The reconstruction of glacial paleolake formation and evolution allows the understanding of glacier advance and retreat behavior for longer periods of time. New datings obtained from paleolacustrine deposits in the Argentinian Patagonian Andes (Northwestern region of Santa Cruz Province) reveal that glacial lakes formed before the Last Glacial Maximum, they being as old as 31,278 cal yr BP, and evolved until 6900 cal yr BP. The interpretation of stratigraphic profiles described in different sectors of the Perito Moreno National Park (PMNP) allows reconstructing lacustrine, glaciolacustrine, glacial till and delta paleoenvironments. In each sector, organic-rich sediments were also sampled to obtain four absolute ages through AMS methodology....
A series of long sediment cores was retrieved from Laguna Potrok Aike, Southern Patagonia, within th...
High-mountain lake records in semiarid foreland settings, such as the central Andes of North-western...
Sediment cores from glacial lakes in the tropical-subtropical Andes provide a nearly continuous reco...
The climatic changes that occurred during the late Pleistocene-early Holocene in Patagonia generated...
We undertook multi-proxy analyses on two sediment cores from Lago Pato, a small lake basin at 51 deg...
A late Pleistocene glaciolacustrine record was studied at Fagnano Lake (54°35´S, 67°20´W), central I...
The Patagonian glaciations developed since the latestMiocene (ca. 6Ma)in multiple events, of varied ...
The valley of Lake Viedma represents one of the main ice flow axes during the Quaternary glaciations...
The Pueyrredon-Posadas-Salitroso lacustrine system (PPS-LS) is located in the Andean Patagonia regio...
The Ullum-Zonda tectonic depression located in the central Andes Precordillera records several lacus...
This paper reviews published geochronological data on glacier fluctuations and environmental changes...
AbSTRACT. A number of glacial moraines are distributed from the eastern margin of the Torres del Pai...
There are still many uncertainties about the climatic forcing that drove the glacier fluctuations of...
Laguna Mar Chiquita (LMC, 30°54′S – 62°51′W) is a highly variable and shallow saline lake, located i...
The spectacular water outburst occurring semi-periodically when the ice-dam formed by the external f...
A series of long sediment cores was retrieved from Laguna Potrok Aike, Southern Patagonia, within th...
High-mountain lake records in semiarid foreland settings, such as the central Andes of North-western...
Sediment cores from glacial lakes in the tropical-subtropical Andes provide a nearly continuous reco...
The climatic changes that occurred during the late Pleistocene-early Holocene in Patagonia generated...
We undertook multi-proxy analyses on two sediment cores from Lago Pato, a small lake basin at 51 deg...
A late Pleistocene glaciolacustrine record was studied at Fagnano Lake (54°35´S, 67°20´W), central I...
The Patagonian glaciations developed since the latestMiocene (ca. 6Ma)in multiple events, of varied ...
The valley of Lake Viedma represents one of the main ice flow axes during the Quaternary glaciations...
The Pueyrredon-Posadas-Salitroso lacustrine system (PPS-LS) is located in the Andean Patagonia regio...
The Ullum-Zonda tectonic depression located in the central Andes Precordillera records several lacus...
This paper reviews published geochronological data on glacier fluctuations and environmental changes...
AbSTRACT. A number of glacial moraines are distributed from the eastern margin of the Torres del Pai...
There are still many uncertainties about the climatic forcing that drove the glacier fluctuations of...
Laguna Mar Chiquita (LMC, 30°54′S – 62°51′W) is a highly variable and shallow saline lake, located i...
The spectacular water outburst occurring semi-periodically when the ice-dam formed by the external f...
A series of long sediment cores was retrieved from Laguna Potrok Aike, Southern Patagonia, within th...
High-mountain lake records in semiarid foreland settings, such as the central Andes of North-western...
Sediment cores from glacial lakes in the tropical-subtropical Andes provide a nearly continuous reco...