Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance
Relict sand wedges are ubiquitous in southern Patagonia. At six sites we conducted detailed investigations of stratigraphy, soils, and wedge frequency and characteristics. Some sections contain four or more buried horizons with casts. The cryogenic features are dominantly relict sand wedges with an...
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ftconicet:oai:ri.conicet.gov.ar:11336/133223 2023-10-09T21:55:14+02:00 Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance Bockheim, J. Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Ercolano, Bettina Ponce, Juan Federico application/pdf http://hdl.handle.net/11336/133223 eng eng Pergamon-Elsevier Science Ltd info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0277379108003727 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2008.12.011 http://hdl.handle.net/11336/133223 Bockheim, J.; Coronato, Andrea Maria Josefa; Rabassa, Jorge Oscar; Ercolano, Bettina; Ponce, Juan Federico; Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 28; 13-14; 6-2009; 1188-1199 0277-3791 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ RELICT SAND WEDGES SOUTHERN PATAGONIA MIDDLE PLEISTOCENE PERIGLACIAL ENVIRONMENTS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.quascirev.2008.12.011 2023-09-24T18:49:50Z Relict sand wedges are ubiquitous in southern Patagonia. At six sites we conducted detailed investigations of stratigraphy, soils, and wedge frequency and characteristics. Some sections contain four or more buried horizons with casts. The cryogenic features are dominantly relict sand wedges with an average depth, maximum apparent width, minimum apparent width, and H/W of 78, 39, 3.8, and 2.9 cm, respectively. The host materials are fine-textured (silt loam, silty clay loam, clay loam) till and the infillings are aeolian sand. The soils are primarily Calciargidic Argixerolls that bear a legacy of climate change. Whereas the sand wedges formed during very cold (-4 to -8 °C or colder) and dry (ca. ≤100 mm precipitation/yr) glacial periods, petrocalcic horizons from calcium carbonate contributed by dustfall formed during warmer (7 °C or warmer) and moister (≥250 mm/yr) interglacial periods. The paleo-argillic (Bt) horizons reflect unusually moist interglacial events where the mean annual precipitation may have been 400 mm/yr. Permafrost was nearly continuous in southern Patagonia during the Illinoian glacial stage (ca. 200 ka), the early to mid-Pleistocene (ca. 800-500 ka), and on two occasions during the early Pleistocene (ca. 1.0-1.1 Ma). Fil: Bockheim, J. University of Wisconsin; Estados Unidos Fil: Coronato, Andrea Maria Josefa. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Rabassa, Jorge Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Ercolano, Bettina. Universidad Austral; Argentina Fil: Ponce, Juan Federico. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Article in Journal/Newspaper permafrost wedge* CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Austral Bockheim ENVELOPE(161.983,161.983,-78.033,-78.033) Patagonia Quaternary Science Reviews 28 13-14 1188 1199 |
institution |
Open Polar |
collection |
CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
op_collection_id |
ftconicet |
language |
English |
topic |
RELICT SAND WEDGES SOUTHERN PATAGONIA MIDDLE PLEISTOCENE PERIGLACIAL ENVIRONMENTS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
spellingShingle |
RELICT SAND WEDGES SOUTHERN PATAGONIA MIDDLE PLEISTOCENE PERIGLACIAL ENVIRONMENTS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Bockheim, J. Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Ercolano, Bettina Ponce, Juan Federico Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance |
topic_facet |
RELICT SAND WEDGES SOUTHERN PATAGONIA MIDDLE PLEISTOCENE PERIGLACIAL ENVIRONMENTS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
description |
Relict sand wedges are ubiquitous in southern Patagonia. At six sites we conducted detailed investigations of stratigraphy, soils, and wedge frequency and characteristics. Some sections contain four or more buried horizons with casts. The cryogenic features are dominantly relict sand wedges with an average depth, maximum apparent width, minimum apparent width, and H/W of 78, 39, 3.8, and 2.9 cm, respectively. The host materials are fine-textured (silt loam, silty clay loam, clay loam) till and the infillings are aeolian sand. The soils are primarily Calciargidic Argixerolls that bear a legacy of climate change. Whereas the sand wedges formed during very cold (-4 to -8 °C or colder) and dry (ca. ≤100 mm precipitation/yr) glacial periods, petrocalcic horizons from calcium carbonate contributed by dustfall formed during warmer (7 °C or warmer) and moister (≥250 mm/yr) interglacial periods. The paleo-argillic (Bt) horizons reflect unusually moist interglacial events where the mean annual precipitation may have been 400 mm/yr. Permafrost was nearly continuous in southern Patagonia during the Illinoian glacial stage (ca. 200 ka), the early to mid-Pleistocene (ca. 800-500 ka), and on two occasions during the early Pleistocene (ca. 1.0-1.1 Ma). Fil: Bockheim, J. University of Wisconsin; Estados Unidos Fil: Coronato, Andrea Maria Josefa. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Rabassa, Jorge Oscar. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Ercolano, Bettina. Universidad Austral; Argentina Fil: Ponce, Juan Federico. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina |
format |
Article in Journal/Newspaper |
author |
Bockheim, J. Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Ercolano, Bettina Ponce, Juan Federico |
author_facet |
Bockheim, J. Coronato, Andrea Maria Josefa Rabassa, Jorge Oscar Ercolano, Bettina Ponce, Juan Federico |
author_sort |
Bockheim, J. |
title |
Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance |
title_short |
Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance |
title_full |
Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance |
title_fullStr |
Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance |
title_full_unstemmed |
Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance |
title_sort |
relict sand wedges in southern patagonia and their stratigraphic and paleo-environmental significance |
publisher |
Pergamon-Elsevier Science Ltd |
url |
http://hdl.handle.net/11336/133223 |
long_lat |
ENVELOPE(161.983,161.983,-78.033,-78.033) |
geographic |
Argentina Austral Bockheim Patagonia |
geographic_facet |
Argentina Austral Bockheim Patagonia |
genre |
permafrost wedge* |
genre_facet |
permafrost wedge* |
op_relation |
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0277379108003727 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2008.12.011 http://hdl.handle.net/11336/133223 Bockheim, J.; Coronato, Andrea Maria Josefa; Rabassa, Jorge Oscar; Ercolano, Bettina; Ponce, Juan Federico; Relict sand wedges in southern Patagonia and their stratigraphic and paleo-environmental significance; Pergamon-Elsevier Science Ltd; Quaternary Science Reviews; 28; 13-14; 6-2009; 1188-1199 0277-3791 CONICET Digital CONICET |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
op_doi |
https://doi.org/10.1016/j.quascirev.2008.12.011 |
container_title |
Quaternary Science Reviews |
container_volume |
28 |
container_issue |
13-14 |
container_start_page |
1188 |
op_container_end_page |
1199 |
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1779319075675045888 |