2013
DOI: 10.1134/s1875372813010071
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Natural and transformed geosystems of the Tunkinskaya depression

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Cited by 3 publications
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“…Western and northern winds prevail in accordance with the latitudinal location of the depression and the deeply incised river valleys descending from the north, originating from slopes of the Tunkinskie Goltzy Range. The landscape-forming units of the Badary area are piedmont sub-taiga pine geomes (Mikheev & Ryashin, 1977;Atutova, 2018), which are characterised by a combination of gray forest soils and soddyslightly podzolic sandy loamy soils (Letunov, 1962). Gently sloping pine grass groups of facies with shrub undergrowth of Rhododendron dauricum L. represent the vegetation of the study area (Atutova, 2018).…”
Section: Methodsmentioning
confidence: 99%
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“…Western and northern winds prevail in accordance with the latitudinal location of the depression and the deeply incised river valleys descending from the north, originating from slopes of the Tunkinskie Goltzy Range. The landscape-forming units of the Badary area are piedmont sub-taiga pine geomes (Mikheev & Ryashin, 1977;Atutova, 2018), which are characterised by a combination of gray forest soils and soddyslightly podzolic sandy loamy soils (Letunov, 1962). Gently sloping pine grass groups of facies with shrub undergrowth of Rhododendron dauricum L. represent the vegetation of the study area (Atutova, 2018).…”
Section: Methodsmentioning
confidence: 99%
“…The landscape-forming units of the Badary area are piedmont sub-taiga pine geomes (Mikheev & Ryashin, 1977;Atutova, 2018), which are characterised by a combination of gray forest soils and soddyslightly podzolic sandy loamy soils (Letunov, 1962). Gently sloping pine grass groups of facies with shrub undergrowth of Rhododendron dauricum L. represent the vegetation of the study area (Atutova, 2018). However, there are no natural pine forests remained, which is caused by frequent wildfires that destroyed 80 km 2 of forest plantations per wildfire season (Lekhatinov & Lekhatinova, 2010).…”
Section: Methodsmentioning
confidence: 99%
“…A nivel internacional, las investigaciones asociadas con el estudio del paisaje han estado enfocadas en caracterizar la estructura (Alcántara y Muñoz, 2015;Erikstad, Uttakleiv y Halvorsen, 2015;Franch, Priego, Bollo, Cancer y Bautista, 2015;Kuzmenko, 2011;Lysanova, Semenov y Sorokovoi, 2011;Mar-dones, 2006;Ramón, Salinas y Remond, 2009;Suvorov y Kitov, 2013), diversidad (Fetisov, 2011) y transformación de los paisajes (Atutova, 2013). Además, de ser la base para evaluar la heterogeneidad (Suárez, Chacón y Ataroff, 2011) y el potencial ecológico de los geocomplejos (Kuznetsova et al, 2011), así como, para realizar el diagnóstico geoecológico de los mismos (García, Miravet, Salinas y Domínguez, 2019;La O, Salinas y Licea, 2012;Salinas, Mirandola, De Souza y Garcia, 2019).…”
Section: Introductionunclassified