ライフサイエンスコーパス: biome

1 xts (e.g. for individual taxonomic groups or biomes).

2 loss of large frugivores in this endangered biome.

3 ges for evergreen conifers across the boreal biome.

4 counter, compared with AS males from the dry biome.

5 genetic variation across the xeric Caatinga biome.

6 insights into the assembly of this important biome.

7 J, Hispanic, and African American cohorts in BioMe.

8 eneral 'greening' trend in the arctic tundra biome.

9 LRBA, with high dominant model penetrance in BioMe.

10 tive net CO2 uptake trends across the boreal biome.

11 species in the Central US shortgrass steppe biome.

12 hich collectively constitute Earth's largest biome.

13 rub vegetation (+7.4 +/- 2.0%) in the Arctic biome.

14 her proportion of unique NCLDVs in the polar biomes.

15 roduction and assess climatic controls among biomes.

16 portant players in ecosystems across Earth's biomes.

17 development in structure and function across biomes.

18 timate it, and known variations across ocean biomes.

19 erate as habitat conversion proceeds in most biomes.

20 trols growth and tree longevity across world biomes.

21 dominated by polar desert and steppe-tundra biomes.

22 in estimating the microbial CUE in different biomes.

23 substantial variation across ecoregions and biomes.

24 ure sensors from 51 countries across all key biomes.

25 ity of Saxifragales is greatest in temperate biomes.

26 strength of this relationship varies across biomes.

27 Rainforest, Succulent, Temperate and Savanna Biomes.

28 tanding of the stability and conservation of biomes.

29 including once-common species and from most biomes.

30 ents from 112 sites spanning all terrestrial biomes.

31 erse and abundant tree genera in Neotropical biomes.

32 reliminary comparisons of metagenomes across biomes.

33 lant-nutrient feedbacks at the scale of land biomes.

34 s, leaf age and canopy position from diverse biomes.

35 ent cycles in boreal, temperate and tropical biomes.

36 in plant-symbiont nutrient strategies across biomes.

37 ate grasslands are the world's most impacted biomes.

38 relative effect in grassland than in wooded biomes.

39 n the land carbon and nutrient cycles across biomes.

40 diversity of LMA in ecosystems across global biomes.

41 esponses to warming can vary greatly between biomes.

42 rease moisture variability within and across biomes.

43 e effects expected to occur in high-latitude biomes.

44 y leaves of 218 plant species spanning seven biomes.

45 evolution of C4 grass- and grazer-dominated biomes.

46 obustness of such a relationship across more biomes.

47 ility structuring plant distributions across biomes.

48 matic variables, plant functional types, and biomes.

49 d and dry regions, such as tundra and desert biomes.

50 anagement activities in temperate and boreal biomes.

51 t methods for mapping multiple traits across biomes.

52 with some generalist species that span both biomes.

53 with further significant differences between biomes.

54 limate change, particularly in hyper-diverse biomes.

55 at 1.5x to 4x the rate of other terrestrial biomes.

56 nd function of terrestrial ecosystems across biomes.

57 e of knowledge on trait change in the tundra biome 1744 IV.

58 using young donor biome (2-3 months) or aged biome (18-20 months).

59 cerebral artery occlusion using young donor biome (2-3 months) or aged biome (18-20 months).

60 This is across 162 sites and 12 terrestrial biomes (89% of heterogeneity explained; Q-value = 1235;

61 closure for 13 temperate and tropical forest biomes across the globe are analyzed.

62 lity) vegetation-type conversion in multiple biomes across the world (131 sites).

63 However, other explanations, such as biome age, immigration and ecological limits, must also

64 lower productivity when compared with other biomes (Ahlstrom et al. 2015 Science, 348, 895).

65 Differences in IgA-Biome alpha diversity were apparent for both stool and s

66 Transition zones between biomes, also known as ecotones, are areas of pronounced

67 ssification performance was obtained for the biomes Amazonia and Caatinga using Multilayer Perceptron

68 Animals risen in the biomes Amazonia, Caatinga, Cerrado, Pampa and Pantanal w

69 s from 0 degrees S-23 degrees S across three biomes (Amazonia, Cerrado, Mata Atlantica).

70 sed especially on the little-known Succulent Biome, an assemblage of succulent-rich, grass-poor, seas

71 l variation in LMA within and across Earth's biomes, an efficient, globally generalizable approach to

72 These data suggest that IgA-Biome analyses can be used to identify novel microbial s

73 mposes high demands on the accuracy of micro-biome analysis techniques.

74 , drylands represent the largest terrestrial biome and are projected to expand by 23% by the end of t

75 We conclude that re-establishing biome and Earth system functions needs to become an urge

76 s represent the planet's largest terrestrial biome and evidence suggests these landscapes have large

77 duan region, phylogenetic reconstructions of biome and geographic range evolution show that extant li

78 tigated the biogeography and trajectories of biome and growth form evolution across the Caesalpinia G

79 OL1 G1 and G2 risk alleles were genotyped in BioMe and imputed in BioVU/NUgene participants.

80 ts represent the world's largest terrestrial biome and provide ecosystem services of global importanc

81 roved IBD prediction for every population in BioMe and significantly improved prediction among Europe

82 cologists to relate information organised by biome and species to new data arrayed by pixels and deve

83 ected metacommunity dynamics in two adjacent biomes and across their ecotone by resurveying 106 sites

84 importance of these factors across different biomes and at the global scale require tests of the rela

85 es richness patterns, biogeographic regions, biomes and biodiversity hotspots.

86 discrepancies through time and across major biomes and climatic regions, we used a model-data fusion

87 (-14.5%), the extents of which varied among biomes and ecosystem compartments.

88 currence data and assigned species to areas, biomes and growth forms.

89 t driver of plant functioning in terrestrial biomes and has been established as a major contributor i

90 tive responses to both pressures in tropical biomes and in the Mediterranean.

91 ge effects in the world's other major forest biomes and indicate that the strength of the temperate b

92 nce the distribution of floral traits across biomes and lineages, thereby influencing organismal evol

93 compared to trees from temperate and boreal biomes and live significantly shorter, on average (186 +

94 gger appear insignificantly different across biomes and plant functional types, suggesting that therm

95 's simplicity and broad applicability across biomes and plant functional types.

96 ive states is crucial to how we manage these biomes and predict their future under global change.

97 the geographical distribution of terrestrial biomes and species targeted by marine capture fisheries

98 -induced mortality rates differ among global biomes and whether functional traits influence the risk

99 drought sensitivity was considerable within biomes and within ecosystems and was mediated by landsca

100 America (2,025 inventories from wet to arid biomes), and a new, large-scale phylogenetic hypothesis

101 of different sizes, morphology, land cover, biomes, and climatic conditions.

102 ine-root traits across root orders, species, biomes, and environmental gradients while also providing

103 areas for restoration across all terrestrial biomes, and estimates their benefits and costs.

104 ions in warm biomes, underestimation in cold biomes, and likely significant overestimation of overall

105 ld and domesticated plants, growth forms and biomes, and to identify crucial knowledge gaps.

106 calculate global fragmentation rates across biomes, and we compared these to an idealized globe with

107 s Forest area (+14.8 +/- 5.2%) in the Boreal biome; and (b) climate-driven expansion of Herbaceous an

108 rmal acclimation of leaf R is common in most biomes; and (2) the high T threshold of respiration dyna

109 ntrasting seasons across several field sites/biomes; and (b) 21 species (subset of those sampled in t

110 l disjunctions confined within the Succulent Biome are frequent and that biome shifts to the Savanna,

111 based on the erroneous assumption that these biomes are deforested and degraded.

112 fts to the Savanna, Rainforest and Temperate Biomes are infrequent and closely associated with shifts

113 f the most abundant viral sequences from all biomes are novel.

114 Tropical biomes are the most diverse plant communities on Earth,

115 Soil biomes are vast, exceptionally diverse and crucial to th

116 aining soil functionality locally and across biomes, as well as providing strong support for the incl

117 of NCLDVs across size fractions, depths and biomes, as well as their associations with eukaryotic co

118 esidence time) and how long it takes for the biome at that site to reestablish following a transition

119 evel impacts across taxa, trophic levels and biomes at a global scale.

120 favourable for carbon accumulation than the biome average.

121 l (DGVM) that simulates the distributions of biomes based on basic plant functional types with projec

122 estimate of global forest extent in dryland biomes, based on analyzing more than 210,000 0.5-hectare

123 y not change as intact units as predicted by biome-based modeling, but are likely to trend toward sim

124 d particular ecosystem function of different biomes become readily apparent.

125 Across biomes, belowground productivity increases with mean ann

126 and without heart failure in the Mount Sinai BioMe Biobank enrolled between 2007 and 2015 using elect

127 ed pedigree information, in the multi-ethnic BioMe biobank in New York City.

128 ic, randomly ascertained health system-based BioMe biobank to define effects of common and rare IBD v

129 ded 5,204 AA participants from Mount Sinai's BioMe biobank.

130 Only four biomes (boreal forests, deserts, temperate coniferous fo

131 story and ecological dynamics that determine biome boundaries and plant distributions.

132 t increased natural vegetation cover in some biomes but increased losses in the Cerrado and especiall

133 Our results are consistent across biomes but not across degrading factors.

134 rate towards higher latitudes and among some biomes, but no biogeographic patterns in the frequency o

135 dence that DBD is strongest in low-diversity biomes, but weaker in more diverse biomes, consistent wi

136 d tree restoration potential across all arid biomes by 33%-45% (316-440 Mha).

137 restoration potential across a third of arid biomes by between 7% and 20% (55-166 million hectares [M

138 present the wide range of trait variation in biomes by grouping ecologically similar species into pla

139 nalysis, we searched PubMed, Web of Science, BioMed Central, Scopus, ResearchGate, Cochrane Library,

140 DLINE, Cochrane Library, Google Scholar, and Biomed Central.

141 ncrease in fire activity, possibly caused by biome changes and accumulation of fuel related to the la

142 ms, for different latitudinal zones, and for biomes characterized by harsher or milder abiotic condit

143 Our results suggest that the Succulent Biome comprises an ecologically constrained evolutionary

144 tween growth forms and test for phylogenetic biome conservatism and correlated evolution of growth fo

145 The extent to which phylogenetic biome conservatism vs biome shifting determines global p

146 d a pattern of strong phylogenetic Succulent Biome conservatism.

147 as with low human influence varies widely by biome, conserving these last intact areas should be a hi

148 diversity biomes, but weaker in more diverse biomes, consistent with biotic interactions initially fa

149 suggest a persistent transition zone between biomes contributes to limiting the redistribution of bir

150 fferential warming of tropical and temperate biomes could result in a similar proportional increase i

151 Dryland biomes cover two-fifths of Earth's land surface, but the

152 cosystems in the context of the global-scale biome crisis that our planet currently faces.

153 ed and two continental to global-scale cross-biome datasets.

154 of 49 species across temperate and tropical biomes, demonstrating that the ageing rate of photosynth

155 of oxidoreductase genes support the highest biome differentiation compared with profiles of other ca

156 ross much, but not all, of the Arctic tundra biome during recent decades.

157 Recent work has suggested that biomes during the Carboniferous Period contained plants

158 these parameters in cold climate species at biome ecotones are positively or negatively influenced b

159 For instance, of the 17 biomes encompassed by our survey, 7 were understudied an

160 mpositional change is prevalent, with marine biomes exceeding and terrestrial biomes trailing the ove

161 suggesting populations from these different biomes experience similar Fe-selective conditions.

162 he beef elemental content from the different biomes for all multivariate contrasts using NPMANOVA.

163 variables was investigated across different biomes from 2010 to 2018 using three climate datasets of

164 ataset contained leaves from a wide range of biomes from the high Arctic to the tropics, included bro

165 mate change and land-use change differ among biomes (geographical units that have marked differences

166 By combining a cross-biome global field survey, including data for 32 soil, p

167 rasting ecosystem responses, differing among biomes globally, independent of changes in mean precipit

168 fication and extinction rates, and evaluated biome/habitat and geographic shifts in Detarioideae.

169 in the early Palaeocene, after which several biome/habitat and geographic shifts occurred.

170 nstructed ancestral states for geography and biome/habitat, estimated diversification and extinction

171 d differences in fragmentation rates between biomes has received little attention.

172 Biomes have a median residence time of only 230-460 year

173 ria genera in the terrestrial and intestinal biomes have no closely related genome sequences.

174 Dryland biomes have repeatedly been recognized as inappropriate

175 In Africa, 1 million km(2), mostly of grassy biomes, have been targeted for 'restoration' by 2030.

176 ldwide and endophytes from diverse temperate biomes, highlighting a high degree of global endemism.

177 iods due to competing effects between Arctic biomes (ice, tundra, taiga).

178 or eliminated the importance of latitude and biome in predicting outcrossing or self-incompatibility.

179 t is also the most heavily fragmented forest biome in the world.

180 to delimit the climatic envelope of the two biomes in Africa using tree species lists gathered for a

181 lands and rhizospheres were the most diverse biomes in oxidoreductases but not in taxonomy.

182 across the circumpolar arctic and subarctic biomes in recent years.

183 One of the most pertinent biomes in this regard is Antarctica, given its geographi

184 ccur with ectomycorrhizal trees in temperate biomes in which seasonally warm-and-wet climates enhance

185 nd size structure across the tropical forest biome, including observed responses to precipitation and

186 The indoor biome is a novel habitat which recent studies have shown

187 iversity have mainly focused on whether this biome is an evolutionary 'cradle' or 'museum', emphasizi

188 ted parts of the world, but, in turn, tundra biome is facing the most rapid climate change on Earth.

189 n vector of simian and human malaria in this biome is the mosquito Anopheles cruzii.

190 mbly of microbial communities across earth's biomes is a major challenge in modern microbial ecology.

191 lant diversity and multifunctionality across biomes is indirectly driven by soil biodiversity.

192 The inclusion of several biomes is key to achieving multiple benefits.

193 rait data collection across all climates and biomes is still necessary.

194 wever, emphasized dryland regions, with arid biomes making up 36%-42% of potential restoration area.

195 African ecosystems, which depend on accurate biome maps to set appropriate targets for the restored s

196 hropologic as well as natural changes in the biome may have effects on IgE sensitization profiles alr

197 Ultimately, an understanding of the IgA-Biome may promote the development of novel strategies to

198 ents such as the Brazilian semiarid Caatinga biome may reveal how severe climate conditions may affec

199 Thus, increasing numbers of species in many biomes may be at risk as heat-wave events become more se

200 Replication cohorts included additional BioMe (n = 1,623), Vanderbilt BioVU (n = 1,809), and Nor

201 Changes in the distribution of biomes occurred throughout the Quaternary.

202 of aggressive fire suppression in the boreal biome of Canada has reduced the proportion of recently b

203 a 4000-km climate transect in two grassland biomes of China, the Inner Mongolian temperate grassland

204 nd represents the largest and least explored biome on Earth (<0.0001% of ocean surface), yet is incre

205 t (TRF) is the most species-rich terrestrial biome on Earth, harbouring just under half of the world'

206 Atacama Desert is the most extreme non-polar biome on Earth, the core region of which is considered t

207 atterns of speciation in the most biodiverse biome on Earth.

208 e with the atmosphere in the most productive biome on earth.

209 d at colonizing the open ocean - the largest biome on Earth.

210 ea represents the largest and least explored biome on the planet.

211 ern mangroves are among the most carbon-rich biomes on Earth, but their long-term (>/=10(6) years) im

212 f the built environment in spanning multiple biomes on Earth.

213 s better characterizes the differences among biomes on the global scale.

214 is loss of megafauna can affect processes at biome or Earth system scales with potentially serious im

215 agnitude of the response depending on forest biomes or between angiosperms and gymnosperms or evergre

216 stimates, which postulated a dry (succulent) biome origin according to the Tethys Seaway hypothesis,

217 findings are generalizable across the tundra biome, our results indicate that consistency and caution

218 ituent lineages tracked post-Gondwanan mesic biomes over thousands of kilometers, underscoring their

219 Our results suggest Arctic marine biomes persisted through cycles of glaciation, leading t

220 A data analysis, as a new paradigm for micro-biome phenotype and biomarker detection.

221 elled as a function of drought, temperature, biomes, phylogenetic and functional groups and functiona

222 1747 SUMMARY: In the rapidly warming tundra biome, plant traits provide an essential link between on

223 D), by estimating genetic penetrance in each BioMe population.

224 understanding of the role of the individual biome predicts likelihood of therapeutic benefit.

225 To evaluate landscape dynamics, we use plant biomes, preserved in the fossil pollen record, to examin

226 ospheric transport model prescribed with net biome productivity (NBP) from an ensemble of nine terres

227 LO is primarily explained by response of net biome productivity (NBP) to climate change, and by chang

228 ugh to a 27% coefficient of variation in net biome productivity (NBP).

229 to analyse the responses of terrestrial net biome productivity to soil-moisture changes, and find th

230 ated shifts in relative abundance in the IgA-Biome profiles between normoglycemic, prediabetic, or di

231 Tropical savannas are a globally extensive biome prone to rapid vegetation change in response to ch

232 r research gaps were revealed, with tropical biomes, protists, and soil macrofauna being especially o

233 dicate that subtropical and temperate forest biomes provide the highest carrying capacity for hunter-

234 piration rates at plot scales within certain biomes, quantitative frameworks for evaluating the relat

235 Only 64% of biomes recover their original biome type, but recovery t

236 Following a transition, biodiverse biomes reestablish more quickly.

237 Identifying distinctive taxa for micro-biome-related diseases is considered key to the establis

238 Closer examination of the transition between biomes (relative percentages of trees vs. shrubs) at the

239 shifts in forest carbon capture in semi-arid biomes remain poorly understood.

240 odel performances for different climates and biomes remain unclear.

241 t ecological change across the Arctic tundra biome remains poorly quantified due to field measurement

242 ce of soil age as an ecosystem driver across biomes remains largely unresolved.

243 A compromise solution avoids 26% of the biome's current extinction debt of 2,864 plant and anima

244 the acceleration of tau(eco) was examined at biome scale and grid scale.

245 m changes in terrestrial productivity at the biome scale.

246 e, the losses of small-ranged species reduce biome-scale (gamma) diversity.

247 obtained at eddy-flux sites covering diverse biomes, setting the stage for future investigations of t

248 ved to transition from tropical to temperate biomes sheds light on how complex traits evolve in the l

249 to which phylogenetic biome conservatism vs biome shifting determines global patterns of biodiversit

250 frequency of transcontinental disjunctions, biome shifts and evolutionary transitions between growth

251 in the Succulent Biome are frequent and that biome shifts to the Savanna, Rainforest and Temperate Bi

252 forecast large-scale vegetation shifts (i.e. biome shifts) in response to climate change.

253 and correlated evolution of growth forms and biome shifts.

254 es that are improving forecasts of semi-arid biome shifts.

255 will rapidly improve forecasts of semi-arid biome shifts.

256 n of experimental investments across Earth's biomes should be done in ecosystems of key importance.

257 ES males, however, from the humid biome, showed a tendency to lunge more per aggressive en

258 The Arctic marine biome, shrinking with increasing temperature and recedin

259 e use reconstructions of global land use and biomes since 1700, and 16 possible climatic and socio-ec

260 Rs in global models; however, within certain biomes soil moisture and soil carbon emerge as dominant

261 Biome-specific carbon inputs deduced from net primary pr

262 ctions of microbiome data already available, biome-specific patterns of microbial structure are not c

263 at it conflates two key explanations, namely biome stability (age and area) and productivity (ecologi

264 Biome stability alone was the strongest predictor of all

265 Climate and biome stability were quantified over the past 140,000 y

266 ts from our spatial regression models showed biome stability, rainfall seasonality, and topographic h

267 model ecosystem changes in four terrestrial biomes subjected to human removal of plant biomass, such

268 characterized yet prevalent members of this biome, such as uncultivated Flavobacteriaceae.

269 elationship, emerging within and among major biomes, suggests a potential adaptive response to water

270 mily, testing whether they originated in dry biomes surrounding the Tethys Seaway as currently hypoth

271 itical challenge is to test whether specific biomes, taxa or types of species benefit or suffer in a

272 ncipient in hitherto relatively intact major biomes that are rapidly succumbing to encroaching defore

273 smell allowed the turkey vulture to colonize biomes that are suboptimal for scavenging birds and beco

274 ed to identify research questions and target biomes that will yield substantial gains in predictive c

275 om 42 eddy covariance sites across six major biomes, that ecological memory-decomposed into environme

276 levels of biodiversity-across many taxa and biomes-that agricultural landscapes can support over the

277 om tropical areas to semi-arid Mediterranean biomes through atmospheric wave trains.

278 We used 247 microbial metagenomes from 18 biomes to determine which set of genes better characteri

279 Further, we find the two biomes to have highly divergent tree species composition

280 Ecologists expect species and biomes to shift poleward and upward with climate change,

281 with marine biomes exceeding and terrestrial biomes trailing the overall trend.

282 Regardless of biome, treatment method and season, increased precipitat

283 y vegetation structure, both in terms of the biome type (wooded vs. grassland environments) and the d

284 fossil pollen record, to examine how long a biome type persists at a given site (residence time) and

285 Only 64% of biomes recover their original biome type, but recovery time is 140-290 years.

286 ze to discern relative responses for a given biome type.

287 ridional transect crossing all major surface biome types.

288 range of C flux responses, across and within biome types.

289 lead to overestimation of emissions in warm biomes, underestimation in cold biomes, and likely signi

290 r a relatively small proportion of the cross-biome variation in multiple ecosystem properties.

291 encing of SIgA-coated/uncoated bacteria (IgA-Biome) was conducted on stool and saliva samples of norm

292 t has been statistically grouped into palaeo-biomes, we show a more transitional nature of terrestria

293 s located along the limits of the rainforest biome were significantly associated with forest losses w

294 ents a large range of climate conditions and biomes where terrestrial primary productivity and its in

295 imal populations throughout many terrestrial biomes, whereas temperature explained little variation.

296 The composition of those biomes will have likely affected hominin hunting behavio

297 mycorrhizal fungi)-are most abundant in arid biomes with alkaline soils and high maximum temperatures

298 Soil bacterial diversity varies across biomes with potential impacts on soil ecological functio

299 ver, the effects were highly variable across biomes, with strongest temperature responses in shrublan

300 ation of plant-symbiont relationships across biomes worldwide and (2) the emergent consequences for p