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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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Threats to Biodiversity01:50

Threats to Biodiversity

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There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
27.9K
What is Climate?01:16

What is Climate?

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Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
21.6K
Microbes and Climate Change01:27

Microbes and Climate Change

65
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
65
The Carbon Cycle01:14

The Carbon Cycle

45.7K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
45.7K
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...
28.6K

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Using Generative Art to Convey Past and Future Climate Transitions
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Using Generative Art to Convey Past and Future Climate Transitions

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アントロポセノーを定義する.

Simon L Lewis1, Mark A Maslin2

  • 11] Department of Geography, University College London, Gower Street, London, WC1E 6BT, UK [2] School of Geography, University of Leeds, Leeds, LS2 9JT, UK.

Nature
|March 13, 2015
PubMed
まとめ
この要約は機械生成です。

人類の影響によって定義された新しい地質学時代の提案された人類新時代は,1610年または1964年に始まった可能性があります. 地球の地質学的記録における人間のサインの証拠は,この重要な環境時代の潜在的な開始日を支持しています.

科学分野:

  • 地球科学 地球科学 地球科学
  • 地質学 地質学 地質学
  • 環境科学 環境科学

背景:

  • 地質時間は,歴史的に地球の状態の重要な変化によって区切られています.
  • グローバルな環境の変化は,人類が支配する新しい時代である人類新世紀 (Anthropocene) の検討を促しています.

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