{"title":"罗马尼亚喀尔巴阡山脉的MIS 5e高海拔岩洞石δ13C-δ18O记录","authors":"V. Drăgușin","doi":"10.4316/GEOREVIEW.2016.0.0.299","DOIUrl":null,"url":null,"abstract":"We present here a speleothem δ 13 C-δ 18 O record from the Last Interglacial period that was retrieved from a small cave in the Făgăras Mountains (2435 m asl). Current monitoring work shows that the average temperature inside the cave is ~3°C. Stalagmite M3-R2/1 is only 5 cm long and its growth model was calculated using six U-Th ages. According to this, the stalagmite formed between 125.5 (±1.3) and 123 (±1.3) ka, during the warmest stage of the Last Interglacial","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"14"},"PeriodicalIF":0.0000,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A MIS 5e high-altitude speleothem δ13C-δ18O record from the Romanian Carpathians\",\"authors\":\"V. Drăgușin\",\"doi\":\"10.4316/GEOREVIEW.2016.0.0.299\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"We present here a speleothem δ 13 C-δ 18 O record from the Last Interglacial period that was retrieved from a small cave in the Făgăras Mountains (2435 m asl). Current monitoring work shows that the average temperature inside the cave is ~3°C. Stalagmite M3-R2/1 is only 5 cm long and its growth model was calculated using six U-Th ages. According to this, the stalagmite formed between 125.5 (±1.3) and 123 (±1.3) ka, during the warmest stage of the Last Interglacial\",\"PeriodicalId\":30470,\"journal\":{\"name\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"volume\":\"26 1\",\"pages\":\"14\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2016-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"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.2016.0.0.299\",\"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.2016.0.0.299","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
A MIS 5e high-altitude speleothem δ13C-δ18O record from the Romanian Carpathians
We present here a speleothem δ 13 C-δ 18 O record from the Last Interglacial period that was retrieved from a small cave in the Făgăras Mountains (2435 m asl). Current monitoring work shows that the average temperature inside the cave is ~3°C. Stalagmite M3-R2/1 is only 5 cm long and its growth model was calculated using six U-Th ages. According to this, the stalagmite formed between 125.5 (±1.3) and 123 (±1.3) ka, during the warmest stage of the Last Interglacial