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相关概念视频

What is Evolutionary History?02:35

What is Evolutionary History?

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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.
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Global Climate Change01:50

Global Climate Change

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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.
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Speciation Rates01:07

Speciation Rates

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Overview
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The Fossil Record02:56

The Fossil Record

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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...
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Criticisms of the Evolutionary Perspective01:23

Criticisms of the Evolutionary Perspective

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In a study where individuals posing as strangers offered compliments and proposed casual sex to students, the responses differed significantly based on gender. Not a single woman accepted the proposal, while 70% of the men agreed. This outcome provides a useful scenario to explore through the lens of evolutionary psychology and social learning theory, highlighting the diverse perspectives on human sexual behaviors.
Evolutionary psychology provides one explanation for these findings, suggesting...
159
Limits to Natural Selection01:38

Limits to Natural Selection

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Organisms that are well-adapted to their environment are more likely to survive and reproduce. However, natural selection does not lead to perfectly adapted organisms. Several factors constrain natural selection.
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相关实验视频

Updated: Sep 13, 2025

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

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一个动态系统的视角,在中期普莱斯托时代的过渡期.

N R Golledge1

  • 1Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand.

Journal of the Royal Society of New Zealand
|August 4, 2025
PubMed
概括

地球的气候周期在普世时期变得更加寒冷和不对称. 这项研究表明,增加内部反同步,而不仅仅是轨道强迫,推动了这些冰川-冰川间的转移.

科学领域:

  • 古气候学 古气候学
  • 地球系统科学 地球系统科学
  • 动态系统理论 动态系统理论

背景情况:

  • 自世以来,地球的气候逐渐冷却,导致越来越严重和不对称的冰川周期在普世时期.
  • 中世转型 (MPT) 标志着这些气候变化的显著加剧,关于外部强迫与内部反的争论正在进行中.
  • 了解冰川 - 冰川间周期的驱动因素对于重建过去的气候动态和预测未来的气候行为至关重要.

研究的目的:

  • 探讨推动纪期间冰川周期不对称性和强度增加的机制,特别是在纪中期过渡 (MPT) 周围.
  • 为了建模在晚普莱斯托时代观察到的不对称温度变化,并探索内部气候系统反的作用.
  • 确定外部驱动因素或内部反是否主要负责全球气候观察到的渐进变化.

主要方法:

  • 使用古老环境代理的Plio-Pleistocene气候周期特征的分析.
  • 开发和应用简单的概念动态系统模型.
  • 模拟晚期普莱斯托时代温度变化以复制观察到的不对称性.
  • 通过MPT调查地球系统内不断增加的合和同步.

主要成果:

  • 动态系统模型成功模拟了晚普莱斯托纪晚期温度变化的不对称模式.
  • 全球气候系统组成部分之间日益增长的合成为气候周期不对称的潜在机制.
关键词:
地球系统动态 地球系统动态这是米兰科维奇周期.古代气候是一种古气候.普利奥 - 普莱斯托时代有关反的反

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  • 有证据表明,通过MPT,由于同步增加,内部反在轨道阳光照射变化上占主导地位.
  • 结论:

    • 该研究提出,地球系统元素的同步日益增加,以10万年频率运行,推动了冰川周期的加剧和不对称.
    • 内部反,通过同步放大,推动全球气温向远离平衡的冰川状态.
    • 这些冰川状态最终被连锁环境事件所终结,这些环境事件与地球系统连接的崩有关.