ライフサイエンスコーパス: montane

1 t higher than averages from plot networks in montane(2,5,6) and lowland(7) forests in the Neotropics,

2 m of dragonfly and anuran larvae in tropical montane (242-3,631 m) and habitat (ponds and streams) gr

3 egrees C) compared with birds occupying cool montane (4.97 +/- 0.99 degrees C) or hot arid (4.11 +/-

4 (4) uptake (in kg CH(4)-C ha(-1) yr(-1)) for montane (-4.28) and lowland forests (-3.52) and a massiv

5 hese results shed light on the complexity of montane-adapted insects responding to changing abiotic c

6 al range covering tropical, temperate, arid, montane and coastal environments from 9.25oS to 43.75oS

7 In the lower montane and lowland zones simulated ecosystem productivi

8 er levels of ERalpha-IR in the MeA than male montane and meadow voles and in the BST relative to mont

9 eaf wetting patterns in contrasting tropical montane and pre-montane cloud forests.

10 er uptake differed significantly between the montane and pre-montane forest plant communities, as wel

11 ish consumers in streams spanning grassland, montane and semi-arid ecoregions of the temperate steppe

12 er dominated discharge year-round across the montane and urban sites, challenging the conceptual emph

13 tly low during snowmelt and baseflow in most montane and urban stream reaches, indicating effective s

14 ground biomass in both lowland Amazonian and montane Andean landscapes.

15 s reveal the potential for radical change to montane ant assemblages by the end of the 21st century i

16 d climate, we propose the 'South East Africa Montane Archipelago' (SEAMA) as a distinct ecoregion of

17 ome lineages colonized lowlands and adjacent montane areas, but diversification in those areas remain

18 re present, thereby shaping the structure of montane assemblages.

19 ne regions is important for the formation of montane assemblages.

20 cycling by northern (lowland) and southern (montane) Atlantic Forest species, triggered by the joint

21 The African montane bamboo Yushania alpina provides both habitat and

22 est that successful conservation of tropical montane bee communities and pollination services will re

23 d of extinction and 'evolutionary rescue' in montane biodiversity hot spots under climate change scen

24 ntial to understanding the forces that shape montane biodiversity.

25 across a sharp latitudinal transition in 21 montane birds of the southern Atlantic Forest in Brazil.

26 Montane birds represent a large proportion of global avi

27 an conifer Athrotaxis selaginoides in remote montane catchments in southern Tasmania.

28 osynthesis in canopy species from a tropical montane cloud forest.

29 Epiphytes are common in tropical montane cloud forests (TMCFs) and play many important ec

30 Tropical montane cloud forests (TMCFs) depend on predictable, fre

31 Tropical montane cloud forests (TMCFs) harbour high levels of bio

32 et of "optimal" climatic conditions found in montane cloud forests is similar to that of maritime tem

33 ecognisable and defining feature of tropical montane cloud forests, little research has focussed on h

34 erns in contrasting tropical montane and pre-montane cloud forests.

35 Tropical montane communities host the world's highest beta divers

36 tructure, diversity, and spatial turnover of montane communities in a phylogenetic context.

37 temperature tracking suggests that tropical montane communities may be on an "escalator to extinctio

38 of the area currently capable of supporting montane conifer forest could become subject to minimal c

39 Oregon, where severe fire initially converts montane conifer forests to systems dominated by broadlea

40 ades across the climatic aridity gradient of montane conifer forests.

41 We use pollen records of montane conifers (Tsuga, Podocarpus, Abies, and Picea) a

42 and beetle body temperature (T(b)) in three montane drainages in the Sierra Nevada, California.

43 xploited potential for studying responses of montane ecosystems to temperature and predicting phenolo

44 ing may disrupt the functional properties of montane ecosystems, particularly where plant community r

45 n drive the evolution of nutrient budgets in montane ecosystems, with implications for predicting for

46 as microbial responses to climate change in montane ecosystems.

47 extinctions from climate change in tropical montane ecosystems.

48 have consequences for amphibians inhabiting montane ecosystems.

49 data for communities of grasshoppers along a montane elevation gradient to assess the impact of clima

50 Along a montane elevation gradient, Argentina anserina flowers w

51 d strong FA of low-elevation perennials in a montane environment.

52 explain FA of low-elevation perennials in a montane environment.

53 ayan valleys could mix multiple impacts from montane environments and signals of transboundary transp

54 Montane environments around the globe are biodiversity '

55 climatic zones along elevation gradients in montane environments.

56 d with low-emission scenarios, most tropical montane epiphyte species will survive, but under emissio

57 humid forests of northwest Madagascar and a montane ericoid formation of the central highlands show

58 Nevada, implying that the risk of increasing montane ET with warming is widespread.

59 ects of Triad zoning on biodiversity in (sub)montane eutrophic European beech forests.

60 inued warming has the potential to transform montane fire regimes with numerous implications for ecos

61 explore landform-specific differences among montane floras based on a dataset comprising 17,576 angi

62 eological processes affect the assemblage of montane floras is a matter of ongoing research.

63 , but also contributes to the composition of montane floras.

64 he role of bedrock and landform processes in montane floristic assembly and provides insights for fut

65 lize cassowary hunting and egg harvesting by montane foragers and discuss the implications of human e

66 We provide country-specific montane forest AGC stock estimates modelled from our plo

67 to warming, we project that decadal semiarid montane forest carbon sequestration will remain relative

68 previously considered to primarily use moist montane forest during the winter, but this seems unlikel

69 pread microbial N limitation across tropical montane forest ecosystems and high sensitivity to climat

70 ere we show that dust may also be crucial in montane forest ecosystems, dominating nutrient budgets d

71 the Northern Hemisphere occurs in seasonal, montane forest ecosystems.

72 We developed a method to model and map the montane forest ecotone using Landsat imagery to observe

73 During the dry season, the montane forest experienced higher precipitation, cloud c

74 t 0.8 million hectares of old-growth African montane forest have been lost since 2000.

75 iscrepancy by hypothesizing the expansion of montane forest in the uplands and replacement of rainfor

76 e from Ecuador reveals the response of lower montane forest on the Andean flank in western Amazonia t

77 The pollen records typically show montane forest persistence during the LGM, while delta(1

78 ed significantly between the montane and pre-montane forest plant communities, as well as among speci

79 anda has been restricted to several disjunct montane forest populations, and habitat loss and fragmen

80 aleoecological record from Neotropical lower montane forest reveals a consistent forest presence and

81 food chains of forest birds in a subtropical montane forest using a bird diet recorded by video and s

82 tions of DOM during four years in a tropical montane forest with the help of stable C isotope ratios

83 ive population size estimates in a temperate montane forest, we accurately predict fluctuations acros

84 tting events of longer duration than the pre-montane forest.

85 included primary and secondary-growth lower montane forests (500-1.200 m above sea level) and primar

86 ing compositional changes in Andean tropical montane forests (TMFs).

87 Humid montane forests are challenging environments for human h

88 High-elevation montane forests are disproportionately important to carb

89 ong-standing generalization is that tropical montane forests are nitrogen (N)-limited whereas lowland

90 evation(3), AGC stocks are lower in tropical montane forests compared with lowland forests(2).

91 r, in some cases similar to the most fertile montane forests in the Hawaiian Islands.

92 a(13)C in earlywood of two pine species from montane forests in western North America using tree ring

93 Although montane forests make up 11% of forested tropical land ar

94 n a very remote area, suggests that tropical montane forests may contain greater AGB than previously

95 hytic species distributed in lowland and pre-montane forests of Central and South America.

96 a dioecious neotropical tree common in lower montane forests of Monteverde, Costa Rica.

97 of tree hyrax (Dendrohyrax sp.) in the moist montane forests of Taita Hills, Kenya.

98 fied forest soils and freshwaters throughout montane forests of the northeastern United States; the r

99 Montane forests of western China provide an opportunity

100 frican lowland forests(4) is mirrored in the montane forests sampled.

101 cause shifts in the composition of tropical montane forests towards increased relative abundances of

102 Upper montane forests were predicted to allocate ~50% of carbo

103 poorly understood, in particular in tropical montane forests(2).

104 born in tropical mountains, descend through montane forests, and feed major rivers, floodplains, and

105 Arid ecoregions, tropical montane forests, and islands showed the highest differen

106 In lower montane forests, regardless of land-use history, we foun

107 Within tropical montane forests, the effects of ErM plants could be part

108 In lowland to montane forests, three invasive tree species replace nat

109 arp transition in NPP between submontane and montane forests, which may be caused by cloud immersion

110 ion of fire severity throughout California's montane forests.

111 remnant and restored patches of subtropical montane forests.

112 f widespread shifts in the size-structure of montane forests.

113 tant drivers of atmospheric Hg deposition to montane forests.

114 n disturbance by fire and forest thinning in montane forests.

115 rtia to climatically induced range shifts in montane forests; the upslope shift may have been acceler

116 kely to promote population viability in this montane frog population.

117 e than 16,500 terrestrial vertebrates on 180 montane gradients.

118 Reconstruction of the distribution of a montane grasshopper species during the last glacial maxi

119 Leveraging long-term data for six montane grasshopper species spanning 1,768-3 901 m, we d

120 n a replicated field experiment where entire montane grassland communities were transplanted in the d

121 Here, we estimate microbial growth rates in montane grassland soils exposed to ambient conditions, d

122 sets, and tropical grasslands, mangroves and montane grasslands also have <1% of land identified as v

123 are comprised of cold (e.g., boreal forests, montane grasslands and tundra) or arid (e.g., deserts) l

124 km yr(-1)), temperate coniferous forest, and montane grasslands.

125 thern Africa, as well as biologically unique montane grasslands.

126 Range expansion into montane habitats and the subsequent development of innov

127 gration and sorting of clades pre-adapted to montane habitats is the primary mechanism shaping tree c

128 have repeatedly and independently adapted to montane habitats on either side of the Andes.

129 ent for completely volant taxa to persist in montane habitats.

130 a trend towards LA among populations within montane habitats.

131 enetic structure of populations of an arctic-montane herb, Saxifraga hirculus (Saxifragaceae), was an

132 elative contributions of these mechanisms to montane invasion resistance, yet such experiments are ra

133 the importance of these factors in limiting montane invasions using a field transplant experiment ab

134 Interpretation of tropical-montane isotope records is controversial, especially con

135 ng aquatic environments stretching from high montane lakes down to the deep ocean.

136 -y period (1949/1951-2007/2009) in a complex montane landscape (the Siskiyou Mountains, Oregon) where

137 Montane landscapes may effectively shelter many species

138 We tested this hypothesis in a montane lizard.

139 3.5, and -0.19 kg N(2)O-N ha(-1) yr(-1) for montane, lowland, non-inundated swamp, and inundated swa

140 and meadow voles and in the BST relative to montane males.

141 ldflower plantings in the Central Valley and montane meadows in the Sierra.

142 es and longer fire-return intervals in these montane mesic systems suggest these changes are largely

143 three species of microtines, the polygynous montane (Microtus montanus) and meadow (M. pennsylvanicu

144 er on migratory routes than summer ranges of montane-migrant tactics, but wolf predation risk traded-

145 population abundance, where abundance of the montane-migratory tactics declined over time.

146 s and nonvascular epiphytes in a subtropical montane moist forest in southwest China.

147 hese patterns are explained by greater time (montane museum) rather than faster speciation at mid-ele

148 n leopard Panthera pardus saxicolor in three montane national parks, northeastern Iran.

149 forest hunter-gatherers managed resources in montane New Guinea and present some of the earliest docu

150 utterflies overwinter in restricted areas in montane oyamel fir forests in central Mexico with specif

151 tic Hawaiian group to two diploid species of montane perennial herbs in California, Madia bolanderi a

152 The altitudinal shifts of many montane populations are lagging behind climate change.

153 nces among PGI genotypes, which suggest that montane populations of this beetle are locally adapted t

154 temperate zone, evolving in situ, or through montane preadaptation.

155 emistry of forest canopies across a Hawaiian montane rain forest landscape.

156 During expeditions to a montane rainforest in the Brazilian Amazon, we obtained

157 fagus gunnii rainforest in Tasmania (hereon "montane rainforest") as a function of climate.

158 low SR (e.g. subtropical monsoon forest and montane rainforest), which were located below the trade-

159 cal year bp induced a disequilibrium between montane rainforests and climate that drove a loss of res

160 ic tree communities of Southeast Asian lower-montane rainforests.

161 argeted conservation measures, especially of montane refuge populations, may yet preserve a represent

162 earing climates are concentrated in tropical montane regions and the poleward portions of continents.

163 ss barriers, implying that dispersal between montane regions is important for the formation of montan

164 is distributed predominantly across arid and montane regions of Asia.

165 self-fertilizing species occurring in mostly montane regions of western North America.

166 settings but also in tectonically quiescent montane regions such as the Appalachian Mountains.

167 Montane regions worldwide have experienced relatively lo

168 tropical species, particularly in biodiverse montane regions, but accurate estimates of extinction ri

169 of birds' elevational range sizes within 31 montane regions, using more than 4.4 million citizen sci

170 In montane regions, where climate change is expected to cau

171 he key drivers of plant species diversity in montane regions.

172 ing anthropogenic changes in the land use of montane regions.

173 n speciation, migration, and biodiversity in montane regions.

174 e can all strongly affect plant invasions in montane regions.

175 or by broadcasting whitewater river noise in montane riparian zones for two summers.

176 prolite assemblage from a rock overhang in a montane river valley in southern New Zealand.

177 Tropical montane rivers (TMR) are born in tropical mountains, des

178 the physiological and regulatory level in a montane salamander (Plethodon metcalfi).

179 the study presented here, genetic data from montane scorpions in the Vaejovis vorhiesi group, restri

180 y estimating the potential distribution of a montane shrew (Mammalia, Soricidae, Cryptotis mexicanus)

181 ct old-growth forests (AfriMont) spanning 44 montane sites in 12 African countries.

182 We find that montane sites in the AfriMont plot network have a mean A

183 actions that help protect the future of the montane skink, and additional surveys to map its full di

184 wcase this challenge by focusing on Africa's montane skink, Proscelotes aenea.

185 Montane species are also typically more vulnerable to en

186 The imminent demise of montane species is a recurrent theme in the climate chan

187 ding that average upslope shifts in tropical montane species match local temperature increases signif

188 er than faster speciation at mid-elevations (montane species pump), despite the recency of the major

189 ndicates that landform type not only affects montane species richness, but also contributes to the co

190 In topographically complex landscapes, montane species typically inhabit multiple mountainous r

191 Many montane species undertake elevational migration in respo

192 rical climate projections suggest that these montane species were able to persist in the southern Atl

193 the upslope retreat of the less thermophilic montane species.

194 ficantly more closely than in temperate-zone montane species.

195 We study two montane, stream-associated species of glassfrogs: Vitreo

196 ons and are most prevalent among Neotropical montane, stream-associated species.

197 (Baetis bicaudatus and B. tricaudatus) from montane streams over an elevation gradient spanning 1400

198 t dominates the hydrograph of many temperate montane streams, yet little work has characterized how s

199 vident from high sediment yields in tropical montane streams.

200 oncentration (n = 332) measurements spanning montane, swamp, and lowland forests.

201 s using two AF social wasp species - the mid-montane Synoeca cyanea and the lowland Synoeca aff.

202 s may be relevant to other Andean clades and montane systems globally.

203 ing temperature with increasing elevation in montane systems has long been recognized as a major fact

204 Heterogeneous terrain in montane systems results in a decoupling of climatic grad

205 ls and could be applied to other species and montane systems to better understand mammalian populatio

206 0-1.200 m above sea level) and primary upper montane to subalpine forests (1,500-2,100 m above sea le

207 establishment ability of subalpine and upper montane trees.

208 minance of the tree, Oreomunnea mexicana, in montane tropical forest in Panama.

209 romiscuous vole species, the meadow vole and montane vole.

210 t not in the relatively asocial, promiscuous montane vole.

211 voles (Microtus ochrogaster) and promiscuous montane voles (Microtus montanus) exhibit remarkable dif

212 differently in infant and adult prairie and montane voles and, thus, could exert differential effect

213 AVP receptor binding showed an early peak in montane voles but did not change significantly in prairi

214 Male and female montane voles did not differ.

215 ult level at weaning, whereas the binding in montane voles remained unchanged into adulthood.

216 ad higher AVP receptor binding at birth than montane voles, and this difference persisted with little

217 Thereafter, the binding increased rapidly in montane voles, but it remained unchanged in prairie vole

218 in bee pollination efficiency under adverse montane weather conditions was proposed to drive these s

219 onosequence of feral pig removal in tropical montane wet forests on the Island of Hawai'i.

220 ained 5.2 degrees C MAT gradient in tropical montane wet forests on the Island of Hawaii.

221 and distribution of carbon pools in tropical montane wet forests will be less sensitive to rising MAT

222 individuals of the forest bird species, the Montane White-eye Zosterops poliogaster from 16 sites an

223 rds to recover food stores and survive harsh montane winters.

224 In the upper montane zone the model predicted a lack of forest vegeta

225 and the archaeological record of hunting in montane zones.