E. Yuzhanina, N. Ryabogina, A.E. Borisov, I. Idrisov
{"title":"67.高加索中部的Tarskoe沼泽(俄罗斯北奥塞梯)","authors":"E. Yuzhanina, N. Ryabogina, A.E. Borisov, I. Idrisov","doi":"10.1080/00173134.2022.2130010","DOIUrl":null,"url":null,"abstract":"TheTarskoe swamp is oneof the largest peatbogs in the central part of theNorthCaucasus, it occupies about 20 ha in the basin between the Lesisty and Pastbishchny ranges (42° 57 ʹ46\" N, 44° 43 ʹ32\" E; 806 m above sea level [a.s.l.]). The climate is temperate continental with warm and very humid summer and medium cold, snowy winter. The swamp is located in the lower montane belt of broad-leaved forests dominated by Fagus orientalis Lipsky and Carpinus betulus L. with Quercus robur L., and an admixture of Corylus avellana L., Ulmus glabra Huds. and Pyrus caucasica Fed. Swamp vegetation is formed by Carex sp. and Phragmites australis (Cav.) Steud. with Matteuccia struthiopteris L. and Sphagnum sp., with thickets of Alnus glutinosa L. in some places. The swamp was drained for pasture and haymaking in the mid-twentieth century. Two previous studies investigated cores from the Tarskoe swamp (Knyazev et al. 1992; Neishtadt 1955, 1957). However, Neishtadt (1995, 1957) did not provide a dating for the sediment core and Knyazev et al. (1992) did not include the upper part of the core, which might have been removed during peat harvesting. The drilling for the present study was made in 2019 in an undisturbed area of the swamp.","PeriodicalId":50414,"journal":{"name":"Grana","volume":"62 1","pages":"73 - 76"},"PeriodicalIF":0.9000,"publicationDate":"2022-11-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"67. Tarskoe swamp, central Caucasus (North Ossetia, Russia)\",\"authors\":\"E. Yuzhanina, N. Ryabogina, A.E. Borisov, I. Idrisov\",\"doi\":\"10.1080/00173134.2022.2130010\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"TheTarskoe swamp is oneof the largest peatbogs in the central part of theNorthCaucasus, it occupies about 20 ha in the basin between the Lesisty and Pastbishchny ranges (42° 57 ʹ46\\\" N, 44° 43 ʹ32\\\" E; 806 m above sea level [a.s.l.]). The climate is temperate continental with warm and very humid summer and medium cold, snowy winter. The swamp is located in the lower montane belt of broad-leaved forests dominated by Fagus orientalis Lipsky and Carpinus betulus L. with Quercus robur L., and an admixture of Corylus avellana L., Ulmus glabra Huds. and Pyrus caucasica Fed. Swamp vegetation is formed by Carex sp. and Phragmites australis (Cav.) Steud. with Matteuccia struthiopteris L. and Sphagnum sp., with thickets of Alnus glutinosa L. in some places. The swamp was drained for pasture and haymaking in the mid-twentieth century. Two previous studies investigated cores from the Tarskoe swamp (Knyazev et al. 1992; Neishtadt 1955, 1957). However, Neishtadt (1995, 1957) did not provide a dating for the sediment core and Knyazev et al. (1992) did not include the upper part of the core, which might have been removed during peat harvesting. The drilling for the present study was made in 2019 in an undisturbed area of the swamp.\",\"PeriodicalId\":50414,\"journal\":{\"name\":\"Grana\",\"volume\":\"62 1\",\"pages\":\"73 - 76\"},\"PeriodicalIF\":0.9000,\"publicationDate\":\"2022-11-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Grana\",\"FirstCategoryId\":\"99\",\"ListUrlMain\":\"https://doi.org/10.1080/00173134.2022.2130010\",\"RegionNum\":4,\"RegionCategory\":\"生物学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"PLANT SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Grana","FirstCategoryId":"99","ListUrlMain":"https://doi.org/10.1080/00173134.2022.2130010","RegionNum":4,"RegionCategory":"生物学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"PLANT SCIENCES","Score":null,"Total":0}
67. Tarskoe swamp, central Caucasus (North Ossetia, Russia)
TheTarskoe swamp is oneof the largest peatbogs in the central part of theNorthCaucasus, it occupies about 20 ha in the basin between the Lesisty and Pastbishchny ranges (42° 57 ʹ46" N, 44° 43 ʹ32" E; 806 m above sea level [a.s.l.]). The climate is temperate continental with warm and very humid summer and medium cold, snowy winter. The swamp is located in the lower montane belt of broad-leaved forests dominated by Fagus orientalis Lipsky and Carpinus betulus L. with Quercus robur L., and an admixture of Corylus avellana L., Ulmus glabra Huds. and Pyrus caucasica Fed. Swamp vegetation is formed by Carex sp. and Phragmites australis (Cav.) Steud. with Matteuccia struthiopteris L. and Sphagnum sp., with thickets of Alnus glutinosa L. in some places. The swamp was drained for pasture and haymaking in the mid-twentieth century. Two previous studies investigated cores from the Tarskoe swamp (Knyazev et al. 1992; Neishtadt 1955, 1957). However, Neishtadt (1995, 1957) did not provide a dating for the sediment core and Knyazev et al. (1992) did not include the upper part of the core, which might have been removed during peat harvesting. The drilling for the present study was made in 2019 in an undisturbed area of the swamp.
期刊介绍:
Grana is an international journal of palynology and aerobiology. It is published under the auspices of the Scandinavian Palynological Collegium (CPS) in affiliation with the International Association for Aerobiology (IAA). Grana publishes original papers, mainly on ontogony (morphology, and ultrastructure of pollen grains and spores of Eucaryota and their importance for plant taxonomy, ecology, phytogeography, paleobotany, etc.) and aerobiology. All submitted manuscripts are subject to initial appraisal by the Editors, and, if found suitable for further consideration, to peer review by independent, anonymous expert referees. All peer review is single blind and submission is online via ScholarOne Manuscripts.