Environmental change
著者
書誌事項
Environmental change
（Contemporary problems in geography）
Clarendon Press , Oxford University Press, 1983
2nd ed
- : pbk
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注記
Bibliography: p. [231]-254
Includes index
内容説明・目次
- 巻冊次
-
ISBN 9780198741329
内容説明
"Global Environments through the Quaternary delves into the environmental changes that have taken place during the Quaternary: the two to three million years during which man has inhabited the Earth. Taking the reader through the Pleistocene and the Holocene, the book describes the evidence that has helped us to characterize environmental changes during these two epochs. It then explores the changes captured by more recent meteorological records in the period up to the present day. Current climate change research foretells of potentially catastrophic sea-level changes in the future; chapter seven examines sea-level changes throughout the Quaternary, putting current concerns into perspective. The book closes with a look at the environmental basis of climate change - and the impact of human activity upon it."--BOOK JACKET.
- 巻冊次
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: pbk ISBN 9780198741350
内容説明
This book examines the environmental changes of the last three million years. It is a concise, modern survey which details the developments in the study of environmental change. There is a wide geographical coverage, using a minimum of technical language, so that it is accessible to non-geomorphologists and non-geologists. Traditional and recent techniques for the study of the Pleistocene are described and then the chronology, nature, and effects of the major events are outlined. This is followed by a discussion of the Holocene and a detailed analysis of changes during the period of meteorological observations. The book ends with sections on sea-level changes and the causes of climatic change. This new edition has been extensively rewritten. The references and guides to reading have been up-dated and many new figures included. Additional information is provided on new techniques for environmental reconstruction, on climatic sequences preserved in ocean sediments and loess, on sea-level curves, and on the causes of climatic change.
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