地球碳循环的缓慢关闭
1Lorenz Center, Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139.
概括
有机物微生物分解速度随着年龄的增长而放缓,影响全球碳循环. 这项研究表明,能量波动解释了这种衰老效应,影响了碳封存和大气氧气水平.
科学领域:
- 地质化学 地质化学
- 微生物学 微生物学
- 环境科学 环境科学
背景情况:
- 碳循环涉及有机碳的生产和消费,微生物调解分解.
- 有机物分解速度随着年龄的增长而放缓,这是海洋沉积物中观察到的现象.
- 这种依赖年龄的微生物降解的潜在机制仍然不太清楚.
研究的目的:
- 阐明控制有机物随年龄衰变的机制.
- 开发一个理论框架,预测有机物衰老中观察到的定量特征.
- 探索这些动态对碳捕获和大气组成的影响.
主要方法:
- 微生物分解过程的理论建模.
- 对微生物活动的能量可用性的分析.
- 模型预测与有机物衰变和微生物种群的实证数据的比较.
主要成果:
- 有机物衰变速度与年龄成反比例,这与观察到的数据一致.
- 微生物种群和有机碳度随着年龄的增长而下降.
- 在微生物的最小能量流条件下,确定了一种新的缩放模式.
- 该理论成功地预测了观察到的缩放指数.
结论:
- 有机物衰老及其对碳循环的影响是由微生物能量可用性的罕见,极端波动驱动的.
- 这些缓慢的,年龄依赖的动态阻止了沉积物中完全的有机碳氧化.
- 这种不完全的氧化允许大气中分子氧的积累.
更多相关视频
07:22Author Spotlight: Unraveling the Role of Earthworms in Enhancing Mineral Weathering for CO2 Removal
Published on: November 10, 2023
3.4K
09:38Single-throughput Complementary High-resolution Analytical Techniques for Characterizing Complex Natural Organic Matter Mixtures
Published on: January 7, 2019
8.6K
相关概念视频
The Carbon Cycle
37.6K
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.
37.6K
Global Climate Change
24.4K
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.
24.4K
The Sulfur Cycle
44.2K
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...
44.2K
The Calvin Benson Cycle
4.5K
Ribulose 1,5- bisphosphate carboxylase/oxygenase (RuBisCo) is a critical enzyme that catalyzes carbon dioxide assimilation during photosynthesis. However, it is an inefficient enzyme, having an extremely slow catalytic rate. A typical enzyme can process about a thousand molecules per second; however, RuBisCo fixes only around three-carbon dioxides per second. Photosynthetic cells compensate for this slow rate by synthesizing very high amounts of RuBisCo, making it the most abundant single...
4.5K
What are Biogeochemical Cycles?
31.9K
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
31.9K
What is Climate?
18.6K
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.
18.6K
