Reconstruction of drip-water δ<sup>18</sup>O based on calcite oxygen and clumped isotopes of speleothems from Bunker Cave (Germany)
The geochemical signature of many speleothems used for reconstruction of past continental climates is affected by kinetic isotope fractionation. This limits quantitative paleoclimate reconstruction and, in cases where the kinetic fractionation varies with time, also affects relative paleoclimate int...
Main Authors: | T. Kluge, H. P. Affek, T. Marx, W. Aeschbach-Hertig, D. F. C. Riechelmann, D. Scholz, S. Riechelmann, A. Immenhauser, D. K. Richter, J. Fohlmeister, A. Wackerbarth, A. Mangini, C. Spötl |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2013-02-01
|
Series: | Climate of the Past |
Online Access: | http://www.clim-past.net/9/377/2013/cp-9-377-2013.pdf |
Similar Items
-
Simulated oxygen isotopes in cave drip water and speleothem calcite in European caves
by: A. Wackerbarth, et al.
Published: (2012-11-01) -
Bunker Cave stalagmites: an archive for central European Holocene climate variability
by: J. Fohlmeister, et al.
Published: (2012-10-01) -
Holocene climate variability in north-eastern Italy: potential influence of the NAO and solar activity recorded by speleothem data
by: D. Scholz, et al.
Published: (2012-08-01) -
Novel method for determining <sup>234</sup>U–<sup>238</sup>U ages of Devils Hole 2 cave calcite (Nevada)
by: X. Li, et al.
Published: (2021-01-01) -
Climate Variability in Central Europe during the Last 2500 Years Reconstructed from Four High-Resolution Multi-Proxy Speleothem Records
by: Sarah Waltgenbach, et al.
Published: (2021-04-01)