Did debris-covered glaciers serve as pleistocene refugia for plants? A new hypothesis derived from observations of recent plant growth on glacier surfaces

Arctic, Antarctic, and Alpine Research

Volumn 39, Issue 2, 2007, Pages 245-257

  Fickert, Thomas ^a   Friend, Donald ^b   Grüninger, Friederike ^a   Molnia, Bruce ^c   Richter, Michael ^d  

^a UNIVERSITY OF PASSAU   (Germany)

^b MINNESOTA STATE UNIVERSITY   (United States)

^c U S GEOLOGICAL SURVEY   (United States)

^d UNIVERSITY OF ERLANGEN NUREMBERG   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

FLORISTICS; GLACIAL DEBRIS; MICROCLIMATE; PLEISTOCENE; REFUGIUM; SOIL TEMPERATURE; SPATIAL DISTRIBUTION; VASCULAR PLANT;

CASCADE RANGE; MOUNT RAINIER; NORTH AMERICA; UNITED STATES; WASHINGTON [UNITED STATES];

TRACHEOPHYTA;

EID: 34249930674     PISSN: 15230430     EISSN: None     Source Type: Journal    
DOI: 10.1657/1523-0430(2007)39[245:DDGSAP]2.0.CO;2     Document Type: Article

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