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- W2209526979 abstract "Paleosols—soils formed in the landscapes of the past, different from the modern ones—constitute an interesting and important object of soil research in Mexico. Buried paleosols of different age are very frequent and could provide an insight in the climate and ecosystem history. They are supposed but yet not investigated in the Pre-Quaternary continental geological strata. Younger paleosols are studied in the Quaternary volcanic sequences, demonstrating evidences of soil evolution under persistent climatic conditions as well as signals of climatic change. In the alluvial sequences, paleosols are frequently associated with paleontological and archeological materials producing combined records. Paleosols frequently occur on the modern land surface being a relict element within the present day soil mantle. Red soils of the karstic geosystems of Yucatan and arid regions of Sonora as well as tepetate (hardened volcanic horizons) of Central Mexico are relict soil bodies." @default.
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- W2209526979 date "2013-01-01" @default.
- W2209526979 modified "2023-10-14" @default.
- W2209526979 title "Paleosols of Mexico: Origin, Paleoecological Significance, Role in the Actual Soil Mantle" @default.
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- W2209526979 doi "https://doi.org/10.1007/978-94-007-5660-1_8" @default.
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