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Medium Preparation for the Cultivation of Microorganisms under Strictly Anaerobic/Anoxic Conditions
Published on: August 15, 2019
Lípidos polares de arquebacterias en sedimentos y petróleos
Resumen
Los tetraéteres de glicerol, comunes en las arquebacterias, se encontraron en sedimentos y petróleo. Estos lípidos microbianos sobreviven a los procesos geológicos, lo que indica un origen microbiano significativo para la materia orgánica geológica.
Área de la Ciencia:
- La geoquímica es la geoquímica.
- Microbiología Microbiología.
- La geoquímica orgánica es la geoquímica orgánica.
Sus antecedentes:
- Las arquebacterias poseen lípidos de membrana únicos, incluidos los tetraéteres de glicerol con cadenas isoprenoides de 40 carbonos.
- Estos lípidos son característicos de grupos microbianos específicos como los metanógenos.
- Comprender el destino de los lípidos microbianos en entornos geológicos es crucial para interpretar la historia de la Tierra.
Objetivo del estudio:
- Para identificar y caracterizar los tetraéteres de glicerol en muestras sedimentarias y de petróleo.
- Para determinar el potencial de preservación de estos lípidos arqueal en entornos subterráneos.
- Proporcionar evidencia del origen microbiano de la materia orgánica geológica.
Principales métodos:
- Análisis de lípidos polares extraídos de sedimentos y petróleos.
- Identificación de estructuras específicas de tetraéter de glicerol utilizando técnicas analíticas avanzadas (por ejemplo, espectrometría de masas).
Principales resultados:
- Los tetraéteres de glicerol con cadenas de 40 carbonos isoprenoides cabeza a cabeza, típicas de las Archaebacteria, se identificaron tanto en sedimentos como en petróleos.
- Se encontró que estos lípidos arqueales se conservan en muestras subterráneas, que se extienden más allá de la etapa de formación del petróleo.
- La presencia de estos lípidos intactos apoya su papel como biomarcadores.
Conclusiones:
- La identificación de los tetraéteres de glicerol conservados confirma su origen en las membranas celulares microbianas.
- Estos hallazgos proporcionan una fuerte evidencia de que una parte sustancial de la materia orgánica geológica se origina en microorganismos.
- Los tetraéteres de glicerol sirven como indicadores confiables de la actividad microbiana en entornos geológicos antiguos y modernos.
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