Reconstruction of the San Lorenzo ice cap during the last glacial cycle: insights into the build-up and demise of the last Patagonian ice sheet
Patagonia in southernmost South America is situated in a climatically sensitive region of the Southern Hemisphere. It is the only stretch of land to fully intersect the southern westerly wind belt, an important component of the global climate system. Robust glacial chronologies from this region can...
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| Other Authors: | , , , |
| Format: | Doctoral or Postdoctoral Thesis |
| Language: | English |
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The University of Edinburgh
2020
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| Subjects: | |
| Online Access: | https://hdl.handle.net/1842/37522 https://doi.org/10.7488/era/806 |
| Summary: | Patagonia in southernmost South America is situated in a climatically sensitive region of the Southern Hemisphere. It is the only stretch of land to fully intersect the southern westerly wind belt, an important component of the global climate system. Robust glacial chronologies from this region can help unravel the interhemispheric (a-)synchronicity of climate events and the underlying drivers of glaciation and climate change. Despite exceptional preservation of moraine records in Patagonia, little is known about the build-up and the evolution of the last Patagonian Ice Sheet (PIS) throughout the entire last glacial cycle. The response of glaciers to abrupt climate events during the last deglaciation and glacier change during the Holocene remain poorly resolved in many parts of Patagonia. This thesis reconstructs the extent and timing of glacial advances and the evolution of palaeolakes on the eastern side of Monte San Lorenzo. This site was chosen for its well preserved geomorphological record and the potential to yield new insights in the glacial and climate history of the region. Geomorphological mapping revealed three landform assemblages. In the Belgrano valley, the geomorphology is dominated by three large moraine systems and associated outwash terraces deposited during advances of the former Belgrano glacier. Once the Belgrano glacier retreated to within its trough, the geomorphology is dominated by glaciolacustrine landforms documenting a formation of a higher, palaeolake Belgrano. Nearer the mountains, moraines, flutes and active outwash tracts evidence recent, Holocene mountain glaciation. Cosmogenic nuclide exposure dating reveals that the maximum extent of the Belgrano glacier occurred at ~75 ka, towards the end of Marine Isotope Stage (MIS) 5. The second advance dated at ~25 ka, coincident with the global Last Glacial Maximum (gLGM), was significantly smaller. Third advance of the Belgrano glacier was dated at ~13 ka, coeval with Antarctic Cold Reversal (ACR). Subsequent rapid ice retreat, ... |
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