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関連する概念動画

Global Climate Change01:50

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 Earth02:06

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 Colonization of Land02:22

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...
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 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...
Conditions on Early Earth02:06

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.

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関連する実験動画

Updated: Jul 7, 2026

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas
07:54

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas

Published on: April 3, 2018

大陸の漂流は1900年以前のものです.

N A Rupke1

  • 1Department of Geological and Geophysical Sciences, Princeton University, Princeton, New Jersey 08540, USA.

Nature
|July 25, 1970
PubMed
まとめ

フランシス・ベーコンのような思想家によって提唱された大陸の漂移に関する初期の科学的な考えは,完全に開発されていませんでしたし,しばしばプロセスを漸進的な漂移ではなく,壊滅的な出来事として記述しました.

科学分野:

  • 地質科学は地質科学である.
  • 科学の歴史 科学の歴史

背景:

  • 大陸の漂流の概念は,近代的なプレート構造理論より前の歴史的ルーツを持っています.
  • 大規模な地殻の水平運動に関する初期の仮説は,17世紀と18世紀に存在しました.

研究 の 目的:

  • 大陸漂移の概念の歴史的起源を批判的に検討する.
  • 大陸の漂流の初期構想を初期の近代思想家に帰属する主張の正確さを評価する.

主な方法:

  • 歴史的文書分析の歴史的文書分析について
  • 地球科学に関する初期の科学的著作の文献レビュー

主要な成果:

  • 大陸の漂流という概念は,フランシス・ベーコンや彼の同時代の人たちによって最初に考えられたものではない.
  • 同様の考え方の初期の表現は,このプロセスを,漸進的な漂流とは異なる,単一の壊滅的な出来事として特徴づけた.

結論:

  • 大陸の漂流の起源に関する歴史的な物語は,改訂を必要としています.
  • 初期の科学思想は,地質学的変化をゆっくりと継続的なものではなく,突然で壊滅的なものとして見ていた.

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Visually Based Characterization of the Incipient Particle Motion in Regular Substrates: From Laminar to Turbulent Conditions
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Visually Based Characterization of the Incipient Particle Motion in Regular Substrates: From Laminar to Turbulent Conditions

Published on: February 22, 2018

Evolution of Staircase Structures in Diffusive Convection
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Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018

関連する実験動画

Last Updated: Jul 7, 2026

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas
07:54

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas

Published on: April 3, 2018

Visually Based Characterization of the Incipient Particle Motion in Regular Substrates: From Laminar to Turbulent Conditions
11:51

Visually Based Characterization of the Incipient Particle Motion in Regular Substrates: From Laminar to Turbulent Conditions

Published on: February 22, 2018

Evolution of Staircase Structures in Diffusive Convection
07:28

Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018