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Jomelli Vincent, Grancher D., Brunstein D., Solomina O. (2008). Recalibration of the yellow Rhizocarpon growth curve in the Cordillera Blanca (Peru) and implications for LIA chronology. Geomorphology, 93 (3-4), 201-212. ISSN 0169-555X

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Lien direct chez l'éditeur doi:10.1016/j.geomorph.2007.02.021

Titre
Recalibration of the yellow Rhizocarpon growth curve in the Cordillera Blanca (Peru) and implications for LIA chronology
Année de publication2008
Type de documentArticle référencé dans le Web of Science WOS:000255899700004
AuteursJomelli Vincent, Grancher D., Brunstein D., Solomina O.
SourceGeomorphology, 2008, 93 (3-4), p. 201-212. ISSN 0169-555X
RésuméA new lichen dating method and new moraine observations enabled us to improve the chronology of glacier advances in the Cordillera Blanca (Peru) during the Little Ice Age (LIA). Our results reveal that an early LIA glacial advance occurred around AD 1330 +/- 29. However, a second major glacial advance at the beginning of the 17th century overlapped the earlier stage for most glaciers. Hence, this second glacial stage, dated from AD 1630 +/- 27, is considered as the LIA maximum glacial advance in the Cordillera Blanca. During the 17th-18th centuries, at least three glacial advances were recorded synchronously for the different glaciers (AD 1670 +/- 24, 1730 +/- 21, and 1760 +/- 19). The moraines corresponding to the two first stages are close to the one in 1630 suggesting a slow recession of about 18% in the total length of the glacier. From the LIA maximum extent to the beginning of the 20th century, the 24 glaciers have retreated a distance of about 1000 in, corresponding to a reduction of 30% in their length. This rate is comparable to that observed during the 20th century. Estimates of palaeo-Equilibrium Line Altitudes show an increase in attitude of about 100 m from the LIA maximum glacial extension at the beginning of the 17th century to the beginning of the 20th century. Because long time series are not available for precipitation and temperature, this glacial retreat is difficult to explain by past climate changes. However, there is a fair correspondence between changes in glacier length and the delta O-18 recorded in the Quelccaya ice core at a century timescale. Our current knowledge of tropical glaciers and isotope variations leads us to suggest that this common tropical signal reflects a change from a wet LIA to the drier conditions of today. Finally, a remarkable synchronicity is observed with glacial variations in Bolivia, suggesting a common regional climatic pattern during the LIA.
Plan de classementGéologie et formations superficielles [064]
LocalisationFonds IRD [F B010042605]
Identifiant IRDfdi:010042605
Lien permanenthttp://www.documentation.ird.fr/hor/fdi:010042605

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