通过在蓝碳生态系统中埋葬碳来预测气候缓解 - - 挑战和陷
Erik Kristensen1, Mogens R Flindt1, Cintia O Quintana1
1Department of Biology, University of Southern Denmark, Odense, Denmark.
Global change biology
|January 6, 2025
概括
沿海生态系统中的蓝色碳封存往往被高估了. 目前的方法无法考虑长期储存,分解和温室气体排放,从而挑战其气候减缓潜力.
科学领域:
- 海洋生态海洋生态学
- 气候科学是气候科学.
- 生物地质化学生物地质化学
背景情况:
- 红树林,盐沼和海草等蓝色碳生态系统 (BCE) 对碳捕获至关重要.
- 准确评估长期碳储存对于评估它们的气候减缓潜力至关重要.
研究的目的:
- 批判性地评估蓝色碳的定义,测量方法和时间尺度.
- 评估目前用于估计欧洲央行蓝色碳封存的方法的可靠性.
- 确定蓝色碳的实际气候缓解潜力,考虑排放和储存限制.
主要方法:
- 对沉积碳库存和积累率的分析.
- 碳质平衡模型的应用.
- 使用3G指数模型进行长期分解模拟.
- 评估来自ECB的温室气体 (GHG) 排放 (CH4和N2O).
主要成果:
- 目前的库存和质量平衡方法高估了蓝色碳封存的3-18倍.
- 沉积物流动性和生物流使长期标记方法 (例如210Pb) 无效.
- 质量平衡模型与气候变化和超过100年的不完整碳预算作斗争.
- 来自ECB的温室气体 (CH4,N2O) 排放可能会抵消或超过碳捕获效益.
结论:
- 已公布的欧洲央行的蓝色碳封存估计可能是显著的高估.
- 蓝色碳的长期气候缓解潜力是值得怀疑的,因为方法上的限制和同时排放的温室气体.
- 为了准确的气候政策和保护工作,需要重新考虑蓝色碳评估.
相关概念视频
The Carbon Cycle
37.0K
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.
37.0K
Bioremediation
18.2K
Bioremediation is the use of prokaryotes, fungi, or plants to remove pollutants from the environment. This process has been used to remove harmful toxins in groundwater as a byproduct of agricultural run-off and also to clean up oil spills.
18.2K
Global Climate Change
24.2K
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.
24.2K
Adaptations that Reduce Water Loss
25.1K
Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
25.1K
The Sulfur Cycle
43.7K
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
43.7K
C4 Pathway and CAM
45.2K
Most plants use the C3 pathway for carbon fixation. However, some plants, such as sugar cane, corn, and cacti that grow in hot conditions, use alternative pathways to fix carbon and conserve energy loss due to photorespiration. Photorespiration is the process that occurs when the oxygen concentration is high. Under such conditions, the rubisco enzyme in the Calvin cycle binds O2 instead of CO2, which halts photosynthesis and consumes energy.
C4 Pathway
The C4 pathway is used by plants such as...
C4 Pathway
The C4 pathway is used by plants such as...
45.2K


