Page 15 - Malatesta
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Alberto Malatesta: 20 years of activity at the Geological Survey of Italy                 25


                             formations of different ages  are recognizable, as   Sardinia and often connected to buildings of burial
                             well as traces of two ancient shorelines at 5 and 30   and cult.
                             meters s.l.m.,  presumably related to two different
                             Tyrrhenian transgressions.                    14. 1955 - MALATESTA A. & SEGRE A.G., “F° 111 Livor-
                                                                              no. Note illustrative della Carta geologica d’Italia”.
                          9. 1954 - MALATESTA A., “Aluni risultati della campagna      It is worth to underline that A. Malatesta alone car-
                             geologica (1953)”.                               ried out the layout of this note, as well as the whole
                             In this  paper  some results related to the field sur-  sheet survey,  wherehas A.G. Segre developed the
                             veys of sheets N°18 “Sondrio”, N°192 “Alghero”, and   continental and marine hydrography. This is also
                             N°273 “Caltagirone” are reported. More in particular,   documented by the words of Beneo, at that moment
                             the stratigraphic and geomorphologic data on the   Director of the Geological Survey of Italy,  when, in
                             Quaternary deposits of  the high Val  Brembana   the 1951 activity annual report textually wrote “… si
                             (Sheet “Sondrio”) are discussed; observations re-  è realizzato in pochi mesi, ad opera del dott. Mala-
                             lated to the Jurassic-Cretaceous sediments of the I   testa il completamento del rilievo ex novo del foglio
                             and IV quadrant of the “Alghero” sheet are reported;   111 (Livorno), ora praticamente pronto per la stam-
                             the Plio-Pliestocene successions of the tablets IV°   pa della 2° edizione.” (BENEO, 1951).
                             NW and SW of the “Caltagirone” sheet are analyzed      Since Leghorn was the native town of Malatesta, it is
                             in a stratigraphic and tectonic perspective.     perhaps easier to understood how much the enthu-
                                                                              siasm and the knowledges already previously ac-
                          10. 1954 - MALATESTA A., “Risultati del rilevamento del   quired by A. Malatesta could have contributed to
                             F° 192 Alghero, Sardegna. Fossili delle spiagge tir-  give those definitive results in such a brief time.
                             reniane”.                                        Particularly interesting are the considerations on the
                             “Le spiagge fossili tirreniane di quota +5 del litorale   genesis of the conglomerate of Calafuria, aged Oli-
                             di Alghero contengono una ricca fauna di molluschi   gocene-Miocene, in which the presence of a marine
                             marini. L’autore fornisce un elenco di oltre 140 for-  bivalve fauna suggested  its deposition in a marine
                             me raccolte  in  quei  depositi ed afferma trattarsi  di   coastal environment.
                             uno dei più ricchi complessi tipicamente tirreniani
                             noti nel Mediterraneo settentrionale. Seguono brevi   15. 1955 - MALATESTA A., “Risultati preliminari del rile-
                             considerazioni  su alcune specie elencate e  viene   vamento in Sicilia e nelle isole Egadi”.
                             descritta la nuova forma Purpura (Stramonita) hae-     Here, the sediments cropping out in the Grammi-
                             mastoma LINNAEUS f. johannae n.”                 chele area (Trubi Fm., tufa and sandstones) and the
                                                                              recent deposits of the Egadi Island  are shortly de-
                          11. 1954 - MALATESTA A. & SETTEPASSI F., “Risultati del   scribed. At Favignana the Calabrian-Tyrrhenian de-
                             rilevamento del F°192  Alghero, Sardegna.  Fossili   posits are covered by reddish sands while at Levan-
                             delle formazioni continentali quaternarie”.      zo and Marettimo only the Tyrrhenian deposits are
                             21 species of terrestrial and fresh water molluscs,   present, followed by aeolian dunes at Levanzo and
                             15 of birds and 5 of mammals coming from the     by breccias at Marettimo.
                             breccias, aeolian sandstones and post-Tyrrhenian
                             travertines in the Alghero area are listed. Most of   16. 1955 - MALATESTA  A.  &  NICOSIA  M.L., “I fossili  del
                             them are reported for the first time in the Quaternary   Pliocene e Pleistocene di Agrigento della Collezione
                             of Sardinia, and some are not present in the present   Lomi”.
                             day fauna of the island. Moreover, a new form of the      The list of 183 Piacenzian and Calabrian species is
                             terrestrial gastropod  Retinella incerta  DRAPARNAUD   reported. Particularly, the Calabrian fauna is  com-
                             n.f. oblivia is described (note n. 3).           posed by 9 Echinodermata, 4 Bryozoa, 70 Bivalvia,
                                                                              72 Gastropoda and 8  Scaphopoda, while the Pia-
                          12. 1954 - MALATESTA A., “Primo dente di elefante fossi-  cenzian one, less diversified, consists of 7 bivalves,
                             le rinvenuto in Sardegna”.                       12 gastropods and 1 Scaphod. It is to be remarked
                             In this paper it is described the upper right M1 re-  that 88 Calabrian species  were not yet reported at
                             covered in a post-Tyrrhenian breccia near Alghero,   that time.
                             referred to E. lamarmorae (species next to E. meri-
                             dionalis). For some characters, this tooth is compa-  17. 1955 - MALATESTA A., “Faune a Cyprina islandica L.
                             rable with the upper molars of the Sicilian species E.   tra piazza Armerina e Mazzarino (Sicilia centro-
                             melitensis.                                      meridionale)”.
                                                                              “Una nuova località fossilifera individuata presso
                          13. 1954 - MALATESTA A., “Il cosidetto Campanile della   S. Cono  (Piazza Armerina) ha fornito una  piccola
                             necropoli nuragica di S. Andrea Priu (Bonorva)”.   fauna nella quale appare assai di frequente Cypri-
                             The Author describes and illustrates a prehistoric   na islandica L.; questa specie è stata raccolta an-
                             monument of the Nuragic necropolis of S. Andrea   che recentemente nel nuovo giacimento di M. Na-
                             Priu in  Sardinia,  which  can be interpreted as  a   vone. Le  faune  delle due località non  sono  suffi-
                             grave. Its shape recalls a not identifiable zoomor-  cienti a definire se si tratti di Pliocene superiore o
                             phic figure (the anterior part  of the head  is  miss-  di Calabriano Sebbene nei molluschi vi sia una cer-
                             ing), possibly a taurine image, very common  in   ta tendenza verso il più recente, l’associazione dei
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