受藻类生物质影响的湖泊沉积物中的循环机制
Yifan Ding1, Hanyue Yang2, Chao Li1
1Department of Chemistry and Environmental Science, New Jersey Institute of Technology, Newark, NJ, 07103, USA.
Journal of environmental management
|February 5, 2026
概括
来自的藻类生物质显著增加了从湖泊沉积物释放的,通过促进微生物活动和有机物分解. 这项研究揭示了蓝藻细菌的碎片如何驱动内部循环,影响过度化的管理.
科学领域:
- 环境微生物学 环境微生物学
- 地质化学 地质化学
- 水生生态学 水生生态学
背景情况:
- 藻类的繁殖,由优化驱动,导致水生系统的生态问题.
- 了解沉积物中的 (P) 循环对于管理缩至关重要.
研究的目的:
- 研究藻类生物质 (Lyngbya) 在无氧条件下如何影响湖泊沉积物中的转化.
- 评估蓝藻细菌碎片对沉积物P池和微生物群落的影响.
主要方法:
- 微观宇宙实验,使用不同的Lyngbya生物质负载.
- 顺序提取用于池分析.
- 16S rRNA基因测序用于微生物社区的表征.
- 溶液31P的NMR和沉积物的化学分析.
主要成果:
- 增加的藻类生物量增强了P溶解和矿化,增加了总可提取的P.
- 从矿物质结合的P转变为具有较高生物质的不稳定形式.
- 微生物群落转向了Firmicutes,无氧发酵剂和Fe (III) 降解剂.
- 有证据表明,铁矿物质的还原性溶解和提高有机P周转率.
结论:
- 藻类碎片显著改变沉积物P动态,促进P的释放.
- 由藻类生物量驱动的微生物代谢转变增强了P溶解.
- 结果提供了对内部P循环的洞察力,这对于安化管理策略至关重要.
相关概念视频
The Phosphorus Cycle
44.0K
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.
44.0K
The Water Cycle
28.7K
The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
28.7K
The Sulfur Cycle
52.0K
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...
52.0K
The Carbon Cycle
43.9K
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.
43.9K
Chirality at Nitrogen, Phosphorus, and Sulfur
7.0K
Chirality is most prevalent in carbon-based tetrahedral compounds, but this important facet of molecular symmetry extends to sp3-hybridized nitrogen, phosphorus and sulfur centers, including trivalent molecules with lone pairs. Here, the lone pair behaves as a functional group in addition to the other three substituents to form an analogous tetrahedral center that can be chiral.
A consequence of chirality is the need for enantiomeric resolution. While this is theoretically possible for all...
A consequence of chirality is the need for enantiomeric resolution. While this is theoretically possible for all...
7.0K
What are Biogeochemical Cycles?
39.6K
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.
39.6K


