Warming nondormant tree roots advances aboveground spring phenology in temperate trees

被引:3
|
作者
Malyshev, Andrey V. [1 ]
Blume-Werry, Gesche [1 ,2 ]
Spiller, Ophelia [1 ]
Smiljanic, Marko [1 ]
Weigel, Robert [3 ,4 ]
Kolb, Alexander [1 ]
Nze, Byron Ye [1 ]
Maerker, Frederik [1 ]
Sommer, Freymuth Carl-Fried Johannes [1 ]
Kinley, Kinley [1 ,4 ]
Ziegler, Jan [1 ,5 ]
Pasang, Pasang [1 ]
Mahara, Robert [1 ,6 ]
Joshi, Silviya [1 ]
Heinsohn, Vincent [1 ]
Kreyling, Juergen [1 ]
机构
[1] Univ Greifswald, Inst Bot & Landscape Ecol, D-17489 Greifswald, Germany
[2] Umea Univ, Dept Ecol & Environm Sci, S-90187 Umea, Sweden
[3] Univ Goettingen, Plant Ecol & Ecosyst Res, D-37073 Gottingen, Germany
[4] Univ Bayreuth, Ecol Bot Garden, D-95447 Bayreuth, Germany
[5] Swiss Fed Res Inst WSL, CH-8903 Birmensdorf, Switzerland
[6] Dept Forest & Pk Serv, Thimphu 1345, Bhutan
关键词
below- vs aboveground dormancy; Betula pendula; Fagus sylvatica; Populus nigra; root-zone temperature; root-to-leaf communication; soil insulation; soil warming; SHOOT GROWTH; ZONE TEMPERATURE; FOREST; WINTER; SENSITIVITY; PHOTOPERIOD; TURNOVER; EXCHANGE; DORMANCY; RELEASE;
D O I
10.1111/nph.19304
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Climate warming advances the onset of tree growth in spring, but above- and belowground phenology are not always synchronized. These differences in growth responses may result from differences in root and bud dormancy dynamics, but root dormancy is largely unexplored. We measured dormancy in roots and leaf buds of Fagus sylvatica and Populus nigra by quantifying the warming sum required to initiate above- and belowground growth in October, January and February. We furthermore carried out seven experiments, manipulating only the soil and not air temperature before or during tree leaf-out to evaluate the potential of warmer roots to influence budburst timing using seedlings and adult trees of F. sylvatica and seedlings of Betula pendula. Root dormancy was virtually absent in comparison with the much deeper winter bud dormancy. Roots were able to start growing immediately as soils were warmed during the winter. Interestingly, higher soil temperature advanced budburst across all experiments, with soil temperature possibly accounting for c. 44% of the effect of air temperature in advancing aboveground spring phenology per growing degree hour. Therefore, differences in root and bud dormancy dynamics, together with their interaction, likely explain the nonsynchronized above- and belowground plant growth responses to climate warming.
引用
收藏
页码:2276 / 2287
页数:12
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