Eric Post
- Published in print:
- 2013
- Published Online:
- October 2017
- ISBN:
- 9780691148472
- eISBN:
- 9781400846139
- Item type:
- chapter
- Publisher:
- Princeton University Press
- DOI:
- 10.23943/princeton/9780691148472.003.0002
- Subject:
- Biology, Ecology
This chapter explores the dynamics of plant and animal species and species assemblages during the Earth's most recent period of rapid warming to garner insights into the potential consequences of ...
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This chapter explores the dynamics of plant and animal species and species assemblages during the Earth's most recent period of rapid warming to garner insights into the potential consequences of future rapid climate change. From the perspective of climate change ecology, the Late Pleistocene and the Pleistocene–Holocene transition are relevant because they represent the end of a prolonged period of climatic fluctuation on multiple temporal scales followed by rapid warming. Not only did Earth's major biomes undergo extensive compositional changes during the late Quaternary and near the termination of the Pleistocene epoch, they also underwent geographically large-scale redistributions, and did so rapidly, in some cases on the scale of decades. If rapid warming during the Pleistocene–Holocene transition contributed to—or even acted as the main driver of—mass extinctions, such a scenario would seem to suggest that contemporary climate change has a similar capacity to precipitate species losses.Less
This chapter explores the dynamics of plant and animal species and species assemblages during the Earth's most recent period of rapid warming to garner insights into the potential consequences of future rapid climate change. From the perspective of climate change ecology, the Late Pleistocene and the Pleistocene–Holocene transition are relevant because they represent the end of a prolonged period of climatic fluctuation on multiple temporal scales followed by rapid warming. Not only did Earth's major biomes undergo extensive compositional changes during the late Quaternary and near the termination of the Pleistocene epoch, they also underwent geographically large-scale redistributions, and did so rapidly, in some cases on the scale of decades. If rapid warming during the Pleistocene–Holocene transition contributed to—or even acted as the main driver of—mass extinctions, such a scenario would seem to suggest that contemporary climate change has a similar capacity to precipitate species losses.
Eric Post
- Published in print:
- 2013
- Published Online:
- October 2017
- ISBN:
- 9780691148472
- eISBN:
- 9781400846139
- Item type:
- chapter
- Publisher:
- Princeton University Press
- DOI:
- 10.23943/princeton/9780691148472.003.0009
- Subject:
- Biology, Ecology
This concluding chapter argues that Earth's climate is warming at a pace that may very well be unprecedented, and it is doing so from a higher baseline average temperature than that which was the ...
More
This concluding chapter argues that Earth's climate is warming at a pace that may very well be unprecedented, and it is doing so from a higher baseline average temperature than that which was the starting point for the most recent episode of rapid warming, which signaled the end of the Pleistocene and the demise of most of its large mammals. That most recent warming episode also coincided with geographically widespread biome shifts. Perhaps more tellingly, current warming, still in its early stages, has already heralded similarly geographically widespread and taxonomically broad shifts in phenological dynamics, population dynamics, species distributions, and ecosystem carbon dynamics. Indeed, some have asserted that Earth may be on the threshold of the sixth major extinction event.Less
This concluding chapter argues that Earth's climate is warming at a pace that may very well be unprecedented, and it is doing so from a higher baseline average temperature than that which was the starting point for the most recent episode of rapid warming, which signaled the end of the Pleistocene and the demise of most of its large mammals. That most recent warming episode also coincided with geographically widespread biome shifts. Perhaps more tellingly, current warming, still in its early stages, has already heralded similarly geographically widespread and taxonomically broad shifts in phenological dynamics, population dynamics, species distributions, and ecosystem carbon dynamics. Indeed, some have asserted that Earth may be on the threshold of the sixth major extinction event.
