The formation of carbonate sediments in continental environments is subject to numerous
environmental controls, of which climate is one of the foremost. Consequently, calcareous …

The mechanisms driving the Dansgaard-Oeschger (DO) cycles remain uncertain, but
promising hypotheses could explain it, and a comprehensive assessment of its impact is …

Many regions of the world experienced abrupt climate variability during the last glacial
period (75–15 thousand years ago,). These changes probably arose from interactions …

From 2012 to 2016, California experienced one of the worst droughts since the start of
observational records. As in previous dry periods, precipitation-inducing winter storms were …

In order to construct a stacked climatic record of millennial‐scale variability for northern
China, grain size was measured for 12,330 samples from eight thick loess sections …

Speleothems are capable of providing information on the response of middle and low-
latitude terrestrial environments to global climate change during the Pleistocene and …

Speleothem oxygen isotope (δ 18 O) records provide key insight into the rate and timing of
terrestrial paleoclimate changes during the late Quaternary. However, it can be difficult to …

Dramatic hydroclimate shifts occurred in western North America during the last deglaciation,
but the timing and mechanisms driving these changes are uncertain and debated, and …

Although quantitative isotopic data from speleothems has been used to evaluate isotope-
enabled model simulations, currently no consensus exists regarding the most appropriate …

Widespread late Pleistocene lake systems of the Basin and Range Province indicate
substantially greater moisture availability during glacial periods relative to modern times, but …