Macrorremains evidence of anthropogenic recession of Pinus nigra Aiton in Northern Spain

Garcia-Amorena Gomez del Moral, Ignacio; Moreno Amat, Elena; Iglesias Gonzalez, Raul; Rubiales Jimenez, Juan Manuel y Gómez Manzaneque, Fernando (2010). Macrorremains evidence of anthropogenic recession of Pinus nigra Aiton in Northern Spain. En: "8th European Palaeobotany-Palynology Conference Program and Abstracts Volume", 06/07/2010 - 10/07/2010, Budapest, Hungría.

Descripción

Título: Macrorremains evidence of anthropogenic recession of Pinus nigra Aiton in Northern Spain
Autor/es:
  • Garcia-Amorena Gomez del Moral, Ignacio
  • Moreno Amat, Elena
  • Iglesias Gonzalez, Raul
  • Rubiales Jimenez, Juan Manuel
  • Gómez Manzaneque, Fernando
Tipo de Documento: Ponencia en Congreso o Jornada (Póster)
Título del Evento: 8th European Palaeobotany-Palynology Conference Program and Abstracts Volume
Fechas del Evento: 06/07/2010 - 10/07/2010
Lugar del Evento: Budapest, Hungría
Título del Libro: Proceedings of the 8th European Palaeobotany-Palynology Conference
Fecha: 2010
Materias:
Escuela: E.T.S.I. Montes (UPM) [antigua denominación]
Departamento: Silvopascicultura [hasta 2014]
Licencias Creative Commons: Reconocimiento - Sin obra derivada - No comercial

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Resumen

The natural forest landscape of the Duero Basin in Spain¿s Northern Meseta is now reduced to small masses, its demise largely owed to the intense agricultural and stock-raising use made of its lands. The composition of the scant natural masses suggests that formations dominated by broadleaved species once occupied a much greater area. This idea has led to the believe that pine trees have few place within the natural dynamics of this area (Carrión and Fernández, 2009). However, P. pinaster Aiton and P.pinea L. on low-land sandy areas, P. sylvestris L. and P.uncinata Ramond ex DC on mountain high areas have been demonstrated to have played an important role during the Holocene (Franco et al., 2005; Rubiales et al., 2010). The abundant plant remains and moulds of pine wood and cones found on Northern Meseta peat bogs and travertines, now demonstrate its presence on mid-lands during the Quaternary until the last millennia

Más información

ID de Registro: 7969
Identificador DC: http://oa.upm.es/7969/
Identificador OAI: oai:oa.upm.es:7969
URL Oficial: http://www.eppc2010.org/index.php
Depositado por: Memoria Investigacion
Depositado el: 12 Jul 2011 11:14
Ultima Modificación: 20 Abr 2016 16:53
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