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      Preindustrial Human Impacts on Global and Regional Environment

      Annual Review of Environment and Resources
      Annual Reviews

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          Abstract

          Humans have had an impact on regional and global environments even prior to the Industrial Revolution through anthropogenic fire, agriculture, and the extinction of the Pleistocene megafauna. The preindustrial impact of anthropogenic fire to modify ecosystems and affect climate may have been small because in regions where impacts were once thought to be large, such as in Australia, the evidence now suggests a smaller effect. Both the extinction of the megafauna, which evidence indicates to be at least partially caused by humans, and preindustrial agriculture may have affected climate, but the effects may have offset each other. For instance, climate simulations indicate that megafauna extinctions may have led to a slight global warming, but later, agriculture led to a slight global cooling. Prior to the industrial era, the largest ecological and climate anomaly may have been associated with forest expansion during the early and mid-Holocene when there were few megafauna and agriculturalists to reduce this expansion.

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          Fire in the Earth system.

          Fire is a worldwide phenomenon that appears in the geological record soon after the appearance of terrestrial plants. Fire influences global ecosystem patterns and processes, including vegetation distribution and structure, the carbon cycle, and climate. Although humans and fire have always coexisted, our capacity to manage fire remains imperfect and may become more difficult in the future as climate change alters fire regimes. This risk is difficult to assess, however, because fires are still poorly represented in global models. Here, we discuss some of the most important issues involved in developing a better understanding of the role of fire in the Earth system.
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            Quantifying and mapping the human appropriation of net primary production in earth's terrestrial ecosystems.

            Human appropriation of net primary production (HANPP), the aggregate impact of land use on biomass available each year in ecosystems, is a prominent measure of the human domination of the biosphere. We present a comprehensive assessment of global HANPP based on vegetation modeling, agricultural and forestry statistics, and geographical information systems data on land use, land cover, and soil degradation that localizes human impact on ecosystems. We found an aggregate global HANPP value of 15.6 Pg C/yr or 23.8% of potential net primary productivity, of which 53% was contributed by harvest, 40% by land-use-induced productivity changes, and 7% by human-induced fires. This is a remarkable impact on the biosphere caused by just one species. We present maps quantifying human-induced changes in trophic energy flows in ecosystems that illustrate spatial patterns in the human domination of ecosystems, thus emphasizing land use as a pervasive factor of global importance. Land use transforms earth's terrestrial surface, resulting in changes in biogeochemical cycles and in the ability of ecosystems to deliver services critical to human well being. The results suggest that large-scale schemes to substitute biomass for fossil fuels should be viewed cautiously because massive additional pressures on ecosystems might result from increased biomass harvest.
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              Causes of climate change over the past 1000 years

              Crowley (2000)
              Recent reconstructions of Northern Hemisphere temperatures and climate forcing over the past 1000 years allow the warming of the 20th century to be placed within a historical context and various mechanisms of climate change to be tested. Comparisons of observations with simulations from an energy balance climate model indicate that as much as 41 to 64% of preanthropogenic (pre-1850) decadal-scale temperature variations was due to changes in solar irradiance and volcanism. Removal of the forced response from reconstructed temperature time series yields residuals that show similar variability to those of control runs of coupled models, thereby lending support to the models' value as estimates of low-frequency variability in the climate system. Removal of all forcing except greenhouse gases from the approximately 1000-year time series results in a residual with a very large late-20th-century warming that closely agrees with the response predicted from greenhouse gas forcing. The combination of a unique level of temperature increase in the late 20th century and improved constraints on the role of natural variability provides further evidence that the greenhouse effect has already established itself above the level of natural variability in the climate system. A 21st-century global warming projection far exceeds the natural variability of the past 1000 years and is greater than the best estimate of global temperature change for the last interglacial.
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                Author and article information

                Journal
                Annual Review of Environment and Resources
                Annu. Rev. Environ. Resour.
                Annual Reviews
                1543-5938
                1545-2050
                October 17 2013
                October 17 2013
                : 38
                : 1
                : 503-527
                Article
                10.1146/annurev-environ-032012-095147
                5a9902b6-5270-4452-a77a-fdc0ddbe1643
                © 2013
                History

                Evolutionary Biology
                Evolutionary Biology

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