Reply to comment by Hillaire-Marcel and de Vernal on “A sedimentary record from the Makarov Basin, Arctic Ocean, reveals changing middle to late Pleistocene glaciation patterns” [Quat. Sci. Rev., 270 (2021), p. 107176]

2022 ◽  
Vol 276 ◽  
pp. 107298
Author(s):  
Wenshen Xiao ◽  
Leonid Polyak ◽  
Christelle Not ◽  
Rujian Wang
Keyword(s):  
Arctic Ocean ◽  
Late Pleistocene ◽  
Pleistocene Glaciation ◽  
Sedimentary Record ◽  
Makarov Basin

A sedimentary record from the Makarov Basin, Arctic Ocean, reveals changing middle to Late Pleistocene glaciation patterns

2021 ◽  
Vol 270 ◽  
pp. 107176
Author(s):  
Wenshen Xiao ◽  
Leonid Polyak ◽  
Rujian Wang ◽  
Christelle Not ◽  
Linsen Dong ◽  
...  
Keyword(s):  
Arctic Ocean ◽  
Late Pleistocene ◽  
Pleistocene Glaciation ◽  
Sedimentary Record ◽  
Makarov Basin

Late Pleistocene glaciation of the Mt Giluwe volcano, Papua New Guinea

2011 ◽  
Vol 30 (19-20) ◽  
pp. 2676-2689 ◽  
Author(s):  
Timothy T. Barrows ◽  
Geoffrey S. Hope ◽  
Michael L. Prentice ◽  
L. Keith Fifield ◽  
Stephen G. Tims
Keyword(s):  
Papua New Guinea ◽  
Late Pleistocene ◽  
New Guinea ◽  
Pleistocene Glaciation

scholarly journals NEW DATA ON THE EXTENT OF THE LAST PLEISTOCENE GLACIATION IN THE GORNAYA SHORIA

2017 ◽  
Vol 2017 (3) ◽  
pp. 24-26
Author(s):  
Марина Адаменко ◽  
Marina Adamenko ◽  
Ярослав Гутак ◽  
Yaroslav Gutak ◽  
Богдан Воробьев ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Field Research ◽  
Early Summer ◽  
Mountain Region ◽  
Pleistocene Glaciation ◽  
Mountain Valley ◽  
North East ◽  
Last Glaciation ◽  
Extreme North

The article presents and summarizes the results of a field research on glacial relief of the Gornaya Shoria mountain region, within the Patyn mountain massif. The Patyn-2017 expedition was organized by the Russian Geographic Society. This region has been very poorly studied in the paleogeographical aspect. The available material can give only an approximate assessment of last glaciation in the Gornaya Shoria mountain region. The massif of Mount Patyn (1630 m) is located in the extreme north-east of the Mountain Shoria on the watershed of the Tashtyk and the Mrassu rivers. At present, the massif is completely devoid of modern glaciation. Early summer snowfields appear on the leeward slopes of the eastern, southern and northern macroslopes. The moraine deposits and the configuration of the relief forms have proved mountain-valley glaciation in the Late Pleistocene. The article also touches upon the issue of the origin of the so-called «megaliths» of the massif of Pustag mountain.

Contrasting glacial/interglacial regimes in the western Arctic Ocean as exemplified by a sedimentary record from the Mendeleev Ridge

2004 ◽  
Vol 203 (1-2) ◽  
pp. 73-93 ◽  
Author(s):  
Leonid Polyak ◽  
William B Curry ◽  
Dennis A Darby ◽  
Jens Bischof ◽  
Thomas M Cronin
Keyword(s):  
Arctic Ocean ◽  
Sedimentary Record ◽  
Western Arctic Ocean ◽  
Western Arctic
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