Late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications

This paper investigates several wedge structures formed in continental deposits covering marine sediments deposited during MIS 5 along the central Patagonian coast of Argentina. The size and surface microtexture characteristics of the infilling sediments are consistent with a depositional environmen...

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Published in:Geografiska Annaler: Series A, Physical Geography
Main Authors: Ribolini, Adriano, Bini, Monica, Consoloni, Ilaria, Isola, Ilaria, Pappalardo, Marta, Zanchetta, Giovanni, Fuck, Enrique, Panzieri, Laura, Martini, Marco, Terrasi, Filippo
Other Authors: #PLACEHOLDER_PARENT_METADATA_VALUE#, Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Ice
Online Access:http://hdl.handle.net/2122/11949
https://doi.org/10.1111/geoa.12038
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record_format openpolar
spelling ftingv:oai:www.earth-prints.org:2122/11949 2023-05-15T14:01:37+02:00 Late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications Ribolini, Adriano Bini, Monica Consoloni, Ilaria Isola, Ilaria Pappalardo, Marta Zanchetta, Giovanni Fuck, Enrique Panzieri, Laura Martini, Marco Terrasi, Filippo #PLACEHOLDER_PARENT_METADATA_VALUE# Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia 2016 http://hdl.handle.net/2122/11949 https://doi.org/10.1111/geoa.12038 en eng Geografiska Annaler: Series A, Physical Geography /96 (2016) http://hdl.handle.net/2122/11949 doi:10.1111/geoa.12038 restricted ice-wedge MIS5 Patagonia Argentina article 2016 ftingv https://doi.org/10.1111/geoa.12038 2022-07-29T06:07:34Z This paper investigates several wedge structures formed in continental deposits covering marine sediments deposited during MIS 5 along the central Patagonian coast of Argentina. The size and surface microtexture characteristics of the infilling sediments are consistent with a depositional environment dominated by aeolian transport. Fragments of Andean volcanic rocks (glass shards) in the wedge-fill suggest long-distance transport via a westerly component of wind direction. The wedges are interpreted as products of deep seasonal frost action in frozen ground, which produced open cracks that filled rapidly with partially non-local aeolian sediments. Many wedges cross cut carbonate crusts that formed under permafrost conditions in coastal Patagonia. The radiocarbon dating of carbonate crusts yielded an age of 25–27 kyr bp, while wedge-fill sediments are OSL dated to 14 670 ± 750 yr bp. This indicates that ground wedge formation occurred during a cold event (the Antarctic Cold Reversal period) that interrupted the permafrost degradation following the Last Glacial Maximum. University of Pisa (Progetto Ateneo 2007, Leader G. Zanchetta) and MIUR (PRIN2008, Leader G. Zanchetta).CADACE no-profit organization for providing logistical support to the field campaign. Published 161-176 5A. Paleoclima e ricerche polari JCR Journal Article in Journal/Newspaper Antarc* Antarctic Ice permafrost wedge* Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Antarctic Argentina Patagonia The Antarctic Geografiska Annaler: Series A, Physical Geography 96 2 161 176
institution Open Polar
collection Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia)
op_collection_id ftingv
language English
topic ice-wedge
MIS5
Patagonia Argentina
spellingShingle ice-wedge
MIS5
Patagonia Argentina
Ribolini, Adriano
Bini, Monica
Consoloni, Ilaria
Isola, Ilaria
Pappalardo, Marta
Zanchetta, Giovanni
Fuck, Enrique
Panzieri, Laura
Martini, Marco
Terrasi, Filippo
Late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications
topic_facet ice-wedge
MIS5
Patagonia Argentina
description This paper investigates several wedge structures formed in continental deposits covering marine sediments deposited during MIS 5 along the central Patagonian coast of Argentina. The size and surface microtexture characteristics of the infilling sediments are consistent with a depositional environment dominated by aeolian transport. Fragments of Andean volcanic rocks (glass shards) in the wedge-fill suggest long-distance transport via a westerly component of wind direction. The wedges are interpreted as products of deep seasonal frost action in frozen ground, which produced open cracks that filled rapidly with partially non-local aeolian sediments. Many wedges cross cut carbonate crusts that formed under permafrost conditions in coastal Patagonia. The radiocarbon dating of carbonate crusts yielded an age of 25–27 kyr bp, while wedge-fill sediments are OSL dated to 14 670 ± 750 yr bp. This indicates that ground wedge formation occurred during a cold event (the Antarctic Cold Reversal period) that interrupted the permafrost degradation following the Last Glacial Maximum. University of Pisa (Progetto Ateneo 2007, Leader G. Zanchetta) and MIUR (PRIN2008, Leader G. Zanchetta).CADACE no-profit organization for providing logistical support to the field campaign. Published 161-176 5A. Paleoclima e ricerche polari JCR Journal
author2 #PLACEHOLDER_PARENT_METADATA_VALUE#
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia
format Article in Journal/Newspaper
author Ribolini, Adriano
Bini, Monica
Consoloni, Ilaria
Isola, Ilaria
Pappalardo, Marta
Zanchetta, Giovanni
Fuck, Enrique
Panzieri, Laura
Martini, Marco
Terrasi, Filippo
author_facet Ribolini, Adriano
Bini, Monica
Consoloni, Ilaria
Isola, Ilaria
Pappalardo, Marta
Zanchetta, Giovanni
Fuck, Enrique
Panzieri, Laura
Martini, Marco
Terrasi, Filippo
author_sort Ribolini, Adriano
title Late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications
title_short Late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications
title_full Late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications
title_fullStr Late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications
title_full_unstemmed Late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications
title_sort late‐pleistocene wedge structures along the patagonian coast (argentina): chronological constraints and palaeo‐environmental implications
publishDate 2016
url http://hdl.handle.net/2122/11949
https://doi.org/10.1111/geoa.12038
geographic Antarctic
Argentina
Patagonia
The Antarctic
geographic_facet Antarctic
Argentina
Patagonia
The Antarctic
genre Antarc*
Antarctic
Ice
permafrost
wedge*
genre_facet Antarc*
Antarctic
Ice
permafrost
wedge*
op_relation Geografiska Annaler: Series A, Physical Geography
/96 (2016)
http://hdl.handle.net/2122/11949
doi:10.1111/geoa.12038
op_rights restricted
op_doi https://doi.org/10.1111/geoa.12038
container_title Geografiska Annaler: Series A, Physical Geography
container_volume 96
container_issue 2
container_start_page 161
op_container_end_page 176
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