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describe how biodiversity has changed over geologic time through speciation and extinction
long-term evolutionary changes in global diversity have largely been the results of speciation and extinction
the number of species has been increasing for the past 600 million years
end of the permian (225 mya)
90% of marine invertebrates lost most likely due to volcanic activity
end of the cretaceous (65 mya)
dinosaurs and many other species went extinct likely due to asteroid
during the pleistocene (10,000 years ago)
ice age mammals went extinct
caused by movement of ice sheets and/or hunting by humans
modern extinctions (since 1600)
75% of extinctions have been the result of human activity
explain major global patterns of biodiversity, including latitudinal, elevational, and species–area trends
latitudinal diversity gradient: biodiversity increases from the poles toward the tropics.
high latitudes have fewer species than low latitudes
arctic tundra has fewer species than tropical rainforests
this pattern is seen in both aquatic and terrestrial environments
vascular plants tend to show peak diversity in the region around the equator
identify the main drivers behind biodiversity patterns, such as energy, climate, habitat heterogeneity, and geographic isolation
energy:
more environmental energy usually means more productivity
more plant growth and more resources for animals
climate:
climate controls how much heat and energy ecosystems receive
PET (potential evapotranspiration)
higher PET means logs of energy, and more energy supports more life
higher biomass
bigger populations
more species
habitat heterogeneity:
geographic isolation:
interpret how energy availability and productivity influence species richness on land and in the ocean
ocean NPP actually increases from the equator toward to poles, especially in the northern hemisphere during summer
changes in thermoclines and vertical nutrient mixing affect how much NPP occurs through the year
apply island biogeography theory to predict how island size and distance affect species richness
species richness on an island reflects a balance between immigration and extinction
island area strongly influences this balance
large island support more species and smaller island support fewer species
differentiate among alpha, beta, and gamma diversity across spatial scales
alpha diversity: the local species diversity of individual communities
beta diversity: variation in species composition among sites (communities) in a geographic area
gamma diversity: total species diversity across all communities within a geographic area