Paleosols are ancient soils that have been incorporated into the geological record. Soils
form in response to interactions among the lithosphere, hydrosphere, biosphere, and …

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 …

Paleosol carbonate-based estimates of paleo-atmospheric CO2 play a prominent role in
constraining radiative-forcing and climate sensitivity in the deep-time. Large uncertainty in …

The mid-Paleozoic colonization of land by plants induced profound changes in the Earth's
surface environments. However, it remains poorly understood how the earliest vascular …

The present work deals with Jurassic deposits belonging to the External Rif chain. It is well
known that the Jurassic time was a crucial period in the earth's history as witness of …

Soils form as a product of physical, chemical, and biological activity at the outermost veneer
of Earth's surface. Once buried and incorporated into the sedimentary record, these soils …

Paleosols (fossil soils) are abundant in the sedimentary record and reflect, at least in part,
regional paleoclimate. Paleopedology thus offers a great potential for elucidating high …

Abstract Paleosols of the Paganzo Group preserve a shift from the cool climate of the
glaciated high-latitudes of Gondwana to a long-term aridification punctuated by shorter-term …

Large igneous provinces (LIPs) have been temporally correlated to mass extinctions
throughout the Phanerozoic, including the emplacement of the Deccan Volcanic Province …

Abstract The Middle Jurassic is characterized by major plate tectonic changes, variable
atmospheric CO 2 concentrations (pCO 2), and climate oscillations in both marine and …