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1 ut had contrasting vegetation cover (moss vs shrub).
2 lly depleted of the ESCRT-III core component Shrub.
3 to systems dominated by broadleaf trees and shrubs.
4 ss of future dendroclimatological studies on shrubs.
5 dingoes relaxed a recruitment bottleneck for shrubs.
6 wo treatments: trenched plots and plots with shrubs.
7 pex predator to the historic encroachment of shrubs.
8 ted a 78% increase in the height of riparian shrubs.
9 on the elevational limits of trees than tall shrubs.
10 soil layers that are exclusively explored by shrubs.
11 states dominated by water spending invasive shrubs.
12 getation is typically dominated by evergreen shrubs.
13 cluding via increased dominance of deciduous shrubs.
14 relative to phenotypically plastic deciduous shrubs.
15 ommunities that are dominated by resprouting shrubs.
16 mate on trees, this is not possible for most shrubs.
17 rganic C (SOCorg ) is significantly lower at shrub (2.98 +/- 0.48 kg m(-2) ) and forest (2.04 +/- 0.2
18 ianas (50.1 +/- 16.3%), angiosperm trees and shrubs (26.3 +/- 12.4%), and conifers (7.6 +/- 2.6%).
21 to estimate the impact of greater deciduous shrub abundance and associated shifts in both leaf area
22 determine the influence of greater deciduous shrub abundance on tundra canopy phenology and subsequen
25 e velocity better than either forest or tall shrub alone, suggesting competitive compensation can be
28 Our model estimates suggest that fires in shrub and fern understories had significantly greater fi
29 In addition, density of poultry, coverage of shrub and temperature played important roles for human H
31 ontrasting root distributions of grasses and shrubs and competitive interactions among plant types, c
34 guminosae), a clade of 225 species of trees, shrubs and lianas distributed across the Rainforest, Suc
43 l Alaska may be due to competition with tall shrubs and/or more complex climate controls on the eleva
44 ss was positively correlated with graminoid, shrub, and ecosystem productivity measured at field site
45 Elaeagnus umbellata is a common invasive shrub, and similar impacts on native species might occur
53 al measurements to test the framework with a shrub (Artemisia tridentata) and a tree (Pinus monophyll
55 en biomes (relative percentages of trees vs. shrubs) at the same vegetative density shows a non-linea
56 ouse experiments using the California-native shrub Baccharis salicifolia and two ecologically distinc
59 ed ecosystems can fuel a surprising burst in shrub belowground productivity, one possible mechanism e
60 and Vaccinium vitis-idaea); (iii) deciduous shrubs (Betula nana and Salix pulchra); and (iv) forbs (
61 eas White-crowned sparrows nested only under shrubs between 20 cm and 1 m in height, with no preferen
62 esent novel dendroecology-based estimates of shrub biomass change under a future climate regime, made
65 sitively correlated with (15) N recovered in shrub biomass Taxon-specific RAF associations could be a
66 in carbon (C) contained within above-ground shrub biomass, it is modest in comparison with the amoun
68 ly greater for exclosures dominated by dwarf shrubs (Calluna vulgaris) than by grasses (Molinia caeru
70 ak season and greater leaf area of deciduous shrub canopies almost tripled the modeled net carbon upt
74 nd that high N availability increased native shrub canopy loss and mortality, likely due to the highe
75 of growth variability of the evergreen dwarf shrub Cassiope tetragona between 1927 and 2012 in the no
77 on protein Comt/NSF and ESCRT-III components Shrub/CHMP4B and CHMP2B, facilitates reintegration of ac
79 llular glandular trichomes of the xerophytic shrub Cistus creticus that accumulate labdane-type diter
80 s dominated by the water use of the invasive shrub Cistus ladanifer, which further increased after th
82 d the modeled net carbon uptake of deciduous shrub communities compared to evergreen/graminoid commun
85 s suggest that areas of minimal or extensive shrub cover (shrub encroachment) may be homogenizing rod
86 ographs spanning a 51-year period to compare shrub cover between areas where dingoes are historically
88 e decades after fire disturbance, the upland shrub cover increased by 1077.2 +/- 83.6 m(2) ha(-1) , ~
89 ns why in most cases the shift from grass to shrub cover is found to be abrupt and often difficult to
92 gery, we characterize dynamics in forest and shrub cover occurring at relatively short spatial scales
98 re correlated on the moss site but not under shrub cover, where the canopy reduced the influence of u
102 m) aerial and satellite imagery to estimate shrub-cover change in 114 study sites across four burned
104 lands (r = 0.78, p < 0.001), but accelerated shrub-cover losses in burned lowlands (r = -0.82, p < 0.
105 hese results highlight divergent pathways of shrub-cover responses to fire disturbance and climate ch
106 orted the most rapid fire spread, angiosperm shrubs delivered the largest amount of heat per unit are
110 ced by management intensity, and postdrought shrub dominance was higher when pathogens acted as codri
115 ur system, particularly ornamental trees and shrubs (e.g. Hydrangea, Rosa, Spiraea, Syringa, Viburnum
116 eads to non-uniform sampling protocols among shrub ecologists, who will favor either root collars or
118 change, likely driven by the invasion of the shrub, Elaeagnus umbellata, on the nest distribution pat
119 populations of the drought-deciduous desert shrub Encelia farinosa to provide insight into water-use
120 For a recent radiation of New World desert shrubs (Encelia: Asteraceae), we use fine-scale geograph
121 sure, plays a significant role in modulating shrub encroachment and ensuing land degradation processe
122 nce modification and elucidate mechanisms of shrub encroachment at the Virginia Coast Reserve, Long-T
123 he hypothesis that dingo removal facilitates shrub encroachment by triggering a four level trophic ca
125 he dingo (Canis dingo), could be a driver of shrub encroachment in the Strzelecki Desert, Australia.
126 climate change that might lead to widespread shrub encroachment reducing the provisioning of ecosyste
128 t areas of minimal or extensive shrub cover (shrub encroachment) may be homogenizing rodents' percept
135 may further benefit deciduous over evergreen shrubs, event and trend climate change may both act agai
137 a feedback can affect the maximum extent of shrub expansion and the configuration of a stable encroa
141 = 0.67, p < 0.001), responsible for 30.8% of shrub expansion in the upland tundra between 1971 and 20
144 ions, changes in microclimate resulting from shrub expansion into desert grasslands have remained poo
146 ver, landscape-scale patterns and drivers of shrub expansion remain poorly understood, inhibiting acc
147 rctic is leading to widespread heterogeneous shrub expansion, but impacts of these habitat changes on
149 n observed in arctic tundra ecosystems, e.g. shrub expansion, resulting in reduction in albedo and gr
150 RP binds shrub mRNA (human Chmp4) to repress Shrub expression, causing overexpression during the dise
156 tested the hypothesis that the mechanism of shrub facilitation on an annual plant community can chan
157 ear of treatment, the control (+0 degrees C) shrub fine-root growth of 0.9 km m(-2) y(-1) increased l
158 cated elevational movements by two tree- and shrub-foraging species with moderate-to-high vagility (C
159 The geographic distribution of tree versus shrub form of species appears to be the result of 4-5 in
164 e rhamnoides ssp. turkestanica) is an alpine shrub growing wild in certain parts of western Himalaya.
165 rost, contrasting earlier notions of limited shrub growth sensitivity to summer warming in the High A
168 nal downscaling to map current and projected shrub habitat for moose on the North Slope of Alaska.
169 ores in the Arctic in response to increasing shrub habitat is a contrasting terrestrial counterpart t
171 rthern Alaska as a case study to examine how shrub habitat will respond to predicted future warming,
175 on dendrochronological techniques applied to shrubs have linked this phenomenon to climate change.
176 s carried out in widespread sub-Arctic dwarf shrub heathland, incorporating both mortality and stress
177 harge and the estimated increase in riparian shrub height are consistent with observed riparian shrub
178 ound in sedge-dominated tussock tundra where shrub height does not exceed 20 cm, whereas White-crowne
180 that snowshoe hares require a mean riparian shrub height of at least 1.24-1.36 m, a threshold which
181 etween cumulative summer warmth and riparian shrub height to reconstruct annual changes in shrub heig
182 n soil moisture and temperature, thaw depth, shrub height, and foliar nitrogen content, indicating th
183 cots, and eudicots) and growth habits (tree, shrub, herbaceous, annual, perennial, evergreen, and dec
184 he establishment of snowshoe hares and other shrub herbivores in the Arctic in response to increasing
185 connectivity and alter the distributions of shrub herbivores in the Arctic, including creation of no
186 A large proportion of dryland trees and shrubs (hereafter referred to collectively as trees) gro
187 rack the fate of seedlings of an encroaching shrub, hopbush (Dodonaea viscosa angustissima), during a
191 The circumpolar expansion of woody deciduous shrubs in arctic tundra alters key ecosystem properties
194 The rapid growth increase in C. tetragona shrubs in response to recent High Arctic summer warming
195 n shrub expansion, mainly of erect deciduous shrubs in the Low Arctic, but the more extreme, sparsely
196 k with microclimate, whereby cold intolerant shrubs increase the minimum nocturnal temperatures in th
197 orate the critically important role of nurse shrub interactions for ameliorating population bottlenec
198 Mediterranean woodland, we show that native shrub invasion and extreme drought synergistically reduc
201 d use, and climate-driven expansion of woody shrubs, is transforming the distribution of plant functi
202 IC and pedogenic carbonate (PIC); converting shrub land to cropland increased PIC stock by 5.2 kg C m
205 f edge habitat), but decreased with a denser shrub layer, deeper leaf litter and higher humidity (cha
206 ii and Eriophorum vaginatum); (ii) evergreen shrubs (Ledum palustre, Cassiope tetragona, and Vacciniu
209 promote an expansion of this evergreen dwarf shrub, mainly through densification of existing shrub pa
210 However, the multi-stemmed structure of shrubs makes them difficult to sample and therefore lead
211 ate that C, recently fixed by trees and tall shrubs, makes a substantial contribution to soil respira
212 k a 10-year study on the effects of invasive shrub management (bitou bush, Chrysanthemoides monilifer
213 soil surface temperature extremes, trees and shrubs may help to reduce the adverse impacts of urbaniz
214 es are the birds' preferred prey, increasing shrubs may result in a net enhancement in preferred prey
217 acerbated woody encroachment by the invasive shrub Mimosa pigra-considered one of the world's 100 wor
221 phila FXS disease model, we found FMRP binds shrub mRNA (human Chmp4) to repress Shrub expression, ca
228 and carbon (up to 2100 years old) when dwarf-shrubs or graminoids are present, an effect not observed
229 e such as foundation plant species including shrubs or local differences in the physical attributes w
231 arning/memory center, we found FMRP loss and Shrub overexpression similarly increase connectivity.
233 ub, mainly through densification of existing shrub patches, at High Arctic sites with sufficient wint
235 diterpene that is isolated from the tropical shrub Persea indica(1) and has potent antifeedant and in
237 nalysis suggests that, with the exception of shrubs, plants affect FIB removal indirectly by changing
239 esized that N addition would increase native shrub productivity, but that this would increase suscept
244 flooded islands, while salt marsh herbs and shrubs replaced forest understory vegetation along a tid
246 land to assess how a nurse plant, the native shrub Rhodomyrtus tomentosa, affects the growth of the t
247 ized ericoid (ERM) and ectomycorrhizal (ECM) shrub roots and occurred below the maximum rooting depth
249 climate and growth for a dominant deciduous shrub, Salix pulchra, on the North Slope of Alaska, USA.
250 location dataset, a 568 km transect of field shrub sampling, and forecasted warming scenarios with re
251 the invasive range of two non-native lowland shrubs, Scotch broom (Cytisus scoparius) and Spanish bro
252 plex mosaic of fens, collapse-scar bogs, low shrub/scrub, and forests growing on elevated ice-rich pe
253 hen quantify contemporary patterns of shrub, shrub seedling and mammal abundances, and use structural
254 ults in suppressed abundance of consumers of shrub seeds and seedlings, rodents and rabbits respectiv
256 We then quantify contemporary patterns of shrub, shrub seedling and mammal abundances, and use str
258 eeline would be at the expense of meadow and shrub species and radically change this high-mountain ec
259 ly our pipeline to the South African endemic shrub species Berkheya cuneata to use the resulting esti
260 ees, whereas flowering of midstory trees and shrub species continued to increase with rising CO2 .
261 e xeric communities, with replacing tree and shrub species exhibiting drier bioclimatic optima and di
262 an economically important genus of tree and shrub species found in temperate regions of Asia, North
266 f Betula glandulosa, a common North American shrub species, we evaluated the relative sensitivity of
267 wer soil pH post-clearance may have favoured shrub species, which are typically tolerant of acidic so
274 ncreased across the transition from heath to shrub, suggesting that the action of ectomycorrhizal sym
276 erous plant Bupleurum spinosum (Apiaceae), a shrub that grows mainly in the Atlas Moroccan Mountains.
277 otch broom (Cytisus scoparius), a leguminous shrub that has become invasive around the world with con
279 Larrea tridentata, a drought-tolerant desert shrub that withstands a wide range of environmental cond
281 lant community composition from grassland to shrub thicket alters the role of barrier islands in prod
285 s indicate that the feedback allows juvenile shrubs to establish in the grassland during average year
286 pportunity to examine the response of desert shrubs to increasing temperature and water stress in a r
287 at the differential responses of grasses and shrubs to precipitation variability and the amplificatio
288 tion of dwarf birch (Betula, a thermophilous shrub) to 5.9 +/- 0.1 ka, ~3 ka after local deglaciation
289 extinction on islands, in the tropics and of shrubs, trees or species with narrow ranges are least li
290 forest (Betula pubescens), through deciduous shrub tundra (Betula nana) to tundra heaths (Empetrum ni
292 ) climate-driven expansion of Herbaceous and Shrub vegetation (+7.4 +/- 2.0%) in the Arctic biome.
294 undra heath to higher-productivity deciduous shrub vegetation in the sub-Arctic may lead to a loss of
295 the second growing season of treatment, the shrub warming response rate increased to 2.54 km m(-2) d
296 rt small-leaved low-specific leaf area (SLA) shrubs with low K(s) in arid relative to tall large-leav
297 agellanica with cyanobacteria, and trees and shrubs with mycorrhizas, to be the key processes driving
299 ures of bean (annual herb) and cotton (woody shrub) would be globally an order of magnitude higher th