Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina)

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 follow...

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Guardado en:
Detalles Bibliográficos
Publicado: 2005
Materias:
Argentina
Lacustrine sediments
Lake level changes
Little Ice Age
Medieval Climate Anomaly
Southern Patagonia
lake level
paleolimnology
Patagonia
Santa Cruz [Argentina]
South America
Western Hemisphere
World
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09212728_v33_n3_p283_Haberzettl
http://hdl.handle.net/20.500.12110/paper_09212728_v33_n3_p283_Haberzettl
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
id paper:paper_09212728_v33_n3_p283_Haberzettl
record_format dspace
spelling paper:paper_09212728_v33_n3_p283_Haberzettl2023-06-08T15:50:17Z Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina) Argentina Lacustrine sediments Lake level changes Little Ice Age Medieval Climate Anomaly Southern Patagonia lake level Little Ice Age paleolimnology Argentina Patagonia Santa Cruz [Argentina] South America Western Hemisphere World 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. © Springer 2005. 2005 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09212728_v33_n3_p283_Haberzettl http://hdl.handle.net/20.500.12110/paper_09212728_v33_n3_p283_Haberzettl
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Argentina
Lacustrine sediments
Lake level changes
Little Ice Age
Medieval Climate Anomaly
Southern Patagonia
lake level
Little Ice Age
paleolimnology
Argentina
Patagonia
Santa Cruz [Argentina]
South America
Western Hemisphere
World
spellingShingle Argentina
Lacustrine sediments
Lake level changes
Little Ice Age
Medieval Climate Anomaly
Southern Patagonia
lake level
Little Ice Age
paleolimnology
Argentina
Patagonia
Santa Cruz [Argentina]
South America
Western Hemisphere
World
Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina)
topic_facet Argentina
Lacustrine sediments
Lake level changes
Little Ice Age
Medieval Climate Anomaly
Southern Patagonia
lake level
Little Ice Age
paleolimnology
Argentina
Patagonia
Santa Cruz [Argentina]
South America
Western Hemisphere
World
description 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. © Springer 2005.
title Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina)
title_short Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina)
title_full Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina)
title_fullStr Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina)
title_full_unstemmed Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina)
title_sort climatically induced lake level changes during the last two millennia as reflected in sediments of laguna potrok aike, southern patagonia (santa cruz, argentina)
publishDate 2005
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_09212728_v33_n3_p283_Haberzettl
http://hdl.handle.net/20.500.12110/paper_09212728_v33_n3_p283_Haberzettl
_version_ 1768546451187564544

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