Holocene hydrological changes in south-western Mediterranean as recorded by lake-level fluctuations at Lago Preola, a coastal lake in southern Sicily, Italy

• Published in: Quaternary science reviews Vol. 30; no. 19; pp. 2459 - 2475
• Main Authors: Magny, Michel, Vannière, Boris, Calo, Camilla, Millet, Laurent, Leroux, Aurélie, Peyron, Odile, Zanchetta, Gianni, La Mantia, Tommaso, Tinner, Willy
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.09.2011; Elsevier
• Subjects: Atmospheric circulation; Environmental Sciences; Environmental studies; Global Changes; Holocene; Humanities and Social Sciences; Lacustrine sediments; Lake-level fluctuations; Mediterranean; Palaeohydrology; Pantelleria tephra; Sicily; MED, Central Mediterranean; Palaeohydrology; Mediterranean; Sicily; Pantelleria tephra; Lake-level fluctuations; Lacustrine sediments; Holocene
• ISSN: 0277-3791; 1873-457X
• DOI: 10.1016/j.quascirev.2011.05.018

This paper presents a high-resolution lake-level record for the Holocene at Lago Preola (Sicily, southern Italy) based on a specific sedimentological approach, with a chronology derived from AMS radiocarbon dates. It gives evidence of three major successive palaeohydrological periods, with (1) a pronounced dryness during the early Holocene until ca 10300 cal BP, (2) a highstand from ca 10300 to 4500 cal BP, and (3) a marked lowstand from 4500 cal BP to present. Large amplitude lake-level fluctuations characterise two transition phases at ca 10300–9000 and 6400–4500 cal BP. Period 2 was interrupted between 8300 and 7000 cal BP by a dry phase that was punctuated to ca 7300 cal BP by the deposition of a tephra from neighbouring Pantelleria Island. Comparisons of the Preola record with other palaeohydrological records along north–south and west–east transects in the Mediterranean show contrasting patterns of hydrological changes: north (south) of around 40°N latitude, the records highlight a mid-Holocene period characterised by lake-level minima (maxima). Humid mid-Holocene conditions over the Mediterranean south of 40°N were probably linked to a strong weakening of the Hadley cell circulation and of monsoon winds. We suggest that the maximum of humidity in the Mediterranean during the mid-Holocene was characterised by humid winters to the north of 40°N and humid summers to the south. On a multi-centennial scale, the high-resolution palaeohydrological reconstructions in the central Mediterranean area reveal a strong climate reversal around 4500–4000 cal BP, with contrasting changes in the hydrological cycle. In addition to seasonal and inter-hemispherical changes related to orbital forcing, this major oscillation might be related to non-linear responses of the climatic system to the gradual decrease in summer insolation at northern latitudes. Another major climate oscillation around 7500–7000 cal BP may have resulted from the combined effects of (1) a strong rate of change in insolation, and (2) variations in solar activity. Finally, comparisons of the Preola lake-level record with Sicilian pollen records suggest a strong influence of moisture availability on vegetation development in Sicily. Very dry early Holocene conditions probably prevented the expansion of coastal evergreen forests, while decreasing moisture availability since the onset of the late Holocene may have exacerbated effects of intensive land-use. ► A Holocene record of lake-level fluctuations at Lago Preola in south-western Sicily, Italy. ► Evidence for marked early Holocene dryness before ca 10600 cal BP. ► Evidence for a wet mid-Holocene between 10300 and 4500 cal BP. ► Evidence for a marked shift towards drier climate conditions at 4500 cal BP.