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Ecology and the Biosphere Chapter 50 Ecology - the study of the interactions between organisms and their environments The interactions between organisms and their environments determine their distributions and abundances • Distribution = geographic range • abundance=individuals per unit area • environmental factors – abiotic - non-living chemical and physical factors – biotic - living factors like other organisms Figure 50.1 Distribution and abundance of the red kangaroo in Australia, based on aerial surveys Figure 50.2 Sample questions at different levels of ecology Examples of ecological questions: • How do diving whales select their feeding areas? • What processes recycle vital chemical elements, such as nitrogen, in a savanna ecosystem • What factors influence the diversity of tree species that make up a particular forest Factors affecting the distribution of organisms • • • • dispersal behavior and habitat selection biotic factors abiotic factors Biogeography • The study of past and present distributions of individual species • continental drift and barriers contribute to distinctive floras and faunas of the Earth’s major regions Figure 50.4 Biogeographic realms Dispersal • Example: Kangaroos may not be in North America because they historically had no way of getting there. • To test this: species transplant experiments Figure 50.6 Set of transplant experiments for a hypothetical species • Transplant successful - distribution limited because of dispersal problems – inaccessible, not enough time to reach area, not recognized as suitable living space • transplant unsuccessful - distribution limited by biotic or abiotic factors, I.e., for some reason cannot survive there. Invasive species • In modern times, normal restrictions on dispersal are lifted and invasive species can proliferate Figure 50.7 Spread of the African honeybee in the Americas since 1956 Figure 50.8 Expansion of the geographic range of the zebra mussel (Dreissena polymorpha) since its discovery near Detroit in 1988 Spartina alterniflora and Spartina anglica • Saltmarsh grasses native to the Eastern U.S. (S. alterniflora) and British Isles (S. anglica). • Invasive species in Puget Sound and Willapa Bay in Washington State. Spartina are physiologically resilient and vigorous • Physiological tolerance – Wide range of salinities – Waterlogged soils • Anoxia • Hydrogen sulfide • Fast rate of spread - average 10-20% per year (can be much greater) Willapa Bay • Spartina alterniflora • 10,000 to 25,000 acres affected • Nearly 4000 solid acres Puget Sound • Spartina anglica • ≈7000 acres affected – Solid acres: • • • • Pink=<1 Peach= 1-5 Blue=6-100 Red=>100 1999 Managing the spartina problem • >$10 million spent since 1990 – Affected areas have increased from a few thousand to >20,000 acres • Herbicide and mechanical control – $2000 per acre per year Distribution of hydrogen sulfide in sediments Oxidized zone No hydrogen sulfide Anoxic zone Hydrogen sulfide-rich Tolerating anoxic sediments • Aerenchyma • Anaerobic metabolism – Alcohol dehydrogenase • Sulfide oxidation Spartina anglica root Biotic factors affect the distribution of organisms • Competition – interspecific – intraspecific • Predation • Mutualism - species helping each other Figure 50.9 Predator-removal experiments Limpet and urchin removal experiments • Results show that the herbivores limit the distribution and abundance of seaweed • limpets appear to be the main herbivores • but why is there more seaweed when both limpets and urchins are removed? Temperature and water are major climatic factors determining the distributions of organisms • Biome-a major type of ecosystem Figure 50.10 A climograph for some major kinds of ecosystems (biomes) in North America Global climate patterns Figure 50.12 What causes the seasons? Figure 50.14 How mountains affect rainfall Figure 50.15 Lake stratification and seasonal turnover (Layer 1) • Winter • cold water at surface • warmer deeper in lake • Spring - surface water warms and sinks allowing mixing. Oxygen to bottom waters and nutrients to surface waters Summer -thermocline development summer • Thermal profile develops • thermocline -separates cold bottom water and warm surface water Figure 50.15 Lake stratification and seasonal turnover (Layer 4) Fall • Surface water cools rapidly and sinks • thermocline disappears • remixing of lake water Figure 50.16 Current geographic range and predicted future range for the American beech (Fagus grandifolia) under two climate-change scenarios Figure 50.17 The distribution of major aquatic biomes Figure 50.18 Zonation in a lake Figure 50.19 Freshwater biomes: Oligotrophic lake (left), eutrophic lake (top right), stream flowing into a river (bottom right) Figure 50.20 Damming the Columbia River Basin Figure 50.21 Wetlands (top) and estuaries (bottom) Figure 50.22 Zonation in the marine environment Figure 50.23 Examples of marine biomes Figure 50.23cx Black smoker Figure 50.24 The distribution of major terrestrial biomes Figure 50.25a Tropical forests Figure 50.25b Savanna Figure 50.25bx Savanna Figure 50.25c Deserts Figure 50.25d Chaparral Figure 50.25dx Chaparral Figure 50.25e Temperate grassland Figure 20.25f Temperate deciduous forest Figure 20.25g Coniferous forests Figure 20.25h Tundra Figure 50.26 A hierarchy of scales for analyzing the geographic distribution of the moss Tetraphis Figure 50.27 Most species have small geographic ranges Figure 50.x1 Patterns of distribution in the biosphere