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The Carbon Cycle01:14

The Carbon Cycle

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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.
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Carbon Skeletons01:12

Carbon Skeletons

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Life on Earth is carbon-based, as all macromolecules that make up living organisms contain carbon atoms. All organic compounds have a carbon backbone. Each carbon atom is tetravalent and can bond with four other atoms, making it an extraordinarily flexible component of biological molecules. Because carbon’s valence electrons are stable, it rarely becomes an ion. As the carbon chain increases in length, structural modifications such as ring structures, double bonds, and branching side...
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Phase Transitions: Sublimation and Deposition02:33

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Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
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Sulfur Assimilation01:20

Sulfur Assimilation

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Sulfur is an essential element in biological systems, contributing to synthesizing key biomolecules, including amino acids such as cysteine and methionine, and cofactors such as coenzyme A and biotin. Microorganisms primarily assimilate sulfur as sulfate (SO₄²⁻) from the environment, which must undergo a series of biochemical transformations before it can be incorporated into cellular components. As sulfate is highly oxidized, it must undergo assimilatory sulfate reduction to...
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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...
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Cell Inclusions01:27

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Prokaryotic cells possess a variety of inclusions that play crucial roles in nutrient storage, metabolic processes, and environmental adaptation. These structures enable bacteria to thrive under fluctuating environmental conditions by storing essential resources and optimizing their metabolic efficiency.Carbon Storage: Poly-β-Hydroxybutyric Acid and Glycogen GranulesBacteria frequently store excess carbon in specialized granules. Poly-β-hydroxybutyric acid (PHB) granules are lipid...
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Updated: Jan 5, 2026

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
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El carbono de subducción

Terry Plank1, Craig E Manning2

  • 1Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA. tplank@ldeo.columbia.edu.

Nature
|October 18, 2019
PubMed
Resumen
Este resumen es generado por máquina.

La Tierra alberga un ciclo oculto de carbono donde megatones de carbono entran en zonas de subducción anualmente. Este proceso influye en los niveles de dióxido de carbono y oxígeno atmosféricos, impactando la historia geológica.

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Área de la Ciencia:

  • Geoquímica
  • Ciencias de la Tierra
  • Volcanología

Sus antecedentes:

  • Una cantidad significativa de carbono ingresa anualmente a las zonas de subducción de la Tierra.
  • Este carbono subducido influye en la composición atmosférica y el equilibrio de carbono a largo plazo de la Tierra.
  • Comprender el destino del carbono subducido es crucial para comprender los ciclos biogeoquímicos globales.

Objetivo del estudio:

  • Elucidar los procesos que rigen el movimiento y la transformación del carbono dentro de las zonas de subducción.
  • Investigar las fuentes y los mecanismos de reciclaje del dióxido de carbono emitido por los volcanes de arco.
  • Analizar la variabilidad global de la entrada de carbono y la remobilización en márgenes convergentes.

Principales métodos:

  • Revisión de los procesos geológicos implicados en el transporte de carbono a las zonas de subducción.
  • Análisis de la transformación del carbono subducido en fluidos, magmas, gases volcánicos y diamantes.
  • Examen de la composición de los gases volcánicos y su relación con los materiales subducidos.

Principales resultados:

  • El carbono entra en las zonas de subducción a través de microfósiles, materia orgánica y precipitados de carbonato.
  • Las emisiones de dióxido de carbono volcánico provienen principalmente de materiales subducidos reciclados.
  • La transformación y liberación de carbono varían significativamente en diferentes zonas de subducción a nivel mundial.

Conclusiones:

  • Las zonas de subducción actúan como conductos críticos para un ciclo de carbono oculto dentro de la Tierra.
  • El reciclaje de carbono subducido impacta significativamente los niveles de CO2 y O2 atmosféricos a lo largo de la historia de la Tierra.
  • Los márgenes convergentes sirven como laboratorios naturales para estudiar el complejo ciclo del carbono de subducción.