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The Influences of Hydrology on the Radiogenic and Stable Carbon Isotope Composition of Cave Drip Water, Grotta di Ernesto (Italy)

Bibliographic Data

ID9246010
AuthorsJ Fohlmeister, A Schröder-Ritzrau, C Spötl, S FRISIA, R Miorandi, B Kromer, A Mangini
Year2010
Volume52
Issue4
Pages1529-1544
Publication date2010-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0033822200056289
OpenAlexW2203657041
LanguageEN
Citations received7
References cited37

14 C and δ 13 C values of C-containing species in cave drip waters are mainly controlled by the C isotope composition of karst rock and soil air, as well as by soil carbon dynamics, in particular the amount of soil CO 2 in the unsaturated soil zone and the process of calcite dissolution. Here, we investigate soil carbon dynamics by analyzing the 14 C activity and δ 13 C values of C dissolved in cave drip water. Monthly over a 2-yr period, we collected drip water from 2 drip sites, one fast and one relatively slow, within the shallow Grotta di Ernesto Cave (NE Italy). The 14 C data reveal a pronounced annual cycle. In contrast, the δ 13 C values do not show an annual pattern and only small interannual variability compared to the δ 13 C values of soil waters. The annual 14 C drip-water cycle is a function of drip-rate variability, soil moisture, and ultimately hydrology

Archaeology · Calcite · Carbon cycle · Cave · Geochemistry · Geography · Isotopes of carbon · Karst · Soil water · Stable isotope ratio · Total organic carbon · Water cycle · δ13C · Chemistry · Environmental Science · Geology and Paleoclimatology Research · Groundwater and Isotope Geochemistry · Karst Systems and Hydrogeology · Ecology · Environmental Chemistry · Geology · Paleontology · Soil Science

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Unique citing works7
Citations per year0,47
Citation span2011 - 2023 (13)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 7

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