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Titlebook: Soils of the Past; An introduction to p Gregory J. Retallack Book 1990 Gregory J. Retallack 1990 Pedogenesis.Sediment.science.soil.soil sci

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书目名称Soils of the Past
副标题An introduction to p
编辑Gregory J. Retallack
视频video
图书封面Titlebook: Soils of the Past; An introduction to p Gregory J. Retallack Book 1990 Gregory J. Retallack 1990 Pedogenesis.Sediment.science.soil.soil sci
描述Landscapes viewed from afar have a timeless quality that is soothing to the human spirit. Yet a tranquil wilderness scene is but a snapshot in the steady stream of surficial change. Wind, water and human activities reshape the landscape by means of gradual to catastrophic and usually irreversible events. Much of this change destroys past landscapes, but at some times and places, landscapes are buried in the rock record. This work is dedicated to the discovery of past landscapes and their life through the fossil record of soils. A long history of surficial changes extending back almost to the origin of our planet can be deciphered from the study of these buried soils, or paleosols. Some rudiments of this history, and our place in it, are outlined in a final section of this book. But first it is necessary to learn something of the language of soils, of what happens to them when buried in the rock record and which of the forces of nature can be confidently reconstructed from their remains. Much of this preliminary material is borrowed from soil science, but throughout emphasis is laid on features that provide most reliable evidence of landscapes during the distant geological past. Thi
出版日期Book 1990
关键词Pedogenesis; Sediment; science; soil; soil science
版次1
doihttps://doi.org/10.1007/978-94-011-7902-7
isbn_softcover978-0-04-445757-2
isbn_ebook978-94-011-7902-7
copyrightGregory J. Retallack 1990
The information of publication is updating

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Paleopedologyhin sedimentary sequences or persisting under changed surface conditions, are the main subject matter of paleopedology. In this book, it is seen as an historical perspective on soil genesis and as a way of reconstructing the geological history of land surfaces on Earth. Soils, like organisms, sedime
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Features of fossil soilsript first impressions, paleosols do have distinctive features. For the most part these are characteristics also found in modern soils, yet many paleosols are no longer loose, cracked, and at the land surface. Important differences result from compaction and alteration upon burial which change many
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Soil-forming processesodern soils than in paleosols in which they ceased to act long ago. Nevertheless, processes often can be inferred from features of paleosols or from suites of paleosols. The reconstruction of processes gives meaning and connection to features and kinds of paleosols. One way to learn about soils is t
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Alteration of paleosols after burialsed in studies of sedimentary petrology to describe alteration after deposition. Diagenesis thus includes soil formation, which on Earth occurs at 1 bar pressure and temperatures from 84 to –88°C (Kimmins 1987). Additional changes after burial pass into what would be called metamorphic alteration at
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