河流对古世/新世边界突然全球变暖的反应
Brady Z Foreman1, Paul L Heller, Mark T Clementz
1University of Wyoming, Department of Geology and Geophysics, 1000 East University Avenue, Laramie, Wyoming 82071, USA. bforema1@uwyo.edu
Nature
|November 7, 2012
概括
古世 - 世热极值 (PETM) 在科罗拉多州西部造成了重大的河流变化,导致厚厚的砂岩沉积. 这些河流反应在变暖事件发生后很长时间仍然存在,突出显示了气候变化.
科学领域:
- 沉积地质的地质学
- 古气候学 古气候学
- 河流的地质形态学
背景情况:
- 气候对沉积物产生,运输和沉积在沉积盆地的沉积有很大的影响.
- 鉴定气候对盆地层级学的影响是具有挑战性的,因为复杂的系统动态.
- 古世 - 世热极值 (PETM) 为快速的全球变暖及其地形后果提供了有价值的模拟.
相关概念视频
Global Climate Change
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Responses to Drought and Flooding
Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
The Fossil Record
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
Microbes and Climate Change
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
Responses to Heat and Cold Stress
Every organism has an optimum temperature range within which healthy growth and physiological functioning can occur. At the ends of this range, there will be a minimum and maximum temperature that interrupt biological processes.
Speciation Rates
Overview


