BIOL 1442 Ch 47 The Biodiversity Crisis

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37 Terms

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ecologist have measured biodiversity by
taking into account both the number of species and their relative abundance to eachother
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adaptive radiation
rapid branching through speciation of a phylogenetic clade into many related species
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extinction
the disappearance of a species
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The rate of species loss today is comparable with
the five periods of mass extinction
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Three human activities have a major impact on the current extinction:
destruction of habitat, introduction of exotic species, and over-harvesting
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genetic diversity/genetic variation
defines the raw material for evolution and adaptation in species
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the species with the most genetic potential for subsequent evolution is the most
genetically diverse one
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genetic diversity can be measured as chemical diversity in that
different species produce a variety of chemicals in their cells
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ecosystem diversity
the number of different ecosystems on the planet of within a given geographic area
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The loss of an ecosystem means
the loss of interactions between species, the loss of unique features of coadaptation, and the loss of biological productivity
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Endemic species
only found in one location
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biodiversity increases
closer to the equator
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The hypothesis for why biodiversity increases closer to the equator include
the greater age of ecosystems in the tropics and the increased direct energy the tropics receive from the sun
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Tropical ecosystem complexity may promote speciation by increasing the
heterogeneity (number of ecological niches) in the tropics relative to higher latitudes
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The tropics have been perceived as being more stable than
temperate regions
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Norman Myers developed the concept of
biodiversity hotspots
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Biodiversity hotspots
geographical areas that contain high numbers of endemic species
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The number of species on the planet are the result of
speciation and extinction
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Five strata in the fossil record that appear to show sudden and dramatic losses in biodiversity are called
mass extinctions
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The Ordovician-Silurian extinction is the
first recorded mass extinction and the second largest, killing 85% of marine species
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The main hypothesis for the Ordovician-Silurian extinction is
a period of glaciation then warming
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The late Devonian extinction may have occurred ( ) and mostly affected ( )
over a relatively long period of time; marine species
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The end-Permian extinction was the ( ) in the history of life
largest
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In the end-Permian extinction, ( ) of all marine species and ( ) of all terrestrial species were lost
96%, 70%
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The leading suspect for the end-Permian extinction is
extended and widespread volcanic activity that led to a global-warming event
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In the end-Permian extinction, the oceans became largely ( ), suffocating marine life
anoxic
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The Triassic-Jurassic extinction may have been caused by
climate change, asteriod impact, and volcanic eruptions
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The end-Cretaceous extinction event was the result of a
cataclysmic impact of a large meteorite off the coast of the Yucatan peninsula
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The Pleistocene extinction was one of the ( ) extinctions and was ( )
lesser; recent
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In North America, the Pleistocene extinction losses included
woolly mammoths, mastodon, giant beavers, giant ground sloths, saber-toothed cats, and the North American camel
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The timing of the Pleistocene extinctions coincided with the arrival of
paleo-humans
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The Holocene extinction is the ( ) and is largely do to activities of ( )
sixth mass extinction; modern homo sapiens
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Some examples of animals going extinct during the Holocene extinction include the
dodo bird, Steller’s sea cow, passenger pigeon, Carolina parakeet, Japanese sea lion, and Carribean monk seal
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The International Union for Conservation of Nature keeps a list of extinct and endangered species called the
red list
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Estimation of extinction rates are hampered bu the fact that
most extinctions are probably happening without observation
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background extinction rate is estimated to be about
one per million species per year
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species-area relationship
the rate at which new species are seen when the area surveyed is increased