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| Home | |
| Climate Change Background | |
| Effects on Terrestrial Biodiversity | |
| Conservation Implications | |
| What Can Be Done? | |
| Conclusion | |
| References |
| A changing climate has strong implications for biodiversity.
Studies of fossil and pollen distribution show that species are very sensitive
to climate changes. When the climate changes, species often die out in
their present areas and colonize new areas. Therefore, as the climate changes
in the future, there will be disruption of natural communities and extinction
of populations and species.
Species track their climatic optima, and retract their ranges where conditions are unsuitable. These shifts are the sum of many local pressures on extinction and colonization due to factors such as physiology and interactions with other species. For plants, increases in heat and decreases in moisture can have direct effects on survival and reproduction. It is unlikely that all species will be able to evolve new tolerances with sudden changes in climate, leading to shifts in community composition and impacts on ecosystem dynamics. Specifically, changes in climate have an impact on the phenology
and distribution
of species, along with community
composition and ecosystem
dynamics. For each of these impacts, I discuss the expected
changes with climate change along with changes that have been observed.
While these impacts can occur in other systems, I am focusing on the terrestrial
system.
Phenology is the timing of seasonal activities and life cycle events. Warming temperatures are expected to impact phenological events, such as flowering and fruiting in plants or larval stages in insects. There have been observed changes in phenology, the timing of seasonal activities. Diurnal temperature ranges have decreased, leading to a lengthening of the freeze-free period in many regions. Studies in Europe and North America show a progressive increase in the timing of spring activities since the 1960s. Evidence of phenological changes include:
Distributions of plants and animals are heavily influenced by temperature and moisture patterns. Studies of fossil and pollen distribution show that species are very sensitive to climate changes. During several of the Pleistocene interglacial periods, the temperature was 2 to 3 degrees higher and vegetation was drastically different. When the climate changes, species often die out in their present areas and colonize new areas. Therefore, as the climate changes in the future, there will be disruption of natural communities and extinction of populations and species. Some species will be able to disperse to new areas but many will not be able to colonize new areas in sufficient time. An rapid increase of 3 degrees may exceed the ability of many species to adapt. Based on similar shifts in the past, it is reasonable to expect a 300 km shift in the temperate zone with a 3 degree increase. Species may also shift attitudinally as well as latitudinal: A 3 degree cooling of 500 meters in elevation is equal to 250 kilometers in latitude. As species move up mountains, they occupy smaller areas, have smaller populations and become vulnerable to genetic pressures. Species at the mountaintops may have nowhere to move to. Studies of sedentary species have shown a poleward and upward shift in species ranges across different taxonomic groups and geographic locations. However, due to the difference in dispersal abilities, there are different rates of range shifts among and within species. Specific examples of observed range shifts are:
Community compositions are expected to shift with changes in climatic variables due to the changes in physiology, phenology, and distributions.. As species distributions change, the composition of communities changes as well. For example, in the diagram below, species A and B initially overlap. After changes in climate, the distribution of species A has moved northward while the distribution of species B did not change. This leads to a reduction in the area where both species A and species B are found.
Changes in patterns of vegetation types are determined by temperature and precipitation. In addition, plant communities are sensitive to a rise in carbon dioxide concentrations, and increases in concentrations may lead to changes in vegetation patterns. Observed changes in community composition include:
There may be complex dynamics from a changing climate as a result of different responses from interacting species. Species that closely interact or compete may have different responses to climate change, influencing the outcome of their interactions. Examples of ecosystem changes include:
Sources: Walther et al. 2002, Hughes 2000, and McCarty 2001.
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Noelle Chambers 2002