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Ice age extinction : cause and human consequences / Jim Snook.

By: Material type: TextTextPublication details: New York : Algora Pub., ©2008.Description: 1 online resource (xiv, 191 pages) : illustrations, mapsContent type:
  • text
Media type:
  • computer
Carrier type:
  • online resource
ISBN:
  • 9780875865591
  • 0875865593
  • 1281398373
  • 9781281398376
  • 9786611398378
  • 6611398376
Subject(s): Genre/Form: Additional physical formats: Print version:: Ice age extinction.DDC classification:
  • 576.8/4 22
LOC classification:
  • QE721.2.E97 S66 2008eb
Online resources:
Contents:
Introduction -- Transitions relating to extinction -- Extinction -- How the glacial cycle works -- Ocean changes relating to glaciation and extinction -- Changes in the atmosphere during the last extinction -- Glacial changes to the land affecting life -- Changes in plants leading to extinction -- Large animal extinction associated with glacial melting -- The human condition during extinction -- First big increase in atmospheric carbon dioxide and population -- Current big increase in atmospheric carbon dioxide and population -- The way we are and where we are heading -- The future.
Action note:
  • digitized 2010 HathiTrust Digital Library committed to preserve
Summary: The author explores the causes of Earth's cyclical temperature changes and shows how those temperature shifts touch off a chain of events in the atmosphere, in the oceans and on land. Cold temperature was the trigger; and the resultant reduction in carbon dioxide, he argues, was the bullet that killed off so many species. The re-warming released more carbon dioxide into the atmosphere and fueled a resurgence. This book provides significant long term background information to put global warming into perspective. In addition, the author describes the human responses to increases in atmospheric carbon dioxide after the last ice age and in the last 150 years. Near the end of the last ice age, atmospheric carbon dioxide was about half of what it is today. Due to the lack of carbon dioxide, most of the vegetation disappeared from the middle and high latitudes. Without plants to eat, many large animals became extinct; North America lost three-fourths of its large animals including the woolly mammoth, mastodon and saber tooth cat. Humans, too, had little to eat in these areas and their population declined dramatically. The book then explains how and why atmospheric carbon dioxide increased by about 50% after the last ice age ended, encouraging a population explosion among plants, animals and humans, all of which then migrated into many previously barren areas. More recently, the 28% increase in atmospheric carbon dioxide in the last 150 years has caused a six-fold increase in the human population. Changes in the next 300 years will reverse some of the current trends. This book has value for anyone interested in the ice age extinction; glaciers; the glacial cycle; the atmosphere and oceans and the past and future of plants, animals and humans. It provides long-term information on atmospheric carbon dioxide, global warming and cooling.
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Includes bibliographical references (pages 175-178) and indexes.

Print version record.

Introduction -- Transitions relating to extinction -- Extinction -- How the glacial cycle works -- Ocean changes relating to glaciation and extinction -- Changes in the atmosphere during the last extinction -- Glacial changes to the land affecting life -- Changes in plants leading to extinction -- Large animal extinction associated with glacial melting -- The human condition during extinction -- First big increase in atmospheric carbon dioxide and population -- Current big increase in atmospheric carbon dioxide and population -- The way we are and where we are heading -- The future.

Use copy Restrictions unspecified star MiAaHDL

Electronic reproduction. [Place of publication not identified] : HathiTrust Digital Library, 2010. MiAaHDL

Master and use copy. Digital master created according to Benchmark for Faithful Digital Reproductions of Monographs and Serials, Version 1. Digital Library Federation, December 2002. MiAaHDL

http://purl.oclc.org/DLF/benchrepro0212

digitized 2010 HathiTrust Digital Library committed to preserve pda MiAaHDL

The author explores the causes of Earth's cyclical temperature changes and shows how those temperature shifts touch off a chain of events in the atmosphere, in the oceans and on land. Cold temperature was the trigger; and the resultant reduction in carbon dioxide, he argues, was the bullet that killed off so many species. The re-warming released more carbon dioxide into the atmosphere and fueled a resurgence. This book provides significant long term background information to put global warming into perspective. In addition, the author describes the human responses to increases in atmospheric carbon dioxide after the last ice age and in the last 150 years. Near the end of the last ice age, atmospheric carbon dioxide was about half of what it is today. Due to the lack of carbon dioxide, most of the vegetation disappeared from the middle and high latitudes. Without plants to eat, many large animals became extinct; North America lost three-fourths of its large animals including the woolly mammoth, mastodon and saber tooth cat. Humans, too, had little to eat in these areas and their population declined dramatically. The book then explains how and why atmospheric carbon dioxide increased by about 50% after the last ice age ended, encouraging a population explosion among plants, animals and humans, all of which then migrated into many previously barren areas. More recently, the 28% increase in atmospheric carbon dioxide in the last 150 years has caused a six-fold increase in the human population. Changes in the next 300 years will reverse some of the current trends. This book has value for anyone interested in the ice age extinction; glaciers; the glacial cycle; the atmosphere and oceans and the past and future of plants, animals and humans. It provides long-term information on atmospheric carbon dioxide, global warming and cooling.

English.

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