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Freshwater Microbial Ecology01:24

Freshwater Microbial Ecology

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 systems...
Inorganic Nitrogen Assimilation01:22

Inorganic Nitrogen Assimilation

Nitrogen is an essential element in biological systems, forming a crucial component of proteins, nucleic acids, and other cellular constituents. Many bacteria and archaea acquire nitrogen in the form of nitrate (NO₃⁻) or ammonia (NH₃), which are then assimilated into biomolecules through specific enzymatic pathways.Assimilatory Nitrate ReductionWhen nitrate enters the cell, it undergoes a two-step reduction process known as assimilatory nitrate reduction. Initially, the enzyme nitrate reductase...
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Microbes and the Nitrogen Cycle

The nitrogen cycle is a complex biogeochemical process critical to maintaining the balance of nitrogenous compounds in ecosystems. This cycle involves multiple microbial-mediated transformations through which nitrogen changes oxidation states, supporting essential ecological functions and contributing to plant and microbial growth.Nitrogen Fixation and AmmonificationNitrogen fixation initiates the cycle by converting inert atmospheric nitrogen (N₂) into bioavailable ammonia (NH₃), a process...
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The Nitrogen Cycle

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Carbon-dioxide Fixation

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Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential
14:38

Establishment of Microbial Eukaryotic Enrichment Cultures from a Chemically Stratified Antarctic Lake and Assessment of Carbon Fixation Potential

Published on: April 20, 2012

在湖泊中的固定.

R Dugdale, V Dugdale, J Neess

    Science (New York, N.Y.)
    |October 2, 1959
    PubMed
    概括

    这项研究测量了自然湖中的固化,使用N(15) 同位素追踪. 结果显示,在各种湖泊生态系统中,固率显著.

    科学领域:

    • 环境科学 环境科学
    • 临界技术 临界技术
    • 生物地质化学生物地质化学

    背景情况:

    • 是水生生态系统的关键营养素.
    • 估计固速率对于了解湖泊的生产力至关重要.
    • 天然湖水是复杂的环境,具有不同的动态.

    研究的目的:

    • 在自然湖水中量化初级固速率.
    • 为了评估固定在不同地理位置的变化.
    • 建立N(15) 纳入作为估计固化的方法.

    主要方法:

    • 使用稳定的同位素N(15) 来追踪的结合.
    • 在宾夕法尼亚州的皮马图宁水库,威斯康星州的门多塔湖和阿拉斯加的两个湖泊进行了实验.
    • 测量了N(15) 加入到有机颗粒分数中的含量.

    主要成果:

    • 在所有研究的湖泊中证明了可测量的固率.
    • 观察到有时高固定率,表明显著的生物活性.
    • ) 加入证明有效量化固定.

    结论:

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  • 在自然湖水中,初级固发生的速度很大.
  • 地理位置和湖泊特征影响固速率.
  • (15) 方法为评估水生系统中循环提供了一种可靠的方法.