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Late Holocene paleoenvironment in northern New Caledonia, southwestern Pacific, from a multiproxy analysis of lake sediments

Published online by Cambridge University Press:  20 January 2017

Denis Wirrmann ,
Anne-Marie Sémah  and
Magali Chacornac-Rault
Denis Wirrmann*
Affiliation:
Institut de recherche pour le développement (IRD), PALÉOTROPIQUE, BP A5, 98848 Nouméa cedex, Nouvelle-Calédonie, France
Anne-Marie Sémah
Affiliation:
Institut de recherche pour le développement (IRD), PALÉOTROPIQUE, 32 Avenue Henri Varagnat, 93143 Bondy cedex, France
Magali Chacornac-Rault
Affiliation:
Institut de recherche pour le développement (IRD), PALÉOTROPIQUE, 32 Avenue Henri Varagnat, 93143 Bondy cedex, France Dpt. de Préhistoire, Muséum National d’Histoire Naturelle, (MNHN) UMR 5198, USM 204, 1 rue René Panhard, 75013 Paris, France
*
⁎Corresponding author. Fax: +33 687 26 43 26. E-mail address:denis.wirrmann@noumea.ird.nc (D. Wirrmann).
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Abstract

Lithostratigraphic and palynological analysis of two cores recovered from the ‘Grand Lac’ (New Caledonia), combined with 35 14C AMS dates, yields a paleoenvironmental record spanning the last 2000 yr. The lithology is represented mainly by clayey or laminated layers. A catastrophic event, which is marked by very coarse deposits, occurred probably between ca 1070–960 cal yr B.P. and possibly is associated with an unusually severe La Niña event. Before and after this event, a similar combination of the two main sediment types is recorded. The repeated alternation of laminated and clayey layers is interpreted as the response to local hydrologic forcing, which may reflect a shift from relatively wet to relatively drier conditions, respectively. Variable amount of micro-charcoal is detected all along the profile. Without additional evidence, notwithstanding the initial local human settlement documented since ca 2900 14C yr B.P., micro-charcoal occurrence and variability cannot be linked directly to an anthropogenic origin. No distinct palynological zonations in relation to the lithology are observed, and the vegetation changes may only represent minor transitions across environmental limits.

Keywords

Lacustrine sedimentologyPalynologyLate HoloceneNew CaledoniaSouth Pacific
Type
Research Article
Information
Quaternary Research , Volume 66 , Issue 2 , September 2006 , pp. 213 - 232
Copyright
University of Washington

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References

Bertaux, J., Frölich, F., and Ildefonse, P. Multicomponent analysis of FTIR spectra: quantification of amorphous and crystallized mineral phases in synthetic and natural sediments. Journal of Sedimentary Research 68, (1998). 440–447.CrossRefGoogle Scholar
Cane, M.A. The evolution of El Niño, past and future. Earth and Planetary Science Letters 230, (2005). 227–240.CrossRefGoogle Scholar
Davison, W. Iron and manganese in lakes. Earth-Science Reviews 34, (1993). 119–163.Google Scholar
Dickinson, W.R. Paleoshoreline record of relative Holocene sea levels on Pacific islands. Earth-Science Reviews 55, 3–4 (2001). 191–234.Google Scholar
Dickinson, W.R. Impact of mid-Holocene hydro-isostatic highstand in regional sea level on habitability of islands in Pacific Oceania. Journal of Coastal Research 19, 3 (2003). 489–502.Google Scholar
Eden, D.N., and Page, M.J. Palaeoclimatic implications of a storm erosion record from late Holocene lake sediments, North Island, New Zealand. Palaeogeography, Palaeoclimatology, Palaeoecology 139, (1998). 37–58.Google Scholar
Frimigacci, D., (1981). Archéologie et Préhistoire. Atlas de la Nouvelle Calédonie et dépendances, planche 16. Éditions de l'ORSTOM, Paris, France.Google Scholar
Galipaud, J.-C. Le site de Tiwi et le peuplement de la Nouvelle-Calédonie. Galipaud, J.-C. Poterie Lapita et Peuplement. (1992). Nouvelle-Calédonie, ORSTOM, Nouméa. 103–109.Google Scholar
Galipaud, J.-C. New Caledonia: some recent archaeological perspectives. New Zealand Journal of Archaeology 18, (1996). 297–305.Google Scholar
Galipaud, J.-C. De quelques impressions. L'exemple de la poterie imprimée au battoir en Océanie lointaine/The case of paddle impressed pottery in remote oceania. Galipaud, J.-C., and Lilley, I. Le Pacifique de 5000 à 2000 avant le présent: suppléments à l'histoire d'une colonisation/The Pacific from 5000 to 2000 BP: colonisation and transformations. (1999). Colloques et Séminaires, IRD, Paris. 531–541.Google Scholar
Hope, G., O'Dea, D., and Southern, W. Holocene vegetation histories in the Western Pacific: alternative records of human impact. Galipaud, J.-C., and Lilley, I. Le Pacifique de 5000 à 2000 avant le présent : suppléments à l'histoire d'une colonisation/The Pacific from 5000 to 2000 BP: colonisation and transformations. (1999). Colloques et Séminaires, IRD, Paris. 387–404.Google Scholar
Jaffré, T., Morat, P., and et Veillon, J.M. Étude floristique et phytogéographique de la forêt sclérophylle de Nouvelle-Calédonie. Bulletin du Muséum national d'Histoire naturelle, Paris, 4ème série, 15, section B. Adansonia 1–4 (1993). 107–146.Google Scholar
Jaffré, T., Morat, P., Veillon, J.-M., Rigault, F., and et Dagostini, G. Composition et caractérisation de la flore indigène de Nouvelle-Calédonie. Documents Scientifiques et Techniques II4, IRD Nouméa 121, (2004). A1–A11.Google Scholar
Kemer, M., and Gramm, H. Changes in oxygen consumption at the sediment–water interface formed by settling seston from the Elbe estuary. Limnology and Oceanography 40, (1995). 544–555.Google Scholar
Maitrepierre, L. Climate variability and trend in New Caledonia. APN Workshop on Climate Variability and Trends in Oceania. (2000). Auckland, Australia. 1–23.Google Scholar
Manton, M.J., Della-Marta, P.M., Haylock, M.R., Hennessy, K.J., Nicholls, N., Chambers, L.E., Collins, D.A., Daw, G., Finet, A., Gunawan, D., Inape, K., Isobe, H., Kestin, T.S., Lefale, P., Leyu, C.H., Lwin, T., Maitrepierre, L., Ouprasitwong, N., Page, C.M., Pahalad, J., Plummer, N., Salinger, M.J., Suppiah, R., Tran, V.L., Trewin, B., Tibig, I., and Yee, D. Trends in extreme daily rainfall and temperature in Southeast Asia and the South Pacific: 1961–1998. International Journal of Climatology 21, (2001). 269–284.Google Scholar
McCormac, F.G., Reimer, P.J., Hogg, A.G., Higham, T.F.G., Baillie, M.G.L., Palmer, J., and Stuiver, M. Calibration of the radiocarbon time scale for the Southern Hemisphere: AD 1850–950. Radiocarbon 44, (2002). 641–651.CrossRefGoogle Scholar
McDonald, G.M., Larsen, C.P.S., Szeicz, J.M., and Moser, K.A. The reconstruction of boreal forest fire history from lake sediments: a comparison of charcoal, pollen, sedimentological and geochemical indices. Quaternary Science Reviews 10, (1991). 53–71.Google Scholar
Météo France, (1995). Atlas climatique de la Nouvelle-Calédonie. Météo France, Direction Interrégionale de Nouvelle-Calédonie et de Wallis et Futuna, Nouméa., 104 pp.Google Scholar
Moore, J., (1999). Microscopic charcoal and taphonomic processes: an evaluation. PhD thesis, University of Sheffield, .Google Scholar
Morlière, A., and Rebert, J.-P. Rainfall shortage and El Niño-Southern Oscillation in New Caledonia, southwestern Pacific. Monthly Weather Review 114, (1986). 1131–1137.2.0.CO;2>CrossRefGoogle Scholar
Patterson, W.A. III, Edwards, K.J., and MacGuire, D.J. Microscopic charcoal as a fossil indicator of fire. Quaternary Science Reviews 6, (1987). 3–23.Google Scholar
Sand, C. Recent developments in the study of New Caledonia's prehistory. Archaeology in Oceania 31, (1996). 45–71.Google Scholar
Schoonen, M.A.A., and Barnes, H.I. Reactions forming pyrite and marcasite from solution: II. Via FeS precursors below 100°C. Geochimica et Cosmochimica Acta 55, (1991). 1505–1514.CrossRefGoogle Scholar
Sémah, A.-M. Recherche des traces de la première conquête des vallées dans le nord de la ‘Grande-Terre’ (Nouvelle-Calédonie). Archéologie en grotte et étude du paléoenvironnement à Koumac. Journal de la Société des Océanistes 2, (1998). 169–178.Google Scholar
Sémah, F., Sémah, A.-M., and et Forestier, H. Nouvelles données sur le peuplement ancien de la Nouvelle-Calédonie: la vallée de la Koumac (‘Grande-Terre’). Comptes Rendus de l'Académie des Sciences, Paris, Série IIA 320, (1995). 539–545.Google Scholar
Sémah, A.-M., Sémah, F., and Forestier, H. La vallée de la Koumac (Nouvelle-Calédonie): fouille du site NKM004. Galipaud, J.-C., and Lilley, I. Le Pacifique de 5000 à 2000 avant le présent: suppléments à l'histoire d'une colonisation/The Pacific from 5000 to 2000 BP: colonisation and transformations. (1996). Colloques et Séminaires, IRD, Paris. 289–299.Google Scholar
Spriggs, M. The Island Melanesians. (1997). Blackwell Publishers Ltd., Oxford, UK. 326 pp. Google Scholar
Stevenson, J. A late-Holocene record of human impact from the southwest coast of New Caledonia. The Holocene 14, (2004). 888–898.Google Scholar
Stevenson, J., and Dodson, J.R. Paleoenvironmental evidence for human settlement of New Caledonia. Archaeology in Oceania 30, (1995). 36–41.Google Scholar
Stevenson, J., Dodson, J.R., and Prosser, I.P. A late Quaternary record of environmental change and human impact from New Caledonia. Paleogeography, Paleoclimatology, Paleoecology 168, (2001). 97–123.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., van der Plicht, J., and Spurk, M. INTCAL98 Radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40, (1998). 1041–1083.Google Scholar
Tinner, W., Ammann, B., Conedera, M., Gaggeler, H.W., Sägesser, B., Gedye, S., and Jones, R. Pollen and charcoal in lake sediments compared with historically documented forest fires in southern Switzerland since ad 1920. The Holocene 8, (1998). 31–42.Google Scholar
Wilkin, R.T., and Barnes, H.L. Formation processes of framboidal pyrite. Geochimica et Cosmochimica Acta 61, (1997). 323–339.Google Scholar
Wirrmann, D., and Sémah, A.-M. Upper-Holocene paleoenvironmental changes inferred from lacustrine sediments in Northern New Caledonia (SW Pacific). First results. European Union of Geosciences EUG XI, Strasbourg, Journal of Conference Abstracts 6, 374. (2001). Cambridge Publication, Google Scholar