Academic literature on the topic 'Dark conifer stands'

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Journal articles on the topic "Dark conifer stands"

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Sultson, S. M., P. V. Mikhailov, A. A. Goroshko, et al. "Ecological characteristics of the siberian silkmoth (Dendrolimus sibiricus) (Insecta, Lasiocampidae) habitat in the Sayan montane conifer forests ecoregion." Povolzhskiy Journal of Ecology, no. 1 (March 23, 2024): 64–78. http://dx.doi.org/10.35885/1684-7318-2024-1-64-78.

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The article is devoted to studying the siberian silkmoth ( Dendrolimus sibiricus Tschetverikov, 1908) outbreaks, which is highly relevant today. The study was aimed at improving the system of forest pathology monitoring by revealing factors contributing to forest stand resistance to the pest attacks. We analyze the habitat conditions that are favorable for the siberian silkmoth in the early stages of its development and during the outbreak in dark coniferous taiga in the mountains of Southern Siberia (particularly, the Krasnoyarsk region). The research was based on remote sensing data combined
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Pereyaslovets, Vladimir M. "Biotopical distribution of sable in state nature reserve «Yuganskiy» area." Environmental Dynamics and Global Climate Change 9, no. 1 (2018): 46–52. http://dx.doi.org/10.17816/edgcc8948.

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The population dynamics and biotope distribution of the sable (Martes zibellina) in the Yuganskiy nature reserve have been a subject of continuous study since 1988. Data for analysis is obtained from annual route census surveys performed in February and March. There are four major types of sable habitats: dark conifer taiga (primarily formed by Pinus sibirica, Abies sibirica and Picea obovata), light conifer taiga (forest stands dominated by Pinus sylvestris), deciduous taiga (secondary forests dominated by Betula and Populus, with conifers in the undergrowth) and raised bogs (poorly drained t
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Klimchenko, Alexander V., and Sergey V. Verkhovets. "Carbon stocks in coarse woody debris in the middle taiga ecosystems located along the Yenisei river." Folia Forestalia, Series A - Forestry 54(2) (July 1, 2012): 134–36. https://doi.org/10.5281/zenodo.30743.

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This paper presents the results of the assessment of carbon stocks in the coarse woody debris in the prevailing forest types of the middle taiga. Carbon stocks in down coarse woody debris were estimated to total 58.2 million tonnes, 80% of which were found in dark conifer stands, 10% in deciduous forests, and 10% in pine forests and pine logging. In pine forests of the two dominant groups of forest types and pine logging, carbon stocks amounted to 1.5– 3.3 and 1.2 million tonnes, respectively. The values obtained in this study will be used to develop a database on ecosystem components re
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Moores, Andrew R., Robert S. Seymour, and Laura S. Kenefic. "Height development of shade-tolerant conifer saplings in multiaged Acadian forest standsPublication 2954 of the Maine Agricultural and Forest Experiment Station, University of Maine, Orono, Maine." Canadian Journal of Forest Research 37, no. 12 (2007): 2715–23. http://dx.doi.org/10.1139/x07-110.

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Understory growth dynamics of northern conifer species were studied in four stands managed under multiaged silvicultural systems in eastern Maine. Height growth of Picea rubens Sarg., Abies balsamea (L.) Mill., and Tsuga canadensis (L.) Carr. saplings between 0.5 and 6.0 m in height was related to the proportion open sky (POS), using sapling height as a covariate. Height growth of T. canadensis equaled A. balsamea and exceeded P. rubens under very low light levels (POS < 0.1) but is much less responsive to both increasing POS and taller heights, reaching 50% of its maximum height growth at
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Oskay, F., A. Lehtijärvi, H. T. Dogmuş-Lehtijärvi, and E. Halmschlager. "First Report of Brown Felt Blight Caused by Herpotrichia juniperi on Cedrus libani in Turkey." Plant Disease 95, no. 2 (2011): 222. http://dx.doi.org/10.1094/pdis-07-10-0547.

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Lebanon cedar (Cedrus libani A. Rich) is an ecologically, economically, and historically important conifer species that currently mainly occurs in the Taurus Mountains in southern Turkey. In former times, extensive forests of this species were also found in Syria and Lebanon. However, because of intensive cutting, burning, and goat grazing, only small populations are left in these countries. Currently, the range of Lebanon cedar covers approximately 600,000 ha in Turkey, including extremely degraded stands and bare karstic land that was previously covered by this species (1). Therefore, effort
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Алесенков Ю, М., and В. Иванчиков С. "PYROGENIC MODIFICATION OF A PINE STAND IN THE «DENEZHKIN KAMEN» RESERVE." Леса России и хозяйство в них, no. 1(88) (March 29, 2024): 112–18. http://dx.doi.org/10.51318/fret.2023.88.1.011.

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The features of the implementation of the initial stage of restoration of mossy pine after the passage of a grass-roots fire below average intensity are considered. The research was conducted three years later, after the fire occurred. Fires are not uncommon in the “Denezhkin Kamen” Nature Reserve, but there is a tendency to decrease the intensity of fires and the size of burned areas due to improved fire protection. The fire made minor changes to the structure of the stand. First of all, the changes affected the undergrowth and the thin layer of dark coniferous species. Quantitative indicator
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Shvetsov, E. G., A. S. Golyukov, and V. I. Kharuk. "Long-Term Dynamics of Forest Fires in Southern Siberia." Contemporary Problems of Ecology 16, no. 2 (2023): 205–16. http://dx.doi.org/10.1134/s1995425523020154.

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Abstract The research focus. Wildfire is a critical environmental disturbance affecting forest dynamics, succession, and the carbon cycle in Siberian forests. Forests of southern Siberia experienced an increase of fire rate. We analyzed spatial and temporal dynamics of burned area in the southern Central Siberian Mountains. We considered burning rate within different forest types: dark needle conifers (DNC) composed by Siberian pine, spruce and fir, light-needle composed by Scotch pine and larch, and mix wood (composed by birch, aspen and conifers). Methods. We used long-term (1982–2021) clima
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Schulze, E. D., C. Wirth, D. Mollicone, et al. "Factors promoting larch dominance in Eastern Siberia: fire versus growth performance and implications for carbon dynamics." Biogeosciences Discussions 9, no. 1 (2012): 21–62. http://dx.doi.org/10.5194/bgd-9-21-2012.

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Abstract. The relative roles of fire and climate in determining canopy species composition and aboveground carbon stocks were investigated. Measurements were made along a transect extending from the dark taiga zone of Central Siberia, where Picea and Abies dominate the canopy, into the Larix zone of Eastern Siberia. We test the hypotheses that the change in canopy species composition is based (1) on climate-driven performance only, (2) on fire only, or (3) on fire-performance interactions. We show that the evergreen conifers Picea obovata and Abies sibirica are the natural late-successional sp
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Schulze, E. D., C. Wirth, D. Mollicone, et al. "Factors promoting larch dominance in central Siberia: fire versus growth performance and implications for carbon dynamics at the boundary of evergreen and deciduous conifers." Biogeosciences 9, no. 4 (2012): 1405–21. http://dx.doi.org/10.5194/bg-9-1405-2012.

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Abstract. The relative role of fire and of climate in determining canopy species composition and aboveground carbon stocks were investigated. Measurements were made along a transect extending from the dark taiga zone of central Siberia, where Picea and Abies dominate the canopy, into the Larix zone of eastern Siberia. We test the hypotheses that the change in canopy species composition is based (1) on climate-driven performance only, (2) on fire only, or (3) on fire-performance interactions. We show that the evergreen conifers Picea obovata and Abies sibirica are the natural late-successional
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Dai, Y. C. "First Report of Laminated Root Rot on Sabina przewalskii Caused by Phellinus weirii sensu stricto in China." Plant Disease 88, no. 5 (2004): 573. http://dx.doi.org/10.1094/pdis.2004.88.5.573c.

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Members of the Phellinus weirii complex cause laminated root rot of living conifers. The cedar type (P. weirii (Murrill) Gilb. sensu stricto) of the complex is usually found on species of the Cupressaceae family, especially Thuja plicata in western North America, and the Douglas-fir type (P. sulphurascens Pilát) is found on species of the Pinaceae family (1,2,3). Outside North America, P. weirii occurs on species of Juniperus in the Ural Mountains, and P. sulphurascens occurs on other conifers in eastern Asia, including China (1). During a field inventory of wood-decay fungi in western China i
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Book chapters on the topic "Dark conifer stands"

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Wohl, Ellen. "January: Of Rocks and Ice." In Saving the Dammed. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190943523.003.0004.

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The beaver meadow is quiet in January. For many plants and animals, winter is a season of subdued activity, or of waiting. North St. Vrain Creek remains open along the main channel, the water flowing clear but tinted brown as pine bark between snowy banks. Densely growing thickets of willow closely line the banks. Each stem starts pale brown near the ground, then grades upward to shades of maroon or yellowish orange at the branch tips. In a bird’s-eye view, these startling colors make the meadow stand out distinctly from the dark green conifers that define the edges of the meadow. Spruce and f
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Wohl, Ellen. "October: Of Beavers and Humans." In Saving the Dammed. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190943523.003.0013.

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By mid-October, the first snow has fallen on the beaver meadow. There is no sign of snow when I visit a few days later, but the air feels chill in the shadows and a cool breeze leavens the sunshine’s warmth. Mostly, the beaver meadow seems a golden place. Many of the willow, aspen, and birch leaves have already fallen, but enough remain to create a glowing ménage of yellow, gold, palest orange, and tan. Each leaf refracts and filters the light so that it comes from every direction rather than only from above. Aspens on the north-facing valley slope stand bare and pale gray. Those on the south
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