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024 7 _ |2 DOI
|a 10.1016/j.palaeo.2007.10.008
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|a WOS:000254695400009
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041 _ _ |a eng
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084 _ _ |2 WoS
|a Geography, Physical
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
084 _ _ |2 WoS
|a Paleontology
100 1 _ |a Haberzettl, T.
|b 0
|u FZJ
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245 _ _ |a Hydrological variability and explosive volcanic activity in southeastern Patagonia during Oxygen Isotope Stage 3 and the Holocene inferred from lake sediments of Laguna Potrok Aike
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2008
300 _ _ |a 213 - 229
336 7 _ |a Journal Article
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336 7 _ |a article
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440 _ 0 |a Palaeogeography Palaeoclimatology Palaeoecology
|x 0031-0182
|0 13362
|v 259
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Seismic reflection studies in the maar lake Laguna Potrok Aike (51 degrees 58' S, 70 degrees 23' W) revealed an erosional unconformity associated with a sub-aquatic lake-level terrace at a water depth of 30m. Radiocarbon-dated, multi-proxy sediment studies of a piston core from this location indicate that the sediment below this discontinuity has an age of 45kyr BP (Oxygen Isotope Stage 3), and was deposited during an interval of high lake level. In comparison to the Holocene section, geochemical indicators of this older part of the record either point towards a different sediment source or to a different transport mechanism for Oxygen Isotope Stage 3 sediments. Holocene sedimentation started again before 6790cal. yr BP, providing a sediment record of hydrological variability until the present. Geochemical and isotopic data indicate a fluctuating lake level until 5310cal. yr BP. During the late Holocene the lake level shows a receding tendency. Nevertheless, the lake level did not drop below the 30m terrace to create another unconformity. The geochemical characterization of volcanic ashes reveals evidence for previously unknown explosive activity of the Reclus and Mt. Burney volcanoes during Oxygen Isotope Stage 3. (c) 2007 Elsevier B.V. All rights reserved.
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653 2 0 |2 Author
|a geochemistry
653 2 0 |2 Author
|a lacustrine sediments
653 2 0 |2 Author
|a lake level changes
653 2 0 |2 Author
|a tephrostratigraphy
653 2 0 |2 Author
|a Argentina
653 2 0 |2 Author
|a palaeoclimate
700 1 _ |a Kück, B.
|b 1
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700 1 _ |a Wulf, S.
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700 1 _ |a Anselmetti, F.
|b 3
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700 1 _ |a Ariztegui, D.
|b 4
|0 P:(DE-HGF)0
700 1 _ |a Fey, M.
|b 5
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700 1 _ |a Janssen, S.
|b 6
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700 1 _ |a Lücke, A.
|b 7
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700 1 _ |a Mayr, C.
|b 8
|0 P:(DE-HGF)0
700 1 _ |a Ohlendorf, C.
|b 9
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700 1 _ |a Schäbitz, F.
|b 10
|0 P:(DE-HGF)0
700 1 _ |a Schleser, G. H.
|b 11
|u FZJ
|0 P:(DE-Juel1)VDB1420
700 1 _ |a Wille, M.
|b 12
|0 P:(DE-HGF)0
700 1 _ |a Zolitschka, B.
|b 13
|0 P:(DE-HGF)0
773 _ _ |a 10.1016/j.palaeo.2007.10.008
|g Vol. 259, p. 213 - 229
|p 213 - 229
|q 259<213 - 229
|0 PERI:(DE-600)1497393-5
|t Palaeogeography, palaeoclimatology, palaeoecology
|v 259
|y 2008
|x 0031-0182
856 7 _ |u http://dx.doi.org/10.1016/j.palaeo.2007.10.008
909 C O |o oai:juser.fz-juelich.de:1495
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