This dataset includes speleothem cabon isotopes, oxygen isotopes, U-Th ages, and fluid inclusion hydrogen isotopes used to reconstruct climate in the Swiss Alps during the Last Interglacial period (~129 and 116 ka). The speleothems were collected from caves in the Malchsee-Frutt region of Switzerland (46°47' N, 8°16'E, ~1720 m.a.s.l.). The four speleothems (M37-1-16A, M37-1-16C, M6-73-3, and M37-1-23A) used in this dataset were found broken and inactive in the caves. The speleothems represent a stacked record, with a combined ~19 ka years of growth between 132.0 ± 0.5 ka and 112.0 ± 0.5 ka. Speleothem length ranges between 0.13 and 0.88 m. The data colletion was done between 2018 and 2019. The data was obtained using mass spectrometry techn...
The climatic controls on the stable carbon isotopic composition (δ13C) of speleothem carbonate are l...
The Vil-car-1 flowstone core from Villars cave (SW France) provides one of the first European speleo...
Marine Isotope Stage 3 (MIS 3, 57–27 ka) was characterised by numerous rapid climate oscillations (i...
A precisely dated speleothem isotope record from the Sieben Hengste cave system, Switzerland, reveal...
We present a new high resolution speleothem stable isotope record from the Villars Cave (SW-France) ...
The Vil-car-1 flowstone core from Villars cave (SW France) provides one of the first European speleo...
Hermannshöhle is a show cave located near Kirchberg/Wechsel in Lower Austria. Together with three ne...
Holocene climate in Central Europe was characterized by variations on millennial to decadal time sca...
We present stable carbon (δ13C) and oxygen (δ18O) isotope records from two partially coeval speleoth...
Western Europe is the region with the highest density of published speleothem δ18O (δ18Ospel) record...
We present stable carbon (δ13C) and oxygen (δ18O) isotope records from two partially coeval speleoth...
The dataset includes speleothem carbon isotopes, oxygen isotopes, U-Th ages, and fluid inlcusion hyd...
The oxygen isotopic composition of calcite speleothems (stalagmites, etc.) can be used as a record o...
Western Europe is the region with the highest density of published speleothem δ18O (δ18Ospel) record...
High-precision TIMS U-series dates and continuous stable oxygen and carbon isotope profiles of a 400...
The climatic controls on the stable carbon isotopic composition (δ13C) of speleothem carbonate are l...
The Vil-car-1 flowstone core from Villars cave (SW France) provides one of the first European speleo...
Marine Isotope Stage 3 (MIS 3, 57–27 ka) was characterised by numerous rapid climate oscillations (i...
A precisely dated speleothem isotope record from the Sieben Hengste cave system, Switzerland, reveal...
We present a new high resolution speleothem stable isotope record from the Villars Cave (SW-France) ...
The Vil-car-1 flowstone core from Villars cave (SW France) provides one of the first European speleo...
Hermannshöhle is a show cave located near Kirchberg/Wechsel in Lower Austria. Together with three ne...
Holocene climate in Central Europe was characterized by variations on millennial to decadal time sca...
We present stable carbon (δ13C) and oxygen (δ18O) isotope records from two partially coeval speleoth...
Western Europe is the region with the highest density of published speleothem δ18O (δ18Ospel) record...
We present stable carbon (δ13C) and oxygen (δ18O) isotope records from two partially coeval speleoth...
The dataset includes speleothem carbon isotopes, oxygen isotopes, U-Th ages, and fluid inlcusion hyd...
The oxygen isotopic composition of calcite speleothems (stalagmites, etc.) can be used as a record o...
Western Europe is the region with the highest density of published speleothem δ18O (δ18Ospel) record...
High-precision TIMS U-series dates and continuous stable oxygen and carbon isotope profiles of a 400...
The climatic controls on the stable carbon isotopic composition (δ13C) of speleothem carbonate are l...
The Vil-car-1 flowstone core from Villars cave (SW France) provides one of the first European speleo...
Marine Isotope Stage 3 (MIS 3, 57–27 ka) was characterised by numerous rapid climate oscillations (i...