| SPELEOTHEMS |
Mangini et al. 2005 Spannagel Cave Stalagmite Oxygen Isotope Data and Temperature Reconstruction
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Mangini, A.;Spoetl, C.;Verdes, P. 2005 Reconstruction of temperature in the Central Alps during the past 2000 yr from a d18O
stalagmite record Earth and Planetary Science Letters Vol. 235, Issues 3-4, Pages 741-751, 15 July 2005.
| Data Coverage |
North: 47.09 * South: 47.09 |
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West: 11.67 * East: 11.67 |
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Altitude: 2531 m |
Start Year: -90 AD
End Year: 1935 AD
Data: Please Cite Data Contributors!
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Summary: The precisely dated isotopic composition of a stalagmite from Spannagel Cave
in the Central Alps is translated into a highly resolved record of temperature
at high elevation during the past 2000 yr. Temperature maxima during the
Medieval Warm Period between 800 and 1300 AD are in average about 1.7°C higher
than the minima in the Little Ice Age and similar to present-day values.
The high correlation of this record to d14C suggests that solar variability
was a major driver of climate in Central Europe during the past 2 millennia. More Info on Speleothems |
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Complete XML Record: noaa-cave-5433
(Last Revised: 2007-10-18 )
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