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1 riana (black spruce) and Picea glauca (white spruce).
2 orth American forest insect pest of pine and spruce.
3 ative-to-reproductive phase change in Norway spruce.
4 oncert to control perennial growth in Norway spruce.
5 ative-to-reproductive phase change in Norway spruce.
6 TR sequences from pea, broad bean and Norway spruce.
7 ree was up to 11 mg for birch and 1.8 mg for spruce.
8 discrimination and growth of black and white spruce.
9 nt-wide masting in European beech and Norway spruce.
10 glycosylated acetophenone pungenin in white spruce.
11 ne, portends range contraction for Engelmann spruce.
12 needles across different genotypes of white spruce.
13 an unstructured natural population of Norway spruce.
14 related species, lodgepole pine and interior spruce.
15 compensatory cis-trans factors is common in spruce.
18 arene is associated with resistance of Sitka spruce against white pine weevil, a major North American
20 e, and yellow birch, and negatively with red spruce and balsam fir - generally more so for adults tha
21 e climates is likely to become a problem for spruce and beech by the end of this century, but probabl
22 ies should be adjusted in the study area for spruce and beech to maintain productive and healthy fore
23 ee climate models, future risks increased in spruce and beech until the end of the century, but remai
24 Case studies with European beech, Qinghai spruce and Douglas-fir illustrate how the combination of
25 large-scale generation of transgenic Norway spruce and may prove useful for other conifer species.
27 s included mature black spruce, burned black spruce and paper birch, allowing us to determine vegetat
29 ciency of heterologous hybridization between spruce and pine species on microarrays has been document
30 nt resistance mechanism against SBW in white spruce and that insects can affect population structure
34 ol of growth cessation and bud set in Norway spruce as well as in local adaptation resulting in clina
35 gnocellulosic biomass, namely, beech, birch, spruce, ash, oak, and pine as well as commercial availab
36 dominant forest types (paper birch and black spruce) associated with location on elevated permafrost
39 ed changes in the phenolic content of Norway spruce bark upon E. polonica infection and the biochemic
40 group of phenolic compounds found in Norway spruce bark with a diaryl-ethene skeleton with known ant
41 h 2,3-trans stereochemistry were detected in spruce bark; dimeric and larger PAs contained flavan-3-o
42 ine beetle (Dendroctonus ponderosae) and the spruce beetle (D. rufipennis) have recently undergone ep
43 e against the insect but can be cleaved by a spruce beta-glucosidase, PgbetaGLU-1, which releases the
44 ugh the total quantity of C emitted from the SPRUCE Bog as CH4 is <2%, CH4 represents >50% of seasona
46 ng over a developmental time course of white spruce bud burst and shoot growth revealed two UGTs, PgU
47 tance of white spruce (Picea glauca) against spruce budworm (Choristoneura fumiferiana), a major fore
48 AFPs from overwintering insects, such as the spruce budworm (sbw) are 10-100 times more effective tha
49 tion between white spruce (Picea glauca) and spruce budworm (SBW, Choristoneura fumiferana) the most
52 a-solenoid protein mutant fibril structures (spruce budworm and Rhagium inquisitor antifreeze protein
53 based on the primary sequence of the mature spruce budworm antifreeze protein (sbwAFP) was construct
54 protein structure-function mechanism for the spruce budworm Choristoneura fumiferana AFP, including s
55 d length-to-width correlation for the mutant spruce budworm protein and the resultant UTS estimate is
56 ism by which the antifreeze protein from the spruce budworm, Choristoneura fumiferana, binds to ice.
60 t, many conifers, including pines, firs, and spruces, can accumulate chlorophyll and the light-harves
61 tland Responses Under Changing Environments (SPRUCE) climate change manipulation experiment to unders
62 ses of boreal forest recovery from prior red spruce decline, or human land use and disturbance, may s
63 likely the first steps in the degradation of spruce defenses to substrates that can enter the tricarb
65 thwest Alaska to explore factors influencing spruce establishment and recruitment near western treeli
66 e abundance suggests a moving front of white spruce establishment through time, driven by changes in
67 eriments wood chips of oak, poplar, hickory, spruce, fir, alder, beech, and beech with an apple-smoki
71 deciduous/hardwood forest (14.1 mug/m2-yr), spruce/fir forest (33.8 mug/m2-yr), and stunted growth a
72 ion hardwoods to throughfall in midelevation spruce/fir to cloudwater in high-elevation alpine forest
73 s pungenol and piceol commonly accumulate in spruce foliage in the form of the corresponding glycosid
74 forests and a relatively continuous gain of spruce forest associated with thermokarst and forest suc
76 dioxide (CO2) flux were measured at a black spruce forest in interior Alaska using the eddy covarian
78 ck tundra), as well as ecotonal boreal white spruce forest, and perform model simulations for the yea
80 -scale assembly of the next-generation white spruce genome sequence and provide a reference resource
82 7111 genomes confirm the reconstructed white spruce genome size in the 20 Gbp range, and show broad s
83 ng the PG29 V3 assembly and additional white spruce genomics and transcriptomics resources, we perfor
84 espectively, resistant and susceptible Sitka spruce genotypes are due to variation of (+)-3-carene sy
86 ibe the draft genome assemblies of two white spruce genotypes, PG29 and WS77111, innovative tools for
87 rticularly high frequencies were observed in spruce, grape (Vitis vinifera), and poplar (Populus tric
88 In this study, we examined patterns of black spruce growth and carbon isotopic composition in tree ri
89 atitudinal shift in the correlation of black spruce growth with temperature and reduced precipitation
90 ggest drought is causing a decline in boreal spruce growth, leading to predictions of widespread mort
92 ite, Western redcedar, Baldcypress, and Blue spruce) had median MAC values ranging from 1.4 x 10(-2)
95 terpenoids, we overexpressed a bifunctional spruce IDS, a geranyl diphosphate and geranylgeranyl dip
96 es C/EC seedlings and lowest in +8 degrees C spruce, implying that moderate, but not extreme, climate
97 system with mixed stands of silver birch and spruce in combination with regular harvest of leaves and
100 ; the presence of a least preferred species (spruce) in a mixture had no significant effect on moose
101 ct (+)-3-carene synthase-like genes of Sitka spruce include the three (+)-3-carene synthases, PsTPS-3
102 ion of phenolic needle metabolites in Norway spruce is regulated by many genes with small and additiv
104 flavan-3-ols, transcript abundance of Norway spruce LEUCOANTHOCYANIDIN REDUCTASE genes also increased
106 12 in three different conifer species, Sitka spruce, lodgepole pine (Pinus contorta), and jack pine (
108 We also comprehensively annotated the white spruce mevalonate, methylerythritol phosphate and phenyl
109 for American beech, downslope shifts for red spruce (more so in cool regions) and sugar maple, and no
112 E. polonica utilization of the most abundant spruce phenolics as carbon sources both correlated posit
113 eech (Fagus sylvatica) and coniferous Norway spruce (Picea abies Karst), planted in the same soil.
114 of Scots pine (Pinus sylvestris L.), Norway spruce (Picea abies L.), Siberian larch (Larix sibirica
115 ysis of the sRNA population from the conifer spruce (Picea abies) and compared the results with those
116 seed plants, including the gymnosperm Norway spruce (Picea abies) and the angiosperms rice (Oryza sat
117 ically important tree species such as Norway spruce (Picea abies) are required, if the frequency and
118 o through a long juvenile period, for Norway spruce (Picea abies) around 20 to 25 years, before devel
122 root formation and nutrient uptake by Norway spruce (Picea abies) seedlings with fast- and slow-growi
123 along hillslopes in four 80 years old Norway spruce (Picea abies) stands (REFs) with those in four si
124 tudy indicated that the resistance of Norway spruce (Picea abies) to Heterobasidion annosum s.l., a p
127 CO2 impacted leaf carbon dynamics in Norway spruce (Picea abies), a dominant northern forest species
128 genomes: white spruce (Picea glauca), Norway spruce (Picea abies), and loblolly pine (Pinus taeda).
129 namely silver birch (Betula pendula), Norway spruce (Picea abies), bird cherry (Prunus padus), mounta
130 in three major European tree species, Norway spruce (Picea abies), silver fir (Abies alba), and Europ
131 ied and functionally characterized in Norway spruce (Picea abies), the most widespread and economical
135 fossil needles that a now-extinct species of spruce (Picea critchfieldii sp. nov.) was widespread in
136 the prospect of implementing GS for interior spruce (Picea engelmannii x glauca) utilizing a genotype
137 ompounds involved in the resistance of white spruce (Picea glauca) against spruce budworm (Choristone
138 d the antagonistic interaction between white spruce (Picea glauca) and spruce budworm (SBW, Choriston
139 sequences from the needle mycobiome of white spruce (Picea glauca) at the northern treeline in Alaska
140 ed tissues of a single self-fertilized white spruce (Picea glauca) individual to dissect eQTLs accord
141 ructure and environmental data from 95 white spruce (Picea glauca) plots sampled across a longitudina
144 e sequenced chloroplast DNA (cpDNA) of white spruce (Picea glauca), a dominant boreal tree species, i
146 nvestigated transcriptome structure in white spruce (Picea glauca), aiming to delineate its modular o
147 publication of three conifer genomes: white spruce (Picea glauca), Norway spruce (Picea abies), and
148 es have been developed for the conifer white spruce (Picea glauca, Pinaceae), which has one of the la
149 ed on the geometry of bordered pits in black spruce (Picea mariana) and scanning electron microscopy
150 olly pine (Pinus taeda) PtCYP720B1 and Sitka spruce (Picea sitchensis) PsCYP720B4, have been characte
152 More than one-fifth of these timbers were spruce (Picea) or fir (Abies) that were hand-carried fro
153 3 years for three coniferous species (Norway spruce [Picea abies], Scots pine [Pinus sylvestris], and
154 crobes, and roots) over 18 months in a Sitka spruce plantation and directly compared the fate of this
161 y to expectations, warming reduced Engelmann spruce recruitment at and above treeline, as well as in
164 van-3-ols and PAs was investigated in Norway spruce saplings after wounding or inoculation with the f
166 ions for the period 2061-2090 were found for spruce seedling height (0.64), and for beech bud break a
169 suggest that PEG may improve the quality of spruce somatic embryos by promoting normal differentiati
170 , an alkaloid isolated from various pine and spruce species, was then carried out to exploit this ste
171 encoding the rate-limiting enzymes in Norway spruce stilbene and flavonoid biosynthesis were actively
172 and more so for saplings than adults of red spruce, sugar maple, yellow birch, cordate birch, and st
173 tely affected the most rapidly growing white spruce, suggesting that, under recent climate warming, d
176 nds and their role in enhanced resistance of spruce to infection by needle bladder rust are unknown.
177 climate and land use, and the return of red spruce to lower elevations where past logging originally
180 C responses to temperature reveal that black spruce trees are experiencing moisture stress on both no
182 We tested our system on black and white spruce, two paleoclimatically significant taxa in the No
183 ponded similarly to the 1976 drought, Norway spruce was least resistant and resilient to the 2003 sum
186 ypes of wood logs, namely, beech, birch, and spruce, were chemically characterized using thermal deso
187 Cultivating these species instead of Norway spruce will contribute to maintaining a high level of pr
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