Six Salt Lakes in Inner Mongolia,China, and a Salt Lake in Argentina

We used cultivation-independent methods to investigate the prokaryotic biogeography of the water column in six salt lakes in Inner Mongolia, China, and a salt lake in Argentina. These lakes had different salt compositions and pH values and were at variable geographic distances, on both local and intercontinental scales, which allowed us to explore the microbial community composition within the context of both contemporary environmental conditions and geographic distance. Fourteen 16S rRNA gene clone libraries were constructed, and over 200 16S rRNA gene sequences were obtained. These sequences were used to construct biotic similarity matrices, which were used in combination with environmental similarity matrices and a distance matrix in the Mantel test to discover which factors significantly influenced biotic similarity. We showed that archaeal biogeography was influenced by contemporary environmental factors alone (Na⁺, CO₃²⁻, and HCO₃⁻ ion concentrations; pH; and temperature). Bacterial biogeography was influenced both by contemporary environmental factors (Na⁺, Mg²⁺, and HCO₃⁻ ion concentrations and pH) and by geographic distance.Biogeography aims to explain spatial patterns of diversity in the context of evolutionary events such as speciation, dispersal, extinction, and species interactions (42). Macroecologists have long studied the biogeography of higher plants and animals in various habitats (9, 13). In contrast, there is very little information available on the biogeography of prokaryotes. This stemmed from the difficulty of assessing microbial communities by cultivation methods, which only sampled 0.1 to 10% of the microbial community (30). However, with the advent of cultivation-independent sequencing techniques, microbial communities of many environments have been characterized, including soil (43), the Arctic and Antarctic Oceans (5), and the Sargasso Sea (61). This in turn facilitated prokaryotic biogeography studies in a number of environments on scales ranging from 20,000 km to 0.002 km (42).A study of the biogeography of soil bacteria across the Americas showed that differences were largely attributed to soil pH, with higher diversity observed in neutral soils (20). Bacterial communities in an estuary in Massachusetts were found to vary with the salinity gradient (14). Such studies demonstrated that environmental parameters influenced biogeographical patterns in microbial diversity. Further studies demonstrated that biogeography of hot spring cyanobacteria, hyperthermophilic archaea, and Pseudomonas strains was influenced by geographic distance, which led to isolation of disparate populations and subsequent genetic divergence (12, 51, 63). The apparent allopatric speciation demonstrated in these studies therefore contested the idea that prokaryotes were not affected by limits to dispersal due to their small size, abundance, and metabolic plasticity (i.e., “everything is everywhere” [see below]) (21).A simple framework was suggested to distinguish between the effects of evolutionary events and contemporary environmental conditions on the spatial variation of microbial diversity (42). At the center of this framework were four hypotheses. The null hypothesis stated that microorganisms were distributed randomly over space. Upon rejection of the null hypothesis, the second hypothesis stated that spatial variation reflected the influence of contemporary environmental variation. It assumed that geographic distance did not affect diversity due to the wide dispersal of microorganisms. This hypothesis represents the famously quoted “everything is everywhere; the milieu selects” by Baas-Becking (4, 6). The third hypothesis stated that variation was shaped by evolutionary events (geographic distance) that limited dispersal and that past environmental conditions led to genetic divergence between different microbial assemblages. The fourth hypothesis stated that the biogeography of microorganisms was determined by both contemporary environmental conditions and past evolutionary events (geographic distance). It is important to note here the possibility that evolutionary events can be represented by geographic distances. (For more details on this framework, see reference 42.)Many studies have been carried out on salt lakes and salterns around the world (28), but few have tried to explain variations in microbial community composition. Those that did identified salinity, altitude, redox and ionic concentration, pO₂, and seasonal events as relevant factors (7, 11, 16, 17, 34, 35, 38, 65). To our knowledge, only two studies have looked at the effect of intercontinental geographic distances on microbial community composition in salt lakes. Foti and colleagues looked specifically at the biogeography of Thioalkalivibrio in soda lakes across Mongolia, Kenya, California, Egypt, and Siberia and found that these bacteria showed a tendency for endemism; hence, geographic distance was a significant factor in influencing community composition (22). A further study looked at the biogeography of Salinibacter ruber strains from salterns in the Mediterranean, Atlantic, and Peruvian regions using a metabolomic approach. Geographically distinct strains were distinguished by characteristic metabolites (58).We examined the prokaryotic community composition in several salt lakes using ribosomal DNA methods. Six of the salt lakes in this study were situated on the Inner Mongolian steppe, northwest of Beijing, which had an average elevation of 1,000 to 2,000 m above sea level. The lakes were mostly several hundred kilometers apart (0.147 to 395.2 km) and were in different climate and vegetation zones: from typical grassland steppe in the north and east to desert steppe bordering the Gobi desert in the south and west (70). The lakes were Bagaejinnor, Chagannor, Ejinnor, Erliannor, Shangmatala, and an unnamed lake near Xilinhot. Lakes Ejinnor and Erliannor were extensively developed into salterns. Salar Guayatayoc Lake was situated in the same basin as the Salinas Grandes in the Argentine Altiplano at an elevation of 3,432 m, north-west of the city Salta, ∼18,000 km from the other lakes. All salt lakes were athalassohaline, located in arid climates, and subjected to high solar radiation and wide ranges of temperature. The lakes had different salt compositions and allowed us to explore the microbial community composition within the context of both contemporary environmental conditions and geographic distance.Here we describe the microbial diversity of six salt lakes in Inner Mongolia and one salt lake in Argentina. Using the framework previously described, we present evidence that biogeography of Archaea in these salt lakes was significantly influenced (P < 0.05) by environmental factors (Na⁺, CO₃²⁻, and HCO₃⁻ ion concentrations, pH, and temperature), but not geographic distance, consistent with the previously stated hypothesis 2. We also show that the biogeography of Bacteria was significantly influenced (P < 0.05) by both environmental factors (Na⁺, Mg²⁺, and HCO₃⁻ ion concentrations and pH) and geographic distance, consistent with the previously stated hypothesis 4.     

Microbial Community Structure and Arsenic Biogeochemistry in an Acid Vapor-Formed Spring in Tengchong Geothermal Area,China

Arsenic biogeochemistry has been studied extensively in acid sulfate-chloride hot springs, but not in acid sulfate hot springs with low chloride. In this study, Zhenzhuquan in Tengchong geothermal area, a representative acid sulfate hot spring with low chloride, was chosen to study arsenic geochemistry and microbial community structure using Illumina MiSeq sequencing. Over 0.3 million 16S rRNA sequence reads were obtained from 6-paired parallel water and sediment samples along its outflow channel. Arsenic oxidation occurred in the Zhenxhuquan pool, with distinctly high ratios of arsenate to total dissolved arsenic (0.73–0.86). Coupled with iron and sulfur oxidation along the outflow channel, arsenic accumulated in downstream sediments with concentrations up to 16.44 g/kg and appeared to significantly constrain their microbial community diversity. These oxidations might be correlated with the appearance of some putative functional microbial populations, such as Aquificae and Pseudomonas (arsenic oxidation), Sulfolobus (sulfur and iron oxidation), Metallosphaera and Acidicaldus (iron oxidation). Temperature, total organic carbon and dissolved oxygen significantly shaped the microbial community structure of upstream and downstream samples. In the upstream outflow channel region, most microbial populations were microaerophilic/anaerobic thermophiles and hyperthermophiles, such as Sulfolobus, Nocardia, Fervidicoccus, Delftia, and Ralstonia. In the downstream region, aerobic heterotrophic mesophiles and thermophiles were identified, including Ktedonobacteria, Acidicaldus, Chthonomonas and Sphingobacteria. A total of 72.41–95.91% unassigned-genus sequences were derived from the downstream high arsenic sediments 16S rRNA clone libraries. This study could enable us to achieve an integrated understanding on arsenic biogeochemistry in acid hot springs.     

Microbial Diversity and Biogeochemistry of a Shallow Pristine Canadian Shield Groundwater System

An investigation was conducted to assess the microbial diversity and biogeochemistry of a pristine shallow glaciofluvial groundwater system on the Canadian Shield. Vadose zone sands were very fine-grained, consisting mostly of iron oxide-coated quartz. Below the water table in the saturated zone, iron oxide-coating on quartz grains were absent, owing presumably to reductive dissolution by Fe(III)-reducing bacteria and chemical weathering, respectively. Groundwater pH was circumneutral at 6.4 + 0.1, and Eh was slightly reducing at 349 ± 15 mV compared to local surface waters at 417 ± 21 mV; the total dissolved solids concentration in groundwater was 45.2 ± 6.9 mg/L. A total of 269 clones were sequenced and compiled into a 16S rRNA gene library, and representative operational taxonomic units (OTU) were retrieved from basic local alignment search tool (BLAST) analyses at the species-level across 7 phyla, including Acidobacteria, Actinobacteria, Bacteroidetes, Chlorobi, Firmicutes, Planctomycetes, and Proteobacteria. Aerobic, anaerobic, and facultative anaerobic heterotrophs were predominant among the OTU. Lithoautotrophic ammonium- and nitrite-oxidizers were especially prominent, as were diazotrophs, nitrate- and nitrite-reducers. Representative OTU also included Fe(II)-oxidizers and Fe(III)-reducers, whereas those associated with sulfur cycling were rare. These observations suggest that there is considerable potential for biogeochemical cycling of nitrogen and iron within shallow glaciofluvial groundwater systems on the Canadian Shield.     

Eocene fossil rodent assemblages from the Erlian Basin (Inner Mongolia,China): Biochronological implications

Rodents from the Nuhetingboerhe-Huheboerhe area in the Erlian Basin, Inner Mongolia, differ stratigraphically: primitive ctenodactyloids such as Chenomys and Yuanomys are dominant in the upper part of the Nomogen Formation; Tamquammys dominates in the Arshanto Formation; Asiomys, Pappocricetodon, and Yuomys appear in the lower part of the Irdin Manha Formation and Tamquammys is rarer in this formation than in the Arshanto Formation. The assemblage of the upper part of the Nomogen Formation is similar to that of the Lingcha Formation of Hunan, the Wutu Formation of Shandong, the Yuhuangding Formation of Hubei, and the Bumban Member of the Nara-Bulak Formation of Mongolia. The assemblage in the upper part of the Arshanto Formation is correlated with that from the locality Andarak 2 in Kyrgyzstan. The assemblage from the lower part of the Irdin Manha Formation resembles that of the lower part of the Hetaoyuan Formation of Henan.On the basis of the comparison of the rodent assemblages, I consider that the age of upper part of the Nomogen Formation corresponds to the Bumbanian land mammal age. The Bumbanian, Arshantan, and Irdinmanhan land mammal ages are correlated respectively to the early Ypresian, the middle–late Ypresian, and the early Lutetian of the Geological Time Scale. The Bumbanian and Irdinmanhan land mammal ages are also correlated to the early Wasatchian and the early Uintan (or the later Bridgerian) of the North American Land Mammal Ages.     

A new middle Miocene pliopithecid from Inner Mongolia, China

In addition to the new fragments of the Omo I skeleton, renewed fieldwork in the Kibish Formation along the lower reaches of the Omo River in southwestern Ethiopia has yielded new hominin finds from the Kibish Formation. The new finds include four heavily mineralized specimens: a partial left tibia and a fragment of a distal fibular diaphysis from Awoke's Hominid Site (AHS), a parietal fragment, and a portion of a juvenile occipital bone. The AHS tibia and fibula derive from Member I and are contemporaneous with Omo I and II. The other specimens derive from Chad's Hominid Site (CHS), and derive from either Member III or IV, which constrains their age between approximately 8.6 and approximately 104ka.     

锡林河流域一个羊草群落中土壤呼吸与生物量之间的相关性分析(英)

采用根系生物量梯度上土壤呼吸变化趋势线外推法对锡林河流域一个羊草 (Leymuschinensis (Trin .)Tzvel.)群落中根系呼吸占土壤总呼吸的比例进行了估计 ,对生物量各组分 (地上、地下部分 )之间以及它们与土壤呼吸间的相关性进行了分析。结果表明 :在测定年度 (1998年 )整个生长季的不同月份 ,该群落中根系呼吸量占土壤呼吸总量的比例在 14 %～ 39%之间 ,平均为 2 7% ;地上总生物量及根系生物量与土壤呼吸间的相关性较差 ,但地上活生物量与土壤呼吸间存在着显著的乘幂关系。上述结果与国外同类研究结果相比 ,具有很好的一致性。     

Light Use Efficiency over Two Temperate Steppes in Inner Mongolia, China

Vegetation light use efficiency (LUE) is a key parameter of Production Efficiency Models (PEMs) for simulating gross primary production (GPP) of vegetation, from regional to global scales. Previous studies suggest that grasslands have the largest inter-site variation of LUE and controlling factors of grassland LUE differ from those of other biomes, since grasslands are usually water-limited ecosystems. Combining eddy covariance flux data with the fraction of photosynthetically active radiation absorbed by the plant canopy from MODIS, we report LUE on a typical steppe and a desert steppe in Inner Mongolia, northern China. Results show that both annual average LUE and maximum LUE were higher on the desert steppe (0.51 and 1.13 g C MJ(-1)) than on the typical steppe (0.34 and 0.88 g C MJ(-1)), despite the higher GPP of the latter. Water availability was the primary limiting factor of LUE at both sites. Evaporative fraction (EF) or the ratio of actual evapotranspiration to potential evapotranspiration (AET/PET) can explain 50-70% of seasonal LUE variations at both sites. However, the slope of linear regression between LUE and EF (or AET/PET) differed significantly between the two sites. LUE increased with the diffuse radiation ratio on the typical steppe; however, such a trend was not found for the desert steppe. Our results suggest that a biome-dependent LUE(max) is inappropriate, because of the large inter-site difference of LUE(max) within the biome. EF could be a promising down-regulator on grassland LUE for PEMs, but there may be a site-specific relationship between LUE and EF.     

内蒙古锡林浩特市鸟类资源调查

2005年5月至2006年11月,采用固定样点法和样带法,对内蒙古自治区锡林浩特市的鸟类资源进行了调查.共记录到鸟类186种,隶属于18目42科98属.其中,留鸟27种,夏候鸟104种,冬候鸟1种,旅鸟54种.鸟类区系以古北界成分为主,有117种,占繁殖鸟总数的88.6%.国家Ⅰ级重点保护鸟类5种,国家Ⅱ级重点保护鸟类28种.湿地生境中鸟类资源最为丰富,有134种.鸟类的G-F指数为0.81.     

Rates of Microbial Metabolism in Deep Coastal Plain Aquifers

Rates of microbial metabolism in deep anaerobic aquifers of the Atlantic coastal plain of South Carolina were investigated by both microbiological and geochemical techniques. Rates of [2-¹⁴C]acetate and [U-¹⁴C]glucose oxidation as well as geochemical evidence indicated that metabolic rates were faster in the sandy sediments composing the aquifers than in the clayey sediments of the confining layers. In the sandy aquifer sediments, estimates of the rates of CO₂ production (millimoles of CO₂ per liter per year) based on the oxidation of [2-¹⁴C] acetate were 9.4 × 10⁻³ to 2.4 × 10⁻¹ for the Black Creek aquifer, 1.1 × 10⁻² for the Middendorf aquifer, and <7 × 10⁻⁵ for the Cape Fear aquifer. These estimates were at least 2 orders of magnitude lower than previously published estimates that were based on the accumulation of CO₂ in laboratory incubations of similar deep subsurface sediments. In contrast, geochemical modeling of groundwater chemistry changes along aquifer flowpaths gave rate estimates that ranged from 10⁻⁴ to 10⁻⁶ mmol of CO₂ per liter per year. The age of these sediments (ca. 80 million years) and their organic carbon content suggest that average rates of CO₂ production could have been no more than 10⁻⁴ mmol per liter per year. Thus, laboratory incubations may greatly overestimate the in situ rates of microbial metabolism in deep subsurface environments. This has important implications for the use of laboratory incubations in attempts to estimate biorestoration capacities of deep aquifers. The rate estimates from geochemical modeling indicate that deep aquifers are among the most oligotrophic aquatic environments in which there is ongoing microbial metabolism.     

Photosynthetic Pathway Types in Rangeland Plant Species from Inner Mongolia,North China

Photosynthetic pathway types, based on ¹³C measurements, were determined for 125 species in 95 genera and 32 families growing in rangelands from Inner Mongolia. Of the total species, 4 species from 3 genera and 2 families had C₄ photosynthesis (2 species in Gramineae and 2 in Chenopodiaceae) and 118 species from 90 genera and 31 families had C₃ photosynthesis. The number of C₄ species differed significantly among four rangeland sites, 4 species in desert, 3 species in steppe, but no C₄ species were identified in meadow and dune. Six species [e.g. Agriophyllum arenarium Bieb., Bassia dasyphylla O. Kuntze, Saussurea japonica (Thunb.) DC.] earlier identified as C₄ species using the enzyme ratio method were found as C₃ species using the carbon isotope ratios (¹³C). Hence the enzyme ratio method for C₃ and C₄ identification may not always be reliable. The ¹³C values of 3 species of Crassulaceae, which had been considered as CAM species, differed remarkably [–25.79 for Sedum aizoon L., –24.42 for Osostachys fimbriatus (Turcz.) Berger, and –16.97 for O. malacophyllus (Pall.) Fisch], suggesting that the use of ¹³C method as a diagnosis for CAM photosynthetic pathway type may not always be reliable and supplementary measurements are needed.     

Niche characteristics of rodents by diverse disturbance in Alashan desert, Inner Mongolia, China

Four diverse disturbance types, namely, farmland, rotationally grazed grassland, overgrazed grassland and forbidden grazing grassland, were identified in the Alashan desert region of Inner Mongolia. Rodents were sampled in April, July and October in 2002 and 2003 using the trap-day method. Their spatial and temporal niches among the four disturbance types were assessed using the Shannon-Wiener niche breadth index and the Pianka niche overlap index. The Shannon-Wiener niche breadth index was the highest for Allactaga sibirica and Meriones meridianus (0.925 and 0.908, respectively), intermediate for Cricetulus eversmanni, Phodopus roborovskii and Citellus dauricus (0.789, 0.782 and 0.711, respectively), and lowest for Cardiocranius paradoxus (0.003). The Pianka niche overlap indices of six-paired species were the highest and varied from 0.900 to 1.000, suggesting their spatial niche overlapped almost completely. Conversely, the spatial niche overlap index for Meriones unguiculatus, Cardiocranius paradoxus, and Salpingotus kozlovi was zero, thus indicating a complete absence of competition among them. In addition, the temporal niche breadth and overlap indices varied greatly in relation to disturbance types and season. The level of temporal niche overlap in spring and autumn was low while in summer it was high. For all disturbance types and for each season, the temporal niche overlap index of Meriones meridianus and Cricetulus barabansis was always highest but for Meriones unguiculatus and Salpingotus kozlovi always lowest. __________ Translated from Acta Ecologica Sinica, 2005, 25(10): 2,637–2,643 [译自: 生态学报]     

Niche characteristics of rodents by diverse disturbance in Alashan desert,Inner Mongolia,China

Four diverse disturbance types,namely,farmland,rotationaUy grazed grassland,overgrazed grassland and forbidden grazing grassland,were identified in the Alashan desert region of Inner Mongolia.Rodents were sampled in April,July and October in 2002 and 2003 using the trap-day method.Their spatial and temporal niches among the four disturbance types were assessed using the Shannon-Wiener niche breadth index and the Pianka niche overlap index.The Shannon-Wiener niche breadth index was the highest for Allactaga sibirica and Meriones meridianus (0.925 and 0.908,respectively),intermediate for Cricetulus eversmanni,Phodopus roborovskii and Citellus dauricus (0.789,0.782 and 0.711,respectively),and lowest for Cardiocranius paradoxus (0.003).The Pianka niche overlap indices of six-paired species were the highest and varied from 0.900 to 1.000,suggesting their spatial niche overlapped almost completely.Conversely,the spatial niche overlap index for Meriones unguiculatus,Cardiocranius paradoxus,and Salpingotus kozlovi was zero,thus indicating a complete absence of competition among them.In addition,the temporal niche breadth and overlap indices varied greatly in relation to disturbance types and season.The level of temporal niche overlap in spring and autumn was low while in summer it was high.For all disturbance types and for each season,the temporal niche overlap index of Meriones meridianus and Cricetulus barabansis was always highest but for Meriones unguiculatus and Salpingotus kozlovi always lowest.