{"title":"Dvina湾(白海)全新世沉积物中的硅藻作为古海洋事件的指示物","authors":"E. Agafonova, Y. Polyakova","doi":"10.33624/2311-0147-2019-2(20)-197-200","DOIUrl":null,"url":null,"abstract":"The small inland White Sea, located in the western part of the vast shallow Eurasian Arctic shelf, is a key area for detailed reconstruction of the degradation of the latest Scandinavian ice sheet. In this work we aim to reconstruct the environmental history of the Dvina Bay inferred from diatom assemblages and a radiocarbon (AMS 14C) dating. In core 6042 we found diatoms in sediments since the first half of the Preboreal.","PeriodicalId":305989,"journal":{"name":"Issues of modern algology (Вопросы современной альгологии)","volume":"15 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Diatoms in the Holocene sediments of the Dvina Bay (White Sea) as indicators of paleooceanological events\",\"authors\":\"E. Agafonova, Y. Polyakova\",\"doi\":\"10.33624/2311-0147-2019-2(20)-197-200\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The small inland White Sea, located in the western part of the vast shallow Eurasian Arctic shelf, is a key area for detailed reconstruction of the degradation of the latest Scandinavian ice sheet. In this work we aim to reconstruct the environmental history of the Dvina Bay inferred from diatom assemblages and a radiocarbon (AMS 14C) dating. In core 6042 we found diatoms in sediments since the first half of the Preboreal.\",\"PeriodicalId\":305989,\"journal\":{\"name\":\"Issues of modern algology (Вопросы современной альгологии)\",\"volume\":\"15 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)-197-200\",\"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)-197-200","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Diatoms in the Holocene sediments of the Dvina Bay (White Sea) as indicators of paleooceanological events
The small inland White Sea, located in the western part of the vast shallow Eurasian Arctic shelf, is a key area for detailed reconstruction of the degradation of the latest Scandinavian ice sheet. In this work we aim to reconstruct the environmental history of the Dvina Bay inferred from diatom assemblages and a radiocarbon (AMS 14C) dating. In core 6042 we found diatoms in sediments since the first half of the Preboreal.