BENTHIC FORAMINIFERA ASSOCIATED WITH THE ZOOXANTHELLATE CORAL CLADOCORA IN THE PLEISTOCENE OF THE KOS ISLAND (AEGEAN SEA, GREECE): SEA LEVEL CHANGES AND PALAEOENVIRONMENTAL CONDITIONS
Περίληψη
A Pleistocene section, cropping out in the northern Kos Island has been selected for study. The main lithology (clayey sands, sandy marls) of the section is interrupted by a prominent Cladocora bank which allows a proper extraction of its faunal contents and identification at species level. The evaluation of benthic foraminiferal assemblages from this bank helps to determine the range of the environmental controls in sedimentation. The foraminiferal assemblage is related to a relatively high supply of organic material and rather strong current intensities in water depth of the coral growth. We suggest that the fossil reef of Cladocora grew in coastal waters characterised by a marked seasonality, with periodical inputs of terrigenous sediments, moderate turbidity and higher temperature than today. Such results, although preliminary, suggest that Cladocora together with benthic foraminifera could be reference species for future work on changing Mediterranean climate and sea level.
Λεπτομέρειες άρθρου
- Πώς να δημιουργήσετε Αναφορές
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Drinia, H., Koskeridou E., K. E., Antonarakou A., A. A., & Tzortzaki, E. (2010). BENTHIC FORAMINIFERA ASSOCIATED WITH THE ZOOXANTHELLATE CORAL CLADOCORA IN THE PLEISTOCENE OF THE KOS ISLAND (AEGEAN SEA, GREECE): SEA LEVEL CHANGES AND PALAEOENVIRONMENTAL CONDITIONS. Δελτίο της Ελληνικής Γεωλογικής Εταιρείας, 43(2), 613–619. https://doi.org/10.12681/bgsg.11223
- Ενότητα
- Παλαιοντολογία, Στρωματογραφία και Ιζηματολογία
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Λήψεις
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Αναφορές
Aguirre, J., Jiménez, A.P. 2008. Fossil analogues of present-day Cladocora caespitose coral banks: Sedimentary
setting, dwelling community and taphonomy (Late Pliocene, W. Mediterranean), Coral
Reefs 17, 203–213.
Albani, A., Serandrei Barbero, R. 1990. I foraminiferi della laguna e del Golfo di Venezia, Memorie di
Scienze Geologiche (Padova) 42, 271–341.
Altherr, R., Keller, J., Kott, K. 1976. Der jungtertiäre Monzonit von Kos und sein Kontaktof (Agäis, Griechenland),
Bulletin de la Société Géologique de France 7, 403–412.
Altherr, R., Kreuzer, H., Wendt, I., Lenz, H., Wagner, G.A., Keller, J., Harre, W., Höhndorf, A. 1982. A
late Oligocene/early Miocene high temperature belt in the Attic-Cycladic Crystalline Comples (SE
Pelagonian, Greece, N. Jahrb. Geol. E23, 97–164.
Altherr, R., Kreuzer, H., Lenz, H., Wendt, I., Harre, W., Dürr, S. 1994. Further evidence for a late Cretaceous
low-pressure/high temperature terrane in the Cyclades, Greece, Chimie der Erde 54, 319–328.
Bardintzeff, J.-M., Dalabakis, P., Traineau, H., Brousse, R. 1989. Recent explosive volcanic episodes on
the Island of Kos (Greece): associated hydrothermal parageneses and geothermal area of Volcania,
Terra Res. I, 15–78.
Barmawidjaja, D.M., Jorissen, F.J., Puskaric, S., van der Zwaan, G.J. 1992. Microhabitat selection by
benthic foraminifera in the northern Adriatic Sea, J. Foram. Res. 22, 297−317.
Bernasconi, M.P., Corselli, C., Carobene, L. 1997. A bank of the scleractinian coral Cladocora caespitosa
in the Pleistocene of the Crati valley (Calabria, southern Italy): growth versus environmental
conditions, Boll. Soc. Paleontol. Ital. 36, 53–61.
Béthoux, J.P., Gentili, B., Raunet, J., Taillez, D. 1990. Warming trend in the Western Mediterranean Deep
Water, Nature 347, 660–662.
Böger, H., Gersonde, R., Willman, R. 1974. Das Neogen im Osten der Insel Kos (Agäis, Dodekanes) –
Stratigraphie und Tektonik, Neues Jahrbuch Geologie und Palaeontologie Abh. 145, 129–152.
Cimerman, F., Langer, M.R. 1991. Mediterranean Foraminifera, Slovenska Academia Znanosti in Umetnosti,
Ljubljania, 119 pp.
Debenay, J.P., Guillou, J.J., Redois, F., Geslin, E. 2000. Distribution trends of foraminiferal assemblages
in paralic environments: a base for using foraminifera as bioindicators, In: Martin, R.E. (ed.), Environmental
Micropaleontology, Topics in Geobiology 15, New York: Kluwer Acad. & Plenum Publ.,
–67.
Donnici, S., Serandrei-Barbero, R., 2005. I foraminiferi di ambiente vallivo della Laguna di Venezia, Lavori
Societa` Veneziana Scienze Naturali 30, 25–36.
Dornbos, S.Q., Wilson, M.A. 1999. Paleoecology of a Pliocene coral reef in Cyprus: recovery of a marine
community from the Messinian salinity crisis, N. Jahrb Geol. Palaeontol Abh, 21, 103–118.
Dürr, St., Jacobschagen, V. 1986. Ostägäische Inseln, In: Jacobshagen, V. (ed.) Geologie von Griechenland,
Berlin, Gebrüder Borntraeger, 169–187.
Gralla, P. 1982. Das Präneogen der Insel Kos (Dodekanes, Griechenland), PhD Thesis, University of
Braunschweig, 182 pp.
Hayward, B.W Sa;baa, A.T., Grenfell, H.R. 2004. Benthic foraminifera and the Late Quaternary (last 150
ka) paleoceanographic and sedimentary history of the Bounty Trough, east of New Zealand, Palaeogeography
Palaeoclimatology Palaeoecology 211(1-2), 59-93.
Henjes-Kunst, F., Altherr, R., Kreuzer, H., Hansen, B.T. 1988. Disturbed U-Th-Pb systematic of young
zircons and uranothorites: the case of the Miocene Aegean granitoids (Greece), Chemical Geology 73,
-145.
XLIII, No 2 – 618
Jacobshagen, V. 1986. Introduction, In: Jacobshagen, V. (ed.) Geologie von Griechenland, Berlin, Gebrüder
Borntraeger, 1-9.
Jorissen, F.J. 1987. The distribution of benthic foraminifera in the Adriatic Sea, Marine Micropaleontology
, 21–48.
Jorissen, F.J. 1988. Benthic foraminifera from the Adriatic Sea: priniciples of phenotypic variation.,
Utrecht Micropaleontological Bulletins 37, 1-174.
Fiorini, F., Vaiani, S.C. 2001. Benthic foraminifers and transgressive-regressive cycles in the Late Quaternary
subsurface sediments of the Po Plain near Ravenna (Northern Italy), Bollettino della Società
Paleontologica Italiana, 40, 357-403.
Kalt, A., Altherr, R., Ludwig, T. 1998. Contact Metamorphism in Pelitic Rocks on the Island of Kos (Greece,
Eastern Aegean Sea): a test for the Na-in- cordierite thermometer, Journal of Petrology, 663-668.
Keller, J. 1969. Origin of thyolites by anatectic melting of granitic crustal rocks. The example of rhyolitic
pumice from the island of Kos (Aegean Sea), Bulletin Volcanologique 33, 942-956.
Langer, M.R, 1993. Epiphytic foraminifera, Marine Micropaleontology 20, 235–265.
Murray, J.W. 1991. Ecology and palaeoecology of benthic foraminifera. Longman, Harlow, 397pp.
Murray, J.W. 2006. Ecology and applications of Benthic Foraminifera. Cambridge University Press, Cambridge,
pp
Peirano, A., Morri, C., Mastonuzzi, G., Bianchi, C.N. 1998. The coral Cladocora caespitosa (Anthozoa,
Scleractonia) as a bioherm builder in the Mediterranean Sea, Mem. Descr. Carta Geol. It. 52, 59-74.
Peirano, A., Abbate, M., Cerrati, G., Difesca, V., Peroni, C., Rodolfo-Metalpa, R. 2005. Monthly variations
in calyx growth, polyp tissue and density banding of the Mediterranean scleractinian Cladocora
caespitosa (L.), Coral Reefs 19, 404-409.
Schiller, C. 1993a. Ecology of the symbiotic coral Cladocora caespitosa (L.) (Faviidae, Scleractinia) in
the Bay of Piran (Adriatic Sea): I Distribution and biometry. Marine Ecology 14, 205-219.
Seidel, E., Schliestedt, M., Kreuzer, H., Harre, W. 1977. Metamorphic rocks of late Jurassic age as components
of the ophiolitic mélange on Gavdos and Crete (Greece), Geologisches Jahrbuch B28, 3-21.
Seidel, E., Kreuzer, H., Harre, W. 1982. A late Oligocene/early Miocene high pressure belt in the external
Hellenides, Geologcisches Jahrbuch E23, 165-206.
Sen Gupta, B.K. 1999. Foraminifera in marginal marine environments, In: Sen Gupta B.K. (ed) Modern
foraminifera, Kluwer, Dordrecht, 141–159.
Sgarrella, F., Moncharmon-Zei, M. 1993. Benthic foraminifera in the Gulf of Naples (Italy): systematic
and autoecology, Boll. Soc. Paleont. Ital. 32, 145-264.
Van der Zwaan, G.J., Jorissen, F.J. 1991. Biofacial patterns in river induced shelf anoxia. Geol. Soc. Spec.
Publ. 58, 65-82.
Willmann, R. 1983. Neogen und jungtertiäre Enwicklung der Insel Kos (Agäis, Griechenland), Geologische
Rundschau 72, 815–860.
Yassini, I., Jones, B.G. 1995. Foraminiferida and Ostracoda from estuarine and shelf environments on the
southeastern coast of Australia, University of Wollongong Press, Wollongong, 484 pp.
Zibrowius, H. 1974. Oculina patagonica, scléractiniaire hermatypique introduit en Méditerranée, Helgoländer
Wissenschaftliche Meeresuntersuchungen 26 (2), 153-173
Zibrowius, H. 1980. Les Scléractinaires de la Méditerranée et de l’ Atlantique nord-oriental, Mém. Inst.
Océanogr. 11, 1-284
