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Paleoclimatic Record of a Long Deep Sea Core from the Eastern Mediterranean

Published online by Cambridge University Press:  20 January 2017

Maria Bianca Cita ,
Colette Vergnaud-Grazzini ,
Christian Robert ,
Hervé Chamley ,
Neri Ciaranfi  and
Sara d'Onofrio
Maria Bianca Cita
Affiliation:
Department of Geology and Paleontology, University of Milano, Milano, Italy
Colette Vergnaud-Grazzini
Affiliation:
Laboratoire de Géologie Dynamique, Université Pierre et Marie Curie, Paris, France
Christian Robert
Affiliation:
Laboratoire de Géologie Marine, Université d' Aix-Marseille II, Marseille, France
Hervé Chamley
Affiliation:
Laboratoire de Géologie Marine, Université d' Aix-Marseille II, Marseille, France
Neri Ciaranfi
Affiliation:
Institute of Geology, University of Bari, Bari, Italy
Sara d'Onofrio
Affiliation:
Institute of Geology, University of Bologna, Bologna, Italy
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Abstract

A deep-sea core over 16 m long from the crestal area of the Mediterranean Ridge has been investigated with different techniques, including quantitative micropaleontology, stable isotopes (measured on the epipelagic species Globigerinoides ruber and on the mesopelagic species Globorotalia inflata), and clay mineralogy. The resulting record of climatic fluctuations can be cross correlated to other Mediterranean cores by means of isochronous lithologies (tephra layers and sapropels). The climatic record of the Mediterranean is similar in character, phase, and chronology to the records investigated in the equatorial Pacific and in the Caribbean. Isotope stages 1 to 17 have been recognized. Cyclically repeated stagnant cycles resulting in sapropel deposition complicate both the isotopic and the faunal signal. The isotopic investigations reveal that the temperature change in the surface layers of the eastern Mediterranean was no greater than 8°C in the late “glacial” Pleistocene. The chronostratigraphic and biostratigraphic interpretation of Core KS09 indicate that the mean sedimentation rate was 2.4 cm/1000 years, a value very close to the 2.5 cm/1000 years calculated for the entire Quaternary section at DSDP Site 125, also located in the crestal area of the Mediterranean Ridge in the Ionian Basin. The base of KS09 is likely to be very close to the Brunhes/Matuyama boundary dated at 0.7 my.

Type
Research Article
Information
Quaternary Research , Volume 8 , Issue 2 , September 1977 , pp. 205 - 235
Copyright
University of Washington

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References

Berger, W.H., Gardner, J.56., (1975). On the determination of Pleistocene temperatures from planktonic foraminifera. Journal of Foraminiferal Research. 5, 2 102-113.Google Scholar
Biahchi, A.J.M., (1971). Distribution de certaines bactéries hétérotrophes aérobies dans les sédiments profonds de Méditerranée orientale. Marine Biology. 11, 2 106-117.Google Scholar
Blanc-Vernet, L., (1964). Contribution à l'étude des Foraminifères de Méditerranée. Relations entre la microfaune et le sédiment. Bioc noses actuelles, thanathocoenoses pliocènes et quaternaires. Doctoral Thesis. University of Marseille, 12/1967, 410 pages and 16 plates.Google Scholar
Blanc-Vernet, L., Contribution à l'étude des Foraminifères de Méditerranée. Relations entre la microfaune et le sédiment. Bioc noses actuelles, thanathocoenoses pliocènes et quaternaires. Records Tr. Stat. mar. Endoume. 48, 281.Google Scholar
Blanc-Vernet, L., Chamley, H., (1971). Sédimentation à attapulgite et Globigerinoides trilobus cf. dehiscens (P. & J.) dans une carotte profonde de Méditerranée. Deep Sea Research. 18, 631-637.Google Scholar
Bonadonna, F.P., Bigazzi, G., (1970). Datazione di tufi intratirreniani della zona di Cerveteri (Roma), mediante il metodo della tracce di fissione. Bollettino della Societa Geologica Italiana. 89, 463-473.Google Scholar
Brecker, W.S., Thurber, D.L., Goddaro, J., Ku, T.L., Matthes, R.K., Mesolella, K.J., (1968). Milankovich hypothesis supported by precise dating of coral reefs and deep-sea sediments. Science. 159, 297-300.Google Scholar
Broecker, W.S., Van Donk, J., (1970). Isolation changes, ice volumes and the O18 record in deep-sea cores. Review of Geophysical Space Physics. 8, 1 169-199.Google Scholar
Butlin, K.R., (1953). The bacterial sulphur cycle. Research. 6, 184-191.Google Scholar
Chamley, H., (1971). Recherches sur la sédimentation argileuse en Méditerranée. Sci. Geol. Strasbourg Mém.. 35, 225.Google Scholar
Chamley, H., (1973). Place des argiles marines parmi les divers indicateurs paléoclimatiques. Colloques Internationaux du Centre National de la Recherche Scientifique. Méthod. quantitat. ét. variat. climat au cours du Pléistoc. Gif-sur-Yvette, juin 1973. 25-37 no129.Google Scholar
Chamley, H., 1975a. Sédimentation argileuse en mer Tyrrhénienne au Plio-Pléistocène d'après l'étude du forage JOIDES 132. Bulletin Groupe Franc. Argiles. in press.Google Scholar
Chamley, M., 1975b. Sédimentation argileuse en mer Ionienne au Plio-Pleistocène d'après l'étude du forage JOIDES 125. Bulletin of the Society of Géological France. in press.Google Scholar
Cita, M.B., d'Onofrio, S., 'Onofrio, 1967. Climatic fluctuations in submarine cores from the Adriatic Sea (Mediterranean). Progress in Oceanography. 4, 161-178.Google Scholar
Cita, M.B., Chierici, M.A., Ciampo, G., Momcharmont Zei, M., d'Ohofrio, S., Ryan, W.B.F., Scorziello, R., (1973). The Quaternary record in the Tyrrhenian and Ionian basins of the Mediterranean. Ryan, W.B.F., Initial Reports of a Deep Sea Drilling Project. Vol. 13, 1263-1339 (2).Google Scholar
Cita, M.B., Ryan, W.B.F., (1973). The Pliocene record in deep-sea Mediterranean sediments. 5. Time-scale and general synthesis. Ryan, W.B.F., Initial Report of a Deep Sea Drilling Project. Vol. 13, 1405-1416 (2).Google Scholar
Cita, M.B., Ciampo, G., Ferone, E., Mohcharmont Zei, M., Scorziello, R., Taddei Ruggiero, E., (1974). II Quaternario del Tirreno abissale. Interpretazione stratigrafica e paleoclimatica del pozzo DSDP 132. Revista Española Micropaleontology. 6, 2 256-326.Google Scholar
Cita, M.B., d'Onofrio, S., Zocchi, M., (1974). Studi sul Pleistocene della Dorsale Mediterranea (Mare Ionio). Rivista Italiana Paleontologin e Stratigrafia. 80, 3 515-562.Google Scholar
Cita, M.B., Bigioggero, B., Ferrario, A., (1975). Micrometeorites in the “glacial” Pleistocene of the Mediterranean Ridge. Bollettino Societa Geologica Italiana. 94, 877.Google Scholar
Cita, M.B., Bigioggero, B., Ferrario, A., Micrometeorites in the “glacial” Pleistocene of the Mediterranean Ridge. Bollettino Societa Geologica Italiana. 94, 887.Google Scholar
Craig, M., (1965). The measurements of oxygen isotope paleotemperatures. Tongiorgi, E., Stable Isotopes in Oceanographic Studies and Paleotemperatures. GNR, Pisa, 161-192.Google Scholar
Debyser, J., (1961). Contribution à l'étude géochimique des vases marines. Technip.. IFP, Rueil-Malmaison, France, 239.Google Scholar
d'Onofrio, S., 'Onofrio, 1959. Foraminiferi di una carota sottomarina del medio Adriatico. Giornale di Geologia. 2, 27 147-194.Google Scholar
d'Onofrio, S., 'Onofrio, 1972. Foraminiferi di carote e campioni di fondo nell'Adriatico meridionale. Giornale di Geologia. 2, 38 449-512.Google Scholar
Duplessy, J.-C., (1972). La Géochimie des isotope stables du carbone dans la mer. Doctoral thesis. Paris.Google Scholar
Emiliani, C., 1955a. Pleistocene temperatures. Journal of Geology. 63, 538-573.Google Scholar
Emiliani, C., 1955b. Pleistocene temperature variations in the Mediterranean. Quaternaria. 2, 87-98.Google Scholar
Emiliani, C., (1966). Paleotemperature analysis of Caribbean Cores P 6304-8 and P 6304-9 and a generalized temperature curve for the last 425,000 years. Journal of Geol.. 74, 109-126.Google Scholar
Emiliani, C., (1971). Isotopic paleotemperatures and shell morphology of Globigerinoides rubra in the type section for the Pliocene/Pleistocene boundary. Micropaleontology. 17, 2 233-238.Google Scholar
Ericson, D.B., (1961). Pleistocene climate record in some deep-sea sediment cores. Annals of the New York Academy of Science. 95, 537-541.Google Scholar
Ericson, D.B., Wollin, W., (1986). Pleistocene climates and chronology in deep-sea sediments. Science. 162, 1227-1234.Google Scholar
Gordon, A.L., (1975). General ocean circulation. Numerical Models of Ocean Circulation. National Academy of Science, Washington, D. C, 39-53.Google Scholar
Herman, Y., (1972). Quaternary eastern Mediterranean sediments: micropaleontology and climatic record. Stanley, D.J., The Mediterranean Sea. Dowden, Hutchinson, & Ross, 129-147.Google Scholar
Hieke , W., (in press).Revision of the stratigraphy of the Late Quaternary eastern Mediterranean deep-sea sediments. ..Google Scholar
Imbrie, J., Kipp, N.G., (1971). A new micropaleontological method for quantitative micropaleontology: Application to a Late Pleistocene Caribbean Core. Turekian, K.K., Late Cenozoic Glacial Ages. Yale University Press, New Haven, 71-181.Google Scholar
Keller, J., Ninkovich, D., (1972). Tephra-Lagen in der Ägäis. Zeitschrift Deuthschen Geologischen, Gesellscaft. 123, 2 579-587.Google Scholar
Keller , J., Ryan , W. B. F., Ninkovich , D., and Altherr , R., (in press).200,000 years of Mediterranean explosive volcanic activity as recorded in deep-sea sediments. . Geological Society of America Bulletin . ..Google Scholar
Kidd , R. B., Cita , M. B., and Ryan , W. B. F., (in press).Stratigraphy and paleoenvironment of eastern Mediterranean sapropels. . In “Initial Reports of the Deep Sea Drilling Project”. , (Ryan , W. B. F., et al., Eds.), 57. 42A..Google Scholar
Ku, T.L., Broecker, W.S., (1966). Atlantic deep-sea stratigraphy: extension of absolute chronology to 320,000 years. Science. 151, 448-450.Google Scholar
Kullenberg, B., (1952). On the salinity of the water contained in marine sediments. Goteborg Kongl. Vet. Vitterh. Sam. Handl.. 6, 6 337 Series B.Google Scholar
McCoy, F.J., (1974). Late Quaternary sedimentation in the eastern Mediterranean Sea. Doctoral Dissertation. Harvard University, Cambridge, Mass. Google Scholar
Mellis, O., (1954). Volcanic ash-horizons in deep-sea sediments from the eastern Mediterranean. Deep Sea Research. 2, 89-92.Google Scholar
Menzies, R.J., Imbrie, J., Heezen, B.C., (1961). Further considerations regarding the antiquity of the abyssal fauna with evidence for a changing abyssal environment. Deep Sea Research. 8, 79-94.Google Scholar
Millot, G., (1964) Géologie des Argiles. Masson edition, Paris, 499.Google Scholar
Müller, C., Blanc-Vermet, L., Chamley, H., Froget, C., üller et al., 1975. les coccolithophorides d'une carotte méditerranéenne. Comparaison paléoclimatique avec les foraminifères, les ptéropodes et les argiles. Tethys. 6, 805-828.Google Scholar
Nesteroff, W.D., (1973). Petrography and mineralogy of sapropels. Ryan, W.B.F., Initial Reports of the Deep Sea Drilling Project. Vol. 13, 713-720 (2).Google Scholar
Ninkovich, D., Heezen, B.C., (1965). Santorini tephra: Submarine Geology and Geophysics. Proceedings of the 17th Symposium of the Colston Research Society. Bristol, 1965 413-453.Google Scholar
Ninkovich, D., Heezen, B.C., (1967). Physical and chemical properties of volcanic glass shards from Pozzolana ash, Thera Island, and from upper and lower layers in eastern Mediterranean deep-sea sediments. Nature. 213, 582-585.Google Scholar
Olausson, E., (1961). Studies of deep-sea cores. Reports of the Swedish Deep-Sea Expedition 1947–1948. 8, 4 323-438.Google Scholar
Olausson, E., (1965). Evidence of climatic changes in North Atlantic deep-sea cores with remarks on isotopic paleotemperature analysis. Progress in Oceanography. 3, 221-252.Google Scholar
Olausson, E., (1972). Tephrachronology and the Late Pleistocene of the Aegean Sea. Strid. Evolution of the Aegean, Opera Bot. 30, 29-39.Google Scholar
Olsson, J., (1959). Uppsala natural radiocarbon measurements. I. American Journal of Science, Radiocarbon supplement. 1, 87-102.Google Scholar
Parker, F.L., (1958). Eastern Mediterranean foraminifera. Reports of the Swedish Deep-Sea Expedition. 8, 4 217-283 1947–1948.Google Scholar
Parker, F.L., (1962). Planktonic foraminiferal species in Pacific sediments. Micropaleontology. 8, 2 219-254.Google Scholar
Pastouret, L., (1970). Etude sédimentologique et paléoclimatique de carottes prelevé es en Méditerranée orientale. Tethys. 2, 1 227-266.Google Scholar
Robert, C., (1974). Contribution à l'étude de la sédimentation argileuse en Méditerranée orientale. Thèse 3me cycle. University of Aix-Marseille, II, 82.Google Scholar
Robert, C., Chamley, M., (1974). Gypse et sapropels profonds de Méditerranée orientale. C. R. Academy of Science of Paris D. 278, 843-846.Google Scholar
Rossignol-Strick, M., (1955). Palynologie des sapropels Méditerranéens du Villafranchien à l'Holocène. Colloques Internationaux du Centre National Researche Scientifique. Méthod. quantitat. ét. variat. climat au cours du Pléistoc., Gif-sur-Yvette, juin 1973. 93-102 no129.Google Scholar
Rossignol-Strick, M., (1973). Palynologie des sapropels Méditerranéens du Villafranchien à l'Holocène. Colloques Internationaux du Centre National Researche Scientifique. . Méthod. quantitat. ét. variat. climat au cours du Pléistoc., Gif-sur-Yvette, juin 1973. 843 no129.Google Scholar
Rubin, M., Suess, H.E., (1955). U. S. Geological Survey radiocarbon dates II. Science. 121, 481-488.Google ScholarPubMed
Ruddiman, W.F., (1971). Pleistocene sedimentation in the equatorial Atlantic: Stratigraphy and Climatology. Geological Society of America Bulletin. 82, 283-302.Google Scholar
Ruddiman, W.F., McIntyre, A., (1976). Paleoceanography of the Quaternary North Atlantic. Joint Oceanographic Assembly, Edinburgh 1976. 20 Abstracts.Google Scholar
Ryan, W.B.F., (1969). The floor of the Mediterranean Sea. Doctoral Thesis. Columbia University, New York. Google Scholar
Ryan, W.B.F., (1972). Stratigraphy of Late Quaternary Sediments in the eastern Mediterranean. Stanley, D.J., The Mediterranean Sea. Dowden, Hutchinson & Ross, 149-170.Google Scholar
Ryan, W.B.F., Heezen, B.C., (1965). Ionian Sea submarine canyons and the 1908 Messina Turbidity current. Geology Society of America Bulletin. 76, 915-932.Google Scholar
Ryan, W.B.F., Hsü, K.J., ü, 1973 Initial Reports of the Deep Sea Drilling Project. Vol. 13, U. S. Government Printing Office, Washington, D. C, 1-1447 (1–2).Google Scholar
Ryan, W.B.F., Flood, J.D., (1973). Preliminary paleomagnetic measurements on sediments from the Ionian (Site 125) and Tyrrhenian (Site 132) Basins in the Mediterranean Sea. Ryan, W.B.F., Initial Reports of the Deep Sea Drilling Project. Vol. 13, 599-603 (2).Google Scholar
Savin, S.M., Douglas, R.G., (1973). Stable isotope and magnesium geochemistry of recent planktonic Foraminifera from the South Pacific. Geological Society of America Bulletin. 84, 2327-2342.Google Scholar
Shackleton, M.J., (1967). Oxygen isotope analysis and Pleistocene temperatures re-assessed. Mature (London). 218, 79-80.Google Scholar
Shackleton, M.J., Opdyke, M.D., (1973). Oxygen isotope and paleomagnetic stratigraphy of equatorial Pacific Core V28-238: Oxygen temperature and ice volume on a 105 year and 106 year scale. Quaternary Research. 3, 39-55.Google Scholar
Shackleton, M.J., Opdyke, M.D., (1976). Oxygen-isotope and paleomagnetic stratigraphy of Pacific Core V28-239. Late Pliocene to Latest Pleistocene. Geological Society of American Bulletin. 145, 449-464.Google Scholar
Thierstein , H., Molfino , B., Geitzemaurer , K., Shackleton , M. J., (in press).Synchroneity of Late Quaternary Coccolith Datums validated by Oxygen isotopes. ..Google Scholar
Todd, R., (1958). Foraminifera from western Mediterranean deep-sea cores. Reports of the Swedish Deep-Sea Expedition. 8, 2 1-167 1947–1948.Google Scholar
Venkatarathnam, K., Ryan, W.B.F., (1971). Dispersal pattern of clay minerals in the sediments of the eastern Mediterranean sea. Marine Geology. 11, 4 261-282.Google Scholar
Vergnaud-Grazzini, C., (1973). Etude écologique et isotopique de Foraminififères actuels et fossiles de Méditerranée. Doctoral Thesis. University of Paris. Google Scholar
Vergnaud-Grazzini, C., Herman-Rosenberg, Y., (1969). Etude paléoclimatique d'une carotte en Méditerranée orientale. Revue du Géographie Physique et du Géologie Dynamique. 11, 3 279-292.Google Scholar
Vergnaud-Grazzini, C., (1975). 18O changes in Foraminifera Carbonates during the last 105 years in the Mediterranean Sea. Science. 190, 272-274.Google Scholar
Vergnaud-Grazzini, C., Letolle, R., Glacon, G., (1974). Note préliminaire à l-étude isotopique 18O/16O) du groupe des Globigerinoides ruber d'Orbigny au Pleistocène inférieur en Mer Ionienne. Colloques Internationaux du Centre National de la Recherche Scientifique. . Méthod. quantitat. ét. variat. climat au cours du Pléist., Gif-sur-Yvette, juin 1973. 221-229 no129.Google Scholar