G. Moseley

Climatic transitions across Marine Isotope Stage 10–12 in the Alps evidenced by subglacial speleothems

Late Pleistocene climate in the European Alps was marked by large, orbitally driven fluctuations in temperature, precipitation, and ice extent. Reconstructing mountain glaciation prior to the Last Glacial Maximum remains challenging, however, because glacial deposits are often eroded or reworked. Here we present a...