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1.
Soil respiration (Rs) is the second-largest source of CO2 to the atmosphere in terrestrial systems. In tropical savannas seasonal moisture availability and frequent fires drive ecosystem dynamics and may have a considerable impact on soil carbon (C) cycling, including Rs. In order to test the effect of fire on soil C cycling we measured Rs in annually burnt and unburnt plots in wet and dry seasons at a long-term fire experiment established in savanna woodlands of northern Australia. There was a significant interaction between season and fire, with highest rates of daily Rs (722 mmol CO2 m−2 d−1) observed in the wet season on unburnt, leaf litter patches. The three fold higher Rs rate on unburnt plots in the wet season was due to greater root-derived respiration (Rroot: 356 mmol CO2 m−2 d−1), while smaller changes to soil-derived respiration (Rsoil: 51 mmol CO2 m−2 d−1) were simply the result of C moving through decomposition rather than combustion pathways. Relationships between instantaneous Rs and soil temperature showed hysteresis with variable direction, suggesting that season and fire treatment also influence the soil depth at which CO2 is produced. We suggest that (1) changes to fire regimes, through active management or climate change, in tropical savannas could have an impact on Rs, and (2) the direct effect of fire on soil C cycling is limited to the removal of aboveground litter inputs.  相似文献   

2.
Fire plays a pivotal role in structuring ecosystems and often occurs as a human-mediated disturbance for land management purposes. An important component of fire regime is the season of burn. In tropical savannas, most fire management occurs during the dry season; however, wet season burning is often used for pastoral management and may be useful for controlling introduced plant species. We used replicated, experimental fire treatments (unburnt, dry season burnt and wet season burnt), spanning two habitats (riparian and adjacent open woodland), to examine the short- (within 12 months of fire) and longer-term (within four years of fire) changes of bird assemblages in response to wet and dry season burning in tropical savannas of northern Australia. Within 12 months of fire, we observed higher abundances of birds in the burnt treatments, although some species (e.g., red-backed fairy-wren, Malurus melanocephalus) were rarely observed in burnt sites. Dry season burnt sites contained higher abundances of insectivores and granivores, while wet season burnt sites had more carnivores. Four years following burning, dry season burnt sites were characterized by lower abundances, especially of nectarivores and granivores. Dry season burnt sites also contained a different assemblage than wet season burnt sites, but few differences were observed between wet season burnt and unburnt sites. Our results confirm that differences in fire regimes can substantially alter bird assemblages, especially in riparian zones, and emphasize the importance of incorporating burning season in fire management strategies.  相似文献   

3.
Grevillea caleyi is an endangered plant species with a restricted range lying partly within Ku-ring-gai Chase and Garigal National Parks in NSW, Australia. The principle threatening processes affecting G. caleyi are habitat destruction and adverse fire regimes combined with high levels of seed predation. A stochastic, spatially explicit, individual-based model was constructed to investigate the population dynamics of small populations of the species and to determine the impact of a variety of management strategies. Results of model simulations indicate there is a high risk of population decline and local extinction in remnant sites with small populations under current management regimes. The most effective fire management strategy is to schedule fires that burn 20-100% of sub-populations every 5-15 years, in combination with reduced predation rates. When predation management strategies are employed in conjunction with a structured fire regime, then a 20-30% reduction in predation rates can improve the chance of long-term persistence substantially.  相似文献   

4.
The short-term effects of wildfire on the characteristics of Mediterranean pine forest soils, exposed to semiarid climatic conditions, were evaluated by measuring different chemical, biochemical and microbiological parameters 9 months after the fire. Soils in which the fire had been intense showed higher electrical conductivity values than unburnt soils. All burnt soils had higher contents of nitrates, exchangeable NH4 + and available P and K while their contents of total organic C, extractable C, humic acids, water-soluble C and total and water-soluble carbohydrates were, in general, lower than those of unburnt soils. Microbial biomass-C in burnt soils represented from 50% to 79% of that of unburnt soils; basal respiration and dehydrogenase activity were also negatively affected by fire. In general, fire decreased urease and N-α-benzoyl-l-argininamide hydrolysing protease activities. Alkaline phosphatase activity in burnt soils was 29–87% that of the respective unburnt control soil. Arylsulphatase activity was also lower in burnt soils as was β-glucosidase activity, although in this case the differences from values of unburnt soils were not always statistically significant. Received: 15 July 1996  相似文献   

5.
We investigated the influence of fire return interval length on the ectomycorrhizal (ECM) community of a Pinus pinaster dominated forest and on the potential for common ECM networks (CMNs) between understorey shrubs and P. pinaster. ECM root tips were sampled from five shrub species belonging to the genera Arbutus, Cistus and Halimium and from maritime pine in four areas of central Portugal characterized by differing fire return interval length. Fungal symbionts were identified using molecular techniques with direct sequencing of the nrDNA ITS region.Twenty nine ECM species and sixteen non-ECM root inhabitants were identified. Six years after wildfire disturbance ECM species richness did not differ significantly between unburnt and burnt areas. Nine ECM fungal species were common to pine and shrubs and both their frequency of occurrence and proportion were significantly higher in the unburnt area when compared with both areas subjected to fire.Our study revealed that while the potential for CMNs between understorey shrub species and pine seemed to be maintained in the long fire return interval area, recurrent fires significantly reduced the frequency of occurrence and the proportion of common symbiont species. High fire frequencies could therefore delay the process of re-colonization by pine seedlings limiting their dispersal in new settings.  相似文献   

6.
Background, aim and scope  Forest fires can result in severe economic and environmental consequences, and little is known about the ecological patterns and processes that may lead to the recovery of burnt areas. In the last decades, Portugal has been the Southern European country with the highest number of fire events and with the highest burnt area per hectare. With this work, we proposed to study the effect of a forest fire on the terrestrial ecosystem. More specifically, this work intended to evaluate the short-term recovery of several soil chemical, biochemical (microbial enzymatic activities) and biological (edaphic macro-arthropod community) variables in a burnt pine tree forest area. Methodology  Soil and macro-arthropod sampling was carried out in a burnt area (transects BI, BII and BIII) and in a neighbouring unburnt area (U) 3 and 8 months after the fire, coinciding with autumn and spring. Soil was collected for the determination of physical (pH and conductivity) and chemical parameters (moisture and organic matter) and soil enzymes (cellulase, acid phosphatase and nitrogen mineralisation rate). Edaphic macro-fauna was captured using pitfall traps. Results  Univariate and multivariate statistics revealed, overall, that burnt sites displayed lower acid phosphatase and cellulase activities and higher conductivity and pH values than the unburnt area. There was a recovery in the measured soil parameters between autumn and spring in the most interior parts of the burnt areas (BII and BIII), but the outer transect (BI, close to a road) still displayed considerable differences to the remaining burnt transects as well as to the unburnt area. A total of 47 macro-arthropod taxa were captured in both seasons, with Linyphiidae spiders (20.2%) and insect families Formicidae (13.4%) and Staphylinidae (11.9%) being the most abundant. Dominance by some taxa was overall stronger in the burnt than in the unburnt area, although dominant taxa varied between seasons. In autumn, the burnt area was dominated by ants and had also a high abundance of scavengers, carrion feeders and some ground active hunters. In spring, there was a general increase in taxa diversity, richness, and total catches; in the burnt area, there was a re-colonisation by several organisms sensitive to litter quality, such as isopods and pseudoscorpions, particularly in the outer transect (closest to the unburnt area). Discussion  Differences in soil parameters between burnt and unburnt areas were most likely due to the deposition of nutrient-rich alkaline ashes. However, low cellulase activity in the outer part of the burnt area (BI) indicated compromised microbial activity in both sampling seasons. Recovery of soil functional parameters was delayed in the outer zone of the burnt area because of (i) fire intensity in that area or (ii) proximity to the road (enhancing erosion and exposure to contaminants). The pattern of arthropod re-colonisation of the burnt area followed the inverse recovery pattern (from the outer zone to the inner zone), stressing the primary role of the adjacent unburnt area as a source of potentially colonizing organisms. Conclusions  Direct and indirect effects of fire on soil parameters (soil alkalinisation and nutrient enrichment) and edaphic fauna had a short-term persistence in the burnt area, and signs of recovery were evident 8 months after the fire (spring). The adjacent unburnt area seemed to act as an important source of arthropod colonisers. Recommendations and perspectives  More prolonged studies on the recovery of soil functional parameters and arthropod community structure are required to understand long-term re-colonisation patterns. Researchers and authorities should also endeavour in the implementation of measures that favour and protect survivors and new indigenous colonisers (microbes, plants and animals) after a forest fire.  相似文献   

7.

Purpose

Pyrogenic organic matter (PyOM) in the soil of a maritime pine forest in Central Italy, formed during a fire of high severity, was characterised by Fourier transform infrared (FT-IR) and 13C nuclear magnetic resonance (NMR). Furthermore, soil samples from burnt and unburnt sampling sites and natural charcoal collected from the ground were characterised after progressive heating under air and nitrogen atmosphere. The aim was to better understand the role fire plays on PyOM formation and oxidation.

Materials and methods

The top 10 cm of mineral soil and the above-lying charcoal particles were collected soon after the fire. Sampling was also performed on an adjacent unburnt portion of the forest. The bulk soil organic matter (SOM), its extractable fraction and charcoal particles were investigated by FT-IR and 13C NMR spectroscopies. They also underwent thermogravimetric analysis under air or N2, stopping the thermal reactions at the end of the first exothermic reaction in the range 350–500 °C.

Results and discussion

The NMR investigation clearly revealed a significant enrichment in aromatic and alkyl C in the burnt soil compared to the unburnt one. Several clues led to hypothesise that SOM was not exposed to extreme heating during the fire, notwithstanding the high fire severity estimated by a vegetation-based visual scale. In the thermal treatment mimicking fire, charcoal lost much of its mass and carbon content. However, at 500 °C, it still maintained a significant recalcitrant fraction. Nitrogen concentration in the bulk soil increased after heating, particularly under air condition. This phenomenon could be due to the formation of heterocyclic nitrogen compounds in the charred material.

Conclusions

In the study area, PyOM is rich in aliphatic compounds presumably because of the understory sclerophyllous vegetation typically found in Mediterranean environments. A large fraction of the charcoal released to the soil during the fire is sensitive to oxidation by subsequent fires. On the other hand, charcoal preserves a significant fraction of C, the most recalcitrant one, with expected long residence time in soil. PyOM formed under high oxygen availability is richer in N than that formed in inert atmosphere, which might make PyOM more susceptible to biochemical degradation.
  相似文献   

8.
Forest wildfires can dramatically affect soil communities and reduce abundance and diversity of soil fauna. The recovery of soil animals after a fire depends both on immigration from the unburnt forest and on local survival in less-burnt spots, but the relative importance of these mechanisms is poorly known. Therefore, these factors were studied with regard to soil macrofauna and soil mites seven years after a wildfire occurring in a pine forest area with shallow soil in 2001 in central Sweden. Three replicate transects, each consisting of four plots were studied. The plots were located in (i) the unburnt forest close to the fire edge; (ii) slightly burnt patches directly attached to the unburnt forest; (iii) slightly burnt patches surrounded by bare rock but connected to the unburnt forest edge by a corridor with mostly unburnt litter and vegetation; and (iv) island patches not connected with a corridor to the unburnt forest edge. The hypothesis was that that soil animals would particularly disperse from the unburnt forest to moderately burnt plots inside a burnt area via the network of less-burnt corridors. Poor dispersers would be especially few in the island patches lacking connection to the “mainland”, whereas good dispersers would be independent of gaps in connectivity. As expected, the highest abundance of both macrofauna and oribatid mites was found in the unburnt forest. Resident soil macro- and mesofauna representatives had half the abundance in the edge and corridor plots as compared to the control, but their abundance was not lower in the island plots than in the corridor plots indicating on-site survival and recovery. Mobile mesostigmatid mites did not show any significant reduction of abundance in any of the plots. The abundance of soil-dwelling oribatid mites did not differ between islands and unburnt forest, but mobile aboveground oribatids had significantly lower abundance on the islands than in the unburnt forest. The opposite was observed for aboveground and belowground oribatid mite species richness. In conclusion, belowground animals showed mainly local survival and seemed to be independent of corridors presence, whereas most aboveground and mobile macro- and mesofauna seemed to be more responsive to isolation induced by forest fires. Soil and litter corridors connecting unburnt patches inside the burnt forests with the unburnt edges were important mainly for less mobile groups of soil macrofauna. This supports the idea that there is a relatively slow process of soil ecosystem recovery and that external colonization of the burnt areas dominates over the local survival and recovery from refuges.  相似文献   

9.
This paper studies fire severity through changes in the composition of the 1:5 soil: water extract in burnt and unburnt samples collected after a wildfire that affected 7.1 ha of mountainous broom scrub (Teide broom, Spartocytisus supranubius L.) in Tenerife (Canary Islands). Soil samples were collected over a regular sampling grid and analysed for pH, electrical conductivity (E.C.), and soluble cations (Ca+2, Mg+2, K+, and NH4+–N) and anions (P, SO4− 2–S, and NO3−?N). A visual estimation of fire effects on individual broom plants was also conducted. The results show significant differences between burnt and unburnt samples for pH, E.C. and soluble ions (except for P), which generally agrees with data reported in the literature. Although fire severity, as estimated from the degree of fuel combustion, correlated significantly with most of the studied parameters, the qualitative fire severity indexes failed to discriminate sample groups apparently exposed to moderate fire severity conditions. Multivariate statistical analysis (PCA) allowed extracting two main factors, capable to account for 88% of total variability, after rejecting three variables (inorganic N-forms and K+). These factors were related to fire severity and pH-dependent Ca+2 and P reactions, respectively.  相似文献   

10.
[目的]研究2002—2017年东北地区自然植被火的发生发展及其对干旱的响应规律,从而为区域火管理、火险等级预报和森林资源保护提供科学依据。[方法]基于MODIS公开的数据产品和改进帕默尔干旱指数(scPDSI),采用统计学方法,分别季节和年际尺度,分析东北地区自然植被火动态特征,探寻其对干湿状况的响应规律。[结果]①在季节尺度上,春季和秋季是森林和草地火的多发期,草地火次数在春季和秋季呈显著增加趋势;②在年际尺度上,森林火次数以18次/a的速度呈显著下降趋势,平均过火面积呈弱上升趋势,草地火次数以36次/a的速度呈极显著上升趋势,平均过火面积呈弱下降趋势;③火次数和过火面积分别与scPDSI呈线性负相关与指数负相关;④随着干旱程度的加深,森林和草地火的平均次数和平均单次过火面积都有增加的趋势。[结论]干旱可能会增加东北地区自然植被的起火次数和单次过火面积。  相似文献   

11.
Heathlands are scattered across fire-prone monsoonal northern Australia mostly in dissected sandstone terrain. Such communities, although floristically depauperate by comparison with heathlands in southern Australia and southern Africa especially, share in common a relatively high proportion of fire-sensitive, obligate-seeder shrub species. The paper explores the implications of frequent fires, and associated short inter-fire intervals, on populations of obligate-seeder shrub species occurring in extensive heathlands occupying the western rim of the Arnhem Plateau, in the Northern Territory. Two studies are presented. With reference to published data concerning the maturation times of regional obligate-seeder shrubs, the first study reports on minimum and maximum intervals between fires determined from a 16-year fire history, 1980-1995, for the Plateau landform unit in Kakadu National Park, interpreted from LANDSAT MSS imagery. While species with maturation times of 5 or more years are common in the regional heath flora, minimum fire interval data for each 1 ha pixel indicate that 69% of heath habitats had been burnt at least once by fires recurring within 3 years, and 64% had a maximum fire interval of 5 years; 11% burnt only once or remained unburnt. The second study reports on the effects of an unreplicated experimental fire, involving observations on ca. 4000 individual shrubs, on ensuing heath floristic composition and abundance, undertaken 3 years after a wildfire had burnt the same site. Despite the experimental fire being highly patchy, substantial declines in the occurrence and density of many obligate-seeder shrub species were attended by increases in many herbs, including flammable grasses. Three years after the experimental fire the number of obligate-seeder shrubs was still less than half that pre-fire despite significant recruitment of some species in latter years. Collectively, these and other published data indicate that minimum fire return intervals of at least 4-5 years are required for conserving rapidly maturing tropical sandstone heath obligate-seeder shrubs, and longer still on sites comprising species with longer maturation times. For conservation management purposes individual fires should be small (especially in relation to the extent of any one tract of heath), patchy, and recurring intervals between fires should be varied as far as practicable.  相似文献   

12.
The variable effect of different types of forest fires on the quantity and quality of soil organic matter (SOM) was analysed by comparing burnt and unburnt soils from six forest ecosystems in central Spain by organic elemental analysis and solid‐state 13C nuclear magnetic resonance (NMR) spectroscopy. Whole soil samples were collected 1 to 2 years after the fires and included one site affected by two fires within 2 years. The fire‐affected soils showed no common pattern with respect to the amount of additional carbon (Cadd) but at all sites, the fire enhanced the aromatic‐C content. The weakest fire intensity resulted in the greatest aromatic‐C enrichment factor, EFI(aromatic C) indicating the greatest local accumulation of char. The respective Cadd disclosed an EFI(aromatic C) to EFI(alkyl C) ratio, Bchar, of c.1, which supports a small degree of charring. Extensive combustion and volatilization at stronger fire intensities yielded a decrease of EFI(aromatic C) and an increase in Bchar. These trends are in good agreement with fire intensity and forest fuel combustibility in the various sites and therefore these indices could be used to elucidate the quality and quantity of char input that occurs during and after forest fires. No 13C NMR evidence for substantial inputs from non‐charred plant necromass was found for any of the single‐burn soils. The large carboxyl‐C content of Cadd is evidence of the occurrence of oxidation reactions very shortly after the fire. In comparing the single and double‐burn sites, no additional char input was observed for the double‐burn site, possibly because of complete combustion of young shrubs and char remains during the second fire. The large O‐alkyl‐C portion found in Cadd of the double‐burn soil is best explained by decreased litter degradation.  相似文献   

13.
Avifaunal responses to understorey fire disturbance and subsequent changes in habitat structure were examined within 20 burnt and unburnt forest plots of 0.25 ha (10×250 m), 10-15 months after an unprecedented understorey fire swept through the Tapajós-Arapiuns Extractive Reserve of central Brazilian Amazonia following the severe 1997-1998 El-Niño dry season. Although these surface fires in the previously undisturbed primary forest were relatively mild, they resulted in dramatic changes in forest structure consistent with those found elsewhere in Amazonia. Bird species negatively affected by these changes tended to be the least common, the most disturbance-sensitive, and habitat specialists. Considering different guilds, ant followers, dead-leaf gleaners, terrestrial gleaners, and arboreal sallying insectivores were the most negatively affected, whereas nectivores and arboreal granivores became more abundant in the burnt forest. The results highlight the severe consequences of even relatively mild surface fires in neotropical forests, and the importance of controlling haphazard frontier expansion for the conservation of susceptible species that are endemic to fire-prone regions.  相似文献   

14.
H.G. Smith  D. Dragovich 《CATENA》2008,73(3):274-285
This paper examines post-fire erosion response in a sub-alpine environment in south-eastern Australia for a period of 2.2 years. Few studies have examined fire impacts on sediment transfer in this environment. Erosion pins were used in grids located at upper, mid and lower slope positions on adjacent burnt and unburnt hillslopes to assess fire effects on the extent of surface level change. The results indicated that there was a significant difference between the surface level change regimes on the burnt and unburnt hillslopes. Estimated erosion rates for the burnt slope over the study period ranged from 2.7 to 94.3 t ha− 1, which could be considered low given the high slope angles, high precipitation and moderate fire severity. Slope position was critical in modifying post-fire erosion response, as it controlled slope angle and the rate of surface cover regrowth. Analysis of lower slope sites, for which more detailed data was available, indicated a second delayed erosion peak after the initial elevated post-fire response during the following spring snowmelt period. Surface recovery on the lower burnt site was slow, with vegetation cover still comparatively low 2.3 years after the fire. Evidence of post-fire sediment supply limitation was found on this site, with a declining rate of increase in the magnitude of total surface level change, despite limited regrowth and an increasing number of precipitation events > 20 mm for measurement intervals since the fire. Modification of the hillslope surface by fire leads to changing hillslope erosion process dominance in this environment. The post-fire hillslope undergoes erosion by direct rain-drop impact and overland flow, whereas the unburnt slope rarely experiences overland flow due to the thick ground cover. As a result surface level change on the unburnt slope was largely influenced by wetting–drying effects rather than sediment transfer by surface flow. Downslope biotransfer appears to be the dominant sediment movement process in the unburnt sub-alpine forest environment.  相似文献   

15.
The wild population of the palm Ptychosperma macarthurii near Darwin, in monsoonal northern Australia, is regionally endangered and provides a focus to illustrate a range of issues pertinent to conservation of rainforest habitat. Surveys in 1990 found that several populations exhibited a polarised size class structure typified by large adults and small juvenile plants. Over the following decade, in the absence of wildfire and in a period of reduced disturbance from introduced buffalo (Bubalus bubalis), cattle (Bos indicus) and pig (Sus scrofa), sufficient small juvenile plants survived and grew so as to infill the intermediate size classes. Three stage (bifid, juvenile and adult) transition matrix models characterised the population as declining under all observed conditions (intrinsic rate of increase: unburnt + few animals 0.9850; unburnt + many animals 0.9584; burnt <1 year 0.8737; burnt 1-2 years 0.9146; burnt >2 years 0.9937). In the absence of fire, simulations conducted to explore management options revealed a positive rate of increase with exclusion of introduced animals. With only partial introduced animal control or supplementation with juvenile plants, the median rate of increase remained negative. The regional population is at risk by more frequent and more intense fire due to the invasion of exotic grass species and land use changes in the catchment which result in an increased drying of the rainforest habitat. Ongoing decline is the most likely outcome in the absence of effective management intervention.  相似文献   

16.
We use population viability analysis of an endangered Florida scrub mint, Dicerandra frutescens, to specify the optimal fire return intervals for its long-term persistence and for its specific habitat. We derived 83 population projection matrices from 13 years of demographic data from eight populations, 59 matrices from scrub populations and 24 from firelane or yard edges. Seed dormancy and germination transitions were inferred based on experimental data and verified by comparing modeled vs. observed population trajectories. Finite rates of increase in scrub sites were highest shortly after fire and declined steeply through 10 years postfire. The break-even value of λ = 1 was passed quickly, in about six years, suggesting that populations >6 years postfire were already facing decline. The decline is probably related to the rapid growth of competing shrubs in the habitat of D. frutescens. In long-unburned sites, finite rates of increase were nearly always <1 and declined the most in the long-unburned site with no foot trails or treefall gaps. Finite rates of increase in firelane populations also declined with years since fire or last disking. The yard edge population showed λ values both >1 and <1, with no temporal trend. Stochastic simulations in scrub sites suggested an optimal regular fire return interval of about 6-12 years. Regular fires at this interval were more favorable than stochastic fire regimes, but stochasticity reduced extinction percentages at longer fire return intervals. Stochastic fire return intervals implied a wider optimal fire return interval of 6-21 years. We suggest that prescribed fire in Florida scrub on yellow sand has occurred (and needs to occur) more frequently than previously recommended.  相似文献   

17.
Data on postpyrogenic dynamics of soils under mountainous taiga cedar (Pinus sibirica) and pine (Pinus sylvestris) forests and subtaiga–forest-steppe pine (Pinus sylvestris) forests in the Baikal region are analyzed. Ground litter–humus fires predominating in this region transform the upper diagnostic organic soil horizons and lead to the formation of new pyrogenic organic horizons (Opir). Adverse effects of ground fires on the stock, fractional composition, and water-physical properties of forest litters are shown. Some quantitative parameters of the liquid and solid surface runoff in burnt areas related to the slope gradient, fire intensity, and the time passed after the fire are presented. Pyrogenic destruction of forest ecosystems inevitably induces the degradation of mountainous soils, whose restoration after fires takes tens of years. The products of soil erosion from the burnt out areas complicate the current situation with the pollution of coastal waters of Lake Baikal.  相似文献   

18.
The principal aim of this research was to determine the influence of wildfires on soil organic matter (SOM) content and composition in soils located on the northern slope of the Cantabrian Cordillera, an Atlantic mountainous region in the North West of Spain, where wildfires are frequent. Samples from soils with similar aspect, slope, elevation and vegetation characteristics, but with different wildfires histories were collected. Total organic carbon and total nitrogen contents were determined as well as the C/N ratio. Furthermore, a qualitative characterization of the soil organic carbon (SOC) was carried out by 13C variable amplitude cross polarization magic angle spinning (VACP/MAS) Nuclear Magnetic Resonance (NMR) spectroscopy. Our results show that, on the one hand, all the sampled soils can be considered important pools of carbon in this Atlantic mountainous region, especially in the heath areas. On the other hand, the fire-affected soils present higher SOM contents than their unburnt counterparts. This could be attributed to an important reaccumulation of fresh vegetal material, which is probably a consequence of the decrease of SOM decomposition rates after fire. Moreover, charred organic compounds are not found in all the burnt soils, which could be due to the long time since the last fires events took place, to different fire severities, or to different post-fire erosion processes in the studied soils.  相似文献   

19.
The Mallee Emu-wren (Stipiturus mallee) is a threatened, narrow-range passerine endemic to south-eastern Australia. To inform future conservation measures for this poorly known species, we used ecological niche factor analysis, habitat suitability modelling and distance sampling to determine landscape-scale habitat requirements and estimate the population size. Using GIS software, we integrated digital layers of ecogeographic variables with; (1) presence-only observations to derive and validate a habitat suitability model using ecological niche factor analysis, and (2) distance sampling to determine population distribution and densities across vegetation types. We detected populations in only five of seven reserves which they had occupied in 2000. We estimate the global population size to be 16,821 individuals (range 8431-39, 104), 68% greater than the previously estimated 10,000 individuals, with a single large reserve containing the majority (∼92%) of the global population. The Mallee Emu-wren is a habitat specialist, primarily occurring in mallee-Triodia vegetation that has not been burnt for at least 15 years. The highest densities were in vegetation associations containing at least a 15% cover of Triodia, however, time since the habitat was last burnt was the overriding factor in determining densities. Large-scale wildfires are a pervasive threat to the global status of the Mallee Emu-wren, and the risk to remaining populations is exacerbated by the adverse impact of prolonged drought and the potential for altered fire regimes caused by global warming. Evaluation of the global population status, and the continued wildfire threat warranted recent reclassification of the Mallee Emu-wren from Vulnerable to Endangered according to IUCN Red List categories and criteria.  相似文献   

20.
The effects of a range of fertilizer applications and of repeated low-intensity prescribed fires on microbial biomass C and N, and in situ N mineralization were studied in an acid soil under subalpine Eucalyptus pauciflora forest near Canberra, Australia. Fertilizer treatments (N, P, N+P, line + P, sucrose + P), and P in particular, tended to lower biomass N. The fertilizer effects were greatest in spring and smaller in summer and late actumn. Low-intensity prescribed fire lowered biomass N at a soil depth of 0–5 cm with the effect being greater in the most frequently burnt soils. No interactions between fire treatments, season, and depth were significant. Only the lime + P and N+P treatments significantly affected soil microbial biomass C contents. The N+P treatment increased biomass C only at 0–2.5 cm in depth, but the soil depth of entire 0–10 cm had much higher (>doubled) biomass C values in the line + P treatment. Frequent (two or three times a year) burning reduced microbial boomass C, but the reverse was true in soils under forest burn at intervals of 7 years. Soil N mineralization was increased by the addition of N and P (alone or in combination), line + P, and sucrose + P to the soil. The same was true for the ratio of N mineralization to biomass N. Soil N mineralization was retarded by repeated fire treatments, especially the more frequent fire treatment where rates were only about half those measured in unburnt soils. There was no relationship between microbial biomass N (kg N ha-1) and the field rates of soil N mineralization (kg N ha-1 month-1). The results suggest that although soil microbial biomass N represents a distinct pool of N, it is not a useful measure of N turnover.  相似文献   

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