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The 4.2 ka BP Event in the Mediterranean region

An overview

Bibliographic Data

ID23327571
AuthorsMonica Bini (0000-0003-1482-2630, University of Pisa, corresponding author), Giovanni Zanchetta (0000-0002-7080-9599, University of Pisa), Aurel Perşoiu (0000-0001-9506-0070, Emil Racovita Institute of Speleology), Rosine Cartier (0000-0002-7448-2693, Lund University), Albert Català (0000-0001-9967-6120, Universitat de Barcelona), Isabel Cacho (0000-0002-6512-0770, Universitat de Barcelona), Jonathan R Dean (0000-0001-8071-000X, University of Hull), Federico Di Rita (0000-0002-3065-8474, Sapienza University of Rome), Russell N Drysdale (0000-0001-7867-031X, The University of Melbourne), Martin Finné (0000-0001-7433-268X, Uppsala University), Ilaria Isola (0000-0002-3911-4676, Istituto Nazionale di Geofisica e Vulcanologia), Bassem Jalali (0000-0002-4171-1664, Centre National de la Recherche Scientifique), Fabrizio Lirer (0000-0003-4938-3252, Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche), Donatella Magri (0000-0001-7254-593X, Sapienza University of Rome), Alessia Masi (0000-0001-9822-9767, Sapienza University of Rome), Leszek Marks (0000-0002-4507-1828, University of Warsaw), Anna Maria Mercuri (0000-0001-6138-4165, University of Modena and Reggio Emilia), Odile Peyron (0000-0002-7028-6302, Université de Montpellier), Laura Sadori (0000-0002-2774-6705, Sapienza University of Rome), Marie-Alexandrine Sicre (0000-0002-5015-1400, Centre National de la Recherche Scientifique), Fabian Welc (0000-0001-6122-1884, Cardinal Stefan Wyszynski University in Warsaw), Christoph Zielhofer (0000-0001-9551-4466, Leipzig University), E Brisset (0000-0001-8706-0505, Institut Català de Paleoecologia Humana i Evolució Social)
Year2019
Volume15
Issue2
Pages555-577
Publication date2019-03-27
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueClimate of the Past (JOURNAL)
Journal identifiersISSN: 1814-9324 • E-ISSN: 1814-9332
PublisherCopernicus GmbH (PUBLISHER • DE)
DOI10.5194/cp-15-555-2019
OpenAlexW2901500389
LanguageEN
Citations received65
References cited181

The Mediterranean region and the Levant have returned some of the clearest evidence of a climatically dry period occurring around 4200 years ago. However, some regional evidence is controversial and contradictory, and issues remain regarding timing, progression, and regional articulation of this event. In this paper, we review the evidence from selected proxies (sea-surface temperature, precipitation, and temperature reconstructed from pollen, δ18O on speleothems, and δ18O on lacustrine carbonate) over the Mediterranean Basin to infer possible regional climate patterns during the interval between 4.3 and 3.8 ka. The values and limitations of these proxies are discussed, and their potential for furnishing information on seasonality is also explored. Despite the chronological uncertainties, which are the main limitations for disentangling details of the climatic conditions, the data suggest that winter over the Mediterranean involved drier conditions, in addition to already dry summers. However, some exceptions to this prevail – where wetter conditions seem to have persisted – suggesting regional heterogeneity in climate patterns. Temperature data, even if sparse, also suggest a cooling anomaly, even if this is not uniform. The most common paradigm to interpret the precipitation regime in the Mediterranean – a North Atlantic Oscillation-like pattern – is not completely satisfactory to interpret the selected data.

Anomaly (physics) · Climate change · Climatology · Geography · Mediterranean Basin · Mediterranean climate · Mediterranean sea · Meteorology · North Atlantic oscillation · Paleoclimatology · Period (music) · Physical geography · Precipitation · Stable isotope ratio · Structural basin · δ18O · Archaeology and ancient environmental studies · Geology · Geology and Paleoclimatology Research · Oceanography · Paleontology · Pleistocene-Era Hominins and Archaeology

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Unique citing works65
Citations per year9,29
Citation span2019 - 2026 (8)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 57
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