We review and synthesize the geologic record that constrains the sources of sea level rise
and freshwater discharge to the global oceans associated with retreat of ice sheets during …

Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …

A comprehensive database of paleoclimate records is needed to place recent warming into
the longer-term context of natural climate variability. We present a global compilation of …

Reproducible climate reconstructions of the Common Era (1 CE to present) are key to
placing industrial-era warming into the context of natural climatic variability. Here we present …

X‐ray fluorescence (XRF) core scanning and X‐ray computed tomography data were
measured every 1 mm to study the structure of Heinrich Event 1 during the last deglaciation …

The demise of the Laurentide ice sheet during the early Holocene epoch is the most recent
and best constrained disappearance of a large ice sheet in the Northern Hemisphere, and …

In this study we review a global set of alkenone-and foraminiferal Mg/Ca-derived sea
surface temperatures (SST) records from the Holocene and compare them with a suite of …

An outstanding climate anomaly 8200 years before the present (BP) in the North Atlantic is
commonly postulated to be the result of weakened overturning circulation triggered by a …

A period of cooling about 13,000 years ago interrupted about 2,000 years of deglacial
warming. Known as the Younger Dryas (YD), the event is thought to have resulted from a …

Abstract The Mg/Ca ratio of planktic foraminifera is a widely used proxy for sea‐surface
temperature but is also sensitive to other environmental factors. Previous work has relied on …