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40Ar/39Ar and K-Ar chronology of Pleistocene glaciations in Patagonia

2004; Geological Society of America; Volume: 116; Issue: 3 Linguagem: Inglês

10.1130/b25177.1

1943-2674

Brad S. Singer, Robert P. Ackert, Hervé Guillou,

Evolution and Paleontology Studies

Research Article| March 01, 2004 40Ar/39Ar and K-Ar chronology of Pleistocene glaciations in Patagonia Brad S. Singer; Brad S. Singer 1Department of Geology and Geophysics, University of Wisconsin—Madison, 1215 West Dayton Street, Madison, Wisconsin 53706, USA Search for other works by this author on: GSW Google Scholar Robert P. Ackert, Jr.; Robert P. Ackert, Jr. 2Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution MS 25, Clark 419, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Hervé Guillou Hervé Guillou 3Laboratoire des Sciences du Climat et de l'Environnement, Domaine du CNRS, Bat. 12, Avenue de la Terrasse, 91198 Gif-sur-Yvette, France Search for other works by this author on: GSW Google Scholar Author and Article Information Brad S. Singer 1Department of Geology and Geophysics, University of Wisconsin—Madison, 1215 West Dayton Street, Madison, Wisconsin 53706, USA Robert P. Ackert, Jr. 2Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution MS 25, Clark 419, Woods Hole, Massachusetts 02543, USA Hervé Guillou 3Laboratoire des Sciences du Climat et de l'Environnement, Domaine du CNRS, Bat. 12, Avenue de la Terrasse, 91198 Gif-sur-Yvette, France Publisher: Geological Society of America Received: 13 May 2002 Revision Received: 23 May 2003 Accepted: 12 Jun 2003 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2004) 116 (3-4): 434–450. https://doi.org/10.1130/B25177.1 Article history Received: 13 May 2002 Revision Received: 23 May 2003 Accepted: 12 Jun 2003 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Brad S. Singer, Robert P. Ackert, Hervé Guillou; 40Ar/39Ar and K-Ar chronology of Pleistocene glaciations in Patagonia. GSA Bulletin 2004;; 116 (3-4): 434–450. doi: https://doi.org/10.1130/B25177.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract During the Pleistocene, east of Lago Buenos Aires, Argentina, at 46.5 °S, at least 19 terminal moraines were deposited as piedmont glaciers from the Patagonian ice cap advanced onto the semi-arid high plains adjacent to the southern Andes. Exceptional preservation of these deposits offers a rare opportunity to document ice-cap fluctuations during the last 1.2 m.y. 40Ar/39Ar incremental-heating and unspiked K-Ar experiments on four basaltic lava flows interbedded with the moraines provide a chronologic framework for the entire glacial sequence. The 40Ar/39Ar isochron ages of three lavas that overlie till 90 km east of the Cordillera at Lago Buenos Aires, and another 120 km from the Andes along Río Gallegos at 51.8 °S that underlies till, strongly suggest that the ice cap reached its greatest eastward extent ca. 1100 ka. At least six moraines were deposited within the 256 k.y. period bracketed by basaltic eruptions at 1016 ± 10 ka and 760 ± 14 ka. Similarly, six younger, more proximal moraines were deposited during an ∼651 k.y. period bracketed by an underlying 760 ± 14 ka basalt and the 109 ± 3 ka Cerro Volcán basalt flow that buried all six moraines. Coupled with in situ cosmogenic surface exposure ages of moraine boulders, the 109 ka age of Cerro Volcán implies that moraines deposited during the penultimate local glaciation correspond to marine oxygen isotope stage 6. Further westward toward Lago Buenos Aires, six additional moraines younger than the Cerro Volcán basalt flow occur. Surface exposure dating of boulders on these moraines, combined with the 14C age of overlying varved lacustrine sediment, indicates deposition during the Last Glacial Maximum (LGM, 23–16 ka). Although Antarctic dust records signal an important Patagonian glaciation at 60–40 ka, moraines corresponding to marine oxygen isotope stage 4 are not preserved at Lago Buenos Aires; apparently, these were overrun and obliterated by the younger ice advance at 23 ka. Notwithstanding, the overall pattern of glaciation in Patagonia is one of diminishing eastward extent of ice during successive glacial advances over the past 1 m.y. We hypothesize that tectonically driven uplift of the Patagonian Andes, which began in the Pliocene, yet continued into the Quaternary, in part due to subduction of the Chile rise spreading center during the past 2 m.y., maximized the ice accumulation area and ice extent by 1.1 Ma. Subsequent deep glacial erosion has reduced the accumulation area, resulting in less extensive glaciers over time. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.