Paleoclimatic Significance of Cave Ice

Author:

Perșoiu Aurel

Publisher

Elsevier

Reference39 articles.

1. The exchange of hydrogen isotopes between ice and water in temperate glaciers;Arnason;Earth Planet. Sci. Lett.,1969

2. Oxygen and carbon stable isotopes in cryogenic cave calcite (CCC)—possible proxy for past climate changes;Bădăluță,2017

3. Is the climate signal adequately recorded in the δ18O isotope composition from ice cave deposits? Climate variations during the little ice age and the industrial era inferred from Pyrenean ice deposits and stalagmites;Bartolomé,2017

4. Stable isotope and mineralogical investigations on clays from the Late Cretaceous sequences, Hateg Basin, Romania;Bojar;Appl. Clay Sci.,2009

5. Observed trends in the chemical composition, d18O and crystal sizes vs. depth in the first ice core from the LoLc 1650 “Abisso sul Margine dell’Alto Bregai” ice cave (Lecco, Italy);Citterio;Theor. Appl. Karstol.,2004

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