Advanced Search

Journal Navigation

Journal Home

Subscriptions

Archive

Contact Us

Table of Contents

Sign In to gain access to subscriptions and/or personal tools.
The Holocene
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Add to Saved Citations
Right arrow Download to citation manager
Right arrowRequest Permissions
Right arrow Request Reprints
Right arrow Add to My Marked Citations
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Right arrow Citing Articles via Scopus
Google Scholar
Right arrow Articles by Múgica, F. F.
Right arrow Articles by Ollerol, H. S.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Social Bookmarking
 Add to CiteULike   Add to Complore   Add to Connotea   Add to Del.icio.us   Add to Digg   Add to Reddit   Add to Technorati   Add to Twitter  
What's this?

The Holocene history of Pinnus forests in the Spanish Northern Meseta

Fáima Franco Múgica

Mercedes García Antón

Departamnento de Biología (Botanicla), Universidad Atutónoma de Madrid, 28049 Cantoblanco, Madrid, Spain

Javier Maldonado Ruiz

Carlos Morla Juaristi

Departamnento de Silvopascicultura, Escuela Tecnica Superior de Ingenieros de Montes, Universidad Politecnica de Madclidc, 28040 lac/rid, Spain

Helios Sainz Ollerol

Departamnento de Biologla (Botanicla), Universidad Atuto6no;na de M1adrid, 28049 Cantoblanco, Madrid, Spain

Pollen analysis from a 14.1 m core recoverecd from a vally mire at Espinosa de Cerrato (Palencia, Spain), suggests that Pinus woodland has dominated thils area of the Northern meseta throughout almost the entire Holocene in contrast to many other locations in lbetia where early-Holocene conifer woodland was progressively replaced by deciduous taxa. This unique pattern ofvegetationi developmenit is attributable to a combination of continental climate, edaphic condition of thesas. Mesetas. and perhaps fire. These data suggest that vegetation in this area has been remarkably stable over an extended timescale and that arguments aconcerning Pinus communities not being native in the region are unfounded. Anthropogenic impact can be detected at c. 4500 14C yr BP, affecting evergreen Quercus woodlands, and between c. 3000 and 2000 14C yr BP affecting Pinus woodlands. The pine forests were replaced by plant communities resembling the present-day landscape (shrubs and cereals) from c. 1500 14C yr BP.

Key Words: Pollen • palacovegetation • vegetationi history • Pious • Holocene • Northern Meseta • Spain

The Holocene, Vol. 11, No. 3, 343-358 (2001)
DOI: 10.1191/095968301669474913


Add to CiteULike CiteULike   Add to Complore Complore   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us   Add to Digg Digg   Add to Reddit Reddit   Add to Technorati Technorati   Add to Twitter Twitter    What's this?


This article has been cited by other articles:


Home page
The HoloceneHome page
M. B. Garzon, R. Sanchez de Dios, and H. Sainz Ollero
The evolution of the Pinus sylvestris L. area in the Iberian Peninsula from the last glacial maximum to 2100 under climate change
The Holocene, August 1, 2008; 18(5): 705 - 714.
[Abstract] [PDF]