Cited by 188Geology and Paleoclimatology ResearchCryospheric studies and observationsArchaeology and ancient environmental studies

Late Pleistocene and Holocene palaeoclimate and glacier fluctuations in Patagonia

Glasser, Neil F, Harrison, Stephan, Winchester, Vanessa, Aniya, Masamu·2004·Global and Planetary Change

Integrity signals

Registry

Crossref · 10.1016/j.gloplacha.2004.03.002

Cites

135 of 135 references verified0 citation errors · 0 not checkable

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  • The Patagonian Ice Sheet covered the southern Patagonian Andes between ∼47 000 and ∼17 000 yr BP, extending from latitudes 38 to 55° S with an estimated area of ∼490 000 km2, volume of ∼550 000 km3, and average and maximum thickness of 1100 and 2500 m.

    “The Patagonian Ice Sheet covered the southern Patagonian Andes between ∼ 47 000 and ∼ 17 000 yr BP, extending from latitudes 38 to 55° S with an estimated area of ∼ 490 000 km 2 (Fig. 1a); volume of ∼ 550 000 km 3 ; and average and maximum thickness of 1100 and 2500 m, respectively, based on preserved glacial geomorphology, stratigraphy, palaeoecology, and geochronological data (Moreno et al., 199”
  • A glacial minimum was attained around 13 000 yr BP.

    “A glacial minimum must have been attained around 13 000 yr BP, but several glacial advances were recorded since that time, and the last recorded one was the Little Ice Age (LIA) with an apex around 1630 CE, well dated by terminal moraines around the present-day NPI and SPI (Ivins andJames, 1999, 2004;McCulloch et al., 2000;Glasser et al., 2004Glasser et al., , 2008Glasser et al., , 2011;;Davies”
  • The last recorded glacial advance was the Little Ice Age with an apex around 1630 CE.

    “A glacial minimum must have been attained around 13 000 yr BP, but several glacial advances were recorded since that time, and the last recorded one was the Little Ice Age (LIA) with an apex around 1630 CE, well dated by terminal moraines around the present-day NPI and SPI (Ivins andJames, 1999, 2004;McCulloch et al., 2000;Glasser et al., 2004Glasser et al., , 2008Glasser et al., , 2011;;Davies”

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Authors
Glasser, N. F., Harrison, S., Winchester, V., & Aniya, M.
Affiliations
  • Aberystwyth University (GB)
  • University of Oxford (GB)
  • University of Tsukuba (JP)
Corresponding author
Glasser, Neil F
Venue
Global and Planetary Change
Publisher
Elsevier BV
Published
2004-08
Volume
43
Issue
1-2
Pages
79-101
ISSN
0921-8181 (ISSN-L)
OpenAlex
W2053944012
Cited by
188
References
145
Citations by year
2026: 2 · 2025: 5 · 2024: 3 · 2023: 16 · 2022: 12 · 2021: 5 · 2020: 18 · 2019: 6 · 2018: 6 · 2017: 6 · 2016: 5 · 2015: 5 · 2014: 8 · 2013: 9 · 2012: 13
FWCI
4.07
Type
journal article
Language
en
Open access
closed
Locations
Global and Planetary Change (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Cryospheric studies and observations
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Archaeology and ancient environmental studies
Keywords
paleoclimate, glacier fluctuations, Late Pleistocene, Holocene, Patagonian Icefields, Younger Dryas, Neoglacial, Little Ice Age, Holocene warming, Andes, radiocarbon dating, paleotemperature

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