Conservation of Soil Cover of the Steppe in Federal Specially Protected Natural Areas

IF 0.6 Q4 ECOLOGY
O. V. Chernova, A. A. Prisyazhnaya
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引用次数: 0

Abstract

The basis of Russia’s natural reserve fund consists of federal state reserves, national parks, and wildlife sanctuaries, the representativeness of which in relation to the diversity of natural complexes, including soils, is the main mechanism for protecting natural diversity. Using the method of geoinformation analysis, the areal and typological representation of the natural diversity of steppe soils in the system of specially protected natural areas (SPNAs) of the country was assessed based on vector maps: Pochvennaya karta Rossii (Soil Map of Russia) on a scale of 1 : 2 500 000 (a combined version of the Pochvennaya karta RSFSR (Soil Map of the RSFSR) and the Pochvennaya karta Kryma (Soil Map of Crimea) and the Karty pochvenno-ekologicheskogo raionirovaniya v Rossiiskoi Federatsii (Map of Soil-Ecological Zoning of the Russian Federation) on a scale of 1 : 8 000 000. The area occupied by steppe soils in Russia is 1 564 000 km2 (9.4% of the total soil area of the country), of which 7.4% are soils of steppes (including forest–steppes and true steppes) and 2.0% are soils of dry steppes and semideserts. In protected areas, steppe soils occupy 11 500 km2 and are found in 23 nature reserves, 14 national parks, and 13 wildlife sanctuaries. The current areal representativeness of protected steppe areas is very low: less than 0.5% for the group “Soils of the steppes” and about 2% for the group “Soils of dry steppes and semideserts. “Of the 55 steppe soils, units of the legend of the “Soil Map of Russia,” 58% are represented in federal protected areas, while reserves, which account for a fifth of the total area of steppe protected areas, provide 81% of the typological representativeness. Currently, many natural steppe soils in Russia, including the most fertile ones, are not represented in protected areas. The most significant compact array of such soils in terms of area is located in Ciscaucasia. The largest area here is occupied by southern and ordinary mycelial–carbonate chernozems (World reference base for soil resources (2014) – Calcic Сhernozems (Pachic)), their area is about 98 000 km2 (7.9% of the soil area of the Russian steppes). There is a real threat of losing the last virgin examples of highly fertile soils typical of Ciscaucasia: southern and ordinary chernozems, dark chestnut, chestnut, light chestnut soils (WRB – Calcic Сhernozems (Pachic), Haplic Kastanozems, Calcic/Gypsic Kastanozems, Luvic Calcisols). Preservation of these soils in the virgin state, at least as samples for comparison with anthropogenically modified analogues, requires an inventory of all areas of their distribution and assignment of a protective status.

Abstract Image

Abstract Image

保护联邦特别自然保护区草原的土壤植被
摘要 俄罗斯自然保护区基金的基础包括联邦国家保护区、国家公园和野生动物保护区,这些保护区在包括土壤在内的自然综合体多样性方面的代表性是保护自然多样性的主要机制。利用地理信息分析方法,在矢量地图的基础上对国家特别保护自然区(SPNAs)系统中草原土壤自然多样性的面积和类型代表性进行了评估:俄罗斯土壤地图》比例尺为 1 : 2 500 000(《俄罗斯苏维埃联邦社会主义共和国土壤地图》和《克里米亚土壤地图》的合订本),《俄罗斯联邦土壤生态区划图》比例尺为 1 : 8 000 000。俄罗斯的草原土壤面积为 1 564 000 平方公里(占全国土壤总面积的 9.4%),其中 7.4%为草原土壤(包括森林草原和真正的草原),2.0%为干草原和半荒漠土壤。在保护区中,草原土壤占 11 500 平方公里,分布在 23 个自然保护区、14 个国家公园和 13 个野生动物保护区。目前,草原保护区的面积代表性非常低:"草原土壤 "组不足 0.5%,"干旱草原和半荒漠土壤 "组约为 2%。"俄罗斯土壤地图 "图例中的 55 个草原土壤单元中,58% 在联邦保护区内,而占草原保护区总面积五分之一的保护区提供了 81% 的类型代表性。目前,俄罗斯的许多天然草原土壤,包括最肥沃的土壤,在保护区中都没有体现。就面积而言,此类土壤最重要的密集区位于西高加索地区。这里面积最大的是南部和普通菌丝碳酸盐钙质土壤(世界土壤资源参考基地(2014 年)--钙质钙质土壤(帕奇克)),其面积约为 98 000 平方公里(占俄罗斯草原土壤面积的 7.9%)。西高加索地区典型的高肥力土壤的最后原始例子:南部和普通栗土、深栗土、栗土、浅栗土(WRB - 钙质Сhernozems (Pachic)、Haplic Kastanozems、钙质/Gypsic Kastanozems、Luvic Calcisols)面临着消失的真正威胁。要保持这些土壤的原始状态,至少将其作为与经过人为改造的类似土壤进行比较的样本,就需要对其分布的所有地区进行清查,并确定其保护状态。
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来源期刊
Arid Ecosystems
Arid Ecosystems ECOLOGY-
CiteScore
1.50
自引率
25.00%
发文量
59
期刊介绍: Arid Ecosystems  publishes original scientific research articles on desert and semidesert ecosystems and environment:systematic studies of arid territories: climate changes, water supply of territories, soils as ecological factors of ecosystems state and dynamics in different scales (from local to global);systematic studies of arid ecosystems: composition and structure, diversity, ecology; paleohistory; dynamics under anthropogenic and natural factors impact, including climate changes; studying of bioresources and biodiversity, and development of the mapping methods;arid ecosystems protection: development of the theory and methods of degradation prevention and monitoring; desert ecosystems rehabilitation;problems of desertification: theoretical and practical issues of modern aridization processes under anthropogenic impact and global climate changes.
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