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Inorganic Nitrogen Assimilation01:22

Inorganic Nitrogen Assimilation

372
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...
372
Carbon-dioxide Fixation01:28

Carbon-dioxide Fixation

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Carbon dioxide fixation in prokaryotes enables the assimilation of inorganic carbon into organic molecules, supporting biosynthetic pathways, sustaining ecosystems, and contributing to the global carbon cycle. It also has industrial applications in carbon capture and bioproduct synthesis. Autotrophic organisms rely on this process to utilize CO₂ as a carbon source in diverse environments.The Calvin CycleThe Calvin cycle is the most widespread carbon fixation mechanism, primarily used by...
501
Metabolism of Chemolithotrophs01:15

Metabolism of Chemolithotrophs

622
Chemolithotrophs are microorganisms that obtain energy by oxidizing inorganic molecules such as hydrogen gas (H₂), ammonia (NH₃), reduced sulfur compounds (H₂S, S²⁻), and ferrous iron (Fe²⁺). Unlike heterotrophic organisms that rely on organic carbon, chemolithotrophs transfer electrons from these inorganic donors to the electron transport chain (ETC), generating a proton motive force (PMF) that drives ATP synthesis through oxidative phosphorylation.
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Overview of Nitrogen Metabolism01:20

Overview of Nitrogen Metabolism

10.8K
Nitrogen is a very important element for life because it is a major constituent of proteins and nucleic acids. It is a macronutrient, and in nature, it is recycled from organic compounds and stored in the form of  ammonia, ammonium ions, nitrate, nitrite, or  nitrogen gas by many metabolic processes. Many of these metabolic processes are carried out only by prokaryotes.
The largest pool of nitrogen available in the terrestrial ecosystem is gaseous nitrogen (N2) from the air, but this...
10.8K
The Nitrogen Cycle01:49

The Nitrogen Cycle

59.2K
Nitrogen atoms, present in all proteins and DNA, are recycled between abiotic and biotic components of the ecosystem. However, the primary form of nitrogen on Earth is nitrogen gas, which cannot be used by most animals and plants. Thus, nitrogen gas must first be converted into a usable form by nitrogen-fixing bacteria before it can be cycled through other living organisms. The use of nitrogen-containing fertilizers and animal waste products in human agriculture has greatly influenced the...
59.2K
Overview of Metabolism01:40

Overview of Metabolism

37.3K
Living cells constantly carry out various chemical reactions which are necessary for their proper functioning. These reactions are interlinked to one another via multiple pathways. The collection of these chemical reactions is known as metabolism.
Plant Metabolism
Sunlight, the primary source of energy in plants, is first absorbed by the chlorophyll pigments present in their leaves. Plants then use this energy to carry out photosynthesis, where water is oxidized into oxygen and carbon dioxide...
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Video Experimental Relacionado

Updated: Dec 21, 2025

Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
08:05

Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O

Published on: October 7, 2020

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Perspectivas cambiantes en la fijación de nitrógeno marino

Jonathan P Zehr1, Douglas G Capone2

  • 1Department of Ocean Sciences, University of California, Santa Cruz, CA 95003, USA. zehrj@ucsc.edu capone@usc.edu.

Science (New York, N.Y.)
|May 16, 2020
PubMed
Resumen
Este resumen es generado por máquina.

La fijación de nitrógeno marino, que convierte el nitrógeno atmosférico (N2O) en amoníaco, es vital para la vida en el océano. Una nueva investigación revela diversos microbios y adaptaciones, transformando nuestra comprensión de este proceso crucial en el ciclo global del nitrógeno.

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Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
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Prospecting Microbial Strains for Bioremediation and Probiotics Development for Metaorganism Research and Preservation
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Área de la Ciencia:

  • Biología marina
  • Biogeoquímica
  • Ecología microbiana

Sus antecedentes:

  • La fijación de nitrógeno (N2 al amoníaco) es esencial para la productividad marina, pero es difícil de estudiar.
  • Los avances recientes integran técnicas moleculares, genómicas, isotópicas y de modelado.
  • Esto ha revelado nuevos diazotrofos y adaptaciones fisiológicas en el océano.

Objetivo del estudio:

  • Para revolucionar la comprensión de la fijación de nitrógeno marino.
  • Explorar el papel de los diazotróficos en el ciclo global del nitrógeno.
  • Investigar el impacto de los cambios antropogénicos en la fijación marina de nitrógeno.

Principales métodos:

  • Estudios de campo durante décadas.
  • Análisis biológicos y genómicos moleculares.
  • Medidas isotópicas y modelado geoquímico.
  • El análisis de patrones biogeográficos.

Principales resultados:

  • Descubrimiento de microorganismos diazotróficos previamente desconocidos.
  • Identificación de adaptaciones fisiológicas inusuales en los microbios marinos.
  • Caracterización de las distribuciones de nutrientes e isótopos.
  • Los patrones biogeográficos revelados de la fijación de N2.

Conclusiones:

  • La fijación de nitrógeno marino es más compleja y diversa de lo que se pensaba anteriormente.
  • Los diazotróficos juegan un papel crítico en el ciclo global del nitrógeno.
  • El calentamiento de los océanos, el aumento de CO2 y la acidificación alterarán la dinámica de fijación de N2, lo que afectará a las redes alimentarias y los ciclos biogeoquímicos.