18,255 research outputs found
Penser l’hégémonie dans le monde contemporain
No full textIs There a Possible Dialogue Between Hegemony and Cosmopolitanism? Interview with Frédéric Ramel -- What do the two concepts of hegemony and cosmopolitanism imply? Are they opposed or is there a possible dialogue between them? In a recently published chapter (“Competition for Hegemony ” in the edited volume Cosmopolitanism in Hard Times), Professor of political science at Sciences Po CERI Frédéric Ramel questions these concepts and explores their scope. The following is an interview with the author. Interview by Miriam Perier, CERI
Caught in the nuclear trap(s)? The responsibility and findings of independent scholarship
No full textBenoit Pelopidas is the author of Repenser les choix nucléaires. La séduction de l'impossible, published last January by Presses de Sciences Po and currently being translated into English. Through systematic research conducted over more than a decade, at the crossroads of nuclear history and international relations, the author addresses essential notions such as proliferation, the security dilemma, vulnerability, and chance to name but a few. He answers our questions about his work, his approach, and his firm stance on the independence of research. This interview was conducted with Benoît Pélopidas on the occasion of the fifth anniversary of the Nuclear Knowledges programme
"jestem zdecydowany nie robić niczego pochopnie..." : elekcja 1697 roku w korespondencji księcia Conti
No full textFranciszek Ludwik de Bourbon, książę Conti, był jednym z ostatnich krewnych
Ludwika XIV w kolejce do tronu francuskiego (za nim stało wówczas
tylko dwóch jego synów – trzyletni nieznany z imienia książę de La
Roche-sur-Yon oraz liczący dwa lata spadkobierca tej linii rodu – Ludwik
Armand II). Wobec wciąż żywych obaw Polaków, że obrany król opuści ich
kraj, by sięgnąć po koronę francuską, gdy tron Francji opustoszeje, jak uczynił
niegdyś Henryk Walezy, fakt ten nie był pozbawiony znaczenia, gdy jesienią
1696 roku wskazywano księcia Conti jako kandydata do elekcji w Polsce.
Ponadto jego godniejszy pozycją kuzyn z głównej linii Kondeuszów – Henryk
Juliusz de Bourbon otrzymał niegdyś, wraz z ojcem – Ludwikiem, obietnicę,
że nie będzie więcej proponowany do tronu polskiego1. Daleko ważniejszym
od wskazanych argumentem przemawiającym za wysunięciem kandydatury
księcia Conti do tronu elekcyjnego po śmierci Jana III Sobieskiego był fakt,
że znał go podskarbi wielki koronny Hieronim Lubomirski[…
Geochemistry of the formation waters in the Po Plain (Northern Italy): an overview
No full textThe Po Valley brines represent the base level of the Quaternary aquifer located in a thick clay-sands sedimentary sequence. Geochemistry indicates that these are marine waters, evaporated to the stage of gypsum precipitation and trapped at the bottom of the basin in the late Messinian. Most of the groundwater samples collected from different springs and wells in the plain result from a mixture of these Na-Cl brines and shallow groundwaters laterally recharged by the Alpine and Apennine chains.
Natural outflows of brackish waters are associated with major tectonic features. Mud volcanoes, located in the eastern sector of the Po plain, are constantly monitored as sudden chemical changes are significant precursors of seismic activity. In the western sector, calcite-filled veins isotopically record different degrees of water-rock interaction. These are outcropping fossil conduits, where mixing between shallow groundwaters and deep seated brines has occurred. The temporal continuity of the hydrological circuits allows the reconstruction of past and present groundwater circulation patterns.
This paper summarises and integrates the geochemical data produced over many years in order to obtain a regional picture of brine origins and the natural mechanisms of groundwater flow
La Chose nue : parité, restitution, spectre
No full text“Disappearance” is at the heart of the studies and novels of Hadrien Laroche, who reexamines for us “the thing” in the work of Martin Heidegger, Jacques Derrida, and Meyer Shapiro. We are familiar with the discussion around Van Gogh’s shoes, a still life lively enough to give rise to some very keen, contradictory interpretations. In introducing the Marquis de Sade into the game, the author allows us to broach the delicate question of the human being’s treatment as a thing by both artists and philosophers.La disparition est au cœur des études et des romans de Hadrien Laroche qui revient pour nous sur « la chose » chez Heidegger, Derrida et Schapiro. Nous connaissons la discussion autour des Souliers de Van Gogh, nature morte suffisamment vivante pour susciter des interprétations contradictoires d’une grande vivacité. En introduisant Sade dans le jeu, l’auteur nous permet d’aborder la question délicate du traitement de l’humain comme chose par l’artiste et le philosophe
La migliore armonia. Dialoghi e interlocutori per il "Globo di Venere"
No full textIl sogno, prima redazione del Globo di Venere, esce nel 1732 come testo proemialedi un’ampia raccolta di «poesie di diversi nobili, ed eccellenti uomini»,invitati dal marchigiano Pietro Paolo Carrara a celebrare in morte la propriamoglie, Donna Antonia Anguissola.1 Il poemetto di Conti si confi gura dunquecome risposta a una sollecitazione ‘d’occasione’, adattandosi, ab initio, al pattopiù connotato della sociabilità poetica primo-settecentesca: una performancemondana e soprattutto ‘autoreferenziale’, secondo una formula un po’ troppoabusata dalla critica, che appunto di norma preferisce non indugiare sopraletture così poco amene
La migliore armonia. Dialoghi e interlocutori per il "Globo di Venere"
No full textIl sogno, prima redazione del Globo di Venere, esce nel 1732 come testo proemialedi un’ampia raccolta di «poesie di diversi nobili, ed eccellenti uomini»,invitati dal marchigiano Pietro Paolo Carrara a celebrare in morte la propriamoglie, Donna Antonia Anguissola.1 Il poemetto di Conti si confi gura dunquecome risposta a una sollecitazione ‘d’occasione’, adattandosi, ab initio, al pattopiù connotato della sociabilità poetica primo-settecentesca: una performancemondana e soprattutto ‘autoreferenziale’, secondo una formula un po’ troppoabusata dalla critica, che appunto di norma preferisce non indugiare sopraletture così poco amene
À propos du populisme
No full textcontribution à un site webOn the basis of a reading of seven books devoted to populism, the author discusses the various ways in which philosophers, political scientists and historians have approached the phenomenon. He addresses the thorny question of how populism is to be defined and the relationship between populists and democracy. He also examines how social scientists position themselves with regard to populism and argues for respecting value neutrality when addressing the topic.À partir d’une lecture de sept ouvrages consacrés au populisme, l’auteur discute différentes approches de ceux-ci proposées par des philosophes, des politistes et des historiens. Il s’intéresse à la question épineuse de la notion de populisme et aux rapports qui s’établissent entre les populistes et la démocratie. Il examine le positionnement qu’adoptent les chercheurs en sciences sociales par rapport au populisme et plaide en faveur du respect de la neutralité axiologique
Sociologie de l’action organisée et analyse des politiques publiques : deux approches pour un même objet ?
No full textPublic policy analysts and organisation sociologists often look at the same objects. The author undertakes a comparison of their respective methodological approaches on three dimensions : how they construct their objects of research ; how they mobilise and lead field studies ; what characteristics of public action does each approach reveal ? While stating the existence of complementarities among the two perspectives on the two first dimensions, she stresses a higher degree of non-compatibility on the third one. Indeed, the latter deals with the role and the centrality recognised to politics and policies in modern societies.Partant du constat qu’analystes des politiques publiques et sociologues de l’action organisée s’intéressent souvent à des objets similaires, l’auteur propose de comparer leurs approches méthodologiques respectives en se centrant sur trois dimensions : la construction des objets de recherche ; la place, l’utilisation et la conduite des enquêtes empiriques ; les caractéristiques de l’action publique que révèlent l’une et l’autre perspective. Elle conclut en mettant en avant la complémentarité des deux approches sur les deux premières dimensions, mais souligne un plus fort degré d’incompatibilité sur la troisième parce qu’elle met en jeu la place et la centralité reconnue au politique par les différents analystes
Synthetic Review and geological framework of the main lucinid deposits (Italy).
No full textSYNTHETIC REVIEW AND GEOLOGICAL FRAMEWORK OF THE MAIN LUCINID DEPOSITS (ITALY)S. CONTI##Dipartimento di Scienze della Terra, Università di Modena, Largo S. Eufemia 19, 41100 Modena ([email protected])INTRODUCTIONThe main italian lucinid deposits, as reported from the geological literature, have been studied and, in many cases, reinterpreted in the field. The results are summarized in the following list. The outcrop localities have been differentiated on the base of various elements: 1) tectonofacies, 2) geographic position, 3) stratigraphy, 4) sedimentology, 5) faunal assemblage, 6) evidences of reworking.Key: In the following format type are indicated the outcrops, sometimes as reported from the literature, found by the author in the field. In many cases the same locality was reported under different names.The term "Lithology" refers to lucinid deposits, whereas "stratigraphy" refers to the sediments embedding lucinid deposits or isolated lucinid valves. "Bibliography" does not include all the papers reported in the “References of the italian lucinid deposits”.PIEDMONT BASINS(TORINO, MONFERRATO, LANGHE HILLS AND PAVIA FOOTHILLS) MARMORITO AND “LUCINA LIMESTONES”Location- Marmorito di Passorano (Cascina Galè, Cascina Fabiasco).Lithology- cream to light brown marly limestones blocks packed with lucinid remains (both articulated and disarticulated shells).Fossil assemblage- planktonic and subordinate benthic foraminifers, echinoid spines, serpulid tubes, gastropods, bivalvs (Anodontia dicomani), solitary and colonial corals, ostracods, bryozoans, fish remains, scaphopods.Stratigraphy- Marmorito and “Lucina Limestones” (late Tortonian?).Reference map- CTR 157090 Cocconato.Geological notes- the original geological framework is lost for poor exposure, lucinids probably enclosed in mudstones; methane-derived autigenic carbonates. POSITION: secondary. ENVIRONMENT: ?Bibliography- CLARI et al. (1988), CLARI et al. (1994), CLARI & MARTIRE (1995).S. AGATA FOSSIL MARLS 1)Portalbera (Pavia oltrepo’). Lithology- marly-calcareous blocks.Fossil assemblage- Lucina globulosa.Stratigraphy- S. Cipriano Po Formation (late Tortonian-early Messinian ?), correlable to the epiligurian deposits?.Reference map- Geological Sheet 59 Pavia.Geological notes- geological framework not known because of the poor exposure. POSITION: Primary? ENVIRONMENT: ?Bibliography- TARAMELLI (1882), SACCO (1891, 1929), PATRINI (1916), BONI (1967).2) Serravalle Scrivia = Carezzano near Fontana (Pavia area), 3) Monticello d'Alba (Roero), 4) Villa Majolo NW of Chieri (Monferrato hill). Fossil assemblage- hundred of species (see bibliography).Stratigraphy- S. Agata Fossil Marls (Tortonian).Reference map- Geological Sheet 70 Alessandria and Geological Sheet 56 Torino.Geological notes- Lucinids as not abundant specimens associated with a numerous high diversity fauna.POSITION: Primary. ENVIRONMENT: outer shelfBibliography- MAYER (1877), SACCO (1899), AUDENINO (1902), NELLI (1903), CAVALLO & REPETTO (1992).SERRAVALLE SANDSTONESRivanazzano e Cappella Montà (Moma), Nazzano hills between S. Antonino and Madonna del Monte (Pavia foothills). Lithology- marly calcareous bodies packed with big lucinids.Fossil assemblage- Lucina doderleini, Amussium denudatum.Stratigraphy- at the top of the Serravalle Sandstones (late Serravallian).Reference map- Geological Sheet 71 Voghera.Geological notes- Lucinid bodies enclosed in mudstones. The faunal association is characterised by low diversity and abundant fauna.POSITION: primary. ENVIRONMENT: inner, outer shelf. Bibliography- TARAMELLI (1882), SACCO (1891,1929), BELLINZONA et al. (1971), DESIO (1973).BALDISSERO FORMATIONBetween Pino Torinese and Pecetto north of Chieri, Superga, Baldissero, Sciolze, Cornaro, Albugnano, Bersano, S. Pietro delle Langhe, La-Moja di Montaldo Torinese, S. Defendente (Tagliolo), S. Mauro Torinese.Lithology- arenaceous calcarenites with red calcareous algae and big isolated lucinid shells, arenaceous siltstones with sparse lucinids.Fossil assemblage- Spirulirostra Bellardii, Sepia sepulta, Aturia aturi, Balantium pedemontanum, B. sinuosum, B. multicostatum, B. sulcosum, B. calix, Vaginella calandrellii, Trophon sculptus, Pollia affinis, P. granifera, Clavella brevicaudata, Ranella marginata, Drillia otusangula, D. cerithioidea, D. crebristriata, D. crispata, Clavatula inedita, Oligotoma pannua, O. ornata, Phos citharella, Nassa tessellata, N. intercisa, N. badensis, N. taurinurum, Purpura arata, Porphyria cylindracea, Ancillarina suturalis, Ancillaria glandiformis, Mitra laxesulcata, M. eofusiformis, M. adsita, Columbella scalaris, C. borsonii, C. compta, Haustator desmarestinus, Aequipecten scrabrellus, Lucina globulosa (L. pomum), Tauriniocrinuus gastaldi). Stratigraphy- at the top of the Baldissero Formation (late Serravallian).Reference map- CTR 156120 Mocucco Torinese, CTR 156110 Montaldo Torinese, CTR 157090 Cocconato, CTR 156100 Superga, CTR 156140 Chieri.Geological notes- Lucinid deposits probably crop out in two different stratigraphic levels. Lucinids as not abundant specimens associated with a numerous high diversity fauna.POSITION: secondary. ENVIRONMENT: inner slope ?.Bibliography- MAYER (1877), COPPI (1877), GIOLI (1887), SACCO (1889), DI ROVASENDA (1892), DE ALESSANDRI (1897), TRABUCCO (1900b), NELLI (1903), BELLINI (1905), PREVER (1907), FERRERO (1909), BONSIGNORE et al. (1969).Other reports without a precise localisation: Lucinids as isolated specimens belonging to a numerous high diversity fauna (inner shelf) are reported in the Pietra da Cantoni del Casalese (DE ALESSANDRI, 1897; SACCO 1935), the Acqui Limestone (TRABUCCO, 1898).CREMOLINO FORMATION1) near Mt. Colma di Rossiglione (Stura valley near Ovada), Carcare; 2) Villaforzano; 3) Tremolino = (Cremolino) at the quarry near the graveyard, Santa Giustina, Sassello, Mioglia, Pareto, Tagliolo Monferrato.Stratigraphy- Cremolino Formation (Aquitanian-Burdigalian).Geological notes- Lucinids as isolated specimens in primary position ? or in resedimented beds (secondary position) ?Bibliography- MAYER (1877), DE STEFANI (1880, 1881a, 1887b, 1891), (TRABUCCO (1891, 1898b), ROVERETO (1900), DI STEFANO (1903), NELLI (1903).SATELLITE BASINSEpiligurian SequenceTermina FormationBOLOGNA FOOTHILLS LOCALITIESHILLS BETWEEN THE RENO AND THE LAVINO RIVERS: Boeria del Santagata, Ducentola, Carbonara on the road from Tizzano towards Mt. Capra (near Mt. della Rocca), 200 m. north of Ponte Rivabella (Lavino riverbed). Lithology- marly-limestones, micritic limestones marls and brecciated limestones in sparse and numerous lens-like bodies gradually passing to surrounding sediments (marly mudstones). Lenses very rich in articulated, often in situ, bivalvs (chiefly lucinids).Fossil assemblage- Lucina pomum, Cardium sp., Lutraria sp., Ostrea sp.Stratigraphy- Termina Marls (Tortonian for Carbonara), (late Tortonian -Globorotalia acostaensis e G. conomiozea Zones, for the other localities).Reference map- CTR - Sez. 220110 Zola predosa, Geological Sheet 87 Bologna.Geological notes- The faunal association is characterized by low diversity and high abundance. Methane-derived autigenic carbonates.POSITION: Primary. ENVIRONMENT: Outer shelf, inner slope.Bibliography- MANZONI (1876b, 1880a, b), BOMBICCI (1881), DI STEFANO (1903), TERZI (1993), RICCI LUCCHI & VAI (1994), CONTI et al. (1994), CONTI et al. (1996).MARECCHIA VALLEY1) San Marino, southern side of the cliff.Lithology- poorly cemented fossiliferous sandstones.Fossil assemblage- Ostrea sp., Pecten sp., Cardium sp., Lucina multilamellata, Donax sp., Thracia sp., Tellina planata, Buccinum sp., Murex sp.Stratigraphy- Acquaviva Formation (Late Tortonian-early Messinian).Reference map- IGM 108 I NE S. Marino.Geological notes- Lucinids as isolated specimens belonging to a high diversity fauna. POSITION: Primary. ENVIRONMENT: inner shelf.Bibliography- MANZONI (1873a, b), FUCHS (1875), SCARABELLI (1880).. 2) Case del Gesso di Secchiano.Lithology- grey fossiliferous mudstones. Fossil assemblage- several species (see bibliography).Stratigraphy- Casa i Gessi Clays (early Messinian).Reference map- IGM 108 I NO Montegelli.Geological notes- Lucinids as isolated specimens belonging to a numerous high diversity fauna. POSITION: primary. ENVIRONMENT: outer shelf.Bibliography- (PRINCIPI 1939b, c).PARMA FOOTHILLS LOCALITIES1) left slope of the Torre di Traversetolo Stream, below Case la Costa.Lithology- marly limestones, brecciated micritic limestones, sometimes crowded with articulated lucinids.Fossil assemblage- Aturia aturi, Lucina globulosa.Stratigraphy- Termina Marls (late Serravallian).Reference map- CTR - Sez.200130 Traversetolo.Geological notes- Type locality of the Termina Formation. Carbonate bodies with a progressive lateral transition to pelitic marls. the faunal association is charaterised by low diversity. Methane-derived autigenic carbonates. POSITION: Primary. ENVIRONMENT: correlable to Modena and Bologna areas.Bibliography- ANELLI (1915), CONTI et al. (1996).2) Cinghio Stream (S. Ilario di Baganza) near Case Cuccarello.Outcrop description- Pteropod pelitic marls passing towards the top to siltitic and arenaceous marls intercalated with folliferous calcarenitic levels. Fossil assemblage- Lunulites sp., Turritella subangulata, Vermetus clathratoides, Sigaretus clathratus, Galeodea echinophora, Ficula condita, Nassa costulata, Aequipecten opercularis, Lucina globulosa, Corbula gibba, Teredo norvegica, Caryophyllia prelongia, Trochocyathus mitratus, Ceratotrochus duodecimcostatus, Flabellum sp., Pteropods.Stratigraphy- Termina Marls (early Tortonian).Reference map- IGM 85 I NO Langhirano.Geological notes- Lucinids as isolated specimens belonging to a numerous high diversity fauna. POSITION: Primary. ENVIRONMENT: slope with a depth > 400-500 m.Bibliography- ANELLI (1913). MODENA FOOTHILLS LOCALITIES1) MONTEGIBBIO (Montebiancano, Montebiancone): along the Serra Stream near the Pozzi Petrolio of Case Pozzo d'Olio, the Vigne along the path of Ca del Chierico (the muletrack going down to the Vigne from the depression located between the hill of the Montegibbio Castle and that one of Ca del Chierico), along the Bizzocchi Stream by S. Michele dei Mucchietti, east and west of the St. Michele dei Mucchietti Castle, Torrano above the Borrazze Stream.2) MONTEBARANZONE: Urbana Valley = Il Poggio di Montebaranzone (Cervarola) = badlands between Sogliano and Bompanaro = steep slopes of the stream going down to the Urbana Valley = between the hills of Casara (Casale) and Cervarola = Sarsetta,right slope of the Urbana Valley, below the path going to the Cervarola from Montebaranzone, 300 m south of the previous locality near the bend of the path going to Pianazza from Montebaranzone, a spur 365 m above sea level NE-ENE of Volpogno, two blocks located at 6-700 m NW of Montebaranzone, west and south of the church of Montebaranzone, by Mt. Scisso (the path running to Montebaranzone through the Braide, western branch of the Chianca (Cianca) Stream near Ominano, slopes underlying Casara. 3) MONTARDONE: Rocca S. Maria di Montardone (Rock of the witches) = southern margin of the flat top of the hill located 900 m SW of Rocca S. Maria = 4 big blocks near the Spezzano Stream, the pond near the stream going down from Montardone = right slope of the Spezzano Stream 1 km WSW of Rocca S. Maria near the confluence of the Montardone Stream, east and north of Poggio Andreotti (the hill 500 m above sea level E of Rocca S. Maria), NW of the confluence of the Pratofiore Stream, 100 m NNE of Montardone along the castle muletrack = the rock projection below the Montardone Castle = north of Montardone. 4) W of Densano (Fosso Pasticcio)Lithology- biomicritic marly calcareous and calcarenitic lenses or column-like bodies (thickness ranging from 50 cm to 20-25 m) crowded with articulated lucinids. Carbonate breccias with disarticulated bivalves. Marly limestones usually crowded with articulated, often in situ, bivalves (chiefly lucinids), whereas calcarenites with rare fossils. Fossil assemblage- Lucina hornesii, L. delbosii (=pomum =appenninica), Cypraea amygdalum, Fusus glomus, F. rostratus, Modiola subcarinata, Ostrea pusilla, Vermetus intortus, Ranella reticulata, Trochus rotelaris, T. magus, Petricula lithophaga.Stratigraphy- Termina Marls (late Serravallian). Geological notes- Lucinid bodies gradually passing to surrounding sediments (marly mudstones) and sometimes (at their base) associated with Ligurian calcareous breccias bearing rare disarticulated lucinids. the faunal association is characterized by low diversity and high abundance. Methane-derived autigenic carbonates.POSITION: primary except for the breccias (secondary). ENVIRONMENT: Outer shelf, inner slope.Reference map- IGM 86 II NE Levizzano, IGM 86 II NO Serramazzoni, IGM 86 I SO Sassuolo.Bibliography- DODERLEIN (1862, 1872), STOHR (1869), COPPI (1869, 1877, 1884, 1886), MAZZETTI (1874), BIANCONI (1877), FERRETTI (1879a, b), MALAGOLI (1886a, b, 1890), PANTANELLI (1886a, b), DE STEFANI (1887, 1900), NELLI (1903), DI STEFANO (1903), FOSSA MANCINI,(1924), MONTANARO (1929a, b, c), LANDI (1930), MORESCHI (1930), ANELLI (1935), DIECI (1959), DIECI & RUSSO (1964), RUSSO (1968), DAVOLI (1972, 1976, 1977, 1982), CONTI et al. (1994), CONTI et al. (1996). Bismantova GroupPARMA APENNINE1) Fosso Bottazzo = from Rusino to Bottazzo (between Moragnano and Rusino).Lithology- carbonate coquina debris, marly calcareous bodies, fossiliferous arenaceous marls.Fossil assemblage- Aturia Aturi, Echinolampas depressa, Lucina globosa, L. Dujardini, L. columbella, L. concentrica ?, Oliva flammulata, Thracia sp., Donax, sp., Ampullaria sp., Conus sp., Buccinum sp., Ringicula sp., Craticularia sp., Laocetes sp.Stratigraphy- Casa Bottazzo Marls (Cigarello marls) near the transition to the Vetto Sandstones (early Serravallian).Reference map- CTR 217120 Ranzano.Geological notes- isolated disarticulated shells, usually at the base of resedimented beds, associated with a high diversity fauna of probable shelf provenance (Pantano marls?). Ligurian clasts occur in some resedimented beds. POSITION: secondary. ENVIRONMENT: slope.Bibliography- DEL PRATO (1881), DEL BUE (1900), ANELLI (1913, 1915).2) Podere Campetello, near the church of Madonna dell'Aiuto, between Rosano and Ca del Grosso, Casa del Cerchio, below the top of Mt. Piano about 750 above sea level (east of Vetto near Rosano), Parmossa Valley by Mt. FusoLithology- carbonate coquina debris, marly calcareous bodies, fossiliferous arenaceous marls.Fossil assemblage- Isis melitensis, Trochocyathus oboesus, Flabellum avicula, Pecten Besseri, Amussium duodecimlamellatus, Dorocidaris blakei, Spatangus austriacus, Nucula nucleus, Chama gryphoides, Lucina sinuosa, L. transversa, Scalaria globosa, Turritella subangulata, Aturia aturi, Natica millepunctata.Stratigraphy- Cigarello marls near the transition to the Vetto Sandstones (early Serravallian).Reference map- Geological Sheet 85 Castelnovo ne’ Monti.Geological notes- isolated disarticulated shells associated with a high diversity fauna, usually at the base of resedimented beds. Associated with Ligurian carbonate breccias, slumps and ligurian-epiligurian olistoliths.POSITION: secondary. ENVIRONMENT: slope.Bibliography- SIMONELLI (1896), DEL BUE (1900), ANELLI (1913, 1935).MODENA-REGGIO APPENNINE1) Rocca Tagliata, Monte Tagliata, Pigneto, Montagnana, Densano, Puianello, Pescale, Ospitaletto, Guiglia, Monte Orsello. 2) Guardone (Guardasone), Bedogno, Borseda, Grassano, Borgo Grassano (Traversetolo), Corboniano, Villa near Carpineto; 3) Castello di Baiso, Pantano, Montese, Paullo, Onfiano, Cologno, Frascara, Castelvecchio di Baiso, N of Roteglia.Lithology- calcarenites (Lucina pomum limestone of the authors).Fossil assemblage- Lucina incrassata, L. isseli, L. rollei, L. borealis, Mitra, Cassis, Nassa, Isocardia, Pholadomia, Teredo Cerithium, Pleurotoma and many other spesies (see bibliography).Stratigraphy- Pantano Formation (Langhian-early Serravallian).Reference map- IGM 86 III NO Carpineti, IGM 86 IV SO Casina, Geological Sheet 85 Castelnovo ne’ Monti, Geological Sheet 86 Modena.Geological notes- Lucinids as isolated specimens belonging to a numerous high diversity fauna. POSITION: primary. ENVIRONMENT: outer shelf-slope.Bibliography- DODERLEIN (1872), COPPI (1877, 1884), MAZZETTI (1879), PANTANELLI (1882, 1883, 1886a, b, c), PANTANELLI & MAZZETTI (1887a, b), MALAGOLI (1887, 1890), DI STEFANO (1903), NELLI (1903).BOLOGNA APENNINE1) Mt. Radicchio between Marzabotto and Vergato= left side of the Reno River over the Pioppe station.Lithology- arenaceous marls.Fossil assemblage- Aturia aturi, Pecten sp., Lucina globulosa, L. callypteryx, Lucina sp., Turritella sp., Pecten dodecimlamellatus, Teredo norvegica, Cassidaria thyrrena, Taonurus flabelliformis.Stratigraphy- Pantano marls (Langhian-early Serravallian).Reference map- CTR 237060 Vedegheto. Geological notes- Lucinids as isolated specimens belonging to a high diversity fauna ?. POSITION: primary. ENVIRONMENT: outer shelf-slope.Bibliography- MANZONI (1881), SIMONELLI (1891), CREMONINI & ELMI (1971), NELLI (1903, 1913).2) San Leone (S. Leo), Mt. Vigese.Lithology- arenaceous marls.Fossil assemblage- Aturia Morrisii, Dentalium sp., Cytherea sp., Lucina sinuosa, L. sp., Solenomya doderleini, Pecten denudatus, P. duodecimlamellatus, Echinoderms.Stratigraphy- Pantano Marls (early Serravallian).Reference map- Geological Sheet 87 Bologna.Geological notes- Lucinids as isolated specimens belonging to a high diversity fauna. POSITION: primary. ENVIRONMENT: outer shelf-slope.Bibliography- FUCHS (1875), MANZONI (1876a).TUSCAN-ROMAGNA APPENNINE1) M. Bosio (Boso) of the Savio Valley.Lithology- arenaceous marls.Stratigraphy- Mt. Fumaiolo Formation (late Langhian-early Serravallian).Reference map- IGM 108 I NO Montegelli.Geological notes-Lucinids as isolated specimens scattered in the sediment. POSITION: primary. ENVIRONMENT: outer shelf.Bibliography- NELLI (1903). 2) La Verna (Calcio del Diavolo).Lithology- limestones with bryozoans and rhodoliths.Fossil assemblage- Lithothamnium seganum, L. langhianum, L. viennae, L. foslie, Lithophyllumn racemus, Clamys scabrella, Pecten malvinae, P. aduncus, Ostrea lamellosa, O. crassissima, Cidaris avenoniensis, Echinolampas angulatus, Lamna hopeli, L. cuspidata, Crysophris sp., Odontapsis contortidens, O. cuspidata, Charcarodon megalodon, Lucina globulosa, Cellepora sp., Smittia sp., Spondylus deshayesi, Conocrinus sp.Stratigraphy- basal part of the S. Marino Formation(late Burdigalian-early Langhian).Reference map- IGM II SE Chiusi della Verna.Geological notes- Lucinids as isolated specimens belonging to a numerous high diversity fauna. POSITION: primary. ENVIRONMENT: inner shelf.Bibliography- SIMONELLI (1883), TRABUCCO (1900a), MIGLIORINI (1910), PRINCIPI (1925b), SACCO (1940). 3) San Marino (Mt. Titano).Lithology- limestones with bryozoans and rhodoliths.Fossil assemblage- Lamna contortidens, Oxyrhina isocelica, O. xiphodon, Carcharodon megalodon, C. crassidens, C. polygyrus, Sphaerodus cintus, Clypeaster scutum, Psammechinus parvus, Conoclypus plagiosomus, Echinolampas Laurillardi, Porites ramosa, Trochocyatus elegans, Balanophyllia sp., Natica sp., Cardium difficile, Lucina transversa, Pecten sp., P. besseri, P. latissimus, P. scabrellus, P. revolutus, Ostrea digitalina, Cellepora sammarinensis, Retepora vibicata, Eschara ondulata, Hornera trabecularis, Membranipora sp., Miriozoon truncatum, Serpula mummulus, Terebratula costae, Cassis mamillaris.Stratigraphy- basal part of the S. Marino Formation(late Burdigalian-early Langhian).Reference map- IGM I NE S. Marino.Geological notes- Lucinids as isolated specimens belonging to a numerous high diversity fauna. POSITION: primary. ENVIRONMENT: inner shelf.Bibliography- SCARABELLI (1848, 1880), MANZONI (1873a, b), FUCHS (1875), TRABUCCO (1906), NELLI (1906, 1907), DE GASPERI (1922). Other reports without a precise localisation: Lucinids as isolated specimens belonging to a numerous high diversity fauna (inner shelf) are reported in the basal part of the Pietra of Bismantova Member (SACCO, 1932).MINOR BASINSMODENA APENNINENNW of Castellara (Ca del Vento of Barigazzo).Lithology- coquina debris in arenaceous limestones blocks, dark grey limestones, carbonate breccias.Fossil assemblage- Cypricardia, Thracia pubescens, Lucina doderleini, Corallinaceae, Lutraria sp, Eburnia eburnoides. Stratigraphy- Barigazzo Sandstones (early Serravallian).Reference map- CTR - Sez. 235120 (Boccassuolo).Geological notes- the original geological framework is lost for poor exposure. Lucinids usually disarticulated, sometimes articulated but randomly disposed. Bivalves probably enclosed in a thick resedimented calcarenitic bed. Carbonate breccias with fauna of shelf provenance ?POSITION: secondary. ENVIRONMENT: inner fan.Bibliography- LOTTI (1895a, b, 1910), TAVANI (1943), FAZZINI (1963), REUTTER (1969), TERZI (1992),BOLOGNA APENNINEMadonna del Ponte quarry (Porretta), railway quarry of Porretta.Lithology- turbiditic sandstones, calcarenites.Fossil assemblage- Modiola exbrocchii, Solenomya doderleini, Cytherea multilamellata, Pecten 12lamellatus, Lucina globulosa, L. dicomani, L. inversa, L. Fuchsi, L. spinifera, L. elliptica, Teredo norvegica, T. appenninica, Syndosmya prismatica, Pholadomya sp., Solenomya doderleini, Naera cuspidata, Aturia aturi, Spatangus austriacus, Taonurus flabelliformis, Tapes, Cassidaria thyrrena, Eudolium fasciatum, Crysodomus bombiccii, Oxyrrhina desorii, Charcarodon megalodon, Craticularia Manzonii, Euplectella bianconii, Clio multicostata, C. triplicata, Serpula capellini. Stratigraphy- Porretta sandstones (early Serravallian)Reference map- CTR 251080 Granaglione.Geological notes- Lucinids as isolated spe
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