证据表明,在沉没的海洋颗粒中,有机物不被选择性地保存
J I Hedges1, J A Baldock, Y Gélinas
1School of Oceanography, University of Washington, Seattle 98195-7940, USA. jihedges@u.washington.edu
Nature
|March 10, 2001
概括
海洋碳捕获依赖于沉没的有机颗粒物. 尽管有广泛的生物降解,但类似氨基酸的材料仍然存在,这表明无机矩阵保护碳,而不是新的生物化学物质.
科学领域:
- 海洋有机地化学 海洋有机地化学
- 生物地质化学循环是什么
- 海洋的碳捕集方式
背景情况:
- 沉没的有机颗粒物将碳运送到海洋内部,影响大气中的CO2.
- 了解沉降颗粒的生物降解过程对于碳捕获至关重要.
- 现有的色谱技术限制了深度分析残留有机物成分的分析.
研究的目的:
- 在沉没粒子中描述有机碳的化学结构.
- 为了研究有机物质在通过海洋水柱运输过程中的命运.
- 确定控制有机碳颗粒物保存的机制.
主要方法:
- 使用了固态13C核磁共振 (NMR) 光谱学.
- 在表面浮游生物和沉降颗粒物中分析了有机碳成分.
- 从太平洋和阿拉伯海收集了样本.
主要成果:
- 尽管有超过98%的生物降解,但在散装有机成分中观察到的变化最小.
- 发现氨基酸类物质在整个水柱的有机物质中占主导地位.
- 剩余有机物质的化学成分与表面植物浮游生物质的生物质非常相似.
结论:
- 水柱中有机碳颗粒的保存主要不是由于异常生物化学物质的形成.
- 这些发现表明,沉没颗粒的无机矩阵可能会保护有机物质免受降解.
- 这对了解海洋碳捕获和气候调节具有重大意义.
更多相关视频
08:57VacuSIP, an Improved InEx Method for In Situ Measurement of Particulate and Dissolved Compounds Processed by Active Suspension Feeders
Published on: August 3, 2016
10.5K
09:01An Ultra-clean Multilayer Apparatus for Collecting Size Fractionated Marine Plankton and Suspended Particles
Published on: April 19, 2018
8.6K
相关概念视频
What are Biogeochemical Cycles?
31.0K
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.
31.0K
Comparative Excretory Systems
19.0K
Animals have evolved different strategies for excretion, the removal of waste from the body. Most waste must be dissolved in water to be excreted, so an animal’s excretory strategy directly affects its water balance.
19.0K
Deleterious Substances in Aggregate
867
Deleterious substances in aggregates can be detrimental to the quality and durability of concrete. These substances include organic impurities like loam, which interfere with cement hydration and are usually present in the sand. These prevent a good bond between aggregate and cement paste. Organic impurities can be detected using the colorimetric test, where the darkness of a solution after agitation indicates the level of organic content.
Another type of impurity is clay and fine material that...
Another type of impurity is clay and fine material that...
867
Marine Microbial Ecology
66
Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
66
Deep Sea Microbial Ecology
53
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches...
53
Freshwater Microbial Ecology
58
Freshwater systems such as streams, rivers, and lakes exhibit distinct physical and biological characteristics that influence their microbial communities. These environments are broadly categorized into lotic systems—those with flowing waters like streams and most rivers—and lentic systems, which include still or slow-moving waters such as lakes, ponds, and marshes.In lentic systems, phytoplankton drive primary production, generating autochthonous organic carbon. In contrast, lotic...
58
