関連する実験動画
Updated: Jul 11, 2026

06:27
Simulating Impacts of Ice Storms on Forest Ecosystems
Published on: June 30, 2020
プレイストセーン時代に東アフリカで劇的な気候変化があったという同位体証拠
T E Cerling1, R L Hay, J R O'Neil
1Department of Geology and Geophysics, University of California, Berkeley, CA 94720, USA.
Nature
|May 12, 1977
まとめ
古代気候の変化により,東アフリカでは約180万~220万年前と50万~60万年前,降雨量が大幅に減少した. これは,古代炭酸塩の酸素同位体比の変化によって証明されています.
科学分野:
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- イソトープ地球化学 イソトープ地球化学
- 東アフリカ パレオ環境
背景:
- 過去の降雨パターンを再構築することは,気候の動態とヒトの進化を理解するために不可欠です.
- ペドゲン系および地下水の炭酸塩の酸素同位体分析は,古気候条件の信頼できるプロキシを提供します.
関連する概念動画
What is Weather?
Overview
What is Climate?
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.
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 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.
Responses to Heat and Cold Stress
Every organism has an optimum temperature range within which healthy growth and physiological functioning can occur. At the ends of this range, there will be a minimum and maximum temperature that interrupt biological processes.
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.

