[HTML][HTML] The evolution of the Patagonian Ice Sheet from 35 ka to the present day (PATICE)
We present PATICE, a GIS database of Patagonian glacial geomorphology and recalibrated
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …
chronological data. PATICE includes 58,823 landforms and 1,669 geochronological ages …
The deglaciation of the Americas during the Last Glacial Termination
This paper reviews current understanding of deglaciation in North, Central and South
America from the Last Glacial Maximum to the beginning of the Holocene. Together with …
America from the Last Glacial Maximum to the beginning of the Holocene. Together with …
A marine record of Patagonian ice sheet changes over the past 140,000 years
Terrestrial glacial records from the Patagonian Andes and New Zealand Alps document
quasi-synchronous Southern Hemisphere–wide glacier advances during the late …
quasi-synchronous Southern Hemisphere–wide glacier advances during the late …
Near-synchronous Northern Hemisphere and Patagonian Ice Sheet variation over the last glacial cycle
Northern Hemisphere insolation intensity is roughly in phase with Southern Hemisphere
climate proxies, leading to a common conclusion that northern insolation forces southern …
climate proxies, leading to a common conclusion that northern insolation forces southern …
The relationships between tectonics, climate and exhumation in the Central Andes (18–36 S): Evidence from low-temperature thermochronology
Abstract The Central Andes between 18° S and 36° S latitude strike north-south for 2000 km
along the Chilean subduction margin, cross several climate zones from hyperarid to humid …
along the Chilean subduction margin, cross several climate zones from hyperarid to humid …
The “missing glaciations” of the Middle Pleistocene
Global glaciations have varied in size and magnitude since the Early–Middle Pleistocene
transition (~ 773 ka), despite the apparent regular and high-amplitude 100 ka pacing of …
transition (~ 773 ka), despite the apparent regular and high-amplitude 100 ka pacing of …
The last two glacial cycles in central Patagonia: A precise record from the Ñirehuao glacier lobe
Milankovitch orbital parameters control cycles of insolation, a primary pacer of long term
changes in climate, but exactly how insolation signals are transmitted around the globe in …
changes in climate, but exactly how insolation signals are transmitted around the globe in …
[HTML][HTML] High-resolution chronology for deglaciation of the Patagonian Ice Sheet at Lago Buenos Aires (46.5 S) revealed through varve chronology and Bayesian age …
JM Bendle, AP Palmer, VR Thorndycraft… - Quaternary Science …, 2017 - Elsevier
Glaciolacustrine varves offer the potential to construct continuous, annually-resolved
chronologies for ice-sheet deglaciation, and improved understanding of glacier retreat …
chronologies for ice-sheet deglaciation, and improved understanding of glacier retreat …
Geomorphology and 10Be chronology of the Last Glacial Maximum and deglaciation in northeastern Patagonia, 43 S-71 W
Abstract In southern South America, well-dated glacial geomorphological records constrain
the last glacial cycle across much of the former Patagonian Ice Sheet, but its northeastern …
the last glacial cycle across much of the former Patagonian Ice Sheet, but its northeastern …
Glacier expansion in central Patagonia during the Antarctic Cold Reversal followed by retreat and stabilisation during the Younger Dryas
The spatial-temporal footprint of millennial-scale climate events during the last glacial-
interglacial transition can yield insights into the underlying drivers of climate change, but …
interglacial transition can yield insights into the underlying drivers of climate change, but …