Chronological control and centennial-scale climatic subdivisions of the Last Glacial Termination in the western Mediterranean region

Chronological control and centennial-scale climatic subdivisions of the Last Glacial Termination in the western Mediterranean region

The Last Glacial Termination is marked by changing environmental conditions affected by abrupt and rapid climate oscillations, such as Heinrich Stadial 1 (HS1), which is characterized by extremely low sea surface temperatures (SST) and significant changes in northern hemisphere terrestrial landscape...

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Bibliographic Details
Main Authors: Anderson, R.S (Author), Camuera, J. (Author), García-Alix, A. (Author), Jiménez-Espejo, F.J (Author), Jiménez-Moreno, G. (Author), Ramos-Román, M.J (Author), Toney, J.L (Author)
Format: Article
Language:English
Published: Elsevier Ltd 2021
Subjects:
Andalucia
Centennial scale variability
chronology
climate conditions
Climatology
environmental conditions
Environmental conditions
Glacial geology
Granada [Andalucia]
Heinrich event
Heinrich stadial 1
Iberian peninsula
Iberian Peninsula
land-sea interaction
Last glacial
Last Glacial Maximum
Last glacial terminations
Mediterranean region
Mediterranean Sea
Northern Hemisphere
Northern Hemispheres
Oceanography
Padul Basin
paleoclimate
Paleoclimate
pollen
Pollen analysis
sea surface temperature
Sea surface temperature (SST)
Solar activity
Spain
Surface waters
Terrestrial landscape
Western Mediterranean
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