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Plants and Climate Change (Paperback, Softcover reprint of hardcover 1st ed. 2006): Jelte Rozema, Rien Aerts, Hans Cornelissen Plants and Climate Change (Paperback, Softcover reprint of hardcover 1st ed. 2006)
Jelte Rozema, Rien Aerts, Hans Cornelissen
R4,505 Discovery Miles 45 050 Ships in 10 - 15 working days

Plants and Climate Change focuses on how climate affects or affected the biosphere and vice versa both in the present and past. The chapters describe how ecosystems from the Antarctic and Arctic and from other latitudes respond to global climate change.

The papers highlight plant responses to atmospheric CO2 increase, to global warming and to increased ultraviolet-B radiation as a result of stratospheric ozone depletion.

Depending on how and how well plant responses to increased temperature, atmospheric CO2 and ultraviolet-B have been preserved in the (sub)-fossil record, past climates and past atmospheric chemistry may be reconstructed. Pollen and tree-ring data reflect plant species composition and variation of temperature and precipitation over long or shorter time intervals. In addition to well preserved morphological and chemical plant properties, new analytical techniques such as stable isotopes are becoming increasingly important in this respect. The development and validation of such biotic climate and environment proxies build a bridge between biological and geological research. This highlights that plant-climate change research is becoming a multi- and transdisciplinary field of relevant research.

Plants and Climate Change (Hardcover): Jelte Rozema, Rien Aerts, Hans Cornelissen Plants and Climate Change (Hardcover)
Jelte Rozema, Rien Aerts, Hans Cornelissen
R4,700 Discovery Miles 47 000 Ships in 10 - 15 working days

This book focuses on how climate affects or affected the biosphere and vice versa both in the present and in the past. The chapters describe how ecosystems from the Antarctic and Arctic, and from other latitudes, respond to global climate change. The papers highlight plant responses to atmospheric CO2 increase, to global warming and to increased ultraviolet-B radiation as a result of stratospheric ozone depletion.

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