Influence of radiata pine seedlings on chemical properties of some New Zealand montane grassland soils

Interaction between soil acidity and vegetation phenolic concentration was investigated to identify mechanisms by which forests sustain productivity on extremely acidic, infertile soils. Contrasting soils on well-preserved marine terraces of the “Ecological Staircase’ near Mendocino, CA comprise an extreme edaphic gradient. Pygmy forests of dwarf (< 5m) Mendocino cypress (Cupressus pygmaea), Bolander pine (Pinus contorta var. bolanderi), and Bishop pine (Pinus muricata) are found on the oldest, most acidic soils, and along a gradient that includes three distinct levels of soil acidity, with pH(CaCl₂) ranging from 5.0 to 3.0 in the upper mineral soil and from 4.0 to 2.0 in the litter layer where fine roots are concentrated. Mature foliage was collected from five sites on this edaphic gradient. Aqueous methanol extracts of the samples were analyzed for concentrations of total phenols and condensed tannin by the Prussian blue and acidified vanillin assays, respectively. There were significant differences (p<0.05) in foliar condensed tannin and phenolic concentrations within each species and concentrations were inversely related to soil pH, approximately doubling along the gradient. Natural selection for soil-regulated variation in polyphenol concentration is interpreted in the context of plant-litter-soil interactions as an adaptation that permits these conifers to survive in extremely acidic soils. H Lambers Section editor     

High occurrence of rare inland halophytes on post‐mining sites in western Ukraine

Rare inland halophytic vegetation including the associations Salicornietum prostratae, Spergulario marginatae‐Suaedetum prostratae, Puccinellietum limosae, com. Puccinellietum limosae – a variant of Aster tripolium subsp. pannonicus and Astero pannonici‐Bolboschoenetum compacti have been found on 3 localities in the Drohobych region of western Ukraine. These are isolated (‘island’) localities, almost unknown until today. Halophytes grew there on salted sites in the vicinity of the old salt industry. Species of halophytes previously not known from this region were discovered: Aster tripolium subsp. pannonicus, Bolboschoenus maritimus, Gypsophila paniculata, Limonium gmelinii, Lotus tenuis, Puccinellia distans, Sonchus palustris, Suaeda prostrata, Trifolium fragiferum var. bonannii, Triglochin maritima, Typha laxmannii and Zannichellia palustris subsp. pedicellata. The occurence of these plants strictly depends on the presence of salt in the soil and they are endangered by shrinkage of salted sites following the termination of the salt industry in Drohobych region.     

La vegetazione degli stagni della zona di Olbia (Sardegna nord-orientale)

Abstract

Vegetation of the ponds in the zone of Olbia (northeast Sardinia). – The present paper contains a study on the vegetation of the ponds and marshes in the neighbourhood of Olbia. The following well determined associations have been ascertained: Chaetomorpho-Ruppietum, Salicornietum fruticosae, Arthrocnemeto-Limoniastretum monopetali, Juncetum maritimi, Scirpetum maritimi, Caricetum divisae, Schoeneto-Plantaginetum crassifoliae. Furthermore, some other consociations have been observed (with: Pholiurus incurvas and Triglochin bulbosum; Juncus subulatus; Scirpus setaceus and Spergularia rubra; Agropyrum elongatum and Spartina juncea).

The authors have also taken into consideration the present distribution of the vegetation in relation to the modifications due to the fact that this area has been reclaimed.     

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.     

外来物种刺槐对土壤微生物功能多样性的影响

以延河流域不同植被区内人工刺槐(Robinia pseudoacacia)群落和乡土植物群落的土壤微生物为研究对象,利用Biolog微平板技术对土壤微生物功能多样性进行测定,分析人工引种刺槐在不同环境梯度(3个植被区)下对土壤微生物功能多样性的影响。结果表明:刺槐对不同环境梯度下的土壤微生物的影响明显不同。从草原区到森林区,刺槐林之间土壤微生物群落的平均颜色变化率(AWCD)和土壤微生物功能多样性指数均没有显著变化;但与乡土植物群落比较,草原区、森林草原区和森林区土壤AWCD分别表现为刺槐乡土植物、刺槐乡土植物、刺槐乡土植物;在草原区和森林草原区刺槐林土壤微生物群落的群落丰富度指数(S)、Shannon-Wiener指数(H)、Simpson指数(D)、Mc Intosh指数(U)均大于乡土植物,森林区刺槐林群落丰富度指数(S)、Shannon指数(H)、Simpson指数(D)均小于乡土植物;刺槐林和乡土植物群落下土壤微生物碳源利用存在差异,主要体现在对糖类、氨基酸类的利用上。PCA分析显示主成分1贡献较大的碳源有24种,在主成分分离中起主要贡献作用的是糖类、氨基酸类和羧酸类。土壤碳氮含量能影响土壤微生物功能多样性指数,土壤含水量和温湿度能够影响碳源的利用类型。刺槐对土壤微生物功能多样性的影响存在区域差异,在评价刺槐对土壤生态过程与功能的影响时必须要考虑这种空间差异性。     

Water availability determines physiognomic gradient in an area of low-fertility soils under Cerrado vegetation

Soil is one of the environmental elements to influence Cerrado vegetation. Aluminum toxicity of Cerrado soils is well known, but the importance of water availability is still to be understood, especially in Cerrado under wetter climates. We studied the association between Cerrado physiognomies (cerrado sensu stricto and cerradão) and morphological, chemical, physical, and physical–hydrical soil attributes at southwestern São Paulo State, Brazil. Characterization of soil morphology, classification and sample collection for particle-size distribution, and chemical and water-retention analyses were carried out in 15 permanent plots, where vegetation was characterized floristically and structurally. Simple correlation and canonical correspondence analyses were performed with soil data. Classification of soils (U.S. Soil Taxonomy) with very low clay contents was not able to separate soils under cerradão—forestry physiognomy—from those under cerrado sensu stricto—savannic physiognomy, even though it tends to distinguish soils under greater biomass from those under lower biomass physiognomies. High soil acidity of all studied soils and increased at the sites with greater contents of organic matter, mainly with the cerradão physiognomy, precluded Al toxicity as a cause of the physiognomic gradient within Cerrado. Clay content, microporosity, and residual and saturation moisture were the most significant soil attributes to correlate directly with the cerradão physiognomy, indicating that water availability is the main factor explaining the physiognomic gradient of Cerrado vegetation in a local scale, where climate and soil fertility do not vary spatially.     

土壤纤毛虫群落对不同退还模式生态恢复的响应

为了探究土壤纤毛虫群落对不同退还模式生态恢复的响应及利用其群落特征来评价退还效果,于2014年4月至2015年7月在甘肃省天祝藏族自治县朵什乡退耕还林区选取了3个不同退还林型样点(云杉、沙棘混交林A1,云杉林A2,沙棘林B1)和2个对照耕地样点(小麦地A0,豌豆地B0)为研究样地,采用"非淹没培养皿法"、活体观察法和培养直接计数法对土壤纤毛虫群落特征进行了研究,同时测定了各样点土壤的相关环境因子,并分析了不同恢复模式下土壤纤毛虫群落特征与植被群落参数、土壤环境因子间的相关性。研究共鉴定到125种土壤纤毛虫,隶属于9纲19目29科34属。结果显示:退还样点和对照样点的土壤纤毛虫群落结构特征存在明显差异(P0.05),退还样点间的物种相似性减小,群落组成复杂化;退还样点土壤纤毛虫物种数、密度、物种多样性指数、均匀度指数和丰富度指数均明显增高(P0.05),且各样点间表现为A1B1A2B0A0;各样点优势类群的演替趋势,由对照样点的肾形目演替为退还样点的散毛目。相关性分析和冗余分析结果表明,退耕还林后,对纤毛虫群落结构稳定影响最主要的是有机质、含水量和全氮的含量,不同林型间土壤纤毛虫群落组成差异较大,表明土壤纤毛虫群落结构可作为对退耕还林生态恢复的评价指标。     

Changes in vegetation patterns on the margins of a constructed wetland after 10 years

Summary A constructed urban wetland in Adelaide was surveyed 18 months and 10 years after construction to see how shoreline vegetation, soil electrical conductivity (EC), texture and pH changed over time and to provide data for future site management. Multivariate analysis detected four plant associations at 18 months: salt‐tolerant taxa on conductive clays; a weed‐dominated community on lower EC soil; and two smaller waterlogged, low EC clusters dominated by Common Reed (Phragmites australis) and Sea Club‐Rush (Bolboschoenus caldwellii), respectively. At 10 years, site cover and heterogeneity was higher, with the margins dominated by Phragmites and salt‐tolerant species. EC was much lower and more uniform, and the soils were heavier and more alkaline. Managed storm water flushing apparently lowered soil EC, but possibly also disturbed the shoreline. However, weeds were still common, and the potential for domination by Phragmites at the expense of other native shoreline species means that ongoing monitoring and hydrological and vegetation management are essential to maintain site habitat diversity.     

Pikas (Ochotona princeps : Lagomorpha) as allogenic engineers in an alpine ecosystem

Pikas (Ochotona princeps: Lagomorpha) build caches of vegetation (“haypiles”), which serve as a food source during winter in alpine and subalpine habitats. Haypiles appear to degrade over time and form patches of nutrient-rich soils in barren talus and scree areas. We sampled soils underneath and next to haypiles, and plants growing on and near haypiles in an alpine cirque in northwestern Wyoming, USA, to determine the effects of pika food caches on N, C, and C/N ratios in soils and plants. We found that (1) haypile soils had significantly higher carbon and nitrogen levels and lower C/N ratios than both adjacent soils and soils in the general study area, (2) two of three plant species tested (Polemonium viscosum and Oxyria digyna) had significantly higher levels of tissue percent N when growing on haypile soils, and (3) total standing plant biomass at the study site increased with soil percent N suggesting that vegetation was nitrogen limited. Pikas may therefore function as allogenic ecosystem engineers by modulating nutrient availability to plants. Received: 5 July 1997 / Accepted: 30 November 1997     

ORDINATION AND CLASSIFICATION OF WESTERN OAK FORESTS IN OKLAHOMA

Ordination and classification techniques were used to analyze patterns of forest vegetation, species diversity, and soil type in the Wichita Mountains Wildlife Refuge of southwestern Oklahoma. Cluster analysis based on tree species produced three general community types: 1) Quercus stellata-Q. marilandica forests; 2) Q. stellata forests; and 3) mesophytic forests. A polar ordination produced a gradient of vegetation that corresponded to a moisture gradient. Many high diversity forests were located on loamy drainageway soils or north facing slopes. Tree species diversity (H') was inversely related to the importance of Quercus stellata. Cluster analysis based on species composition of the tree seedlings produced four general community types: 1) Q. marilandica type; 2) Q. marilandica-Q. stellata-Juniperus virginiana type; 3) Ulmus americana-Celtis reticulata-Bumelia lanuginosa type; and 4) Acer saccharum type. The third seedling type occurred almost exclusively on loamy drainageway soils. There was no relationship between stand location on the first axis of the tree ordination and the first axis of the seedling ordination suggesting that trees and seedlings respond differently along the moisture gradient.     

Diversity of subalpine and alpine vegetation of the eastern part of the Nízke Tatry Mts in Slovakia: major types and environmental gradients

Changes in composition and structure of alpine and subalpine plant communities in relation to ecological factors were analysed in the Nízke Tatry Mts, Slovakia. Species cover values of vascular and non-vascular plants in each vegetation plot were recorded on the nine-degree scale. A data set of 156 relevés of alpine and subalpine vegetation was sampled recently during one year in the eastern part of the Nízke Tatry National Park. The data set was analysed by cluster analysis and Detrended Correspondence Analysis. analyses were carried out on the entire data set, including the subset of short grassland and dwarf-shrub vegetation. Major gradients and clusters were ecologically interpreted using Ellenberg indicator values. In the entire data set, the major gradient in species composition was associated with nutrient availability and the second most important gradient with light. In the case of short grassland and dwarf-shrub vegetation, the gradients were different. The first one was associated with soil reaction and the second gradient was associated with moisture. Clusters proposed by numerical classification reproduced many traditional phytosociological associations, namely Seslerietum distichae, Sphagno capillifolii-Empetretum nigri, Junco trifidi-Callunetum vulgaris, Juncetum trifidi, Dryopterido dilatatae-Pinetum mugo, Luzuletum obscurae, Agrostio pyrenaiceae-Nardetum strictae, while some other associations were less clearly differentiated (communities of the alliances Calamagrostion villosae, Adenostylion alliariae, Trisetion fusci, Cratoneuro filicini-Calthion laetae or Salicion herbaceae). The next clusters included Vaccinium and Festuca supina dominated communities and artificial roadside grasslands sown 50 years ago. Bryophytes and lichens were highly represented among diagnostic species of particular associations. Distribution pattern of particular plant communities was strongly influenced by site position either on northern or southern slope of the mountains.     

Syntaxonomical study of Italian wall vegetation

A syntaxonomical study of Italian wall vegetation based on classification and ordination of a large phytosociological data set from various authors (using the IAHOPA program) has confirmed the alliances Centrantho-Parietarion and Galio-Parietarion (order Parietarietalia judaicae, class Parietarietea judaicae), as already proposed by traditional syntaxonomy. The variation in humidity and the north-south geographical gradient are shown to be the most significant factors for the differentiation of this vegetation in Italy. The presence of some associations belonging to the class Asplenietea trichomanis (alliance Cystopteridion, Potentillion caulescentis and Centaureo-Campanulion) shows a strong connection with natural rock vegetation.     

Influence of Soil Characteristics on the Diversity of Bacteria in the Southern Brazilian Atlantic Forest

The Brazilian Atlantic Forest is one of the 25 biodiversity hot spots in the world. Although the diversity of its fauna and flora has been studied fairly well, little is known of its microbial communities. In this work, we analyzed the Atlantic Forest ecosystem to determine its bacterial biodiversity, using 16S rRNA gene sequencing, and correlated changes in deduced taxonomic profiles with the physicochemical characteristics of the soil. DNAs were purified from soil samples, and the 16S rRNA gene was amplified to construct libraries. Comparison of 754 independent 16S rRNA gene sequences from 10 soil samples collected along a transect in an altitude gradient showed the prevalence of Acidobacteria (63%), followed by Proteobacteria (25.2%), Gemmatimonadetes (1.6%), Actinobacteria (1.2%), Bacteroidetes (1%), Chloroflexi (0.66%), Nitrospira (0.4%), Planctomycetes (0.4%), Firmicutes (0.26%), and OP10 (0.13%). Forty-eight sequences (6.5%) represented unidentified bacteria. The Shannon diversity indices of the samples varied from 4.12 to 3.57, indicating that the soils have a high level of diversity. Statistical analysis showed that the bacterial diversity is influenced by factors such as altitude, Ca²⁺/Mg²⁺ ratio, and Al³⁺ and phosphorus content, which also affected the diversity within the same lineage. In the samples analyzed, pH had no significant impact on diversity.The Brazilian Atlantic Forest is one of the 25 biodiversity hot spots in the world. Altogether, these hot spots contain more than 60% of the total terrestrial species of the planet (17). The Atlantic Forest is a dense ombrophilous forest with several variations, including coastal (3 to 50 m), submontane (50 to 500 m), montane (500 to 1,200 m), and high montane (1,200 to 1,400 m) forests, creating a vegetation gradient ranging from shrubs to well-developed montane forest (4). The Serra do Mar is a mountainous system that shelters the main remainder of the Atlantic Forest following the Brazilian east coast, from north to south along the coastal line, and it is divided into diverse sections of high and low blocks, which have regional denominations.The most important law-protected conservation area of the Brazilian Atlantic Forest is located in the Serra do Mar of the southern state of Paraná. This conservation area (∼5,000 km²) shelters 72% of the fauna and flora species that occur in Paraná and was declared a Biosphere Reserve by UNESCO in 1992. Much is known about the diversity of its fauna and flora, but little is known of its microbial diversity, particularly the soil microbial diversity and the soil characteristics that influence it.The soil microbial diversity is vast, and it is estimated that >99% of species remain unidentified (1, 28). Acidobacteria and Proteobacteria are the most abundant groups in soil (15). However, the Proteobacteria lineage is more diverse and stable than the Acidobacteria lineage, suggesting that the latter group is more susceptible to variation in soil properties and to disturbing factors (33). Seasonal, physical, and physicochemical factors can be relevant to the structure and diversity of microbial communities. For example, seasonal changes in vegetation and temperature led to replacement of dominant groups in a wheat field (25) and in grassland soils (16). The particle size also has an influence on the bacterial diversity of soils. The clay fraction has a more diverse bacterial community than do silt or sand fractions (23). Finally, analyses of communities from North and South American soils showed that pH plays a major role in bacterial diversity, with less diverse communities associated with a lower pH (9).Human activity can also change the microbial diversity of soils, both qualitatively and quantitatively. Analyses of microbial communities on coral atolls in the central Pacific Ocean under different degrees of human impact showed that the least-impacted atoll had autotrophs and heterotrophs equally distributed in the community, whereas the most-impacted atoll had a dominance of heterotrophs and about 10 times more microbial cells and virus-like particles in the water column, including a large percentage of potential pathogens (7). A comparison between bacterial communities in forest and pasture soil showed that there is a less diverse and more restricted community in pasture soils. The vegetation shift from forest to pasture resulted in changes to G+C% contents of soil bacterial DNA and amplified rRNA gene restriction analysis (ARDRA) profiles (18). Similar changes occurred with communities of soils submitted to agroindustrial treatments and pollutants (3, 30).In this work, we used a culture-independent approach based on 16S rRNA gene sequences to survey the bacterial community of the Atlantic Forest soils and determined the physicochemical factors affecting its bacterial biodiversity.     

Yeast Communities of the Moscow City Soils

Yeast abundance and diversity were studied in the soils (topsoil) of Moscow city: urban soils under lawn vegetation and close to the areas of household waste disposal, as well as in zonal soddy-podzolic soils (retisols) in parks (Losiny Ostrov and Izmailovo). The numbers of soil yeasts were similar in all studied urban biocenoses (on average ~3.5 × 10³ CFU/g). From all studied soils, 54 yeast species were isolated. The highest yeast diversity was found in the soils adjacent to the areas of household waste storage. Soils from different urban sites were found to have different ratios of ascomycetous and basidiomycetous yeasts: basidiomycetes predominated in urban soils under lawn vegetation, while in the areas close to the waste disposal sites their share was considerably lower. The differences between the studied urban soils were also found in the structure of soil yeast complexes. In urban soils with high anthropogenic impact, the isolation frequency of clinically important yeast species (Candida parapsilosis, C. tropicalis, Diutina catenulata, and Pichia kudriavzevii) was as high as 35% of all studied samples, while its share in the community was 17%. The factors responsible for development of specific features of yeast communities in various urban soils are discussed in the paper.     

Classification and ecological characterization of coniferous forest phytogeocoenoses of Hokkaido,Japan

Coniferous forest phytogeocoenoses of Hokkaido Island, Japan, were studied to classify them based on vegetation characteristics, to analyse their soils, to correlate the vegetation and soil characteristics, and to provide some ecological interpretation for the phytogeocoenosis differentiation and establishment. Five forest types were distinguished based on the vegetation structure, each of which was comparable to plant association of Krajina (1960); 1. the moss type, 2. the Sasa kurilensis type, 3. the Sasa senanensis type, 4. the Carex sachalinensis type, and 5. the Dryopteris crassirhizoma type. Soil base status indicated by pH, electric conductivity, amount of calcium and magnesium, and base saturation showed a fair correlation with the forest types. The forest types were, therefore, arranged along a soil nutritional gradient. The moss type developed in the least fertile habitats whereas the Dryopteris crassirhizoma type in the most fertile habitats, and others were in between the two. It was suggested that in the island, where climate was humid with excess of soil water throughout a year, soil nutritional regime, more specifically availability of bivalent cations which tended to be removed by the excessive soil water, seemed to be a critical factor to differentiate and establish the forest types.This study was financially supported by the Science Research Grant of the (Monbusho) Japanese Goverment (Grant No. 60540422).     

La végétation des sols polygonaux aux étages alpin supérieur et subnival en Valais (Alpes centro-occidentales, Suisse)

Béguin Cl., Progin Sonney M. and Vonlanthen M. 2006. The vegetation of polygonal soils at the upper alpine and subnival belts in Switzerland. Bot. Helv. 116: 41–54. Polygonal soils are typical formations of arctic regions but occur locally at high elevation in the Alps. A vegetation survey of sites with polygonal patterning of soils in the Western Swiss Alps revealed a clear distinction between (1) periglacial polygonal soils, whose structure is created by frost action, and whose occurrence is limited to the subniveal belt (2700–3000 m a.s.l.) and (2) soils whose polygonal structures are mere contraction cracks created by desiccation, which are found in the alpine belt (2300–2750 m a.s.l). Two new plant associations characteristic of these sites are described: periglacial polygonal soils of the subniveal belt are colonized by the association Saxifrago oppositifoliae- Poetum alpinae ass. nov. of the alliance Drabion hoppeanae. Conversely, soils with polygonal contraction cracks shelter the association Epilobio anagallidifolii- Saginetum saginoidis ass. nov., which is related to the alliance Salicion herbaceae. We describe the particular geomorphological and climatic factors leading to the local formation of these soil types with their specialised vegetation. We conclude that their future existence is strongly threatened by climate warming. Manuscrit accepté le 6 mars 2006     

Rooting depth,water availability,and vegetation cover along an aridity gradient in Patagonia

Above-and belowground biomass distribution, isotopic composition of soil and xylem water, and carbon isotope ratios were studied along an aridity gradient in Patagonia (44–45°S). Sites, ranging from those with Nothofagus forest with high annual rainfall (770 mm) to Nothofagus scrub (520 mm), Festuca (290 mm) and Stipa (160 mm) grasslands and into desert vegetation (125 mm), were chosen to test whether rooting depth compensates for low rainfall. Along this gradient, both mean above-and belowground biomass and leaf area index decreased, but average carbon isotope ratios of sun leaves remained constant (at-27), indicating no major differences in the ratio of assimilation to stomatal conductance at the time of leaf growth. The depth of the soil horizon that contained 90% of the root biomass was similar for forests and grasslands (about 0.80–0.50 m), but was shallower in the desert (0.30 m). In all habitats, roots reached water-saturated soils or ground water at 2–3 m depth. The depth profile of oxygen and hydrogen isotope ratios of soil water corresponded inversely to volumetric soil water contents and showed distinct patterns throughout the soil profile due to evaporation, water uptake and rainfall events of the past year. The isotope ratios of soil water indicated that high soil moisture at 2–3 m soil depth had originated from rainy periods earlier in the season or even from past rainy seasons. Hydrogen and oxygen isotope ratios of xylem water revealed that all plants used water from recent rain events in the topsoil and not from water-saturated soils at greater depth. However, this study cannot explain the vegetation zonation along the transect on the basis of water supply to the existing plant cover. Although water was accessible to roots in deeper soil layers in all habitats, as demonstrated by high soil moisture, earlier rain events were not fully utilized by the current plant cover during summer drought. The role of seedling establishment in determining species composition and vegetation type, and the indirect effect of seedling establishment on the use of water by fully developed plant cover, are discussed in relation to climate change and vegetation modelling.     

A Multivariate Analysis of Soil Yeasts Isolated from a Latitudinal Gradient

Yeast isolates from soil samples collected from a latitudinal gradient (>77°S to >64°N) were subjected to multivariate analysis to produce a statistical foundation for observed relationships between habitat characteristics and the distribution of yeast taxa (at various systematic levels) in soil microbial communities. Combinations of temperature, rainfall (highly correlated with net primary productivity), and electrical conductivity (EC) could explain up to ca. 44% of the distribution of the predominant yeast species, rainfall and pH could explain ca. 32% of the distribution of clades in the most common orders (Filobasidiales and Tremellales), whereas vegetation type (trees, forbs, and grass) played the same role for orders. Cryptococcus species with appropriate maximum temperatures for growth predominated in most soils. Cryptococcus species in the Albidus clade of the Filobasidiales predominated in desert soils; Cryptococcus species of other clades in the Filobasidiales and Tremellales predominated in wetter and more-vegetated soils, with Tremellalean species favored in soils of lower pH or higher EC. The predominance of Cryptococcus species in soils has been attributed to their polysaccharide capsules, particularly important when competing with bacteria in arid soils.     

The vegetation of ultrabasic soils on the Isle of Rhum II. The causes of the debris

Summary

The relationship between the Rhum ultrabasic skeletal soils and their debris vegetation was investigated by plant analyses and field and laboratory experiments. Samples of Agrostis vinealis, Arenaria norvegica ssp norvegica, Calluna vulgaris, Festuca vivipara, Plantago maritima and Racomitrium lanuginosum from these soils usually had low concentrations of potassium and calcium, and high concentrations of sodium, magnesium (and high Mg/Ca quotients), iron and nickel. There were instances of very high iron concentrations (up to 22.4mg g^?1 in Plantago maritima), very high Mg/Ca quotients (up to 27.8 in Arenaria novegica spp. norvegica) and high nickel concentrations (up to 0.48mg g^?1 in Plantago maritima). A nutrient addition experiment which was set up in 1965 on an exposed barren area had in 1982 over twice as many species as originally recorded and a nearly complete plant cover. Shorter-term work has confirmed that nutrient availability limits the ultrabasic vegetation. An experiment on Agrostis vinealis in simulated soil solutions showed that a gabbro (non-ultrabasic) clone had a higher R.G.R. (relative growth rate), even at the higher of two experimental Mg/Ca quotients, than two peridotite (ultrabasic) clones and was moreover not significantly affected by the higher nickel concentration used. It is concluded that the low vegetation cover on the skeletal soils is maintained by low soil nutrients which might interact with the coarsely sandy texture in exacerbating the effects of periodic drought and frost heaving. There is no unequivocal evidence for plant toxicities associated with high magnesium or nickel in the Rhum soils.