Monica Bini
The 4.2 ka BP Event in the Mediterranean region: an overview
Bini, Monica; Zanchetta, Giovanni; Per?oiu, Aurel; Cartier, Rosine; Català, Albert; Cacho, Isabel; Dean, Jonathan R.; Di Rita, Federico; Drysdale, Russell N.; Finnè, Martin; Isola, Ilaria; Jalali, Bassem; Lirer, Fabrizio; Magri, Donatella; Masi, Alessia; Marks, Leszek; Mercuri, Anna Maria; Peyron, Odile; Sadori, Laura; Sicre, Marie Alexandrine; Welc, Fabian; Zielhofer, Christoph; Brisset, Elodie
Authors
Giovanni Zanchetta
Aurel Per?oiu
Rosine Cartier
Albert Català
Isabel Cacho
Dr Jonathan Dean J.Dean2@hull.ac.uk
Lecturer in Quaternary Science, Director of Education, Co-Deputy Head of School
Federico Di Rita
Russell N. Drysdale
Martin Finnè
Ilaria Isola
Bassem Jalali
Fabrizio Lirer
Donatella Magri
Alessia Masi
Leszek Marks
Anna Maria Mercuri
Odile Peyron
Laura Sadori
Marie Alexandrine Sicre
Fabian Welc
Christoph Zielhofer
Elodie Brisset
Abstract
© Author(s) 2019. 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, δ 18 O on speleothems, and δ 18 O 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.
Citation
Bini, M., Zanchetta, G., Perşoiu, A., Cartier, R., Català, A., Cacho, I., Dean, J. R., Di Rita, F., Drysdale, R. N., Finnè, M., Isola, I., Jalali, B., Lirer, F., Magri, D., Masi, A., Marks, L., Mercuri, A. M., Peyron, O., Sadori, L., Sicre, M. A., …Brisset, E. (2019). The 4.2 ka BP Event in the Mediterranean region: an overview. Climate of the Past, 15(2), 555-577. https://doi.org/10.5194/cp-15-555-2019
Journal Article Type | Article |
---|---|
Acceptance Date | Feb 26, 2019 |
Online Publication Date | Mar 27, 2019 |
Publication Date | Mar 27, 2019 |
Deposit Date | Apr 1, 2019 |
Publicly Available Date | Apr 2, 2019 |
Journal | Climate of the Past |
Print ISSN | 1814-9324 |
Publisher | European Geosciences Union |
Peer Reviewed | Peer Reviewed |
Volume | 15 |
Issue | 2 |
Pages | 555-577 |
DOI | https://doi.org/10.5194/cp-15-555-2019 |
Public URL | https://hull-repository.worktribe.com/output/1512218 |
Publisher URL | https://www.clim-past.net/15/555/2019/ |
Contract Date | Apr 1, 2019 |
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Copyright Statement
© Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License.
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