Sedimentology and geochemistry of Oxygen Isotope Stage 3 and Holocene sediments from Laguna Potrok Aike, Patagonia

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Main Authors: Haberzettl, Torsten, Kück, Barbara, Wulf, Sabine, Anselmetti, Flavio S, Ariztegui, Daniel, Corbella, Hugo, Fey, Michael, Janssen, Stephanie, Lücke, Andreas, Mayr, Christoph, Ohlendorf, Christian, Schäbitz, Frank, Schleser, Gerhard Hans, Wille, Michael, Zolitschka, Bernd
Format: Dataset Open Access
Language:en
Published: PANGAEA 2007
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author Haberzettl, Torsten
Kück, Barbara
Wulf, Sabine
Anselmetti, Flavio S
Ariztegui, Daniel
Corbella, Hugo
Fey, Michael
Janssen, Stephanie
Lücke, Andreas
Mayr, Christoph
Ohlendorf, Christian
Schäbitz, Frank
Schleser, Gerhard Hans
Wille, Michael
Zolitschka, Bernd
author_facet Haberzettl, Torsten
Kück, Barbara
Wulf, Sabine
Anselmetti, Flavio S
Ariztegui, Daniel
Corbella, Hugo
Fey, Michael
Janssen, Stephanie
Lücke, Andreas
Mayr, Christoph
Ohlendorf, Christian
Schäbitz, Frank
Schleser, Gerhard Hans
Wille, Michael
Zolitschka, Bernd
collection Datos científicos de ciencias marinas y ambientales
contents Seismic reflection studies in the maar lake Laguna Potrok Aike (51°58? S, 70°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 Reclús and Mt. Burney volcanoes during Oxygen Isotope Stage 3.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_672052
institution PANGAEA
language en
publishDate 2007
publisher PANGAEA
record_format pangaea
spellingShingle Sedimentology and geochemistry of Oxygen Isotope Stage 3 and Holocene sediments from Laguna Potrok Aike, Patagonia
Haberzettl, Torsten
Kück, Barbara
Wulf, Sabine
Anselmetti, Flavio S
Ariztegui, Daniel
Corbella, Hugo
Fey, Michael
Janssen, Stephanie
Lücke, Andreas
Mayr, Christoph
Ohlendorf, Christian
Schäbitz, Frank
Schleser, Gerhard Hans
Wille, Michael
Zolitschka, Bernd
Laguna Potrok Aike, Patagonia; PC; Piston corer; PTA03-06
Seismic reflection studies in the maar lake Laguna Potrok Aike (51°58? S, 70°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 Reclús and Mt. Burney volcanoes during Oxygen Isotope Stage 3.
title Sedimentology and geochemistry of Oxygen Isotope Stage 3 and Holocene sediments from Laguna Potrok Aike, Patagonia
topic Laguna Potrok Aike, Patagonia; PC; Piston corer; PTA03-06
url https://doi.org/10.1594/PANGAEA.672052