Geological evidence for a drought episode in the western Pampas (Argentina, South America) during the early-mid 20th century

Drought episodes during the early-mid 20th century were recognized and described in several places around the world, with extreme dry conditions and widespread landscape denudation, like during the famous 'Dust Bowl' in North America. However, there is scant documentation of droughts in so...

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Autores principales: Tripaldi, A., Zárate, M.A., Forman, S.L., Badger, T., Doyle, M.E., Ciccioli, P.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_09596836_v23_n12_p1731_Tripaldi
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spelling todo:paper_09596836_v23_n12_p1731_Tripaldi2023-10-03T15:53:10Z Geological evidence for a drought episode in the western Pampas (Argentina, South America) during the early-mid 20th century Tripaldi, A. Zárate, M.A. Forman, S.L. Badger, T. Doyle, M.E. Ciccioli, P. 20th century aeolian record optically stimulated luminescence dating Pampas Dust Bowl South America western Pampas anthropogenic effect depositional environment drought stress eolian deposit landscape luminescence mobilization precipitation (climatology) rainfall sea surface temperature sedimentation twentieth century Argentina Atlantic Ocean Atlantic Ocean (South) Pampas Drought episodes during the early-mid 20th century were recognized and described in several places around the world, with extreme dry conditions and widespread landscape denudation, like during the famous 'Dust Bowl' in North America. However, there is scant documentation of droughts in southern South America, particularly from the Pampas, and none based on the geological record. In this article, we provide clear evidence of aeolian reactivation and sand deposition in some areas of La Pampa and San Luis provinces, western Pampas (Argentina), during early-mid 20th century in response to drier conditions, probably amplified, like historic droughts in North America, by anthropogenic factors (e.g. significant population increase and agriculture expansion into a fragile environment). Evidence includes widespread bare sand blowouts, extensive surfaces with active sand migration, steep dune lee slopes, and sharp crests covered by weak soil development (A/C profile), accompanied by historical documents. Optically stimulated luminescence (OSL) ages on aeolian beds confirm mobilization and sedimentation by wind processes c. 95-60 yr BP. Considering the dominant (over 70%) austral spring-summer precipitation, it is possible the rainfall deficit in western Pampas was linked to positive sea surface temperature (SST) anomalies in the western subtropical South Atlantic Ocean (20-30°S and 30-50° W), according to significant canonical correlation between the precipitation field in subtropical South America and the Atlantic Ocean SST anomalies. © The Author(s) 2013. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_09596836_v23_n12_p1731_Tripaldi
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic 20th century
aeolian record
optically stimulated luminescence dating
Pampas Dust Bowl
South America
western Pampas
anthropogenic effect
depositional environment
drought stress
eolian deposit
landscape
luminescence
mobilization
precipitation (climatology)
rainfall
sea surface temperature
sedimentation
twentieth century
Argentina
Atlantic Ocean
Atlantic Ocean (South)
Pampas
spellingShingle 20th century
aeolian record
optically stimulated luminescence dating
Pampas Dust Bowl
South America
western Pampas
anthropogenic effect
depositional environment
drought stress
eolian deposit
landscape
luminescence
mobilization
precipitation (climatology)
rainfall
sea surface temperature
sedimentation
twentieth century
Argentina
Atlantic Ocean
Atlantic Ocean (South)
Pampas
Tripaldi, A.
Zárate, M.A.
Forman, S.L.
Badger, T.
Doyle, M.E.
Ciccioli, P.
Geological evidence for a drought episode in the western Pampas (Argentina, South America) during the early-mid 20th century
topic_facet 20th century
aeolian record
optically stimulated luminescence dating
Pampas Dust Bowl
South America
western Pampas
anthropogenic effect
depositional environment
drought stress
eolian deposit
landscape
luminescence
mobilization
precipitation (climatology)
rainfall
sea surface temperature
sedimentation
twentieth century
Argentina
Atlantic Ocean
Atlantic Ocean (South)
Pampas
description Drought episodes during the early-mid 20th century were recognized and described in several places around the world, with extreme dry conditions and widespread landscape denudation, like during the famous 'Dust Bowl' in North America. However, there is scant documentation of droughts in southern South America, particularly from the Pampas, and none based on the geological record. In this article, we provide clear evidence of aeolian reactivation and sand deposition in some areas of La Pampa and San Luis provinces, western Pampas (Argentina), during early-mid 20th century in response to drier conditions, probably amplified, like historic droughts in North America, by anthropogenic factors (e.g. significant population increase and agriculture expansion into a fragile environment). Evidence includes widespread bare sand blowouts, extensive surfaces with active sand migration, steep dune lee slopes, and sharp crests covered by weak soil development (A/C profile), accompanied by historical documents. Optically stimulated luminescence (OSL) ages on aeolian beds confirm mobilization and sedimentation by wind processes c. 95-60 yr BP. Considering the dominant (over 70%) austral spring-summer precipitation, it is possible the rainfall deficit in western Pampas was linked to positive sea surface temperature (SST) anomalies in the western subtropical South Atlantic Ocean (20-30°S and 30-50° W), according to significant canonical correlation between the precipitation field in subtropical South America and the Atlantic Ocean SST anomalies. © The Author(s) 2013.
format JOUR
author Tripaldi, A.
Zárate, M.A.
Forman, S.L.
Badger, T.
Doyle, M.E.
Ciccioli, P.
author_facet Tripaldi, A.
Zárate, M.A.
Forman, S.L.
Badger, T.
Doyle, M.E.
Ciccioli, P.
author_sort Tripaldi, A.
title Geological evidence for a drought episode in the western Pampas (Argentina, South America) during the early-mid 20th century
title_short Geological evidence for a drought episode in the western Pampas (Argentina, South America) during the early-mid 20th century
title_full Geological evidence for a drought episode in the western Pampas (Argentina, South America) during the early-mid 20th century
title_fullStr Geological evidence for a drought episode in the western Pampas (Argentina, South America) during the early-mid 20th century
title_full_unstemmed Geological evidence for a drought episode in the western Pampas (Argentina, South America) during the early-mid 20th century
title_sort geological evidence for a drought episode in the western pampas (argentina, south america) during the early-mid 20th century
url http://hdl.handle.net/20.500.12110/paper_09596836_v23_n12_p1731_Tripaldi
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