ライフサイエンスコーパス: nitrogen cycle

1 rchaea that plays a major role in the global nitrogen cycle.

2 endence on climate-driven differences in the nitrogen cycle.

3 al mitigation of anthropogenic impact on the nitrogen cycle.

4 n denitrification and other processes of the nitrogen cycle.

5 do not necessitate a revision to the global nitrogen cycle.

6 gradation is an important step in the marine nitrogen cycle.

7 s interval as a key transition in the marine nitrogen cycle.

8 onment resulting in severe disruption of the nitrogen cycle.

9 cts or dependence of economic sectors on the nitrogen cycle.

10 atter is an important feature of the aquatic nitrogen cycle.

11 economic activities and various flows in the nitrogen cycle.

12 habitats, necessitates a reassessment of the nitrogen cycle.

13 x, denitrification) components of the marine nitrogen cycle.

14 stantial and hitherto overlooked role in the nitrogen cycle.

15 xation, a crucial step in the biogeochemical nitrogen cycle.

16 ted an important role for them in the global nitrogen cycle.

17 tion of fixed nitrogen to the biogeochemical nitrogen cycle.

18 e role of ozone in the atmosphere's reactive nitrogen cycle.

19 important implications for the global ocean nitrogen cycle.

20 , leading to an imbalance in the terrestrial nitrogen cycle.

21 management in agriculture and in the Earth's nitrogen cycle.

22 ments and plays a central role in the global nitrogen cycle.

23 previously unrecognized, role in the global nitrogen cycle.

24 p plants and a cornerstone in the biological nitrogen cycle.

25 conversion of nitrite to nitric oxide in the nitrogen cycle.

26 ve on nontarget organisms and the ecological nitrogen cycle.

27 archaea (AOA) play a key role in the aquatic nitrogen cycle.

28 tentially contributing notably to the global nitrogen cycle.

29 waste nitrate to ammonia and help close the nitrogen cycle.

30 promising approach to closing the artificial nitrogen cycle.

31 ) to NO during denitrification in the global nitrogen cycle.

32 e primary perturbation of the 21(st) century nitrogen cycle.

33 denitrifying bacterium of importance in the nitrogen cycle.

34 rably causing inefficient utilization of the nitrogen cycle.

35 complex chemistry of the enzymes used in the Nitrogen Cycle.

36 cient ecology in the formation of the modern nitrogen cycle.

37 an important intermediate in the atmospheric nitrogen cycle.

38 d thus impacts air quality, climate, and the nitrogen cycle.

39 heme-catalyzed NO(x) interconversions in the nitrogen cycle.

40 pe of coupling between known pathways in the nitrogen cycle.

41 derstanding of the different pathways of the nitrogen cycle.

42 tribution of taxa that mediate the microbial nitrogen cycle.

43 ompelling evidence for a significant aerobic nitrogen cycle.

44 the emergence of a pervasive aerobic marine nitrogen cycle.

45 inking the reduced and oxidized sides of the nitrogen cycle.

46 to the chemical industry and to the Earth's nitrogen cycle.

47 ation dynamics impact directly on the global nitrogen cycle.

48 on ozone, other oxidants, aerosols, and the nitrogen cycle.

49 ine N(2) fixation and its role in the global nitrogen cycle.

50 while implying a more important role for the nitrogen cycle.

51 dvance with the introduction of a prognostic nitrogen cycle.

52 the metabolic intersection of the carbon and nitrogen cycles.

53 es; they play key roles in global carbon and nitrogen cycles.

54 occus and its role in the oceanic carbon and nitrogen cycles.

55 haeota may be important to global carbon and nitrogen cycles.

56 tinue to be key players in global carbon and nitrogen cycles.

57 nificant threats to water quality and global nitrogen cycles.

58 M) plays a key role in the global carbon and nitrogen cycles.

59 play an important role in marine carbon and nitrogen cycles.

60 of organic matter and subsequent carbon and nitrogen cycling.

61 wildly different effects on ecosystem-level nitrogen cycling.

62 ated the expression of genes associated with nitrogen cycling.

63 to be significant contributors to carbon and nitrogen cycling.

64 trogen, and sulfur assimilation, and aerobic nitrogen cycling.

65 d properties, ultimately increasing rates of nitrogen cycling.

66 the microbial communities involved in global nitrogen cycling.

67 significant consequences for biogeochemical nitrogen cycling.

68 is typically low in nitrogen, and in global nitrogen cycling.

69 ich suggests a practical approach for carbon-nitrogen cycling.

70 ations in metabolic pathways associated with nitrogen cycling.

71 iers play crucial roles in global carbon and nitrogen cycling.

72 and many play a critical role in carbon and nitrogen cycling.

73 s, significantly impacting global carbon and nitrogen cycling.

74 nique biogeochemical conditions that promote nitrogen cycling.

75 anding climate change effects on legumes and nitrogen cycling.

76 vative resource-use strategies and slow soil nitrogen cycling.

77 robe-mediated biogeochemical cycles, such as nitrogen cycling.

78 ecosystem carbon use efficiency, and altered nitrogen cycling.

79 limate alteration can affect both carbon and nitrogen cycling.

80 ))-makes them important mediators of benthic nitrogen cycling.

81 lta(15)NNO3 and delta(18)ONO3 to investigate nitrogen cycling.

82 or the microorganisms that govern carbon and nitrogen cycling.

83 important in understanding marine carbon and nitrogen cycling.

84 y of soils and how the disruption influences nitrogen cycling.

85 ty, 32-42% for carbon cycling and 31-41% for nitrogen cycling.

86 e biogeochemical models in simulating global nitrogen cycling.

87 n had a measurable effect on ecosystem-scale nitrogen cycling.

88 izing archaeon that is crucial to the global nitrogen cycle(1,2).

89 modern marine sediments, signify an aerobic nitrogen cycle ~100 My earlier than previously accepted.

90 eric oxidation and interacts with the global nitrogen cycle(4-8).

91 d in regulating the global marine and limnic nitrogen cycles [5, 6].

92 aded biodiversity(3,4), disrupted carbon and nitrogen cycles(5,6) and added prodigious quantities of

93 (1) Whether this surprising stimulation of nitrogen cycling activities reflects the need to generat

94 ne environments, potentially restricting the nitrogen cycle, affecting primary productivity, and limi

95 nitrogen, contributing significantly to the nitrogen cycle, agriculture and biogeochemical history o

96 Nitric oxide (NO) is an intermediate of the nitrogen cycle, an industrial pollutant, and a marker of

97 rd metabolism of Asn by the photorespiratory nitrogen cycle and accumulation of aromatic amino acids.

98 ) and N2O) are key components of the natural nitrogen cycle and are intermediates in a range of proce

99 Nitrite is a central intermediate in the nitrogen cycle and can persist in significant concentrat

100 century has resulted in a heavily imbalanced nitrogen cycle and consequently, the large-scale accumul

101 mium, is an integral component of the marine nitrogen cycle and contributes significant amounts of ne

102 ctions: in the first section, nitrate in the nitrogen cycle and human health, taxonomy of nitrate red

103 ng in the soil as part of the biogeochemical nitrogen cycle and in acidified nuclear waste.

104 ase may play a role in the global biological nitrogen cycle and iron-only nitrogenase may contribute

105 species involved in various pathways of the nitrogen cycle and is therefore indicative of numerous b

106 harshly contributed to the disruption of the nitrogen cycle and its consequences have severely affect

107 h process, and have not addressed the global nitrogen cycle and its environmental implications.

108 ata require that any explanation for the OAE nitrogen cycle and its isotopic values be consistent wit

109 enitrification - a key process in the global nitrogen cycle and main source of the greenhouse gas N(2

110 enges our understanding of a key step in the nitrogen cycle and masks our ability to distinguish betw

111 Furthermore, abundances of nitrogen cycle and phosphorus cycle genes were concomita

112 teria contribute significantly to the global nitrogen cycle and play a major role in sustainable wast

113 le strategy that simultaneously realizes the nitrogen cycle and resource integration.

114 key timepoint in the evolution of the marine nitrogen cycle and the oxidation of the Earth's surface

115 n offers a promising pathway for sustainable nitrogen cycles and hydrogen generation.

116 oil microbial activity drives the carbon and nitrogen cycles and is an important determinant of atmos

117 complete understanding of global carbon and nitrogen cycling and a reduction in the uncertainty of c

118 cterial and fungal groups that contribute to nitrogen cycling and a reproducible network of decompose

119 ce melt), which alter controls on carbon and nitrogen cycling and expose organic matter from meters b

120 influence over ecosystem processes, such as nitrogen cycling and fire regimes, is still largely unkn

121 minimum zones (OMZs) are critical to marine nitrogen cycling and global climate change.

122 ial-scale changes in climate, fire activity, nitrogen cycling and herbivore density in an Irish heath

123 Nitrogen cycling and hydrogen oxidation are likely to co

124 Biomass burning can alter soil nitrogen cycling and potentially influence soil NO fluxe

125 hich has implications for oceanic carbon and nitrogen cycling and raises questions regarding the evol

126 budgets, but also changes our view of global nitrogen cycling and the predicted impact of climate cha

127 und in denitrification enzymes of the global nitrogen cycle, and free HNO exhibits pharmacological pr

128 te through changes in biodiversity, climate, nitrogen cycle, and land use.

129 ecting an anthropogenic impact on the global nitrogen cycle, and the impact was thought to be amplifi

130 ) to ammonia (NH3), a key step in the global nitrogen cycle; and the reduction of carbon monoxide (CO

131 , because anthropogenic contributions to the nitrogen cycle are 100-200% compared with a contribution

132 Carbon and nitrogen cycles are coupled through both stoichiometric

133 ized form (as nitrate) is represented in the nitrogen cycle as a multiphasic process involving severa

134 ely recognized as an important player in the nitrogen cycle as well as one of the most abundant membe

135 Nitrogenase is a key player in the global nitrogen cycle, as it catalyzes the reduction of dinitro

136 bacteria, along with the prevalence of their nitrogen cycling-associated gene transcripts, suggested

137 Humans continue to transform the global nitrogen cycle at a record pace, reflecting an increased

138 ecifically, for the potential evolution of a nitrogen cycle at some point in martian history.

139 In the nitrogen cycle atmospheric nitrogen is fixated by bacter

140 ne (PEI) were more toxic to pure cultures of nitrogen-cycling bacteria than QDs coated with anionic p

141 There were many more nitrogen cycling Betaproteobacteria (e.g., Limnohabitans

142 Relatives of microbes involved in nitrogen cycling bloomed during times of ice cover as se

143 haumarchaeota are important organisms in the nitrogen cycle, but the mechanisms driving their radiati

144 fication have major effects on the microbial nitrogen cycle, but widespread ocean deoxygenation is pe

145 enase plays a crucial role in the biological nitrogen cycle by catalyzing the reduction of dinitrogen

146 em dominates anthropogenic disruption of the nitrogen cycle by generating excess fixed nitrogen.

147 Alteration of the global nitrogen cycle by man has increased nitrogen loading in

148 Planctomycetes play a key role in the global nitrogen cycle by releasing fixed nitrogen back to the a

149 a economy (30 EJ/y) could perturb the global nitrogen cycle by up to 65 Mt/y with a 5% nitrogen loss

150 Grasshoppers may speed up nitrogen cycling by changing the abundance and decomposi

151 onmental and energy challenge underlying the nitrogen cycle, by valorizing a pollutant to a carbon-fr

152 t composition, core symbiont functions (e.g. nitrogen cycling) can be maintained in sponge microbiome

153 by modeled NPP and autotrophic respiration, nitrogen cycle, carbon allocation, and soil moisture dyn

154 forests can physiologically track changes in nitrogen cycling caused by climate change.

155 rture from a largely anaerobic to an aerobic nitrogen cycle complete with nitrification and denitrifi

156 sults of these incubations shed new light on nitrogen cycling complexity and possible factors underly

157 mical and electrical energies leveraging the nitrogen cycle could be an effective approach in mitigat

158 ming-induced inequality in forest carbon and nitrogen cycles could widen the economic gap between the

159 is is crucial for reliably predicting carbon-nitrogen cycle coupling in Earth System Models (ESMs).

160 Considering the devastating implications of nitrogen cycle disruption, these systems for nitrite ion

161 ped to quantify anthropogenic impacts on the nitrogen cycle do not explicitly consider nitrate stored

162 fuelled by chemoautotrophic production and a nitrogen cycle dominated by nitrogen loss processes usin

163 ozoic and ~40% of the Mesoproterozoic ocean, nitrogen cycling dominated.

164 suggested a significant role of bacteria in nitrogen cycle during wood decomposition.

165 MF modifies the soil microbial community and nitrogen cycling during litter decomposition.

166 iotic N2 fixation can have a central role in nitrogen cycling during tropical forest stand developmen

167 r aqueous NO2- as part of the biogeochemical nitrogen cycle, e.g., in the investigation of fertilizat

168 Microbial populations provide nitrogen cycling ecosystem services at the nexus of agri

169 redicted to be involved in sulfur reduction, nitrogen cycling, energy conservation, and degradation o

170 sms in the presence and absence of light and nitrogen cycling enzyme inhibitors.

171 hat microbial processes mediating sulfur and nitrogen cycling exert a significant control on the carb

172 ading to questions about whether root-driven nitrogen cycling extends into weathered bedrock as well.

173 plant species can change internal ecosystem nitrogen cycling feedbacks and this mechanism can allow

174 is higher than expected and that stabilizing nitrogen-cycle feedbacks are weaker than previously thou

175 it difficult to separate natural aspects of nitrogen cycling from those induced by human perturbatio

176 carbon fixation and phylogenetic analyses of nitrogen cycling genes and transcripts indicated a diver

177 More nitrogen cycling genes were detected in the rare members

178 included the upregulation of decarboxylases, nitrogen cycling genes, and basic amino acid production

179 ase chain reaction of archaeal and bacterial nitrogen cycling genes.

180 The nitrogen cycle has been radically changed by human activ

181 the contribution of sponge holobionts to the nitrogen cycle has been recognized in past years, their

182 This reorganization of the nitrogen cycle has led to an increase in food production

183 intricate linkages with the ocean carbon and nitrogen cycles has emerged.

184 Tracking the chemicals involved in the nitrogen cycle have become a crucial point in fighting a

185 Genes and pathways involved in inorganic nitrogen cycles have been found in traditional as well a

186 librate," but because the water, carbon, and nitrogen cycles have different response times, inclusion

187 ve feedbacks between exotic grasses and soil nitrogen cycling have broken down, but rather than facil

188 necessary to perform processes important to nitrogen cycling (i.e., ammonia oxidation, nitrite oxida

189 xamined how grasshoppers influence nutrient (nitrogen) cycling (i) by their excrement, (ii) by changi

190 of excess nitrate is critical to balance the nitrogen cycle in aquatic systems.

191 um oxidation) bacteria are important for the nitrogen cycle in both natural environments and wastewat

192 nt techniques elucidate the unique microbial nitrogen cycle in nutrient-poor coastal Antarctica soils

193 ropogenic land use had severe impacts on the nitrogen cycle in stream ecosystems.

194 human influence on ammonia emissions and the nitrogen cycle in the Anthropocene.

195 The diurnal odd-nitrogen cycle in the stratosphere will be marked by a c

196 nt infected tissue, coupled to a distinctive nitrogen cycle in the uninfected cortical tissue.

197 Nitrogen cycles in Chlamydomonas reinhardtii have histor

198 ontribute significantly to marine carbon and nitrogen cycles in the oligotrophic subtropical and trop

199 resent evidence that soil carbon storage and nitrogen cycling in a grassland ecosystem are much more

200 naerobic metabolisms are thought to dominate nitrogen cycling in anoxic marine zones (AMZs).

201 y of isotopic studies aimed at understanding nitrogen cycling in aquatic environments.

202 We summarize what is known about nitrogen cycling in corals and conclude that disturbance

203 hips between precursor biotransformation and nitrogen cycling in ecosystems would help inform site re

204 g the dynamic spatial and temporal nature of nitrogen cycling in freshwater ecosystems.

205 n data that enable improved understanding of nitrogen cycling in freshwater sediments.

206 rovide quantitative constraints on microbial nitrogen cycling in open ocean oligotrophic sediments fr

207 st, we documented changes in soil carbon and nitrogen cycling in order to investigate the consequence

208 ractions in the rhizosphere shape carbon and nitrogen cycling in soil organic matter (SOM).

209 Bedforms are a focal point of carbon and nitrogen cycling in streams and coastal marine ecosystem

210 beling technique revealed increased rates of nitrogen cycling in surface soil layers around HL+ plant

211 also substantially enhance decomposition and nitrogen cycling in surface soils.

212 rees and their associated microbes influence nitrogen cycling in temperate forest soils, less is know

213 Conceptual and numerical models of nitrogen cycling in temperate forests assume that nitrog

214 To demonstrate the approach in practice, nitrogen cycling in the Arabian Sea oxygen minimum zone

215 We thus hypothesize that nitrogen cycling in the Pliocene-Pleistocene Mediterrane

216 s and KEGG orthology (KO) groups involved in nitrogen cycling in the riverine sites, suggesting a hig

217 ers of the ocean, and fundamentally altering nitrogen cycling in the sea.

218 vide an opportunity to understand better how nitrogen cycling in the terrestrial biosphere responded

219 Nitrogen cycling in X. muta appears to be more complex t

220 The nitrogen cycle, in particular, is driven by microorganis

221 f the ocean that are critical for the global nitrogen cycle, including the base of the euphotic zone,

222 Salt marsh sediments are known hotspots for nitrogen cycling, including the production and consumpti

223 have different response times, inclusion of nitrogen cycling into ecosystem models adds behavior at

224 Dinitrogen reduction in the biological nitrogen cycle is catalyzed by nitrogenase, a two-compon

225 ic reactions are still important, the extant nitrogen cycle is driven by reductive fixation of dinitr

226 delta(15)N values of guano indicate that the nitrogen cycle is hydrologically controlled and the delt

227 Thus, results suggest that the Cariaco Basin nitrogen cycle is influenced by autotrophic carbon cycli

228 The million-year variability of the marine nitrogen cycle is poorly understood.

229 The nitrogen cycle is responsible for spreading nitrogen com

230 Although nitrogen cycling is considered to dominate the microbial

231 Nitrification is a key stage in the nitrogen cycle; it enables the transformation of nitroge

232 iew emphasises the recent advances in marine nitrogen cycle lipid biomarkers, underlines the missing

233 ow that the effect of subduction on the deep nitrogen cycle may be less important than has been sugge

234 nisms with key roles in the ocean carbon and nitrogen cycles may respond to these changes in the Eart

235 s and conclude that disturbance of microbial nitrogen cycling may be tightly linked to coral bleachin

236 s highly dependent on nitrogen availability, nitrogen-cycling microbes may be of fundamental importan

237 ironments, contingent on the presence of key nitrogen-cycling microbes.

238 In the biogeochemical nitrogen cycle, microbial respiration processes compete

239 similatory nitrate reduction and interacting nitrogen cycling microorganisms, but the effect of tides

240 Ectomycorrhizal effects on nitrogen cycling might therefore provide an explanation

241 the strong interlinkages between carbon and nitrogen cycling must be considered.

242 Legumes play a vital role in maintaining the nitrogen cycle of the biosphere.

243 tion is a much more important process in the nitrogen cycle of the oceans than previously thought.

244 ch mats and their possible importance in the nitrogen cycle of the SBB.

245 moss microbial communities play key roles in nitrogen cycling of boreal forests.

246 cyanobacteria plays an important role in the nitrogen cycling of terrestrial ecosystems.

247 ay that constitutes an important part of the nitrogen cycle on earth.

248 e facilitated the development of a primitive nitrogen cycle on the surface of ancient Mars, potential

249 an evolutionary link between the carbon and nitrogen cycles on Earth and establish a solid foundatio

250 chanism and evolution between the carbon and nitrogen cycles on Earth.

251 t strategies and climatic constraints on the nitrogen cycle over evolutionary time.

252 nd-use change-have substantially altered the nitrogen cycle over large regions, making it difficult t

253 l factors and anammox was the most sensitive nitrogen cycling pathway responding to variation of the

254 nitrification and denitrification to predict nitrogen cycling patterns which agree with those provide

255 rs, whereas nitrogen isotopes record aerobic nitrogen cycling perhaps in surface waters.

256 filtration rates of the bivalves, inorganic nitrogen cycling, primary productivity of sediment dwell

257 differential warming mechanisms on this key nitrogen cycle process.

258 application of fertilizers, is accelerating nitrogen cycling processes in salt marsh sediments.

259 recent advances in our understanding of key nitrogen cycling processes in salt marshes and discuss a

260 obiont and bacterial food in driving intense nitrogen cycling processes in sponges' tissue, helping t

261 Substrate utilization rates of key nitrogen cycling processes revealed links between functi

262 ine the impact of long-term fertilization on nitrogen cycling processes with a focus on N(2)O dynamic

263 markers and geochemical assays of microbial nitrogen cycling processes, including autotrophic and he

264 ty, including the participation in different nitrogen cycling processes, likely are key factors for t

265 t with topsoil more than doubled several key nitrogen cycling processes, more research is required to

266 The nitrogen cycle provides essential nutrients to the biosp

267 ivore pressure through conserved belowground nitrogen cycling, rather than via defensive properties.

268 fects of global warming on forest carbon and nitrogen cycling remain uncertain.

269 s Review, we discuss the wealth of new ocean nitrogen cycle research in disciplines from metaproteomi

270 As N(2)-sensing is crucial for nitrogen cycle research in general and studies of denitr

271 eria play key roles in the global carbon and nitrogen cycles, respectively.

272 How the nitrogen cycle responds will determine long-term trends

273 system evolves to contain its impacts on the nitrogen cycle, several lessons can be extracted from en

274 e that strong vertical mixing drives complex nitrogen cycling, shaping community metabolism and bioge

275 Microbial functions related to nitrogen cycling showed increased spatial variability un

276 of the microbiome of H. heliophila represent nitrogen cycling taxa that have the potential to contrib

277 itrification is more prevalent in the marine nitrogen cycle than accounted for in current biogeochemi

278 fication is a central process of the aquatic nitrogen cycle that controls the supply of nitrate used

279 It has remained a challenge to describe a nitrogen cycle that could achieve such isotopic depletio

280 back to the atmosphere is a key step in the nitrogen cycle that has been researched widely.

281 ation is one of the main steps of the global nitrogen cycle that is sustained by prokaryotic organism

282 Nitrification is a central process in the nitrogen cycle that produces both the greenhouse gas nit

283 , an essential process of the biogeochemical nitrogen cycle that supports life on Earth, is catalyzed

284 linked biogeochemical processes-such as the nitrogen cycle-that can impact the quality of groundwate

285 es in the environment, such as in carbon and nitrogen cycling, their eradication is not possible.

286 mplexes in both human biology and the global nitrogen cycle, there has been interest in understanding

287 nitrogen and its rapid integration into the nitrogen cycle through multiple pathways within the well

288 mists because of their critical roles in the nitrogen cycle through symbiotic and asymbiotic biologic

289 t viruses may directly manipulate sulfur and nitrogen cycling throughout the epipelagic ocean.

290 t in predicting impacts of oil spills on the nitrogen cycle under oil spill conditions, and in improv

291 , we provide insights into the global marine nitrogen cycle under severe ocean deoxygenation.

292 To assess these processes, nitrogen cycling was evaluated over a 3-year period in a

293 Nitrogen cycling was not strongly controlled by plant po

294 carbon-cycling) and l-leucin aminopeptidase (nitrogen-cycling), was reduced following exposure to sur

295 This is especially the case for nitrogen cycling, which involves several coupled redox-s

296 proportionate influence on global carbon and nitrogen cycling, while also acting as 'sentinels' of en

297 escribe the interconnection of the metal and nitrogen cycles with nitrogenase evolution and the impor

298 United States have substantially altered the nitrogen cycle, with serious effects on climate change.

299 zotroph-derived nitrogen integrates into the nitrogen cycle within the euphotic zone remains unknown.

300 Nitrogenase plays a key role in the global nitrogen cycle; yet, the evolutionary history of nitroge