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Late local glacial maximum in the Central Altiplano triggered by cold and locally-wet conditions during the paleolake Tauca episode (17–15 ka, Heinrich 1)

Blard, P.-H. and Lavé, J. and Farley, K. A. and Fornari, M. and Jiménez, N. and Ramirez, V. (2009) Late local glacial maximum in the Central Altiplano triggered by cold and locally-wet conditions during the paleolake Tauca episode (17–15 ka, Heinrich 1). Quaternary Science Reviews, 28 (27-28). pp. 3414-3427. ISSN 0277-3791. https://resolver.caltech.edu/CaltechAUTHORS:20100119-134535247

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Abstract

The timing and causes of the last deglaciation in the southern tropical Andes is poorly known. In the Central Altiplano, recent studies have focused on whether this tropical highland was deglaciated before, synchronously or after the global last glacial maximum (~ 21 ka BP). In this study we present a new chronology based on cosmogenic ^3He (^3He_c) dating of moraines on Cerro Tunupa, a volcano that is located in the centre of the now vanished Lake Tauca (19.9°S, 67.6°W). These new ^3He_c ages suggest that the Tunupa glaciers remained close to their maximum extent until 15 ka BP, synchronous with the Lake Tauca highstand (17–15 ka BP). Glacial retreat and the demise of Lake Tauca seem to have occurred rapidly and synchronously, within dating uncertainties, at ~15 ka BP. We took advantage of the synchronism of these events to combine a glacier model with a lake model in order to reconstruct precipitation and temperature during the Lake Tauca highstand. This new approach indicates that, during the Tauca highstand (17–15 ka BP), the centre of the Altiplano was characterized by temperature ~ 6.5 °C cooler and average precipitation higher by a factor ranging between ×1.6 and ×3 compared to the present. Cold and wet conditions thus persisted in a significant part of the southern tropical Andes during the Heinrich 1 event (17–15 ka BP). This study also demonstrates the extent to which the snowline of glaciers can be affected by local climatic conditions and emphasizes that efforts to draw global climate inferences from glacial extents must also consider local moisture conditions.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/j.quascirev.2009.09.025DOIUNSPECIFIED
ORCID:
AuthorORCID
Farley, K. A.0000-0002-7846-7546
Additional Information:© 2009 Elsevier Ltd. Received 8 July 2009; revised 18 September 2009; accepted 28 September 2009. Available online 25 October 2009. Constructive comments by Wallace S. Broecker, Joerg M. Schaefer and Ano N. Ymous improved an earlier version of this manuscript. This work was mainly funded by the French INSU program "Relief de la Terre" and by the Caltech Tectonics Observatory. It is part of the Post Doc of P.-H. Blard. The authors thank the IRD (Institut de Recherche pour le De´veloppement) of La Paz, Bolivia, which provided a precious technical and logistical assistance in the field. This is CRPG contribution #2017.
Funders:
Funding AgencyGrant Number
French INSU (Institut National des Sciences de l'Univers) program ‘‘Relief de la Terre’’UNSPECIFIED
Caltech Tectonics ObservatoryUNSPECIFIED
Issue or Number:27-28
Record Number:CaltechAUTHORS:20100119-134535247
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20100119-134535247
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:17217
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:25 Jan 2010 17:39
Last Modified:03 Mar 2020 13:01

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