ライフサイエンスコーパス: biome

1 ity may lead to an increase in grass in this biome.

2 /GPP remains approximately constant within a biome.

3 n previous estimates for the tropical forest biome.

4 characteristic drought time-scales for each biome.

5 genetic variation across the xeric Caatinga biome.

6 Bee responses varied slightly by biome.

7 nge of temperatures that occur in the tundra biome.

8 taxonomic units identified in a given ICoMM biome.

9 insights into the assembly of this important biome.

10 of deforestation in this globally important biome.

11 ica, which represent an arid, lower-latitude biome.

12 influencing the net C balance of the tundra biome.

13 identification of multiple species within a biome.

14 vannas in what is otherwise a highly dynamic biome.

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

16 tive net CO2 uptake trends across the boreal biome.

17 nd least explored resource in this inspiring biome.

18 l work has been limited in scope to a single biome.

19 and response to disturbance) in the tropical biome.

20 esearch Council, AstraZeneca UK, US Army, EU-Biomed.

21 st of P acquisition varies only 2-fold among biomes.

22 lower productivity when compared with other biomes.

23 of decentralization, especially in tropical biomes.

24 ation responses across disturbance types and biomes.

25 M-associated plants in mid- and low-latitude biomes.

26 sitively with its specific leaf area in most biomes.

27 fire feedback in tropical savanna and forest biomes.

28 anging, with unknown consequences for forest biomes.

29 y information across terrestrial and aquatic biomes.

30 with implications for diversity within both biomes.

31 t biomes and 4.2 to 5.3 years for non-forest biomes.

32 ompensation in many tropical and subtropical biomes.

33 om the atlantic forest, caatinga and cerrado biomes.

34 protocol to each of the world's major forest biomes.

35 al separation is widespread across different biomes.

36 d P) additions across temperate vs. tropical biomes.

37 transforming fire regimes in many of Earth's biomes.

38 es capture major observed patterns in marine biomes.

39 genus Myrciaria occurs in various Brazilian biomes.

40 d and uninvaded plant communities from three biomes.

41 ements (R(2) > 0.7) in most of the evaluated biomes.

42 d N have shown inconsistent patterns between biomes.

43 ay invoke massive nonlinear shifts in boreal biomes.

44 d elimination among geographically separated biomes.

45 of plant and animal communities vary across biomes.

46 versity and function vary across terrestrial biomes.

47 nzymes) across a wide variety of terrestrial biomes.

48 rease moisture variability within and across biomes.

49 humid tropical, dry tropical, and temperate biomes.

50 Delta(leaf) of up to 6 per thousand between biomes.

51 d with shifts between temperate and tropical biomes.

52 rranean-type and temperate coniferous forest biomes.

53 ted areas may mitigate the problem in desert biomes.

54 rees of latitude, from subtropical to boreal biomes.

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

56 y leaves of 218 plant species spanning seven biomes.

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

58 obustness of such a relationship across more biomes.

59 g boreal, temperate and Mediterranean forest biomes.

60 nd for sharing of pathogens across hosts and biomes.

61 biguously extrapolate these results to other biomes.

62 irically with experiments that spanned three biomes.

63 P), and East Asia, corresponding to distinct biomes.

64 transition zone between boreal and temperate biomes.

65 -arcmin global grid, ecoregions (501 units), biomes (14 units), countries (124 units), continents, an

66 arrangements were amplified according to the BIOMED-2 protocol and PCR products were sequenced direct

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

68 sion has occurred in the neighboring Cerrado biome, a biodiversity hotspot comprised of dry forests,

69 led reactive N inputs to the tropical forest biome, a far greater change than previously thought.

70 We analyzed 100 time series from biomes across Earth to ask how diversity within assembla

71 vs. altered disturbance regimes for various biomes across the eastern United States.

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

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

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

75 Humid biomes also respond to drought at short time-scales, but

76 Our cross-biome analyses shows significant implications for such f

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

78 it the largest fire on record for the tundra biome and doubling the cumulative area burned since 1950

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

80 will be highly correlated with annual ES at biome and global scales; (2) there will be parallel patt

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

82 2000 forest cover was highest in the boreal biome and lowest in the humid tropics.

83 y diverse vegetation in the temperate forest biome and provide support for recent moves toward rewild

84 ch of the midwestern United States, but this biome and the soil microbial diversity that once sustain

85 me, ranging from 12 to 53.7 years for forest biomes and 4.2 to 5.3 years for non-forest biomes.

86 ifferences in modeled carbon processes among biomes and as influenced by nitrogen processes.

87 mically as pollinators in cool and temperate biomes and as model organisms for scientific research.

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

89 hic occurrence of N(2) fixers across diverse biomes and at the global scale.

90 ift of attention to previously ignored major biomes and careful application of verified methods for v

91 eled fires, and the relationship of these to biomes and climate are not deterministic.

92 evel phylogeny, and paleo-reconstructions of biomes and climate to examine Cenozoic imprints on the p

93 Differing biomes and climates may be represented within the same p

94 ble interface between terrestrial and marine biomes and even small changes in the magnitude and predi

95 ion on microbial communities across multiple biomes and explore what determines the vulnerability of

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

97 ampled from 11 locations covering a range of biomes and latitudes around the world.

98 af forest had the highest NPP among the nine biomes and moderate residence times, leading to a relati

99 E experiments in mature forests in different biomes and over a wide range of climate space and biodiv

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

101 atures that is remarkably uniform across all biomes and plant functional types.

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

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

104 related to patterns of climate, vegetation (biomes), and human activity.

105 nd biotic and abiotic factors at individual, biome, and global scales, and developed a global gridded

106 sification of the lineages that inhabit this biome, and/or a long recovery period from the terminal C

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

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

109 ated negatively with its wood density in all biomes, and positively with its specific leaf area in mo

110 with drought to a maximum WUE(e) across all biomes; and a minimum native state in wetter years that

111 turnover rates of carbon pools in semi-arid biomes are an increasingly important driver of global ca

112 Arid and humid biomes are both affected by drought, and we suggest that

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

114 biome clearing occurs within only 6% of the biome area, emphasizing the presence of forest clearing

115 timated to be 1.39% (SE 0.084%) of the total biome area.

116 s likely differ from those operating in arid biomes, as plants usually have a poor adaptability to wa

117 s ago is among the most dramatic examples of biome assembly in the geological record.

118 nual net C sink for the entire Arctic tundra biome averaged over the last quarter of the twentieth ce

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

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

121 ugh processes and sensitivities differ among biomes, based on expert opinion, we expect forests to ex

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

123 e combine the process-based ecosystem model (Biome-BGC) with climate change-scenarios based on both R

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

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

126 y available on the web at http://fairbrother.biomed.brown.edu/spliceman/

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

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

129 have long utilized resources from all forest biomes, but the most indelible anthropogenic signature h

130 icrobial diversity that once existed in this biome by analyzing relict prairie soils and found that t

131 is the case for BMC Bioinformatics and other BioMed Central journals).

132 The trial was registered at BioMed Central Ltd (www.controlledtrials.com) as ISRCTN0

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

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

135 thin the context of regional, climate-driven biome changes.

136 Fifty-five percent of total biome clearing occurs within only 6% of the biome area,

137 t loss in Brazil accounts for 47.8% of total biome clearing, nearly four times that of the next highe

138 from 2000 to 2005 and to compare GFCL among biomes, continents, and countries.

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

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

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

142 romogenic media, which included Colorex VRE (BioMed Diagnostics, White City, OR) or Oxoid VRE (Oxoid,

143 analyse climate, CO2 and fire influences on biome distribution and net primary production (NPP) in l

144 c and natural factors contributed to current biome distribution is thus a crucial issue to understand

145 tly through photosynthesis, but also through biome distribution, which is strongly influenced by fire

146 tions played a major role in shaping current biome distributions well before humans arrived.

147 Changes in biome distributions, whether at the cost of savanna (due

148 Forest and savanna biomes dominate the tropics, yet factors controlling the

149 mmunicate stoichiometric signals from remote biomes dominated by diatoms with low N:P ratios.

150 y biota, such as the rise of grass-dominated biomes during the mid-Tertiary.

151 learned from a given disturbance regime and biome (e.g. crown-fire Mediterranean ecosystems) can gui

152 ar mainly at the edges of globally important biomes (e.g., boreal and tropical forests).

153 Biodiversity intactness within most biomes (especially grassland biomes), most biodiversity

154 ltiple times and C4 plants now dominate many biomes, especially in the tropics and subtropics.

155 inance is one of the most dramatic events of biome evolution in Earth history.

156 oxide measurements, we derived the basin net biome exchange (that is, the carbon flux between the non

157 ssions from fires and the suppression of net biome exchange by drought.

158 portance for the global carbon budget is net biome exchange of CO2 with the atmosphere (NBE), which r

159 The boreal biome experienced the largest area of GFCL, followed by

160 antic forest means that 12% of the remaining biome experiences altered microclimate conditions.

161 of soil fauna on decomposition rates between biomes, from climate-driven biomes to those where climat

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

163 We utilize a large, unmanaged biome (>135 000 km(2) ) which spans a broad latitudinal

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

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

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

167 ter availability across the temperate forest biome have the potential to offset gains in carbon (C) u

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

169 atterns in clades endemic to different major biomes illuminate the evolutionary process.

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

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

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

173 rders of magnitude), and habitats (all major biomes) in our database allows us to quantify novel feat

174 ed with water availability within and across biomes, indicating power for anticipating drought respon

175 d simultaneous stress for these nutrients at biome interfaces.

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

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

178 he majority of estimated GFCL for the boreal biome is due to a naturally induced fire dynamic.

179 This is highly significant because the skin biome is rich with potential TLR4 agonists.

180 We demonstrate that the regional biome is shifting; gains exceed losses and are located i

181 lines will affect carbon storage across this biome is unclear.

182 We conclude that the distribution of biomes is a better predictor of vulnerability than posit

183 Despite their ecological importance for many biomes, knowledge regarding herb hydraulics remains very

184 is synthesis identifies the need to consider biome, landscape position, and vascular/moss vegetation

185 h a recently compiled global data set at the biome level.

186 do this, we create a new dataset that merges biome-level associations for all monocot genera with cou

187 Biome-level trends in tree density demonstrate the impor

188 ecies' niches, even in disturbance-dependent biomes like savanna, remains poorly understood.

189 Resilience of rainfed agriculture in both biomes likely depends on water recycling in undisturbed

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

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

192 Climate-driven shifts in these marine biomes may alter the mean N/P ratio and the associated c

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

194 relations among traits observed in different biomes; models lacking these details would behave poorly

195 ess within most biomes (especially grassland biomes), most biodiversity hotspots, and even some wilde

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

197 this varies considerably within this diverse biome; N deposition explains a much smaller proportion o

198 We apply this technique to the biome of the oral mucosa and find that greater than 25%

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

200 n dioxide with the atmosphere than any other biome on Earth, and thus play a disproportionate role in

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

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

203 -sea ecosystems, which represent the largest biome on Earth, viruses have a recognised key ecological

204 e oligotrophic open ocean-the most extensive biome on Earth.

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

206 served in the tropics, with the most diverse biome on the planet treated as a single type in models.

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

208 e these results to the whole Atlantic Forest biome, one of the most disturbed biodiversity hotspots.

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

210 ated or modeled at very coarse scales (e.g., biomes or ecoregions).

211 Here, we ask whether the distribution of biomes or range position better reflects spatial variati

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

213 ersification suggests that the boreal forest biome originated via genetic coevolution of above- and b

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

215 tus of present-day species, communities, and biomes over the last few decades to millennia and on the

216 We then discuss cross-biome patterns of insect-driven tree mortality and draw

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

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

219 -annual variability patterns of European Net Biome Productivity (NBP) are linked to anomalies in heat

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

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

222 British Heart Foundation, European Community Biomed Programme, Australian National Health and Medical

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

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

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

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

227 rimary production/evapotranspiration) across biomes ranging from grassland to forest that indicates a

228 e residence time (tau'E) was stable for each biome, ranging from 12 to 53.7 years for forest biomes a

229 Inferences from palaeo-biome reconstruction (PBR) and phylogeography regarding

230 viral nucleic acid sequences from different biomes, relies on several concentration, purification, e

231 Metagenomic characterization of complex biomes remains challenging.

232 scribe a modification of digital karyotyping-biome representational in silico karyotyping (BRISK)-as

233 d a representational deep-sequencing method (biome representational in silico karyotyping [BRiSK]) we

234 On the contrary, semiarid and subhumid biomes respond to drought at long time-scales, probably

235 We found that arid biomes respond to drought at short time-scales; that is,

236 We conclude that biome-scale differences in the abundance of nitrogen fix

237 lost by fire, relative to both ecosystem and biome-scale fluxes, demonstrates that a climate-driven i

238 This biome-scale pattern presents an evolutionary paradox(3),

239 This indicates biome-scale resilience to the interannual variability as

240 At biome-scale, terrestrial carbon uptake is controlled mai

241 nced litter decomposition at both global and biome scales (average increment ~ 37%).

242 litter decomposition rates at the global and biome scales, and to assess how climate, litter quality

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

244 n suggest the potential for relatively rapid biome shifts and biomass changes.

245 h lack of fuel and potentially driving local biome shifts from fynbos shrubland to nonburning semides

246 onstruct changes in fire activity as well as biome shifts over time.

247 the context of climate-driven forest-savanna biome shifts through the mid-to-late Holocene.

248 s of habitat intactness and vulnerability to biome shifts, using multiple measures of habitat intactn

249 fication dynamics associated with subsequent biome shifts.

250 arameters analyzed and across different land biomes, showing that the response of vegetation to droug

251 re has been largely absent from most of this biome since the early Holocene epoch, but its frequency

252 l rainforest families have characterized the biome since the Paleocene, maintaining their importance

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

254 t changes in environmental conditions (e.g., biomes), spatial variation in vulnerability to extirpati

255 Our results advocate for the inclusion of biome-specific soil fauna effects on litter decompositio

256 ced forest die-off is widespread in multiple biomes, strongly affecting the species composition, func

257 n regimes even within relatively homogeneous biomes such as grasslands.

258 vation attention in the Andes has focused on biomes such as rain forest, cloud forest, and paramo, wh

259 temperature change is lowest in mountainous biomes such as tropical and subtropical coniferous fores

260 hich may be higher than in other neotropical biomes, such as savanna.

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

262 iderably greater area of the tropical forest biome than deforestation and logging combined.

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

264 e in soil and sediment-two underinvestigated biomes that combined account for only approximately 2.5%

265 In the Mediterranean biome, there are differences in functional strategies to

266 extensively studied across a broad range of biomes, there is surprisingly little consensus on how th

267 Rapid warming across northern biomes threatens to accelerate rates of peatland ecosyst

268 as been no comparative study across tropical biomes to determine rates of forest re-growth, and how t

269 We evaluated the response of the Earth land biomes to drought by correlating a drought index with th

270 role in determining the sensitivity of land biomes to drought.

271 ts, but they lack the rapid response of arid biomes to drought.

272 on rates between biomes, from climate-driven biomes to those where climate effects were mediated by c

273 st flammable ecoregions of the boreal forest biome, to infer causes and consequences of fire regime c

274 PsychARTICLES, Web Of Science, EBM Reviews, BioMed, TRIP, ERIC, SCOPUS (January 2000-April 2011) was

275 early within the Pliocene, driving complete biome turnover.

276 factors tested in these analyses, including biome type, dispersal ability, and elevation preference.

277 crops and forests and substitution of these biome types for ethanol production implies trade-offs.

278 eal, conifer, deciduous, and tropical forest biomes using the LIDET-provided climatic decomposition i

279 es into the CABLE model decreased Xss in all biomes via reduced NPP (e.g., -12.1% in shrub land) or d

280 ehensive database for 231 species spanning 7 biomes, we demonstrate that temperature-dependent increa

281 In contrast to these mesic biomes, we present evidence for a different, older diver

282 , spanning 44 countries and most terrestrial biomes, we reveal a globally consistent positive concave

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

284 degrees of latitude in the Arctic and Boreal biomes, we show that air temperature explains c.

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

286 Relationships in the grassland biome were significantly different from the global avera

287 When all biomes were normalized by rainfall, shrublands however,

288 ections of change largely dependent upon the biome where change is occurring.

289 protect forest fragments, especially within biomes where contiguous forest cover has diminished dram

290 onger growing season, especially in years or biomes where water is a limiting factor, is not due to w

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

292 on agricultural lands in the tropical forest biome, wherein lies the greatest potential to conserve o

293 cover across Central America, stratified by biomes, which we related to socioeconomic variables asso

294 llaboration between researchers of disparate biomes who recognize common patterns in shared data.

295 studies by searching MEDLINE, Embase, Pascal Biomed, WHOLIS, and African Index Medicus databases for

296 Russia's boreal (taiga) biome will likely contract sharply and shift northward i

297 several more recent studies predict that the biome will remain largely intact.

298 es of similar magnitude were observed across biomes with no apparent effect on tree growth raises the

299 icators of ancient precipitation and PFT (or biome) with modern Delta(leaf) patterns has potential to

300 etworks from 28 studies representing diverse biomes worldwide.