{"title":"在整个冰川期和全新世,火作为中欧和东欧生态系统动态的驱动因素","authors":"G. Florescu, A. Feurdean","doi":"10.4316/GEOREVIEW.2016.0.0.305","DOIUrl":null,"url":null,"abstract":"Sedimentary microscopic charcoal (particles smaller than 150 microns) has been used to describe multi-decadal to millennial scale biomass burning at regional scales, whereas macroscopic charcoal (particles larger than 150 microns) analysis is increasingly used to investigate past biomass burning at a local scale","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"21-22"},"PeriodicalIF":0.0000,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Fire as a driver of ecosystem dynamics in Central and Eastern Europe throughout the Lateglacial and Holocene\",\"authors\":\"G. Florescu, A. Feurdean\",\"doi\":\"10.4316/GEOREVIEW.2016.0.0.305\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Sedimentary microscopic charcoal (particles smaller than 150 microns) has been used to describe multi-decadal to millennial scale biomass burning at regional scales, whereas macroscopic charcoal (particles larger than 150 microns) analysis is increasingly used to investigate past biomass burning at a local scale\",\"PeriodicalId\":30470,\"journal\":{\"name\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"volume\":\"26 1\",\"pages\":\"21-22\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2016-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.4316/GEOREVIEW.2016.0.0.305\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.305","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Fire as a driver of ecosystem dynamics in Central and Eastern Europe throughout the Lateglacial and Holocene
Sedimentary microscopic charcoal (particles smaller than 150 microns) has been used to describe multi-decadal to millennial scale biomass burning at regional scales, whereas macroscopic charcoal (particles larger than 150 microns) analysis is increasingly used to investigate past biomass burning at a local scale