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Dating of Lake and Loess Sediments

Bibliographic Data

ID9244206
AuthorsJuerg Beer, Michael Sturm (0000-0003-2414-7894)
Year1995
Volume37
Issue1
Pages81-86
Publication date1995-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s003382220001482x
OpenAlexW2506730750
LanguageEN
Citations received1
References cited10

Lake and loess sediments represent archives that record important information about the iocal, regional and global climate conditions in the past. Lake sediments consist of autochthonous particles formed by biogeochemical processes within the lake and allochthonous particles brought into the lake from the catchment area. After deposition, the stratigraphy of the sediment can be altered by chemical, physical and biological processes. Under favored conditions, the sediment shows individual annual layers (varves), which can be used to date the sediment. Other dating methods are based on radioactive decay ( 14 C, 210 Pb) or on time markers such as tephra layers, deposits of natural catastrophes, e.g., floods, or radioactivity, e.g., emissions from a nuclear power plant

Biogeochemical cycle · Earth science · Geochemistry · Geomorphology · Loess · Paleolimnology · Radiocarbon dating · Sediment · Sedimentary rock · Sedimentology · Tephra · Varve · Volcano · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Ecology · Geology · Paleontology · Stratigraphy

  • Last 40ka climate changes as deduced from the lacustrine sediments of Lake Biwa, central Japan

    Open Access•Kazuyoshi Yamada•Quaternary International•2004

  • Magnetostratigraphical dating of loess deposits in China

    Open Access•Friedrich Heller, Tungsheng Liu et al.•Nature•1982

Unique citing works1
Citations per year0,05
Citation span2004 - 2004 (1)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 1

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