Reversal of multicentury tree growth improvements and loss of synchrony at mountain tree lines point to changes in key drivers

Journal of Ecology

Volumn 100, Issue 3, 2012, Pages 782-794

  Fajardo, Alex ^a   Mcintire, Eliot J B ^b,c  

^a CENTRO DE INVESTIGACIÓN EN ECOSISTEMAS DE LA PATAGONIA CIEP   (Chile)

^b UNIVERSITÉ LAVAL   (Canada)

^c LAURENTIAN FORESTRY CENTRE   (Canada)

Author keywords

Altitudinal gradients; Chile; Climate change; Nothofagus pumilio; Patagonia; Pinus albicaulis; Plant climate interactions; Tree line ecotone

Indexed keywords

ALTITUDE; BASAL AREA; CLIMATE CHANGE; CONIFEROUS TREE; DEMOGRAPHY; ECOLOGICAL MODELING; ECOTONE; GLOBAL WARMING; GROWTH RATE; MOUNTAIN REGION; POPULATION DECLINE; RECRUITMENT (POPULATION DYNAMICS); SYNCHRONY; TEMPERATURE EFFECT; TREELINE; TWENTIETH CENTURY;

CHILE; MONTANA; UNITED STATES;

MIMOSA; NOTHOFAGUS PUMILIO; PINUS ALBICAULIS;

EID: 84859710020     PISSN: 00220477     EISSN: 13652745     Source Type: Journal    
DOI: 10.1111/j.1365-2745.2012.01955.x     Document Type: Article

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