Cited by 75

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Ice-Core Pollen Record of Climatic Changes in the Central Andes during the last 400 yr

Liu, Kam-biu, Reese, Carl A., Thompson, Lonnie G.·2005·Quaternary Research

Abstract

This paper presents a high-resolution ice-core pollen record from the Sajama Ice Cap, Bolivia, that spans the last 400 yr. The pollen record corroborates the oxygen isotopic and ice accumulation records from the Quelccaya Ice Cap and supports the scenario that the Little Ice Age (LIA) consisted of two distinct phases�"a wet period from AD 1500 to 1700, and a dry period from AD 1700 to 1880. During the dry period xerophytic shrubs expanded to replace puna grasses on the Altiplano, as suggested by a dramatic drop in the Poaceae/Asteraceae (P/A) pollen ratio. The environment around Sajama was probably similar to the desert-like shrublands of the Southern Bolivian Highlands and western Andean slopes today. The striking similarity between the Sajama and Quelccaya proxy records suggests that climatic changes during the Little Ice Age occurred synchronously across the Altiplano.

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Crossref · 10.1016/j.yqres.2005.06.001

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  • Paleoclimatic data, based on Mount Sajama's ice core and the Polylepis growth rings, indicates relatively stable conditions since late pre-Hispanic times, with a significantly wetter period in the 19th century A.D.

    “Paleoclimatic data, based on Mount Sajama's ice core and the Polylepis growth rings, indicates relatively stable conditions since late pre-Hispanic times, with a significantly wetter period in the 19th century A.D. (Thompson 1995;Liu, Reese, and Thompson 2005;Morales et al. 2012).”

    From The longue durée of andean movement networks: case study in the lauca altiplano (2025) · cites this paper as Liu, Reese, and Thompson 2005

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Metadata

Authors
Liu, K.-B., Reese, C. A., & Thompson, L. G.
Venue
Quaternary Research
Published
2005-09
Volume
64
Issue
2
Pages
272-278
ISSN
  • 0033-5894
  • 1096-0287
Cited by
75
References
0
Language
en

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