まとめ
太平洋は,1970年から1990年にかけて,主に化石燃料から毎年2.1ギガトンもの二酸化炭素 (CO2) を吸収しました. これは,海洋が CO2 の主要な吸収源であり,生物圏から有意な放出がないことを示しています.
科学分野:
- 海洋学 海洋学とは
- 気候科学 気候科学
- バイオジオケミストリー バイオジオケミストリー
背景:
- 太平洋の表面水における溶解した無機炭素のデルタ13C値は,1970年から1990年の間に1ミリあたり0.4で減少した.
- この同位体シフトは,化石燃料の燃焼と森林伐採から発生する大気中の二酸化炭素 (CO2) の吸収に起因する.
研究 の 目的:
- 1970年から1990年の間に海洋に吸収され,生物圏に放出されたCO2の純量を定量化する.
- 炭素吸収源としての海洋の役割を決定し,この期間中に生物圏のCO2排出量を評価する.
主な方法:
- 大気中のCO2濃度の変化の分析.
- 大気中のCO2のデルタを測定する.
- 海洋における溶解した無機炭素のデルタ"3C値の評価.
主要な成果:
- 計算された平均的な海洋CO2の純吸収量は,年間2.1ギガトンであった.
- 同位体データは,海洋が人為的なCO2の支配的なネットシンクであることを示しています.
結論:
- 海洋は,大気中のCO2の増加を緩和する上で重要な役割を果たしています.
- 20年間の研究期間中,生物圏からの有意な純CO2排出は検出されなかった.
さらに関連する動画
関連する概念動画
The Carbon Cycle
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.
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...
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.
Carbon-13 (¹³C) NMR: Overview
Carbon-13 is a naturally occurring NMR-active isotope of carbon with a low natural abundance of 1.1%. In contrast, carbon-12 is the most abundant isotope of carbon with zero nuclear spin. Therefore, it is NMR inactive. The gyromagnetic ratio of carbon-13 is smaller than that of protons. As a result, carbon-13 resonance is about 6000 times weaker than proton resonance. For a given magnetic field strength, the resonance frequency of carbon-13 is about one-fourth of the resonance frequency for...
Carbon-dioxide Fixation
Carbon dioxide fixation in prokaryotes enables the assimilation of inorganic carbon into organic molecules, supporting biosynthetic pathways, sustaining ecosystems, and contributing to the global carbon cycle. It also has industrial applications in carbon capture and bioproduct synthesis. Autotrophic organisms rely on this process to utilize CO₂ as a carbon source in diverse environments.The Calvin CycleThe Calvin cycle is the most widespread carbon fixation mechanism, primarily used by...
Carbon Dioxide Transport in the Blood
Carbon dioxide (CO2) transport in the blood is critical to human physiology. On average, our body cells produce around 200 mL of CO2 per minute, precisely the quantity expelled by the lungs. This process involves the transportation of CO2 from the tissue cells to the lungs in three primary forms.
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...
Forms of CO2 Transport
1. Dissolved in plasma: A small percentage (7-10%) of CO2 is transported and dissolved directly in the plasma.
2. Carbaminohemoglobin: Just over 20% of CO2 is chemically bound to...


