4.7 Article

Dynamics of low-temperature acclimation in temperate and boreal conifer foliage in a mild winter climate

Journal

TREE PHYSIOLOGY
Volume 28, Issue 9, Pages 1365-1374

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/treephys/28.9.1365

Keywords

abies; cold; frost; LN2-quench hardiness tolerance; Picea; Pinus; raffinose; stachyose; sucrose; sugar

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To provide baseline data for physiological studies of extreme low-temperature (LT) tolerance in boreal conifers. we profiled LT stress responses, liquid nitrogen (LN2)-quench tolerance, and sugar concentrations in foliage of boreal-temperate species pairs in the genera Abies, Picea and Pinus, growing in an arboretum in a temperate oceanic climate from August 2006 through April 2007. The boreal species acclimated more rapidly and deeply than the temperate species, acquiring LN2-quench tolerance by late November, despite unusually warm conditions throughout the autumn and early Winter. Maximum LT tolerance in the temperate species was in the -25 to -35 degrees C range, and was reached only after a period of freezing temperatures in late January and February. During LT acclimation in the temperate species, sigmoid temperature-relative electrolyte leakage (REL) curves shifted toward lower temperatures, whereas in boreal species there was both a temperature shift and a lowering of the maximum REI.. Until it fell below a threshold associated with irreversible injury. These differences may reflect differences in mechanisms of LT acclimation and LT tolerance. The concentrations of total and individual sugars did not show a clear pattern that could differentiate the boreal and temperate groups. Raffinose and, in three of the six species, stachyose showed the closest association with LT tolerance. Sugar concentrations, principally sucrose, decreased during mild weather, perhaps because of respiratory losses or phloem export, and increased after periods of freezing temperatures. Low-temperature acclimation in boreal species appears to follow a rigid program that may affect their ability to avoid excessive respiratory losses in the event of continued climate warming in boreal regions.

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