Interhemispheric Correlation of Late Pleistocene Glacial Events

@article{Lowell1995InterhemisphericCO,
  title={Interhemispheric Correlation of Late Pleistocene Glacial Events},
  author={Thomas V. Lowell and Christoph Heusser and Bj{\o}rn G. Andersen and Patricio I. Moreno and Arturo Hauser and Linda E. Heusser and C. Schl�chter and David R. Marchant and George H. Denton},
  journal={Science},
  year={1995},
  volume={269},
  pages={1541 - 1549}
}
A radiocarbon chronology shows that piedmont glacier lobes in the Chilean Andes achieved maxima during the last glaciation at 13,900 to 14,890, 21,000, 23,060, 26,940, 29,600, and ≥33,500 carbon-14 years before present (14C yr B.P.) in a cold and wet Subantarctic Parkland environment. The last glaciation ended with massive collapse of ice lobes close to 14,00014C yr B.P., accompanied by an influx of North Patagonian Rain Forest species. In the Southern Alps of New Zealand, additional glacial… Expand
Radiocarbon chronology of the last glacial maximum and its termination in northwestern Patagonia
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Interhemispheric climate links revealed by a late-glacial cooling episode in southern Chile
TLDR
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Abstract The Late Pleistocene glacial and climate history in the dry Central Andes is not well known so far, mainly because of the lack of suitable material for radiocarbon dating. In order toExpand
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Spatial variability of deglaciation and warming since the last glacial maximum is critical for relating hemispheric or regional climate-forcing mechanisms to global orbitally-induced insolationExpand
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Late Glacial to Holocene ice retreat was investigated along a 120 km long fjord system, reaching from Gran Campo Nevado (GCN) to Seno Skyring in the southernmost Andes (53°S). The aim was to improveExpand
The deglaciation of the Americas during the Last Glacial Termination
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Deglacial and postglacial climate history in east-central Isla Grande De Chiloé, Southern Chile (43°S)
Palynologic and stratigraphic data from Laguna Tahui (42°50′S, 73°30′W) indicate cool–temperate and humid conditions there between 14,000 and 10,000 14C yr B.P., followed by warmer andExpand
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