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Late Quaternary Eolian Deposition in Central Italy

Published online by Cambridge University Press:  20 January 2017

Biancamaria Narcisi
Biancamaria Narcisi*
Affiliation:
ENEA - C.R. Casaccia, C.P. 2400, 00100, Rome, Italy, E-mail: [email protected]
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Abstract

Records of eolian quartz from two continuous sediment sequences drilled in Lagaccione and Lago di Vico volcanic lakes in central Italy contribute to the knowledge of eolian deposition in the central Mediterranean during the last 100,000 years. The chronology is based on 14C and 40Ar/39Ar dating and tephra analysis. Pollen data provide the paleoenvironmental framework and enable correlation between the cores. Eolian inputs were high during the steppe phases corresponding to oxygen isotope stages 4 and 2. Low inputs correspond to the forest phases of the last interglacial and the middle Holocene. Eolian inputs have increased in the late Holocene. Patterns of eolian deposition in central Italy resemble the Antarctic dust record from the Vostok ice core. The Italian patterns may also correspond with hydrological changes registered in North Africa. The main source of dust loading over the Mediterranean now, North Africa, may have played an important role in dust supply throughout the last climatic cycle.

Keywords

eolian quartzlacustrine sedimentscentral Italylate Quaternary
Type
Research Article
Information
Quaternary Research , Volume 54 , Issue 2 , September 2000 , pp. 246 - 252
Copyright
University of Washington

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References

Adams, J. M. (1997). Global Land Environments since the Last Interglacial. Oak Ridge National Laboratory,TN., http://www.esd.ornl.gov/ern/qen/nerc.html.Google Scholar
Antoine, P, Rousseau, D.-D, Lautridou, J.-P, Hatté, C(1999). Last interglacial–glacial climatic cycle in loess–palaeosol successions of north-western France. Boreas, 28, 551–563.Google Scholar
Bergametti, G, Gomes, L, Remoudaki, E, Desbois, M, Martin, D, Buat-Ménard, P. Present transport and deposition patterns of African dusts to the north-western Mediterranean. Leinen, M, Sarnthein, M(1989). Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport.227–252.Google Scholar
Biscaye, P.E, Grousset, F.E, Revel, M, Van der Gaast, S, Zielinski, G.A, Vaars, A, Kukla, G(1997). Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 ice core, Summit, Greenland. Journal of Geophysical Research, 102, 26,765–26,781.Google Scholar
Chester, R, Sharples, E.J, Sanders, G.S, Saydam, A.C(1984). Saharan dust incursion over the Tyrrhenian Sea. Atmospheric Environment, 18, 929–935.Google Scholar
Coudé-Gaussen, G. Local, proximal and distal Saharan dusts: Characterization and contribution to the sedimentation. Leinen, M, Sarnthein, M(1989). Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport.339–358.Google Scholar
Coudé-Gaussen, G (1990). The loess and loess-like deposits along the sides of the western Mediterranean sea: Genetic and palaeoclimatic significance. Quaternary International, 5, 1–8.Google Scholar
Cowgill, U.M, Hutchinson, G.E(1970). Chemistry and mineralogy of the sediments and their source materials. Hutchinson, G.E Ianula: An Account of the History and Development of the Lago di Monterosi, Latium, Italy 37–101.Google Scholar
Cremaschi, M (1990). Stratigraphy and palaeoenvironmental significance of the loess deposits on Susak Island (Dalmatian archipelago). Quaternary International, 5, 97–106.Google Scholar
Cremaschi, M (1990). The loess in northern and central Italy: A loess basin between the Alps and the Mediterranean region. Quaderni di Geodinamica Alpina e Quaternaria, 1, 1–187.Google Scholar
Cremaschi, M (1990). Sedimentazione loessica nel bacino padano–adriatico durante il Pleistocene superiore. Memorie della Società Geologica Italiana, 45, 843–856.Google Scholar
Cremaschi, M, Fedoroff, N, Guerreschi, A, Huxtable, J, Colombi, N, Castelletti, L, Maspero, A(1990). Sedimentary and pedological processes in the Upper Pleistocene loess of Northern Italy. The Bagaggera sequence. Quaternary International, 5, 23–38.Google Scholar
d'Almeida, G.A (1986). A model for Saharan dust transport. Journal of Climate and Applied Meteorology, 25, 903–916.Google Scholar
De Angelis, M, Barkov, N.I, Petrov, V.N(1987). Aerosol concentrations over the last climatic cycle (160 kyr) from an Antarctic ice core. Nature, 325, 318–321.CrossRefGoogle Scholar
De Angelis, M, Gaudichet, A(1991). Saharan dust deposition over Mont Blanc (French Alps) during the last 30 years. Tellus, 43B, 61–75.CrossRefGoogle Scholar
De Angelis, M, Steffensen, J.P, Legrand, M, Clausen, H, Hammer, C(1997). Primary aerosol (sea salt and soil dust) deposited in Greenland ice during the last climatic cycle: Comparison with east Antarctic records. Journal of Geophysical Research, 102, 26,681–26,698.Google Scholar
Debard, E (1987). L'apport allochtone éolien dans les remplissages karstiques quaternaires du Bas-Vivarais (S. E. France). Bulletin de l'Association française pour l'étude du Quaternaire, 4, 183–193.CrossRefGoogle Scholar
Derbyshire, E (1995). Aeolian sediments in the Quaternary record. Quaternary Science Reviews, 14, 641–809.Google Scholar
Follieri, M, Giardini, M, Magri, D, Sadori, L(1998). Palynostratigraphy of the last glacial period in the volcanic region of Central Italy. Quaternary International, 47/48, 3–20.Google Scholar
Frezzotti, M, Giraudi, C(1990). Late Glacial and Holocene aeolian deposits and geomorphological features near Roccaraso (Abruzzo-Central Italy). Quaternary International, 5, 89–95.Google Scholar
Frezzotti, M, Giraudi, C(1990). Sedimenti eolici tardopleistocenici ed olocenici nell'Appennino centrale. Memorie della Società Geologica Italiana, 45, 883–886.Google Scholar
Fuhrer, K, Neftel, A, Anklin, M, Maggi, V(1993). Continuous measurements of hydrogen peroxide, formaldehyde, calcium and ammonium concentrations along the new GRIP ice core from Summit, central Greenland. Atmospheric Environment, 27A, 1873–1880.Google Scholar
Gasse, F (2000). Hydrological changes in the African tropics since the Last Glacial Maximum. Quaternary Science Reviews, 19, 189–211.Google Scholar
Giraudi, C (1995). Sedimenti eolici, variazioni climatiche ed influenza antropica: Considerazioni su alcune piane intermontane dell'Appennino Abruzzese. Il Quaternario, 8, 211–216.Google Scholar
Nature, 364, (1993). 203–207.CrossRefGoogle Scholar
Grousset, F.E, Biscaye, P.E, Revel, M, Petit, J.R, Pye, K, Joussaume, S, Jouzel, J(1992). Antarctic (Dome C) ice core dust at 18 k.y. B.P.: Isotopic constraints on origins. Earth and Planetary Science Letters, 111, 175–182.CrossRefGoogle Scholar
Grousset, F.E, Rognon, P, Coudé-Gaussen, G, Pédemay, P(1992). Origins of peri-Saharan dust deposits traced by their Nd and Sr isotopic composition. Palaeogeography, Palaeoclimatology, Palaeoecology, 93, 203–212.Google Scholar
Grousset, F.E, Parra, M, Bory, A, Martinez, P, Bertrand, P, Shimmield, G, Ellam, R.M(1998). Saharan dust regimes traced by the Sr–Nd isotopic composition of subtropical atlantic sediments: Last Glacial Maximum vs today. Quaternary Science Reviews, 17, 395–409.Google Scholar
Guerzoni, S, Chester, R(1996). The Impact of Desert Dust across the Mediterranean. Kluwer Academic, Dordrecht.Google Scholar
Guerzoni, S, Molinaroli, E, Chester, R(1997). Saharan dust inputs to the western Mediterranean Sea: Depositional patterns, geochemistry and sedimentological implications. Deep-Sea Research II, 44, 631–654.Google Scholar
Hooghiemstra, H, Stalling, H, Agwu, C.O.C, Dupont, L.M(1992). Vegetational and climatic changes at the northern fringe of the Sahara 250,000–5000 years B.P.: Evidence from 4 marine pollen records located between Portugal and the Canary Islands. Review of Palaeobotany and Palynology, 74, 1–53.Google Scholar
Hovan, S.A, Rea, D.K, Pisias, N.G, Shackleton, N.J(1989). A direct link between the China loess and marine δ18O records: Aeolian flux to the north Pacific. Nature, 340, 296–298.Google Scholar
Janecek, T.R, Rea, D.K. Pleistocene fluctuations in Northern Hemisphere trade winds and westerlies. Berger, A.L(1984). Milankovitch and Climate.331–347.Google Scholar
Kolla, V, Biscaye, P.E, Hanley, A.F(1979). Distribution of quartz in Late Quaternary Atlantic sediments in relation to climate. Quaternary Research, 11, 261–277.Google Scholar
Krom, M.D, Cliff, R.A, Eijsink, L.M, Herut, B, Chester, R(1999). The characterisation of Saharan dusts and Nile particulate matter in surface sediments from the Levantine basin using Sr isotopes. Marine Geology, 155, 319–330.CrossRefGoogle Scholar
Kukla, G.J (1977). Pleistocene land–sea correlations. I. Europe. Earth Science Reviews, 13, 307–374.CrossRefGoogle Scholar
Kukla, G, An, Z(1989). Loess stratigraphy in central China. Palaeogeography, Palaeoclimatology, Palaeoecology, 72, 203–225.Google Scholar
Laurenzi, M. A., Villa, I. M.(1985). K/Ar Chronology of the Vico Volcano (Latium, Italy). IAVCEI Scientific Assembly,Giardini Naxos.,Abstract.Google Scholar
Legrand, M.R, Lorius, C, Barkov, N.I, Petrov, V.N(1988). Vostok (Antarctica) ice core: Atmospheric chemistry changes over the last climatic cycle (160,000 years). Atmospheric Environment, 22, 317–331.CrossRefGoogle Scholar
Lenaz, R, Landuzzi, V, Tomadin, L(1986). Apports et concentrations de masse des poussières éoliennes sur le bassin oriental et occidental de la Méditerranée. Memorie della Società Geologica Italiana, 36, 189–200.Google Scholar
Lézine, A.-M (1989). Late Quaternary vegetation and climate of the Sahel. Quaternary Research, 32, 317–334.Google Scholar
Littmann, T. Recent African dust deposition in West Germany—Sediment characteristics and climatological aspects. Okuda, S, Rapp, A, Linyuan, Z(1991). Loess—Geomorphological Hazards and Processes.57–73.Google Scholar
Lorius, C, Jouzel, J, Ritz, C, Merlivat, L, Barkov, N.I, Korotkevich, Y.S, Kotlyakov, V.M(1985). A 150,000-year climatic record from Antarctic ice. Nature, 316, 591–596.Google Scholar
Loÿe-Pilot, M.D, Martin, J.M, Morelli, J(1986). Influence of Saharan dust on the rain acidity and atmospheric input to the Mediterranean. Nature, 321, 427–428.CrossRefGoogle Scholar
Magri, D (1999). Late Quaternary vegetation history at Lagaccione near Lago di Bolsena (central Italy). Review of Palaeobotany and Palynology, 106, 171–208.CrossRefGoogle Scholar
Magri, D, Sadori, L(1999). Late Pleistocene and Holocene pollen stratigraphy at Lago di Vico (central Italy). Vegetation History and Archaeobotany, 8, 247–260.Google Scholar
Mees, F, Verschuren, D, Nijs, R, Dumont, H(1991). Holocene evolution of the crater lake at Malha, Northwest Sudan. Journal of Paleolimnology, 5, 227–253.Google Scholar
Narcisi, B (1999). Nuovi ritrovamenti del tephra tardiglaciale etneo in Italia Centrale. Il Quaternario, 12, 69–78.Google Scholar
Narcisi, B, Anselmi, B, Catalano, F, Dai Pra, G, Magri, G(1992). Lithostratigraphy of the 250,000 year record of lacustrine sediments from the Valle di Castiglione crater, Roma. Quaternary Science Reviews, 11, 353–362.Google Scholar
Narcisi, B, Anselmi, B(1998). Sedimentological investigations on a Late Quaternary lacustrine core from the Lagaccione crater (Central Italy): Palaeoclimatic and palaeoenvironmental inferences. Quaternary International, 47/48, 21–28.Google Scholar
Narcisi, B, Vezzoli, L(1999). Quaternary stratigraphy of distal tephra layers in the Mediterranean—an overview. Global and Planetary Change, 21, 31–50.Google Scholar
Nihlén, T, Mattsson, J.O, Rapp, A, Gagaoudaki, C, Kornaros, G, Papageorgiou, J(1995). Monitoring of Saharan dust fallout on Crete and its contribution to soil formation. Tellus, 47B, 365–374.Google Scholar
Petit, J.R, Mounier, L, Jouzel, J, Korotkevich, Y.S, Kotlyakov, V.I, Lorius, C(1990). Palaeoclimatological and chronological implications of the Vostok core dust record. Nature, 343, 56–58.Google Scholar
Petit-Maire, N, Damnati, B. Climatic change in the present-day Saharan area over the last 140 ka. Le Bolloch, O, Repetto, C(1995). The Impact of African Dust across the Mediterranean—Abstract Book. Oristano, Google Scholar
Petit-Maire, N. Interglacial environments in presently hyperarid Sahara: Palaeoclimatic implications. Leinen, M, Sarnthein, M(1989). Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport.637–661.Google Scholar
Porter, S.C. Volcanic records and loess deposits. Bradley, R.S(1989). Global Changes of the Past. UCAR/OIES Global Change Institute, Boulder.295–320.Google Scholar
Prodi, F, Fea, G(1979). A case of transport and deposition of Saharan dust over the Italian peninsula and Southern Europe. Journal of Geophysical Research, 84, 6951–6960.CrossRefGoogle Scholar
Pye, K (1987). Aeolian Dust and Dust Deposits. Academic Press, San Diego.Google Scholar
Ram, M, Koenig, G(1997). Continuous dust concentration profile of pre-Holocene ice from the Greenland Ice Sheet Project 2 ice core: Dust stadials, interstadials, and the Eemian. Journal of Geophysical Research, 102, Google Scholar
Rapp, A, Nihlén, T. Desert dust-storms and loess deposits in North Africa and South Europe. Okuda, S, Rapp, A, Linyuan, Z(1991). Loess—Geomorphological Hazards and Processes.43–55.Google Scholar
Rea, D.K (1994). The paleoclimatic record provided by eolian deposition in the deep sea: The geological history of wind. Reviews of Geophysics, 32, 159–195.Google Scholar
Roberts, N (1990). Ups and downs of African lakes. Nature, 346, 107 CrossRefGoogle Scholar
Robinson, C (1994). Lago Grande di Monticchio, southern Italy: A long record of environmental change illustrated by sediment geochemistry. Chemical Geology, 118, 235–254.Google Scholar
Ruddiman, W.F (1997). Tropical Atlantic terrigenous fluxes since 25,000 yr B.P. Marine Geology, 136, 189–207.Google Scholar
Sarnthein, M (1978). Sand deserts during glacial maximum and climatic optimum. Nature, 272, 43–46.CrossRefGoogle Scholar
Sarnthein, M, Tetzlaff, G, Koopmann, B, Wolter, K, Pflaumann, U(1981). Glacial and interglacial wind regimes over the eastern subtropical Atlantic and north-west Africa. Nature, 293, 193–196.Google Scholar
Seret, G, Gujot, J, Wansard, G, de Beaulieu, J.L, Reille, M(1992). Tentative palaeoclimatic reconstruction linking pollen and sedimentology in La Grande Pile (Vosges, France). Quaternary Science Reviews, 11, 425–430.Google Scholar
Sevink, J, Kummer, E.A(1984). Eolian dust deposition on the Giara di Gesturi Basalt Plateau, Sardinia. Earth Surface Processes and Landforms, 9, 357–364.CrossRefGoogle Scholar
Street-Perrott, F.A, Harrison, S.P. Lake levels and climate reconstruction. Hecht, A.D(1985). Paleoclimate Analysis and Modeling. Wiley, New York.291–340.Google Scholar
Tomadin, L, Lenaz, R. Eolian dust over the Mediterranean and its contribution to the present sedimentation. Leinen, M, Sarnthein, M(1989). Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport.267–282.Google Scholar