ライフサイエンスコーパス: deciduous

1 erbaceous, annual, perennial, evergreen, and deciduous).

2 rgreen) to low-LMA/short-lived leaves (i.e., deciduous).

3 Ra)(0) ~ 0.3, but in several instances, both deciduous and coniferous tree species show a preference

4 where it infests and damages a wide range of deciduous and coniferous tree species, including orchard

5 mycorrhizal species that associate with both deciduous and coniferous trees is delayed in deciduous,

6 he accumulation of both (7)Be and (210)Pb in deciduous and coniferous vegetation is predicted by a mo

7 th response function and parameter range for deciduous and evergreen conifers.

8 anscript was seasonally expressed in sibling deciduous and evergreen genotypes of peach, and also ind

9 Deciduous and evergreen oaks showed fundamental leaf mor

10 pecies native climates and phylogeny, across deciduous and evergreen species.

11 S and CO(2) in 22 plant species representing deciduous and evergreen trees, grasses, and shrubs, unde

12 ous), early Eocene (humid subtropical, mixed deciduous and evergreen), and middle Eocene (seasonally

13 from standardized breeding bird censuses in deciduous and mixed forests of eastern North America.

14 re more common in transitional areas between deciduous and mixed-wood forests, and at lower elevation

15 duous, broad-leaved evergreen, needle-leaved deciduous and needle-leaved evergreen.

16 Both the deciduous and permanent dentitions are affected, resulti

17 ith the number of affected surfaces for both deciduous and permanent teeth in all age groups, even af

18 rate metaregressions for untreated caries in deciduous and permanent teeth, respectively, using model

19 ogressive periodontitis resulting in loss of deciduous and permanent teeth.

20 At the northern mid-/high-latitude broadleaf deciduous and the needleleaf evergreen tree sites, the c

21 e Eocene (seasonally dry, subtropical, mixed deciduous and thick-leaved evergreen).

22 Forests (evergreen and deciduous) and wetlands are by far the dominant land cov

23 and ecosystem type (arid shrubs, coniferous, deciduous, and mixed forests, grasslands, and tundra sed

24 s in tundra, grassland, and boreal, conifer, deciduous, and tropical forest biomes using the LIDET-pr

25 and in a larger comparison of evergreen vs. deciduous angiosperms, high LMA resulted principally fro

26 and strongest in the wet tropics and within deciduous angiosperms.

27 t ecosystem C loss in one of four sites with deciduous B. pubescens stands; no net gain in ecosystem

28 -Later Life Health Study (SLBT), who donated deciduous (baby) teeth in childhood during the 1950s thr

29 mperature strongly regulated the SGS of both deciduous broad-leaf and coniferous forests, whereas the

30 ing four functional types: i.e. broad-leaved deciduous, broad-leaved evergreen, needle-leaved deciduo

31 spring leaf emergence across five different deciduous broadleaf forest types in the eastern United S

32 isms with a unique example from a temperate, deciduous broadleaf forest.

33 odel grid cells over the Northern Hemisphere deciduous broadleaf forests (5.5 million km(2) ), we fou

34 osition affects the phenological response of deciduous broadleaf forests to climate forcing at spatia

35 h eddy-covariance observations of GPP in two deciduous broadleaf forests with low SSWS: the Missouri

36 era site to calibrate a single model for all deciduous broadleaf forests.

37 water availability for the 20 most dominant deciduous broadleaf tree species across the eastern and

38 advanced to being delayed, in the temperate deciduous broadleaved forests across the Northern Hemisp

39 (OR, 1.4; 95% CI, 1.1-1.8) tooth surfaces in deciduous but not in permanent teeth.

40 deciduous and coniferous trees is delayed in deciduous, but not in coniferous, forests.

41 rowing of the internal nasal fossa, retained deciduous canine, clefts of the first cervical vertebra,

42 antity of carbon lost annually by shedding a deciduous canopy is significantly greater than that lost

43 antly by wind speed and the formation of the deciduous canopy.

44 We find a consistent increase in dry forest, deciduous, canopy species with intermediate light demand

45 But the evolutionary significance of their deciduous character has remained a matter of conjecture

46 Trifoliate orange (Poncirus trifoliata), a deciduous close relative of evergreen Citrus, has import

47 pe (conifer needle, deciduous simple leaf or deciduous compound leaf) and canopy height variability,

48 ights in all plots except those dominated by deciduous compound-leaved trees where lidar underestimat

49 een conifer) and tamarack (Larix laricina, a deciduous conifer) were grown under ambient (407 ppm) or

50 rmation regarding the molecular signature of deciduous (DecPDL) and permanent (PermPDL) PDL tissues.

51 mals have two sets of teeth (diphyodont) - a deciduous dentition replaced by a permanent dentition; h

52 vey data from two populations of the drought-deciduous desert shrub Encelia farinosa to provide insig

53 es), as well as leaf phenology (evergreen or deciduous), diameter of hydraulic conduits (that is, xyl

54 Predicted shifts from spruce- to deciduous-dominated stands will interact with the relati

55 warm temperate to subtropical, predominantly deciduous), early Eocene (humid subtropical, mixed decid

56 A largely deciduous ecosystem has been suggested as a possible lan

57 ntially larger than is currently assumed for deciduous ecosystems.

58 was collected from Ramfjord teeth (or their deciduous equivalent).

59 ically distant tree species of the same age, deciduous European beech (Fagus sylvatica) and coniferou

60 To better understand how the brevi-deciduous (experiencing a short, drought-induced leaf fa

61 ovariance records collected above a hardwood deciduous forest (HW) and a pine plantation (PP) co-loca

62 +/- 3.0% relative to 1984) and increases in Deciduous Forest area (+14.8 +/- 5.2%) in the Boreal bio

63 hlorophyll fluorescence (SIF) in a temperate deciduous forest at Harvard Forest, Massachusetts, USA.

64 alone enhanced noontime photosynthesis of a deciduous forest by 23% in 1992 and 8% in 1993 under clo

65 al factors on the timing of fall dormancy of deciduous forest communities in New England, United Stat

66 n increase in a recently harvested temperate deciduous forest community in central Pennsylvania, USA,

67 id regional increase in the ratio of pine to deciduous forest ecosystems at the same time it is exper

68 ract to affect autumn phenology in temperate deciduous forest ecosystems, and points the way to build

69 ns of carbon and water exchange in temperate deciduous forest ecosystems.

70 luxes at high frequency in a temperate mixed deciduous forest for 15 months using a tower-based flux-

71 important habitat type in both seasons, with deciduous forest fragments embedded in broadly deforeste

72 ergreen Forest Gain and substantial areas of Deciduous Forest Gain.

73 ia and North and South America, the Caatinga deciduous forest in eastern South America, and eastern a

74 rge, long-term (7-y) soil-warming study in a deciduous forest in New England.

75 on measurements in a coniferous forest and a deciduous forest in northeastern USA, along with flux pa

76 e-ring records for 12 species in a broadleaf deciduous forest in Virginia (USA) to test hypotheses fo

77 Deciduous forest is the most important habitat type in b

78 egime, sufficiently similar that the generic deciduous forest model based on repeat digital photograp

79 g with two case studies: wood phenology in a deciduous forest of the northeastern USA and leaf phenol

80 hesis and daytime respiration in a temperate deciduous forest over a three-year period.

81 ole Northern Hemisphere boreal and temperate deciduous forest region for the revised model, whereas t

82 Across the deciduous forest region, water stress induced similar de

83 nutrient conditions played a greater role in deciduous forest RUEs than evergreen forest RUEs.

84 Enrichment (FACE) within a mature broadleaf deciduous forest situated in the United Kingdom.

85 able states in the presence of evergreen and deciduous forest types.

86 genera found in Eastern North American (ENA) deciduous forest understories, where growth is constrain

87 f a diverse suite of 11 plant species in the deciduous forest understory (Duke Forest, North Carolina

88 Here we present data from a deciduous forest vertebrate, the eastern chipmunk (Tamia

89 nges from 0.99 mg m(-2) in the low elevation deciduous forest zone to 7.6 mg m(-2) in the higher elev

90 niferous forest) and 25.1 +/- 2.4 mug m(-2) (deciduous forest) dominating mercury inputs (62 and 76%

91 s (marine plankton, intertidal mollusks, and deciduous forest), and recover hidden linearity embedded

92 This model, parameterised for a deciduous forest, demonstrates that anthropogenic nutrie

93 Even so, specific land cover types, such as deciduous forest, influenced ant and pest diversity more

94 eastern North America, including the eastern deciduous forest, remains largely hidden.

95 census data of a diverse temperate broadleaf deciduous forest, seeking to resolve whether ANPP(stem)

96 The consequent view of temperate deciduous forests (an important CO2 sink) is that, first

97 ocal soils by planting a widespread grass of deciduous forests (Milium effusum) into an experimental

98 and P availability were manipulated in mixed deciduous forests across eastern Ohio, USA.

99 toward earlier advancement are predicted for deciduous forests across the whole Northern Hemisphere b

100 The distribution of evergreen and deciduous forests agreed reasonably well with the median

101 The estimated sink is located mainly in the deciduous forests along the East Coast (32%) and the bor

102 forests, suggesting that over the long-term deciduous forests are more efficient in using photosynth

103 Strategies of herbaceous species in deciduous forests are often characterized by the timing

104 erved successional dynamics of evergreen and deciduous forests at three sites spanning the temperate

105 has the potential to decrease the C sink of deciduous forests by up to 17% (0.04 Pg C yr(-1) ) in th

106 Deciduous forests covered the ice-free polar regions 280

107 Fossils demonstrate that deciduous forests covered the polar regions for much of

108 tions in LMBE while percent land coverage by deciduous forests did not.

109 non-native shrub and liana species common to deciduous forests in the eastern United States, I show t

110 Deciduous forests in two eco-regions showed contrasting,

111 Importantly, CUE of deciduous forests is typically 15% higher than that of e

112 Many understorey wildflowers in deciduous forests leaf out and flower in the spring when

113 hree dominant broadleaf species in temperate deciduous forests of New England.

114 gene arrangements in most of its range, the deciduous forests of North America east of the Rocky Mou

115 ong 76 native and non-native woody plants of deciduous forests of North America, invaders express a u

116 stern rainforests are separated from the dry deciduous forests of the west by a large expanse of pres

117 Surprisingly, invaders of deciduous forests show the same small-genome tendencies

118 antly, soil nitrogen (N) increased in mature deciduous forests through time but decreased in older ev

119 25 nonnative species that occur in temperate deciduous forests throughout the Eastern USA.

120 deposition, land coverage by coniferous and deciduous forests, and average Hg concentrations in larg

121 er accumulation following agriculture and in deciduous forests, and continued to accumulate at a slow

122 dominant woodland seed dispersers in eastern deciduous forests, and that their thermal tolerances dri

123 leaf phenology of 54 species of eastern USA deciduous forests, including native and invasive shrubs

124 The phenology of growth in temperate deciduous forests, including the timing of leaf emergenc

125 mmencement of CO(2) uptake(1,3) in temperate deciduous forests, resulting in a tendency towards incre

126 ecrease in NEP, which mostly occurred in the deciduous forests, was mostly driven by the reduction in

127 be affected is the competition for light in deciduous forests, where early vernal species have a nar

128 -stress tended to induce earlier dormancy of deciduous forests, whereas moderate heat- and drought-st

129 in conifer forests but a negative impact in deciduous forests.

130 y linked to ecosystem processes in temperate deciduous forests.

131 predictions of autumn phenology in temperate deciduous forests.

132 wing season length in northern croplands and deciduous forests.

133 s continuously increased with age for mature deciduous forests.

134 thropogenic-derived, degraded descendants of deciduous forests.

135 ses in a critical detritus-based food web of deciduous forests.

136 inties in tropical forests and evergreen and deciduous forests.

137 In addition, the deciduous fourth premolars and permanent first and secon

138 evolution of disease management programs for deciduous fruit trees in the United States over the past

139 agged behind and declined sooner than in the deciduous genotype.

140 The evergreen and deciduous genotypes differ significantly in both their a

141 The rest of the "deciduous" germ cells are lost, most likely by apoptosis

142 Their deciduous habit is frequently interpreted as an adaptati

143 chanisms controlling fire-induced changes in deciduous hardwood cover are similar among different bor

144 The likely fire-induced shift toward greater deciduous hardwood cover may affect climate-vegetation f

145 vel and covered three distinct forest types: deciduous/hardwood forest (14.1 mug/m2-yr), spruce/fir f

146 onal pathways, representing the dominance of deciduous hardwoods vs. evergreen conifers at different

147 minance of conifers and greater abundance of deciduous hardwoods, with potential biogeochemical and b

148 alence of successional pathways dominated by deciduous hardwoods.

149 Data from the temperate, predominantly deciduous Hubbard Brook Experimental Forest (HBEF) in Ne

150 The upper deciduous incisor from Grotta di Fumane contains ancient

151 The lower deciduous incisor from Riparo Bombrini is modern human,

152 r/ (86)Sr intra-tooth variability of a human deciduous incisor from the Middle Pleistocene layers of

153 In general, healthy deciduous incisors displayed a higher degree of crystal

154 ter; umbilical cord blood at birth; and shed deciduous incisors when the child was approximately 7 ye

155 indicated that winter carbon losses through deciduous leaf abscission and respiration were recovered

156 ture gradients and between the evergreen and deciduous leaf habits.

157 piders accelerated the disappearance rate of deciduous leaf litter under low rainfall, but had no, or

158 more frequently in temperate regions and in deciduous lineages; this pattern is concordant with a la

159 -air CO(2) enrichment (FACE) experiment in a deciduous Liquidambar styraciflua (sweetgum) forest stan

160 nology and temporal growth patterns of three deciduous Mediterranean species: almond (Prunus dulcis (

161 on-loss hypothesis as an explanation for the deciduous nature of polar forests.

162 Deciduous needle leaf forest had the longest residence t

163 The longest tauE in deciduous needle leaf forest was ascribed to its longest

164 increasing for evergreen and decreasing for deciduous oaks with elevation.

165 ty, the dominant leaf strategy may be either deciduous or evergreen depending on the initial conditio

166 The basal one-third of the axes bore deciduous organs of uncertain affinities.

167 iven that summer warming may further benefit deciduous over evergreen shrubs, event and trend climate

168 tinct herbivory syndromes: one for taxa with deciduous, palatable foliage, and the other for hosts wi

169 indicates that the greater expense of being deciduous persists in mature forests, even up to latitud

170 izes for all lower primary postcanine teeth (deciduous premolars and permanent molars) in hominins.

171 evertheless, our results reveal how planting deciduous riparian trees along temperate headwaters as a

172 ed methodology to study evergreen (EF), semi-deciduous (SDF), dry forests (DF) and woody savanna (WS)

173 Contrastingly, the temperate centred deciduous section, Yulania, showed high rates of hydraul

174 Associated fascicles of needle leaves with deciduous sheaths and bulbous bases are recognized as Pi

175 NEE model to estimate the impact of greater deciduous shrub abundance and associated shifts in both

176 These results suggest that greater deciduous shrub abundance increases carbon uptake not on

177 im was to determine the influence of greater deciduous shrub abundance on tundra canopy phenology and

178 longer peak season and greater leaf area of deciduous shrub canopies almost tripled the modeled net

179 We found that deciduous shrub canopies reached the onset of peak green

180 ost tripled the modeled net carbon uptake of deciduous shrub communities compared to evergreen/gramin

181 one resulted in 84% greater carbon uptake in deciduous shrub communities.

182 To understand how increasing deciduous shrub dominance may alter breeding songbird ha

183 vegetation and an expansion of the range of deciduous shrub species.

184 rom birch forest (Betula pubescens), through deciduous shrub tundra (Betula nana) to tundra heaths (E

185 uctivity tundra heath to higher-productivity deciduous shrub vegetation in the sub-Arctic may lead to

186 athway (C3 vs. C4 ), or growth form (drought-deciduous shrub vs. evergreen shrub vs. grass).

187 ip between climate and growth for a dominant deciduous shrub, Salix pulchra, on the North Slope of Al

188 We compared deciduous shrub-dominated and evergreen/graminoid-domina

189 tetragona, and Vaccinium vitis-idaea); (iii) deciduous shrubs (Betula nana and Salix pulchra); and (i

190 tal community biomass by promoting growth of deciduous shrubs (dwarf birch and gray willow).

191 ions including the expansion of conifers and deciduous shrubs (shrubs).

192 erall, warming increased height and cover of deciduous shrubs and graminoids, decreased cover of moss

193 Concurrently, deciduous shrubs are becoming increasingly abundant in t

194 Evidence suggests that deciduous shrubs are increasing in abundance, but the im

195 The circumpolar expansion of woody deciduous shrubs in arctic tundra alters key ecosystem p

196 resulted in shrub expansion, mainly of erect deciduous shrubs in the Low Arctic, but the more extreme

197 The expansion of deciduous shrubs onto potentially vulnerable arctic soil

198 Deciduous shrubs that were previously exposed to an extr

199 es (dwarf birch shrubs, willow shrubs, other deciduous shrubs, grasses, sedges, and forbs) in arctic

200 e ways, including via increased dominance of deciduous shrubs.

201 advantage relative to phenotypically plastic deciduous shrubs.

202 and slightly reduced the cover of C3 drought-deciduous shrubs.

203 fluenced by vegetation type (conifer needle, deciduous simple leaf or deciduous compound leaf) and ca

204 drier tropical forests have increased their deciduous species abundance and generally changed more f

205 on effects, primarily driven by fast-growing deciduous species and associated traits.

206 Deciduous species from shorter growing seasons tended to

207 However, drought-deciduous species showed high Psi(TLP) and Psi(P50) valu

208 Deciduous species showed marked variability in freezing

209 he ancestral Meliaceae is reconstructed as a deciduous species that inhabited seasonal habitats.

210 f trait datasets, we show that evergreen and deciduous species with diverse construction costs (assum

211 n forests formerly dominated by broad-leaved deciduous species).

212 Deciduous species, and evergreen species from xeric clim

213 ated acceptable vulnerability curves for the deciduous species, but overestimated drought resistance

214 Annual growth rates were constrained in all deciduous species, but those that evolved in warm latitu

215 Across nine deciduous species, we find that hydraulic resistance in

216 ially higher leaf mass fractions (LMFs) than deciduous species, whereas graminoids maintained higher

217 density in evergreens but reduced density in deciduous species.

218 ially outperformed the standard CLM seasonal-deciduous spring phenology submodel at both coarse (0.9

219 (15) N-NO3- tracer over 5-6 years in a mixed deciduous stand that was evenly composed of trees with e

220 and tannins significantly decreased for the deciduous stand WEOM.

221 DOC reductions reached 32% when deciduous stands dominated.

222 e results suggest that the standard seasonal-deciduous submodel in CLM should be reconsidered, otherw

223 hly divergent physiological strategies, with deciduous swamp-adapted genera-like Taxodium at one extr

224 m minirhizotron analysis of a closed-canopy, deciduous sweetgum forest in a free-air CO(2) enrichment

225 Stem cells from human exfoliated deciduous teeth (SHED) are a unique postnatal stem cell

226 Stem cells from exfoliated deciduous teeth (SHED) exposed to endothelial growth med

227 fected into stem cells from human exfoliated deciduous teeth (SHED) for evaluation of gene/protein fu

228 Stem cells from exfoliated deciduous teeth (SHED) possess multipotent differentiati

229 em cells (DPSCs), stem cells from exfoliated deciduous teeth (SHED), periodontal ligament stem cells

230 stem cells [stem cells from human exfoliated deciduous teeth (SHED)].

231 ns in the Sr isotope composition of 14 human deciduous teeth and the N and C stable isotope ratios of

232 Deciduous teeth can reveal historical exposure to metals

233 dy coined the "Truth Fairy" Project, 50 shed deciduous teeth from 43 children living their entire liv

234 Measuring Pb and As in shed deciduous teeth is a promising technique to assess prena

235 ed more than 150 enamel microsamples from 51 deciduous teeth of 12 different modern human individuals

236 2.4 billion people, and untreated caries in deciduous teeth was the 10th-most prevalent condition, a

237 he cilia of stem cells from human exfoliated deciduous teeth with key FOP signaling components, inclu

238 , and SHED (stem cells from human-exfoliated deciduous teeth) cells produce a more highly mineralized

239 al dental eruption, early replacement of the deciduous teeth, high dental endowment at weaning, and r

240 teeth) and stem cells from human exfoliated deciduous teeth, possess unique properties based on thei

241 For dental caries in deciduous teeth, the adjusted OR was 1.8 (95% CI, 1.2-2.

242 the neonatal line, a histological feature in deciduous teeth, to identify regions of mantle dentine f

243 ross thin sections of enamel from exfoliated deciduous teeth.

244 al/isotopic analyses and histomorphometry of deciduous teeth.

245 potential dental pulp capping materials for deciduous teeth.

246 7 and 2020, the women provided their child's deciduous teeth.

247 d premolar in maxilla, as well as persistent deciduous teeth: right second molar, left canine and sec

248 We studied C dynamics of a deciduous temperate forest of Hungary that has been subj

249 hanced deposition across the transition from deciduous to coniferous forest.

250 ent sites in tropical forests, including dry deciduous to wet evergreen forest on two continents.

251 In this study we found that exfoliated human deciduous tooth contains multipotent stem cells [stem ce

252 fe dietary transitions are recorded in human deciduous tooth enamel as marked variations in Ca isotop

253 ic composition of enamel of the most ancient deciduous tooth ever discovered in Italy to assess human

254 er-child pairs provided blood, urine, and/or deciduous tooth samples.

255 have been isolated from the dental pulp, the deciduous tooth, and the periodontium.

256 ic composition determination in such ancient deciduous tooth.

257 By 2100, boreal deciduous tree area is expected to increase by 1-15%, po

258 Root architecture differs between the four deciduous tree seedlings.

259 on genetics and evolutionary history of this deciduous tree species across its distributed range.

260 Current distributions of evergreen and deciduous tree species across local and regional moistur

261 %) in the canopies of eight northeastern USA deciduous tree species during two consecutive years and

262 sis (Topt ) of two boreal and four temperate deciduous tree species grown in the field in northern Mi

263 e-driven patterns of growth for six dominant deciduous tree species in the southern Appalachians.

264 American chestnut (Castanea dentata) is a deciduous tree species of eastern North America that was

265 0 nm to 20 um) of leaves from five temperate deciduous tree species over the 8 wk following spring le

266 Many deciduous tree species require chilling for dormancy rel

267 angiosperms and gymnosperms or evergreen and deciduous tree species.

268 This study is the first to show that deciduous tree water uptake of snowmelt water represents

269 centron sinense is an endemic and endangered deciduous tree.

270 straints on the productivity of broad-leaved deciduous trees and highlight that shifting spring pheno

271 ent plant functional types (evergreen trees, deciduous trees and lawn) and (ii) different ages (const

272 es in the late twentieth century resulted in deciduous trees and mosses increasing production at the

273 red carbon losses through leaf abscission of deciduous trees are significantly greater than losses th

274 e light-capturing capability, of overtopping deciduous trees by intrusive growth from below a palm.

275 of SOA formation from direct VOC emission of deciduous trees damaged by known defoliating herbivores

276 ethyl-1,3-butadiene (isoprene) is emitted by deciduous trees each year.

277 temperatures shifted stem diameter growth of deciduous trees earlier but had no consistent effect on

278 Deciduous trees exhibit a spectacular phenomenon of autu

279 n plant pigment chlorophyll in the leaves of deciduous trees has long been a fascinating biological p

280 aracterized by relatively open formations of deciduous trees in C(4)-grass dominated understories, ar

281 n the distribution patterns of evergreen and deciduous trees in the temperate and boreal zones based

282 osphere to investigate the effects of adding deciduous trees on bare ground at high northern latitude

283 carbon sequestration and favors broad-leaved deciduous trees over conifers.

284 Deciduous trees reached saturation between snowmelt and

285 We found that deciduous trees removed 17.8-20.9 billion m(3) of snowme

286 ow the iWUE and growth of several species of deciduous trees that span a gradient of isohydric to ani

287 Deciduous trees transpired 2-12% (0.4-2.2 billion m(3))

288 ant harvests of mature and juvenile tropical deciduous trees, evergreen trees, and lianas and model s

289 to control autumn color change in temperate deciduous trees, it is possible that climate change migh

290 ots with coniferous trees than in those with deciduous trees.

291 ing, but severe fires favored less-flammable deciduous vegetation, such that fire frequency remained

292 luence of plant nitrogen fixation ability or deciduous vs. evergreen leaf habit.

293 theless, streams draining the most extensive deciduous woodland had the greatest stocks of coarse par

294 the summer of 2018 in Wytham Woods, a mixed deciduous woodland in southern England.

295 forest in Brazil; BIFoR-FACE in a 150-yr-old deciduous woodland stand in central England; and SwedFAC

296 ons showed that macroinvertebrate biomass in deciduous woodland streams was around twice that in moor

297 By contrast, most deciduous woody lineages had an evolutionary shift to se

298 This could explain why temperate deciduous woody plants exhibit considerable variation in

299 Warming advanced budburst of six deciduous woody species by 5-15 days and delayed leaf co

300 ) and anthocyanin-deficient mutants of three deciduous woody species, Cornus sericea, Vaccinium ellio