在黄色海中沉积的空气中的有机物质的分子水平组成和来源
Haryun Kim1, Kyoung-Soon Jang2, Tae-Wook Kim3
1Korea Institute of Ocean Science & Technology, Busan, 49111, Republic of Korea; University of Science & Technology, Daejeon, 34113, Republic of Korea.
Marine pollution bulletin
|October 31, 2025
概括
黄海空气中的有机物显示出区域成分的差异,影响了海洋的碳循环. 离岸沉积物更不稳定,而沿海沉积物更反抗,影响微生物的可用性和碳动态.
科学领域:
- 海洋化学 海洋化学
- 大气科学 大气科学
- 生物地质化学生物地质化学
背景情况:
- 空气中的有机物 (OM) 在海洋生物地球化学循环中起着至关重要的作用.
- 了解空气中的OM的分子组成对于预测其命运和对海洋环境的影响至关重要.
- 黄海是一个边缘海洋,受到各种陆地和海洋来源的影响,这使得它成为研究空中OM沉积的关键区域.
研究的目的:
- 为了分析空气中的有机物质 (OM) 的分子组成,这些有机物质沉积在黄海的近海和近海地区.
- 为了比较这两个不同的区域之间的空中OM的组成和来源.
- 评估空气中的OM成分区域差异对微生物利用和海洋碳循环的影响.
主要方法:
- 福利埃变换离子循环子共振质谱法 (FT-ICR MS) 用于确定空中OM的详细分子组成.
- 从黄海的近海和近海沉积区采集了样本.
- 化学表征的重点是识别OM中的反复性,可变性和人为性化合物.
主要成果:
- 海上空气中的OM主要是由来自陆地来源 (亚洲尘埃,河流排水,生物质燃烧) 的反抗性树脂素/树脂素化合物组成的.
- 来自海洋浮游生物的性蛋白质/碳水化合物类化合物是离岸的第二大部分,来源于海喷气气溶.
- 岸内地区显示出相似的反抗性和不稳定性OM比例,这两个地区都含有人为衍生的缩芳香/不和碳化合物类OM.
结论:
- 空气中的OM成分的区域差异影响其对海洋微生物和初级生产者的生物可用性.
- 与海上OM相比,内陆空气中的OM可能降解程度较低,并在水柱中持续更长时间.
- 该研究强调了陆地和海洋来源在塑造空气中的OM中的复杂相互作用,以及其在边际海洋碳循环和长期碳动态中的重要作用.
相关概念视频
The Sulfur Cycle
51.7K
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...
51.7K
What are Biogeochemical Cycles?
39.1K
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.
39.1K
The Carbon Cycle
43.1K
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.
43.1K
The Soil Ecosystem
24.4K
Plants obtain inorganic minerals and water from the soil, which acts as a natural medium for land plants. The composition and quality of soil depend not only on the chemical constituents but also on the presence of living organisms. In general, soils contain three major components:
24.4K


