Untangling the Quaternary Period—A Legacy of Stephen C. Porter
Stephen C. Porter was an international leader in Quaternary science for several decades, having worked on most of the world’s continents and having led international organizations and a prominent interdisciplinary journal. His work influenced many individuals, and he played an essential role in linking Chinese Quaternary science with the broader international scientific community. This volume brings together nineteen papers of interdisciplinary Quaternary science honoring Porter. Special Paper 548 features papers from six continents, on wide-ranging topics including glaciation, paleoecology, landscape evolution, megafloods, and loess. The topical and geographical range of the papers, as well as their interdisciplinary nature, honor Porter’s distinct approach to Quaternary science and leadership that influences the field to this day.
Pliocene–Pleistocene landscape evolution and watershed reorganization east of the central Andes in Argentine Patagonia
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Published:April 07, 2021
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CiteCitation
Corinne Y. Griffing, John J. Clague, Rene W. Barendregt, Brian Menounos, Sidney R. Hemming, Jorge Rabassa, Bettina Ercolano, Oscar Martinez, 2021. "Pliocene–Pleistocene landscape evolution and watershed reorganization east of the central Andes in Argentine Patagonia", Untangling the Quaternary Period—A Legacy of Stephen C. Porter, Richard B. Waitt, Glenn D. Thackray, Alan R. Gillespie
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ABSTRACT
Uplift of the central Andes during the Miocene was followed by large-scale reorganization of Atlantic-draining rivers in Argentine Patagonia. Here, we document the abandonment of one large river in the late Pliocene and the establishment of the modern drainage in the Early Pleistocene. A chronology for these events is provided by 40Ar/39Ar ages on basalt flows. Remnants of the Pliocene paleovalley system are well preserved in the Lago Cardiel–Gobernador Gregores area, where they are eroded into flat-lying basalt flows dated from ca. 13.9 Ma to 8.6 Ma. Younger basalts that erupted onto the abandoned floor of the paleovalley are as young as 3.7 Ma. Abandonment of the Pliocene paleovalley and establishment of the modern Río Chico and Río Shehuen catchments happened near the close of the Pliocene when Andean glaciers incised the east-sloping pediment on which the late Miocene drainage was established. Lago Cardiel sits within a large endorheic basin that is inset into the late Pliocene paleovalley. The basin began to develop just before 4 Ma, after the paleovalley was abandoned. It became larger and deeper during the Pleistocene due to mass movements along its margins, deflation of the basin floor during times when Lago Cardiel was dry or nearly dry, and possibly lowering along bounding faults. The Pliocene–Pleistocene landscape and drainage changes that we have documented are not unique to the Lago Cardiel–Gobernador Gregores area; similar changes are apparent elsewhere in Patagonia east of the crest of the Andes.
- Andes
- Argentina
- basalts
- Cenozoic
- Central Andes
- data processing
- depositional environment
- digital terrain models
- erosion
- erosion rates
- flood basalts
- fluvial environment
- geographic information systems
- glacial erosion
- Google Earth
- igneous rocks
- information systems
- landform evolution
- Landsat
- lithofacies
- mass movements
- Neogene
- paleoenvironment
- paleogeography
- paleohydrology
- paleolakes
- paleorelief
- Patagonia
- Pleistocene
- Pliocene
- Quaternary
- remote sensing
- satellite methods
- Shuttle Imaging Radar
- South America
- terraces
- Tertiary
- topography
- volcanic rocks
- Lago Cardiel
- Tres Lagunas Argentina
- Rio Shehuan
- Canadon Leon Valley Argentina