Stages Of Biological Soil Crusts Research Articles

Soil depths and developmental stages of biological soil crusts are more important than shrub cover in structuring prokaryotic communities

The influence of microhabitat factors on prokaryotic communities within desert ecosystems, particularly those residing in biological soil crusts (biocrusts), remains poorly understood. This study aimed to elucidate the relative importance of different microhabitats, including soil depths, biocrust developmental stages, and shrub cover, in shaping soil prokaryotic communities. To achieve this, we conducted an in-depth investigation of soil prokaryotic communities using high-throughput amplicon sequencing in the Tengger desert, China. Our results showed that difference of soil properties, prokaryotic alpha, beta diversities and abundances of taxa and functional groups primarily differed between soil depths and among biocrust developmental stages. Furthermore, the impact of shrub cover on the aforementioned parameters was found to be modified by biocrust development. Specifically, we observed higher soil nutrient levels in the upper biocrust layer compared to the subsoil, with a consistent increasing trend during biocrust development in both soil layers. Conversely, soil pH displayed contrasting patterns. Prokaryotic alpha diversity exhibited a V-shaped pattern with biocrust development, initially decreasing and then increasing, and was higher in the subsoil compared to the biocrust layer. Additionally, although prokaryotic alpha diversity showed differences between shrub cover or not, the specific effect depended on biocrust stages. Cyanobacteria, phototrophic and nitrogen-fixing prokaryotes were more abundant in the upper biocrust layer, following a unimodal pattern with biocrust development, initially increasing, and then decreasing; while Actinobacteriota and Acidobacteriota showed higher abundance in the subsoil, with varying trends between the two soil depths during biocrust development. Soil pH and total P emerged as key regulators of prokaryotic communities across different microhabitats. This study contributes to our comprehensive understanding of the complex dynamics governing prokaryotic communities in desert ecosystems.

Changes of bacterial community structure,monosaccharide composition and CO2 exchange along the successional stages ofbiological soil crusts.

Biological soil crusts (BSCs) are a dominantecological landscape of drylands, which have asignificant impact on global biogeochemical flux. However, it is unclear how bacterial community and physiological characteristics vary along the BSCssuccessional stages. In this study, bacterial community composition, physiological characteristics, and monosaccharide composition of extracellular polysaccharides (EPSs)were compared among different successional stages. Our findings demonstrated that besidesthe dominant bacterial species, the bacterial communities also showed considerable differences between these two stages. Cyanobacteria were keystone taxain the early stage, while heterotrophic bacteria (Proteobacteria, Actinobacteria and Acidobacteria) were keystone taxa in the later stages. According to the results ofCO2 exchange, cyanobacterial crusts accumulated net carbon faster than moss crusts, whilemoss crusts had a significantly higher respiration rate. The monosaccharide analysis indicated that the EPSs components also varied depending on BSCs' successional stages. Specifically, the contents of rhamnose and arabinose were higher in thecyanobacterial cruststhan other types of crusts, while the contents of fucose, xylose, mannose and glucose were the highest in cyanobacterial-lichen crusts, andgalactose contentwas highest inthe moss crusts. Altogether, our results stress the heterogeneous variation of BSCs along with succession, andthis work offered a fresh viewpoint for a deeper comprehension of the interactions between the monosaccharide components of EPS and the networks of bacterial communities in BSCs.

Stimulating effects of snow cover on gaseous nitrogen emissions are intensified by biological soil crusts

Winter weather patterns are changing due to global climate change, which impacts the soil nitrogen cycle and greenhouse gas flux in these ecosystems, particularly the snow cover in temperate deserts. Biological soil crusts are important soil communities of the desert ecosystem and are sensitive to environmental changes. However, knowledge of the responses of gaseous nitrogen emissions from biological soil crusts to changes in snow cover is limited. In this study, the effects of snow cover on gaseous nitrogen emissions and the abundance of nitrifier (amoA) and denitrifier (narG, nirS, nirK, nosZ) genes were investigated in three snow cover treatments (snow removal, ambient snow, and increased snow depth). Snow cover significantly affected N2O and NO emissions from bare sand and biological soil crusts in winter. The abundance of denitrifier genes in bare sand and biological soil crusts and the abundance of nitrifier genes in moss crust increased with the depths of snow addition. N2O emissions increased with the successional stages of biological soil crusts during the winter. Both N2O and NO emissions from bare sand and biological soil crusts peaked in the freeze–thaw period (March) and were lowest in mid-winter (January). The emissions of N2O increased with increasing the abundance of amoA, nirK and nosZ genes. Our findings show that N2O emissions generally increased with increasing snow cover through their effects on nitrogen cycle related functional microbial groups. These effects were regulated by the types of biological soil crust, which can increase the effect of snow cover in winter.

Differences of bacterial communities in different biological soil crusts around thermal power plant and their influencing factors.

To understand the effects of heavy metal pollution derived from atmospheric dust fall on bacterial community structure under different types of biological soil crusts near mining area, we measured the diversity, community composition, and relative abundance of bacteria communities in three different developmental stages of biological soil crusts (BSCs), including algae (ZB), mixed (HB), and moss (TB) crusts, and control (CK, bare soil) around a typical thermal power plant in Ningdong Energy Industrial Base, using the high-throughput sequencing technique. Environmental factors affecting the bacterial community structure were further investigated. The results showed that there were significant differences in physicochemical properties and heavy metal contents among different BSCs. The BSCs were heavily polluted due to the enrichment of heavy metals from atmospheric dust fall. Among the top ten dominant bacterial phyla, Gemmatimonadetes and Cyanobacteria were significantly distinct among different BSCs. Bacterial α diversity decreased in an order of CK>TB>HB>ZB. The NMDS ordination plots indicated that there were significant differences in the bacteria community composition of the three kinds of BSCs and the CK. The correlation analysis showed that the succession of BSCs significantly affected bacterial community composition in BSCs. Bacterial diversity and composition were closely related to pH, nutrients, and heavy metal contents. The relative abundance of Actinomycetes and Chloroflexi was positively correlated with pH, but negatively correlated with total N, total P, and the contents of heavy metal Pb, Zn, Cd. Results of the redundancy analysis showed that organic carbon, pH, total N, and total P were the major soil factors affecting bacterial α diversity, relative abundance of some dominant phyla, whereas heavy metal contents of Zn, Cd, Pb were the major heavy metals affecting structure of bacterial community which inhibited or stimulated the abundance and diversity of bacterial communities. We concluded that pH, heavy metals, and nutrients were the key factors affecting soil bacteria community composition. The succession of BSCs would improve their physicochemical properties and significantly impacted bacterial community composition. Long term heavy metals enrichment would affect bacterial diversity and community composition of BSCs.

Changes in soil carbon sequestration and emission in different succession stages of biological soil crusts in a sand-binding area

BackgroundWe investigated the spatio-temporal dynamics of soil carbon dioxide (CO2)- and soil methane (CH4)-flux during biological soil crust (BSCs) deposition in a sand-binding area in the eastern Chinese Hobq Desert. The trends in soil organic carbon (C) content and density were analyzed during this process. The sampling sites comprised a mobile dune (control) and those with algal, lichen, and moss crust-fixed sands. The desert soil CO2- and CH4-flux, temperature, and water content were measured from May to October in 2017 and 2018. Simultaneously, organic C content and density were measured and analyzed by stratification.ResultsThe spatio-temporal variation in desert soil CO2-flux was apparent. The average CO2- fluxes in the control, algal, lichen, and moss sites were 1.67, 2.61, 5.83, and 6.84 mmol m−2 h−1, respectively, during the growing season, and the average CH4-fluxes in the four sites were − 1.13, − 1.67, − 3.66, and − 3.77 µmol m−2 h−1, respectively. Soil temperature was significantly positively correlated with CO2-flux but could not influence CH4 absorption, and C flux had minimal correlation with soil water content. The soil total organic C density at all sites was significantly different and decreased as follows: moss > lichen > algal > control; moreover, it decreased with soil depth at all sites. The accumulation of desert soil organic C could enhance soil C emissions.ConclusionIn a semi-arid desert, artificial planting could promote sand fixation and BSCs succession; therefore, increasing the C storage capacity of desert soils and decreasing soil C emissions could alter the C cycle pattern in desert ecosystems. Soil temperature is the major factor controlling desert soil CO2 flux and vegetation restoration, and BSCs development could alter the response patterns of C emissions to moisture conditions in desert soils. The results provide a scientific basis for studying the C cycle in desert ecosystems.

Population dynamics of Echinops gmelinii Turcz. at different successional stages of biological soil crusts in a temperate desert in China.

The effects of biological soil crusts (BSC) on vascular plant growth can be positive, neutral or negative, and little information is available on the impacts of different BSC successional stages on vascular plant population dynamics. We analysed seedling emergence, survival, plant growth and reproduction in response to different BSC successional stages (i.e. habitats: bare soil, cyanobacteria, lichen and moss crusts) in natural populations of Echinops gmelinii Turcz. in the Tengger Desert of northwest China. The winter annual E. gmelinii is a dominant pioneer herb after sand stabilisation. During the early stages of BSC succession, the studied populations of E. gmelinii were characterised by high density, plant growth and fecundity. As the BSC succession proceeded beyond moss crusts, the fecundity decreased sharply, which limited seedling recruitment. Differences in seedling survival among the successional stages were not evident, indicating that BSC have little effect on survival in arid desert regions. Moreover, E. gmelinii biomass allocation exhibited low plasticity, and only reproductive allocation was sensitive to the various habitats. Our results further suggest that the negative effects of BSC succession on population dynamics are primarily driven by increasing topsoil water-holding capacity and decreasing rain water infiltration into deeper soil. We conclude that BSC succession drives population dynamics of E. gmelinii, primarily via its effect on soil moisture. The primary cause for E. gmelinii population decline during the moss-dominated stage of BSC succession is decreased fecundity of individual plants, with declining seed mass possibly reducing the success of seedling establishment.

Greenhouse gas fluxes at different growth stages of biological soil crusts in eastern Hobq desert, China.

We analyzed greenhouse gas fluxes at the different growth stages of algae and lichen crusts in fixed sand with mobile dune as control in the eastern Hobq Desert, China, using the spatio-temporal substitution method. We explored the correlation of these fluxes with environmental factors and with biological soil crust growth. The results showed that variation of CO2 fluxes followed the order: lichen crust (128.5 mg·m-2·h-1) > algae crust (70.2 mg·m-2·h-1) > mobile dune (48.2 mg·m-2·h-1). CH4 absorption rates were in the following order: lichen crust (30.4 μg·m-2·h-1) > algae crust (21.2 μg·m-2·h-1) > mobile dune (18.2 μg·m-2·h-1). The N2O fluxes were in the following order: lichen crust (6.6 μg·m-2·h-1) > algae crust (5.4 μg·m-2·h-1) > mobile dune (2.5 μg·m-2·h-1). CO2 emission had obvious seasonal variation, with higher emission in the growing season. CH4 and N2O fluxes had no seaonal variation. CH4 absorption mainly occurred in the growing season and N2O emission mainly occurred in non-growing season. Contents of soil total nitrogen and organic carbon and the abundance of microorganisms were important factors affecting greenhouse gas fluxes. Hydrothermic factors were important for soil CO2 emission, but not for CH4 and N2O fluxes. The cumulative greenhouse gas emissions were gradually increased with vegetation restoration and the development of biological soil crust. The global warming potential increased following an order: lichen crust (1135.7 g CO2-e·m-2·a-1) > algae crust (626.5 g CO2-e·m-2·a-1) > mobile dune (422.7 g CO2-e·m-2·a-1).

Development of bacterial communities in biological soil crusts along a revegetation chronosequence in the Tengger Desert, northwest China

Abstract. Knowledge of structure and function of microbial communities in different successional stages of biological soil crusts (BSCs) is still scarce for desert areas. In this study, Illumina MiSeq sequencing was used to assess the compositional changes of bacterial communities in different ages of BSCs in the revegetation of Shapotou in the Tengger Desert. The most dominant phyla of bacterial communities shifted with the changed types of BSCs in the successional stages, from Firmicutes in mobile sand and physical crusts to Actinobacteria and Proteobacteria in BSCs, and the most dominant genera shifted from Bacillus, Enterococcus and Lactococcus to RB41_norank and JG34-KF-361_norank. Alpha diversity and quantitative real-time polymerase chain reaction (PCR) analysis indicated that bacterial richness and abundance reached their highest levels after 15 years of BSC development. Redundancy analysis showed that silt + clay content and total K were the prime determinants of the bacterial communities of BSCs. The results suggested that bacterial communities of BSCs recovered quickly with the improved soil physicochemical properties in the early stages of BSC succession. Changes in the bacterial community structure may be an important indicator in the biogeochemical cycling and nutrient storage in early successional stages of BSCs in desert ecosystems.

Use of quantitative PCR with the chloroplast gene rps4 to determine moss abundance in the early succession stage of biological soil crusts

The quantitative PCR (qPCR) method was firstly used to measure moss abundance with moss chloroplast gene rps4 as compared to that with cyanobacterial 16S rRNA gene and fungal 25-28S rRNA gene in the early succession stage of biological soil crusts (BSCs). Four sites with three BSC types collected from Hobq Desert of China, representing cyanobacterial-, lichen-, and moss-dominated BSCs were investigated. The copies of the moss rps4 gene, cyanobacterial 16S rRNA gene, and fungal 25-28S rRNA gene, chlorophyll a content, and the community composition variated significantly. The moss rps4 gene copies attained a significant positive correlation with chlorophyll a content and showed a cross-validation with relative moss biomass.

Fractal Scaling of Particle Size Distribution and Relationships with Topsoil Properties Affected by Biological Soil Crusts

BackgroundBiological soil crusts are common components of desert ecosystem; they cover ground surface and interact with topsoil that contribute to desertification control and degraded land restoration in arid and semiarid regions.Methodology/Principal FindingsTo distinguish the changes in topsoil affected by biological soil crusts, we compared topsoil properties across three types of successional biological soil crusts (algae, lichens, and mosses crust), as well as the referenced sandland in the Mu Us Desert, Northern China. Relationships between fractal dimensions of soil particle size distribution and selected soil properties were discussed as well. The results indicated that biological soil crusts had significant positive effects on soil physical structure (P<0.05); and soil organic carbon and nutrients showed an upward trend across the successional stages of biological soil crusts. Fractal dimensions ranged from 2.1477 to 2.3032, and significantly linear correlated with selected soil properties (R2 = 0.494∼0.955, P<0.01).Conclusions/SignificanceBiological soil crusts cause an important increase in soil fertility, and are beneficial to sand fixation, although the process is rather slow. Fractal dimension proves to be a sensitive and useful index for quantifying changes in soil properties that additionally implies desertification. This study will be essential to provide a firm basis for future policy-making on optimal solutions regarding desertification control and assessment, as well as degraded ecosystem restoration in arid and semiarid regions.

不同尺度苔藓结皮土壤性状的空间分布特征

Biological soil crusts are the organic complexes composed of bacteria,cyanobacteria,algae,lichen and moss with soil particles. They play critical roles in desert ecosystems,including enhancing soil stability and fertility,preventing soil erosion by water or wind,facilitating seed germination. Moss crust is the latest successional stage of biological soil crusts in arid and semiarid land,which perform important functions. Most of the studies focused on the difference of soil properties between moss crust and lack of moss crust. Generally,moss crust distributes in patches in interdune areas of sand dunes,it is a small scale. Little is known about its nutrients distribution at patch scale. The aims of this research are to( 1) make sure the strength of soil heterogeneity for moss crust at both quadrate scale and patch scale;( 2) support basic data for moss crust according to patch size. In this study,patch' s area is calculated by Photoshop CS 5. 0. Five soil physiochemical properties were analyzed with standard soil analytical methods. Classical statistics,geostatistic techniques,semivariogram model fitting and mapping methods were used to describe the spatial distribution of soil properties at both scales. The results indicated that there were medium variations for five soil properties of moss crusts at both scales.Coefficient variations of five properties at quadrate scale varied from 12% to 30%. With the exception of total phosphorus,most coefficient valuations of the other four properties at patch scale were less than 20%,which indicated the soil spatial heterogeneity of moss crust at quadrate scale is much stronger than that at patch scale. The spatial autocorrelation of five soil properties at quadrate scale ranged from 65% to 92%. For patch scale, except for total phosphorous, spatialautocorrelations of the other four parameters were over 90%,which means,that the proportion of spatial autocorrelations of moss crust increase with the decreasing of sampling scale. Additionally,the effect of structure factors increased on patch scale with the decreasing proportion of the random factors,which was consistent with the result of spatial autocorrelation. In this study,values of soil water,organic matter and total nitrogen decreased from center of moss patch to edge,however,total phosphorus increased from center to edge at patch scale,which indicated that there was heterogeneity for moss crust patch at micro scale. There was irregular change for total soluble salt at patch scale,but at quadrate scale,total soluble salt content with mosses was much higher than that without mosses,which implied that with the decreasing of sampling scale,the heterogeneity of soil salt disappeared. The autocorrelation ranges of water,organic,total nitrogen and total phosphorus at patch scale were smaller than the diameter of the moss crusts patch,autocorrelation range of total soluble salt was out of patch size,on the whole,autocorrelation ranges in creased with the sampling size. Thus,sampling distance can be increased at quadrate scale, but for patch scale, sampling distance should be reduced to avoid missing the tiny heterogeneity. At both scales,the lowest autocorrelation range of total phosphorus was observed. Therefore,the sampling distance must be short for variation of phosphorus,while for total salt,sampling distance can be increased properly due to its big variation range.

Functional reactivation of photosystem II in lichen soil crusts after long-term desiccation

Aims As an important successional stage of biological soil crusts, lichen soil crusts (LSCs) are often in the dry and inactive state in desert environments, so it is vital for their survival and development in these areas to reactivate the photosynthetic systems during a rehydration event.

Dew formation on the surface of biological soil crusts in central European sand ecosystems

Abstract. Dew formation was investigated in three developmental stages of biological soil crusts (BSC), which were collected along a catena of an inland dune and in the initial substrate. The Penman equation, which was developed for saturated surfaces, was modified for unsaturated surfaces and used for prediction of dewfall rates. The levels of surface saturation required for this approach were predicted using the water retention functions and the thicknesses of the BSCs. During a first field campaign (2–3 August 2011), dewfall increased from 0.042 kg m−2 for the initial sandy substrate to 0.058, 0.143 and 0.178 kg m−2 for crusts 1 to 3, respectively. During a second field campaign (17–18 August 2011), where dew formation was recorded in 1.5 to 2.75-h intervals after installation at 21:30 CEST, dewfall increased from 0.011 kg m−2 for the initial sandy substrate to 0.013, 0.028 and 0.055 kg m−2 for crusts 1 to 3, respectively. Dewfall rates remained on low levels for the substrate and for crust 1, and decreased overnight for crusts 2 and 3 (with crust 3 &gt; crust 2 &gt; crust 1 throughout the campaign). Dew formation was well reflected by the model response. The suggested mechanism of dew formation involves a delay in water saturation in near-surface soil pores and extracellular polymeric substances (EPS) where the crusts were thicker and where the water capacity was high, resulting in elevated vapor flux towards the surface. The results also indicate that the amount of dewfall was too low to saturate the BSCs and to observe water flow into deeper soil. Analysis of the soil water retention curves revealed that, despite the sandy mineral matrix, moist crusts clogged by swollen EPS pores exhibited a clay-like behavior. It is hypothesized that BSCs gain double benefit from suppressing their competitors by runoff generation and from improving their water supply by dew collection. Despite higher amounts of dew, the water availability to the crust community decreases with crust development, which may be compensated by ecophysiological adaptation of crust organisms, and which may further suppress higher vegetation or mosses.

Successional stage of biological soil crusts: an accurate indicator of ecohydrological condition

ABSTRACTBiological soil crusts are a key component of many dryland ecosystems. Following disturbance, biological soil crusts will recover in stages. Recently, a simple classification of these stages has been developed, largely on the basis of external features of the crusts, which reflects their level of development (LOD). The classification system has six LOD classes, from low (1) to high (6). To determine whether the LOD of a crust is related to its ecohydrological function, we used rainfall simulation to evaluate differences in infiltration, runoff, and erosion among crusts in the various LODs, across a range of soil depths and with different wetting pre‐treatments. We found large differences between the lowest and highest LODs, with runoff and erosion being greatest from the lowest LOD. Under dry antecedent conditions, about 50% of the water applied ran off the lowest LOD plots, whereas less than 10% ran off the plots of the two highest LODs. Similarly, sediment loss was 400 g m−2 from the lowest LOD and almost zero from the higher LODs. We scaled up the results from these simulations using the Rangeland Hydrology and Erosion Model. Modelling results indicate that erosion increases dramatically as slope length and gradient increase, especially beyond the threshold values of 10 m for slope length and 10% for slope gradient. Our findings confirm that the LOD classification is a quick, easy, nondestructive, and accurate index of hydrological condition and should be incorporated in field and modelling assessments of ecosystem health. Published in 2012. This article is a U.S. Government work and is in the public domain in the USA.

Do development stages of biological soil crusts determine activity and functional diversity in a sand-dune ecosystem?

Biological soil crusts (BSCs) cover up to 70% of the sparsely-vegetated open spaces in semiarid and arid regions throughout the world and fulfill a wide range of ecological functions. Previous investigations on BSCs mainly focused on the taxonomic or genetic diversity of their components and physical properties, while little attention was given to the functional diversity of microbial community, which plays crucial roles in carbon cycling. In order to distinguish between microbial functional diversity in BSCs with different developmental levels, MicroResp™ plates were used to determine the utilization rate of fifteen added carbon sources. Five types of crusts, A–E, were taken from the western Negev Desert (Israel) during the morning hours of March 2011. Abiotic and biotic variables were measured. The well-developed high-biomass BSCs exhibited pronounced increases in their chlorophyll a and organic-matter content. Higher activity and biomass of microbial communities, as well as higher density of viable microfungi, were also found in the well-developed BSCs. Marked increases in the utilization rates of aromatic acid, carbohydrates and carboxylic acid were consistent with the well-developed crusts. Although the utilization rates of the four carbon groups followed the order: carboxylic acid > amino acid > carbohydrates and aromatic acid, the redundancy analysis revealed that crust A preferred consuming amino acids while crusts C and E preferred carboxylic acids and carbohydrates. No significant differences in functional diversity were observed between BSCs with different developmental levels. More carbon sources, as well as molecular and stable isotopic approaches, should be used in further studies.

Composition of photosynthetic organisms and diurnal changes of photosynthetic efficiency in algae and moss crusts

In Dalateqi region of Inner Mongolia (at eastern edge of Qubqi Desert), man-made algae crusts were constructed with two filamentous cyanobacteria. Two to three years later, the algae crusts began to succeed to moss crusts under some microterrain conditions. In order to characterize the community structure and compare the photosynthetic characteristics in different successional stages of biological soil crusts (BSCs). This paper studied composition of photosynthetic organisms and diurnal changes of photosynthetic efficiency, with microscopic observation and chlorophyll fluorescence monitoring techniques. Compared with the early successional algae crusts, later moss crusts had a higher photosynthetic efficiency, which was closely related with the different community structure of photosynthetic organisms. Further, moss crusts had a higher total photosynthetic biomass, although the algal biomass decreased along the successional sequence. Similar to higher vascular plants, a midday depression of photosynthetic efficiency was detected in BSCs, although the depression extents were different in different successional stages. Analysis demonstrated the depression was mainly caused by non-stomata limitations, and photosynthetically active radiation (PAR) was a significant influencing factor in the down-regulation of photosynthetic efficiency. We conclude, cyanobacterial inoculation effectively promotes the formation, development and seccession of BSCs. Furthermore, the later successional BSCs have a better photosynthetic performance and thus are expected to play a more effective role in desertification control.

Successional stages of biological soil crusts and their microstructure variability in Shapotou region (China)

In order to investigate succession of biological soil crusts (BSCs) and their microstructure variability, we conducted this work in Shapotou revegetation region at the southeast edge of Tengger Deser. The results showed that BSCs generally succeeded as a pathway of “Algae crusts, algae–lichen crusts, lichen crusts, lichen–moss crusts and moss crusts”. Occasionally mosses directly occurred on algae crusts, and BSCs succeeded from algae crusts to moss crusts. Crust vertical stratification was a common phenomenon, from top to bottom an inorganic layer, algae-dense layer and algae-sparse layer were divided in algae crusts; a thallus layer, rhizoid layer and sub-rhizoid layer in lichen crusts; a “stem-leaf” layer, rhizoid layer and sub-rhizoid layer in moss crusts, respectively. The main crust binding organisms varied from filamental cyanobacteria (dominated by Microcoleus) in algae crusts to lichen rhizoids, free-living cyanobacterial filaments and fungal hyphaes in lichen crusts, and to moss rhizoids and fungal hyphaes in moss crusts. The dominant phototrophic organisms varied from Microcoleus (algae) in algae crusts to Collema (lichens) in lichen crusts, and to Bryum (or Didymodon and Tortula; mosses) in moss crusts. Total phototrophic biomass increased while the free-living algal biomass decreased with the succession of BSCs. In addition, exopolysaccharides and fine particles accumulated in the course of development and succession of BSCs, all of which lead to a gradual increase in crust thickness and porosity, while decrease in the bulk density.

Association of ant nests with successional stages of biological soil crusts in the Tengger Desert, Northern China

Biological soil crusts are important cover in arid desert landscapes, yet their importance as habitats to secondary producers such as ants is relatively unknown. This study was conducted to determine if the presence and development of biological soil crusts on dune surfaces stabilized by revegetation facilitates ant establishment and survival. We measured topsoil properties and crustal features during different successional stages, which were characterized by cyanobacteria and algae, lichens, and mosses, respectively. The species richness and abundance (nest density) of ants were closely associated with silt content, soil organic matter, nitrogen and soil moisture, as well as topsoil temperature. However, ant nest distribution was largely dependent on the biomass and thickness of crusts and topsoil. These findings provide evidence that the recovery or development of biological soil crusts on dune surfaces in the Tengger Desert could favor and maintain higher ant species diversity. Therefore, the disturbance of crusts would result in a reduction of ant species richness and abundance in desert systems.

Effects of drought and salt stresses on man-made cyanobacterial crusts

As a primary successional stage of biological soil crusts (BSCs), cyanobacterial crusts form firstly in the arid and semiarid areas. At the same time, they suffer many stress conditions, such as drought, salt, etc. In this study, we constructed man-made cyanobacterial crusts with Microcoleus vaginatus Gom. and comparatively studied the effects of drought and salt stresses on the crusts. The results showed that crust growth and photosynthetic activity was significantly inhibited by the stress conditions ( P < 0.05), and inhibitory effect increased with the increasing stress intensity and treated time. Compared with salt stress, drought completely stopped crust metabolic activity, so the crust biomass was conserved at a higher level, which meant that drought itself might provide the crusts some protection, especially when the crusts simultaneously suffered drought and salt stresses. That is very important for the survival of crusts in the high-salt areas. In addition, to some extent the crusts could adapt to the stress conditions through metabolic adjustment. In our experiment, we found the accumulation of exopolysaccharides (EPS) increased under stress conditions within a certain threshold.

Chlorophytes of biological soil crusts in Gurbantunggut Desert, Xinjiang Autonomous Region, China

In this paper, chlorophytes collected from 253 biological soil crust samples in Gurbantunggut Desert in Xinjiang Autonomous Region, China were studied by field investigation and microscopical observation in lab. The flora composition, ecological distribution of chlorophytes in the desert and dynamic changes of species composition of chlorophytes in different developing stages of biological soil crusts are preliminarily analyzed. Results showed that there were 26 species belonging to 14 genera and 10 families, in which unicellular chlorophytes were dominant. There existed some differences in distribution of varied sand dune positions. The taxa of chlorophytes in leeward of sand dunes are most abundant, but the taxa in windward, interdune and the top of sand dunes reduced gradually. Chlorophytes were mainly distributed within the crust and the taxa of chlorophytes decrease obviously under the crust. In the developing stages of the biological soil crust, species diversity of chlorophytes changed a little, but species composition presented some differences. Chlorococcum humicola, Chlorella vulgaris, Chlamydomonas ovalis and Chlamydomonas sp. nearly existed in all developing stages of biological crusts. In several former stages of the biological soil crust there were spherical chlorophytes and filamentous ones. When moss crust formed, filamentous chlorophytes disappeared, such as Microspora and Ulothrix.