Beaver canals and their environmental effects

2019 ◽  
Vol 44 (2) ◽  
pp. 189-211 ◽  
Author(s):  
Bartosz P Grudzinski ◽  
Hays Cummins ◽  
Teng Keng Vang

Beaver canals and their environmental effects are much less studied than beaver dams, despite being widespread in some beaver-inhabited areas. In this study, we completed a systematic review of previous research on the structure and ecosystem effects of beaver canals to provide an increasingly holistic understanding of these landscape features. Specifically, we: 1) summarized why, where, when, and how beaver develop canals; 2) chronicled all published descriptions on beaver canal morphology; and 3) summarized the literature on the environmental effects of beaver canals. Thirty-one relevant studies were identified and incorporated into this review. Beaver canals have been identified in numerous environments ranging from largely undeveloped mountainous regions to heavily developed agricultural landscapes. Beaver primarily develop canals to increase accessibility to riparian resources, facilitate transport of harvested resources, and to decrease predation risk. As with beaver dams, beaver canals exhibit large structural variability, particularly in lengths, which can be over 0.5 km. Widths of about 1 m and depths of about 0.5 m are common. Beaver canals alter watershed hydrology by creating new aquatic habitats, connecting isolated aquatic features, and diverting water into colonized areas. Beaver canals have been identified as favored habitats for several biotic species and are sometimes used during critical life stages (e.g. dispersal). In addition to increasing overall floral and faunal species richness and diversity, beaver canals may benefit biota by mitigating habitat fragmentation and climate change impacts. Based on the results of this review, incorporating beaver canals into stream restoration practices may be environmentally beneficial.

2013 ◽  
Vol 83 (2) ◽  
pp. 332-342 ◽  
Author(s):  
Sinead English ◽  
Andrew W. Bateman ◽  
Rafael Mares ◽  
Arpat Ozgul ◽  
Tim H. Clutton‐Brock

2021 ◽  
Author(s):  
Gabriel Földes ◽  
Marija Mihaela Labat ◽  
Silvia Kohnová ◽  
Miroslav Kandera

<p>The study focuses on future changes in short-term rainfall characteristics. The analysis was performed for the mountainous regions in the northern part of Slovakia at 10 selected climatological stations. The rainfall data are simulated by Community Land Model Scenario which represents the future climate change.  The Community Land Model Scenario is a multidisciplinary project between scientists and several working groups mainly in the USA. The model includes impacts of changes in vegetation on the climate. The scenario has semi- pessimistic characteristics with a predicted global temperature increase by 2.9°C by the 2100. The analysis was performed for five rainfall durations (60, 120, 180, 240 and 1440 minutes) for the historical (1961-2020) and for the future (2071-2100) periods.  The detection of the future changes in short-term rainfall characteristics was made by several methods; for the seasonal changes the Burn´s vector was used, for the trend testing the data the Mann-Kendall test was applied. Results provide information how climate change impacts the short-term rainfall intensities in the mountainous regions of Slovakia.</p>


2013 ◽  
Vol 280 (1765) ◽  
pp. 20131149 ◽  
Author(s):  
Lauren B. Buckley ◽  
Joshua J. Tewksbury ◽  
Curtis A. Deutsch

Whether movement will enable organisms to alleviate thermal stress is central to the biodiversity implications of climate change. We use the temperature-dependence of ectotherm performance to investigate the fitness consequences of movement. Movement to an optimal location within a 50 km radius will only offset the fitness impacts of climate change by 2100 in 5 per cent of locations globally. Random movement carries an 87 per cent risk of further fitness detriment. Mountainous regions with high temperature seasonality (i.e. temperate areas) not only offer the greatest benefit from optimal movement but also the most severe fitness consequences if an organism moves to the wrong location. Doubling dispersal capacity would provide modest benefit exclusively to directed dispersers in topographically diverse areas. The benefits of movement for escaping climate change are particularly limited in the tropics, where fitness impacts will be most severe. The potential of movement to lessen climate change impacts may have been overestimated.


2012 ◽  
Vol 60 (3) ◽  
pp. 192 ◽  
Author(s):  
Melanie L. Lancaster ◽  
Michael G. Gardner ◽  
Alison J. Fitch ◽  
Talat H. Ansari ◽  
Anita K. Smyth

Land alteration for intensive agriculture has been a major cause of species decline and extinction globally. In marginal grazing regions of southern Australia, native perennial shrubs are increasingly being planted to supplement pasture feeding of stock. Such revegetation has the benefits of reducing erosion and salinity, and importantly, the potential provision of habitat for native fauna. We explored the use of revegetated native saltbush by the sleepy lizard (Tiliqua rugosa) an endemic Australian species common in the region. We repeatedly sampled revegetated saltbush throughout 2010 and 2011 for adults (n = 55) and juveniles (n = 26). Using genotypes from eight microsatellite loci, parents were assigned to half of all juveniles with high statistical confidence. Parents were sampled in the same patch of revegetated saltbush as their offspring, thus supporting the observation that juvenile sleepy lizards remain within the home range of their parents before dispersal. Most importantly, our findings indicate that revegetated saltbush provides important habitat for T. rugosa at significant life stages – before and during breeding for adults, and before dispersal for juveniles. We conclude that revegetation using simple, monoculture plantations provides beneficial habitat for T. rugosa and may also be beneficial habitat for other native species in human-altered agricultural landscapes.


1970 ◽  
Vol 3 ◽  
pp. 119-127
Author(s):  
Bharat Gotame

There are ample of evidences to prove the impacts of Climate Change and will be with us for a long time to come. It will have significant impact on natural systems so that most of the habitat of living organism is directly influenced moreover the human being (which is heterotrophic in nature) and their roles to sustain the development and earth at summary are being vulnerable. This literature review article tries to summarize some climate change scenario and its increasing impact over the livelihood assets and their direct/indirect influence to development fronts. Nepal a developing country having more than 70% of mountainous regions with agriculture based economy is more susceptible to climate change impacts. Planning of development activities remarked with increasing trend of climate change impact with pivotal theme should make the development more sustainable and long living. Existing initiatives to make adaptation options are insufficient to halt the expected danger and redesigning the module of development is urgent in Nepal. On adaptation and vulnerability, a continuing effort must take place to exchange experiences and look for emerging best practices and frameworks. The urgency of the issue requires planners, policy makers, evaluators, practitioners and researchers to become involved in designing and in empowering communities and government as well. Key Words: Climate change, Development, Planning, Economic impact, Adaptation   DOI: 10.3126/init.v3i0.2503 The Initiation Vol.3 2009 p.119-127


2020 ◽  
Vol 21 (2) ◽  
pp. 519-530
Author(s):  
Mayank Dhaundiyal ◽  
Joseph Coughlan

This paper contributes to the strategic alliance literature by undertaking a literature review of the burgeoning strategic alliance literature published in the last three decades in the mainstream management journals to fulfil two primary objectives. First, to bring a coherent structure into the fairly vast and growing alliance literature and second, to serve as a medium for a holistic understanding of the major life stages of strategic alliances. This is done by first dividing the alliance literature into three distinct yet related alliance life stages namely the pre-alliance stage, alliance formation stage and the alliance management and performance stage, and then by discussing in detail the three alliance stages individually. The paper would be useful for academics as well as practitioners looking to get a holistic understanding of strategic alliances and its three distinct yet related life stages and the key research papers which have been published focussing on each of these alliance stages.


Author(s):  
Asim Jahangir Khan ◽  
Manfred Koch

This study focusses on identifying a set of representative future climate projections for the Upper Indus Basin (UIB). Although a large number of GCM’s predictor sets are nowadays available in the CMIP5 archive, the issue of their reliability for specific regions must still be confronted. This situation makes it imperative to sort out the most appropriate, single or small-ensemble set of GCMs for the assessment of climate change impacts in a region. Here a set of different approaches is adopted and applied for a step-wise shortlist and selection of appropriate climate models for the UIB under two RCPs: RCP 4.5 and RCP 8.5, based on, a) range of projected mean changes, b) range of projected extreme changes, and c) skill in reproducing the past climate. Furthermore, because of higher uncertainties in climate projection for high mountainous regions like the UIB, a wider range of future GCM climate projections is considered by using all possible future extreme scenarios (wet-warm, wet-cold, dry-warm, dry-cold). Based on this two-fold procedure, a limited number of climate models is pre-selected, out of which the final selection is done by assigning ranks to the weighted score for each of the mentioned selection criteria. The dynamically downscaled climate projections from the Coordinated Regional Downscaling Experiment (CORDEX) available for the top-ranked GCMs are further statistically downscaled (bias-corrected) over the UIB. The downscaled projections up to year 2100 indicate temperature increases ranging between 2.3 °C and 9.0 °C and precipitation changes that range, from a slight annual increase of 2.2% under the drier scenarios,  to as high as 15.9% for the wet scenarios.  Moreover, for all scenarios, the future precipitation will be more extreme, as the probability of wet days will decrease, while, at the same time, the precipitation intensities will increase. The spatial distribution of the downscaled predictors across the UIB also shows similar patterns for all scenarios, with a distinct precipitation decrease over the south-eastern parts of the basin, but an increase in the northeastern parts. These two features are particularly intense for the “Dry-Warm” and the “Median” scenarios over the late 21st century.


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