Page 7 - 36 Elevation of the last interglacial highstand in Sicily
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23 Acitrezza                              Lava age 180 ka              Inner edge marine terrace  175            75    1344  B  23
24 Taormina                               ESR on littoral fossils      Inner edge marine terrace  115, 130, 185  73     864  A  This paper,
                                                                                                                                24, 25
25 Capo d’Alı`                            Geomorphologic correlation   Inner edge marine terrace  140, 210       73    1064  C  This paper, 25
26 Capo Peloro/Ganzirri                   Strombus b. amino acid       Inner edge marine terrace  110            73     704  A  25–28
27 Capo Rasocolmo                         Geomorphologic               Inner edge marine terrace  110            73     824  C  25
28 Milazzo                                Amino acid and warm fauna    Marine Terrace             90             710    664  B  This paper, 29
29 Tyndari                                Geomorphologic correlation   Lithofaga holes band       85             71.5   624  C  30
30 Naso                                   Geomorphologic correlation   Inner edge marine terrace  120            710    904  C  29
31 Acquedolci                             Geomorphologic correlation   Inner edge marine terrace  130            73     984  C  31

Mean uplift rate Sector 4 (NE) 924 mm/ka  U/Th on Cladocora C.         Inner edge marine terrace  45             73     304  B  29, 32, 33, 34                                                                     ARTICLE IN PRESS
32 Lipari                                 Geomorphologic correlation   Inner edge marine terrace  50             73     344  C  32
33 Salina                                 Age of lava                  Inner edge marine terrace  40–45          73     304  C  32                                                                              F. Antonioli et al. / Quaternary International 145– 146 (2006) 3–18
34 Filicudi                               Geomorfologica./Amino acid   Inner edge marine terrace  115/50         73     864  C  32,34
35 Panarea                                U/Th on Cladocora, Strombus  Inner edge-beach deposit   30             73     184  A  35, 36, 28
36 Ustica                                 Strombus b.                  Fossil beach               4              73    À24   B  37,38
37 Lampedusa

References: (1) Antonioli et al. (1994); (2) Fabiani (1941); (3) Gignoux (1913); (4) Mauz et al. (1997); (5,6) Abate et al. (1991, 1993); (7) Antonioli et al. (1999b); (8) Antonioli et al. (2001); (9)
Antonioli et al. (2002); (10) Ruggieri et al. (1968); (11) Ruggieri and Unti (1974); (12) Malatesta (1957); (13) Abate et al. (1996); (14) Abate et al. (1992); (15) Ruggieri et al. (1975); (16) Ruggieri and
Unti (1988); (17) D’Angelo and Vernuccio (1996); (18) Malatesta (1985); (19) Rhodes (1996); (20) Bianca et al. (1999); (21) Di Grande and Scamarda (1973); (22) Di Grande and Neri (1988); (23)
Monaco et al. (2000); (24) Bonfiglio (1981); (25) Catalano and De Guidi (2003); (26) Antonioli et al. (2004b); (27) Bonfiglio and Violanti (1983); (28) Hearty et al. (1986a, b); (29) Hearty (1986); (29)
Catalano and Di Stefano (1997); (30) Gliozzi and Malatesta (1982); (31) Bonfiglio (1991); (32) Lucchi et al. (2004a); (33) Lucchi et al. (2004b); (34) Radtke (1986); (35) Ruggieri and Buccheri (1968);
(36) de Vita et al. (1998); (37) Buccheri et al. (1999); (38) Segre (1960).
For location of the sites see Fig. 1. We calculated the uplift rate using for MIS 5.5 a eustatic sea level of 7 m. The formula to calculate the uplift rate is: elevation (m)À7/125. In the elevation column
we report the published attribution at MIS 5.5 by different authors but the elevations that we used to calculate uplift rates (discussed in the text) are in bold.

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