ライフサイエンスコーパス: anthropogenic

1 origin of these genes is local and possibly anthropogenic.

2 tracer studies using the transient signal of anthropogenic (236)U.

3 Anthropogenic activities contribute benzene, toluene, an

4 Anthropogenic activities have led to large-scale mercury

5 e find that increased aerosol loading due to anthropogenic activities in China substantially increase

6 Anthropogenic activities resulting in releases of seleni

7 Anthropogenic activities since the industrial revolution

8 r, they indicate that, without intervention, anthropogenic activities will soon precipitate a double

9 only have to contend with increasing coastal anthropogenic activities, but also have to adapt to larg

10 nadium, an important pollutant produced from anthropogenic activities, has been suggested to be embry

11 c tundra soil with limited/no connections to anthropogenic activities.

12 ame extinct during the 17(th) century due to anthropogenic activities.

13 hese highly stressed systems from a range of anthropogenic activities.

14 that vertical land motion induced by recent anthropogenic activity and glacial isostatic adjustment

15 Much of the geochemical record of recent anthropogenic activity has been eroded and lost at the H

16 diometric, isotopic and elemental records of anthropogenic activity have been retained in the Hythe m

17 /phosphorus (P) have changed dramatically as anthropogenic additions of N or P are not matched by Si.

18 Anthropogenic Aerosols (AA) have slowed down the warming

19 We demonstrated that the signal was anthropogenic and attributed to a combination of plastic

20 Interactions between anthropogenic and biogenic emissions, and implications f

21 The combined effects of anthropogenic and biological CO2 inputs may lead to more

22 0th century, reflecting interactions between anthropogenic and ecological forces.

23 reas is likely to depend on a combination of anthropogenic and environmental factors, with anthropoge

24 W seepage, but conclusive differentiation of anthropogenic and natural sources remained difficult.

25 us boron reservoir with possible but limited anthropogenic and/or biogenic contributions.

26 Elevated levels of geogenic and anthropogenic arsenic are found along many coasts around

27 amplitude of change suggests that, by 2010, anthropogenic atmospheric N deposition represented 20 +/

28 atter, which signals increased deposition of anthropogenic atmospheric N on the open ocean and its in

29 zation of nitrogen (N)-limited ecosystems by anthropogenic atmospheric nitrogen deposition (Ndep) may

30 r capability of crossing through natural and anthropogenic barriers, even reaching drinking water.

31 0 times higher than that of BC, we find that anthropogenic BC causes the majority (60% on average) of

32 emission sources have not been exploited for anthropogenic-biogenic interaction studies until now.

33 )C(16)O) represent an integrated signal from anthropogenic/biogeochemical processes, including fossil

34 Here we estimate the contribution of anthropogenic black carbon (BC) to snowmelt in glacier a

35 ction in seawater pH due to rising levels of anthropogenic carbon dioxide (CO2) in the world's oceans

36 Acidification of seawater caused by anthropogenic carbon dioxide (CO2) is anticipated to inf

37 The ocean is the largest sink for anthropogenic carbon dioxide (CO2), having absorbed roug

38 From 1890 to 2015, anthropogenic carbon dioxide emissions have increased at

39 Less than half of anthropogenic carbon dioxide emissions remain in the atm

40 est carbon sink and its capacity to mitigate anthropogenic carbon emissions may be stronger, but also

41 is responsible for around one tenth of total anthropogenic carbon emissions, and tropical protected a

42 Sole anthropogenic causes for particular variations in the CO

43 cosystems, and the potential implications of anthropogenic change to fundamentally alter these proces

44 stocks in British semi-natural landscapes to anthropogenic change.

45 Understanding how anthropogenic changes alter community composition and fu

46 The effects of anthropogenic changes in Lake Superior, which is Earth's

47 It is hypothesized that rapid evolution to anthropogenic changes may alter fundamental physiologica

48 climate simulations forced with natural and anthropogenic changes, but is inconsistent with simulati

49 facing an unprecedented set of comprehensive anthropogenic changes.

50 It is well established that anthropogenic chlorine-containing chemicals contribute t

51 of tropical flower phenology in response to anthropogenic climate and atmospheric change.

52 In the context of anthropogenic climate change and habitat degradation, th

53 tered precipitation patterns associated with anthropogenic climate change are expected to have many e

54 Anthropogenic climate change compromises reef growth as

55 Anthropogenic climate change has emerged as a critical e

56 Anthropogenic climate change has the potential to alter

57 derable uncertainty surrounds the impacts of anthropogenic climate change on the composition and stru

58 mechanistic basis to project the effects of anthropogenic climate change on tuna habitats.

59 The salient feature of anthropogenic climate change over the last century has b

60 There is growing empirical evidence that anthropogenic climate change will substantially affect t

61 atistical analyses to compare the effects of anthropogenic climate change with the effects of natural

62 perature variations, which may be induced by anthropogenic climate change, are often associated with

63 tland carbon stocks are highly threatened by anthropogenic climate change, including drought, which l

64 e contested issues, such as the existence of anthropogenic climate change, public opinion is polarize

65 dentified as a major, ongoing contributor to anthropogenic climate change, thus making historical emi

66 o concern about the response of parasites to anthropogenic climate change.

67 ic thermal acclimation regimes and potential anthropogenic climate change.

68 sease outbreaks, both of which are linked to anthropogenic climate change.

69 for avoiding the most devastating impacts of anthropogenic climate change.

70 rongest and most widespread contributions of anthropogenic climate forcing occur in the tropics, incl

71 ger ice-free periods in Lake Superior due to anthropogenic climate warming.

72 transformation of CO2 not only mitigates the anthropogenic CO2 emission into the Earth's atmosphere b

73 risks of protein deficiency attributable to anthropogenic CO2 emissions by 2050.

74 orage (CCS) technologies that seek to offset anthropogenic CO2 emissions into the atmosphere by buryi

75 Anthropogenic CO2 emissions threaten the adequacy of pro

76 ay turn into net CO2 sources under continued anthropogenic CO2 emissions.

77 Anthropogenic CO2 is expected to drive ocean pCO2 above

78 sensitivity, to detect localized natural and anthropogenic CO2 sources.

79 edict the future of the terrestrial sink for anthropogenic CO2(1) .

80 , but ultimately may limit oceanic uptake of anthropogenic CO2.

81 isual Environments to assess the patterns in anthropogenic combustion ratios (DeltaECa/DeltaCO and De

82 en fewer measurements have examined BrC from anthropogenic combustion sources like motor vehicle emis

83 Overall, anthropogenic communities are not diminished subsets of

84 nces (PFASs) are persistent, bioaccumulative anthropogenic compounds associated with adverse health i

85 miles downstream of the WWTP, implying that anthropogenic compounds were not fully removed or degrad

86 Designed-bioactive anthropogenic contaminants (biocides, pharmaceuticals) c

87 this population: reduced prey availability, anthropogenic contaminants, and marine vessel disturbanc

88 able abundance to some of the most important anthropogenic contaminants, such as the halogenated flam

89 enriched in Mo, and thus present a potential anthropogenic contamination source.

90 /L), and elevated levels are associated with anthropogenic contamination, although geogenic sources h

91 We find earliest anthropogenic Cu pollution during the Early Horizon peri

92 osystem processes are sensitive to increased anthropogenic degradation but biotic communities provide

93 sources of environmental disturbance, namely anthropogenic destruction of natural habitats and wildfi

94 Land-use change due to anthropogenic development is pervasive across the globe

95 s can be used in consenting and licensing of anthropogenic developments to determine local abundance.

96 The anthropogenic disruption of hydrological habitat connect

97 es is critical for evaluating the impacts of anthropogenic disturbance on physiology and fitness, key

98 ses, has been linked to different sources of anthropogenic disturbance.

99 secondary grasslands, the latter created by anthropogenic disturbance.

100 s than urban parks that are under continuous anthropogenic disturbance.

101 However, anthropogenic disturbances are altering the abundance an

102 s began ca. 165 ya (around 1850) after major anthropogenic disturbances ceased.

103 sessing community-level effects of potential anthropogenic-driven mass mortality events, owing to the

104 h for assessing impacts of environmental and anthropogenic drivers in wild animal populations.

105 models, and (iii) identify environmental and anthropogenic drivers using ANOVAs.

106 es of ecoevolutionary change have focused on anthropogenic drivers, but none of these studies has spe

107 re degrading rapidly in response to numerous anthropogenic drivers.

108 While bimodality can hence be explained by anthropogenic edge effects and natural spatial heterogen

109 These observations demonstrate that anthropogenic effects have become a prominent influence

110 t midlatitudes and is strongly determined by anthropogenic effects, most notably the number of specie

111 and the possibility that weak, low-frequency anthropogenic electromagnetic fields may have biological

112 A ratio-based method is used to characterize anthropogenic elemental carbon (ECa) using in situ measu

113 Despite active research in this area, real anthropogenic emission sources have not been exploited f

114 Although recent increases in anthropogenic emissions are the main factor causing haze

115 remain present for more than 200 y, even if anthropogenic emissions cease altogether, despite the 10

116 sol fields and increased importance of local anthropogenic emissions in dictating aerosol burdens.

117 ations and a dispersion model, coupled to an anthropogenic emissions inventory and a fire emissions i

118 Regional and national reductions in anthropogenic emissions of aerosol precursors are leadin

119 produce approximately 20 per cent of global anthropogenic emissions of nitrogen oxides (NOx), which

120 Anthropogenic emissions of the toxic heavy metal mercury

121 ion of isoprene SOA is influenced largely by anthropogenic emissions through multiphase chemistry of

122 lands are caused by human activity, they are anthropogenic emissions, and reducing them will have an

123 orth America can be attributed to East Asian anthropogenic emissions, compared with 0.7 ppbv using th

124 ganic aerosol can be explained by changes in anthropogenic emissions, primarily from vehicle emission

125 In addition to anthropogenic emissions, the winter aerosol pollution ov

126 ection Agency regulations continue to reduce anthropogenic emissions, wildland fire emissions will be

127 eposition predating the onset of large-scale anthropogenic emissions.

128 ess the impact of meteorology under constant anthropogenic emissions.

129 pproach in understanding the consequences of anthropogenic environmental change on natural population

130 ially concerning within the context of rapid anthropogenic environmental change.

131 Anthropogenic environmental changes are accelerating the

132 nthropogenic and environmental factors, with anthropogenic factors affecting the number of species in

133 onmental, agricultural, epidemiological, and anthropogenic factors are implicated in RVF spread, the

134 e seasonality of diseases, the importance of anthropogenic factors is less commonly evaluated.

135 Environmental and anthropogenic factors often drive population declines in

136 esents quantitative analysis of climatic and anthropogenic factors to streamflow alteration in the Ta

137 overflow (WWF) can be broadly influenced by anthropogenic factors, such as nonpoint sources of paved

138 A nonmodeled anthropogenic feature was also indicated.

139 to 2015 to inventory sources of natural and anthropogenic fecal indicator bacteria (FIB).

140 ate, or perfluorooctane sulfonic acid) is an anthropogenic fluorosurfactant widely used in consumer p

141 out of urban spaces that contain high-energy anthropogenic food sources.

142 These results suggest that anthropogenic forces can dramatically reshape equid gast

143 ns may be paralleled in mammals subjected to anthropogenic forces such as domestication and captivity

144 e size and the rate of response to continued anthropogenic forcing and the magnitude and phasing of i

145 torical climate model simulations subject to anthropogenic forcing display an increase in the project

146 increased in recent decades, consistent with anthropogenic forcing driving enhanced Saharan warming.

147 d extremely high statistical confidence that anthropogenic forcing increased the probability of recor

148 risk to human health and also contribute to anthropogenic forcing of climate.

149 changing, and if so, whether this is due to anthropogenic forcing, are subjects of ongoing debate.

150 pendent, abrupt and enhanced response to the anthropogenic forcing, at the same time that the last gl

151 M, which remains significant with or without anthropogenic forcing.

152 pon the response of natural climate modes to anthropogenic forcing.

153 lyphs; however, construction occurred within anthropogenic forest that had been actively managed for

154 ich could influence C storage under combined anthropogenic global change drivers.

155 ination with exposure to the longer-duration anthropogenic global change factors, influenced the dyna

156 nternal variability on changes in ENSO under anthropogenic global warming using the Community Earth S

157 SLR), a well-documented and urgent aspect of anthropogenic global warming, threatens population and a

158 Our results imply that anthropogenic greenhouse forcing may be driving an incre

159 Methane is the second strongest anthropogenic greenhouse gas and its atmospheric burden

160 ng interest in those ecosystems as sites for anthropogenic greenhouse gas emission offset projects (s

161 Mitigation of anthropogenic greenhouse gases with short lifetimes (ord

162 e response of the H2 soil sink to changes in anthropogenic H2 emissions and shifting soil conditions

163 opulation declines in the face of concurrent anthropogenic habitat and climate change.

164 adient, potentially concurrent with Holocene anthropogenic habitat conversion for agriculture.

165 onary timescale should not be conflated with anthropogenic habitat loss or degradation when consideri

166 g wildlife with particular trait profiles in anthropogenic habitats to reduce infectious disease risk

167 Rather, forest species do not persist in anthropogenic habitats, but are replaced by different na

168 ) EEM-PARAFAC fitted terrestrial humic-like, anthropogenic humic-like, tryptophan-like, and tyrosine-

169 se in delta(15)N values is evidence of early anthropogenic impact in Chesapeake Bay.

170 ecosystems is increasingly difficult because anthropogenic impacts are pervasive and accelerating.

171 scale nitrogen budgets developed to quantify anthropogenic impacts on the nitrogen cycle do not expli

172 Understanding the combined effects of anthropogenic impacts such as climate change and polluti

173 lines due to global climate change and local anthropogenic impacts.

174 he concentrations of ibuprofen and caffeine, anthropogenic indicators of untreated wastewater dischar

175 citation-emission matrix (EEM) measurements, anthropogenic influence of a wastewater treatment plant

176 There is an urgent need to quantify anthropogenic influence on forest carbon stocks.

177 pected for a species with such strong, known anthropogenic influence.

178 m non-tectonic processes, either natural and anthropogenic, influence the occurrence of earthquakes i

179 lecules but first reported here in a natural/anthropogenic-influenced system-offers exciting insight

180 of the selected USA aquifers, a decrease in anthropogenic influences by 20% may change the conditio

181 erstanding of soil feedbacks to the combined anthropogenic influences of climate change and nitrogen

182 This study focused on the anthropogenic influences of the paved runoff and sanitar

183 s and consumer populations are among the top anthropogenic influences on ecosystems.

184 explores a general framework for quantifying anthropogenic influences on groundwater budget based on

185 ts in combination with other longer-duration anthropogenic influences on the dynamics of soil carbon

186 itigated or even reversed in the presence of anthropogenic influences.

187 50% for P, and 83% for Gd), indicating large anthropogenic inputs via the wastewater stream.

188 omogeneous prior to large-scale 20th century anthropogenic inputs, this evidence suggests a relativel

189 ributed either to predominant geogenic or to anthropogenic inputs.

190 of their evolution and their relations with anthropogenic land transformation are scarcer.

191 treams flowing through forest (upstream) and anthropogenic land use (downstream) areas in southwester

192 The aquatic impacts of anthropogenic land use are often first observed in strea

193 Anthropogenic land use change is an important driver of

194 Anthropogenic land use had negative effects on the persi

195 both the stream water and biofilms caused by anthropogenic land use had severe impacts on the nitroge

196 The results showed that anthropogenic land use increased nutrient and organic ca

197 lty development due to the contribution from anthropogenic land-cover changes.

198 al to determine the environmental impacts of anthropogenic land-use and conversion.

199 d vegetation, including those resulting from anthropogenic land-use change, are underrepresented in s

200 nto eastern North America was facilitated by anthropogenic landscape changes and followed two broad e

201 Anthropogenic landscapes are associated with biodiversit

202 not detectably different between natural and anthropogenic landscapes, but community phenologies diff

203 This raises the possibility that anthropogenic LMH declines might interact with changing

204 Whether anthropogenic mixing of marine Bacteria restructures the

205 is essential to understanding the impact of anthropogenic modification of land use/cover on the temp

206 ns from sites experiencing elevated rates of anthropogenic N deposition but varying in soil N availab

207 ic matter accumulating under future rates of anthropogenic N deposition could remain in soil for long

208 our experiment, then unabated deposition of anthropogenic N from the atmosphere has the potential to

209 communities may be particularly sensitive to anthropogenic N inputs.

210 may be compounded by other drivers, such as anthropogenic nitrogen (N) deposition and nonnative plan

211 t marshes play a key role in removing excess anthropogenic nitrogen (N) loads to nearshore marine eco

212 Anthropogenic nitrogen sources become more important in

213 Anthropogenic noise across the world's oceans threatens

214 ontinental-scale sound models, we found that anthropogenic noise doubled background sound levels in 6

215 eas with more stringent regulations had less anthropogenic noise.

216 ld decrease by 20-30% in the absence of U.S. anthropogenic NOx emissions.

217 kalinity data from the Chesapeake Bay, where anthropogenic nutrient inputs have led to eutrophication

218 al ecosystems are experiencing high rates of anthropogenic nutrient inputs.

219 hydrate dissociation, possibly triggered by anthropogenic ocean warming.

220 res in Antarctica in the last decades) is of anthropogenic or natural origin is of great importance f

221 We estimate that the decrease in anthropogenic organic aerosol is responsible for avertin

222 The 10 most-frequently detected anthropogenic-organics included eight pesticides (desulf

223 discovered in a quest for biodegradation of anthropogenic organohalogens, these organohalide-respiri

224 es data revealed more than 13000 profiles of anthropogenic origin in both lakes, defining the beginni

225 Historical sources suggest an anthropogenic origin of this badland landscape, caused b

226 onmental conditions may be natural and/or of anthropogenic origin, and may interface with cancer risk

227 ially considered to be of almost exclusively anthropogenic origin.

228 compounds were the most abundant classes of anthropogenic origin.

229 esults suggest a significant contribution of anthropogenic P deposition to C storage, and additional

230 According to our results, the low level of anthropogenic particles intake from the salts (maximum 3

231 n extraction protocols are needed to isolate anthropogenic particles smaller than 149 mum.

232 tituted a mix of background (natural) Pb and anthropogenic Pb inputs from preceding decades.

233 roduct of coal combustion and is a source of anthropogenic PM with worldwide health relevance.

234 fluoroalkyl substances (PFAS) are ubiquitous anthropogenic pollutants almost universally detected in

235 from both domestic and foreign emissions of anthropogenic precursors.

236 e with geographical differences in levels of anthropogenic pressure and conservation effort.

237 lumn and fish gut) in a coastal lagoon under anthropogenic pressure.

238 nitoring to reconstruct the impacts of major anthropogenic pressures and to identify meaningful tempo

239 This study reveals that anthropogenic pressures can induce decoupled effects bet

240 Anthropogenic pressures continue to squeeze available ha

241 iated late in the 20(th) century, well after anthropogenic pressures had already reached half of thei

242 These findings reinforce the potential for anthropogenic pressures to shape the landscape epidemiol

243 antly with areas currently under significant anthropogenic pressures, they also include much of the M

244 and compare those with the rise of important anthropogenic pressures.

245 restimate the full range of impacts of major anthropogenic pressures.

246 Together, these anthropogenic processes reduce the connectivity of popul

247 on and interpreting recent changes driven by anthropogenic processes.

248 the relative influence of these natural and anthropogenic processes.

249 heric circulation, and climate's response to anthropogenic radiative forcings.

250 d is still receiving a considerable input of anthropogenic radionuclides from nuclear reprocessing fa

251 The finding that anthropogenic rather than environmental factors are the

252 in stabilizing climate even with increasing anthropogenic release of CO2 .

253 ther in near surface environments, or due to anthropogenic releases from waste rich in antimony, a co

254 The spatio-temporal anthropogenic rescaling (STAR) hypothesis suggests that

255 ral and external forcings (e.g., natural and anthropogenic) responsible for ST variability are studie

256 ted halogenation of a variety of natural and anthropogenic seawater organics may be a significant pro

257 warmer temperatures is less compromised when anthropogenic sedimentation is maintained at the lowest

258 n in fall 2015 was undertaken to monitor for anthropogenic seepage while also considering natural sou

259 the established natural baselines and other anthropogenic signals.

260 sing China as the world's largest emitter of anthropogenic SO2.

261 tracers, representing different natural and anthropogenic sources and geochemical behaviors, were us

262 Manganese oxides from anthropogenic sources can promote the formation of sulfa

263 tigation efforts typically focus on reducing anthropogenic sources of mortality.

264 sults of our study suggest that reduction of anthropogenic sources of NOx, VOCs, and PM, for example,

265 Anthropogenic sources of PHCZs may exist, particularly f

266 d to understand contributions of natural and anthropogenic sources to the total fine particulate carb

267 4% of the BC is emitted from mostly regional anthropogenic sources while the remaining contribution c

268 ic compounds (VOCs) emitted from natural and anthropogenic sources, chemical composition measurements

269 in field studies might have originated from anthropogenic sources, such as photooxidation of hydroca

270 the coverage of species while accounting for anthropogenic stress.

271 Increasing effects of anthropogenic stressors and those of natural origin on a

272 Natural and anthropogenic stressors can cause phase shifts from cora

273 comprehensive model to quantify the roles of anthropogenic stressors on hydrologic alteration and bio

274 tem services, but are threatened by multiple anthropogenic stressors, including warming.

275 trajectories and the relative importance of anthropogenic stressors.

276 ients affect coral reefs isolated from other anthropogenic stressors.

277 following sublethal exposure to natural and anthropogenic stressors.

278 o reef-ecosystems maintenance, is altered by anthropogenic stressors.

279 ex mixtures of known and unknown natural and anthropogenic substances.

280 -2015 is not likely due to recent changes in anthropogenic sulfate aerosols.

281 ation likely represents another link between anthropogenic sulfate enrichment and MeHg production in

282 tresses experienced in microbial habitats or anthropogenic systems (with water-activities from 0.765

283 lass that is ubiquitous in nature as well as anthropogenic systems, as an example to demonstrate the

284 g systems compared with natural and nonurban anthropogenic systems.

285 Protected areas buffer species from anthropogenic threats and provide places for the process

286 c Ocean provides a data-rich case to explore anthropogenic threats on population viability.

287 rtunities and spatially explicit natural and anthropogenic threats that could affect key life-history

288 bility is the missing step in uncovering the anthropogenic trend in sea level and understanding the p

289 f the area are exposed to elevated levels of anthropogenic underwater sound, particularly due to comm

290 spaces and alteration of these spaces due to anthropogenic underwater sound.

291 imply a dynamic EAIS response with continued anthropogenic warming and suggest that the EAIS contribu

292 Ice Sheet will be governed more by long-term anthropogenic warming combined with multi-centennial nat

293 Because anthropogenic warming is expected to reduce northern hem

294 lar responses will likely mediate impacts of anthropogenic warming on biodiversity and ecosystem func

295 rming are comparable to those of the current anthropogenic warming, our measurements suggest that lar

296 similar to those anticipated with continued anthropogenic warming.

297 scale seepage reported here is not caused by anthropogenic warming.

298 tural climate variability well before recent anthropogenic warming.

299 e Ag(0) and Ag2S nanoparticles (NPs) through anthropogenic waste streams.

300 anging climate, while explicitly considering anthropogenic water demand scenarios and water supply in