The major cause of sea-level change during ice ages is the exchange of water between ice
and ocean and the planet's dynamic response to the changing surface load. Inversion of∼ …

The timing and cause of megafaunal extinctions are an enduring focus of research interest
and debate. Despite the developments in the analysis of coprophilous fungal spores (CFS) …

We present a novel method for joint inversion of receiver functions and surface wave
dispersion data, using a transdimensional Bayesian formulation. This class of algorithm …

Both bog surface wetness and atmospheric dust deposition are intricately linked to changes
in the hydrological cycle and pairing these types of records at the same site provides …

Non-linear inverse problems in the geosciences often involve probabilistic sampling of
multimodal density functions or global optimization and sometimes both. Efficient algorithmic …

A meaningful interpretation of seismic measurements requires a rigorous quantification of
the uncertainty. In an inverse problem, the data noise determines how accurately …

Seismologists construct images of the Earth's interior structure using observations, derived
from seismograms, collected at the surface. A common approach to such inverse problems …

The evolution of land plants during the Palaeozoic era transformed Earth's biosphere.
Because the Earth's surface and interior are linked by tectonic processes, the linked …

Receiver functions are a powerful tool to isolate and interpret receiver-side structure effects
in teleseismic seismic records. They are easily constructed by deconvolving one component …

Although archaeological research suggests that mining/metallurgy already started in the
Chalcolithic (3rd millennium BC), the earliest atmospheric metal pollution in SW Europe has …