CO2 elevation and soil warming reduce cold hardiness of jack pine under photoperiods of seed origin and latitudes of potential migration

New Forests ◽  
2021 ◽  
Author(s):  
Shah Md. Newaz ◽  
Qing-Lai Dang ◽  
Rongzhou Man
1976 ◽  
Vol 52 (6) ◽  
pp. 283-289 ◽  
Author(s):  
C. W. Yeatman

A program of provenance testing, seed production and genetic improvement of jack pine was developed in the Baskatong region of western Quebec through sustained collaboration among government forest services and forest industry. Research plantations demonstrated, within a period of 10 years from establishment, the superiority in growth, cold hardiness and disease resistance of regionally adapted local seed sources. Critical differences were evident between provenances from the Boreal Forest Region and those from the adjacent Sections of the Great Lakes — St. Lawrence Forest Region.A 300-acre (120 ha) seed production area was created within a genetically superior jack pine population of natural origin in the Côte Jaune area west of Lake Baskatong. Within this population, 325 plus trees were selected, marked and recorded over two years by student crews employed in the summer. Seed harvested from the felled plus trees will be used to create a seedling seed orchard and to establish progeny tests. The plus trees are to be grafted for controlled breeding among selected progeny-tested clones at a later date. This cooperative program of tree improvement will ensure the future supply of high quality seed that will maintain and enhance the value of the forest resource.


2017 ◽  
Vol 47 (8) ◽  
pp. 1116-1122 ◽  
Author(s):  
Rongzhou Man ◽  
Pengxin Lu ◽  
Qing-Lai Dang

Conifer winter damage results primarily from loss of cold hardiness during unseasonably warm days in late winter and early spring, and such damage may increase in frequency and severity under a warming climate. In this study, the dehardening dynamics of lodgepole pine (Pinus contorta Dougl. ex. Loud), jack pine (Pinus banksiana Lamb.), white spruce (Picea glauca (Moench) Voss), and black spruce (Picea mariana (Mill.) B.S.P.) were examined in relation to thermal accumulation during artificial dehardening in winter (December) and spring (March) using relative electrolyte leakage and visual assessment of pine needles and spruce shoots. Results indicated that all four species dehardened at a similar rate and to a similar extent, despite considerably different thermal accumulation requirements. Spring dehardening was comparatively faster, with black spruce slightly hardier than the other conifers at the late stage of spring dehardening. The difference, however, was relatively small and did not afford black spruce significant protection during seedling freezing tests prior to budbreak in late March and early May. The dehardening curves and models developed in this study may serve as a tool to predict cold hardiness by temperature and to understand the potential risks of conifer cold injury during warming–freezing events prior to budbreak.


Botany ◽  
2016 ◽  
Vol 94 (2) ◽  
pp. 117-126 ◽  
Author(s):  
Rongzhou Man ◽  
Steve Colombo ◽  
Pengxin Lu ◽  
Qing-Lai Dang

Compared with the effects of spring frosts on opening buds or newly flushed tissues, winter freezing damage to conifers, owing to temperature fluctuations prior to budbreak, is rare and less known. In this study, changes in cold hardiness (measured based on electrolyte leakage and needle damage) and spring budbreak were assessed to examine the responses of four boreal conifer species — black spruce (Picea mariana (Mill.) B.S.P.), white spruce (Picea glauca) (Moench) Voss), jack pine (Pinus banksiana Lamb.), and lodgepole pine (Pinus contorta Dougl. ex. Loud.) — to different durations of experimental warming (16 °C day to –2 °C night with a 10 h photoperiod, except for night temperatures during November warming (+2 °C)). Seedlings showed increased responses to warming from November to March, while the capacity to regain the cold hardiness lost to warming decreased during the same period. This suggests an increasing vulnerability of conifers to temperature fluctuations and freezing damage with the progress of chilling and dormancy release from fall to spring. Both lodgepole pine and jack pine initiated spring growth earlier and had greater responses to experimental warming in bud phenology than black spruce and white spruce, suggesting a greater potential risk of frost/freezing damage to pine trees in the spring.


Botany ◽  
2018 ◽  
Vol 96 (2) ◽  
pp. 111-119 ◽  
Author(s):  
Md. Shah Newaz ◽  
Qing-Lai Dang ◽  
Rongzhou Man

Trees may migrate northward in response to climate change and become exposed to new photoperiod and soil moisture regimes. This study assessed the impacts of photoperiod and its interaction with soil moisture and carbon dioxide concentration ([CO2]) on the hydraulic conductivity in jack pine (Pinus banksiana Lamb.) and its vulnerability to xylem embolism. Seedlings were exposed to 400 vs. 950 μmol·mol−1 [CO2], 60%–70% vs. 30%–40% (of field capacity) soil moisture, and photoperiods of seed origin and 5° and 10° north of seed origin in greenhouses. Cavitation vulnerability curves were measured for determining the xylem pressure at which 50% hydraulic conductivity was lost (ΨPLC50). It was found that elevated [CO2] significantly increased hydraulic conductivity, whereas low soil moisture decreased it. Under elevated [CO2], the xylem became progressively more vulnerable to embolism with changes in photoperiod regime from the seed origin to 10° north of the seed origin, as indicated by the progressively less negative ΨPLC50. However, no such a trend was detected under the ambient [CO2]. The results suggest that the species may become less resistant to drought as the atmospheric [CO2] increases, hindering the northward migration or seed transfers. Even within its current natural distribution range, trees near its northern boundary of the range may be more vulnerable to embolism as the atmospheric [CO2] increases even without any change in moisture conditions.


1969 ◽  
Vol 45 (6) ◽  
pp. 428-433 ◽  
Author(s):  
C. W. Yeatman ◽  
A. H. Teich

Genetic variation of jack pine and lodgepole pine is reviewed in relation to artificial regeneration in Canada. Broad patterns of variation conform to adaptational gradients in relation to latitude, length of growing season, temperature, and altitude. Intensive selection and breeding to increase productivity of these species has been initiated recently by a number of agencies in Canada but it will be some time before superior seed is available from seed orchards.Natural populations of jack pine and lodgepole pine will continue to supply bulk quantities of seed. Early improvement in the genetic quality of seed for reforestation will be made by the proper choice of seed source. Until provenance tests provide more definitive answers to seed movement, seed should be collected locally, i.e. within the geo-climatic zone in which it is to be used. Stands of good phenotypic quality should be designated for seed production well in advance of anticipated requirements for seed. Such stands may be developed as seed production areas or incorporated into harvesting schedules. Accurate records of seed origin should be maintained from seed collection to outplanting or direct seeding to provide a basis for future selection of prime sources for seed collection and of breeding stock.


1996 ◽  
Vol 26 (11) ◽  
pp. 2006-2014 ◽  
Author(s):  
Annette van Niejenhuis ◽  
William H. Parker

To improve our understanding of adaptive variation in jack pine, Pinusbanksiana Lamb., from north central Ontario, 64 seed sources were grown in three common garden tests, and relationships were determined between seedling performance and environment at seed origin. Twenty-three growth and phenological variables were studied, including seedling heights, needle flushing dates, timing of shoot elongation, fall foliage colour change, and drought survival. Significant components of variation were expressed among seed sources for all growth traits and many phenological characters. Linear regressions were run between seedling traits and climatic variables as well as spatial, soil, and vegetative variables that described the environment at seed origin. Resulting coefficients of determination were as high as 0.30. Principal component analysis was used to summarize the variation, with 33% and 21% of the variation accounted for by the first and second components, respectively. Regressions and mapping of principal component analysis scores indicated that the patterns of variation in this portion of the range of jack pine were clinal in nature; the patterns could be predicted by environment at seed origin. The greater growth potential of seedlings from the southwestern portion of the range, in contrast with those of the north shore of Lake Superior, reflected clinal trends seen in previous studies. Multiple regressions were run on the first and second sets of factor scores produced from principal component analysis against the climate variables, resulting in coefficients of determination of 0.30 and 0.38, respectively. Including soil and vegetative variables in the models resulted in only slightly higher coefficients. Thus, climate at seed origin should be considered as the prime factor when seed transfers are necessary in this area.


Trees ◽  
2009 ◽  
Vol 24 (1) ◽  
pp. 53-65 ◽  
Author(s):  
Yulia Savva ◽  
Ahmed Koubaa ◽  
Francine Tremblay ◽  
Yves Bergeron

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