Video Experimental Relacionado
Updated: Mar 20, 2026

09:06
Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
Published on: July 3, 2016
8.7K
Una edad de hielo registrada en los depósitos polares de Marte
Isaac B Smith1, Nathaniel E Putzig2, John W Holt3
1Department of Space Studies, Southwest Research Institute, Boulder, CO 80302, USA. isaac@boulder.swri.edu.
Resumen
Marte también.
Área de la Ciencia:
- Ciencias planetarias
- Ciencias del clima
- Geología
Sus antecedentes:
- Los depósitos de hielo polar en Marte preservan un registro del cambio climático.
- Los datos de radar revelan estructuras de hielo en capas indicativas de procesos climáticos pasados.
Objetivo del estudio:
- Para analizar los datos de observación de la acumulación de hielo polar en Marte.
- Comprender la historia de la acumulación de hielo y su relación con los ciclos climáticos.
Principales métodos:
- Análisis detallado de los datos de observación de radar de los polos marcianos.
- Cuantificación del volumen de hielo acumulado desde la última glaciación.
Principales resultados:
- Aproximadamente 87.000 kilómetros cúbicos de hielo se han acumulado en los polos marcianos en los últimos 370.000 años.
- Este volumen de hielo es equivalente a una capa global de ~ 60 centímetros.
- La mayoría del hielo acumulado se encuentra en el Polo Norte.
Conclusiones:
- El hielo polar marciano registra la historia del clima vinculada a los ciclos orbitales.
- Los resultados proporcionan restricciones para modelar climas marcianos pasados y futuros.
Videos de Conceptos Relacionados
Global Climate Change
29.6K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
29.6K
The Fossil Record
28.3K
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
28.3K
Conditions on Early Earth
103.0K
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.
103.0K
Conditions on Early Earth
2.9K
2.9K
Microbes and Climate Change
2
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...
2
The Carbon Cycle
45.4K
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.
45.4K

