Mineralogy of deep-sea sediments around Reunion Island (Western Indian Ocean)

• Autorzy: Duczmal-Czernikiewicz Agata , Lorenc Stanisław , Stattegger Karl

Warianty tytułu

PL

Charakterystyka osadów z rejony wyspy Reunion (Zachodni Ocean Indyjski)

• Języki publikacji: EN

Abstrakty

EN

Detailed petrographic and mineralogical analyses were performed in order to determine and classify ocean sediments in the vicinity of Reunion Island. Surface sediments from the ocean floor and samples from cores of thickness down to 560 cm were classified as hemipelagic muds of volcanogenic origin, pelagic calcareous oozes and basaltic breccia. Heavy, light and pelitic fractions were investigated separately. Basaltic breccia consists of rock fragments and glass shards. Hemipelagic muds consist mostly of basaltic fragments, plagioclases, pyroxenes and olivines, basaltic glass shards, zeolites, and clay minerals. Moreover, various amounts of carbonate and siliceous bioclasts also occur. Pelagic oozes (nannoplankton and foraminifera) are composed mainly of carbonate bioclasts and micrite. The mineral composition of the sediments and the relationship between pelagic and volcanogenic components were determined referring to the depth and distance from the Reunion Island. The sediments from the southernmost profile are different than others taken at a smaller distance from the island not only with respect to the fossil assemblage but also with respect to the occurrence of concretions (and quartz, staurolite and apatite) and greater degree of glass alteration. These sediments were formed under the conditions of pelagic sedimentation, and so the slow sedimentation rate facilitated the formation of concretions. The mineral composition of the sediments differs according to the distance from the volcanic Reunion Island and the depth from which the sediment was sampled.

PL

Przedmiotem badań była charakterystyka osadów z rejonu wyspy Reunion na podstawie szczegółowej analizy petrograficznej i mineralogicznej. Osady z dna oceanu oraz rdzenie o długości do 560 cm (150 próbek) zostały zaklasyfikowane jako: hemipelagiczne muły wulkanogeniczne, pelagiczne muły węglanowe (nannoplanktonowe i otwornicowe) oraz wulkanogeniczna brekcja bazaltowa. Brekcję bazaltową tworzą okruchy skal bazaltowych i szkliwa wulkanicznego. Muły wulkanogeniczne składają się głównie z fragmentów skał bazaltowych, minerałów pochodzenia wulkanicznego (plagioklazów, piroksenów i oliwinów), okruchów szkliwa wulkanicznego, zeolitów oraz minerałów ilastych. Ponadto występują w zmiennych ilościach bioklasty węglanowe i podrzędnie krzemionkowe. Muły pelagiczne są utworzone głównie z bioklastów węglanowych oraz mikrytu. Skład mineralny oraz wzajemne relacje składników pelagicznych i wulkanogenicznych osadu są zdeterminowane głębokością i położeniem punktów badawczych względem wyspy. Osady z profilu położonego najbardziej na SE różnią się od innych położonych bliżej wyspy nie tylko zespołem skamieniałości, ale również występowaniem konkrecji (także kwarcu, staurolitu i apatytu) oraz większym stopniem przeobrażenia szkliwa wulkanicznego. Osady te powstawały w warunkach sedymentacji pelagicznej oraz powolnym tempem sedymentacji wyznaczonym przez formowanie się konkrecji. Skład mineralny osadów zależy od odległości od wulkanicznej wyspy Reunion oraz od głębokości, z której osad był pobrany.

Słowa kluczowe

EN

deep-sea sediments; mineralogy; Reunion Island

PL

osady głębokomorskie; mineralogia; wyspa Reunion

• Wydawca: Uniwersytet im. Adama Mickiewicza. Instytut Geologii
• Czasopismo: Geologos
• Rocznik: 2003
• Tom: Vol. 6
• Strony: 9--56
• Opis fizyczny: Bibliogr. 63 poz.

Twórcy

autor

Duczmal-Czernikiewicz Agata

• Institute of Geology, Adam Mickiewicz University, Poznań

autor

Lorenc Stanisław

• Institute of Geology, Adam Mickiewicz University, Poznań

autor

Stattegger Karl

• Institute of Geological Science, Kiel University, Germany

Bibliografia

• Albarede F., Tamagnan V., 1988: Modelling the recent geochemical evolution of the Piton de la Foumaise volcano, Reunion Island, 1931-1986. Journal of Petrolology, 29: 997-1030.
• Backman J., Duncan R.A., 1988: Scientific Results of the Ocean Drilling Program, 115: 17-41.
• Bassinot F.C., Beaufort L., Vincent E., Labeyrie L.D., Rostek F., Muller P.J., Qui-Delleur X., Lancelot Y., 1994: Coarse fraction fluctuations in pelagic carbonate sediments from the tropical Indian Ocean: A 1500-kyr record of carbonate dissolution. Paleoceanography, 9, 4: 579-600.
• Baxter A.N., 1985: Major and trace elements variation in basalts from leg 115. Scientific Results of the Ocean Drilling Program, 115: 19-21.
• Bearman G., 1997: Ocean chemistry and deep-sea sediments. The Open University, Pergamon, 134 pp.
• Berger W.H., 1981: Oxygen and carbon isotopes in foraminifera: an introduction. Pa- laeogeography, Palaeoclimatology, Palaeoecology, 33: 3-7.
• Berner R.A. 1971: Sedimentary piryte formation. An update. Geochimica Cosmochimica Acta, 48: 605-615.
• Burns R.G., Burns V.M., 1997, Marine Minerals. [In:] Bums R.G. (ed): Revews in Mineralogy, 6, 1-11.
• Daymond J., Corliss J.B., Cobler R., Muratli Ch.M., Chou Ch., Conrad R., 1980: Composition and origin of sediments recovered by deep drilling of sediment mounds, Galapagos spreading center. Initial Reports of the Deep Sea Drilling Project, 54: 377-385.
• Deer W.A., Howie R.A., Zussman J., 1997: Rock-forming minerals. Single-Chain Silicates. The Geological Society, London, 667 pp.
• Deniel C., Kieffer G., Lecointre J., 1992: New 230Th-238U and 14c age determinations from Piton des Neiges volcano, Reunion - A revised chronology for the Differentiated Series. Journal of Volcanology and Geothermal Research, 51: 253-267.
• Duczmal-Czernikiewicz A., 1999: Mineralogia osadów z rejonu wyspy Reunion (zachodni Ocean Indyjski). Unpublished PhD thesis, University of Poznań, 131 pp.
• Duncan R.A., Backman J., Peterson L., 1989: Reunion hot-spot activity through Tertiary time. Initial results from the Ocean Drilling Program. Journal of Volcanology and Geothermal Research, 36: 193-198.
• Duncan R.A., 1990: The volcanic record of the Reunion Hot-spot. Scientific Results of the Ocean Drilling Program, 115: 3-10.
• Duplessy J. C., Be A. W. H., Blanc P.L., 1981: Oxygen and carbon isotopic composition and biogeographic distribution of planctonic foraminifera in the Indian Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology, 33: 9-46.
• Fisher R.V., Schminke H.-U., 1984: Pyroclastic Rocks. Springer, Berlin-Heidelberg, 472 pp.
• Fretzdorff S., 1997: The Reunion Hotspot: History of explosive activity and geochemical evolution. Berichte Reports, Geologisch-Palaontologisches Institut Univ. Kiel, 81, 98 pp.
• Gillot P.-Y., Lefevre J.-C., Nativel R, 1994: Model for the structural evolution of the volcanoes of Reunion Island. Earth and Planetary Science Letters, 51: 253-267.
• Gillot R- Y., Nativel R, 1982: K-Ar chronology of the ultimate activity of Piton des Neiges volcano, Reunion Island, Indian Ocean. Journal of Volcanology and Geothermal Research, 13: 131-146.
• Gillot R- Y., Nativel R, 1989: Eruptive history of the Piton de la Fournaise volcano, Reunion Island, Indian Ocean. Journal of Volcanology and Geothermal Research, 36: 53-65.
• Glasby G. R, Emelyanov E. M., Zhamoida V. A., Baturin G. N., Leipe T., Bahlo R., Bonacker R, 1997: Enviroments of formation of ferromanganese concretions in the Baltic Sea: a critical review. [In:] K. Nicholson et al. (Eds.): Manganese mineralization: geochemistry and mineralogy of terrestrial and marine deposits. Geological Society of America Special Publ., 119: 213-237.
• Goldberg E. D., Griffin J. J., 1970: The sediments of the northern Indian Ocean. Deep Sea Research, 17: 513-537.
• Griffin J. J., Windom H., Goldberg E. D., 1968: The distribution of clay minerals in the World Ocean. Deep Sea Research, 15: 433-459.
• Iyer S.D., Shyam Pradas M., Gupta S.M., Charan S.N., Mukherjee A.D., 1997: Hydro volcanic activity in the Central Indian Ocean Basin. Does nature mimic laboratory experiments? Journal of Volcanology and Geothermal Research, 78: 209-220.
• Jackson M. L., 1975: The soil chemical analysis - Advanced course. 2nd edition. Published by the author, Madison, Visconsin, 877 pp.
• Kastner M., 1981: Autigenic silicates in deep-sea sediments formation and diagenesis. [In:] C. Emiliani (Ed): The Sea. The Oceanic Lithosphere. New York, 915-981.
• Kolla V., Biscaye P.E., 1973: Clay mineralogy and sedimentation in the eastern Indian Ocean. Deep Sea Research, 20: 727-738.
• Kolla V., Biscaye P.E., 1977: Distribution and origin of quartz in the sediments of the Indian Ocean. Journal of Sedimentary Petrology, 47: 642-649.
• Kolla V., Henderson L., Biscaye P.E., 1976: Clay mineralogy and sedimentation in western Indian Ocean. Deep Sea Research, 23: 949-961.
• Lacroix A., 1936: Le Volcan Actif de File de la Reunion et ses Produits. Paris, Gauthiers-Villars, 297 pp.
• Lenat J.-P., Vincent R, Bachelery R, 1989: The offshore continuation of an active basaltic volcano: Piton de la Foumaise (Reunion Island, Indian Ocean) structural and geomorphological interpretation of Sea Beam mapping. Journal of Volcanology and Geothermal Research, 36: 1-36.
• Ludden J.N., 1978: Magmatic evolution of the basaltic shield volcanoes of Reunion Island. Journal of Volcanology and Geothermal Research, 4: 171-198.
• MacDonald G.A., Katsura T., 1964. Chemical composition of Hawaiian Lavas. Journal of Petrology, 5: 82-133.
• McDougall I., 1971: The geochronology and evolution of the young volcanic island of Reunion, Indian Ocean. Geochimica at Cosmochimica Acta, 35: 261-288.
• Molnar R, Stock J., 1987: Relative motion of hotspots in the Pacific, Atlantic and Indian Oceans since Late Cretaceous time. Nature, 327: 587-591.
• Moore D.M., Reynolds R.C. Jr., 1998: X-ray diffraction and the identification and analysis of clay minerals. Oxford University Press, New York, 332 pp.
• Morgan, W.J., 1981: Hot-spot tracks and the opening of the Atlantic and Indian Oceans. [In:] C. Emiliani (Ed.): The Sea. The Oceanic Lithosphere, New York, 443-487.
• Nercessian A., Hirn, A., Lepine J-C., Sapin, M., 1996: Internal structure of Piton de la Furnaise volcano from seismic wave propagation and earthquake distribution. Journal of Volcanology and Geothermal Research, 70: 123-143.
• Ollier G., Cochonat J.F., Lenat J.F., Labazuy R, 1998: Deep-sea volcaniclastic sedimentary systems: an example from La Fournaise volcano, Reunion Island, Indian Ocean. Sedimentology, 45: 293-330.
• Orton G. J., 1997: Volcanic environments. [In:] H.G. Reading (Ed.): Sedimentary environments and facies. Blackwell Scientific Publications, Oxford, 485-567.
• Pablo-Galan L., Chavez-Garcia M., 1996: Diagenesis of Oligocene vitric tufs to zeolites, Mexican Volcanic Belt. Clays & Clay Minerals, 44: 324-338.
• Philippot F., 1984: La sedimentation volcanogene recente autour del lie de la Reunion., Unpublished, Universite de Paris-Sud, Orsay, 187 pp.
• Piper D.Z., Blueford J.R., 1982: Distribution, mineralogy, and texture of manganese nodules and their relation to sedimentation at DOMES Site A in the equatorial North Pacific. Deep Sea Research, 29: 927-952.
• Robinson P.T., Von Herzen R.P. 1989: College Station. Scientific Results of the Ocean Drilling Program, 118: 3-235.
• Rocher R, Westercamp D., 1989: The Salazie Cirque ignimbrite (Piton des Neiges Volcano, Reunion Island): chronostratigraphy, description and significance of lithic fragments and eruptive machanisms. Journal of Volcanology and Geothermal Research, 36: 177-191.
• Rothwell R.G., 1987: The mineralogy of marine sediments. Elsevier Sc. Publ., Amsterdam, 234 pp.
• Sapin, M., Hirn, A., Lepine J-C., Nercessian A., 1996: Stress, failure and fluid flow deduced from earthquakes accompanying eruptions at Piton de la Furnaise volcano. Journal of Volcanology and Geothermal Research, 70, 145-167.
• Shiftman R, Southard R.J., 1996: Cation exchange capacity of layer silicates and palagonitized glass in mafic volcanic rocks: a comparative study of bulk extraction and in situ techniques. Clays & Clay Minerals, 44, 5: 624-634.
• Schiffman R, Staudigel H., 1995: The smectite to chlorite transition in a fossil seamount hydrotermal system: the Basement Complex of La Palma, Canary Islands. Journal of Metamorphic Geology, 13: 487-498.
• Seibold E., Berger W.H., 1996: The sea floor. An introduction to marine geology. Springer Verlag. Berlin, 356 pp.
• Singer A., 1974: Mineralogy of palagonitic material from the Golan Hights, Israel. Clays & Clay Minerals, 22, 3: 231-240.
• Stoffers R, Devey C., Ackermand D., Berner Z., Cantin B., Durand J., Franke- Bruckmaier B., Fretzdorff S., Graupner T., Haug G„ Heikinian R., Labazuy R, Lorenc S., Muhlhan S., Muhlhan N., Parterne M., Schmidt M., Stattegger K„ Uhlig S., Whitechurch H., 1994: Cruise report S087: The Reunion Hotspot. Berichte-Reports, Geologische-Palaontogisches Institut Univ. Kiel, 65, 71 pp.
• Tilley C.E., Thompson R.N., Wadsworth W.J., Upton B.G.J., 1971: Melting relations of some lavas of Reunion Island, Indian Ocean. Mineralogical Magazine, 38: 344-352.
• Trokowicz D., 1998: Genesis of ferromanganese nodules in the Baltic Sea. Prace PIG, 163: 1-62.
• Tucker M.E., Wright V.P., 1990: Carbonate sedimentology. Blackwell Sc. Publ., Oxford, 482 pp.
• Underwood M.B., Pickering K„ Gieskes J.M., Kastner M„ Orr R., 1993: Sediment geochemistry, clay mineralogy, and diagenesis: a synthesis of data from Leg 131, Nankai Trough. Scientific Results of the Ocean Drilling Program, 131: 343-362.
• Upton B.G.J., Wadsworth W.J., 1965: Geology of Reunion Island, Indian Ocean. Nature, 207: 151-154.
• Upton B.G.J., Wadsworth W.J., 1966: The basalts of Reunion Island, Indian Ocean. Bulletin of Volcanology, 29: 7-24.
• Upton B.G.J., Wadsworth W.J., 1972a: Peridotic and Gabbroic Rocks Associated with the Shield-Forming Lavas of
• Reunion. Contributions to Mineralogy & Petrology, 35: 139-158.
• Upton B.G.J., Wadsworth W.J., 1972b: Aspects of magmatic evolution on Reunion Island. Philosophical Transactions of the Royal Society of London, A., 271: 105-130.
• Van Der Flier-Keller E., 1991: Geochemistry and mineralogy of sediments, Atlantis II Fracture Zone, southwestern Indian Ocean. Scientific Results of the Ocean Drilling Program, 118: 145-151.
• Zevenbergen C., Van Reeuwijk L.P, Bradley J.P., Bloemen P, Comans R.N.1, 1996: Mechanism and conditions of clay formation during natural weathering of MSWI bottom ash. Clays & Clay Minerals, 44, 4: 546-552.

Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).