RICERCA ITALIANA     

Programmi di ricerca simili:

• 1 - Paleoambienti continentali pleistocenici ed olocenici: ricostruzioni multidisciplinari integrate
• 2 - Fasi evolutive dei sistemi di rifting Atlantico e Ionico attraverso l'indagine sugli eventi registrati nelle successioni sedimentarie alpine ed appenniniche.
• 3 - Caratterizzazione stratigrafica, paleoambientale e geochimico-petrografica di eventi al passaggio Triassico-Giurassico nei margini passivi dell'area alpina e centro atlantica: un approccio integrato
• 4 - La transizione climatica tra Pliocene Medio e Pliocene Superiore: una prospettiva Mediterranea
• 5 - EREDITA' TARDO-PALEOZOICHE E MESOZOICHE NELLA STRUTTURAZIONE DELLA CATENA ALPINA
• 6 - L'inizio dopo la fine: scomparse e riprese evolutive durante e dopo l'estinzione di massa del tardo Ordoviciano nel Nord Gondwana
• 7 - Tyrrhenian Seamounts ecosystems: an Integrated Study (TySEc)
• 8 - RICOSTRUZIONE AD ALTA RISOLUZIONE DELL'EVOLUZIONE PALEOCLIMATICA, PALEOCEANOGRAFICA ED ECO-BIOSTRATIGRAFICA DEL BACINO MEDITERRANEO NEL TARDO QUATERNARIO (0-450 KY BP)IN BASE ALL'ANALISI DI TRACCIANTI FAUNISTICI, FLORISTICI, CHIMICI ED ISOTOPICI.
• 9 - Rift mesozoici nell'area centro-mediterranea: paleogeografia ed evoluzione tettonica
• 10 - Contributo della meiofauna alla biodiversità marina italiana

Classificazione scientifico-disciplinare

• Area scientifico disciplinare: Scienze della terra
  • PALEONTOLOGIA E PALEOECOLOGIA
  • GEOLOGIA STRATIGRAFICA E SEDIMENTOLOGICA
  • GEOLOGIA STRUTTURALE

Classificazione geografica

• Regione: Emilia Romagna

Bibliografia

Adams C.G., Lee D.E. & Rosen B.R. 1990. Conflicting isotopic and biotic evidence for tropical sea-surface temperatures during the Tertiary. Palaeogeogr., Palaeoclimatol., Palaeoecol., 77, 289-313.
Amodio Morelli L., Bonardi G., Colonna V., Dietrich D., Giunta G., Ippolito F., Liguori V., Lorenzoni E., Paglionico A., Perrone V., Piccarreta G., Russo M., Scandone P., Zanettin Lorenzoni E. & Zuppetta A. (1976): L’Arco calabro-peloritano nell’orogene appenninico maghrebide. Mem. Soc. Geol. Ital., 17, 1-60.
Bosellini A., 1984, Progradation geometries of carbonate platforms: Examples from the Triassic of the Dolomites, northern Italy: Sedimentology, v. 31, p. 1-24.
Bosellini A.; Gianolla P.; And Stefani M. (2003). Geology of the Dolomites. Episodes. (vol. 26 pp. 181-185)
Bosellini A.& Hardie L.A.,1988. Facies e cicli della Dolomia Principale delle Alpi Venete.Mem.Soc.Geol.Ital., 30, 245-266.
Bosellini F.R. & Russo A.(1992) - The Castro Limestone: stratigraphy anf facies of an Oligocene fringing reef (Salento Peninsula, Southern Italy). Facies, 26, 145-166., Pl.31-38,6 Figs., Erlangen.
Bosellini F.R. (1998) - Diversity, composition and structure of Late Eocene shelf- edge coral associations (Nago Limestone, Northern Italy). Facies, 39, 203-226, Erlangen.
Bosellini F.R., Russo A. & Vescogni A. (2001) - Palaeobathymetric significance of different reef-building assemblages (Early Messinian, Salento Peninsula (Southern Italy). Palaeogeogr. Palaeoclim. Palaeoec., vol. 175/1-4, 7-26.
Bosscher H. & Schlager W. (1993): Accumulation rates of carbonate platforms: J. Geol., vol. 101, no. 2, p. 345-355
Climaco A., Boni M., Iannace A. & Zamparelli V. (1999): Praia a Mare Mountains. In: Colacicchi, R., Parisi, G. & Zamparelli, V. (eds.):Bioevents and Integrate Stratigraphy of the Triassic and Jurassic in Italy. Palaeopelagos Special publication N°. 3, 38-40.
Damiani A. V. (1970): Osservazioni geologiche in alcune tavolette del Foglio 220 nella Calabria nord occidentale. Parte I – Stratigrafia. Boll. Soc. Geol. It., 89, 65-80.
Esteban M. (1996) - An Overview of Miocene Reefs from Mediterranean Areas: General Trend and Facies Models. - In: Franseen, E.K., Esteban, M., Ward, W.C. & Rouchy, J. (Eds.): Models for Carbonate Stratigraphy from Miocene Reef Complexes of Mediterranean Region. SEPM Concepts in Sedimentology and Paleontology, 5, 3-53, Tulsa
Fairbanks R.G., 1989. A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature 342, 637-642.
Flügel E. (2002) – Triassic reef patterns. In: Phanerozoic Reef Patterns. SEPM Special Publication n°72, 391-463.
Gianolla P., De Zanche V. and Roghi, G. (2003): An Upper Tuvalian (Triassic) Platform-Basin System in the Julian Alps: the Start-up of the Dolomia Principlae (Southern Alps, Italy). Facies, 49, 135-150.
Hollaus S.-S., Hottinger L., 1997. Temperature dependence of endosymbiotic relationships? Evidence from the depth range of mediterranean Amphistegina lessonii (foraminiferida) trun- cated by the thermocline. Eclog. Geol. Helv. 90, 591-597.
Haq B.U., Hardenbol J. & Vail P.R. 1988. Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change. Soc. Econ. Petrol. Min. Spec. Publ., 42, 71-105.
Jadoul F., Berra F. & Frisia S. (1992): Stratigraphic and paleogeographic evolution of carbonate platform in an extensional tectonic regime: the example of the Dolomia Principale in Lombardia Italy. Riv. It. Paleont. Strat., 98,: 29-44.
Jadoul F., Berra F., Claps M., & Trombetta L. (1999): The Lombardy Basin (Western Southern Alps). In: Colacicchi, R., Parisi, G. & Zamparelli, V. (eds.):Bioevents and Integrate Stratigraphy of the Triassic and Jurassic in Italy. Palaeopelagos Spec. Publ. n°. 3, 10-18.
Kiessling W. (2001) – Paleoclimatic significanceof Phanerozoic reefs. Geology, 29 (8), 751-754.
Kiessling W., Flügel E. & Golonka J. (1999) – Paleoreefs Maps: Evaluation of a comprehensive database on Phanerozoic reefs. AAPG Bulletin, 8(10), 1552-1587.
Macoux J., Baud A., Ricoux L., Gaetani M., Krystyn L., Bellion Y., Guiraud R. Besse J., Gallet Y., Jaillard E., Moreau C. & Theveniaut H. (1993): Late Norian (215-212 My). In: J. Dercourt, L.E. Ricou & B. Vrielynick (eds.): Altas Tethys paleoenvironmental maps. Explanatory Notes, 35-53, Gauthier-Villars Paris.
Mutti M. & Weissert H., 1995. Triassic monsoonal climate and ist signature in Ladinian-Carnian carbonate platforms (Southern Alps, Italy). – J. Sediment. Res., B65 (3): 357-367.
Parrish J.T., 1993. Climate of the Supercontinent Pangea. – The Journal of Geology, 101: 213-233, Chicago.
Perri E., Mastandrea A., Neri C. & Russo F. 2003 – A micrite-dominated Norian carbonate platform from Northern Calabria (Southern Italy). Facies, 49, 101-118, 5 pls., Erlangen.
Pescatore T., Renda P., Schiattarella M. & Tramutoli M. (1999): Stratigraphic and structural relationships between Meso-Cenozoic Lagonegro basin and coeval carbonate platforms in southern Apennines, Italy. Tectnophysics, 315, 269-286.
Perrin C. 2002, Tertiary: the emergence of modern reef ecosystems. In: Phanerozoic Reef Patterns. SEPM Special Publication n°72, 587-621.
Reinhardt L. & Ricken W., 2000. The stratigraphic and geochemical record of Playa Cycles: monitoring a Pangaean monsoon-like system (Triassic, Middle Keuper, S. Germany). – Palaeogeogr. Paleoclimatol. Palaeoecol. 161 (2000): 205-227.
Retallack G.J., 2001. A 300-million-year record of atmosphaeric carbon dioxide from fossil plant cuticle. – Nature: 411: 287-290.
Robinson P.L., 1973. Palaeoclimatological ad continental drift. – In: Tarling, D.H. & Runcorn, S.K. (ed.), Implications of Continental Drift to the Earth Sciences, Academic Press, 451-476, London/New York.
Rohde K. 1992. Latitudinal gradients in species diversity: the search for the primary cause. Oikos, 65, 514-527.
Russo F., Mastandrea A., Stefani M. & Neri C. (2000): Carbonate facies dominated by syndepositional cements: a key component of Middle Triassic platforms. The Marmolada case history (Dolomites,Italy). Facies, 42: 211-226.
Russo F., Neri C., Mastandrea A., & Baracca A. (1997): The mud mound nature of the S. Cassiano platform margins of the Dolomites. A case history: the Cipit Boulders from Punta Grohmann (Sasso Piatto Massif, Northern Italy). Facies, 36: 25-36.
Sbaffi L., Wezel F.C., Kallel N., Paterne M., Cacho I., Ziveri P. & Shackleton N. (2001). Response of the pelagic environment to palaeoclimatic changes in the central Mediterranean Sea during the Late Quaternary. Marine Geology 178: 39-62.
Scandone, P. (1975): Triassic seaway and the Jurassic Tethys in the Central Mediterranean area. Nature, 256, 117.
Schlager W., 1999, Scaling of sedimentation rates and drowning of reefs and carbonate platforms, Geology, vol. 27, n. 2, pp. 183-186.
Tucker M.E. & Benton M.J., 1982. Triassic environments, climates and reptile evolution. – Palaeogeogr. Paleoclimatol. Palaeoecol., 40:361-379.
Veron J.E.N. (1995) - Corals in space and time. The biogeography and evolution of the Scleractinia. UNSW Press, 321 pp.
Wood A. W. (1981): Extensional tectonics and the birth of the Lagonegro basin. N. Jb. Geol. Palaont. Abh. 161, 93-131.
Zamparelli V., Cirilli S. & Iannace A. & Jadoul F. (coord.) (1999): Paleotectonic and palaeoceanographic controls on microbial-serpulid communities in the Norian-Rhaetian carbonates of Italy: a synthesis. In: Colacicchi, R., Parisi, G. & Zamparelli, V. (eds.):Bioevents and Integrate Stratigraphy of the Triassic and Jurassic in Italy. Palaeopelagos Special publication N°. 3, 7-84.
Ziegler A.M., Parrish J.M., Jiping Y., Gyllenhaal E.D., Rowley D.B., Totman Parrish J., Shanyou N., Bekker A. & Hulver M.L., 1994. Early Mesozoic phytogeography and climate. – In: Allen J.R.L., Hoskins B.J., Sellwood B.W., Spicer R.A. & Valdes P.J. (eds.), Palaeoclimates and their modelling with special reference to the Mesozoic era. – The Royal Society by Champman & Hall, 89-96, London.

Parole Chiave

CLIMA; PRODUTTIVITÀ CARBONATICA; STRATIGRAFIA; PALEOECOLOGIA; ORGANISMI BIOCOSTRUTTORI