Lateglacial and holocene hydroclimate inferred from a groundwater flow-through lake, northern rocky mountains, USA

Holocene

Volumn 19, Issue 4, 2009, Pages 523-535

  Shapley, M D ^a   Ito, E ^a   Donovan, J J ^b  

^a UNIVERSITY OF MINNESOTA   (United States)

^b WEST VIRGINIA UNIVERSITY   (United States)

Author keywords

Aragonite; Endogenic carbonate mineralogy; Lakes and groundwater; Oxygen isotopes; Western North American paleoclimate.

Indexed keywords

ARAGONITE; CLIMATE EFFECT; CLIMATE VARIATION; GROUNDWATER FLOW; GROUNDWATER-SURFACE WATER INTERACTION; HOLOCENE; INSOLATION; LAKE; LATE GLACIAL; MOUNTAIN REGION; PALEOCLIMATE; RECHARGE; RESIDENCE TIME; SEASONALITY; WARMING;

NORTH AMERICA; ROCKY MOUNTAINS;

EID: 67749088397     PISSN: 09596836     EISSN: None     Source Type: Journal    
DOI: 10.1177/0959683609104029     Document Type: Article

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