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Late Pleistocene and Holocene palaeoclimate and glacier fluctuations in Patagonia
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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 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”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Glasser et al., 2004
In the citing paper
“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”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Glasser et al., 2004
In the citing paper
“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”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Glasser et al., 2004
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10 of the 145 references couldn’t be matched to a known paper.
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Hu, Y., Huang, R., Zhu, H., Zhu, X., Grießinger, J., Liang, E., Farías-Barahona, D., Tabone, I., & Meier, W. J.-H. (2026) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2026.114056
Trends in south pole particle concentrations imply holocene westerly wind strengthening
Chesler, A., Winski, D., Kreutz, K. J., Koffman, B., Osterberg, E. C., Ferris, D., Thundercloud, Z., Cole‐Dai, J., Kurbatov, M. W. A., Putnam, A., et al. (2026) · Climate of the past · doi:10.5194/cp-22-1741-2026
Metadata
- 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
- Social Sciences › Archeology › 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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