Age determination of sediment core PTA02-04 from Laguna Potrok Aike, Patagonia (Table 1)

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Autores principales: Haberzettl, Torsten, Fey, Michael, Lücke, Andreas, Maidana, Nora, Mayr, Christoph, Ohlendorf, Christian, Schäbitz, Frank, Schleser, Gerhard Hans, Wille, Michael, Zolitschka, Bernd
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2005
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author Haberzettl, Torsten
Fey, Michael
Lücke, Andreas
Maidana, Nora
Mayr, Christoph
Ohlendorf, Christian
Schäbitz, Frank
Schleser, Gerhard Hans
Wille, Michael
Zolitschka, Bernd
author_facet Haberzettl, Torsten
Fey, Michael
Lücke, Andreas
Maidana, Nora
Mayr, Christoph
Ohlendorf, Christian
Schäbitz, Frank
Schleser, Gerhard Hans
Wille, Michael
Zolitschka, Bernd
collection Datos científicos de ciencias marinas y ambientales
contents The volcanogenic lake Laguna Potrok Aike, Santa Cruz, Argentina, reveals an unprecedented continuous high resolution climatic record for the steppe regions of southern Patagonia. With the applied multi-proxy approach rapid climatic changes before the turn of the first millennium were detected followed by medieval droughts which are intersected by moist and/or cold periods of varying durations and intensities. The 'total inorganic carbon' content was identified as a sensitive lake level indicator. This proxy suggests that during the late Middle Ages (ca. AD 1230-1410) the lake level was rather low representing a signal of the 'Medieval Climate Anomaly' in southeastern Patagonia. At the beginning of the 'Little Ice Age' the lake level rose considerably staying on a high level during the whole period. Subsequently, the lake level lowered again in the course of the 20th century.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_672035
institution PANGAEA
language en
publishDate 2005
publisher PANGAEA
record_format pangaea
spellingShingle Age determination of sediment core PTA02-04 from Laguna Potrok Aike, Patagonia (Table 1)
Haberzettl, Torsten
Fey, Michael
Lücke, Andreas
Maidana, Nora
Mayr, Christoph
Ohlendorf, Christian
Schäbitz, Frank
Schleser, Gerhard Hans
Wille, Michael
Zolitschka, Bernd
Age; Age, 14C AMS; Age, 14C calibrated, CALIB 4.4 (Stuiver et al., 2003); Age, dated; Age, dated, error to older; Age, dated, error to younger; Age, dated, standard deviation; Age, dated material; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Laguna Potrok Aike, Patagonia; PTA02-04; Sample code/label; Sample comment
The volcanogenic lake Laguna Potrok Aike, Santa Cruz, Argentina, reveals an unprecedented continuous high resolution climatic record for the steppe regions of southern Patagonia. With the applied multi-proxy approach rapid climatic changes before the turn of the first millennium were detected followed by medieval droughts which are intersected by moist and/or cold periods of varying durations and intensities. The 'total inorganic carbon' content was identified as a sensitive lake level indicator. This proxy suggests that during the late Middle Ages (ca. AD 1230-1410) the lake level was rather low representing a signal of the 'Medieval Climate Anomaly' in southeastern Patagonia. At the beginning of the 'Little Ice Age' the lake level rose considerably staying on a high level during the whole period. Subsequently, the lake level lowered again in the course of the 20th century.
title Age determination of sediment core PTA02-04 from Laguna Potrok Aike, Patagonia (Table 1)
topic Age; Age, 14C AMS; Age, 14C calibrated, CALIB 4.4 (Stuiver et al., 2003); Age, dated; Age, dated, error to older; Age, dated, error to younger; Age, dated, standard deviation; Age, dated material; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GC; Gravity corer; Laguna Potrok Aike, Patagonia; PTA02-04; Sample code/label; Sample comment
url https://doi.org/10.1594/PANGAEA.672035