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相关概念视频

Life Histories01:29

Life Histories

Constrained by limited energy and resources, organisms must compromise between offspring quantity and parental investment. This trade-off is represented by two primary reproductive strategies; K-strategists produce few offspring but provide substantial parental support, whereas r-strategists produce much progeny that receives little care. These strategies are related to an organism’s survival likelihood across its lifespan, which is represented by a survivorship curve. Three general types of...
Speciation Rates01:07

Speciation Rates

Speciation can proceed at markedly different rates, and evolutionary biologists commonly describe these differences through the models of gradualism and punctuated equilibrium. Both patterns explain how new species arise, but they differ in the tempo and continuity of evolutionary change. In both cases, evolutionary change arises from heritable variation within populations, with natural selection often shaping traits that improve survival and reproduction under specific environmental conditions.
What is Evolutionary History?02:35

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.Phylogenetic trees illustrate the evolutionary relationships among these organisms. Scientists infer organisms’ common ancestry by evaluating shared morphological and genetic characteristics. Together, the fossil...
The Evidence for Evolution02:55

The Evidence for Evolution

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.The collection of fossils within sedimentary rocks give a record of common ancestry and often depicts the history of evolution.
The Fossil Record02:56

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...
The Tree of Life - Bacteria, Archaea, Eukaryotes02:40

The Tree of Life - Bacteria, Archaea, Eukaryotes

The “tree of life” describes the evolution of life and the evolutionary relationships between organisms. The root of the tree is the common ancestor to all life on Earth. All other species radiate from this point, much like the branches of a tree. The numerous tips of these branches on the tree of life represent every living, or extant, species. Extinct species, which are species that no longer exist, can be found towards the center of the tree. Currently, these organisms, both extant and...

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相关实验视频

Updated: Jul 18, 2026

Linking Predation Risk, Herbivore Physiological Stress and Microbial Decomposition of Plant Litter
10:20

Linking Predation Risk, Herbivore Physiological Stress and Microbial Decomposition of Plant Litter

Published on: March 12, 2013

考古时期的生物圈是颠倒的吗?

J C Walker1

  • 1Department of Atmospheric and Oceanic Sciences, University of Michigan, Ann Arbor 48109, USA.

Nature
|October 22, 1987
PubMed
概括

光合作用产生有机碳和氧化剂. 这些产品的差异运输,如氧和铁,塑造了地球的古代生物圈,使其在底部氧化,在顶部减少.

科学领域:

  • 生物地质化学生物地质化学
  • 地质地质地质地质地质地
  • 古气候学 古气候学

背景情况:

  • 光合作用产生相当数量的减少有机碳和氧化伴侣.
  • 这些产品可以发生反应,但环境的运输过程往往会将它们分开,导致不同的氧化还原区.
  • 了解这些氧化还原动力学对于解释地球早期的生物地球化学循环至关重要.

研究的目的:

  • 为了研究光合作用产品在无氧古生物圈中的差异化运输.
  • 为了将古生物圈的氧化还原分层与现代生物圈的氧化还原分层进行对比.
  • 提出地球早期历史中氧化剂和减少剂的分布模型.

主要方法:

  • 基于化学性质和运输过程的概念建模.
  • 现代和古代生物地质化学条件的比较.
  • 分析氧气,铁和有机碳等关键化合物的可溶性和流动性.

主要成果:

  • 在现代生物圈中,氧气在大气中积累,而有机物沉降.
  • 在无氧的古老地球上,氧化铁的溶解性较低,可能比有机碳更快.
  • 这种差异性运输将导致氧化"底部" (沉积物) 和减少"顶部" (海洋/大气层).
关键词:
美国宇航局的学科是外生态学.美国宇航局的纪律号为52-30号.美国国家航空航天局 (NASA) 计划外生态学.非NASA中心的中心.

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Preparation of Free-Surface Hyperbolic Water Vortices
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Preparation of Free-Surface Hyperbolic Water Vortices

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Using Archival Japanese Paper and Thermoplastic Resins to Prepare Fossils for Storage, Display, Transport, and Radiography
07:30

Using Archival Japanese Paper and Thermoplastic Resins to Prepare Fossils for Storage, Display, Transport, and Radiography

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相关实验视频

Last Updated: Jul 18, 2026

Linking Predation Risk, Herbivore Physiological Stress and Microbial Decomposition of Plant Litter
10:20

Linking Predation Risk, Herbivore Physiological Stress and Microbial Decomposition of Plant Litter

Published on: March 12, 2013

Preparation of Free-Surface Hyperbolic Water Vortices
04:35

Preparation of Free-Surface Hyperbolic Water Vortices

Published on: July 28, 2023

Using Archival Japanese Paper and Thermoplastic Resins to Prepare Fossils for Storage, Display, Transport, and Radiography
07:30

Using Archival Japanese Paper and Thermoplastic Resins to Prepare Fossils for Storage, Display, Transport, and Radiography

Published on: November 14, 2025

结论:

  • 生物圈的氧化还原结构受到光合作用产品化学性质的显著影响.
  • 与现代生物圈相比,古生物圈可能表现出相反的氧化还原分层.
  • 这表明,地球早期的生物地化学环境从根本上有所不同.