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Sediments (Geology) --- Weathering --- Congresses.
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'The Great Ice Age' documents and explains the natural climatic and palaeoecologic changes that have occurred during the past 2.6 million years, outlining the emergence and global impact of our species during this period. Exploring a wide rage of records of climate change, the authors demonstrated the interconnectivity of the components of the Earth's climate system, show how the evidence for such change is obtained, and explain some of the problems in collection and dating proxy climate data.
Climatic changes. --- Glacial epoch. --- Nature --- Paleoecology --- Effect of human beings on. --- 551.336 --- 581.54 --- Ice age --- Climatic conditions. Seasons. Cosmic factors in plant ecology. Phenology --- 581.54 Climatic conditions. Seasons. Cosmic factors in plant ecology. Phenology --- Climatic changes --- Glacial epoch --- 551.583 --- 572.1/.4 --- 551.583 Variations of climate. Climatic change --- Variations of climate. Climatic change --- 572.1/.4 Anthropogeny. Human development in general. Origin of the human species --- Anthropogeny. Human development in general. Origin of the human species --- Quaternary Period --- Anthropogenic effects on nature --- Ecological footprint --- Human beings --- Anthropogenic soils --- Human ecology --- Ice Age --- Geology, Stratigraphic --- Changes, Climatic --- Climate change --- Climate changes --- Climate variations --- Climatic change --- Climatic fluctuations --- Climatic variations --- Global climate changes --- Global climatic changes --- Climatology --- Climate change mitigation --- Teleconnections (Climatology) --- Effect of human beings on --- Environmental aspects --- Climat --- Epoque glaciaire --- Paléoécologie --- Homme --- Changements --- Influence sur la nature --- Changes in climate --- Climate change science --- Global environmental change --- Paleoecology - Quaternary --- Nature - Effect of human beings on
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SCIENCES DE LA TERRE --- GENERALITES --- GENERALITES --- SCIENCES DE LA TERRE --- GENERALITES --- GENERALITES
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