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Submerged archaeological sites along the Ionian coast of southeastern Sicily (Italy) and implications for the Holocene relative sea-level change

Published online by Cambridge University Press:  20 January 2017

Giovanni Scicchitano ,
Fabrizio Antonioli ,
Elena Flavia Castagnino Berlinghieri ,
Andrea Dutton  and
Carmelo Monaco
Giovanni Scicchitano
Affiliation:
Dipartimento di Scienze Geologiche, Università di Catania, Corso Italia, 55, 95129 Catania, Italy
Fabrizio Antonioli
Affiliation:
ENEA — Special Project Global Change, via Anguillarese 301, 00060 S. Maria di Galeria, Roma, Italy
Elena Flavia Castagnino Berlinghieri
Affiliation:
Corso di Laurea in Beni Culturali, Università di Catania, sede distaccata di Siracusa, Italy
Andrea Dutton
Affiliation:
Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia
Carmelo Monaco*
Affiliation:
Dipartimento di Scienze Geologiche, Università di Catania, Corso Italia, 55, 95129 Catania, Italy
*
*Corresponding author. E-mail address:cmonaco@unict.it (C. Monaco).
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Abstract

Precise measurements of submerged archaeological markers in the Siracusa coast (Southeastern Sicily, Italy) provide new data on relative sea-level change during the late Holocene. Four submerged archaeological sites have been studied and investigated through direct observations. Two of them are Greek archaic in age (2.5–2.7 ka) and are now 0.98–1.48 m below sea level; the other two developed during the Bronze age (3.2–3.8 ka) and are now 1.03–1.97 m below sea level. These archaeological data have been integrated with information derived from a submerged speleothem collected in a cave located along the Siracusa coast at − 20 m depth. The positions of the archaeological markers have been measured with respect to present sea level, corrected for tide and pressure at the time of surveys. These data were compared with predicted sea-level rise curves for the Holocene using a glacio-hydro-isostatic model. The comparison with the curve for the southeastern Sicily coast yields a tectonic component of relative sea-level change related to regional uplift. Uplift rates between 0.3 and 0.8 mm/yr have been estimated.

Keywords

Submerged archaeological sitesSoutheastern SicilyRelative sea levelHolocene
Type
Original Articles
Information
Quaternary Research , Volume 70 , Issue 1 , July 2008 , pp. 26 - 39
Copyright
University of Washington

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References

A.A., V.V., (1987). Carta Geologica della Sicilia sud-orientale.. S.El.Ca., Firenze.Google Scholar
Alberti, G., (2004). Contributo alla seriazione delle necropoli siracusane.. La Rosa, V. Le presenze micenee nel territorio siracusano Università degli Studi di Catania, Corso di Laurea in Scienze dei Beni Culturali (Siracusa).Google Scholar
Antonioli, F., Silenzi, S., Frisia, S., (2001). Tyrrhenian Holocene palaeoclimate trends from spelean serpulids.. Quaternary Sciences Reviews 20, 1661–1670.Google Scholar
Antonioli, F., Kershaw, S., Renda, P., Rust, D., Belluomini, G., Cerasoli, M., Radtke, U., Silenzi, S., (2006). Elevation of the last interglacial highstand in Sicily (Italy): a benchmark of coastal tectonics.. Quaternary International 145–146, 3–18.Google Scholar
Antonioli, F., Anzidei, M., Lambeck, K., Auriemma, R., Gaddi, D., Furlani, S., Orrù, P., Solinas, E., Gaspari, A., Karinja, S., Kovačić, V., Surace, L., (2007). Sea level change during the Holocene in Sardinia and in the North-eastern Adriatic (Central Mediterranean sea) from archaeological and geomorphological data.. Quaternary Science Revue 26, 2463–2486.CrossRefGoogle Scholar
Anzidei, M., Esposito, A., Antonioli, F., Benini, A., Tertulliani, A., Del Grande, C., (2006). I movimenti verticali nell’area di Briatico: evidenze da indicatori archeologici marittimi nell’area del terremoto del 1905.. Guerra, I., Bavaglio, A. 8 settembre 1905 Terremoto in Calabria Deputazione di Storia Patria per la Calabria, Università della Calabria, Regione Calabria.Google Scholar
Azzaro, R., Barbano, S., (2000). Analysis of the seismicity of southeastern Sicily: a proposed tectonic interpretation.. Annali di Geofisica 43, 171–188.Google Scholar
Basile, B., (1995). Sul porto di Megara Iblea e le antiche linee di costa del territorio siracusano Relazione presentata alla X Rassegna internazione di Archeologia Subacquea di Giardini Naxos..Google Scholar
Basile, B., Di Stefano, G., Lena, G., (1988). Landings, ports, coastal settlements and coastlines in Southeastern Sicily from prehistory to late antiquity.. Raban, A. Archaeology of Coastal Changes”, Proceedings of the First International Symposium “Cities on the Sea—Past and Present 404, BAR International Series, 15–33.Google Scholar
Bernabo’ Brea, L., (1958). La Sicilia prima dei Greci. Il Saggiatore..Google Scholar
Bernabo’ Brea, L., (1966a). Thapsos (Augusta-Siracusa): scavo di tombe nella necropoli dell’età del Bronzo (XIV inizi XIII secolo a.C.).. Bollettino d’Arte 51, 113.Google Scholar
Bernabo’ Brea, B., , (1966b). Abitato neolitico ed insediamento dell’età del Bronzo nell’isola di Ognina (Siracusa) ed i rapporti tra Sicilia e Malta dal XVI al XIII sec. a.C.. Kokalos 12, 40–69.Google Scholar
Bianca, M., Monaco, C., Tortorici, L., Cernobori, L., (1999). Quaternary normal faulting in southeastern Sicily (Italy): a seismic source for the 1693 large earthquake.. Geophysical Journal International 139, 370–394.Google Scholar
Bordoni, P., Valensise, G., (1998). Deformation of the 125 ka marine terrace in Italy: tectonic implications.. Stewart, I.S., Vita-Finzi, C. Coastal Tectonics Geological Society of London Special Publication 46, 71–110.Google Scholar
Boschi, E., Ferrari, G., Ferrari, P., Guidoboni, E., Smriglio, G., Valensise, G., (1995). Catalogo dei forti terremoti in Italia dal 461 a.c. al 1980 Istituto Nazionale di Geofisica, S.G.A., Roma..Google Scholar
Caputo, M., Pieri, L., (1976). Eustatic variation in the last 2000 years in the Mediterranean.. Journal of Geophysical Research 81, 5787–5790.CrossRefGoogle Scholar
Catalano, S., De Guidi, G., (2003). Late Quaternary uplift of northeastern Sicily: relation with the active normal faulting deformation.. Journal of Geodynamics 36, 445–467.Google Scholar
Catalano, S., De Guidi, G., Monaco, C., Tortorici, G., Tortorici, L., (2003). Long-term behaviour of the Late Quaternary normal faults in the Straits of Messina area (Calabrian Arc): structural and morphological constraints.. Quaternary International 101–102, 81–91.Google Scholar
Castagnino Berlinghieri, E.F. (1993–1995). ) Ognina (Siracusa): Note Preliminari All’indagine di Topografia Marittima. 137–148, Klearchos, Taranto.5–13.Google Scholar
Castagnino Berlinghieri, E.F., (2002). Attività umana e assetto costiero nella Protostoria eoliana: nuovi risultati di ricerca Atti del Convegno Internazionale Strumenti per la Protezione e la Valorizzazione del Patrimonio Culturale Marino nel Mediterraneo”, Università di Milano Bicocca, Università degli Studi di Palermo e Regione Siciliana, (Palermo–Siracusa 2001), Milano, 23–35..Google Scholar
Castagnino Berlinghieri, E.F., (2003). Il contesto archeologico sottomarino di Pignataro di Fuori: una testimonianza diretta dell’imprenditoria mercantile eoliana nell’età del Bronzo Antico Atti della XXXV Riunione Scientifica: Le Comunità della Preistoria Italiana. Studi e Ricerche sul Neolitico e le Età dei Metalli”, Lipari, 2000, Volume II, Firenze.. 1043–1048.Google Scholar
Cavallari, F.S., (1892). La Topografia Megara Hyblaea, Storia, Topografia, Necropoli e Anathemata”, Monumenti Antichi, I, 1889 (1892), coll.. 914–950.Google Scholar
Cosentino, D., Ghiozzi, E., (1988). Considerazioni sulle velocità di sollevamento di depositi eutirreniani dell’Italia Meridionale e della Sicilia.. Memorie Società Geologica Italiana 41, 653–665.Google Scholar
De Guidi, G., Catalano, S., Monaco, C., Tortorici, L., (2003). Morphological evidences of Holocene coseismic deformation in the Taormina area (NE Sicily).. Journal of Geodynamics 36, 193–211.Google Scholar
Di Grande, A., Raimondo, W., (1982). Linee di costa pliopleistoceniche e schema litostratigrafico del Quaternario siracusano.. Geologica Romana 21, 279–309.Google Scholar
Doglioni, C., (1991). A proposal of kinematic modelling for W-dipping subductions. Possible applications to the Tyrrhenian–Apennines system.. Terra Nova 3, 423–434.Google Scholar
Dutton, A., Scicchitano, G., Monaco, C., Desmarchelier, J., Antonioli, F., Lambeck, K., Esat, T.M., Fifield, L.K., submitted. Uplift rates defined by U-series ages of speleothems from submerged caves near Siracusa, Sicily (Italy). Submitted to Quat. Geochronol.Google Scholar
Ferranti, L., Antonioli, F., Mauz, B., Amorosi, A., Dai Pra, G., Mastronuzzi, G., Monaco, C., Orrù, P., Pappalardo, M., Radtke, U., Renda, P., Romano, P., Sansò, P., Verrubbi, V., (2006). Markers of the last interglacial sea level high stand along the coast of Italy: tectonic implications.. Quaternary International 145–146, 30–54.Google Scholar
Firth, C., Stewart, I., McGuire, W.M., Kershaw, S., Vita-Finzi, C., (1996). Coastal elevation changes in eastern Sicily: implications for volcano instability at Mount Etna.. McGuire, W.M., Jones, A.P., Neuberg, J. Volcano Instability on the Earth and Other Planets Geological Society of London Special Publication 110, 153–167.Google Scholar
Flemming, N.C. (1969). Archaeological Evidence for Eustatic Changes of Sea Level and Earth Movements in the Western Mediterranean in the Last 2000 Years, Special Paper Geological Society of America. 109, 1–125.Google Scholar
Flemming, N.C., Webb, C.O., (1986). Tectonic and eustatic coastal changes during the last 10,000 years derived from archaeological data.. Zeits chrift fur Geomorphologie., N.F. 62, 1–29.Google Scholar
Gras, M., (1995). Mégara Hyblaea avant Augusta.. Signorina, Alla Une fontaine dans l’histoire Mélange offerts à Noelle de la Blanchardière, Roma.Google Scholar
Gras, M., Tréziny, H., Broise, H., (2004). Mégara Hyblaea, 5. La Ville Archaïque d’une cité grecque de Sicile orientale École Française de Rome..Google Scholar
Grasso, M., Lentini, F., (1982). Sedimentary and tectonic evolution of the eastern Hyblean Plateau (southeast Sicily) during Late Cretaceous to Quaternary times.. Palaeogeography, Palaeoclimatology, Palaeoecology 39, 261–280.Google Scholar
Goes, S., Giardini, D., Jenny, S., Hollenstein, C., Kahle, H.G., Geiger, A., (2004). A recent tectonic reorganization in the south-central Mediterranean.. Earth and Planetary Science Letters 226, 335–345.CrossRefGoogle Scholar
Guzzardi, L., Germanà, G., Mondo, A., (2007). Rinvenimenti nel Santuario sul porto di Megara Hyblaea Atti del Convegno: Ceramica Attica da Santuari della Grecia, della Ionia e dell’Italia”, Perugia 14–17 Marzo 2007..Google Scholar
Gvirtzman, Z., Nur, A., (2001). Residual topography, lithospheric structure and sunken slabs in the central Mediterranean.. Earth and Planetary Science Letters 187, 117–130.Google Scholar
Hirn, A., Nicolich, R., Gallart, J., Laigle, M., Cernobori, L., (1997). Roots of Etna volcano in faults of great earthquakes.. Earth and Planetary Science Letters 148, 171–191.Google Scholar
Houel, J., (1785). Voyage Pittoresque in Sicilie, III.. 68–69.Google Scholar
Jacques, E., Monaco, C., Tapponnier, P., Tortorici, L., Winter, T., (2001). Faulting and earthquake triggering during the 1783 Calabria seismic sequence.. Geophysical Journal International 147, 499–516.Google Scholar
Kapitaen, G., (1970). Perlustrazioni sottomarine sulla topografia originaria e la situazione portuale dell’abitato preistorico di Ognina (relazione preliminare 1969) In Sicilia Archeologica.. 43–56.Google Scholar
Kapitaen, G., (2003). Come navigavano nel Neolitico, in ATTI della XXXV Riunione Scientifica “Le comunità della Preistoria italiana: studi e ricerche sul Neolitico e le età dei Metalli”, in memoria di Luigi Bernabò Brea (Lipari, 2–7 giugno 2000), II, pp. 1037–1041, Firenze..Google Scholar
Lambeck, K., Anzidei, M., Antonioli, F., Benini, A., Esposito, E., (2004a). Sea level in Roman time in the Central Mediterranean and implications for modern sea level rise.. Earth and Planetary Science Letters 224, 563–575.Google Scholar
Lambeck, K., Antonioli, F., Purcell, A., Silenzi, S., (2004b). Sea level change along the Italian coast for the past 10,000 yrs.. Quaternary Quaternary Science Reviews 23, 1567–1598.Google Scholar
Lambeck, K., Purcell, A., (2005). Sea level change in the Mediterranean Sea since the LGM: model predictions for tectonically stable areas.. Quaternary Science Reviews 24, 1969–1988.Google Scholar
Lajoie, K.R., (1986). Coastal tectonics Active Tectonics.. National Academy Press, Washington.95–124.Google Scholar
Lena, G., Basile, B., (1986). Coastal geomorphology and exploration of lithic resources (latomies and limekilns) in the territory of Syracuse in ancient time.. Thalassa 117–122.Google Scholar
Leonardi, R., (1994). Contributo alla conoscenza delle grotte sommerse della Penisola della Maddalena (SR).. Bollettino Accademia Gioenia Scienze Naturali, Catania 27, (348) 599–620.Google Scholar
Leighton, R., (1986). Paolo Orsi (1859–1935) and the prehistory of Sicily.. Antiquity 60, 15–20.Google Scholar
Monaco, C., Tortorici, L., (2000). Active faulting in the Calabrian arc and eastern Sicily.. Journal of Geodynamics 29, 407–424.Google Scholar
Monaco, C., Tapponnier, P., Tortorici, L., Gillot, P.Y., (1997). Late Quaternary slip rates on the Acireale–Piedimonte normal faults and tectonic origin of Mt. Etna (Sicily).. Earth and Planetary Science Letters 147, 125–139.CrossRefGoogle Scholar
Monaco, C., Antonioli, F., De Guidi, G., Lambeck, K., Tortorici, L., Verrubbi, V., (2004). Tectonic uplift and sea-level change during the Holocene in the Catania Plain (eastern Sicily).. Quaternaria Nova 8, 171–185.Google Scholar
Orsi, P., (1890). Megara Hyblaea Monumenti Antichi dei Lincei, coll.. 757–761.Google Scholar
Orsi, P., (1895). Thapsos, necropoli sicula con vasi e bronzi micenei Monumenti Antichi dei Lincei, VI, coll.. 89–150.Google Scholar
Parker, A.J., (1980). Sicilia e Malta nel commercio marittimo dell’antichità Kokalos, XXVI–XXVII.. 726–729.Google Scholar
Piatanesi, A., Tinti, S., (1998). A revision of the eastern Sicily earthquake and tsunami.. Journal Geophysical Research 103, 2749–2758.Google Scholar
Pirazzoli, P.A., (1976). Sea level variations in the northwest Mediterranean during Roman times.. Science 194, 519–521.Google Scholar
Postpischl, D., (1985). Catalogo dei terremoti italiani dall’anno 1000 al 1980 CNR, Progetto Finalizzato Geodinamica, Graficoop, Bologna.. 239 pp.Google Scholar
Sartori, R., Colalongo, M.L., Gabbianelli, G., Bonazzi, C., Carbone, S., Curzi, P.V., Evangelisti, D., Grasso, M., Lentini, F., Rossi, S., Selli, L., (1991). Note stratigrafiche e tettoniche sul rise di Messina (Ionio nord-occidentale).. Giornale di Geologia 53, 49–64.Google Scholar
Scandone, P., Patacca, E., Radoicic, R., Ryan, W.B.F., Cita, M.B., Rawson, M., Che zar, H., Miller, E., Mckenzie, J., Rossi, S., (1981). Mesozoic and Cenozoic rocks from Malta Escarpment (Central Mediterranean).. A.A.P.G. Bulletin 65, 1299–1319.Google Scholar
Scicchitano, G., Monaco, C., (2006). Grotte carsiche e linee di costa sommerse tra Capo Santa Panagia e Ognina (Siracusa, Sicilia sud-orientale).. Il Quaternario 19, (2) 187–194.Google Scholar
Schmiedt, G., (1966). Antichi porti d'Italia. I porti delle colonie greche. L'Universo, XLVI.. 253–296.Google Scholar
Schmiedt, G., (1972). Linea di costa della Sicilia orientale compresa fra la foce del fiume Simeto ed il Capo Ognina.. Il livello antico del Mar Tirreno II, 201–221.Google Scholar
Schubring, J., (1864). Umwanderung des Megarischen Meerbusens in Sizilien Zeitschrift fur allgemeine Erdkunde, N.S. XVII.. 434–464.Google Scholar
Stewart, I., Cundy, A., Kershaw, S., Firth, C., (1997). Holocene coastal uplift in the Taormina area, northeastern Sicily: implications for the southern prolongation of the Calabrian seismogenic belt.. Jornal of Geodynamics 24, 37–50.Google Scholar
Stuiver, M., Reimer, P.J., Reimer, R., (2005). Calib radiocarbon calibration, execute version 5.0.2 html.. http://calib.qub.ac.uk/calib.Google Scholar
Tinti, S., Armigliato, A., (2003). The use of scenario to evacuate the tsunami impact in southern Italy.. Marine Geology 199, 221–243.Google Scholar
Tortorici, G., Bianca, M., De Guidi, G., Monaco, C., Tortorici, L., (2003). Fault activity and marine terracing in the Capo Vaticano area (southern Calabria) during the Middle-Late Quaternary.. Quaternary International 101–102, 269–278.Google Scholar
Tréziny, H., (2002). Urbanisme et voire das les colonies grecques archaïques de la Sicile orientale.. Pallas 58, 267–282.Google Scholar
Valensise, G., Pantosti, D., (1992). A 125 Kyr-long geological record of seismic source repeatability: the Messina Straits (southern Italy) and the 1908 earthquake (Ms 71/2).. Terra Nova 4, 472–483.Google Scholar
Villard, F., Vallet, G., (1953). Megara Hyblaea, III. Les Fouilles de 1951, Parigi.. 23–27.Google Scholar
Voza, G., (1972). Thapsos, primi risultati delle più recenti ricerche. Atti della XIV Riunione Scientifica dell’Istituto Italiano di Preistoria e Protostoria, Firenze.. 175–204.Google Scholar
Voza, G., (1973a). Thapsos Resoconto sulle campagne di scavo del 1970–1971. Atti della XV riunione Scientifica dell’Istituto Italiano di Preistoria e Protostoria, Firenze.. 133 pp.Google Scholar
Voza, G., (1973b). Thapsos.. Voza, G. Archeologia della Sicilia sud orientale Napoli, 30–52.Google Scholar
Waelbroeck, C., Labeyrie, L., Michel, A., Duplessy, J.C., McManus, J.F., Lambeck, K., Balbon, E., Labracherie, M., (2002). Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records.. Quaternary Science Reviews 21, 295–305.Google Scholar
Westaway, R., (1993). Quaternary uplift of Southern Italy.. Journal of Geophysical Reseacrh 98, 21722–21741.Google Scholar
Wortel, M.J.R., Spakman, W., (2000). Subduction and slab detachment in the Mediterranean-Carpathian region.. Science 290, 1910–1917.Google Scholar