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 …

A prominent, abrupt climate event about 8200 years ago brought generally cold and dry
conditions to broad northern-hemisphere regions especially in wintertime, in response to a …

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

The application of stable isotopes in speleothem records requires an understanding of the
extent to which speleothem calcite isotopic compositions reflect the compositions of the cave …

Evidence for climatic change across the North American Monsoon (NAM) and adjacent
areas is reviewed, drawing on continental and marine records and the application of climate …

A Holocene stalagmite from Botuverá Cave, southeastern Brazil was analyzed by LA-ICPMS
for Mg/Ca, Sr/Ca, Ba/Ca. The observed variability in the record was demonstrated to be …

Characterizing the temporal uncertainty in palaeoclimate records is crucial for analysing
past climate change, correlating climate events between records, assessing climate …

This paper is a review of cave sediments: their characteristics and their application as
paleoclimate archives. Cave sediments can be separated into two broad categories, clastic …

To improve our understanding of the mechanism behind the 8.2 kaBP cooling event, we
compare proxy evidence with climate model simulations in which the thermohaline ocean …

Paleoenvironmental data from a stalagmite from western Belize provide a 3300-year record
of droughts that impacted the Maya civilization at least four times across a span of 1500 …