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V. Karakitsios, H. Tsikos, K. Agiadi - Katsiaouni, S. Dermitzoglou, E. Chatziharalambous
V. Karakitsios, H. Tsikos, K. Agiadi - Katsiaouni, S. Dermitzoglou, E. Chatziharalambous


In the present paper we examine the use of carbon and oxygen stable isotopes in the study of global palaeoceanographic changes, with special reference to the oceanic anoxic events (OAEs). The analysis of stable isotopes was applied to the examination of Cretaceous sediments from the Ionian and Pindos zones of Western Greece. In the Ionian zone the carbon and oxygen stable isotopes, combined with biostratigraphic data, record the palaeoenvironmental change corresponding to the anoxic events Bonarelli (Cenomanian/Turonian, OAE2) and Paquier (Lower Albian, OAE1b). In the Pindos zone, within the Cretaceous sediments, we observed two organic-carbon-rich levels. According to the biostratigraphic and isotopie analysis, the first level corresponds to an OAE of Santonian age. This local oceanic anoxic event is described for the first time. The second level, Aptian - Albian age, possibly correlates to either the Paquier event (OAE 1b) or the Selli event (OAE 1a), which in Greece were until now known only in the Ionian zone.

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Aubouin, J., 1959. Contribution a I'etude géologique de la Grece septentrionale: les confines de l'Epire et de la Thessalie, Annales Geologioues des Pays Helléniques, 1 : 1-483.

Bernoulli, D., & Renz, O., 1970. Jurassic Carbonate Facies and New Ammonite Faunas from Western Greece, Eclogae Geologicae Helvetiae, 63: 573-607.

Clift, P.D., Robertson, A.H.F., 1990. Deep-water basins within the Mesozoic carbonate platform of Argolis, Greece, J. Geol. Soc. London, 47: 825-836.

Creaney, S., & Passey, Q.R., 1993. Recurring patterns of total organic carbon and source rock quality within a sequence stratigraphie framework American Association of Petroleum Geologists, Bulletin, 77: 386-401.

Danelian, T., Tsikos, H., Gardin, S., Baudin, F., Bellier, J.-P., Emmanuel, L, 2004. Global and regional palaeoceanographic changes as recorded in the mid-Cretaceous (Aptian-Albian) sequence of the Ionian zone (NW Greece), Journal of the Geological Society, London, 161, 703-709.

Demaison, G., & Moore, G.T., 1980. Anoxic environments and oil source bed genesis, American Association of Petroleum Geologists, Bulletin, 64: 1179-1209.

Dommergues, J.-L, Karakitsios, V., Meister, C, Bonneau, M., 2002. New ammonite data about the earliest synrift deposits (Lower Jurassic) in the Ionian Zone of NW Greece (Epirus), Neues Jahrbuch fur Geologie und Palaeontologie, Abhandlungen, 223: 299-316.

Fleury, J.-J., 1980. Les zones de Gevrovo- Tripolitza et du Pinde-Olonos (Grece Continentale et Péloponnèse du Nord). Evolution d'une platforme et une bassin dans le cadre alpin, Soc. Geol. Nord, 4 : 1-651.

Gonzalez-Bonorino, G., 1996. Foreland sedimentation and plate interaction during closure of the Tethys ocean (Tertiary; Hellenides; western continental Greece), J. Sediment. Res., 66: 1148-1155.

Harris, N.B., 2005. Introduction, In: Harris, N.B., (ed.) The deposition of organic-carbon-rich sediments: models, mechanisms, and consequences, SEPM special publication No. 82, 1-5.

Huss, Α., Gaitanakis, P., Neugebauer, J., 1987/88. Der Ammonotico Rosso und seine sedimentaere und ophiolithische Bedeckung bei Ano Fanari (Argolis, Griechenland) - Tektonik einer obduzierten Melange und seines Unterlagers, Annales Géologique des Pays Hell., 33: 85-112.

IGRS-IFP, 1966. Etude Géologique de L'Epire (Grece Nord-Occidentale), Paris, Technip Editions, 306 pp.

Jenkyns, H.C., (2003). Evidence for rapid climate change in the Mesozoic - Palaeogene greenhouse world, Phil. Trans. R. Soc. London A, 361: 1885-1916.

Karakitsios, V., 1990. Chronologie et geometrie de l'ouverture d'un basin et de son inversion tectonique : le bassin ionien (Epire, Grece), Mémoires Sciences de la Terre, Université Pierre et Marie Curie, Paris, 91(4) :310 pp.

Karakitsios, V., 1992. Ouverture et Inversion Tectonique du Bassin Ionien (Epire, Grece), Annales Géologiques de Pays Helléniques, 35 : 85-318.

Karakitsios, V., 1995. The influence of preexisting structure and halokinesis on organic matter preservation and thrust system evolution in the Ionian Basin, Northwestern Greece, American Association of Petroleum Geologists Bulletin, 79: 960-980.

Karakitsios, V., Danelian, Τ & De Weverm, P., 1988. Datation par les radiolaires des Calcaires a Filaments, Schists a Posidonies supérieurs et Calcaires de Vigla (zone ionienne, Epire, Grece) du Callovien au Tithonique terminal, Comptes Rendus de Γ Académie des Sciences, Paris, Series II, 306 : 367-372.

Karakitsios, V., & Koletti, L, 1992. Critical revision of the age of the basal Vigla Limestones (Ionian Zone, Western Greece) based on Nannoplankton and Calpionellids, with Paleogeographical conse quences, Proceedings of the fourth International Nannoplankton Association Conference (Prague, 1991) (eds. B. Hamersmid and J. Young), pp. 165-177,

Knihovnika Zemniho Plynu a Nafty, 14a. Karakitsios, V., & Tsaila, - Monopolis, S., 1988. Données nouvelles sur les niveaux supérieur (Lias inférieurmoyen) des Calcaires de Pantokrator (zone ionienne moyenne, Epire, Grece continenale), Description des Calcaires de Louros, Revue de Micropaleontologie, 31 : 49-55.

Karakitsios, V., Tsikos, H., Van Breugel, Y., Bakopoulos, I., Koletti, L, 2004. Cretaceous oceanic anoxie events in western continental Greece, Bulletin Geol. Soc. Greece, 34: 846-855.

Laubscher, HP. & Bernoulli, D. (1977). Mediterranean and Tethys, In: The ocean basins and margins, Vol. 4A, The eastern Mediterranean (eds A.E.M. Nairn, W.H. Kanes, and F.G. Stehli), pp. 1-28, New York: Plenum Press.

McCrea, Ü.M. (1950). On the isotopie chemistry of carbonates and a paleotemperature scale, J. Chem. Phys., 16(6): 849-857.

Neumann, P. & Zacher, W. (2004). The Cretaceous sedimentary history of the Pindos basin (Greece), Int. J. Eart Sci (Geol. Rundsch.), 93: 119- 131.

Pedersen, T.F. & Calvert, S.E. (1990). Anoxia vs. productivity: what controls the formation of organic-carbon-rich sediments and sedimentary rocks?, American Association of Petroleum Geologists, Bulletin, 74: 454-466.

Richter, D., Muller, C, Mihm, Α., Risch, H. (1996). Die Flysch-zonen Griechenlands. XII. Das Bootikum und seine Flysche im Bereich des Iti-Parnass-Elikon-Gebirges, des nordwestlichen Kallidromon-Gebirges und des sudwestlichen Othrys- Gebirges (Mittelgriechenland), Neues Jahrb. Geol. Palaeont. Abh., 201(3): 367-409.

Rigakis, N. & Karakitsios, V. (1998). The source rock horizons of the Ionian Basin (NW Greece), Marine and Petrolem Geology, 15: 593-617.

Robertson, A.H.F., Clift, P.D., Degnan, P.J., Jones, G. (1991). Palaeogeographic and palaeotectonic evolution of the Eastern Mediterranean Neotethys, Palaeogeogr. Palaeoclimatol. Plaeoecol., 87: 289-343.

Stampili, G.M. (2000). Tethyan Oceans, In: Bozkurt, E., Winchester, JA, Piper, J.D.A. (eds.) Tectonics and magmatism in Turkey and the surrounding area, Geol. Soc. Lond. Sp. Pubi., 173: 1-23.

Suess, E., Kulm, L.D., Killingley, J.S. (1987). Coastal upwelling and a history of organic-rich mudstone deposition off Peru, In: Brooks, J. & Fleet, A.J. (eds.) Marine Petroleum Source Rocks, Geological Society of London special pubi. No. 26, 181-197.

Tsikos, H., Karakitsios, V., Bombardiere, L., Van Breugel., Y., Sinninghe- Damste, J., Schouten, S., Farrimond, P., Tyson, R.V., Jenkyns, H.C. (2003). The Oceanic Anoxic Event (OAE) 1 b in the Ionian Basin, NW Greece: Organic geccnemical evidence, Abstract, Mesczoic paleoceanography, SGF, 49-50.

Tsikos, H., Karakitsios, V., Breugel, Y., Walswarth-Bell, B., Bombardiere, L, Petrizzo, M.R., Sinninghe Damste, J.S., Schouten, S., Erba, E., Premoli Silva, I., Farrimond, P., Tyson, R.V., Jenkyns, H.C. (2004). Organic-carbon deposition in the Cretaceous of the Ionian Basin, NW Greece: the Paquier Event (OAE1b) revisited, Geol. Mag., 141(4): 401-416.

Tyson, R.V. (1987). The genesis and palynofacies characteristics of marine petroleum source rocks, In: Brooks, J. & Fleet, A.J. (eds.) Marine Petroleum Source Rocks, Geological Society of London special pubi. No. 26, 47-67.

Tyson, R.V. (2001). Sedimentation rate, dilution, preservation and total organic carbon; some results of a modeling study, Organic Geochemistry, 32: 333-339.

Tyson, R.V. (2005). The "productivity versus preservation" controversy: cause, flaws and resolution, In: Harris, N.B. (ed.) The deposition of organic-carbon-rich sediments: models, mechanisms, and consequences, SEPM special publication No. 82, 17-33.

Urey, H.C., Lowenstan, M.A., Epstein, S., McKinney, C.R., 1951. Measurements of paleotemperature of the Upper Cretaceous of England, Denmark and the Southeastern United States, Geological Society of America Bulletin, 62: 399-416.-


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