ライフサイエンスコーパス: land

1 ngling governance regimes across unprotected land.

2 rk matter by observations in air, water, and land.

3 rge crop production into previously unfarmed land.

4 ther local communities formal legal title to land.

5 etaceous to recent expansion of diversity on land.

6 ush occurring at a subsite draining suburban land.

7 olid in the mid-latitudes and solid over dry lands.

8 ee thorny bamboo plantations and nearby bare lands.

9 ted lands, but not the SoGS in non-irrigated lands.

10 ations (17.5%), clean-up on water (17.4%) or land (14.6%), decontamination (14.3%), and administrativ

11 se of nature restoration on abandoned arable land a compositional shift in soil biota, preceded by ti

12 s seems to coincide with the colonization of land, a likely requirement for plant adaptations to the

13 lassify the intensity of aeolian desertified land (ADL).

14 creases 3-4% K(-1) globally, 4-5% K(-1) over land and 2-4% K(-1) over ocean, and is remarkably robust

15 undergone 470 million years of evolution on land and different groups have distinct body shapes.

16 s declining exponentially with distance from land and indicate that islands may act as stepping stone

17 il fuel-derived CO2 but is also sensitive to land and ocean carbon cycling and uptake.

18 fluence of human activities due to increased land and sea use.

19 rchards and vineyards, suggest that Fresno's land and water management have become increasingly disco

20 ected activities in natural and agricultural lands and assess the degree to which these actions could

21 n spatial optimization modeling we highlight lands and waters that together achieve joint conservatio

22 Evidence for Neoproterozoic 'greening of the land' and intensification of weathering c. 0.85-0.54 Ga

23 biochemical and physiological adaptations to land, and a life cycle with an alternation between multi

24 lity and reduce pressure on water resources, land, and ecosystem in Iran.

25 and production, which indicates that barren land, and woody crop areas are most vulnerable to potent

26 can guide optimal investments to counteract land- and ocean-based stressors: (1) marine restoration

27 We use a dynamic land- and sea-scape model to determine whether limited f

28 Immediately following land application, the ARGs abundant in manure were detec

29 Reduction in arable land area and reduced water availability make it paramou

30 tons to maximize FEW production from a given land area.

31 Large land areas have lost SOC as a result of land use practic

32 ther, the daytime convective atmosphere over land areas is full of small migrant insects, among them

33 ed of image motion during forward flight and landing, as well as estimate flight distances (odometry)

34 balance, but also have significantly altered land-atmosphere CH4 emissions for this region, potential

35 of the summer monsoon, suggesting that local land-atmosphere feedbacks involving desiccated soils and

36 Classic, model-based theory of land-atmosphere interactions across the Sahel promote po

37 Tree phenology mediates land-atmosphere mass and energy exchange and is a determ

38 ships are important both ecologically and to land-atmosphere models that couple terrestrial vegetatio

39 Land availability for growing feedstocks at scale is a c

40 lagic and benthic environments, and show how land-barriers, salinity, depth, and environmental hetero

41 nd has a low rate of vegetation decline; (3) land-based actions are optimal when the ratio of marine

42 ntrast the cost-effectiveness of marine- and land-based conservation actions.

43 Implementation of a range of land-based emissions reduction activities can materially

44 ion of marine plastic debris originates from land-based sources and rivers potentially act as a major

45 k prey in irrigated lands over non-irrigated lands because of higher quality prey on irrigated lands,

46 ke advantage of the isolation of West Indian land-bridge islands by rising postglacial sea levels to

47 tively associated with the SoGS in irrigated lands, but not the SoGS in non-irrigated lands.

48 habitat has coincided with increased use of land by polar bears (Ursus maritimus) from the southern

49 d continuous peat C reconstructions with the land C balance inferred from double deconvolution analys

50 ecosystems and widespread degradation of the land carbon sink.

51 climatic extreme that negatively affects the land carbon sink.

52 gnal in the year-to-year fluctuations of the land carbon sink.

53 interactions, which could potentially inform land-carbon models that explicitly include mineral-bound

54 When tested against a human landing catch during peak mosquito abundance, this "host

55 at integrate spatially explicit modelling of land change and ecosystem services in a Land-Use Change

56 ies expanded and forest burning was used for land clearance.

57 magnitude and interannual variability of the land CO2 sink.

58 lexity and robustness concomitantly with the land colonization by flowering plants and, by inference,

59 asts: the Arctic Ocean is near surrounded by land compared with the Antarctic continent, which is sur

60 The hypothesis that realistic land conditions such as soil moisture/soil temperature (

61 sults show that the overall effectiveness of land consolidation in improving agricultural productivit

62 Furthermore, we found effectiveness of land consolidation projects displayed clear regional dif

63 trends of MODIS NDVI after implementation of land consolidation.

64 i) profound reconfigurations in land use and land control over the past several decades and (ii) evid

65 Normalized Burn Ratio (NBR), existing MODIS Land Cover (LC) and Vegetation Continuous Fields (VCF) p

66 However, at the local scale, land use and land cover (LULC) change strongly affects the occurrence

67 To understand the connections between land cover and childhood DD, we compiled a database of 2

68 lights the importance of regional changes in land cover and dust concentrations in affecting the pote

69 anding their role on historical land use and land cover change (LULCC) and on the carbon cycle is ess

70 l contribution of non-oceanic factors (e.g., land cover change and CO2-induced warming) to the 2016 d

71 irect climate change rather than by indirect land cover change impacts.

72 access to high-quality Landsat data, we map land cover change in Southeast Sulawesi, Indonesia, from

73 e of long-term, multidirectional analyses of land cover change.

74 ing unprecedented high rates of land use and land cover change.

75 sites in heterogeneous landscapes with four land cover classes: semi-natural habitat, olive groves,

76 Land cover diversity and fragmentation were more explana

77 nto the causes and potential consequences of land cover map error, and suggest several recommendation

78 ror, and suggest several recommendations for land cover map users.

79 uantify uncertainties in global and European land cover projections over a diverse range of model typ

80 As little as 1% impervious land cover surrounding a lake increased the likelihood o

81 A lower diversity of land cover types is purported to decrease arthropod dive

82 Even so, specific land cover types, such as deciduous forest, influenced a

83 y, which may occur at different rates across land cover types.

84 and fragmentation were more explanatory than land cover types.

85 d for each site demonstrated that impervious land cover was a strong predictor of chloride trends in

86 drivers related to climate, topography, and land cover.

87 inning population performance, and change in land cover.

88 Land-cover change from energy development, including sol

89 evolution from models able only to deal with land-cover change to more sophisticated approaches that

90 t due to the contribution from anthropogenic land-cover changes.

91 ided by the existing availability of natural land-cover types outside the current network of NAM prot

92 c relocation patterns in terms of associated land-cover types.

93 With over 30% global land coverage, the forest is one of nature's most genero

94 km foot print) SM/ST dataset prepared from a land data assimilation system, as part of a national mon

95 in modulating shrub encroachment and ensuing land degradation processes.

96 ultant shifts in fish community composition, land development is estimated to decrease fish nutrient

97 pth from below (reflecting topography-driven land drainage).

98 vection from ice-covered ocean onto adjacent land during the growing season), the large-scale compone

99 tional soil C sequestration, the capacity of land ecosystems to slow the rise in atmospheric CO2 conc

100 marily from fluctuations in carbon uptake by land ecosystems.

101 freestanding graphene were prepared by soft-landing electrospray ion beam deposition, which allows c

102 damage was mainly related to the energy and land footprints, the latter being mainly determined by a

103 illion people globally, many of whom use the land for agricultural and pastoral activities.

104 e of population growth, decreasing water and land for agriculture, and increasing climate variability

105 re is growing evidence that life has been on land for billions of years.

106 ta sets, we evaluated the capacity of Iran's land for sustainable crop production based on the soil p

107 ica, most likely due to fire suppression and land fragmentation.

108 season (SoGS) in irrigated and non-irrigated lands from 1992 to 2015 and tested whether either estima

109 trialization of Earth and diversification of land fungi and plants.

110 three decades and tested how the surrounding land has influenced these changes.

111 of protected areas: an additional 5% of the land has the potential to more than triple the protected

112 ons for several millions of years, with most land ice-covered and much of the ocean seasonally freezi

113 Nationwide, 77.6% of the national arable land is considered to be in good condition.

114 s, with large extents of intensively managed land limiting 'adaptive' community reorganization in res

115 ndividual Golgi cisternae are separated and "land-locked" between mitochondria.

116 idual energy use in human societies to other land mammals.

117 ility across spatial scales is important for land management and policy decisions.

118 Australia, rising atmospheric CO2 , changing land management and rainfall are likely causes.

119 at allow also for the partial integration of land management changes.

120 remains a key limitation to joint water and land management decision-making.

121 is thus required to achieve the inclusion of land management in ESMs.

122 itization of implementation, we evaluate ten land management practices-forestry harvest, tree species

123 For the longer term a comprehensive land management representation can be anticipated for al

124 Appropriate land management strategies must be implemented across th

125 ifies the landscape approach as an ethic for land management, demonstrates how it relates to landscap

126 ost influential methods for multi-functional land management.

127 Climatic models were developed to aid land managers in predicting disease severity and accordi

128 ge impacts and uncertainties and should help land managers to maximize the value of conservation inve

129 applied the matrix approach to the Community Land Model (CLM4.5) with vertically-resolved biogeochemi

130 adjustments cause the eye movement again to land near the target.

131 ne 2211 kg CO2 equivalents/capita/annum) and land occupation increases (<1% of baseline 9000 m(2) lan

132 y's environmental impacts (carbon emissions, land occupation, water use, etc.) Urban farming (UF) has

133 upation increases (<1% of baseline 9000 m(2) land occupation/capita/annum) under optimal production s

134 estuaries (STEs) are of major importance for land-ocean biogeochemical fluxes.

135 ffective conservation outcomes for connected land-ocean systems can proceed without complex modelling

136 The two dice land on side [Formula: see text] with unknown probabilit

137 In 2012, NASA's Curiosity rover landed on Mars to assess its potential as a habitat for

138 lls that attack bacterial membranes and upon landing on phospholipid bilayers instantaneously (second

139 ionally variable, depending on surface type (land or ocean) and surrounding continental configuration

140 and, protection in the ocean, restoration on land, or restoration in the ocean-to maximise the extent

141 because of higher quality prey on irrigated lands, or earlier prey abundance may release former cons

142 s may preferentially track prey in irrigated lands over non-irrigated lands because of higher quality

143 rget genes has been largely conserved during land plant evolution, with evidence of lineage-specific

144 f stomatal development and patterning across land plant evolution.

145 ements to correspond to the needs of various land plant groups over the past 400 million years.

146 s (mitogenomes) are available from all major land plant lineages except ferns.

147 ey arose independently across newly evolving land plant lineages has long been a matter of debate.

148 DNA barcodes (rbcL + matK) for about 15% of land plant species and that comprehensive species covera

149 tomatal development in model dicot and basal land plant species.

150 quired to gain insight into the evolution of land plant stomatal responses.

151 A new study finds that, in an ancient land plant, growth rate variation patterned by meristema

152 on tolerant spores, evolved in the ancestral land plant.

153 from symbiosis in the roots of the 80-90% of land plants able to develop rhizobial and/or mycorrhizal

154 constriction of the cortex inward, cells of land plants divide by initiating a new cell-wall segment

155 Early diverging land plants do not form lignin, but already have element

156 Land plants evolved from an ancestral charophycean alga

157 is result implies that, at the global scale, land plants have regulated their stomatal conductance so

158 We conclude that land plants inherited two Pi uptake mechanisms - mediate

159 cation within the charophyte sister group to land plants led to distinct Class I and Class II KNOX ge

160 In land plants several transporters are involved in ion and

161 for fertilization in both animals and early land plants such as bryophytes and pteridophytes.

162 ering-negative feedback and the expansion of land plants that together ensured Earth's long-term habi

163 y were established in the common ancestor of land plants, but the 24-nucleotide siRNA pathway that gu

164 s from streptophyte algae, sister species to land plants, instead use phycocyanobilin (PCB).

165 In land plants, several exocyst subunits are encoded by dou

166 of glaucophytes, red algae, green algae, and land plants, share a common ancestor that lived approxim

167 ganic material through the photosynthesis of land plants-may provide a negative feedback for climate

168 vity and intensified weathering by the first land plants.

169 A families as well as small RNA machinery in land plants.

170 a crucial barrier on the aerial surfaces of land plants.

171 perate in parallel in extant early diverging land plants.

172 can be far more productive than other living land plants.

173 mplications for nutrient and carbon cycling, land productivity and in turn, worldwide socio-economic

174 ally the most cost-effective action; and (4) land protection should be prioritised if the catchment i

175 ternative conservation actions-protection on land, protection in the ocean, restoration on land, or r

176 that potential, using data from state-level land registries (CAR) in Para and Mato Grosso that were

177 The government claims that a new national land registry (SICAR), introduced under the revised law,

178 cioeconomic stress with increased hereditary land sales, and the issuance of priestly decrees to rein

179 sumption of animal-based products, decreases land scarcity, prevents emissions leakage, and concentra

180 a view to estimate PFAS mass budgets at the land-sea interface.

181 dust emissions (29%) moderate the wintertime land-sea surface air temperature difference and further

182 med at bridging knowledge gaps regarding the land-sea transport of per- and polyfluoroalkyl substance

183 mate change mitigation policies that involve land-sector C accounting.

184 e contrasting strategies of land sparing and land sharing has suggested that land sparing-combining h

185 yield agriculture and thus fare better under land sharing.

186 been a weathering fluid interacting with dry-land silicate rocks.

187 obial respiration to biomass C ratio in bare land soils confirmed environmentally induced stress.

188 Research into the contrasting strategies of land sparing and land sharing has suggested that land sp

189 The benefits of land sparing for both biodiversity and carbon storage su

190 sparing and land sharing has suggested that land sparing-combining high-yield agriculture with the p

191 The most landed species are crustaceans such as rose shrimp and N

192 sea level rise results from a combination of land subsidence, which has long been known to be present

193 mosphere, oceans, and across the terrestrial land surface are not only driving species to extinction,

194 ults highlight the significance of realistic land surface conditions on numerical prediction of initi

195 In turn, biocrust community shifts affect land surface cover and roughness-changes that can dramat

196 level ozone ([O3 ]) over much of the Earth's land surface have more than doubled since pre-industrial

197 one-tenth of the ice-free land surface is under intense human management, half und

198 nvergence-induced soil moisture variation to land surface models (LSM) can help explain spatial patte

199 The development of first-generation land surface models as a unifying framework for ecophysi

200 ata, reanalysis, satellite observations, and land surface models, we find that the heat wave included

201 Cryogenic land surface processes (LSPs) control landscape developm

202 defined as the total flux of water from the land surface to the atmosphere, is a major component of

203 of the world's plant species in c. 7% of the land surface.

204 allow for more rapid transport of MtBE from land-surface releases.

205 tion of the modeling, Earth observation, and land system science communities is thus required to achi

206 comprise availability of biomass and arable land, technology- and system-specific capacities, and re

207 sition that could take place in the no-man's land, the temperature-pressure window in which homogeneo

208 nce productivity and SOC storage in degraded lands through improved management practices.

209 It is more difficult (that is, requires more land) to maximize basic representation of the global bio

210 ution and their relations with anthropogenic land transformation are scarcer.

211 ns for interpreting geodetic measurements of land uplift and gravity changes in northern Greenland.

212 Changes in land use and climate, nitrogen deposition and invasive s

213 laria transmission is influenced by climate, land use and deliberate interventions.

214 roecosystems and is dependent on patterns of land use and fragmentation.

215 tically quantify these losses in relation to land use and greenhouse gas (GHG) emissions associated w

216 l gap given (i) profound reconfigurations in land use and land control over the past several decades

217 However, at the local scale, land use and land cover (LULC) change strongly affects t

218 Understanding their role on historical land use and land cover change (LULCC) and on the carbon

219 are experiencing unprecedented high rates of land use and land cover change.

220 Land use and land-use changes (LULUC) information is ess

221 udy of how changes in urban form and related land use and transportation policies impact urban air po

222 Our results suggest land use and vegetation cover type, as opposed to rock p

223 e conclude that pesticides from agricultural land use are a major threat to small streams and their b

224 The aquatic impacts of anthropogenic land use are often first observed in stream benthic biof

225 Changes in precipitation and land use are therefore more likely to govern biomass and

226 Changes in land use are thought to be driving the rise in reported

227 Importantly, the area of intensively managed land use around monitoring sites appears to influence th

228 Overall, a history of BT release and land use associated with urbanization have led to higher

229 greenhouse gases (GHGs), eutrophication, and land use because these have impacts reaching or exceedin

230 Human activity and related land use change are the primary cause of accelerated soi

231 Anthropogenic land use change is an important driver of impacts to bio

232 re pollination limitation is most severe and land use change is rapid.

233 nt regulators of community disassembly under land use change.

234 ed these changes occurred within one year of land use change.

235 , we noticed that the major discrepancies in land use changes among the three maps were as a result o

236 he contrasting effects of climate change and land use changes could explain why the predicted enrichi

237 ails and the conversion types for historical land use changes, the majority of historical land use re

238 oad scale representations of change in major land use classes impact modelled future distribution pat

239 A land use conversion experiment showed these changes occu

240 Anthropogenic land use had negative effects on the persistence of seve

241 m water and biofilms caused by anthropogenic land use had severe impacts on the nitrogen cycle in str

242 Grazing is the primary land use in the Hulunber meadow steppe.

243 The results showed that anthropogenic land use increased nutrient and organic carbon in both s

244 Historical land use information is essential to understanding the i

245 ted northern hardwood species indicates that land use may mask species range shifts caused by changin

246 systems and are profoundly influenced by the land use of the surrounding landscape.

247 used the model-derived estimates to identify land use patterns and characteristics of the street netw

248 Analysis of land use patterns of riparian zone in the cold and hot s

249 arge land areas have lost SOC as a result of land use practices, yet there are compensatory opportuni

250 hat a higher degree of uncertainty exists in land use projections than currently included in climate

251 land use changes, the majority of historical land use reconstructions do not sufficiently meet the re

252 emical transport models, and satellite-based land use regression models to estimate neighborhood annu

253 ion differed significantly between all three land use types, as did phylogenetic composition.

254 oduction and consumption of animal products, land use under organic agriculture remains below the ref

255 depth (AOD) data, meteorological fields, and land use variables to estimate daily 24 h averaged groun

256 hronous demographic responses to climate and land use, and the return of red spruce to lower elevatio

257 e investigated the influence of agricultural land use, catchment size, as well as precipitation and s

258 mulated without static snapshots of historic land use, taken at a single point in time.

259 ons as well as with soil characteristics and land use.

260 vironmental pressures such as high-intensity land use.

261 ge and biodiversity impacts due to water and land use.

262 based sample data from the European Union's Land Use/Cover Area frame statistical Survey (LUCAS) soi

263 the impact of anthropogenic modification of land use/cover on the temporal dynamics of environmental

264 ver the last two centuries due to historical land-use and climate change.

265 e the environmental impacts of anthropogenic land-use and conversion.

266 of inconsistencies in the classification of land-use categories during the study period, rather than

267 ell in the spatial reconstruction of various land-use categories, and had a higher figure of merit (4

268 This stored carbon is vulnerable to land-use change and any future reduction in precipitatio

269 Third, by modeling increased land-use change and resultant shifts in fish community c

270 g of land change and ecosystem services in a Land-Use Change Improved (LUCI)-LCA.

271 Land-use change is one of the primary drivers of species

272 Alternatively, land-use change might overwhelm natural buffering and am

273 erently regarding the type of scenarios, but land-use change was an important driver of vegetation ch

274 vestigation correlating temporal patterns of land-use change with the demographic rates of mule deer,

275 including those resulting from anthropogenic land-use change, are underrepresented in species distrib

276 Land use and land-use changes (LULUC) information is essential to det

277 Climatic, atmospheric, and land-use changes all have the potential to alter soil mi

278 ed in forested tropical regions experiencing land-use changes and where wildlife biodiversity (mammal

279 mbined with data from permanent monitors and land-use data into seasonally adjusted land-use regressi

280 Thus both land-use decisions and aerosols are important factors go

281 an zone in the cold and hot spots found that land-use patterns had an important effect on riparian co

282 t broad-scale climate combined with changing land-use regimes are causal factors in species' range sh

283 Land-use regression (LUR) models are useful for resolvin

284 e largest relative risk was observed for the land-use regression model that included traffic informat

285 s and land-use data into seasonally adjusted land-use regression models.

286 into how other societal outcomes vary across land-use strategies.

287 across the soils despite the differences in land-use.

288 luding solar energy, presents trade-offs for land used for the production of food and the conservatio

289 Industrial-scale development introduces new land uses into the landscape, with unknown repercussions

290 al C:N:P ratios), itself linked to different land uses, and secondarily driven by other important bio

291 Land vertebrates have returned to the ocean several time

292 sually acquire the targets immediately after landing was 7-10% (30-34 ms) slower than mean preflight

293 Advanced SoGS in irrigated lands was related to earlier planting of crops after rel

294 for genotypic sex determination facilitating land-water transitions in amniotes.

295 lder muscles and responses to reloading upon landing were rapid.

296 e a substance from their tarsi wherever they land, which can be detected by conspecifics.

297 restoration of natural habitats on nonfarmed land-will have lower environmental impacts than other st

298 r (Populus), which will be grown on marginal lands with little or no water input.

299 wastage and food-competing feed from arable land, with correspondingly reduced production and consum

300 Life on land would have selected for the precise traits that now