2016/11/01 by Dulce Oliveira, Stéphanie Desprat, Stephanie Desprat +14 · 81 citations
Earth and Planetary Sciences · #Archaeology and ancient environmental studies #Atlantic multidecadal oscillation #Climate change #Climate model #Climatology #Geology #Geology and Paleoclimatology Research #North Atlantic oscillation #Oceanography #Paleoclimatology #Sea surface temperature #Tree-ring climate responses #Vegetation (pathology)
paper · doi:10.1016/j.yqres.2016.09.002
published in Quaternary Research 86(3), 373-387 (Cambridge University Press)
openalex publication_date 2016/11/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/30
Abstract Climatic variability of Marine Isotope Stage (MIS) 11 is examined using a new high-resolution direct land—sea comparison from the SW Iberian margin Site U1385. This study, based on pollen and biomarker analyses, documents regional vegetation, terrestrial climate and sea surface temperature (SST) variability. Suborbital climate variability is revealed by a series of forest decline events suggesting repeated cooling and drying episodes in SW Iberia throughout MIS 11. Only the most severe events on land are coeval with SST decreases, under larger ice volume conditions. Our study shows that the diverse expression (magnitude, character and duration) of the millennial-scale cooling events in SW Europe relies on atmospheric and oceanic processes whose predominant role likely depends on baseline climate states. Repeated atmospheric shifts recalling the positive North Atlantic Oscillation mode, inducing dryness in SW Iberia without systematical SST changes, would prevail during low ice volume conditions. In contrast, disruption of the Atlantic meridional overturning circulation (AMOC), related to iceberg discharges, colder SST and increased hydrological regime, would be responsible for the coldest and driest episodes of prolonged duration in SW Europe.