Here we present an overview of speleothem δ18O records from South America, most of
which are available in the Speleothem Isotopes Synthesis and Analysis (SISAL_v1) …

Due to the many factors controlling δ 13 C values in stalagmites, complicating their
paleoclimatic and paleoenvironmental interpretation, most studies do not present δ 13 C …

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 …

Speleothems can provide high-quality continuous records of the direction and relative
paleointensity of the geomagnetic field, combining high precision dating (with U-Th method) …

Disentangling the effects of climate and human impact on the long-term evolution of the
Earth Critical Zone is crucial to understand the array of its potential responses to the ongoing …

Commonly used speleothem-based paleoclimate proxies such as δ 18 O, δ 13 C, and trace
element ratios are capable of high temporal resolution, but their interpretations are often …

The diminishing strength of the Earth's magnetic dipole over recent millennia is
accompanied by the increasing prominence of the geomagnetic South Atlantic Anomaly …

Considerable ambiguity remains over the triggers for the abrupt climate deterioration that
terminated the Last Interglacial Marine Isotope Stage 5e (MIS5e) period. A prevailing …

This study demonstrates the feasibility of speleothem magnetism as a paleo-hydrology proxy
in speleothems growing in semi-arid conditions. Soil-derived magnetic particles in …

The study presents three sedimentary profiles from Tarimba cave in central Brazil. The data
allow constraining the late Quaternary sedimentary evolution of cave systems in the region …