ライフサイエンスコーパス: carbon cycle

1 cascading effects on the ocean food web and carbon cycle.

2 rivers, are active components of the global carbon cycle.

3 forests play an important role in the global carbon cycle.

4 tions about the roles of SUP05 in the marine carbon cycle.

5 f the marine food web and are crucial in the carbon cycle.

6 nce at those depths including effects on the carbon cycle.

7 ical forests, which dominate the terrestrial carbon cycle.

8 haea that play a critical role in the global carbon cycle.

9 Mg(CO(3))(2)) plays a key role in the global carbon cycle.

10 in understanding the dynamics of the marine carbon cycle.

11 13) in order to preserve mass balance in the carbon cycle.

12 s and the associated imbalance in the global carbon cycle.

13 composition, with concomitant impacts on the carbon cycle.

14 tant, but often overlooked, component of the carbon cycle.

15 surface ocean, is a large driver of Earth's carbon cycle.

16 certainty in our understanding of the global carbon cycle.

17 d preservation play a key role in the global carbon cycle.

18 crucial for understanding and predicting the carbon cycle.

19 and interpreting their impact on the global carbon cycle.

20 POM) by microbes is a key part of the global carbon cycle.

21 for accurate projections of the future land carbon cycle.

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

23 couple terrestrial vegetation to the global carbon cycle.

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

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

26 marine ecosystem engineers and in the global carbon cycle.

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

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

29 in regulating seasonal changes in the global carbon cycle.

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

31 allenge despite its importance in the global carbon cycle.

32 groups that play a major role in the global carbon cycle.

33 g the role of tropical forests in the global carbon cycle.

34 and discuss implications on the terrestrial carbon cycle.

35 ecause of their important role in the global carbon cycle.

36 ing the impacts of climatic variables on the carbon cycle.

37 ems, fungi are critical agents of the global carbon cycle.

38 osystem properties and effects on the global carbon cycle.

39 ed for their potential to perturb the global carbon cycle.

40 determining the fate of carbon in the global carbon cycle.

41 aid the budgeting and modeling of the global carbon cycle.

42 gae and is a critical parameter in the ocean carbon cycle.

43 cosystem dynamics and changes in the oceanic carbon cycle.

44 ly increasing component of the inland waters carbon cycle.

45 tionships between subnival ecology and water/carbon cycles.

46 tial significance to the global nitrogen and carbon cycles.

47 l role on the terrestrial water, energy, and carbon cycles.

48 tential implications for natural halogen and carbon cycles.

49 isms, intrinsically linking the nitrogen and carbon cycles.

50 Forests play an important role in global carbon cycles.

51 ing to both the organic and inorganic marine carbon cycles.

52 otentially important consequences for global carbon cycling.

53 ebrate herbivores and measured indicators of carbon cycling.

54 in pantropical ecosystem dynamics and global carbon cycling.

55 mosphere, with substantial effects on global carbon cycling.

56 ay represent an overlooked component of soil carbon cycling.

57 function of vegetation with implications for carbon cycling.

58 group of zooplankton, have affected biogenic carbon cycling.

59 e volumes of crustal CO(2) may impact global carbon cycling.

60 ing such as ecosystem primary production and carbon cycling.

61 ovide insight into climate change effects on carbon cycling.

62 a more comprehensive understanding of global carbon cycling.

63 esting a potential for high molecular weight carbon cycling.

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

65 bing feedbacks to regional and global marine carbon cycling.

66 anding their role in global marine inorganic carbon cycling.

67 e evolution of Southern Ocean ecosystems and carbon cycling.

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

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

70 timated role in tropical forest dynamics and carbon cycling.

71 n of distinct copiotrophic bacterial taxa to carbon cycling.

72 ments highlighting the role of DOM in global carbon cycling.

73 for nutrient and water uptake, and influence carbon cycling.

74 he Southern Ocean control on global exogenic carbon cycling.

75 lf seas play an important role in the global carbon cycle, absorbing atmospheric carbon dioxide (CO(2

76 th's mantle is a critical pathway in Earth's carbon cycle, affecting both the climate and the redox c

77 osystem model accurately represents observed carbon cycle and active layer depth responses to short-t

78 y used in modelling, for example, the global carbon cycle and climate change, and for interpreting tr

79 ant to improve our knowledge of the regional carbon cycle and climate change.

80 in is important for understanding the global carbon cycle and could aid in developing systems for pro

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

82 ustry and plays a crucial role in the global carbon cycle and formation of sedimentary rocks.

83 n to climate change has implications for the carbon cycle and global climate.

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

85 inconsistent with the dynamics of the global carbon cycle and its response to anthropogenic carbon di

86 vital role that soil moisture exerts on the carbon cycle and other environmental threats such as hea

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

88 the active role of ice sheets in the global carbon cycle and potential ramifications of enhanced mel

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

90 s which play an important role in the global carbon cycle and risk releasing large quantities of GHGs

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

92 n geology, diamond forms as part of the deep carbon cycle and typically displays a highly ordered cub

93 archaea are major contributors to the global carbon cycle and were long thought to belong exclusively

94 ith the need to maintain mass balance in the carbon cycle and without requiring increases in the sili

95 toms effectively couple the silicon (Si) and carbon cycles and ballast substantial vertical flux of c

96 the marine food chain as well as oxygen and carbon cycles and thus plays a global role in climate an

97 subsidy to distant habitats and for inshore carbon cycling and (potentially) carbon sequestration.

98 es and carbon to Lake Untersee, evaluate the carbon cycling and assess the metabolic functioning of m

99 Microorganisms catalyze carbon cycling and biogeochemical reactions in the deep

100 ing of how oxygen deficiency affects organic carbon cycling and burial.

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

102 streambed is an important pathway in organic carbon cycling and energy transfer in the biosphere that

103 Despite their importance in oceanic carbon cycling and export, little is known about the bio

104 global change drivers on grassland ecosystem carbon cycling and highlight a crucial role for positive

105 The framework emulates carbon cycling and its component processes in a global d

106 ould aid in our collective knowledge of both carbon cycling and microbial strategies to valorize lign

107 onstitute an important component in regional carbon cycling and nutrient release and to influence dow

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

109 onse to drought of soil functions related to carbon cycling and the capture and transfer below-ground

110 crucial role of rare bacterial taxa in ocean carbon cycling and the importance of bacterial community

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

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

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

114 a key but uncertain component of the global carbon cycle, and accordingly, of Earth System Models (E

115 Given the importance of forests in the carbon cycle, and the pivotal role for wood decay, accur

116 real forests play a large role in the global carbon cycle, and the responses of northern trees to cli

117 ich drought can continue to affect ecosystem carbon cycling, and a potential plant strategy to facili

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

119 t the dominant mechanisms that determine the carbon cycling are different between the consolidated gu

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

121 growth being controlled by traits related to carbon cycling (assimilation and respiration) in well-wa

122 tem metabolic processes and contributions to carbon cycles at watershed to global scales.

123 for advancing predictions of the terrestrial carbon cycle because hydraulic traits affect both ecosys

124 BC is an important component of the global carbon cycle because, compared to unburned biogenic OC,

125 is important to our understanding of Earth's carbon cycle, because similar processes control both (e.

126 an important role in the regional and global carbon cycles, but, despite considerable in situ and spa

127 These changes directly affect the global carbon cycle by altering the transport of organic materi

128 of CO and CO(2) are regulated in the global carbon cycle by chemolithoautotrophic bacteria and archa

129 Closing the anthropogenic carbon cycle by converting CO(2) into reusable chemicals

130 wn algae are important players in the global carbon cycle by fixing carbon dioxide into 1 Gt of bioma

131 and constitute a substantial fraction of the carbon cycled by inland waters.

132 The regulation of aquatic carbon cycles by temperature is a significant uncertaint

133 es influence soil water dynamics, as well as carbon cycling by changing soil CO(2) emission and uptak

134 mpact phytoplankton primary productivity and carbon cycling by supplying bioavailable Fe to remote ar

135 h mass extinction and biologically amplified carbon cycle change.

136 ur models show that these extinction-related carbon cycle changes would have allowed the ocean to abs

137 l productivity and carbon storage, land use, carbon cycle-climate feedback, diversity-productivity re

138 crobial metabolism of soil carbon, causing a carbon-cycle-climate feedback whereby carbon is redistri

139 The global carbon cycle connects organic matter (OM) pools in soil,

140 Here, we synthesized ecosystem carbon-cycling data from 1,119 experiments performed ove

141 The consequences for ecosystem carbon cycling depend on the feedbacks from other limiti

142 (~44 km), representing a barrier to the deep carbon cycle depending on the buoyancy and viscosity of

143 fied, limiting our understanding of the deep carbon cycle during geologic time and in modern Earth.

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

145 ects of elevated pCO(2) on bacteria-mediated carbon cycling during phytoplankton bloom conditions in

146 anging circulation patterns in understanding carbon cycle dynamics observed from atmospheric observat

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 ted a treasure trove of Cenozoic climate and carbon cycle dynamics.

150 significant uncertainty in predicting global carbon cycle dynamics.

151 ality satellite SIF for studying terrestrial carbon cycle dynamics.

152 could provide novel insights into nuances of carbon cycling dynamics by alleviating important uncerta

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

154 text]C in shallow carbonates with a diurnal carbon cycle engine, where daily transfer of carbon betw

155 etecting regional changes in the terrestrial carbon cycle even where anthropogenic emissions are not

156 A hidden carbon cycle exists inside Earth.

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

158 contributor to the proposed positive global carbon-cycle feedback to climate change.

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

160 Carbon cycle feedbacks represent large uncertainties in

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

162 onsiderable uncertainty in the prediction of carbon cycle feedbacks to climate change.

163 nt of 0.4 +/- 0.2 PgC yr(-1) attributable to carbon cycle feedbacks, amounting to a combined sink inc

164 f land use in modulating future land climate-carbon cycle feedbacks, climate mitigation efforts shoul

165 net)) is important to predict future climate-carbon cycle feedbacks.

166 with important implications for the climate-carbon cycle feedbacks.

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

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

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

170 s and assessment of its significance for the carbon cycle has been hindered by limited data density a

171 The terrestrial carbon cycle has been strongly influenced by human-induc

172 This engine maintains a carbon-cycle hysteresis that is most amplified in shallo

173 Here we overviewed the literature on carbon cycle IAV about current understanding of these is

174 ical land ecosystems to the signal of global carbon cycle IAV, where tropical semiarid ecosystems con

175 , constituent fluxes and climatic factors to carbon cycle IAV.

176 itions, is emerging as key regulators of the carbon cycle IAV.

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

178 ersity and their implications for the global carbon cycle in greater detail than ever before.

179 al communities, which are key drivers of the carbon cycle in marine soft sediments.

180 p us to elucidate links between nitrogen and carbon cycle in microbial communities in the near future

181 nd their drivers, based on theory of dynamic carbon cycle in non-steady state and process-based ecosy

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

183 ainfall is thus crucial to project water and carbon cycles in the future.

184 le of plants' water use for global water and carbon cycling in a changing climate.

185 last mass extinction, the recovery of marine carbon cycling in a postextinction world, and the way in

186 nitrogen cycle is influenced by autotrophic carbon cycling in addition to organic matter oxidation a

187 pes that perform differently in nitrogen and carbon cycling in dark oceans.

188 n-damo) play important roles in nitrogen and carbon cycling in fresh waters but we do not know how th

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

190 ity fire is an overlooked factor influencing carbon cycling in peatlands, which is relevant to global

191 n appears to be a significant contributor to carbon cycling in some ecosystems.

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

193 the impact of large earthquakes on long-term carbon cycling in the deep-sea.

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

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

196 o improve the predictions of fire effects on carbon cycling in tropical forests.

197 x) ) is critical for determining terrestrial carbon cycling in tropical forests.

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

199 This implies a shift to a domain of carbon cycling in which these forests become a net sourc

200 Ecosystem carbon cycling integrates the independent physiological

201 Yet, it remains unclear how climate and carbon cycle interacted under changing geologic boundary

202 experienced state-dependent modes of climate-carbon cycle interaction.

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 history of the carbon cycle is punctuated by enigmatic transient change

206 ity played in this process and ultimately in carbon cycle is still poorly understood due to its compl

207 A critical driver of the ocean carbon cycle is the downward flux of sinking organic par

208 A major uncertainty in the land carbon cycle is whether symbiotic nitrogen fixation acts

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

210 ry production, a key regulator of the global carbon cycle, is highly responsive to variations in clim

211 ial activity, and the related impact on soil carbon cycling, is thus greater in regions with lower MA

212 cale of the disruption are properties of the carbon cycle itself rather than its perturbation.

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

214 Cement plays a dual role in the global carbon cycle like a sponge: its massive production contr

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

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

217 Here we use a parsimonious carbon cycle model that tracks two weathering-sensitive

218 oupled this diagenetic framework to a global carbon cycle model.

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

220 We used carbon cycle modeling and paleotemperature records to co

221 Through carbon cycle modeling, we attribute this decline primari

222 n predicting stomatal behavior and improving carbon cycle modeling.

223 Current carbon cycle models also demonstrate a declining CFE tre

224 for the re-evaluation of global terrestrial carbon cycle models and also suggest that current global

225 but remain a major source of uncertainty in carbon cycle models and climate change projections.

226 Carbon cycle models overestimate BPE, although models wi

227 namical and biological processes into global carbon cycle models.

228 ng field measurements from 113 sites with 14 carbon cycle models.

229 to incorporate this mechanism into most IPCC carbon-cycle models for convincing projection of terrest

230 With accumulation of carbon cycle observations and model developments over th

231 ested at interannual timescale and expanding carbon cycle observations at broader spatial and longer

232 ng empirical evidence that lianas affect the carbon cycle of tropical forests.

233 atio increases, with potential impact on the carbon cycle of water-limited ecosystems.

234 uman land use co-regulate the vegetation and carbon cycles of a tropical lagoon system and its catchm

235 g interannual variation (IAV) of terrestrial carbon cycle offers the opportunity to better understand

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

237 which could be crucial to understand how the carbon cycle operated in the past.

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

239 y and their contribution to global water and carbon cycles, our knowledge of the genetic basis of sto

240 ions, aiming to model the full extent of the carbon cycle perturbations around the T-J boundary.

241 have driven observed extinction patterns and carbon cycle perturbations is still lacking.

242 mass extinction (ETE), and associated major carbon cycle perturbations occurred synchronously around

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

244 espiration, enzymatic activity, nitrogen and carbon cycling potentials and Arabidopsis biomass in sal

245 framework to explore controls on belowground carbon cycling: Probabilistic Representation of Organic

246 linking species-rich plant communities to a carbon cycle process of importance to Earth's climate sy

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

248 he short-term influence of this species over carbon cycle processes.

249 to be physiologically critical to growth and carbon cycling processes.

250 ted, but decreased precipitation slowed down carbon-cycle processes.

251 A) in the northern hemisphere is an emerging carbon cycle property.

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

253 Algal viruses are important contributors to carbon cycling, recycling nutrients and organic material

254 the opportunity to better understand climate-carbon cycle relationships.

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

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

257 sing the long-term ocean-atmosphere-sediment carbon cycle reservoir (LOSCAR) model.

258 As the abiotic carbon cycle responds, further metabolic evolution (anae

259 patial climate covariation drives the global carbon cycle response.

260 woody productivity (ANPP(stem) ) influences carbon cycle responses to climate change.

261 m of cell sizes coincides with indicators of carbon-cycle restoration and a fully functioning biologi

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

263 with implications for conservation biology, carbon cycle science, and international policy.

264 (CFE), remains a key area of uncertainty in carbon cycle science.

265 their interaction,that is, the dependence of carbon cycle sensitivity to temperature on moisture cond

266 al publications have examined leaf-trait and carbon-cycling shifts along an Amazon-Andes transect spa

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

268 gests that only marginal improvement in land carbon cycle simulations can be gained from comparisons

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

270 red the seafloor habitat and modified global carbon cycling since the Cambrian.

271 , signalling a reorganization of the climate-carbon cycle system.

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

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

274 find that CDJ are pervasive features of the carbon cycle that can occur during interglacial climate

275 nesis is a key biogeochemical process in the carbon cycle that is responsible for 70% of global emiss

276 and pacing of changes in the Early Jurassic carbon cycle that provide context for these events are t

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

278 g a time [Formula: see text] y in the modern carbon cycle, the threshold flux is constant; for smalle

279 ystem Models (ESMs) to project future global carbon cycling; these models have been criticized for no

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

281 ng and predicting the response of the Arctic carbon cycle to global change.

282 strates particular sensitivity of the marine carbon cycle to long-eccentricity orbital forcing.

283 hts the susceptibility of the late Paleocene carbon cycle to perturbations and suggests that climate

284 of the response of the ocean's nitrogen and carbon cycles to environmental change.

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

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

287 Empirical evidence for the response of soil carbon cycling to the combined effects of warming, droug

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

289 patial heterogeneity in multi-decadal Arctic carbon cycle trajectories and argue for more mechanistic

290 Observations and models of the carbon cycle unanimously show the dominance of tropical

291 of fire impacts on global tree cover and the carbon cycle under current climate and anthropogenic lan

292 ate biochemical modelling efforts to project carbon cycling under future climate scenarios.

293 om the interannual to the centennial, global carbon cycle variability will be increasingly contribute

294 Due to the importance of the Earth's carbon cycle, we focus on carbonate and bicarbonate ions

295 ications for understanding annual to decadal carbon cycling where ecotypes could influence ecosystem

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

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

298 er-hemispheric climate variability on global carbon cycling within centuries and millennia.

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

300 productivity and strongly affect the global carbon cycle, yet little is known about the forces that