相关实验视频
Updated: Jul 23, 2026

10:00
Assaying DNA Damage in Hippocampal Neurons Using the Comet Assay
Published on: December 19, 2012
地化学证据表明,在伊欧纪晚期发生了一场彗星阵雨
K A Farley1, A Montanari, E M Shoemaker
1Division of Geological and Planetary Sciences, California Institute of Technology, MS 170-25, Pasadena, CA 91125, USA. farley@gps.caltech.edu
概括
地球经历了增加的外星-3,一个尘埃追踪器,在晚期的伊欧纪. 这种250万年的流动与主要的小行星撞击相吻合,这表明太阳系尘埃和地球穿越物体的短暂增强.
科学领域:
- 地质化学 地质化学
- 行星科学 行星科学
- 古气候学 古气候学
背景情况:
- 类石灰岩含有外星-3,是一种行星间尘埃的标记物.
- 大型撞击事件,如波皮盖和切萨皮克湾石坑,大约发生在3600万年前.
- 纪晚期经历了重要的地质和天文事件.
研究的目的:
- 为了分析外层-3度的海底石灰岩.
- 为了将-3流与地球历史上重大冲击事件相关联.
- 为了研究地球穿越物体和太阳系内部尘埃的动态.
主要方法:
- 地质石灰岩样本的地化学分析.
- 同位素分析以量化-3度.
- 年代测算是为了确定事件之间的时间关系.
主要成果:
- 一个2.5百万年 (My) 期间的增强的外星-3流被确定在Eocene晚期.
- -3增强开始于波皮盖伊和切萨皮克湾撞击事件前1小时,结束在波皮盖伊和切萨皮克湾撞击事件后1.5小时.
- 3度的增加与大型撞击事件相关,表明地球穿越物体和太阳系内部尘埃的同时,短暂增强.
结论:
- 同时的相关性表明由奥尔特云扰动引发的彗星雨.
- 穿越地球的物体和星际尘埃在以欧纪晚期经历了短暂的增长.
- 这一事件为太阳系内部影响地球的动态过程提供了证据.
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.
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.
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...
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.
Preparation of Samples for Electron Microscopy
To be visualized by an electron microscope, either transmission or scanning, biological samples need to be fixed (stabilized) so the electron beam does not destroy them and dried thoroughly (desiccated/dehydrated) so the vacuum does not affect them. Fixation needs to be done as quickly as possible because the sample properties will start changing as soon as it is removed from its natural environment. For example, in a tissue sample, the oxygen levels begin decreasing, causing an altered...
Momentum And Radiation Pressure
An object absorbing an electromagnetic wave would experience a force in the direction of propagation of the wave. This force occurs because electromagnetic waves contain and transport momentum. The force accounts for the wave's radiation pressure exerted on the object. Maxwell's prediction was confirmed in 1903 by Nichols and Hull by precisely measuring radiation pressures with a torsion balance. The measuring instrument had mirrors suspended from a fiber kept inside a glass container. Nichols...

