软体动物中的碳储存:陆地生态系统中一个被忽视但重要的碳沉积点
Yajie Dong1, Naiqin Wu2, Fengjiang Li3
1Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing 100029, China.
The Science of the total environment
|January 13, 2024
概括
软体动物的贝显著储存碳,为中国的陆地碳汇贡献了1.68-2.71%. 这种外碳沉积至少持续了2万年,提供了大量的,被忽视的碳储存机制.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 生态生态学 生态生态学
背景情况:
- 软体动物构成了第二大动物类,在全球范围内居住在多样化的生态系统中.
- 软体动物的外是由碳酸组成的,碳酸是一个重要的碳沉.
- 陆地软体动物对碳捕获的定量贡献在很大程度上尚未评估.
研究的目的:
- 量化中国各种生态系统中现代陆地软体动物中的碳沉积量.
- 为了估计过去2万年来在软体动物中储存的历史碳流量.
- 评估软体动物外碳沉积在中国陆地碳预算中的重要性.
主要方法:
- 来自中国470个现代地表土壤地点的软体动物的实地采样.
- 地质统计分析以估计不同土地使用类型的外碳总沉积量.
- 分析了来自洛斯矿床的十多个化石序列,以重建过去的碳流.
主要成果:
- 中国的现代陆地软体动物表现出碳沉积率因生态系统而异,在落叶宽叶森林和灌木中,碳沉积率更高.
- 据估计,中国的外碳总沉积量在3.39-5.45 × 10^6 t C yr-1之间,占全国陆地碳汇的1.68-2.71%.
- 对沉积物的分析显示,在过去的2万年中,持续且大量的外碳沉积,全球估计达到1.29 × 10^9t C.
结论:
- 陆地软体动物的贝代表着一个重要的和历史上持久的碳汇.
- 这些发现突出了全球碳循环的一个被忽视的组成部分,这对于准确的气候建模至关重要.
- 软体动物的碳储存提供了一个与大规模植树努力相提并论的自然机制.
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
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
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
The Phosphorus Cycle
36.9K
Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
36.9K
Fats as Energy Storage Molecules
25.2K
Triglycerides are a form of long-term energy storage molecules. They are made of glycerol and three fatty acids. To obtain energy from fat, triglycerides must first be broken down by hydrolysis into their two principal components, fatty acids and glycerol. This process, called lipolysis, takes place in the cytoplasm. The resulting fatty acids are oxidized by β-oxidation into acetyl-CoA, which is used by the Krebs cycle. The glycerol that is released from triglycerides after lipolysis...
25.2K
Bioremediation
18.4K
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.
18.4K


