Results 161 to 170 of about 3,446 (227)
Neanderthal coasteering and the first Portuguese hominin tracksites. [PDF]
Sci Repde Carvalho CN +16 more
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Characteristics and paleoclimate significance of authigenic ferrimagnetic minerals in the Xuancheng red earth, southern China. [PDF]
Sci RepZhang D +11 more
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Hydro-mechanical behavior of unsaturated intact paleosol and intact loess
Engineering Geology, 2023 Many geo-hazards occurred in regions incorporating loess-paleosol sequences. Understanding the hydro-mechanical behavior of unsaturated intact paleosol and intact loess is a prerequisite to address these geo-hazards.
Zhao Lu, Limin Zhang
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Quaternary International, 2018 The paleosol unit S5S1, which corresponds to Marine Isotope Stage (MIS) 13, is the most prominent paleosol layer in the central Chinese Loess Plateau (CLP). S5S1 has extremely high magnetic susceptibility, but it remains uncertain whether this is related
Jia Jia, Youjun Wang, Qiuzhen Yin
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Water (Switzerland), 2020 To determine the permeability characteristics and the groundwater enrichment conditions of loess and paleosol layers, this article systematically investigated the permeability, magnetic susceptibility, porosity, and carbonate mass percentage of ...
Tianjie Shao, Jingbo Zhao, Junjie Niu
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2021
This article reviews the nature of modern and ancient soils. Soils are naturally occurring bodies that mantle most of the land surface of the Earth. They are found on virtually every part of the Earth’s land surface, other than areas covered by water bodies (lakes and rivers), glacial ice, or steep slopes in mountainous terrain.
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This article reviews the nature of modern and ancient soils. Soils are naturally occurring bodies that mantle most of the land surface of the Earth. They are found on virtually every part of the Earth’s land surface, other than areas covered by water bodies (lakes and rivers), glacial ice, or steep slopes in mountainous terrain.
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Geological Society of America Bulletin, 1993
Despite increased interest in paleosols during the past decade, no satisfactory classification is in current use. Presented here is a largely descriptive classification system that utilizes those pedogenic features that have the highest preservation potential in the rock record.
GREG H. MACK +2 more
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Despite increased interest in paleosols during the past decade, no satisfactory classification is in current use. Presented here is a largely descriptive classification system that utilizes those pedogenic features that have the highest preservation potential in the rock record.
GREG H. MACK +2 more
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Geological Society of America Bulletin, 1961
Sayles recognized five buried soils that stratigraphically separate eolianites and interbedded marine limestones in Bermuda. He considered that the paleosols represent interglacial ages or interstadials. Some soils were considered residual, and some accretionary.
R. V. RUHE, J. G. CADY, R. S. GOMEZ
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Sayles recognized five buried soils that stratigraphically separate eolianites and interbedded marine limestones in Bermuda. He considered that the paleosols represent interglacial ages or interstadials. Some soils were considered residual, and some accretionary.
R. V. RUHE, J. G. CADY, R. S. GOMEZ
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Classification of paleosols — A comment
Quaternary International, 1998Abstract The paper ‘Classification of Paleosols’ by Mack et al. (1993, hereafter called ‘the authors’), read from a soil scientist's scope, evokes considerable criticism, some of which follows below.
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Paleosols and pedostratigraphy
Applied Soil Ecology, 2018Abstract Paleopedology and pedostratigraphy are devoted to the use of buried and relict soils in interpreting the record of environmental conditions that are different from the current ones. As such, paleosols may be used in models that aim at predicting future earth system reactions to changing environmental conditions.
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