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Mid-Holocene emergence of a low-frequency millennial oscillation in western Mediterranean climate

Implications for past dynamics of the North Atlantic atmospheric westerlies

Dados Bibliográficos

ID12266643
AutoresWilliam J Fletcher (0000-0001-8918-0690, EPHE, Université Bordeaux 1, France, autor correspondente), Maxime Debret (0000-0002-8852-0152, Université Joseph Fourier), Marı́a Fernanda Sánchez Goñi (0000-0001-8238-7488, Université de Bordeaux), María Fernanda Sánchez Goñi (EPHE, Université Bordeaux 1, France)
Ano2012
Volume23
Fascículo2
Páginas153-166
Data de publicação2012-10-26
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoThe Holocene (JOURNAL)
Identificadores do periódicoISSN: 0959-6836 • E-ISSN: 1477-0911
EditoraSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683612460783
OpenAlexW2062142674
IdiomaEN
Citações recebidas38
Referências citadas103

The nature and tempo of Holocene climate variability is examined in the record of forest vegetation from western Mediterranean marine core MD95-2043. Episodes of forest decline occurred at 10.1, 9.2, 8.3, 7.4, 5.4–4.5 and 3.7–2.9 cal. ka BP, and between 1.9 cal. ka BP and the top of the record (1.3 cal. ka BP). Wavelet analysis confirms a ~900 yr periodicity prior to and during the early Holocene and the dominance of a ~1750 yr periodicity after 6 cal. ka BP. The ~900 yr periodicity has counterparts in numerous North Atlantic and Northern Hemisphere palaeoclimate records, and in solar irradiance proxies (Δ 14 C and 10 Be), and may relate to a Sun–climate connection during the early Holocene. Comparisons between the MD95-2043 forest record and strategically located records from Morocco, Iceland, Norway and Israel suggest that the ~1750 yr mid- to late-Holocene oscillation reflects shifts between a prevailing strong and weak state of the zonal flow, with impacts similar to the positive and negative modes of the present-day North Atlantic Oscillation (NAO). The mid- to late-Holocene millennial oscillation in zonal flow appears closely coupled to North Atlantic surface ocean circulation dynamics, and may have been driven by an internal oscillation in deep-water convection strength. The findings suggest that the mid-Holocene transition in western Mediterranean climate was accompanied by a shift in the fundamental tempo of millennial-scale variability, reflecting contrasting sensitivity of the North Atlantic climate system to different forcing factors (solar versus oceanic) under deglacial and fully interglacial conditions

Atlantic multidecadal oscillation · Atmospheric Circulation · Climate change · Climatology · Foraminifera · Geography · Holocene · Holocene climatic optimum · Mediterranean climate · North Atlantic oscillation · Northern Hemisphere · Paleoclimatology · Westerlies · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Geology · Oceanography

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