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  • 1
    Online-Ressource
    Online-Ressource
    Canadian Science Publishing ; 2015
    In:  Canadian Journal of Forest Research Vol. 45, No. 5 ( 2015-05), p. 595-606
    In: Canadian Journal of Forest Research, Canadian Science Publishing, Vol. 45, No. 5 ( 2015-05), p. 595-606
    Kurzfassung: The main environmental factors that drive lichen communities are still poorly known in northern boreal ecosystems. This study compares the effects of forest stand characteristics (height, canopy cover, and age) on fruticose epiphytic and terricolous lichen communities across a large region located at the interface between closed-crown boreal forests and northern open woodlands in the province of Quebec (Canada). The dataset consists of 875 plots spread across a 242 000 km 2 territory that ranges from the eastern to the western extremities of the province. The biomass of fruticose epiphytic lichens (Alectoria, Bryoria, Evernia, and Usnea) was evaluated at the branch, tree, and plot levels, and terricolous lichen cover (Cladonia spp.) was evaluated at the plot level. The results indicate that epiphytic and terricolous lichens respond significantly but differently to variations in forest characteristics. At the plot level, epiphytic lichen biomass was highest in the oldest stands ( 〉 100 years) and lowest in stand with low canopy cover ( 〈 25%) or in stands dominated by relatively short trees ( 〈 7 m). By contrast, terricolous lichen cover was highest in stands dominated by short ( 〈 7 m) or mid-sized (7–12 m) trees and lowest in stands with a relatively high canopy cover ( 〉 40%) or stands of intermediate age (60 to 100 years old). Species composition of epiphytic communities was also examined, and some species or genera exhibit a strong association with older stands (Alectoria sarmentosa (Ach.) Ach., Bryoria spp.) or with specific regions along the ca. 1500 km east–west gradient (Evernia mesomorpha Nyl. in the western part, Bryoria spp. in the central part, and A. sarmentosa in the eastern part). In terms of conservation, these results indicate that epiphytic lichens communities are potentially sensitive to the preferential logging of older stands. Both epiphytic and terricolous lichen communities are also potentially sensitive to expected climate change effects such as increased fire frequencies or increased forest growth.
    Materialart: Online-Ressource
    ISSN: 0045-5067 , 1208-6037
    Sprache: Englisch
    Verlag: Canadian Science Publishing
    Publikationsdatum: 2015
    ZDB Id: 1473096-0
    SSG: 23
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    In: Canadian Journal of Forest Research, Canadian Science Publishing, Vol. 53, No. 8 ( 2023-08-01), p. 556-578
    Kurzfassung: Regional analyses assessing the vulnerabilities of forest ecosystems and the forest sector to climate change are key to considering the heterogeneity of climate change impacts as well as the fact that risks, opportunities, and adaptation capacities might differ regionally. Here we provide the Regional Integrated Assessment of climate change on Quebec's forests, a work that involved several research teams and focused on climate change impacts on Quebec's commercial forests and on potential adaptation solutions. Our work showed that climate change will alter several ecological processes within Quebec's forests. These changes will result in important modifications in forest landscapes. Harvest will cumulate with climate change effects to further alter future forest landscapes, which will also have consequences on wildlife habitats (including woodland caribou habitat), avian biodiversity, carbon budget, and a variety of forest landscape values for Indigenous peoples. The adaptation of the forest sector will be crucial to mitigate the impacts of climate change on forest ecosystem goods and services and improve their resilience. Moving forward, a broad range of adaptation measures, notably through reducing harvest levels, should be explored to help strike a balance among social, ecological, and economic values. We conclude that without climate adaptation, strong negative economic and ecological impacts will likely affect Quebec's forests.
    Materialart: Online-Ressource
    ISSN: 0045-5067 , 1208-6037
    Sprache: Englisch
    Verlag: Canadian Science Publishing
    Publikationsdatum: 2023
    ZDB Id: 1473096-0
    SSG: 23
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Online-Ressource
    Online-Ressource
    Canadian Science Publishing ; 2000
    In:  Canadian Journal of Microbiology Vol. 46, No. 5 ( 2000), p. 433-440
    In: Canadian Journal of Microbiology, Canadian Science Publishing, Vol. 46, No. 5 ( 2000), p. 433-440
    Materialart: Online-Ressource
    ISSN: 1480-3275 , 0008-4166
    RVK:
    Sprache: Unbekannt
    Verlag: Canadian Science Publishing
    Publikationsdatum: 2000
    ZDB Id: 280534-0
    ZDB Id: 1481972-7
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Online-Ressource
    Online-Ressource
    Canadian Science Publishing ; 1989
    In:  Canadian Journal of Earth Sciences Vol. 26, No. 10 ( 1989-10-01), p. 1932-1943
    In: Canadian Journal of Earth Sciences, Canadian Science Publishing, Vol. 26, No. 10 ( 1989-10-01), p. 1932-1943
    Kurzfassung: In the Appalachians of southern Quebec, the contact between Siluro-Devonian rocks of the Connecticut Valley – Gaspé Synclinorium and the Cambro-Ordovician rocks of the Dunnage Zone is marked by an important thrust fault striking northwest, La Guadeloupe fault. This fault separates two stratigraphically distinct domains, but the regional deformations are related to the same orogenic period. In the Sherbrooke and Weedon areas, different structural features show evidence of La Guadeloupe fault and reveal its kinematics. The exposed rocks near the fault exhibit structures that indicate a strong deformation zone. The deformation includes well-developed stretching lineations and shearing zones. The ductile deformation is restricted to the Cambro-Ordovician rocks. Macroscopic and microscopic studies of samples from the shear zones related to La Guadeloupe fault reveal, systematically, a tectonic transport from southwest to northwest. This interpretation is supported by the quartz crystallographic c-axis orientation. In New England, La Guadeloupe fault seems to coincide with the Taconic unconformity, though a bifurcation of the pre-Silurian units exposed on the western side of this unconformity remains possible. In Quebec, the correlation and kinematics of La Guadeloupe fault extension towards the northeast are not completely understood. [Journal Translation]
    Materialart: Online-Ressource
    ISSN: 0008-4077 , 1480-3313
    Sprache: Englisch
    Verlag: Canadian Science Publishing
    Publikationsdatum: 1989
    ZDB Id: 417294-2
    ZDB Id: 1491201-6
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    In: Canadian Journal of Microbiology, Canadian Science Publishing, Vol. 46, No. 9 ( 2000), p. 866-866
    Materialart: Online-Ressource
    ISSN: 1480-3275 , 0008-4166
    RVK:
    Sprache: Unbekannt
    Verlag: Canadian Science Publishing
    Publikationsdatum: 2000
    ZDB Id: 280534-0
    ZDB Id: 1481972-7
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Online-Ressource
    Online-Ressource
    Canadian Science Publishing ; 2000
    In:  Canadian Journal of Microbiology Vol. 46, No. 9 ( 2000-09-01), p. 866-866
    In: Canadian Journal of Microbiology, Canadian Science Publishing, Vol. 46, No. 9 ( 2000-09-01), p. 866-866
    Materialart: Online-Ressource
    ISSN: 0008-4166 , 1480-3275
    RVK:
    Sprache: Englisch
    Verlag: Canadian Science Publishing
    Publikationsdatum: 2000
    ZDB Id: 280534-0
    ZDB Id: 1481972-7
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Online-Ressource
    Online-Ressource
    Canadian Science Publishing ; 1989
    In:  Canadian Journal of Earth Sciences Vol. 26, No. 11 ( 1989-11-01), p. 2268-2277
    In: Canadian Journal of Earth Sciences, Canadian Science Publishing, Vol. 26, No. 11 ( 1989-11-01), p. 2268-2277
    Kurzfassung: The Ascot–Weedon Formation and Magog Group are part of the Cambro-Ordovician oceanic domain of the Quebec Appalachians. The purpose of this work is to define the stratigraphic and structural relationships that exist between these units and the Siluro-Devonian sedimentary rocks: the Lac Aylmer Formation, to the northwest, and the St-Francis Group, to the southeast. Two structural domains are defined in the area. The first one, the northwestern zone, is essentially autochthonous. The Magog Group units are overlain by the Siluro-Devonian sediments of the Lac Aylmer Formation. Both units make up the northwest flank of the St-Victor Synclinorium, plunging slightly to the southwest. The second domain, to the southeast is made up of allochthons (Ascot–Weedon Formation and St-Francis Group) thrust on a large part of the southeast flank of the St-Victor Synclinorium. Structural analysis at mesoscopic, microscopic, and macroscopic scales indicates that the Ascot–Weedon Formation and the St-Francis Group are thrust northwesterly on southeast-dipping imbricate faults. Rocks of both units underlie the major La Guadeloupe Fault, bringing the Connecticut Valley – Gaspé Synclinorium over the St-Victor Synclinorium.
    Materialart: Online-Ressource
    ISSN: 0008-4077 , 1480-3313
    Sprache: Englisch
    Verlag: Canadian Science Publishing
    Publikationsdatum: 1989
    ZDB Id: 417294-2
    ZDB Id: 1491201-6
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Online-Ressource
    Online-Ressource
    Canadian Science Publishing ; 2000
    In:  Canadian Journal of Microbiology Vol. 46, No. 5 ( 2000-05-01), p. 433-440
    In: Canadian Journal of Microbiology, Canadian Science Publishing, Vol. 46, No. 5 ( 2000-05-01), p. 433-440
    Kurzfassung: A flow cytometric method (FCM) was used to detect and accurately enumerate a polycyclic aromatic hydrocarbon-degrading bacterial strain, Sphingomonas sp. 107, inoculated into a soil sample artificially contaminated with pyrene. To compare the FCM method with colony forming unit (CFU) assays, a rifampicin-resistant Sphingomonas sp. 107 was obtained which could be distinguished from the indigenous microflora, since there was no organism resistant to rifampicin in the soil that could transform indole to indigo (naphthalene dioxygenase activity). By combining light-scattering profiles (i.e., morphological properties), ethidium bromide influx (i.e., cell wall permeability), and fluorescence in situ hybridization against the 16S rRNA (i.e., detection specificity), we could enumerate the bacterial population of interest from the indigenous microflora and soil debris during the biotreatment. The FCM technique revealed that the number of inoculated Sphingomonas cells decreased gradually for 15 days of incubation before reaching a steady level of 7 to 12 × 10 5 cells·g -1 of soil. Similar values were obtained with the CFU assay. During this period, pyrene concentration decreased from 632 to 26 mg·kg -1 of dry soil. The FCM detection was improved by adding blocking reagent to the hybridization buffer to minimize the non-specific attachment of the fluorescent probe to soil particles. Combined with the improvements in probe technology, FCM detection was shown to be a good alternative to the conventional culture methods for the analysis of bacterial populations in environmental samples. This technique could be potentially useful for the detection of microorganisms that grow poorly in culture.Key words: polycyclic aromatic hydrocarbons, Sphingomonas, bioremediation, soil, laser flow cytometry.
    Materialart: Online-Ressource
    ISSN: 0008-4166 , 1480-3275
    RVK:
    Sprache: Englisch
    Verlag: Canadian Science Publishing
    Publikationsdatum: 2000
    ZDB Id: 280534-0
    ZDB Id: 1481972-7
    SSG: 12
    Standort Signatur Einschränkungen Verfügbarkeit
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