首页> Isotopes in environmental and health studies> Do n-alkane biomarkers in soils/sediments reflect the δ²H isotopic composition of precipitation? A case study from Mt. Kilimanjaro and implications for paleoaltimetry and paleoclimate research.

Do n-alkane biomarkers in soils/sediments reflect the δ²H isotopic composition of precipitation? A case study from Mt. Kilimanjaro and implications for paleoaltimetry and paleoclimate research.

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第一作者： Michael,Zech

第一单位： a Department of Soil Physics , Chair of Geomorphology and Institute of Soil Science and Soil Geography, University of Bayreuth , Bayreuth , Germany.;b Department of Soil Biogeochemistry , Martin Luther University Halle-Wittenberg , Halle , Germany.

作者： Michael,Zech ^[1] ; Roland,Zech ^[2] ; Kazimierz,Rozanski ^[3] ; Gerd,Gleixner ^[4] ; Wolfgang,Zech ^[5]

作者单位： a Department of Soil Physics , Chair of Geomorphology and Institute of Soil Science and Soil Geography, University of Bayreuth , Bayreuth , Germany.;b Department of Soil Biogeochemistry , Martin Luther University Halle-Wittenberg , Halle , Germany. ^[1] c Geographical Institute, University of Bern , Bern , Switzerland. ^[2] d Faculty of Physics and Applied Computer Science , AGH University of Science and Technology , Kraków , Poland. ^[3] e Max Planck Institute for Biogeochemistry , Jena , Germany. ^[4] a Department of Soil Physics , Chair of Geomorphology and Institute of Soil Science and Soil Geography, University of Bayreuth , Bayreuth , Germany. ^[5]

关键词 Mt. Kilimanjaro altitude effect evaporative enrichment hydrogen-2 isotope ecology lipid biomarkers n-alkanes oxygen-18 paleoaltimetry paleoclimate soil

医学主题词烷烃类(Alkanes);氘(Deuterium);地质沉积物(Geologic Sediments);气象学(Meteorology);古生物学(Paleontology);雨(Rain);土壤(Soil)

DOI 10.1080/10256016.2015.1058790

PMID 26156121

发布时间 2017-11-16

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