Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

Speleothems are primarily studied in order to generate archives of climatic change and
results have led to significant advances in identifying and dating major shifts in the climate …

The Milandre test site is a karst aquifer characterized by diffuse infiltration, a well developed
conduit network, and several tributaries feeding an underground river. Field data include …

Most proxy records used for reconstruction of Holocene climate of Amazonia are unable to
quantitatively distinguish between the effect of temperature and rainfall amounts. We present …

This study presents new stable isotope data for precipitation (δ 18 O p) and drip water (δ 18
O d) from eight cave sites in the monsoon regions of China (MRC), with monthly to bi …

One quarter of the world's population lives in karst terrains, yet karsts are highly vulnerable
to stresses caused by human activity. This book surveys human impact on karst water …

We analyze the interannual monthly variability of oxygen isotope ratios in data from IAEA
stations along the Atlantic coast of South America between 23° and 34° S to evaluate the …

Interest in speleothems (secondary cave carbonates such as stalagmites) as recorders of
continental palaeo–environments has increased markedly during the past decade, reflecting …

Oxygen isotope data for well dated Holocene speleothems from Europe have been
compiled for the first time. The data were analysed at 1ka time slices through the Holocene …

This article presents isotopic measurements (δ 18 O and δD) of precipitation and cave drip
water from two sites in southern France in order to investigate the link between rainfall and …