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Indicators of Pedogenic Processes in Red Clayey Soils of the Cape Martyan Reserve, South Crimea
AbstractSpecific red clayey soils on the eluvium of limestone, which are traditionally associated with Mediterranean terra rossa, have been...
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Response of grain-size components of loess-paleosol sequence to Quaternary climate in the Southern Loess Plateau, China
A new, thick, and complete loess-paleosol sequence is a good response to climate changes. In this paper, the distribution and parameters of grain...
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Sedimentation Rate of the Floodplain Alluvium in the Center of European Russia According to the Study of Buried Soil Series
AbstractThe deposition rate of the floodplain alluvium in various periods of the Holocene is determined for the Istra, Oka, and Seim rivers using a...
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Soil selenium transformation across different parent materials in Pothwar uplands of Pakistan
Selenium (Se) is an essential trace element for humans but non-essential for plants. Selenium bioavailability depends on selenium forms in soil....
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Mineralogy and Magnetic Properties of the Loess-Soil Formation as the Reflection of the Landscape and Climatic Conditions in the Terek–Kuma Lowland in the Pleistocene
AbstractA detailed mineralogical and geochemical study of the Otkaznoe reference section, representing a loess–soil complex confined to the...
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Soils and Sediments of the Lacustrine-Alas Depressions in Tundra Zone of the Kolyma Lowland
Abstract—Pedogenesis on the terraces of lacustrine–alas depressions in the tundra zone of the Kolyma Lowland takes place on sediments that are...
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Pedochronosequences of Medieval Burial Mounds, Pskov Oblast
AbstractThe soils buried under the early medieval mounds of the 9th and early 11th centuries AD were studied. The reconstruction of environmental...
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Environmental Magnetic Properties of Lateritic Soils from Southwestern India
AbstractSoil formation is influenced mainly by lithology, climate, organic matter, vegetation, topography, and time. Soil-forming processes have been...
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Soil Formation on Loamy Deposits in Technogenic Landscapes of the Taiga Zone in the Northeast of the European Part of Russia
AbstractThe formation of soils on loamy deposits during the primary succession of vegetation after biological reclamation of a technogenically...
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Weathering and paleoprecipitation indices in a Late Pleistocene–Holocene loess–paleosol sequence in central Argentina
A Late Pleistocene–Holocene loess–paleosol sequence in central Argentina was studied to obtain a weathering insight and to probe geochemical tools as...
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Holocene dust dynamics archives in archaeological ruins in arid and semi-arid environments in the Southern Levant
Ruins of archaeological structures, mainly dating to the Bronze Age till Byzantine period, were investigated in a case study in the Petra region in...
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Paleosols in an outcrop of red beds from the Upper Cretaceous Yaojia Formation, southern Songliao Basin, Jilin Province, NE China
Paleosols in an outcrop of fluvial–lacustrine red beds have been recognized in the Upper Cretaceous Yaojia Formation in southern Songliao Basin,...
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A site formation history of Obishir-5, the earliest Neolithic site in the Fergana Valley (Kyrgyzstan)
Obsihir-5 holds some of the earliest evidence for the utilization of livestock in the mountainous regions of Central Asia. However, direct evidence...
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Soil and Ecological Features of the Neo-Eneolithic Algai Settlement in the Lower Volga Region
AbstractThe results of the study of the Algai archeological site in the Lower Volga region (Aleksandrov-Gai district, Saratov oblast) are presented....
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A Paleosol on a Pre-Cambrian Ferruginous Quartzite Weathering Crust (Stary Oskol, Belgorod Region, Russia)
AbstractThis study describes the results of a detailed study (morphology, XRD, Mössbauer and FTIR- spectroscopies, SEM-EDS) of paleosol (PS)...
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Influence of faults on alteration, mineralogy, and geotechnical behavior of granitic residual soils
Contact metamorphism and metasomatism are imposed on granitic rocks by late intrusions. This study shows the consequences of this phenomenon on the...
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