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Updated: Jul 12, 2026

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Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
Published on: July 3, 2016
Variaciones vegetacionales y climáticas del Mioceno tardío inferidas de un registro de polen en el noroeste de
Resumen
El análisis del polen de los depósitos de lagos del Mioceno tardío en Wyoming revela una flora similar a la moderna y climas húmedos / secos alternados. Este registro de alta resolución muestra cambios climáticos similares a los registros marinos de los períodos Terciario y Cuaternario tardíos.
Área de la Ciencia:
- La paleobotánica es la paleobotánica.
- Ciencias del clima Ciencias del clima Ciencias del clima Ciencias del clima
- La estratigrafía es la estratigrafía.
Sus antecedentes:
- Los depósitos terciarios terrestres a menudo carecen de una alta resolución temporal para la historia de la vegetación y el clima.
- Los estratos lacustrinos ofrecen potencial para reconstrucciones paleoambientales detalladas.
Objetivo del estudio:
- Para analizar la vegetación y la historia del clima del Mioceno tardío utilizando la estratigrafía del polen.
- Para lograr una mayor resolución temporal de lo que se informó anteriormente de los depósitos terciarios terrestres.
Principales métodos:
- Análisis del polen de los estratos lacustre de la Formación Teewinot en Jackson Hole, Wyoming.
- Análisis estratigráfico de depósitos del Mioceno tardío.
Principales resultados:
- La flora identificada fue esencialmente moderna.
- Seis ensamblajes sucesivos de polen indican condiciones climáticas alternas secas y húmedas.
- La frecuencia del cambio climático es comparable a los registros de isótopos marinos.
Conclusiones:
- La estratigrafía del polen de los depósitos lacustres proporciona información de alta resolución sobre la vegetación y el clima del Mioceno tardío.
- El Mioceno tardío experimentó frecuentes fluctuaciones climáticas, similares a los períodos geológicos posteriores.
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