{"title":"基于区域硅藻温度指示性质的波尔鞋米索沃湖温度状态重建","authors":"N. A. Isakova, A. G. Rogozin, L. V. Snitko","doi":"10.33624/2311-0147-2019-2(20)-210-214","DOIUrl":null,"url":null,"abstract":"Diatom assemblages from the top levels of botton sediments in Lake Bol’shoe Miassovo (Southern Urals) has been studied. On the basis of species composition and termoindication properties of algae a reconstruction of the thermal regime of the lake for the last 1000 years is made. It is established that its significant change was caused by rapid climate warming that began in the 19th century in the Southern Urals.","PeriodicalId":305989,"journal":{"name":"Issues of modern algology (Вопросы современной альгологии)","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Reconstruction of the temperature regime of Bol’shoe Miassovo Lake on the basis of regional diatoms termoindication properties\",\"authors\":\"N. A. Isakova, A. G. Rogozin, L. V. Snitko\",\"doi\":\"10.33624/2311-0147-2019-2(20)-210-214\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Diatom assemblages from the top levels of botton sediments in Lake Bol’shoe Miassovo (Southern Urals) has been studied. On the basis of species composition and termoindication properties of algae a reconstruction of the thermal regime of the lake for the last 1000 years is made. It is established that its significant change was caused by rapid climate warming that began in the 19th century in the Southern Urals.\",\"PeriodicalId\":305989,\"journal\":{\"name\":\"Issues of modern algology (Вопросы современной альгологии)\",\"volume\":\"1 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Issues of modern algology (Вопросы современной альгологии)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.33624/2311-0147-2019-2(20)-210-214\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Issues of modern algology (Вопросы современной альгологии)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.33624/2311-0147-2019-2(20)-210-214","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Reconstruction of the temperature regime of Bol’shoe Miassovo Lake on the basis of regional diatoms termoindication properties
Diatom assemblages from the top levels of botton sediments in Lake Bol’shoe Miassovo (Southern Urals) has been studied. On the basis of species composition and termoindication properties of algae a reconstruction of the thermal regime of the lake for the last 1000 years is made. It is established that its significant change was caused by rapid climate warming that began in the 19th century in the Southern Urals.
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