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Timing and dynamics of glaciation in the Ikh Turgen Mountains, Altai region, High Asia

Blomdin, Robin (author)
Stockholms universitet,Institutionen för naturgeografi
Stroeven, Arjen P. (author)
Stockholms universitet,Institutionen för naturgeografi
Harbor, Jonathan M. (author)
Stockholms universitet,Institutionen för naturgeografi,Purdue University, USA
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Gribenski, N. (author)
Stockholms universitet,Institutionen för naturgeografi,University of Bern, Switzerland
Caffee, M. W. (author)
Heyman, Jakob (author)
Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences
Rogozhina, I. (author)
Ivanov, M. N. (author)
Petrakov, D. A. (author)
Walther, M. (author)
Rudoy, A. N. (author)
Zhang, W. (author)
Orkhonselenge, A. (author)
Hättestrand, Clas (author)
Stockholms universitet,Institutionen för naturgeografi
Lifton, N. A. (author)
Jansson, Krister N. (author)
Stockholms universitet,Institutionen för naturgeografi
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 (creator_code:org_t)
Elsevier BV, 2018
2018
English.
In: Quaternary Geochronology. - : Elsevier BV. - 1871-1014 .- 1878-0350. ; 47, s. 54-71
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Spanning the northern sector of High Asia, the Altai region contains a rich landform record of glaciation. We report the extent, chronologies, and dynamics of two paleoglaciers on opposite flanks of the Ikh Turgen mountains (In Russian: Chikhacheva Range), straddling the border between Russia and Mongolia, using a combination of remote sensing-based glacial geomorphological mapping, 10Be surface exposure dating, and geomorphometric analysis. On the eastern side (Mongolia), the Turgen-Asgat paleoglacier, with its potential for developing a large accumulation area (∼257 km2), expanded 40 km down valley, and mean ages from a latero-frontal moraine indicate deglaciation during marine oxygen isotope stage (MIS) 3 (45.1 ± 1.8 ka, n = 4) and MIS 2 (22.8 ± 3.3 ka, n = 5). These minimum age constraints are consistent with other 10Be glacial chronologies and paleoclimate records from the region, which indicates glacier culmination during cold and wet conditions coinciding with MIS 3 (piedmont-style glaciation; inferred for a few sites across the region) and glacier culmination during cold and dry conditions coinciding with MIS 2 (mainly valley-style glaciation; inferred from several sites across the region). On the western side (Russia), the Boguty paleoglacier had a smaller accumulation area (∼222 km2), and advanced 30 km down valley across a low gradient forefield. Surface exposure ages from two moraine complexes on this side of the mountains exhibit wide scatter (∼14–53 ka, n = 8), making paleoclimate inferences and comparison to other proxies difficult. Ice surface profile reconstructions imply that the two paleoglaciers likely shared an ice divide. © 2018 Elsevier B.V.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Keyword

10Be surface exposure dating
Altai
Chikhacheva range
Geomorphometric analysis
Glacial geomorphology
Ikh Turgen mountains
Paleoglaciology
Altai

Publication and Content Type

ref (subject category)
art (subject category)

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