Vulnerability of boreal indicators (ground-dwelling beetles, understory plants and ectomycorrhizal fungi) to severe forest soil disturbance

2017 ◽  
Vol 402 ◽  
pp. 213-222 ◽  
Author(s):  
J.M. Kranabetter ◽  
S. Haeussler ◽  
C. Wood
Soil Research ◽  
2004 ◽  
Vol 42 (7) ◽  
pp. 767 ◽  
Author(s):  
Sally J. Price ◽  
Francis M. Kelliher ◽  
Robert R. Sherlock ◽  
Kevin R. Tate ◽  
Leo M. Condron

Tropospheric methane (CH4) is oxidised by soil microbes called methanotrophs. We examined them in soil samples from a pristine Nothofagus forest located in New Zealand. Laboratory incubations indicated the presence of high-affinity methanotrophs that displayed Michaelis–Menton kinetics (Km = 8.4 µL/L where Km is the substrate concentration at half the maximal rate). When the soil was dried from its field capacity water content of 0.34 to 0.16 m3/m3, CH4 oxidation rate increased nearly 7-fold. The methanotrophs were thus metabolically poised for very high activity, but substrate availability was commonly limiting. When water content was held constant, CH4 oxidation rate nearly doubled as temperature increased from 5 to 12°C, a range found in the forest. By contrast, CH4 oxidation rate did not change much from 12 to 30°C, and it was zero at 35°C. When water content and temperature were held constant, the optimal soil pH for CH4 oxidation was 4.4, as found in the forest. Soil disturbance by nitrogen (N) and non-N salt amendment decreased CH4 oxidation rate, but this depended on the amendment species and concentration. The methanotrophs were adapted to native conditions and exhibited a great sensitivity to disturbance.


1991 ◽  
Vol 21 (6) ◽  
pp. 942-943 ◽  
Author(s):  
John W. Groninger ◽  
Larry H. McCormick

A greenhouse experiment was conducted to examine the effects of the herbicide sulfometuron on hay-scented fern (Dennstaedtiapunctilobula (Michx.) Moore) spore emergence. Sulfometuron was applied at rates ranging from 0.025 to 0.21 kg active ingredient per hectare to forest soil inoculated with hay-scented fern spores. Emergence based on the occurrence of prothalli was evaluated 30, 37, 44, and 52 days after inoculation. Sulfometuron at all rates completely controlled spore emergence. The data suggest that applications of sulfometuron could be effective in preventing the sexual reproduction of ferns in forest stands following soil disturbance.


2003 ◽  
Vol 33 (12) ◽  
pp. 2514-2518 ◽  
Author(s):  
Daniel G Gavin

Forest soil disturbance intervals are usually too long to measure using plot-based studies, and thus they are poorly understood. The mean soil disturbance interval (MSDI) in an old-growth forest on the west coast of Vancouver Island was estimated from radiocarbon dates of charcoal from organic and mineral soil horizons. Two assumptions are required to estimate the MSDI: (1) charcoal from forest fires is deposited within the organic horizon and eventually mixed into deeper mineral horizons by soil disturbances, and (2) the probability of soil disturbance is spatially homogeneous and affected only by the time since the last fire or the last soil disturbance. The MSDI is then estimated by the rate at which the proportion of undisturbed sample sites (determined by the proportion of sites with charcoal from the most recent fire in the organic horizon) decreases with increasing time since the last fire. Soil charcoal evidence of time since fire was determined at 83 sites using 141 radiocarbon dates. The estimated MSDI was greater on slopes (ca. 2010 years) than on terraces (ca. 920 years). The long periods between soil disturbances, especially on slopes, are consistent with other evidence from the study area that suggests infrequent tree uprooting is the predominant mode of soil disturbance.


2009 ◽  
Author(s):  
Deborah S. Page-Dumroese ◽  
Ann M. Abbott ◽  
Thomas M. Rice

1996 ◽  
Vol 60 (1) ◽  
pp. 291-298 ◽  
Author(s):  
C. J. Dulohery ◽  
Lawrence A. Morris ◽  
Richard Lowrance

Purpose. We attempted to quantify the contribution of wild-growing mycelium of ectomycorrhizal fungi to the soil level of selected metals and non-metals in upper (0−10 cm) layer of forest soil of boreal forest ecosystems. The content of selected elements were also analyzed and compared in such fractions of soil as bulk soil, rhizosphere and soil-root interface. Specifically we analyzed the content of phosphorus (P), manganese (Mn), iodine (I), chromium (Cr), nickel (Ni), copper (Cu), zinc (Zn), cadmium (Cd), cobalt (Co), mercury (Hg) lead (Pb) and arsenic (As). Methods. The concentration of the elements in the samples (dry weight, d.w.) was determined by the mass spectrometric method (ICP-MS) in the laboratory ALS Scandinavia AB, Luleå according to the method given in Rodushkin et al. [13]. Statistical data processing was performed using dispersion analysis (ANOVA) and Pearson correlation coefficients. Software Minitab (© 2010 Minitab Inc.). Results. It has been shown that concentration of phosphorus in the mycelium of fungi is about 1.5 times, and in the fruit bodies is about 7 times higher of that the plant plant tissue (soil+root interface). The concentration of manganese in the mycelium is about the same as in the bulk soil and much lower in the fraction of rhizosphere. Iodine, chromium and nickel are not accumulated, neither the mycelium of fungi nor in their fruitful bodies. Copper, zinc and cadmium are accumulated in both fruit bodies and mycelium of the studied species intensively. The concentration of cadmium in the mycelium is found to be about three times higher than in the bulk soil fraction, and about twice as high as in the fraction of rhizosphere. At such concentrations of cadmium in mycelium, the later may account from 16.2 to 32.3% of the total amount of cadmium in the upper, 0-10 cm layer of forest soils. The content of cobalt and mercury in the mycelium appeared to be somewhat higher in the bulk soil, about the same as in the rhizosphere fraction, and significantly higher than in the soil-root interface fraction. Fungi did not accumulate lead neither in the mycelium nor in their fruit bodies, whereas arsenic does not accumulated in soil-root interface and only weakly accumulated by fungal fruit bodies. Conclusions As a result of the study, it was found that the content of most of the analyzed metals and non-metals in the mycelium of ectomycorrhizal fungi of the upper (0-10 cm) soil enriched with organic matter in the forest ecosystem, except for cadmium and phosphorus, does not exceed 10% of their total amount. At the same time, the content of cadmium in the mycelium of fungi was the highest − 16.2 to 32.3%, which indicates the ability of fungi to accumulate this metal. It is suggested that the percentages of the content of the elements studied in the mycelium of upper layers of forest soil is rather underestimated than overestimated.


2009 ◽  
Vol 89 (1) ◽  
pp. 3-11 ◽  
Author(s):  
M P Curran ◽  
D G Maynard

The challenge for all agencies managing public or private forest lands is to develop resource management policy and procedures based on the best available information. Science-based resource management occurs through an adaptive management process that includes three types of monitoring: implementation (compliance), effectiveness, and validation (research). Continued research, and the establishment of new trials is required to support soil conservation efforts and to investigate new concerns, such as climate change, bio-fuel harvest, and changing practices. Cooperative scientific networks and other collaborations are required to secure benefits from a common approach to soil disturbance management and reporting under various provincial/state, national and international sustainability protocols such as the Montréal Process. The technical session on Forest Soil Disturbances at the 2006 Annual Meeting of the Canadian Society of Soil Science in Banff, Alberta, is one step in collaboration, and brought together a group of experts from across Canada, and some from the United States of America, to share knowledge and experience and to discuss issues related to soil disturbance effects, policies and practices on forest lands. Selected papers are presented in this special issue on Forest Soil Disturbance, with this background paper focusing on the types of scientific support activities needed for science-based management of forest soil disturbance. Key words: Soil compaction, adaptive management, soil conservation, Montréal Process, natural resource management, monitoring


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