Soils of the Past [electronic resource] : An introduction to paleopedology / by Gregory J. Retallack.
Erişim Adresi
ISBN
9789401179027
Dil Kodu
İngilizce
Yer Numarası
DK/9296
Yazar
Basım Bildirimi
1st ed. 1990.
Yayın Bilgisi
Dordrecht : Springer Netherlands : Imprint: Springer, 1990.
Fiziksel Niteleme
XVIII, 520 p. online resource.
İçindekiler Notu
One: Soils and Paleosols -- 1 Paleopedology -- 2 Soils on and under the landscape -- 3 Features of fossil soils -- 4 Soil-forming processes -- 5 Soil classification -- 6 Mapping and naming paleosols -- 7 Alteration of paleosols after burial -- Two: Factors in Soil Formation -- 8 Models of soil formation -- 9 Climate -- 10 Organisms -- 11 Topographic relief as a factor -- 12 Parent material as a factor -- 13 Time as a factor -- Three: Fossil Record of Soils -- 14 A long-term natural experiment in pedogenesis -- 15 Soils of other worlds -- 16 Earth’s earliest landscapes -- 17 Early life on land -- 18 Large plants and animals on land -- 19 Afforestation of the land -- 20 Grasses in dry continental interiors -- 21 Human impact on landscapes -- References.
Özet, vb.
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. This book has evolved primarily as a text for senior level university courses in paleopedology: the study of fossil soils.
Konu
Social sciences.
Humanities.
Humanities and Social Sciences.
Humanities.
Humanities and Social Sciences.
Kurum Adı
Eseri Alıntıla
Referansları kullanmadan önce gözden geçirmeniz ve varsa gerekli düzeltmeleri yapmanız önerilir.
Dijital Kaynak
MARC Görünümü
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520 |aLandscapes 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. This book has evolved primarily as a text for senior level university courses in paleopedology: the study of fossil soils.
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532 8 |aInaccessible, or known limited accessibility
532 8 |aNo reading system accessibility options actively disabled
532 8 |aPublisher contact for further accessibility information: accessibilitysupport@springernature.com
650 0|aSocial sciences.
650 0|aHumanities.
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100 1 |aRetallack, Gregory J.|eauthor.|4aut|4http://id.loc.gov/vocabulary/relators/aut
245 10|aSoils of the Past|h[electronic resource] :|bAn introduction to paleopedology /|cby Gregory J. Retallack.
250 |a1st ed. 1990.
264 1|aDordrecht :|bSpringer Netherlands :|bImprint: Springer,|c1990.
300 |aXVIII, 520 p.|bonline resource.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
347 |atext file|bPDF|2rda
505 0 |aOne: Soils and Paleosols -- 1 Paleopedology -- 2 Soils on and under the landscape -- 3 Features of fossil soils -- 4 Soil-forming processes -- 5 Soil classification -- 6 Mapping and naming paleosols -- 7 Alteration of paleosols after burial -- Two: Factors in Soil Formation -- 8 Models of soil formation -- 9 Climate -- 10 Organisms -- 11 Topographic relief as a factor -- 12 Parent material as a factor -- 13 Time as a factor -- Three: Fossil Record of Soils -- 14 A long-term natural experiment in pedogenesis -- 15 Soils of other worlds -- 16 Earth’s earliest landscapes -- 17 Early life on land -- 18 Large plants and animals on land -- 19 Afforestation of the land -- 20 Grasses in dry continental interiors -- 21 Human impact on landscapes -- References.
520 |aLandscapes 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. This book has evolved primarily as a text for senior level university courses in paleopedology: the study of fossil soils.
532 8 |aAccessibility summary: This PDF is not accessible. It is based on scanned pages and does not support features such as screen reader compatibility or described non-text content (images, graphs etc). However, it likely supports searchable and selectable text based on OCR (Optical Character Recognition). Users with accessibility needs may not be able to use this content effectively. Please contact us at accessibilitysupport@springernature.com if you require assistance or an alternative format.
532 8 |aInaccessible, or known limited accessibility
532 8 |aNo reading system accessibility options actively disabled
532 8 |aPublisher contact for further accessibility information: accessibilitysupport@springernature.com
650 0|aSocial sciences.
650 0|aHumanities.
650 14|aHumanities and Social Sciences.
710 2 |aSpringerLink (Online service)
773 0 |tSpringer Nature eBook
776 08|iPrinted edition:|z9780044457572
776 08|iPrinted edition:|z9789401179034
856 40|uhttps://doi.org/10.1007/978-94-011-7902-7
912 |aZDB-2-SHU
912 |aZDB-2-SXH
912 |aZDB-2-BAE
950 |aHumanities, Social Sciences and Law (SpringerNature-11648)
950 |aHistory (R0) (SpringerNature-43722)
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