When Milankovitch cycles are preserved in the geologic record they provide a direct link
between chronometer and climate change, and thus a remarkable opportunity to constrain …

Abstract The Pliocene Epoch (∼ 5.3–2.6 million years ago, Ma) was characterized by a
warmer than present climate with smaller Northern Hemisphere ice sheets, and offers an …

Abstract The Mid‐Pleistocene Transition (MPT), where the Pleistocene glacial cycles
changed from 41 to∼ 100 kyr periodicity, is one of the most intriguing unsolved issues in the …

A range of future climate scenarios are projected for high atmospheric CO 2 concentrations,
given uncertainties over future human actions as well as potential environmental and …

Abstract The Indian Ocean provides a source of salt for North Atlantic deep-water convection
sites, via the Agulhas Leakage, and may thus drive changes in the ocean's overturning …

Chronological uncertainty is a hallmark of the paleoenvironmental sciences and
geosciences. While many tools have been made available to researchers to quantify age …

We present a Python package geared toward the intuitive analysis and visualization of
paleoclimate timeseries, Pyleoclim. The code is open‐source, object‐oriented, and built …

The dominant feature of large-scale mass transfer in the modern ocean is the Atlantic
meridional overturning circulation (AMOC). The geometry and vigour of this circulation …

Geologic intervals of sustained warmth such as the mid-Pliocene Warm Period can inform
our understanding of future climate change, including the long-term consequences of …

Much of our understanding of Cenozoic climate is based on the record of δ18O measured in
benthic foraminifera. However, this measurement reflects a combined signal of global …