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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
-
Africa
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East Africa
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Kenya (1)
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Tanzania
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Kilimanjaro (1)
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Oldoinyo Lengai (1)
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Kalahari Desert (1)
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Namib Desert (1)
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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Morocco
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Sahara (2)
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Southern Africa
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South Africa
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Western Cape Province South Africa (1)
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Antarctica (2)
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Greenland
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Asia
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Arabian Peninsula
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Oman (5)
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Far East
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China
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Mexico
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North America
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Oceania
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Polynesia
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Hawaii
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Niue (1)
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Pacific Ocean
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South Pacific (1)
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Argentina
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Brazil
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United States
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Primary terms
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Mesozoic
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Paleozoic
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Devonian
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speleothems
Fluid-inclusion petrography in calcite stalagmites: Implications for entrapment processes
The chronostratigraphy of the Anthropocene in southern Africa: Current status and potential
Dryland dunes and other dryland environmental archives as proxies for Late Quaternary stratigraphy and environmental and climate change in southern Africa
Holocene wet episodes recorded by magnetic minerals in stalagmites from Soreq Cave, Israel
Abstract For the first time, we present a decadal-scale stable isotope record (δ 18 O, δ 13 C) of 67 speleothem calcite samples coming from an artificial tunnel network located in Graz, Austria. Stable isotope data are interpreted with the help of time series (TS) analysis of mean air temperatures (MAT) and mean annual precipitations (MAP) that have been monitored and recorded in a neighbouring meteorological station. Speleothem records have proved to be very useful in reconstructing changes of environmental conditions. For studied stalagmites, which grew between 1945 and 2018, the δ 18 O values average −18.64‰ and range from −23‰ to −17‰ (VPDB, Vienna Pee Dee Belemnite), suggesting variable climatic conditions. The δ 18 O values of calcite increase along the growth axis and are correlated with high temporal resolution MAT, MAP and weighted mean annual δ 18 O of precipitations. For the same time interval, while the temperature TS show an increasing trend, with a steeper gradient since the 1980s, the precipitation TS presents a weak decreasing tendency. Increase in the δ 13 C values of speleothems from −33‰ to −24‰ (VPDB) is correlated with increasing temperature and drought, associated CO 2 degassing and soil erosion over the tunnel system.