Revealing climatic variability of the last three millennia in northwestern Iberia using pollen influx data

Climatic variability of the last 3 millennia in NW Iberia has been documented using high-resolution pollen analysis of Vir-18 core. retrieved from the Ria de Vigo (42degrees14.07'N, 8degrees47.37'W). The depth-age model is based on two accelerator mass spectrometry C-14 dates and three his...

Full description

Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Desprat, S, Goni, MFS, Loutre, Marie-France
Other Authors: UCL
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science Bv 2003
Subjects:
pollen influx
NW Iberia
Galicia
Roman Warm Period
Medieval Warm Period
Little Ice Age
Dark Ages
human impact
palaeoclimate
North Atlantic
Online Access:http://hdl.handle.net/2078.1/40868
https://doi.org/10.1016/S0012-821X(03)00292-9
Description
Summary:Climatic variability of the last 3 millennia in NW Iberia has been documented using high-resolution pollen analysis of Vir-18 core. retrieved from the Ria de Vigo (42degrees14.07'N, 8degrees47.37'W). The depth-age model is based on two accelerator mass spectrometry C-14 dates and three historically dated botanical events in Galicia: the expansion of Juglans and Pinus, as well as the introduction of Eucalyptus. During the last 3000 years, the relative pollen record demonstrates the occurrence of an open deciduous oak forest, indicating a humid and temperate climate in northwestern Iberia. Two-step forest reduction since 975 cal BC suggests climate as the main cause rather than major socio-economic changes documented in historical archives. Absolute pollen influx has been compared with instrumental summer and winter temperatures and tentatively used as a proxy of short (decadal-scale) and low-amplitude (similar to 1degreesC) temperature variations. This new approach allows us to detect for the first time in NW Iberia the millennial-scale climatic cyclicity suggested by North Atlantic records, challenging the apparent climatic stability reflected by the relative pollen record. The Little Ice Age is recorded as low pollen influx values between 1400 and 1860 cal AD. with a cold maximum at 1700 cal AD (Maunder Minimum). The Roman and Medieval Warm Periods are detected through high pollen influx values at 250 cal BC-450 cal AD and 950-1400 cal AD, respectively. (C) 2003 Elsevier Science B.V. All rights reserved.

Similar Items