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Uplift of Quaternary shorelines in Eastern Patagonia : Darwin revisited
Pedoja K., Regard V., Husson L., Martinod J., Et Al
Geomorphology 127, 3-4 (2011) 121-142 - http://hal-insu.archives-ouvertes.fr/insu-00610899
Article in peer-reviewed journal
Sciences of the Universe/Earth Sciences/Stratigraphy
Sciences of the Universe/Earth Sciences/Tectonics
Environmental Sciences/Global Changes
Uplift of Quaternary shorelines in Eastern Patagonia : Darwin revisited
Kevin Pedoja () 1, Vincent Regard () 2, Laurent Husson () 3, 4, Joseph Martinod () 2, . Et Al
1:  Morphodynamique continentale et côtière (MCC)
http://WWW.geos.unicaen.fr
CNRS : UMR6143 – INSU – Université de Caen Basse-Normandie – Université de Rouen
24 Rue des tilleuls 14000 CAEN
France
2:  Laboratoire des Mécanismes et Transfert en Géologie (LMTG)
http://www.lmtg.obs-mip.fr/
CNRS : UMR5563 – Observatoire Midi-Pyrénées – Université Paul Sabatier [UPS] - Toulouse III – Institut de recherche pour le développement [IRD] : UMR154
14 avenue Edouard Belin 31400 Toulouse
France
3:  Géosciences Rennes (GR)
http://www.geosciences.univ-rennes1.fr/
CNRS : UMR6118 – INSU – Centre Armoricain de Recherches en Environnement – Université de Rennes 1
Bâtiment 15 - Université de Rennes 1 - Campus de Beaulieu - CS 74205 - 35042 Rennes Cedex - France
France
4:  Laboratoire de Planétologie et Géodynamique de Nantes (LPGN)
CNRS : UMR6112 – INSU – Université de Nantes
2 Rue de la Houssinière - BP 92208 44322 NANTES CEDEX 3
France
During his journey on the Beagle, Darwin observed the uniformity in the elevation of coastal Eastern Patagonia along more than 2000 km. More than one century later, the sequences of Quaternary shorelines of eastern Patagonia have been described and their deposits dated but not yet interpreted in terms of geodynamics. Consequently, we i) mapped the repartition of the Quaternary coastal sequences in Argentinean Patagonia, ii) secured accurate altitudes of shoreline angles associated with erosional morphologies (i.e. marine terraces and notches), iii) took into account previous chrono-stratigraphical interpretations in order to calculate mean uplift rates since ~440 ka (MIS 11) and proposed age ranges for the higher and older features (up to ~180 m), and iv) focused on the Last Interglacial Maximum terrace (MIS 5e) as the best constrained marine terrace (in terms of age and altitude) in order to use it as a tectonic benchmark to quantify uplift rates along the entire passive margin of Eastern South America. Our results show that the eastern Patagonia uplift is constant through time and twice the uplift of the rest of the South American margin. We suggest that the enhanced uplift along the eastern Patagonian coast that interested Darwin during his journey around South America on the Beagle could originate from the subduction of the Chile ridge and the associated dynamic uplift.
English

Geomorphology
Publisher Elsevier
ISSN 0169-555X 
international
2011
127
3-4
121-142

Quaternary – Coastal sequences – Uplift – Passive margin – Patagonia – Argentina – South America
PL02686