Variations in speleothem oxygen-isotope values (δ18O) result from a complicated interplay
of environmental controls and processes in the ocean, atmosphere, soil zone, epikarst, and …

The role of seasonality is indisputable in climate and ecosystem dynamics. Seasonal
temperature and precipitation variability are of vital importance for the availability of food …

The climatic controls on the stable carbon isotopic composition (δ 13 C) of speleothem
carbonate are less often discussed in the scientific literature in contrast to the frequently …

Speleothems are now established as important palaeoenvironmental archives and contain a
number of suitable proxies, although trace elements have been much less widely used than …

The Mediterranean region contains a diverse and interesting climate ranging from areas
with permanent glaciers to areas of subtropical, semiarid regions. The region is potentially …

Understanding the relationships between speleothem stable isotopes (δ13C δ18O) and in
situ cave forcing mechanisms is important to interpreting ancient stalagmite paleoclimate …

Speleothems have become a cornerstone of the approach to better understanding Earth's
climatic teleconnections due to their precise absolute chronologies, their continuous or …

A review of 2000 years of paleoclimatic evidence in the Mediterranean - HAL-SHS -
Sciences de l'Homme et de la Société Accéder directement au contenu Documentation FR …

In general, the rate and timing of calcite precipitation is in part affected by variations in cave
air CO2 concentrations. Knowledge of cave ventilation processes is required to quantify the …

Speleothem oxygen isotopic (δ18O) records are used to reconstruct past hydroclimate yet
records from the same cave do not always replicate. We use a global database of …