Contrasting patterns of precipitation seasonality during the Holocene in the south- and north-central Mediterranean
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Contrasting patterns of precipitation seasonalityduring the Holocene in the south- andnorth-central Mediterranean
MICHEL MAGNY,1* ODILE PEYRON,1 LAURA SADORI,2 ELENA ORTU,1 GIOVANNI ZANCHETTA,3
BORIS VANNIE`RE1 and WILLY TINNER41Laboratoire de Chrono-Environnement, UMR 6249 du CNRS, UFR des Sciences et Techniques, 16 route de Gray,25 030 Besancon, France2Dipartimento di Bilogia Ambientale, Universita La Sapienza, Roma, Italy3Dipartimento di Scienze della Terra, and IGC-CNR, Pisa, Italy4Paleoecology, Institute of Plant Sciences and Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
Received 30 May 2011; Revised 26 August 2011; Accepted 28 August 2011
ABSTRACT: Pollen-based quantitative estimates of seasonal precipitation from Lake Pergusa and lake-level data fromLake Preola in Sicily (southern Italy) allow three successive periods to be distinguished within the Holocene: an earlyHolocene period before ca. 9800cal a BP with rather dry climate conditions in winter and summer, a mid-Holoceneperiod between ca. 9800 and 4500cal a BPwithmaximumwinter and summerwetness, and a lateHolocene period after4500 cal a BP with declining winter and summer wetness. This evolution observed in the south-central Mediterraneanshows strong similarities to that recognized in the eastern Mediterranean. But, it contrasts with that reconstructed innorth-central Italy, where the mid-Holocene appears to be characterized by a winter (summer) precipitation maximum(minimum), while the late Holocene coincided with a decrease (increase) in winter (summer) precipitation. Maximumprecipitation at ca. 10 0004500 cal a BP may have resulted from (i) increased local convection in response to aHolocene insolation maximum at 10 000cal a BP and then (ii) the gradual weakening of the Hadley cell activity, whichallowed the winter rainy westerlies to reach the Mediterranean area more frequently. After 4500 cal a BP, changes inprecipitation seasonality may reect non-linear responses to orbitally driven insolation decrease in addition to seasonaland inter-hemispheric changes of insolation. Copyright # 2011 John Wiley & Sons, Ltd.
KEYWORDS: Mediterranean; Holocene; modern analogues technique; precipitation seasonality; sapropel 1.
The Mediterranean area lies in a transitional zone that isinuenced by both the dynamics of (i) the tropical circulationcells with the subtropical anticyclone belt and associatedaridity, and (ii) the mid-latitude westerlies and cyclogenesis(Tzedakis et al., 2009). This results in a marked precipitationseasonality that is crucial for both Mediterranean ecosystemsand societies.Recent studies have pointed to the role of seasonality in
abrupt climate change and in the Mediterranean region(Denton et al., 2005; Kotthoff et al., 2008; Davis and Brewer,2009; Dormoy et al., 2009; Pross et al., 2009). They have alsohighlighted that seasonality can explain apparent discrepanciesbetween palaeoclimatic data derived from pollen, refrequency, lake levels and isotopes for the mid-Holoceneclimate in the central Mediterranean (Magny et al., 2007;Zanchetta et al., 2007b; Vannie`re et al., 2011; Roberts et al.,2008; Peyron et al., 2011; Giraudi et al., 2011; Sadori et al.,2011). However, given the relative scarcity of reliablepalaeoclimatic records for the Holocene in the south-centralMediterranean, additional data are needed to test thishypothesis and provide a more precise picture of variationsin the seasonality in the Mediterranean area.Using the modern analogues technique (MAT; Guiot, 1990),
this study aims to provide a record of quantitative estimates ofthe Holocene climate based on the pollen sequence of LakePergusa in Sicily (Sadori and Narcisi, 2001), with particularattention to the reconstruction of precipitation seasonality. Incombination with the lake-level record established at LakePreola in south-western Sicily (Magny et al., 2011b), thesequantitative estimates provide new insight into the seasonal
precipitation patterns and climatic trends which have charac-terized the Holocene in the south-central Mediterranean.Finally, a comparison with other lake-level data and quanti-tative estimates of climatic parameters obtained at Lake Accesain central Italy (Magny et al., 2007; Peyron et al., 2011) allowscontrasting seasonality patterns to be distinguished betweensouthern and northern border regions of the central Mediterra-nean (Fig. 1).
Site, data and methods
Lake Pergusa (378310N, 148180E; 667m a.s.l.) is located incentral Sicily. The catchment area of the lake is about 7.5 km2
and reaches its maximum elevation at Monte Carangiano(911m a.s.l.). The lakes surface area was ca. 1.4 km2 in 1968.Mean annual precipitation in the area is between 500 and700mm. At the weather station of Enna (about 5 km NNW ofthe lake), mean annual temperature is 13.4 8C, with 37 8C forthe warmest month and 3 8C for the coldest (Zampino et al.,1997).According to Sadori and Narcisi (2001), Lake Pergusa is
located in the meso-Mediterranean bio-climate belt of theMediterranean region, in the subhumid ombrotype and inferiorthermotype (Brullo et al., 1995). The potential vegetation isformed by mesophilous Mediterranean evergreen woodsdominated by Quercus ilex L.The Holocene pollen record of Lake Pergusa has been
established by L. Sadori from a 4.5-m-long core taken in thelake basin, and extensively published in a previous study(Sadori and Narcisi, 2001). The chronology is based on eightradiocarbon dates in addition to a tephra layer probably relatedto the Sicans event (late Holocene explosion from the Etnavolcano). A calendar chronological scale was recently assessed(Sadori et al., 2011). Seven successive pollen zones have been
JOURNAL OF QUATERNARY SCIENCE (2012) 27(3) 290296 ISSN 0267-8179. DOI: 10.1002/jqs.1543
Copyright 2011 John Wiley & Sons, Ltd.
*Correspondence: M. Magny, as above.E-mail: firstname.lastname@example.org
distinguished within the pollen sequence as follows (Sadori andNarcisi, 2001).
Before ca. 11 000 cal a BP, herbaceous plants are dominant[non-arboreal pollen (NAP) between 56 and 83%] and totalpollen concentration values are low. Both Quercus roburtype and Q. ilex type show continuous curves.
During the period around 11 00010000 cal a BP, herbs arestill dominant (5674%) although decreasing, and total pol-len concentration values increase slightly. Deciduous andevergreen oaks show an increase both in percentage (2133%) and in concentration.
The period around 10 0008000 cal a BP began with anabrupt increase of arboreal pollen (AP) percentages (expan-sion of the forest) and concentrations. The proportion of AP ismainly around 80%. The main taxon is Quercus robur type(4060%) followed by Q. ilex type (1225%). As inferredfrom pollen percentages, other important arboreal taxa areQ. suber/cerris, Ericaceae, Ulmus, Corylus and Fagus.
During the period around 80005000 cal a BP, the APpercentages reach the highest value (94%) while AP andNAP concentrations decrease. Quercus robur type andQ. ilex type are always present at high percentages, whilepercentages of Corylus, Fagus and Ericaceae decrease, andthose of Olea show an increasing trend.
During the period around 50003000 cal a BP, AP remaindominant (ca. 70%) and total pollen concentrations are low.Ulmus percentages reach their maximum values.
The period around 30002300 cal a BP is characterized bythe highest expansion of Olea (1019%).
Finally, the period from ca. 2300 cal a BP to the presentshows alternate dominant AP and NAP percentages, whiletotal pollen concentrations are very low (values comparablewith those reached before 11 000 cal a BP). Oaks are stilldominant in the AP percentages.
In summary, maximal total pollen concentrations areobserved between ca. 9800 and 4700 cal a BP with valuespeaking between ca. 9300 and 6600 cal a BP (Fig. 2). Fromabout 5000 cal a BP, the forest has become more open. Per-centages of deciduous oaks decrease while those of evergreenelements become relatively more important and dominate afteraround 2800/2700 cal a BP. Important res occurred at the endof the Lateglacial and since the end of the Bronze Age, i.e. in thelast 3200 years (Sadori and Giardini, 2007). On the basis of thepollen data, Sadori and Naricisi (2001) come to the generalconclusion that, at Pergusa, human impact on the vegetationduring the late Holocene overlapped a drying trend that startedaround 8000 cal a BP and did not produce important effects onthe already open landscape.The method used for the reconstruction of climatic
parameters is the MAT, which was rst developed by Overpeck
Figure 1. Geographical location of LakesPergusa and Preola and reference sites in theMediterranean and in west-central Europe. LA,Lake Accesa; LAl, Lake Albano; LC, LakeCerin; LMe, Lake Mezzano; NF, Nisi Fen;SC, Soreq Cave; TP, Tenaghi Philippon; SL152 is a marine core. The dotted line showsthe limit of the Mediterranean sensu strictobiogeographical zone. This gure is availablein colour online at wileyonlinelibrary.com.
0 500 km
AGE (ka cal BP)11 10 9 8 7 6 5 4 3 2 1 0
> 17 x 104 > 10 x 104
Total Pollen conc.(grain