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 fundamental issue in the interpretation of speleothem calcite δ 18 O cc records is the
correct partitioning of the effects of temperature and water δ 18 O variations. This study …

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 …

During glacial terminations, massive iceberg discharges and meltwater pulses in the North
Atlantic triggered a shutdown of the Atlantic Meridional Overturning Circulation (AMOC) …

Stable isotope records from speleothems provide information on past climate changes, most
particularly information that can be used to reconstruct past changes in precipitation and …

Understanding supra-regional climate variability such as the changes in the North Atlantic
realm is important to identify the drivers of the climate system. In this study maar lake …

In recent decades speleothems have become valuable climate archives and are of crucial
importance for the investigation of past climate conditions. Albeit much progress has been …

This study presents the reconstructed evolution of sea surface conditions in the central-
western Mediterranean Sea during the late Holocene (2700 years) from a set of multi-proxy …

Western Europe is the region with the highest density of published speleothem δ18O
(δ18Ospel) records worldwide. Here, we review these records in light of the recent …

Due to the scarcity of reliable and highly resolved moisture proxies covering much of the
Holocene, there has been increased interest in the study of living and subfossil peatland …