ライフサイエンスコーパス: deciduous

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

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

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

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

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

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

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

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

9 Both the deciduous and permanent dentitions are affected, resulti

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

37 ntially larger than is currently assumed for deciduous ecosystems.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

69 Deciduous forests covered the ice-free polar regions 280

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

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

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

73 Deciduous forests in two eco-regions showed contrasting,

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

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

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

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

78 25 nonnative species that occur in temperate deciduous forests throughout the Eastern USA.

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

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

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

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

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

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

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

86 wing season length in northern croplands and deciduous forests.

87 inties in tropical forests and evergreen and deciduous forests.

88 y linked to ecosystem processes in temperate deciduous forests.

89 predictions of autumn phenology in temperate deciduous forests.

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

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

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

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

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

95 Their deciduous habit is frequently interpreted as an adaptati

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

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

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

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

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

101 alence of successional pathways dominated by deciduous hardwoods.

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

103 The upper deciduous incisor from Grotta di Fumane contains ancient

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

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

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

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

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

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

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

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

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

113 Deciduous needle leaf forest had the longest residence t

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

142 Concurrently, deciduous shrubs are becoming increasingly abundant in t

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

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

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

146 The expansion of deciduous shrubs onto potentially vulnerable arctic soil

147 Deciduous shrubs that were previously exposed to an extr

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

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

150 advantage relative to phenotypically plastic deciduous shrubs.

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

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

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

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

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

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

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

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

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

160 and tannins significantly decreased for the deciduous stand WEOM.

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

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

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

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

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

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

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

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

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

170 2.4 billion people, and untreated caries in deciduous teeth was the 10th-most prevalent condition, a

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

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

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

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

175 ross thin sections of enamel from exfoliated deciduous teeth.

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

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

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

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

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

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

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

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

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

185 ic composition determination in such ancient deciduous tooth.

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

187 Root architecture differs between the four deciduous tree seedlings.

188 %) in the canopies of eight northeastern USA deciduous tree species during two consecutive years and

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

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

191 Many deciduous tree species require chilling for dormancy rel

192 angiosperms and gymnosperms or evergreen and deciduous tree species.

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

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

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

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

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

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

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

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

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

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

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

204 Deciduous trees reached saturation between snowmelt and

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

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

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

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

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

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

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

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

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

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

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