Paleoclimatic time series from Permian and Triassic paleosols reveal transient episodes of
unusually warm and wet conditions, interrupting long periods of cool and dry conditions …

It has been 10 years since publication of the first edition ofSoils of the Past. In that time the
subject of paleopedology hasgrown rapidly, and established itself within the mainstream …

Sandy braided dryland rivers, deposited under arid to semi-arid conditions, constitute
important clastic reservoirs worldwide whose reservoir quality reflects the effect of primary …

The ultimate driver of the end-Permian mass extinction is a topic of much debate. Here, we
used a multiproxy and paleoclimate modeling approach to establish a unifying theory …

Abstract The northern Madrid Basin contains paleosols and lacustrine sequences composed
of ordered dolomite. Smectite-rich mudstones with analcime deposited in distal alluvial fans …

This study aims to provide the depositional facies, sequence stratigraphic and paleoclimatic
characteristics of the Mid-Eocene (Bartonian) continental succession exposed at Gebel El …

Global tectonic and climatic models for the Permian-Triassic boundary (PTB) are highly
debated. One of the most disputed topics is the temperature increase associated with CO 2 …

The mid-Ludfordian Carbon Isotope Excursion (CIE) is one of the biggest perturbation in the
isotope and facies record in the Palaeozoic. However, its causes still remain unknown. In the …

The precipitation of primary dolomite in soil is rare and controversial, and its occurrence
indicates highly unusual geochemical and climatic conditions. We utilize isotopic and …

The sedimentology, petrography and mineralogy of the seemingly monotonous Late Triassic
Mercia Mudstone Group across the Severn Basin and Bristol Channel region reveals a …