Response of carbonicolous ascomycetes to aerated steam temperatures and treatment intervals

1978 ◽  
Vol 56 (19) ◽  
pp. 2313-2318 ◽  
Author(s):  
J. C. Zak ◽  
D. T. Wicklow

This laboratory study was designed to examine the response of a postfire ascomycete community to elevated temperatures and treatment intervals corresponding to those recorded during the burning of a tallgrass prairie. Aerated steam treatment of prairie soil samples (35, 40, 55, 70, 85, or 100 °C) for intervals of 60, 100, 140, or 180 s enabled us to examine the response of individual species comprising the carbonicolous ascomycete community.Simulation of a grassland fire by aerated steam treatment of prairie soils promoted the development of 20 species of ascomycetes. Generalists such as Sporomiella subtilis Ahmed and Cain occurred at high frequencies over most of the temperature range while specialists Podospora curvispora (Cain) Cain, Sordaria macrospora Awd., and Leptosphaeria sp. were important at only one temperature. Species diversity, richness, and number of species per sample were significantly affected by the temperature of the steam treatment. The temperature–treatment interval combination allowing for the greatest expression of diversity in the carbonicolous ascomycete community was 55 °C for 60 s. Since a grassland fire does not uniformly heat the soil surface, the environmental patchiness created by this physical perturbation may be an important factor in determining the composition of the carbonicolous ascomycete community in prairies.

1970 ◽  
Vol 10 (42) ◽  
pp. 76 ◽  
Author(s):  
RT Parrott ◽  
CM Donald

A study was conducted at Adelaide of the ignitability of monospecific swards of four Mediterranean annual pasture plants under windless conditions throughout the normal field desiccation of the swards in the spring. For any individual species the ignitability depended almost wholly on the percentage of water or the very closely correlated percentage of dead herbage. Atmospheric conditions had no measurable influence on ignitability during desiccation. Trifolium subterraneum was much less ignitable at any particular level of moisture content than were the grasses. Lolium rigidum was more inflammable early in the desiccation process than was Hordeum leporinum of equal water content, presumably due to the greater continuity of dry leaf; but H. leporinum was ignitable much earlier in the spring because it matured and dried sooner than did L. rigidum. In the case of the grasses, only those firebrands that fell to or near the soil surface started a fire, whereas the more compact sward of T. subterraneum, when sufficiently dry, lit readily at the upper surface.


Solid Earth ◽  
2013 ◽  
Vol 4 (2) ◽  
pp. 381-385 ◽  
Author(s):  
A. Novara ◽  
L. Gristina ◽  
J. Rühl ◽  
S. Pasta ◽  
G. D'Angelo ◽  
...  

Abstract. The aim of this work was to investigate the effect of an experimental fire used for grassland management on soil organic carbon (SOC) stocks. The study was carried out on Hyparrhenia hirta (L.) Stapf (Hh) grassland and Ampelodesmos mauritanicus (Desf.) T. Durand & Schinz (Am) grasslands located in the north of Sicily. Soil samples were collected at 0–5 cm before and after the experimental fire, and SOC was measured. During the grassland fire, soil surface temperature was monitored. Biomass of both grasses was analysed in order to determine dry weight and its chemical composition. The results showed that SOC varied significantly with vegetation type, while it is not affected in the short term by grassland fire. Am grassland stored more SOC compared with Hh grassland thanks to lower content in the biomass of the labile carbon pool. No significant difference was observed in SOC before and after fire, which could be caused by several factors: first, in both grassland types the measured soil temperature during fire was low due to thin litter layers; second, in a semiarid environment, a higher mineralization rate results in a lower soil carbon labile pool; and third, the SOC stored in the finest soil fractions, physically protected, is not affected by fire.


1999 ◽  
Vol 50 (7) ◽  
pp. 1203 ◽  
Author(s):  
G. B. Taylor ◽  
C. K. Revell

Studies were made on the preconditioning stage (which produces latent soft seeds) and the final stage of seed softening in newly ripened seeds of the GEH72-1A accession of yellow serradella (Ornithopus compressus L.). Pods grown at Yelbeni, Western Australia, in 1996 were collected in December and placed on the soil surface or buried at a depth of 0.5 cm at a site near Perth. Other pods were subjected to a gradual diurnal temperature fluctuation of 60/15°C in darkness in a laboratory chamber. Pod samples were taken from the field at intervals from January to June in 1997, and over 336 days from the 60/15°C treatment. Pods were broken into segments and the number of soft seeds determined. Numbers of latent soft seeds were then determined by subjecting residual hard seeds to 7 gradual diurnal temperature cycles of 48/15°C in darkness and retesting for permeability. In a second experiment, seeds preconditioned at the soil surface until 3 March were subjected to a range of light levels in the field in March before testing for permeability. The time taken for seeds to precondition under a range of constant temperatures between 30° and 70°C was determined in a third experiment. Preconditioning commenced early in summer in both surface and buried seeds. All buried seeds that preconditioned completed the softening process to produce about 80% soft seeds, with most seeds softening in March when diurnal temperatures fluctuated between maxima of 45–50°C and minima of 10–20°C. Only 15% of the seeds at the soil surface softened so that relatively few preconditioned seeds completed the softening process. Preconditioning occurred more rapidly than did the completion of softening in the 60/15°C treatment, indicating that this temperature regime was above optimum for the final stage of softening. Reversal of the preconditioning process took place in the field as temperatures declined during May. Effects of reduced temperatures in causing this reversion were confirmed in the laboratory on seeds preconditioned at 60/15°C. The final stage of softening was inhibited in some seeds by light levels as low as 0.3% of daylight, and in all seeds at a light level between 5 and 25%. A close negative linear relation was obtained between the log of the time taken for 50% of seeds to precondition and the constant temperature treatment between 30°C and 70°C, with the rate of preconditioning doubling with every 5.2°C rise in temperature within this range. Although many seeds preconditioned at the soil surface, the main constraint to completion of the seed softening process during autumn was the inhibitory effect of light.


2013 ◽  
Vol 10 (85) ◽  
pp. 20130326 ◽  
Author(s):  
L. J. Bridge ◽  
K. A. Franklin ◽  
M. E. Homer

Plants display a range of striking architectural adaptations when grown at elevated temperatures. In the model plant Arabidopsis thaliana , these include elongation of petioles, and increased petiole and leaf angles from the soil surface. The potential physiological significance of these architectural changes remains speculative. We address this issue computationally by formulating a mathematical model and performing numerical simulations, testing the hypothesis that elongated and elevated plant configurations may reflect a leaf-cooling strategy. This sets in place a new basic model of plant water use and interaction with the surrounding air, which couples heat and mass transfer within a plant to water vapour diffusion in the air, using a transpiration term that depends on saturation, temperature and vapour concentration. A two-dimensional, multi-petiole shoot geometry is considered, with added leaf-blade shape detail. Our simulations show that increased petiole length and angle generally result in enhanced transpiration rates and reduced leaf temperatures in well-watered conditions. Furthermore, our computations also reveal plant configurations for which elongation may result in decreased transpiration rate owing to decreased leaf liquid saturation. We offer further qualitative and quantitative insights into the role of architectural parameters as key determinants of leaf-cooling capacity.


2016 ◽  
Vol 69 (3) ◽  
Author(s):  
Maria Licznar-Małańczuk ◽  
Iwona Sygutowska

<p>The weed composition and the dominance of individual species occurring in an orchard were assessed at the Research Station of the Wrocław University of Environmental and Life Sciences, Poland, during the first 10 years after orchard establishment. ‘Ligol’ apple trees were planted in the spring of 2004 (3.5 × 1.2 m). Foliar herbicides were applied in 1 m wide tree rows twice or three times per each vegetation period. In the inter-row spaces, perennial grass was maintained.</p><p>Ten years of maintenance of herbicide fallow contributed to a change in the weed composition in the orchard. It changed as a result of different responses of the most important weed species to the foliar herbicides. Total suppression of <em>Elymus repens</em> was observed in the first year after planting the trees. <em>Convolvulus arvensis</em>, <em>Cirsium arvense</em>, and other perennial weeds, completely disappeared in the succeeding periods. The maintenance of herbicide fallow did not affect the abundance of <em>Taraxacum officinale</em>. The percentage of the soil surface covered by <em>Trifolium repens</em> and <em>Epilobium adenocaulon</em>, perennial weeds with considerable tolerance to post-emergence herbicides, increased during the fruit-bearing period of the trees. The abundance of these weeds was significantly reduced only in the rows with the stronger growing trees on the semi-dwarf P 2 rootstock. <em>Stellaria media</em> was the dominant annual weed. <em>Senecio vulgaris</em>, <em>Poa annua</em>, <em>Capsella bursa-pastoris</em>, and <em>Lamium</em> spp. were also frequently observed. A significant increase in the abundance of annual and perennial weeds was found in the tree rows as a result of improved water availability after a period of high precipitation.</p>


2017 ◽  
Vol 28 (1-2) ◽  
pp. 17-27
Author(s):  
V. M. Pomohaibo ◽  
L. D. Orlova ◽  
N. A. Vlasenko

Free DNA in nature or the environmental DNA (eDNA) contains unique information about the diversity not only of unicellular but also of multicellular organisms – fungi, plants, invertebrates and vertebrates in the past and contemporary nature. eDNA of a soil surface and of an aquatic environment may indicate a presence of contemporary living organisms and deposits, sediments and glaciers – wildlife diversity in the geological past. Fungi are reducers, symbions and parasites and play an important ecological role in nature, and so it is important to know their taxonomic and functional characteristics. Analysis eDNA in samples of forest soil showed that ascomycetes and basidiomycetes are represented most of all. They were identified as mycorrhizal types, plant pathogens and saprotrophes. In soils of different climatic zones DNA of numerous taxons of plant (herbs, shrubs, trees), unicellular and multicellular animals (protozoans, earthworms, birds, mammals) was discovered. In spite of this unknown species of fungi and earthworms were discovered. It was ascertained that eDNA of soil surface layer do not move practically and it is able to display a complete taxonomic filling of vertebrates and relative biomass of individual species. Researches of eDNA of freshwater ecosystems is focused to identify and control spreading of invasive species of crustaceans, mollusks, fishes, amphibians and reptiles with the goal of conservation of biological diversity and ecological balance. It is shown that eDNA may be a better tool to identify these species in comparison with traditional methods of audio and visual observation. At the same time a population size and an ontogenetic stage are not important. Another research direction of eDNA in a fresh water aims to identify species of aquatic animals (crustaceans, insects, fish, amphibians and mammals) at risk of extinction. A short time of eDNA existence in freshwater ecosystems is very useful for a nature protecting, because it can indicate a presence, status and disappearance of species. Thus eDNA of previous population, which is rapidly destroyed, will not interfere with the analysis. However, it is necessary to remember that in river ecosystems eDNA moves with the stream at a great distance. Further researches of eDNA in seawater samples are necessary, because in this aquatic environment the ability to move and storage time of free genetic material is insignificant. In land deposits, water sediments and glaciers free DNA do not move and may be preserved for long periods – till hundreds of thousands of years, that gives a possibility to obtain valuable information about the wildlife of paleoenvironments. In samples of permafrost deposits was found eDNA of numerous taxons of fungi, plants, three species of beetles, two species of fossil bird moa, mammoth, bison, horse. Water sediments is rich in eDNA also. In sea sediments extracellular DNA is much more than in sea water. Moreover, the anoxic conditions slow down destructive processes that ensures its long-term preservation. Sea sediments, especially estuary sediments are used to determine influence of human activities on the biological communities of ecosystems. Sediments of freshwater lake also contain eDNA, which represent degrading consequences of human interaction with the environment. Results of eDNA study of lake sediments as well as a study of soil deposits complement results of a study of pollen and fossil plant residues. It confirms a feasibility to combine traditional and molecular genetic methods in ecological researches to obtain most authentic data about past plant diversity. eDNA of many organisms is contained in glaciers. The analysis of this DNA permitted to identify 57 taxons of fungi, 8 orders of higher plants, taxons of protozoans and insects.


2013 ◽  
Vol 5 (2) ◽  
pp. 883-895 ◽  
Author(s):  
A. Novara ◽  
L. Gristina ◽  
J. Rühl ◽  
S. Pasta ◽  
G. D'Angelo ◽  
...  

Abstract. The aim of this work was to investigate the effect of a experimental fire, used for grassland management, on soil organic carbon (SOC) reservoirs. The study was carried out on Hyparrhenia hirta (L.) Stapf (Hh) grassland and Ampelodesmos mauritanicus (Desf.) T. Durand and Schinz (Am) grasslands, located in the north of Sicily. Soil samples were collected at 0–5 cm before and after experimental fire and SOC was measured. During grassland fire soil surface temperature was monitored. Biomass of both grasses was analyzed in order to determine dry weight and its chemical composition. The results showed that SOC varied significantly with vegetation cover, while it is not affected in the short period by grassland fire. Am grassland stored more SOC compared with Hh grassland thanks to lower content in biomass of labile carbon pool. No significant difference was observed in SOC before and after fire which could be caused by several factors: first, in both grassland types the measured soil temperature during fire was low due to thin litter layers; second, in semiarid environment higher mineralization rate results in lower soil carbon labile pool; and third, the C stored in the finest soil fractions, physical protected, is not affected by fire.


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