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Primeros resultados palinológicos de la base de la secuencia sedimentaria de la laguna del cañizar de villarquemado

Primeros resultados palinológicos de la base de la secuencia sedimentaria de la laguna del cañizar de villarquemado

          
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About the Book

Tesis de Máster del año 2011 en eltema Geología / Geografía - Meteorología, Aeronomía, Climatología, Nota: 9,0, Materia: Máster de iniciación a la investigación en Geología, Idioma: Español, Resumen: Estudiar la dinámica de la vegetación frente a las fluctuaciones climáticas del comienzo y terminación de los periodos interglaciares, como el que vivimos actualmente, nos ayudará a comprender mejor la respuesta a los cambios que puedan acontecer en el futuro. . El anterior periodo interglaciar (MIS 5), se considera más cálido y húmedo que el actual (MIS1-Holoceno), manifestando una expansión forestal similar en su comienzo. Este trabajo intenta caracterizar las formaciones vegetales durante parte del MIS 5 en la secuencia del Cañizar de Villarquemado (74m de largo, 120 ka BP), complementando un estudio multiproxy previamente realizado. Para ello se realizó un análisis palinológico de nueve muestras de los seis metros inferiores del registro. Los resultados obtenidos no reflejan las expansiones forestales mesófitas registradas en otras secuencias Europeas durante esta fase. Al contrario, la base de la secuencia del Cañizar manifiesta un paisaje abierto con presencia de escasos pinos y abundantes Juniperus, Artemisia, Chenopodiaceae y Poaceae. Sin embargo, se observa un incremento del polen arbóreo a partir de 67.5m hacia niveles superiores del registro, unido a la presencia de taxones termófilos arbóreoarbustivos y cierta disminución de Artemisia y Chenopodiadiaceae. Estos espectros se corresponden también con un cambio de facies, de limos grises a limos laminados, y un aumento de Typha y Botryococcus, interpretándose como una tendencia hacia un incremento de temperatura y mejora en las condiciones de humedad). Estos resultados, y considerando el rango de error en las dataciones OSL, hacen pensar que los niveles analizados pueden corresponderse con el final del periodo glaciar Riss (MIS 6). Frente a estos primeros resultados, se necesita mayor número de muestras ana


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Product Details
  • ISBN-13: 9783346091369
  • Publisher: Grin Verlag
  • Publisher Imprint: Grin Verlag
  • Height: 210 mm
  • No of Pages: 62
  • Spine Width: 4 mm
  • Width: 148 mm
  • ISBN-10: 3346091368
  • Publisher Date: 18 Nov 2019
  • Binding: Paperback
  • Language: Spanish
  • Returnable: N
  • Weight: 91 gr


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