New palynological data from the Late Pleistocene glacial refugium of South-West Iberia: The case of Doñana

2021 ◽  
pp. 104431
Author(s):  
S. Fernández ◽  
J.S. Carrión ◽  
J. Ochando ◽  
P. González-Sampériz ◽  
M. Munuera ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Glacial Refugium ◽  
Palynological Data ◽  
South West

A late Pleistocene marine glacial refugium in the south-west of Hainan Island, China: Phylogeographical insights from the brown alga Sargassum polycystum

2017 ◽  
Vol 45 (2) ◽  
pp. 355-366 ◽  
Author(s):  
Zi-Min Hu ◽  
Attachai Kantachumpoo ◽  
Ruo-Yu Liu ◽  
Zhong-Min Sun ◽  
Jian-Ting Yao ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Brown Alga ◽  
Hainan Island ◽  
Glacial Refugium ◽  
The South ◽  
Sargassum Polycystum ◽  
South West

scholarly journals Late Pleistocene stratigraphy of IODP Site U1396 and compiled chronology offshore of south and south west Montserrat, Lesser Antilles

2014 ◽  
Vol 15 (7) ◽  
pp. 3000-3020 ◽  
Author(s):  
Deborah Wall-Palmer ◽  
Maya Coussens ◽  
Peter J. Talling ◽  
Martin Jutzeler ◽  
Michael Cassidy ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Lesser Antilles ◽  
South West

scholarly journals Late Pleistocene speciation of three closely related tree peonies endemic to the Qinling–Daba Mountains, a major glacial refugium in Central China

2019 ◽  
Vol 9 (13) ◽  
pp. 7528-7548 ◽  
Author(s):  
Xing‐Xing Xu ◽  
Fang‐Yun Cheng ◽  
Li‐Ping Peng ◽  
Yan‐Qiang Sun ◽  
Xian‐Ge Hu ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Central China ◽  
Glacial Refugium

scholarly journals Depositional system and palaeoclimatic interpretations of Middle to Late Pleistocene travertines: Kocabaş, Denizli, south-west Turkey

Sedimentology ◽  
2015 ◽  
Vol 62 (5) ◽  
pp. 1360-1383 ◽  
Author(s):  
Ezher Toker ◽  
Mine Sezgül Kayseri-Özer ◽  
Mehmet Özkul ◽  
Sándor Kele
Keyword(s):  
Late Pleistocene ◽  
South West ◽  
Depositional System

Rock Glaciers of the Dalton Range, Kluane Ranges, South-West Yukon Territory, Canada

1988 ◽  
Vol 34 (118) ◽  
pp. 327-332 ◽  
Author(s):  
Peter G. Johnson ◽  
Diane Lacasse
Keyword(s):  
Late Pleistocene ◽  
Lower Cretaceous ◽  
Drainage System ◽  
Upper Jurassic ◽  
Yukon Territory ◽  
High Susceptibility ◽  
Frost Action ◽  
South West ◽  
Glacier Ice ◽  
Rock Glaciers

Abstract Glaciated valleys of the Dalton Range in the south-west Yukon Territory are dominated by rock glaciers identified as glacier ice-cored debris systems. The two rock glaciers studied have different amounts of deformation at present, resulting from post-formation mechanics. The primary formation of lobes of the rock glaciers resulted from periods of glacier activity in the Neoglacial, although older lobes, probably late Pleistocene in age, occur below the Neoglacial lobes. The hydrological systems of the rock glaciers have played a major role in the post-formation deformation of the land forms and the present drainage system is entirely sub-surface. The explanation for the extensive occurrence of rock glaciers in the Dalton Range is lithological as a result of the high susceptibility of the Upper Jurassic/Lower Cretaceous sediments to frost action and glacier erosion.

scholarly journals Rock Glaciers of the Dalton Range, Kluane Ranges, South-West Yukon Territory, Canada

1988 ◽  
Vol 34 (118) ◽  
pp. 327-332
Author(s):  
Peter G. Johnson ◽  
Diane Lacasse
Keyword(s):  
Late Pleistocene ◽  
Lower Cretaceous ◽  
Drainage System ◽  
Upper Jurassic ◽  
Yukon Territory ◽  
High Susceptibility ◽  
Frost Action ◽  
South West ◽  
Glacier Ice ◽  
Rock Glaciers

AbstractGlaciated valleys of the Dalton Range in the south-west Yukon Territory are dominated by rock glaciers identified as glacier ice-cored debris systems. The two rock glaciers studied have different amounts of deformation at present, resulting from post-formation mechanics.The primary formation of lobes of the rock glaciers resulted from periods of glacier activity in the Neoglacial, although older lobes, probably late Pleistocene in age, occur below the Neoglacial lobes. The hydrological systems of the rock glaciers have played a major role in the post-formation deformation of the land forms and the present drainage system is entirely sub-surface. The explanation for the extensive occurrence of rock glaciers in the Dalton Range is lithological as a result of the high susceptibility of the Upper Jurassic/Lower Cretaceous sediments to frost action and glacier erosion.

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