Abstract The Eocene-Oligocene transition (EOT) at∼ 34 Ma marked a significant global
cooling on Earth when the ice cover in the Antarctic was formed. How the regional …

The arid interior of Asia is the largest source of dust deposited in the North Pacific Ocean,
and some dust is even transported to Greenland. Investigating the provenance history of …

The dating of continuous Eocene sediments in the Fushun Basin, NE China, provides a
good opportunity to study the evolution of the land paleoclimate during extreme high …

Evaporites are of great significance because they provide crucial information on
paleoclimate and hydrochemistry. This paper presents a depositional system comprising a …

A detailed uplift history of the Tibetan Plateau is essential for disentangling the proposed
geodynamical models and assessing its impacts on climate and biodiversity. However …

Reactive transport modeling (RTM) is an emerging method used to address geological
issues in diagenesis research. However, the extrapolation of RTM results to practical …

An integrated multiproxy dataset involving both mineralogical and geochemical
investigations of the northern Tibetan Plateau helps in assessing regional weathering …

A thorough understanding of sub-decadal paleoclimate variability typically depends on ultra-
precise geochronological constraints that are rarely obtained. While the seasonally resolved …

Abstract The Qaidam Basin in the northeastern part of the Tibetan Plateau preserves a
continuous and thick Cenozoic sedimentary succession, which is of great significance to …

In this paper, we present organic carbon isotope records from continental sediments
spanning the late Paleocene-middle Miocene (57.9–15.0 Ma) in the Lanzhou Basin …