Approximation of K carrying capacity for moose in eastern Quebec

1989 ◽  
Vol 67 (2) ◽  
pp. 373-380 ◽  
Author(s):  
Michel Crête

Estimation of moose density ranged between 18 and 20 animals/10 km2 in a 120-km2 boreal area of eastern Quebec that has been excluded from hunting for many decades. Moose were sedentary; 81% of telemetry locations of 12 adults (6 of each sex) that were captured in the area were within the block boundary. Use of winter forage was low for balsam fir, but variable and relatively high (29%) for deciduous twigs. When pooling the present results with comparable studies done elsewhere in Quebec, a significant positive linear relationship was found between percent deciduous browse removal and moose density. Annual summer and winter forage production of deciduous species was low in the study area in comparison with other areas in Quebec; however, the situation was the reverse for balsam fir. The K carrying capacity was estimated to exceed 20 moose/10 km2 when considering actual density in the study area. The same conclusion was reached by comparing forage consumption rate by moose for the whole winter and the annual production of 14 kg∙ha−1 of deciduous twigs. Daily forage needs versus annual production led to an unrealistic estimate of the K carrying capacity when also taking into account the annual production of balsam fir. Prime moose habitats in eastern North America probably possess comparable or higher K carrying capacities.

1982 ◽  
Vol 12 (2) ◽  
pp. 151-159 ◽  
Author(s):  
Michel Crête ◽  
Peter A. Jordan

Production of summer and of winter forage used by moose (Alcesalces Cl.) was estimated in six 530-km2 study blocks in southwestern Quebec. Annual production of summer forage (leaves of predominantly mountain maple (Acerspicatum Lam.) and beaked hazelnut (Coryluscornuta Marsh.)) averaged from 73 to 321 kg dry weight/ha, varying among 3 years and five forest types. Winter forage (twigs of deciduous species, predominantly the same two, plus needles and associated twigs of balsam fir (Abiesbalsamea (L.) Mill.)) averaged ca. 0.2 the production of summer forage. Annual production in all species, plus levels of crude protein, cellulose, Ca, and P in mountain maple and hazel, were comparable to those reported for other North American moose ranges. Among the six blocks, no relationship was found between moose density and forage factors. It was concluded that in lightly hunted regions of southwestern Quebec, further growth of moose populations was not being limited by nutritional factors.


1983 ◽  
Vol 59 (3) ◽  
pp. 128-131
Author(s):  
Steven A. Sinclair ◽  
Robert L. Govett

A total of 819 North American sawmills were surveyed concerning their production and distribution of balsam fir lumber. Seventy-one mills reported a total annual production of 275 million board feet (648 585 m3) of balsam fir lumber. The larger mills of eastern Canada represented 72% of this total. Canadian and large eastern US sawmills used middlemen heavily in marketing their softwood lumber while the remaining US sawmills used direct selling and captive retail yards as primary market channels. The only major production problem reported was the longer drying time needed for balsam fir lumber when compared to other northern softwood species.


2009 ◽  
Vol 31 (1) ◽  
pp. 1 ◽  
Author(s):  
G. M. McKeon ◽  
G. S. Stone ◽  
J. I. Syktus ◽  
J. O. Carter ◽  
N. R. Flood ◽  
...  

Grazing is a major land use in Australia’s rangelands. The ‘safe’ livestock carrying capacity (LCC) required to maintain resource condition is strongly dependent on climate. We reviewed: the approaches for quantifying LCC; current trends in climate and their effect on components of the grazing system; implications of the ‘best estimates’ of climate change projections for LCC; the agreement and disagreement between the current trends and projections; and the adequacy of current models of forage production in simulating the impact of climate change. We report the results of a sensitivity study of climate change impacts on forage production across the rangelands, and we discuss the more general issues facing grazing enterprises associated with climate change, such as ‘known uncertainties’ and adaptation responses (e.g. use of climate risk assessment). We found that the method of quantifying LCC from a combination of estimates (simulations) of long-term (>30 years) forage production and successful grazier experience has been well tested across northern Australian rangelands with different climatic regions. This methodology provides a sound base for the assessment of climate change impacts, even though there are many identified gaps in knowledge. The evaluation of current trends indicated substantial differences in the trends of annual rainfall (and simulated forage production) across Australian rangelands with general increases in most of western Australian rangelands (including northern regions of the Northern Territory) and decreases in eastern Australian rangelands and south-western Western Australia. Some of the projected changes in rainfall and temperature appear small compared with year-to-year variability. Nevertheless, the impacts on rangeland production systems are expected to be important in terms of required managerial and enterprise adaptations. Some important aspects of climate systems science remain unresolved, and we suggest that a risk-averse approach to rangeland management, based on the ‘best estimate’ projections, in combination with appropriate responses to short-term (1–5 years) climate variability, would reduce the risk of resource degradation. Climate change projections – including changes in rainfall, temperature, carbon dioxide and other climatic variables – if realised, are likely to affect forage and animal production, and ecosystem functioning. The major known uncertainties in quantifying climate change impacts are: (i) carbon dioxide effects on forage production, quality, nutrient cycling and competition between life forms (e.g. grass, shrubs and trees); and (ii) the future role of woody plants including effects of fire, climatic extremes and management for carbon storage. In a simple example of simulating climate change impacts on forage production, we found that increased temperature (3°C) was likely to result in a decrease in forage production for most rangeland locations (e.g. –21% calculated as an unweighted average across 90 locations). The increase in temperature exacerbated or reduced the effects of a 10% decrease/increase in rainfall respectively (–33% or –9%). Estimates of the beneficial effects of increased CO2 (from 350 to 650 ppm) on forage production and water use efficiency indicated enhanced forage production (+26%). The increase was approximately equivalent to the decline in forage production associated with a 3°C temperature increase. The large magnitude of these opposing effects emphasised the importance of the uncertainties in quantifying the impacts of these components of climate change. We anticipate decreases in LCC given that the ‘best estimate’ of climate change across the rangelands is for a decline (or little change) in rainfall and an increase in temperature. As a consequence, we suggest that public policy have regard for: the implications for livestock enterprises, regional communities, potential resource damage, animal welfare and human distress. However, the capability to quantify these warnings is yet to be developed and this important task remains as a challenge for rangeland and climate systems science.


1994 ◽  
Vol 74 (3) ◽  
pp. 531-537 ◽  
Author(s):  
T. Harrison ◽  
J. T. Romo

Regrowth and production of tillers in smooth bromegrass (Bromus inermis Leyss.) following defoliation to a 5-cm stubble height were monitored throughout the summer and in early spring the following year in central Saskatchewan. After defoliation, while smooth bromegrass was vegetative, forage began accumulating in 45–75 growingdegree-days (GDD) when moisture was favorable. Regrowth ranged from 34 to 84 g m−2. Plants also produced ≤ 51 g m−2 of regrowth when defoliated at or before culm elongation in a year with above-average precipitation. In two dry years, regrowth was minimal and plants did not regrow after defoliation in the later vegetative growth stages; however, new leaves were produced within 110–140 GDD. Following defoliation at early vegetative growth stages, 1030–1180 GDD were needed to reach maximum regrowth. Total annual production was either unaffected or reduced by defoliation. Total annual production ranged from 35 to 139 g m−2, with yields lowest when defoliated in early May or early June and highest when herbage was removed in mid-May or near flowering and seed production. When plants were defoliated during vegetative growth most tillers were produced the following spring, whereas when plants were defoliated during reproductive phases the majority of tillers emerged in the fall. The year after defoliation, the density of tillers (871–951 m−2) was not significantly different among treatments. Regrowth following defoliation cannot be related to a particular growth stage, but rather it depends on growing conditions. If smooth bromegrass is defoliated once and rested until the next year, it should be recovered by early spring and its productivity should be unaffected. Key words: Etiolated growth, forage production, grazing management, regrowth, rest requirement, tillering


2011 ◽  
Vol 87 (05) ◽  
pp. 669-683 ◽  
Author(s):  
Martin Riopel ◽  
Jean Bégin ◽  
Jean-Claude Ruel

For certain mature forests dominated by balsam fir (Abies balsamea [L.] Mill.) or black spruce (Picea mariana [Mill.] BSP), it may be preferable to harvest trees with diameter at breast height greater than 15 cm while conserving smaller ones. This treatment, called harvesting with protection of small merchantable trees, produces strips, where partial cutting is applied, alternating with corridors, which are disturbed by heavy equipment during harvesting. This project studied stocking levels five years after treatment on 4896 sub-plots of 4 m2 in 22 blocks. Stocking coefficients (SC) for coniferous and deciduous species were modeled in order to identify variables affecting stocking. The strips had well-distributed coniferous regeneration, while SC in the corridors were more variable and lower, occasionally less than 60%. Black spruce-dominated sites were not as well stocked as balsam fir-dominated sites. Stocking levels of protected coniferous merchantable trees positively influence coniferous and deciduous SC in the corridors. The presence of coniferous species is also affected by harvest season and total annual rainfall. Alternative silvicultural treatments applicable in certain corridors are presented.


2010 ◽  
Vol 40 (6) ◽  
pp. 1128-1135 ◽  
Author(s):  
M.J. Krasowski ◽  
M.B. Lavigne ◽  
J. Olesinski ◽  
P.Y. Bernier

We used 15 site-years of minirhizotron observations (1998–2006 at one site; 1998–2000 and 2004–2006 at second site) from two mature balsam fir ( Abies balsamea (L.) Mill.) sites to quantify interannual variability in fine root demography and assess the accuracy of estimates from early years of observation. Annual production varied fourfold at Forêt Montmorency (FM) (5.8–26.5 roots·100 cm–2) and twofold at Green River (GR) (7.2–14.2 roots·100 cm–2). Annual mortality varied more than 30-fold at the two sites (FM: 0.7–23.2 roots·100 cm–2; GR: 0.3–10.9 roots·100 cm–2), year-end standing crops varied two- to eight-fold (FM: 3.6–28.4 roots·100 cm–2; GR 8.5–18.6 roots·100 cm–2), and median life-span of annual cohorts varied from 180 to 540 days at FM and from 350 to 577 days at GR. This variation illustrates that root demography estimates from short-term studies may differ widely from long-term means. Annual mortality and standing crops were lowest in the first year of observation and tended to increase for two or more years at both sites, whereas these trends were not observed for annual production. Our results indicate that minirhizotron tubes must be in place for more than 2 years to accurately estimate fine root demography at balsam fir sites.


2017 ◽  
Vol 93 (1) ◽  
pp. 95-102 ◽  
Author(s):  
M. P. Clavijo ◽  
P. S. Cornaglia ◽  
A. Batisttella ◽  
E. Borodowski

1953 ◽  
Vol 31 (3) ◽  
pp. 334-360 ◽  
Author(s):  
J. T. Basham ◽  
P. V. Mook ◽  
A. G. Davidson

Four separate investigations of decay in balsam fir (Abies balsamea (L.) Mill.) have been carried out in recent years by forest pathologists in Eastern North America. Early in these studies it became apparent that the existing ideas concerning the identity of the fungi responsible for decay in living balsam fir trees required considerable revision. Trunk rot was confirmed as being caused mainly by Stereum sanguinolentum Alb. and Schw. ex Fries; however, five fungi, headed by Corticium galactinum (Fries) Burt, were found associated with most of the white stringy butt rots, and two fungi, Coniophora puteana (Schum. ex Fries) Karst. and Polyporus balsameus Peck, were associated with most of the brown cubical butt rots. Hitherto Poria subacida (Peck) Sacc. and P. balsameus were believed to cause practically all white and brown butt rots, respectively, in this species. The effect of site on the decay of living balsam fir is discussed, as is the extent and kind of decay with which each of the nine predominant heart-rot fungi was found associated. A brief outline is presented concerning the fungi found associated with the deterioration of dead balsam fir.


The Holocene ◽  
2018 ◽  
Vol 28 (10) ◽  
pp. 1672-1679 ◽  
Author(s):  
Abed Nego Jules ◽  
Hugo Asselin ◽  
Yves Bergeron ◽  
Adam A Ali

Marginal stands of balsam fir ( Abies balsamea [L.] Mill.) and eastern white cedar ( Thuja occidentalis L.) are found north of their limits of continuous distribution in eastern North America. Regional-scale paleoecological studies have suggested that fir and cedar populations could have had larger extents in the past. This study aimed at verifying this hypothesis at the local scale. Wood charcoal fragments were collected from the soils of two marginal fir and cedar stands as well as from 15 sites in the surrounding forest matrix where the species are absent currently. Anatomical identification and radiocarbon-dating showed that fir was more extensive in the study area until about 680 cal. BP, representing up to 31% of the charcoal assemblages at sites where it is currently absent. The evidence is less conclusive for cedar, however, although some of the charcoal fragments from the matrix sites could have been either fir or cedar (undistinguishable). Most of the dated fir/cedar charcoal in the matrix were from the ‘Medieval Warm Period’ (ca. 1000 cal. BP), suggesting contraction may have occurred at that time. Marginal fir – and possibly cedar – stands are thus relics of once more extensive populations. Fire is likely the main factor having contributed to the contraction of the species’ distributions. Fir and cedar are now relegated to areas where fires are less frequent and severe, such as the shores of lakes and rivers.


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