ライフサイエンスコーパス: carbon cycle

1 troph has a considerable impact on the wider carbon cycle.

2 might facilitate carbon transfer in the deep carbon cycle.

3 nd degradation/assimilation into the natural carbon cycle.

4 change will have on feedbacks to the global carbon cycle.

5 ict and mitigate human impacts on the global carbon cycle.

6 will exert greater future impacts on global carbon cycle.

7 s a promising way to close the anthropogenic carbon cycle.

8 growth has large consequences for the global carbon cycle.

9 major control on the evolution of the global carbon cycle.

10 f the most important reactions of the marine carbon cycle.

11 ible to terrestrial food webs and the global carbon cycle.

12 mortality and forest feedbacks to the global carbon cycle.

13 couple terrestrial vegetation to the global carbon cycle.

14 of the oceanic lithosphere through the deep carbon cycle.

15 ly change the seasonality of the terrestrial carbon cycle.

16 edicting forest's contribution to the global carbon cycle.

17 ntly underestimated sinks in the terrestrial carbon cycle.

18 important microbial metabolism in the global carbon cycle.

19 mmunities that play a key role in the global carbon cycle.

20 alysing the role of vegetation in the global carbon cycle.

21 at are of critical importance for the global carbon cycle.

22 mportant role of inland waters in the global carbon cycle.

23 eric CO2 and climate through the geochemical carbon cycle.

24 ior workings of the early Earth and the deep carbon cycle.

25 hrough which climate extremes may act on the carbon cycle.

26 edback between climate change and the global carbon cycle.

27 thane (AOM), is a crucial part of the global carbon cycle.

28 ynthesis, and are a major sink in the global carbon cycle.

29 ), represents a major CO2 flux in the global carbon cycle.

30 (SOC) plays an important role in the global carbon cycle.

31 he climate impacts via lagged effects on the carbon cycle.

32 and thus they play a key role in the global carbon cycle.

33 rvoirs and fluxes, and the global geodynamic carbon cycle.

34 nerals, thus contributing to the geochemical carbon cycle.

35 ons are an important component of the global carbon cycle.

36 tive feedback between climate change and the carbon cycle.

37 and are an integral component of the global carbon cycle.

38 marine ecosystem engineers and in the global carbon cycle.

39 ck weathering, thus regulating the long-term carbon cycle.

40 ynthesis, but is a major part of the world's carbon cycle.

41 in regulating seasonal changes in the global carbon cycle.

42 ria makes a major contribution to the global carbon cycle.

43 allenge despite its importance in the global carbon cycle.

44 process of great significance to the global carbon cycle.

45 ux of methane and its relation to the global carbon cycle.

46 olistic organismal biology and of the global carbon cycle.

47 s and key players in the global nitrogen and carbon cycles.

48 isms, intrinsically linking the nitrogen and carbon cycles.

49 Forests play an important role in global carbon cycles.

50 tential implications for natural halogen and carbon cycles.

51 ing of controls on ecosystem functioning and carbon cycling.

52 a more comprehensive understanding of global carbon cycling.

53 key role in ecosystem functioning and marine carbon cycling.

54 trong biological role in high-CO2 subsurface carbon cycling.

55 perform an important sink function in global carbon cycling.

56 and their interactions with biodiversity and carbon cycling.

57 edbacks via surface albedo, Bowen ratio, and carbon cycling.

58 mediate and potentially prolonged effects on carbon cycling.

59 ulating wood decomposition can affect global carbon cycling.

60 t and most widespread effects on terrestrial carbon cycling.

61 aches to linking climate and tropical forest carbon cycling.

62 a phytoplankton group that is important for carbon cycling.

63 ns that might play a critical role in global carbon cycling.

64 esting a potential for high molecular weight carbon cycling.

65 nderstanding the ocean's role in Pleistocene carbon cycling.

66 bing feedbacks to regional and global marine carbon cycling.

67 anding their role in global marine inorganic carbon cycling.

68 e evolution of Southern Ocean ecosystems and carbon cycling.

69 pheric H2 and mechanisms linking soil H2 and carbon cycling.

70 ly thought and thus it plays a major role in carbon cycling.

71 ear-complete decoupling between nutrient and carbon cycling-a "lipid shunt," and its direct transport

72 g models predicting forest water, energy and carbon cycles accordingly.

73 OCs), are an important element in the global carbon cycle, accounting for a significant proportion of

74 en devoted to quantifying how warming alters carbon cycling across diverse ecosystems, less is known

75 nsoon Asia, substantially affecting climate, carbon cycle and biodiversity.

76 carbon storage, and of feedbacks between the carbon cycle and climate, remain poorly constrained.

77 obally and is projected to affect the global carbon cycle and climate.

78 It is therefore linked to the global carbon cycle and climate.

79 k and contribute to our understanding of the carbon cycle and ecosystem function of karst subterranea

80 elled pteropods play key roles in the global carbon cycle and food webs of various ecosystems.

81 enic archaea are major players in the global carbon cycle and in the biotechnology of anaerobic diges

82 ant cell walls is a central component of the carbon cycle and is of increasing importance in environm

83 observational constraints on the terrestrial carbon cycle and its processes is, therefore, necessary

84 time RS play an important role in regulating carbon cycle and its response to climate change in alpin

85 cosystems are key contributors to the global carbon cycle and may even dominate the inter-annual vari

86 ystems play a significant role in the global carbon cycle and offset a large fraction of anthropogeni

87 water oxidations associated with the global carbon cycle and oxygenic photosynthesis, respectively.

88 semi-arid regions to the global terrestrial carbon cycle and posit that there will be larger GPP and

89 ntle is important for understanding the deep carbon cycle and related geochemical and geophysical pro

90 Lignocellulose degradation is central to the carbon cycle and renewable biotechnologies.

91 tope datasets reflecting fluctuations in the carbon cycle and seawater temperatures.

92 It plays a decisive role in the Earth's carbon cycle and significant effort is spent to quantify

93 major challenge to our understanding of the carbon cycle and the climate system.

94 ce, 27-33% for species diversity, 32-42% for carbon cycling and 31-41% for nitrogen cycling.

95 important role for regional and global scale carbon cycling and are significant sources of the atmosp

96 Marine algae are instrumental in carbon cycling and atmospheric carbon dioxide (CO2) regu

97 Microorganisms catalyze carbon cycling and biogeochemical reactions in the deep

98 otential impacts of subsurface microbiota on carbon cycling and biogeochemistry.

99 ies will likely improve our understanding of carbon cycling and climate.

100 ults highlight hysteresis in ecosystem-level carbon cycling and delayed recovery from climate extreme

101 dings challenge precepts surrounding wetland carbon cycling and demonstrate the environmental relevan

102 FE measured here may feedback and influence carbon cycling and dynamics in these forest ecosystems.

103 the dark ocean has a major impact on global carbon cycling and ecological relationships in the ocean

104 onding shifts in the lake's biogeochemistry, carbon cycling and food web structure.

105 of understanding the close linkages between carbon cycling and hydrological processes, not just temp

106 ctioning of terrestrial ecosystems, and thus carbon cycling and its feedbacks to the climate system.

107 hat chemoautotrophs can play a large role in carbon cycling and that this carbon is heavily influence

108 ommunity dynamics are important in modelling carbon cycling and the impacts of global change(3).

109 ic nitrogen (N)-fixing trees can drive N and carbon cycling and thus are critical components of futur

110 CO2 but is also sensitive to land and ocean carbon cycling and uptake.

111 id deposition mitigation strategies for both carbon cycling and watershed N export.

112 ct heterotrophic biofilms, beta-glucosidase (carbon-cycling) and l-leucin aminopeptidase (nitrogen-cy

113 hus a new connection in the manganese-driven carbon cycle, and a new variable for models that use man

114 al plays a significant role in the long-term carbon cycle, and its use as a soil amendment is promote

115 emissions play a key role in the geological carbon cycle, and monitoring of volcanic CO2 fluxes help

116 survival, form a key component of the global carbon cycle, and record an archive of past oceanographi

117 ther the most abundant species also dominate carbon cycling, and whether dominant species are charact

118 oor weathering in controlling the geological carbon cycle are unknown.

119 ay a vital role in global water, energy, and carbon cycling, are predicted to experience both longer

120 corrhiza (AM) symbioses contribute to global carbon cycles as plant hosts divert up to 20% of photosy

121 ectly impacts the microbial component of the carbon cycle, as it may drive bacterioplankton communiti

122 ration of drought-induced disruptions to the carbon cycle, as well as the mechanisms responsible, rem

123 nian trees are a key component of the global carbon cycle, assimilating and storing more carbon than

124 Models of forest energy, water and carbon cycles assume decreased stomatal conductance with

125 lts clearly demonstrate large differences in carbon cycling between forests with and without lianas.

126 em functioning, drinking water resources and carbon cycling between land and sea.

127 Based on carbon cycle box model [i.e., Long-Term Ocean-Atmosphere

128 Carbon cycle box models were used to estimate OA consequ

129 , thereby playing a major role in the global carbon cycle, but the morphologic expression of increasi

130 ates of future climate-change impacts on the carbon cycle, but this will require several important kn

131 resents a critical step within the long-term carbon cycle by sequestering volatile CO2 in solid carbo

132 land area) and are significant in the global carbon cycle by storing about 40-90 Gt C in peat.

133 ter chemistry, while inferring their role in carbon cycling by matching taxa to known taxon-specific

134 es in response to the need for better marine carbon cycle characterization.

135 ve to global change factors, which can drive carbon cycle-climate feedbacks with the potential to enh

136 and may influence the sign and magnitude of carbon cycle-climate feedbacks.

137 capacity to dampen the strength of positive carbon cycle-climate feedbacks.

138 gent constraint on predictability of various carbon cycle components in response to five classes of e

139 (VOCs) form an important part of the global carbon cycle, comprising a significant proportion of net

140 circulation and its implications for global carbon cycling continue to be debated.

141 ic diamonds may reflect differences in their carbon cycles, controlled by the evolution of geodynamic

142 ciation, chemical weathering, and the global carbon cycle could steer the evolution of global climate

143 indicates the potential for changes in local carbon cycling, depending on how these methanogens and a

144 of this deep subsurface community reveals a carbon cycle driven by autotrophic hydrogen oxidizers be

145 rtance of orbital cycles for the climate and carbon cycle during the late Paleozoic ice age and the c

146 systems can be addressed by studies of past carbon cycle dynamics and related climate change recorde

147 when met, will improve our understanding of carbon cycle dynamics, as well as forecasts of ecosystem

148 mes are strongly associated with climate and carbon cycle dynamics, with biodiversity and CO2 fertili

149 experiencing large changes in vegetation and carbon cycle dynamics.

150 ality satellite SIF for studying terrestrial carbon cycle dynamics.

151 g circulation, seem to be influencing global carbon-cycle dynamics and are at present not widely cons

152 model in order to reconstruct the unfolding carbon-cycle dynamics during the event.

153 , the results also suggest that the positive carbon cycle effect of warm spring enhances water limita

154 egetation-atmosphere feedbacks in the global carbon cycle, especially as the climate warms.

155 ed fundamental properties of the terrestrial carbon cycle, examined its intrinsic predictability, and

156 tainties in emission scenarios, climate, and carbon cycle feedback, we interpret the Paris Agreement

157 erscore the importance of climate-vegetation-carbon cycle feedbacks at high latitudes; moreover, they

158 changing amplitude of CO2 to better predict carbon cycle feedbacks in the Arctic climate system.

159 obal models that incorporate coupled climate-carbon cycle feedbacks made a significant advance with t

160 d deeper post-MPT ice ages were sustained by carbon cycle feedbacks related to dust fertilization of

161 eric O2 Future work on glaciation-weathering-carbon cycle feedbacks should consider weathering of tra

162 orly understood but important for predicting carbon cycle feedbacks to climate change.

163 Terrestrial ecosystem and carbon cycle feedbacks will significantly impact future

164 n climate-change mitigation, adaptation, and carbon cycle feedbacks, thereby reducing uncertainties i

165 Our findings suggest that future climate/carbon-cycle feedbacks may depend more strongly on chang

166 with associated effects on biodiversity and carbon-cycle feedbacks to climate change.

167 toplankton play a crucial role in the global carbon cycle, fixing CO2 into organic carbon, which may

168 t the effects of altered fire regimes on the carbon cycle; for instance, we do not fully understand t

169 The link between the nitrogen and one-carbon cycles forms the metabolic basis for energy and b

170 genous internal processes of the terrestrial carbon cycle from exogenous forcing variables.

171 variability and greening trend of the global carbon cycle given their mean lower productivity when co

172 variability and greening trend of the global carbon cycle given their mean lower productivity when co

173 d influence of marine plankton on the global carbon cycle has been recognized for decades, particular

174 ntial role of hydrocarbon fluids in the deep carbon cycle has long been controversial.

175 s represents an important sink in the global carbon cycle; however, large-scale OC burial rates are p

176 While the exact magnitude of the resulting carbon cycle impacts remains to be confirmed, the radioc

177 ed system, and provides a model of microbial carbon cycle in deep subsurface environments where hydro

178 d compounds is an important component of the carbon cycle in the Arctic.

179 ms that underpin this key step of the global carbon cycle in the deep oceans.

180 as a key component of such an anthropogenic carbon cycle in the framework of a "Methanol Economy".

181 re autotrophic control of the growing season carbon cycle in these carbon-rich permafrost ecosystems.

182 iagnostic studies of GPP and the terrestrial carbon cycle in urban areas.

183 ough highly populated areas, which may alter carbon cycles in anthropogenically disturbed ecosystems

184 er, reduces the reliability of assessing the carbon cycles in entire forest ecosystems.

185 tive effects of pulse- and press-droughts on carbon cycling in a mesic grassland of the US Great Plai

186 age flows, local microclimate, and ecosystem carbon cycling in a southern Appalachian valley.

187 e microhabitats promote the understanding of carbon cycling in macroalgae-rich waters worldwide.

188 al mutualisms, including those important for carbon cycling in nutrient-limited anaerobic environment

189 ionships between soil food web structure and carbon cycling in soils need to be reconsidered.

190 dissolved organic carbon (DOC) affects both carbon cycling in surface waters and drinking water prod

191 significance of this process as a control on carbon cycling in terrestrial ecosystems is not known.

192 globally, reflecting large perturbations of carbon cycling in the Late Ordovician oceans.

193 ss indicators to elucidate the complexity of carbon cycling in these ecosystems.

194 oorly quantified and understood component of carbon cycling in tropical forests, especially outside o

195 Global carbon models assume that carbon cycling in upland soils is entirely driven by aer

196 inties in models of the key processes in the carbon cycle, including their impacts on biodiversity, w

197 e an increasingly important driver of global carbon cycle inter-annual variability and that tropical

198 ed that a single dominant process determines carbon cycle interannual variability.

199 refore, we investigated whether this key one-carbon cycle intermediate directly affects adipocyte dif

200 question: to what extent is the terrestrial carbon cycle intrinsically predictable?

201 However, a comprehensive model of the carbon cycle is challenged by unicellular eukaryotes (pr

202 The terrestrial carbon cycle is currently the least constrained componen

203 and water cycles are intimately linked: the carbon cycle is driven by photosynthesis, while the wate

204 use and land cover change (LULCC) and on the carbon cycle is essential to provide guidance for enviro

205 The global carbon cycle is highly sensitive to climate-driven fluct

206 Also, if the subduction zone carbon cycle is nearly closed on time scales of 5-10 Ma,

207 A major contributor to the global carbon cycle is plant respiration.

208 g-term (>/=10(6) years) impact on the global carbon cycle is unknown.

209 The role of soil organic carbon in global carbon cycles is receiving increasing attention both as

210 A process of global importance in carbon cycling is the remineralization of algae biomass

211 hat, its potential role in methylotrophy and carbon cycling is unknown.

212 dbacks (apart from those associated with the carbon cycle) is removed, both the EECO and the late Eoc

213 as substantial implications for nutrient and carbon cycling, land productivity and in turn, worldwide

214 d efforts to identify key currencies of this carbon cycle link.

215 alginate degradation processes in the marine carbon cycle, little information is available on the bac

216 pite its critical role in controlling global carbon cycle, little is known about spatial patterns of

217 Here we develop a new carbon cycle model that explicitly captures the kinetics

218 om forest inventory data and a process-based carbon cycle model tracking decomposition, as well as ae

219 h mass balance constraints from an ecosystem carbon cycle model.

220 ts an important next step in coupled climate-carbon cycling model development, particularly for lowla

221 tion changes on the oceanic CO2 sink using a carbon cycling model.

222 Carbon cycle modeling has indicated that the shape and m

223 Through carbon cycle modeling, we attribute this decline primari

224 Our carbon cycle modelling identifies the Cryogenian as a un

225 nt means to test and refine land surface and carbon cycle models at the ecosystem scale.

226 y-driven flux of POC is unresolved in global carbon cycle models but can contribute as much as half o

227 historical simulations of the latest climate-carbon cycle models demonstrates that the increase in th

228 Climate-carbon cycle models generally agree that elevated atmosp

229 The incorporation of mycorrhizae in global carbon cycle models is feasible, and crucial if we are t

230 Coupled climate-carbon cycle models typically assume that vegetation rec

231 that is currently not acknowledged by global carbon cycle models.

232 y rate constants in most conventional global carbon cycle models.

233 critical role in improving land surface and carbon cycle models.

234 sed vegetation indices, nor for more complex carbon cycle models.

235 n release is presumably driven by changes in carbon cycling occurring in the stressed soil microbial

236 for a revision of the role of Archaea in the carbon cycle of marine sediments.

237 of deep-carbon storage as well as the global carbon cycle of the planet.

238 single, low-intensity fires weakly influence carbon cycling of this primary neotropical forest, altho

239 of oceanic microbial communities and in the carbon cycle on Earth.

240 mangrove OC sequestration within the global carbon cycle on geological timescales.

241 nsider slow climate feedbacks related to the carbon cycle or interactions between ice sheets and clim

242 mportance of picocyanobacteria in the global carbon cycle, our results indicate that picocyanobacteri

243 reports of the importance of land use on the carbon cycle over climate change.

244 inent cyclicity of approximately 9 My in the carbon cycle paced by changes in the seasonal dynamics o

245 A rapid carbon cycle perturbation and global warming event about

246 , harbor a 'deep carbonated biosphere' with carbon cycling potential.

247 eathering paradox', and the evolution of the carbon cycle probably depended on multiple processes.

248 ry particulate organic carbon (POC) is a key carbon cycle process that fuels the deep subseafloor bio

249 phic anaerobic photosynthesis is therefore a carbon cycling process that could take place in anoxic e

250 Soil carbon cycling processes potentially play a large role i

251 rhaps mimicking in some respects the natural carbon cycles/production, utilization of natural, abunda

252 olysaccharides forms an essential arc in the carbon cycle, provides a percentage of our daily caloric

253 Here, we review the literature on carbon cycle relevant responses of ecosystems to extreme

254 of the responses of oceanic and terrestrial carbon cycle remain poorly constrained in space and time

255 in sediment production and marine inorganic carbon cycling, remain poorly understood.

256 on (GPP) remains a major challenge in global carbon cycle research.

257 l [i.e., Long-Term Ocean-Atmosphere-Sediment Carbon Cycle Reservoir (LOSCAR) model] experiments, we s

258 ne food web and are a crucial element of the carbon cycle, respond to major environmental disturbance

259 patial climate covariation drives the global carbon cycle response.

260 importance of land-use dynamics for modeling carbon cycle responses to climate change in integrated a

261 n and enhancement, (b) simulate land-use and carbon cycle responses to moderate climate change (RCP2.

262 al respiration are a key component of global carbon cycling, resulting in the transfer of 40-70 Pg ca

263 A model of the long-term carbon cycle shows that increases in delta(13)C need not

264 tions to assess the detectability of Alaskan carbon cycle signals as future warming evolves.

265 Feedbacks from the terrestrial carbon cycle significantly affect future climate change.

266 ignored in global biogeochemical models and carbon cycle simulations.

267 vide a global-scale benchmark for historical carbon-cycle simulations.

268 onounced climate sensitivity for this global carbon cycle sink.

269 first global estimates, to our knowledge, of carbon cycle state and process variables at a 1 degrees

270 tionships in the spatial distribution of key carbon cycle states and processes.

271 w opportunities for quantitative, autonomous carbon-cycle studies.

272 meters to measure for high-quality, in situ, carbon-cycle studies.

273 e oxidation may have a greater impact on the carbon cycle than previously assumed.

274 ift and erosion via changes to the inorganic carbon cycle that are independent of changes to the isot

275 nsistent with simulations of climate and the carbon cycle that assume large GPP growth during the twe

276 carbon fixation is a key step in the global carbon cycle that regulates the atmosphere's composition

277 n carbon sink suggest a rather dynamic ocean carbon cycle that varies more in time than previously re

278 s an important component of local and global carbon cycles that is characterized by tight linkages be

279 Little was known of the carbon cycle there, but recent work showed it was a very

280 als, Actinobacteria contribute to the global carbon cycle through the breakdown of plant biomass.

281 3)Ccarb documents eccentricity modulation of carbon cycling through the period and a strong obliquity

282 The response of the terrestrial carbon cycle to climate change is among the largest unce

283 show divergent responses of the terrestrial carbon cycle to global change over the next century.

284 rdwood forest, we documented changes in soil carbon cycling to investigate the potential consequences

285 (MMEM) shows that the response of ecosystem carbon cycling to rising CO2 concentration (eCO2 ) and c

286 But the response of tropical forest carbon cycling to these droughts is not fully understood

287 d model is an accurate representation of the carbon cycle, to fit proxies the temperature dependence

288 ake accurate predictions of RS and ecosystem carbon cycle under climate change scenarios.

289 Current theory and models of tropical forest carbon cycling under projected scenarios of global atmos

290 Carbon cycle volatility persists for approximately 500 k

291 behavior and fire-induced changes in forest carbon cycling, we manipulated fine fuel loads in a fire

292 reates a short circuit in the biogeochemical carbon cycle, where soils release significant amounts of

293 tter decomposition is a key component of the carbon cycle, which is largely controlled by saprotrophi

294 How soil processes such as carbon cycling will respond to future climate change dep

295 Based on these results, predicting future carbon cycling with climate change will require an under

296 Methane is a key component in the global carbon cycle, with a wide range of anthropogenic and nat

297 he surface ocean is a key step in the global carbon cycle, with almost half of marine primary product

298 The traditional view of carbon cycling within the pelagic zone of freshwater lak

299 production (GPP) is the largest flux in the carbon cycle, yet its response to global warming is high

300 acts on forest carbon storage and the global carbon cycle, yet these effects may depend on mechanisms