Environmental and climate change in the southern Central Pyrenees since the Last Glacial Maximum: A view from the lake records

In this contribution we compile and summarize the available paleo-environmental lacustrine data for the last 20,000 years from the southern Central Pyrenees (from west to east: El Portalet, Tramacastilla, Basa de la Mora, Estanya, Redon, Montcortès and Marcelino lakes) and present a new sequence fro...

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Detalles Bibliográficos
Autores: González Sampériz, Penélope, Aranbarri Erkiaga, Josu, Pérez Sanz, Ana, Gil Romera, Graciela, Moreno, Ana, Leunda Esnaola, María, Sevilla Callejo, Miguel, Corella, Juan Pablo, Morellón Marteles, Mario, Oliva Urcia, Belén, Valero Garcés, Blas
Tipo de recurso: artículo
Fecha de publicación:2017
País:España
Institución:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:inglés
OAI Identifier:oai:docta.ucm.es:20.500.14352/96277
Acceso en línea:https://hdl.handle.net/20.500.14352/96277
Access Level:acceso abierto
Palabra clave:556.55(234.12)
Central Pyrenees
Long-term geoecological evolution
Lacustrine sequences
Climate changes
Human impact
Geología estratigráfica
2502.07-1 Climatología Regional. Montaña
2508.08 Limnología
Descripción
Sumario:In this contribution we compile and summarize the available paleo-environmental lacustrine data for the last 20,000 years from the southern Central Pyrenees (from west to east: El Portalet, Tramacastilla, Basa de la Mora, Estanya, Redon, Montcortès and Marcelino lakes) and present a new sequence from mid altitude (Holocene record of Lake Estanya). Multiproxy analyses of lake records have identified large vegetation and hydrological changes during last glacial, deglaciation and the Holocene periods at millennial, centennial and even decadal scales and documented their timing, intensity and varied nature. The review indicates that landscape dynamics in the Pyrenees have been greatly controlled by both long term and abrupt climate changes and, since the Middle Holocene, and particularly since Medieval times, by human activities as new transforming agent. Although high internal variability characterized every site, common temporal trends are evidenced, as well as a suggestive western–eastern gradient superimposed to the expected altitudinal one (highlands versus lowlands). Thus, the long-term Central Pyrenees environmental history presents a relatively high degree of internal coherence across space and provides some past scenarios of landscape-climate interactions to evaluate the expected impacts of current and future Global Change.