垃圾填埋场渗滤液中古细菌群落16S rRNA基因的ARDRA分析

利用特异性的引物对,选择性扩增垃圾填埋场渗滤液中古细菌群落的18S rRNA基因片断,在此基础上建立16S rDNA克隆文库,经古细菌通用寡核苷酸探针的原位杂交筛选后,克隆文库内古细菌16S rDNA扩增片断的多样性通过ARDRA分析（amplified rDNA restriction analysis)而获得,利用PCR将各组重克隆子内的16S rDNA外源片断再扩增出来后,两种限制性内切酶－Hha I和HaeⅢ－被分别用于16S rDNA克隆片断的限制酶切分析,结果表明,随机选出的70个古细菌16S rDNA克隆片断被妥为21个不同的ARDRA型（组）,其中的两个优势型总共占了所有被分析克隆子的60％,而其余19个型的相对丰度均处于较低的水平,当中的14个型更仅含有1个克隆子,通过对16S rRNA基因的PCR扩增,克隆及其ARDRA分析,能快速地获得有关填埋场渗滤液中古细菌群落的结构及其多样性的初步信息。     

Response of Aerobic Anoxygenic Phototrophic Bacterial Diversity to Environment Conditions in Saline Lakes and Daotang River on the Tibetan Plateau,NW China

Variations of the pufM gene [encoding the M subunit of the photosynthetic reaction center in aerobic anoxygenic phototrophic (AAnP) bacteria] diversity in response to environmental changes were investigated in waters of six aqueous regimes (including Daotang River and five saline/hypersaline lakes on the Tibetan Plateau) representing a full salinity gradient from freshwater to NaCl-saturation. AAnP bacterial community structures responded to salinity change: Gamma-like AAnP community was predominant in freshwater Daotang River (0.01% salinity). AAnP community structure shifted from Loktanella-like sequences of the Alphaproteobacteria in saline Qinghai Lake to Roseobacter-like sequences in hypersaline lakes (Gahai, Xiaochaidan and Charhan). In addition to salinity, other environmental variables (e.g. N and P availability, TOC and/or DOC, and HCO^? ₃/CO^2? ₃ ions) were also important in affecting the pufM gene diversity in hypersaline lakes. These data have important implications for our understanding of the response of AAnP bacterial community to environmental variables in high-altitude aquatic ecosystems.     

Bacterial Community of the Largest Oligosaline Lake,Namco on the Tibetan Plateau

Bacterial abundances and diversity in the surface water of Lake Namco, the largest oligosaline lake on the Tibetan Plateau, were examined using flow cytometry approach and constructing 16S rRNA gene clone libraries. Bacterial abundances were from 0.08 × 10⁶ to 1.6 × 10⁶ cells mL^?1, and were in the reported range of other lakes of the Tibetan Plateau and high mountain regions. Bacterial abundances were significantly correlated with the concentrations of chlorophyll a (chl a), but showed no significant relationship with the dissolved organic carbon (DOC), which suggested that the amount of DOC released by algae was the key factor determining the bacterial abundance rather than the total DOC. The total trace elements concentrations also obviously connected with bacterial abundances, and 9 of 20 elements showed significant relationship. Bacterial 16S rRNA gene clone sequences were affiliated to the α-, β-, γ-, δ-, and ?-Proteobacteria, Actinobacteria, Bacteroidetes, Cyanobacteria, Firmicutes, Acidobacteria, Planctomycetes, Verrucomicrobia, Candidate division OD1, or unclassified, and among these the β-Proteobacteria dominated. Bacteria in Lake Namco were most closely related to those retrieved from freshwater habitats. Relatively few sequences were closely related to those recovered from saline habitats. Eleven of 34 typical freshwater bacterial clusters were detected in the oligosaline Lake Namco. Bacterial diversity within the lake varied and was connected with the concentrations of DOC and chl a.     

Phylum-Level Archaeal Distributions in the Sediments of Chinese Lakes With a Large Range of Salinity

Uncovering microbial diversity and their influencing factors is a primary goal for microbial ecology. In comparison with studies on bacterial diversity, limited is known about archaeal diversity and its response to influencing factors in lakes. Here, we investigated the archaeal community compositions (ACCs) and their correlation with spatial/environmental factors in the sediments from 38 Chinese lakes with a large range of salinity (0.2–363.1 g/l) and pairwise geographic distance (3–3656 km). Illumina-Miseq sequencing was employed to characterize the ACCs in the lakes samples. The results showed that Euryarchaeota, Bathyarchaeota, Thaumarchaeota, and Woesearchaeota were the dominant archaeal phyla in the studied samples, and they each can occur in the samples with a wide range of salinity (0.2–363.1 g/l) although their abundance was relatively low (<1%) in certain samples. The Thaumarchaeota and Woesearchaeota phyla dominated (up to 90% of total sequences) some lake sediments. Mantel test indicated that compositions of total archaeal community and the Euryarchaeota and Woesearchaeota populations were significantly (p < 0.05) correlated with geographic distance in the studied lake sediments. Salinity was the most important environmental factor influencing the compositions of the total archaeal community and the Euryarchaeota population, while it did not show significant influence on the distribution of the Woesearchaeota and Thaumarchaeota populations. Taken together, this survey expands our current knowledge on the ecology of lacustrine archaea and give clues for studying the archael role in biogeochemical cycles in lakes.     

一株青藏高原冻土溶栓菌的筛选及鉴定

【目的】心脑血管疾病是一种世界性疾病,严重危害人类健康,溶栓酶是治疗该病的有效药物之一。而极端环境中的溶栓微生物因其特殊的生存方式,可能分泌高效、安全的新型溶栓酶。因此,为了获得这种具有特殊功能的溶栓酶,我们从青藏高原高海拔冻土中进行了溶栓菌的筛选。【方法】首先,本文通过血粉-琼脂平板初步筛选具有血粉水解功能的菌株,然后对其进行体外溶栓试验以检验其人工血栓溶解功能,并用纤维蛋白平板法测定其纤溶活性,最后通过生理生化试验和16S rRNA基因序列分析方法对该菌进行分类鉴定。【结果】本文从青海省玉树藏族自治州海拔4300 m的冻土样品中筛选获得了菌株DR-536,不仅具有水解血粉的功能,还具有体外溶栓功能,且能够水解纤维蛋白,纤溶活性为51.80 IU/mL(以尿激酶为标准)。最后,分类鉴定结果显示菌株DR-536是一株金黄节杆菌(Arthrobacter aurescens)。【结论】本文首次从青藏高原高海拔土壤中进行了溶栓菌的筛选,并获得了一株新型溶栓菌,为进一步研究和开发高效、安全的新型溶栓酶提供了菌源。     

西藏米拉山土壤古菌16S rRNA及amoA基因多样性?分析

摘要：【目的】硝化作用在全球土壤氮循环中具有重要的作用,虽然细菌一度被认为单独负责催化这个过程的限速步骤,但是最近一些研究结果表明泉古菌具有氨氧化的能力。本文通过构建古菌16S rRNA 基因克隆文库和氨氧化古菌amoA基因文库,分析西藏米拉山高寒草甸土壤中古菌及氨氧化古菌群落结构组成情况,为揭示青藏高原高寒草甸土壤古菌的多样性提供理论基础。【方法】采用未培养技术直接从土壤中提取微生物总DNA,分别利用通用引物构建古菌16S rRNA 基因和氨氧化古菌amoA基因克隆文库。【结果】通过构建系统发育树,表明古菌16S rRNA 基因克隆文库包括泉古菌门和未分类的古菌两大类,并且所有泉古菌均属于热变形菌纲。氨氧化古菌amoA基因克隆文库中序列均为泉古菌。通过DOTUR软件分析,古菌16S rRNA基因和古菌amoA基因克隆文库分别包括64个OTUs和 75个OTUs。【结论】西藏米拉山高寒草甸土壤中古菌多样性比较丰富,表明古菌在高寒草甸土壤的氮循环中可能具有重要的作用。所获得的一些序列与已知环境中土壤、淡水及海洋沉积物中获得的一些序列具有很高的相似性,其古菌及氨氧化古菌来自不同环境的可能性比较大,可能与青藏高原的地质历史变迁过程有关。米拉山古菌及氨氧化古菌与陆地设施土壤中相似性最高,说明与西藏米拉山高寒草甸土壤的退化有关。     

PCR-RFLP法探讨三个人工湖微生物群落多样性

目的：探讨牡丹江市区三个人工湖（月牙湖、牛角湖、南湖）的微生物群落多样性。方法：从三个水样中分别提取微生物DNA,选取通用引物扩增16S rDNA片段,对扩增产物进行RFLP分析。结果：不同的样品由于其中的微生物多样性的差异,酶切产物在凝胶上显示的相对位置和条带数目都有一定差异。结论：牛角湖样品的条带数目最多,表明牛角湖的微生物群落多样性最为丰富。     

Community Structure of Archaea in the Water Column above Gas Hydrates in the Gulf of Mexico

Microorganisms play fundamental roles in the ecosystem of the Gulf of Mexico (GOM), yet their vertical distributions along the depth continuum of water column are not well known. In this study, we presented the 16S rDNA sequences and lipid profiles in the context of water chemistry to characterize the archaeal community structure above a gas hydrate mound (MC 118) in GOM. Our results showed that all archaeal sequences were related to unknown species of Crenarchaeota or Euryarchaeota. Phylogenetically, group II –β Euryarchaeota dominated the surface water and mid-depth (400-m) water (74% and 58% of total archaeal species, respectively) whereas the marine group I-γ Crenarchaeota dominated the bottom (869 m) water (61% of total archaeal species). Estimates of the Shannon index showed the highest diversity of planktonic Archaea at the 400 m depth. Glycerol dialkyl glycerol tetraether (GDGT) lipids were detected from the 400- and 869-m depths only and characterized by relatively high abundances of GDGT-5 (crenarchaeol) and GDGT-0. Our studies suggested a possible zonation of archaeal community in the water column, which did not seem to be affected by the possible venting of hydrocarbons from the hydrate location in GOM.     

Salinity Impact on Bacterial Community Composition in Five High-Altitude Lakes from the Tibetan Plateau,Western China

The influence of salinity and geographical distance on bacterial community composition (BCC) in five freshwater, oligosaline or polysaline lakes located at altitudes higher than 4400 m on the central and southern Tibetan Plateau were investigated using the 16S rRNA gene clone library approach together with multivariate analysis of environmental variables. A total of 10 clone libraries were constructed with two libraries in each lake, one in the epilimnion and the other in the hypolimnion. Geographical distance was not found to impact BCC significantly, but salinity, chl a and lake hydraulic retention time were significant factors influencing the BCC. Bacteria in lakes located on the central and southern Plateau owned the same community composition as that observed from the eastern Tibetan lakes. They were both predominated by Bacteroidetes and Cyanobacteria, had low taxon richness, and similar typical freshwater clusters and distributed characteristics. Supplemental materials are available for this article. Go to the publisher's online edition of Geomicrobiology Journal to view the supplemental file.     

Homogenisation of water and sediment bacterial communities in a shallow lake (lake Balihe,China)

1. Planktonic and benthic bacterial communities hold central roles in the functioning of freshwater ecosystems and mediate key ecosystem services such as primary production and nutrient remineralisation. Although it is clear that such communities vary in composition both within and between lakes, the environmental factors and processes shaping the diversity and composition of freshwater bacteria are still not fully understood.
2. In order to assess seasonal and spatial variability in lake bacterial communities and identify environmental factors underpinning biogeographical patterns, we performed a large-scale sampling campaign with paired water and sediment sample collection at 18 locations during four seasons in Lake Balihe, a subtropical shallow fish-farming lake in mid-eastern China.
3. Pelagic and benthic bacterial communities were distinctly different in terms of diversity, taxonomic composition and community structure, with Actinobacteria, Bacteroidetes, Cyanobacteria and Alphaproteobacteria dominating lake water, and Acidobacteria, Bacteroidetes, Chloroflexi, Gammaproteobacteria and Deltaproteobacteria dominating sediment. Nevertheless, these two communities had stronger spatial concordance and overlap in taxa during spring and autumn seasons. Together, the main drivers of both the spatial and temporal variations in Lake Balihe bacterial communities were identified as water temperature, turbidity, nitrogen and phosphorus availability, and thermal stratification controlled by wind-mixing and activity of the dense farmed fish populations. Notably, populations affiliated with Firmicutes, known to be abundant in fish gut microbiome, were especially abundant in the summer season and locations where high fish biomass was found, suggesting a potential link between fish gut microbiome and the pelagic bacterial communities.
4. Our findings demonstrated seasonal homogenisation of pelagic and benthic bacterial communities linked to marked shifts in a set of seasonally-driven environmental variables including water temperature and nutrient availability.

     

Detection by polmerase chain reaction-amplification and sequencing of an archaeon in a commercial-scale copper bioleaching plant

An archaeon was detected in the leaching solution from a commercial copper production plant and in copper sulfide ores leached with the solution. The leaching solution in this plant contains a high concentration of sulfate salts. Analysis of the microbial population by polymerase chain reaction-amplification of archaeal 16S rDNAs indicated the presence of a single sequence type. Comparison of the nucleotide sequence of the polymerase chain reaction product with available reference sequences suggested that this archaeon corresponds to a new species of a novel genus and family within the order Thermoplasmales. This archaeon grows in synthetic media but it has not been possible to obtain isolates free of chemolithotrophic bacteria.     

Biogeographic patterns in below-ground diversity in New York City's Central Park are similar to those observed globally

Soil biota play key roles in the functioning of terrestrial ecosystems, however, compared to our knowledge of above-ground plant and animal diversity, the biodiversity found in soils remains largely uncharacterized. Here, we present an assessment of soil biodiversity and biogeographic patterns across Central Park in New York City that spanned all three domains of life, demonstrating that even an urban, managed system harbours large amounts of undescribed soil biodiversity. Despite high variability across the Park, below-ground diversity patterns were predictable based on soil characteristics, with prokaryotic and eukaryotic communities exhibiting overlapping biogeographic patterns. Further, Central Park soils harboured nearly as many distinct soil microbial phylotypes and types of soil communities as we found in biomes across the globe (including arctic, tropical and desert soils). This integrated cross-domain investigation highlights that the amount and patterning of novel and uncharacterized diversity at a single urban location matches that observed across natural ecosystems spanning multiple biomes and continents.     

Archaeal communities in High Arctic wetlands at Spitsbergen, Norway (78 degrees N) as characterized by 16S rRNA gene fingerprinting

Emissions of the greenhouse gas methane from Arctic wetlands have been studied extensively, though little is known about the ecology and community structure of methanogenic archaea that catalyze the methane production. As part of a project addressing microbial transformations of methane in Arctic wetlands, we studied archaeal communities in two wetlands (Solvatnet and Stuphallet) at Spitsbergen, Norway (78 degrees N) during two summer seasons. Directly extracted peat community DNA and enrichment cultures of methanogenic archaea were analyzed by nested PCR combined with denaturing gradient gel electrophoresis and subsequent sequencing of 16S rRNA gene fragments. Sequences affiliated with Methanomicrobiales, Methanobacteriaceae, Methanosaeta and Group I.3b of the uncultured crenarchaeota were detected at both sites. Sequences affiliated with Methanosarcina were recovered only from the site Solvatnet, while sequences affiliated with the euryarchaeotal clusters Rice Cluster II and Sediment 1 were detected only at the site Stuphallet. The phylogenetic affiliation of the recovered sequences suggested a potential of both hydrogenotrophic and acetoclastic methanogenesis at both sites. At Solvatnet, there were clear temporal trends in the archaeal community structure over the Arctic summer season. The archaeal community composition was significantly affected by factors influencing the activity of the overall bacterial community, as measured by in situ emissions of CO2. Methane emissions at both sites were influenced more by peat temperatures and thaw depth than by the archaeal community structure. Enrichment cultures for methanogenic archaea determined that most of the methanogens detected directly in peat could grow in culture at 10 degrees C. Culture based biases were indicated in later enrichment steps by the abundant growth of a Methanosarcina strain that was not detected directly in peat samples.     

Microbial Diversity in the Deep Marine Sediments from the Qiongdongnan Basin in South China Sea

The continental shelf and slope in the northern South China Sea is well known for its prospect of oil/gas/gas-hydrate resources. To study microbial communities and their roles in carbon cycling, a 4.9-m sediment core was collected from the Qiongdongnan Basin on the continental slope of the South China Sea during our cruise HY4-2005-5 in 2005. Geochemical, mineralogical, and molecular phylogenetic analyses were carried out. Sulfate concentration in pore water decreased with depth. Abundant authigenic carbonates and pyrite were observed in the sediments. The bacterial community was dominated by aerobic and facultative organisms. Bacterial clone sequences belonged to the Gamma-, Alpha-, Deltaproteobacteria and Firmicutes group, and they were related to Fe(III) and/or Mn(IV) reducers, sulfate reducers, aromatic hydrocarbon degraders, thiosulfate/sulfite oxidizers, and denitrifiers. Archaeal clone sequences exhibited greater overall diversity than the bacterial clones with most sequences related to Deep-Sea Archaeal Group (DSAG), Miscellaneous Crenarchaeotic Group (MCG), and Uncultured Euryarchaeotic Clusters (UECs). Archaeal sequences related to Methanosarcinales, South African Gold Mine Euryarchaeotic Group (SAGMEG), Marine Benthic Group-D (MBG-D) were also present. Most of these groups are commonly present in deep-sea sediments, particularly in methane/organic-rich or putative methane hydrate-bearing sediments.     

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.     

Molecular diversity analysis of rumen methanogenic Archaea from goat in eastern China by DGGE methods using different primer pairs

Aims:  To screen a pair of primers suitable for denaturing gradient gel electrophoretic (DGGE) analysis of ruminal methanogenic Archaea and to detect the archaeal communities in the rumen of goat.
Methods and Results:  Nine primer pairs for 16S rDNA of methanogenic Archaea , including six for directed polymerase chain reaction (PCR) and three for nested PCR were first evaluated by PCR amplification of the total DNA from rumen fluids and bacteria. The DGGE analysis of rumen fluids was then conducted with three primer sets (344fGC/915r, 1106fGC/1378r and 519f/915rGC) of the nine pairs tested. Good separation and quality of patterns were obtained in DGGE analysis with primer pairs 1106fGC/1378r and 519f/915rGC. A total of 40 DNA fragments were excised from the DGGE gels and their sequences were determined. All fragments belonged to methanogenic Archaea while primer pair 519f/915rGC had better amplification ranges than the other two primer pairs.
Conclusions:  The procedure of DGGE analysis with primer pair 519f/915rGC was more suitable for investigating methanogenic archaeal community in the rumen. The dominant methanogenic Archaea in the rumen of goat was Methanobrevibacter sp. and an unidentified methanogenic Archaea .
Significance and Impact of the Study:  One pair of primers suitable for DGGE analysis of ruminal methanogenic Archaea was obtained and the molecular diversity of ruminal methanogenic Archaea in goat was investigated by PCR-DGGE.     

Phylogenetic relationships among Rhacophorinae (Rhacophoridae, Anura, Amphibia), with an emphasis on the Chinese species

The partial nucleotide sequence of mitochondrial 12S and 16S rRNA genes was determined for 23 Chinese species of Rhacophoridae (Amphibia: Anura), representing four of the eight recognized genera. Using Buergeriinae as the outgroup, phylogenetic analyses (maximum parsimony, maximum likelihood, and Bayesian inference) were performed in combination with already published mitochondrial 12S and 16S sequences of Rhacophorinae frogs. In all cases, Philautus romeri Smith, 1953 is recovered as the sister taxon to all other Rhacophorinae, although the support values are weak. Chirixalus doriae Boulenger, 1893 is closer to Chiromantis [ Chiromantis rufescens (Günther, 1868) and Chiromantis xerampelina Peters, 1854] than to Chirixalus vittatus (Boulenger, 1887). The clade { Philautus odontotarsus Ye & Fei, 1993, [ Philautus idiootocus (Kuramoto & Wang, 1987), Kurixalus eiffingeri (Boettger, 1895)]} is recovered with strong support. The monophyly of Theloderma and Rhacophorus rhodopus Liu & Hu, 1959 is not supported. It is suggested that Philautus albopunctatus Liu & Hu, 1962 should be placed into the synonymy of Theloderma asperum (Boulenger, 1886), and that Philautus rhododiscus Liu & Hu, 1962 should be assigned to Theloderma , so as to correct the paraphyly. Additionally, the monophyly of ' Aquixalus ' is not supported, and this requires further examination. Results also indicate that the Rhacophorus leucomystax (Gravenhorst, 1829)/ Rhacophorus megacephalus (Hallowell, 1861) complex needs further revision. Studies employing broader sampling and more molecular markers will be needed to resolve the deep relationships within the subfamily Rhacophorinae.  © 2008 The Linnean Society of London, Zoological Journal of the Linnean Society, 2008, 153 , 733–749.     

Soil pH regulates the abundance and diversity of Group 1.1c Crenarchaeota

Archaeal communities in many acidic forest soil systems are dominated by a distinct crenarchaeal lineage Group 1.1c. In addition, they are found consistently in other acidic soils including grassland pasture, moorland and alpine soils. To determine whether soil pH is a major factor in determining their presence and abundance, Group 1.1c community size and composition were investigated across a pH gradient from 4.5 to 7.5 that has been maintained for > 40 years. The abundances of Group 1.1c Crenarchaeota, total Crenarchaeota and total bacteria were assessed by quantitative PCR (qPCR) targeting 16S rRNA genes and the diversity of Group 1.1c crenarchaeal community was investigated by denaturing gradient gel electrophoresis (DGGE) and phylogenetic analysis. The abundance of Group 1.1c Crenarchaeota declined as the pH increased, whereas total Crenarchaeota and Bacteria showed no clear trend. Community diversity of Group 1.1c Crenarchaeota was also influenced with different DGGE bands dominating at different pH. Group 1.1c Crenarchaeota were also quantified in 13 other soils representing a range of habitats, soil types and pH. These results exhibited the same trend as that shown across the pH gradient with Group 1.1c Crenarchaeota representing a greater proportion of total Crenarchaeota in the most acidic soils.     

Community structures of ammonia‐oxidising archaea and bacteria in high‐altitude lakes on the Tibetan Plateau

1. Community structures of planktonic ammonia‐oxidising archaea (AOA) and bacteria (AOB) were investigated for five high‐altitude Tibetan lakes, which could be classified as freshwater, oligosaline or mesosaline, to develop a general view of the AOA and AOB in lakes on the Tibetan Plateau. 2. Based on PCR screening of the ammonia monooxygenase α‐subunit (amoA) gene, AOA were present in 14 out of 17 samples, whereas AOB were detected in only four samples. Phylogenetic analyses indicated that the AOB communities were dominated by a unique monophylogenetic lineage within Nitrosomonas, which may represent a novel cluster of AOB. AOA, on the other hand, were distinct among lakes with different salinities. 3. Multivariate statistical analyses indicated a heterogeneous distribution of the AOA communities among lakes largely caused by lake salinity, whereas the uniform chemical properties within lakes and their geographical isolation may favour relatively homogeneous AOA communities within lakes. 4. Our results suggest a wide occurrence of AOA in Tibetan lakes and provide the first evidence of salinity‐related differentiation of AOA community composition as well as potential geographical isolation of AOA in inland aquatic environments.