N. Rahimzadeh, Tobias Sprafke, C. Thiel, B. Terhorst, M. Frechen
{"title":"德国南部Franconia黄土多矿物和钾长石红外后红外激发发光年龄的比较","authors":"N. Rahimzadeh, Tobias Sprafke, C. Thiel, B. Terhorst, M. Frechen","doi":"10.5194/EGQSJ-70-53-2021","DOIUrl":null,"url":null,"abstract":"Abstract. Loess-paleosol sequences (LPSs) are essential records for reconstructing Quaternary paleoenvironments. No previous study has provided\nnumerical chronologies of loess in Lower Franconia, southern Germany; their\nchronostratigraphic assumptions have relied mainly on German\n(pedo)stratigraphic schemes. In this study, we provide for the first time a\nchronology for LPSs in Lower Franconia based on optically stimulated\nluminescence (OSL) dating using quartz and a comparison of K-feldspar\n(63–100 µm) and the polymineral fraction (4–11 µm). Our results show that all obtained ages are in stratigraphic order, ranging from\nHolocene to late Pleistocene, and in general confirm the former\nstratigraphical interpretations. A good agreement of the obtained ages is\nobserved between both feldspar grain size fractions; they also agree well\nwith the quartz OSL ages up to ∼50 ka. However, a marked\ndifference between the growth pattern of the dose response curves and\nconsequently different saturation characteristics of fine and coarse grains\nis found. Even though in our samples the discrepancy in ages is not very\nsignificant, we suggest the use of coarse-grained K-feldspar whenever\npossible in order to not be confronted with unknowns such as the mineral\ncomposition of the polymineral fraction.\n","PeriodicalId":11420,"journal":{"name":"E&G Quaternary Science Journal","volume":"115 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-02-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"A comparison of polymineral and K-feldspar post-infrared infrared stimulated luminescence ages of loess from Franconia, southern Germany\",\"authors\":\"N. Rahimzadeh, Tobias Sprafke, C. Thiel, B. Terhorst, M. Frechen\",\"doi\":\"10.5194/EGQSJ-70-53-2021\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. Loess-paleosol sequences (LPSs) are essential records for reconstructing Quaternary paleoenvironments. No previous study has provided\\nnumerical chronologies of loess in Lower Franconia, southern Germany; their\\nchronostratigraphic assumptions have relied mainly on German\\n(pedo)stratigraphic schemes. In this study, we provide for the first time a\\nchronology for LPSs in Lower Franconia based on optically stimulated\\nluminescence (OSL) dating using quartz and a comparison of K-feldspar\\n(63–100 µm) and the polymineral fraction (4–11 µm). Our results show that all obtained ages are in stratigraphic order, ranging from\\nHolocene to late Pleistocene, and in general confirm the former\\nstratigraphical interpretations. A good agreement of the obtained ages is\\nobserved between both feldspar grain size fractions; they also agree well\\nwith the quartz OSL ages up to ∼50 ka. However, a marked\\ndifference between the growth pattern of the dose response curves and\\nconsequently different saturation characteristics of fine and coarse grains\\nis found. Even though in our samples the discrepancy in ages is not very\\nsignificant, we suggest the use of coarse-grained K-feldspar whenever\\npossible in order to not be confronted with unknowns such as the mineral\\ncomposition of the polymineral fraction.\\n\",\"PeriodicalId\":11420,\"journal\":{\"name\":\"E&G Quaternary Science Journal\",\"volume\":\"115 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-02-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"E&G Quaternary Science Journal\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5194/EGQSJ-70-53-2021\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"E&G Quaternary Science Journal","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/EGQSJ-70-53-2021","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
A comparison of polymineral and K-feldspar post-infrared infrared stimulated luminescence ages of loess from Franconia, southern Germany
Abstract. Loess-paleosol sequences (LPSs) are essential records for reconstructing Quaternary paleoenvironments. No previous study has provided
numerical chronologies of loess in Lower Franconia, southern Germany; their
chronostratigraphic assumptions have relied mainly on German
(pedo)stratigraphic schemes. In this study, we provide for the first time a
chronology for LPSs in Lower Franconia based on optically stimulated
luminescence (OSL) dating using quartz and a comparison of K-feldspar
(63–100 µm) and the polymineral fraction (4–11 µm). Our results show that all obtained ages are in stratigraphic order, ranging from
Holocene to late Pleistocene, and in general confirm the former
stratigraphical interpretations. A good agreement of the obtained ages is
observed between both feldspar grain size fractions; they also agree well
with the quartz OSL ages up to ∼50 ka. However, a marked
difference between the growth pattern of the dose response curves and
consequently different saturation characteristics of fine and coarse grains
is found. Even though in our samples the discrepancy in ages is not very
significant, we suggest the use of coarse-grained K-feldspar whenever
possible in order to not be confronted with unknowns such as the mineral
composition of the polymineral fraction.