Video Experimental Relacionado
Updated: Jun 18, 2026

11:10
Conducting Miller-Urey Experiments
Published on: January 21, 2014
Polvo de cometa como fuente de aminoácidos en el límite Cretácico / Terciario
1NASA Ames Research Center, Moffett Field, California 94035, USA.
Nature
|November 8, 1990
Resumen
Los aminoácidos extraterrestres encontrados cerca de la frontera Cretácico / Terciario (K / T) sugieren la deposición de polvo de cometa, no el impacto. Esta teoría explica su presencia por encima y por debajo de la capa límite, y su ausencia en la arcilla de impacto en sí.
Área de la Ciencia:
- Astrobiología Astrobiología.
- La geoquímica es la geoquímica.
- Paleontología Paleontología.
Sus antecedentes:
- Aminoácidos extraterrestres detectados en el límite Cretácico / Terciario (K / T) en Stevns Klint, Dinamarca.
- Aminoácidos que se encuentran en las capas por encima y por debajo de la arcilla límite, pero no dentro de ella.
Objetivo del estudio:
- Investigar el origen y el mecanismo de deposición de aminoácidos extraterrestres en el límite K/T.
- Para conciliar la presencia de aminoácidos con el evento de impacto K/T.
Principales métodos:
- Análisis geoquímico de muestras de roca del límite K/T.
- Comparación de la distribución de aminoácidos con modelos de impacto y de deposición de polvo cometario.
Principales resultados:
- Los aminoácidos están ausentes en la arcilla límite K / T, lo que dificulta la entrega de impactos.
- La presencia de aminoácidos en las capas que flanquean el límite sugiere deposición independiente del evento de impacto principal.
Conclusiones:
- Los aminoácidos extraterrestres en el límite K / T probablemente se originaron del polvo de cometa.
- El polvo cometario, no el propio impactador, entregó estas moléculas prebióticas a la Tierra antes y después del evento de impacto.
Videos de Conceptos Relacionados
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Conditions on Early Earth
Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Overview of Nitrogen Metabolism
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 nitrogen...
The largest pool of nitrogen available in the terrestrial ecosystem is gaseous nitrogen (N2) from the air, but this nitrogen...
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...
Amino Acid Biosynthetic Pathways
Amino acid biosynthesis is essential for cell growth, protein synthesis, and metabolic regulation. Cells generate essential and non-essential amino acids from metabolic intermediates to sustain vital biological functions. These intermediates originate from key metabolic pathways: glycolysis, the tricarboxylic acid (TCA) cycle, and the pentose phosphate pathway. Important precursors include α-ketoglutarate, pyruvate, oxaloacetate, phosphoenolpyruvate, and erythrose-4-phosphate, which provide...
Microbes and Climate Change
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...

