Results 31 to 40 of about 3,414 (218)
The limited knowledge of Late Cretaceous terrestrial environments and their response to tectonic events in mid-latitudes can be addressed through continental basin deposits such as paleosols.
Luxing Dou, Changmin Zhang, Li Zhang
core +1 more source
Durations of paleosols within the Strelley Pool Formation.
Durations of paleosols within the Strelley Pool Formation.
Mark D. Schmitz (2843513) +1 more
core +1 more source
Durations of Jurta paleosols using various modern chronofunctions.
Durations of Jurta paleosols using various modern chronofunctions.
Mark D. Schmitz (2843513) +1 more
core +1 more source
Abstract Studies investigating paleopathologies in sauropods remain scarce despite their relative abundance in the fossil record. In this study we report new occurrence of paleopathological features, corresponding to a neoplasm found in a middle caudal vertebra (MCT.R.2120) of an advanced titanosaur from the Presidente Prudente Formation (Bauru Basin ...
Maria Luiza Peres Bertolossi +5 more
wiley +1 more source
Grain size of Archean paleosols from point counting (500 points).
Grain size of Archean paleosols from point counting (500 points).
Mark D. Schmitz (2843513) +1 more
core +1 more source
ABSTRACT The Aso‐3 tephra is one of the most significant widespread marker layers from the Middle to Late Pleistocene, generated by a large caldera‐forming eruption at the Aso volcano in Kyushu, southwestern Japan. Despite its importance, a distal co‐ignimbrite ash correlative has yet to be clearly identified, primarily because although volcanic glass ...
Toshinori Sasaki +6 more
wiley +1 more source
Chemical composition (wt %) of Archean paleosols by XRF.
Chemical composition (wt %) of Archean paleosols by XRF.
Mark D. Schmitz (2843513) +1 more
core +1 more source
Late Pleistocene to Holocene environmental changes from δ13C determinations in soils at Teotihuacan, Mexico [PDF]
Stable carbon isotopic signature (δ13C) of soil organic matter (SOM) is used as a high-spatial resolution tool to infer environmental changes during late Pleistocene to Present in the Teotihuacan valley, Mexico.
E. Vallejo Gómez +6 more
doaj
The studies of paleosoils buried beneath burial mounds of the Early, Middle, and Late Sarmatian time (4th c. BC to 4th c. AD) were carried out in the dry and desert steppes of the Lower Volga river area (the Volga and Yergenino uplands, the Caspian ...
Demkin Vitaliy A. +2 more
doaj +1 more source

