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相关概念视频

The Evidence for Evolution02:55

The Evidence for Evolution

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Genetic variations accumulating within populations over generations give rise to biological evolution. Evolutionary changes can result in the formation of novel varieties and entire new species. These changes are responsible for the diverse forms of life inhabiting the planet. The evidence for evolution suggests that all living organisms descended from common ancestors.
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Convergent Evolution01:54

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Evolution shapes the features of organisms over time, ensuring that they are suited for the environments in which they live. Sometimes, selection pressure leads to the rise of similar but unrelated adaptations in organisms with no recent common ancestors, a process known as convergent evolution.
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The endosymbiont theory is the most widely accepted theory of eukaryotic evolution; however, its progression is still somewhat debated. According to the nucleus-first hypothesis, the ancestral prokaryote first evolved a membrane to enclose DNA and form the nucleus. Conversely, the mitochondria-first hypothesis suggests that the nucleus was formed after endosymbiosis of mitochondria.
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John H. Renwick first coined the term “synteny” in 1971, which refers to the genes present on the same chromosomes, even if they are not genetically linked. The species with common ancestry tend to show conserved syntenic regions. Therefore, the concept of synteny is nowadays used to describe the evolutionary relationship between species.
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No description available
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The genomes of eukaryotes are punctuated by long stretches of sequence which do not code for proteins or RNAs. Although some of these regions do contain crucial regulatory sequences, the vast majority of this DNA serves no known function. Typically, these regions of the genome are the ones in which the fastest change, in evolutionary terms, is observed, because there is typically little to no selection pressure acting on these regions to preserve their sequences.
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相关实验视频

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塞雷斯上的石坑:对其地和演变的影响

H Hiesinger1, S Marchi2, N Schmedemann3

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黎明航天器的观测显示,星球表面有大量的石坑,这与冰的预测相矛盾. 坑道形态表明冰岩组成混合, 年代可追溯到几亿年的光滑区域.

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科学领域:

  • 星球科学
  • 地质学
  • 天文地质学

背景情况:

  • 热化学模型预测Ceres的内部有差异化和冰的地,撞击坑最小.
  • 之前的模型表明,由于预期的冰表面有利于放松,因此缺乏大坑.

研究的目的:

  • 来自"黎明"号探测器的观测数据.
  • 根据火山口形态和分布,调查塞雷斯地的组成和地质历史.

主要方法:

  • 分析来自"黎明"航天器的高分辨率图像.
  • 对撞击坑的形态研究,包括形状,特征和分布.
  • 使用火山口约会技术确定特定区域的绝对模型年龄 (AMA).

主要成果:

  • 塞雷斯表面有大量的石坑,而且石坑分布不同,这与之前的预测相反.
  • 坑道形态表明地既不是纯冰,也不是纯岩石,具有多边形,露台和倾斜等特征.
  • 根据时间模型,Kerwan火山口附近的光滑区域的绝对模型年龄表明形成于5.5亿和7.2亿年前.

结论:

  • 塞雷斯的表面比预期的要有更多的石坑,这表明地质历史更为复杂.
  • 塞雷斯地的混合冰岩组成影响了火山口的形态和保存.
  • 表面特征的约会为塞雷斯的地质演变提供了新的约束.