Reconstructions of Earth's past climate strongly influence our understanding of the dynamics
and sensitivity of the climate system. Yet global temperature has been reconstructed for only …

This paper addresses two fundamental issues in cyclostratigraphy and paleoclimatology:
identification of astronomical forcing in sequences of stratigraphic cycles, and accurate …

After more than a century of doubt and equivocation, cyclostratigraphy–the stratigraphic
record of astronomically forced paleoclimatic change–has come to be widely accepted in the …

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 …

Because interpretations of paleoclimate records from ocean sediment cores rely on age
models to estimate age as a function of core depth, age model uncertainty can affect the …

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 …

We present a 5-Myr probabilistic stack, which we name the Prob-stack. It is constructed from
180 globally distributed benthic δ18O records using a profile hidden Markov model (HMM) …

Quantifying variability in, and identifying the mechanisms behind, East Asian dust production
and transport across the last several million years is essential for constraining future dust …