By Edward I. Newman(auth.)
Chapter 1 advent (pages 1–6):
Chapter 2 power, Carbon stability and international weather swap (pages 7–47):
Chapter three Water (pages 48–78):
Chapter four Soil (pages 79–116):
Chapter five Fish from the ocean (pages 117–144):
Chapter 6 administration of Grazing Lands (pages 145–171):
Chapter 7 administration of Forests (pages 172–204):
Chapter eight Pest keep watch over (pages 205–244):
Chapter nine toxins (pages 245–280):
Chapter 10 Conservation and administration of untamed Species (pages 281–321):
Chapter eleven recovery of groups (pages 322–344):
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Additional resources for Applied Ecology and Environmental Management, Second Edition
The evidence includes the facts that [ l )different species extended at different rates, suggesting that properties of the plants and their hspersers, rather than temperature change, were controlling the pace; and (2)study of present-day plants does not suggest an ability to migrate faster than they did in the past. This section on dispersal rates has been all about plants. We have no similar data on past rates of dispersal for any animal groups. Some 45 Will wildspecies be abletomovefost enougbl ENERGY, CARBON A N D CLIMATE C H A N G E mammal groups are now far from where they were in the late Pleistocene.
Problem: requires large supply of CO,, as well as sophisticatedcontrol of its supply rate. Further information: Ceulemans & Mousseau ( 1994),McLeod &Long (1999). Mousseau 1994); see also note 3 of the table. Species with the C4 photosynthetic mechanism have a different initial CO, capture step, which makes them more efficient at capturing it from low concentrations. They might therefore be expected to benefit less than C3 species from increased CO,. Although there is some tendency towards this, there is a wide range of responses in both groups and much overlap between them (Poorter 1993).
5 15 Thousand years BP 0 o'2 i t 1860 1880 1900 1920 1940 1960 1980 2000 Year Fig. 7 Air temperatures in the past, on various timescales. [a)Antarctica, during past 50 000 years. (b)At a site [Dye3) in Greenland, from about 15-10 000 BP. (a)and (b)are based on oxygen-isotope determinations on ice from deep cores; they indicate the amount of temperature change, but not the exact temperature at any particular time. (c)World mean air temperature, land and sea sites, 1861-1994. The line has smoothed year-to-year fluctuations, to show trends on a decade-by-decade timescale.