{"title":"Ancient Agrolandscapes of the Darkhat Basin (Northern Mongolia)","authors":"T. N. Prudnikova","doi":"10.1134/S2079096124700471","DOIUrl":null,"url":null,"abstract":"<p>According to remote sensing (space image decoding), the Darkhat Basin of Northern Mongolia is a sparsely populated cattle-breeding territory, which was an area of developed agriculture in the past. Quite numerous land plots are recognized at the end spills of rivers flowing from its mountainous frame, lake and river terraces, floodplains, and deluvial–proluvial slopes, at absolute elevations from 1535 to 1700 meters a.s.l. or more. Among the wide soil range, here are fertile chernozems, chestnut, and dark chestnut soils. The geological position of the region and its confinement to the southwestern periphery of the Baikal rift contributed to both the formation of the basin and its modern seismic activity, manifestations of basaltoid volcanism, as well as the emergence of a “regional thermal anomaly” (Vilor et al., 2019). The basin also belongs to the Khubsugul Upper Riphean–Cambrian phosphorite-bearing basin, where deposits and numerous manifestations of phosphorites, the basis of mineral fertilizers, are known (Il’in, 1973). The long history of the formation of the relief of the Darkhat Basin led to the enrichment to a greater or lesser extent of its Quaternary deposits with phosphorus compounds useful for agricultural practices. Modern volcanism and continental rifting processes contributed to the emergence of thermal springs in this area; nitrogen baths, which are a kind of liquid nitrogen fertilizer, are known here (<i>Mongol’skaya...</i>, 1990). The combination of the following features: fertile soils, the thermal anomaly of the Baikal rift, and the presence of nitrogen thermal springs, as well as deposits and manifestations of phosphorites, products of their destruction, enriching the soil, contributed to the development of agriculture here. Manifestations of Cenozoic basaltoid volcanism, causing the presence of fertile volcanic ash, as well as processes of medieval volcanic activation (Arzhannikov et al., 2017), played a possible role in the development of agricultural practices on this territory. Social and political events are also important reasons. According to an earlier analysis of ancient agriculture in the arid territories of Central Asia (Prudnikova, 2020), its maximum development in the Darkhat Basin occurred in the early Middle Ages, a time attributed to the small climatic optimum.</p>","PeriodicalId":44316,"journal":{"name":"Arid Ecosystems","volume":"14 4","pages":"496 - 506"},"PeriodicalIF":0.6000,"publicationDate":"2025-02-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Arid Ecosystems","FirstCategoryId":"1085","ListUrlMain":"https://link.springer.com/article/10.1134/S2079096124700471","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"ECOLOGY","Score":null,"Total":0}
引用次数: 0
Abstract
According to remote sensing (space image decoding), the Darkhat Basin of Northern Mongolia is a sparsely populated cattle-breeding territory, which was an area of developed agriculture in the past. Quite numerous land plots are recognized at the end spills of rivers flowing from its mountainous frame, lake and river terraces, floodplains, and deluvial–proluvial slopes, at absolute elevations from 1535 to 1700 meters a.s.l. or more. Among the wide soil range, here are fertile chernozems, chestnut, and dark chestnut soils. The geological position of the region and its confinement to the southwestern periphery of the Baikal rift contributed to both the formation of the basin and its modern seismic activity, manifestations of basaltoid volcanism, as well as the emergence of a “regional thermal anomaly” (Vilor et al., 2019). The basin also belongs to the Khubsugul Upper Riphean–Cambrian phosphorite-bearing basin, where deposits and numerous manifestations of phosphorites, the basis of mineral fertilizers, are known (Il’in, 1973). The long history of the formation of the relief of the Darkhat Basin led to the enrichment to a greater or lesser extent of its Quaternary deposits with phosphorus compounds useful for agricultural practices. Modern volcanism and continental rifting processes contributed to the emergence of thermal springs in this area; nitrogen baths, which are a kind of liquid nitrogen fertilizer, are known here (Mongol’skaya..., 1990). The combination of the following features: fertile soils, the thermal anomaly of the Baikal rift, and the presence of nitrogen thermal springs, as well as deposits and manifestations of phosphorites, products of their destruction, enriching the soil, contributed to the development of agriculture here. Manifestations of Cenozoic basaltoid volcanism, causing the presence of fertile volcanic ash, as well as processes of medieval volcanic activation (Arzhannikov et al., 2017), played a possible role in the development of agricultural practices on this territory. Social and political events are also important reasons. According to an earlier analysis of ancient agriculture in the arid territories of Central Asia (Prudnikova, 2020), its maximum development in the Darkhat Basin occurred in the early Middle Ages, a time attributed to the small climatic optimum.
根据遥感(空间图像解码),蒙古北部达哈特盆地是一个人口稀少的养牛区,过去是一个农业发达的地区。相当多的地块被确认在河流从它的山脉、湖泊和河流梯田、洪泛平原和洪积斜坡的末端,绝对海拔从1535米到1700米或更高。在广阔的土壤范围内,这里有肥沃的黑钙土、栗子土和黑栗子土。该地区的地质位置及其对贝加尔湖裂谷西南边缘的限制有助于盆地的形成及其现代地震活动,玄武岩火山活动的表现以及“区域热异常”的出现(Vilor et al., 2019)。该盆地还属于Khubsugul上里菲—寒武系含磷岩盆地,在该盆地中,磷岩的沉积和大量表现是已知的矿物肥料的基础(Il’in, 1973)。达克哈特盆地的长期形成历史使其第四纪沉积物或多或少地富集了对农业生产有用的磷化合物。现代火山作用和大陆裂陷作用是该区温泉形成的主要原因;氮浴,是一种液氮肥料,在这里被称为(蒙古的skaya…, 1990)。肥沃的土壤、贝加尔湖裂谷的热异常、氮温泉的存在,以及磷矿的沉积和表现,它们的破坏产物,丰富了土壤,这些特征的结合促进了这里农业的发展。新生代玄武岩类火山活动的表现,导致了肥沃火山灰的存在,以及中世纪火山活动的过程(Arzhannikov et al., 2017),在该地区农业实践的发展中发挥了可能的作用。社会和政治事件也是重要原因。根据对中亚干旱地区古代农业的早期分析(Prudnikova, 2020),其在Darkhat盆地的最大发展发生在中世纪早期,这一时期归因于小型气候最佳。
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.