大陆的挖掘历史超过十亿年的时间尺度
Terrence J Blackburn1, Samuel A Bowring, J Taylor Perron
1Earth Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA. terrence@mit.edu
概括
古代大陆石化层保留了地球上最古老的结构. -热年代学揭示了数十亿年的极低侵蚀率,与大陆的年龄相一致.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
背景情况:
- 大陆石化层拥有地球上最古老,最稳定的地质结构.
- 这些古老的碎片提供了对地质时间尺度上的构造和表面过程的洞察.
- 了解升起,侵蚀和冷却的历史,揭示了大陆的物理特性和挖掘力.
研究的目的:
- 为了重建古代石质层冷却的连续记录.
- 调查大陆残骸的长期侵蚀速度.
- 为了了解驱动地下层挖掘的力量在地质时间的推移.
主要方法:
- 在火山挖掘的下层地碎片上利用- (U-Pb) 热年代学.
- 应用热和扩散模型来解释热时间学数据.
- 构建了古代石质层的连续冷却记录.
主要成果:
- 据U-Pb数据显示,侵蚀率非常低.
- 这些低的侵蚀率一直持续在接近大陆年龄的时间尺度上.
- 这些发现限制了古代大陆碎片可能的侵蚀历史.
结论:
- 大陆石化层表现出显著的长期稳定性.
- 极其缓慢的侵蚀速度是古代大陆遗迹的特征.
- 该研究为了解大陆的长期演变和弹性提供了关键数据.
更多相关视频
09:06Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
Published on: July 3, 2016
06:55Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
Published on: August 5, 2016
相关概念视频
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...
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.
What is Evolutionary History?
Scientists record evolutionary history by analyzing fossil, morphological, and genetic data. The fossil record documents the history of life on Earth and provides evidence for evolution. However, both fossil and living organisms offer evidence that outlines Earth’s evolutionary history.
The Colonization of Land
Changes in the environment of the early Earth drove the evolution of organisms. As prokaryotic organisms in the oceans began to photosynthesize, they produced oxygen. Eventually, oxygen saturated the oceans and entered the air, resulting in an increase in atmospheric oxygen concentration, known as the oxygen revolution approximately 2.3 billion years ago. Therefore, organisms that could use oxygen for cellular respiration had an advantage. More than 1.5 years ago, eukaryotic cells and...
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
