ライフサイエンスコーパス: SOC

1 SOC increases in topsoil were observed for all types of

2 templating anion to induce the assembly of a SOC within silver NC.

3 isturbance under WP-CT and WF-CT accelerated SOC mineralization leading to soil C loss.

4 of nutrients and water, thereby accelerating SOC turnover through both stabilization and destabilizat

5 Perennial crops generally accumulate SOC through time, especially woody crops; and temperatur

6 bial necromass C, and >76% of the additional SOC enhanced by land-use transition from annual to peren

7 Specifically, ~92% of the additional SOC enhanced by plant diversity was estimated to be micr

8 and use combined with soil conditions affect SOC changes throughout the soil profile.

9 Simutaneously, SOC in WSA(>5 mm) affected SOC concentration in bulk soils.

10 nges in plant diversity and how this affects SOC content.

11 stabilization causing SOC accrual, but also SOC destabilization causing SOC loss.

12 tandard-of-care (SOC) treatments (arm 1) and SOC plus SABR (arm 2).

13 r as well as carbon use efficiency (CUE) and SOC accumulation is unknown.

14 were 11.8% and 21.6% for the eculizumab and SOC groups, respectively (nominal P = .288).

15 Over a 50-year co-evolution of landscape and SOC turnover, we find that the dominant mechanisms that

16 hronous responses of microbial necromass and SOC to land-use change.

17 soil organic carbon (SOC) stabilization and SOC response to climate change.

18 crobial necromass biomarker amino sugars and SOC, from two long-term agricultural field studies condu

19 also for soil mass-based properties such as SOC mass percent, C:N mass ratio, and delta(13) C.

20 u(i) mainly captures fresh readily available SOC.

21 ng changes in SOC, with MMM equal to average SOC (and standard deviation) of 39.2 (+/-15.5) Mg C/ha c

22 ion of carbon translate poorly to pool-based SOC models; as a result, we are challenged to mechanisti

23 nt of PKCdelta in stimulation of TRPC1-based SOCs and highlight that store-operated PKCdelta activity

24 fore important to understand how TRPC1-based SOCs are activated.

25 P(2) and TRPC1 and activation of TRPC1-based SOCs by PIP(2) required PKCdelta.

26 orm(s) is involved in activating TRPC1-based SOCs in contractile rat mesenteric artery VSMCs.

27 C isoform involved in activating TRPC1-based SOCs in rat mesenteric artery VSMCs.

28 Activation of TRPC1-based SOCs requires protein kinase C (PKC) activity, which is

29 Stimulation of TRPC1-based SOCs requires protein kinase C (PKC) activity, with stor

30 ental protocols used to activate TRPC1-based SOCs suggest that the PKC isoform involved requires diac

31 TRPC1-based SOCs were reduced by PKCdelta inhibitors and knockdown o

32 an obligatory role in activating TRPC1-based SOCs, through regulating PIP(2) -mediated channel openin

33 morpholinos oligomers inhibited TRPC1-based SOCs.

34 stem C storage that includes soil organic C (SOC) must be considered to determine whether planting tr

35 ys incubation, where more than 70% of (14) C-SOC was concentrated in the relatively stable humin frac

36 to those ascribed to store-operated calcium (SOC) channels, particularly those involving transient re

37 e we show that NGH in serous ovarian cancer (SOC) can be accurately measured when informed by the mol

38 nts on how roots affect soil organic carbon (SOC) an apparent paradox has emerged where roots drive S

39 potential to sequester soil organic carbon (SOC) and mitigate global climate change.

40 spatial distribution of soil organic carbon (SOC) and total nitrogen (TN) concentrations in croplands

41 physical properties and soil organic carbon (SOC) are considered as important factors of soil quality

42 Soil organic carbon (SOC) concentration in WSA(0.106-0.25),WSA(2-5 mm) and WS

43 Soil organic carbon (SOC) content increased under High-N, corresponding to a

44 The soil organic carbon (SOC) content of our top soils increases linearly not onl

45 soil condition such as soil organic carbon (SOC) content remains unknown.

46 aging soils to increase soil organic carbon (SOC) content to contribute to climate change mitigation,

47 lation models represent soil organic carbon (SOC) dynamics in global carbon (C) cycle scenarios to su

48 and the balance between soil organic carbon (SOC) formation and loss will drive powerful carbon-clima

49 ncreasing the amount of soil organic carbon (SOC) has agronomic benefits and the potential to mitigat

50 Soil organic carbon (SOC) is primarily formed from plant inputs, but the rela

51 warming will stimulate soil organic carbon (SOC) losses via heterotrophic respiration remains uncert

52 ues may not only affect soil organic carbon (SOC) pool but also impact SOC stability through soil agg

53 ally contributes to the soil organic carbon (SOC) pool.

54 and salinity increase, soil organic carbon (SOC) sequestration mechanisms in estuarine wetlands rema

55 resenting mechanisms of soil organic carbon (SOC) stabilization and SOC response to climate change.

56 Quantifying changes in soil organic carbon (SOC) stocks and other soil properties is essential for u

57 tively small changes in soil organic carbon (SOC) stocks can significantly alter atmospheric C and gl

58 Among these, increasing soil organic carbon (SOC) stocks is an important lever because carbon in soil

59 Global soil organic carbon (SOC) stocks may decline with a warmer climate.

60 bit increased long-term soil organic carbon (SOC) storage.

61 aluates the dynamics of soil organic carbon (SOC) under perennial crops across the globe.

62 The fate of soil organic carbon (SOC) under warming is poorly understood, particularly ac

63 ining 171 patients elected standard of care (SOC) (103), investigational therapy (28) or palliative c

64 Outcomes of standard of care (SOC) and early corticosteroid groups were evaluated, wit

65 red at 4 time points, with standard of care (SOC) education on improving readiness to pursue DDKT and

66 gnosis of VTE treated with standard of care (SOC) for >=3 months, or had completed dabigatran or SOC

67 positive blood cultures is standard of care (SOC) in many clinical microbiology laboratories.

68 was randomized to receive standard of care (SOC) lidocaine-based anesthesia and the other eye receiv

69 Patients randomized to standard of care (SOC) or evolocumab 420 mg monthly (evolocumab + SOC) for

70 egy (TEG group; n = 49) or standard-of-care (SOC) group (n = 47).

71 ens previously analyzed by standard-of-care (SOC) NAATs.

72 tcomes with axi-cel in the standard-of-care (SOC) setting for the approved indication.

73 2 ratio between palliative standard-of-care (SOC) treatments (arm 1) and SOC plus SABR (arm 2).

74 re site or local hospital (standard of care [SOC]).

75 tion on former agricultural land also caused SOC decreases in the 20-60 cm soil layers, while SOC dec

76 ccrual, but also SOC destabilization causing SOC loss.

77 where roots drive SOC stabilization causing SOC accrual, but also SOC destabilization causing SOC lo

78 ctures by the secondary ossification center (SOC).

79 and N sinks of coastal wetlands by changing SOC and SON pools size, stability and dynamics changes f

80 f Ca(2+) -permeable store-operated channels (SOCs) composed of canonical transient receptor potential

81 nel 1 (TRPC1)-based store-operated channels (SOCs) mediates Ca(2+) entry pathways that regulate cell

82 sodalite-type silver orthophosphate cluster (SOC) {(Ag(3) PO(4) )(8) }, reminiscent of the Ag(3) PO(4

83 Seed oil content (SOC) is a highly important and complex trait in oil crop

84 quantitative trait loci (QTLs) that control SOC in eight environments, evaluated the effect of each

85 ng force from efficient spin-orbit coupling (SOC) between the singlet and triplet wavefunctions.

86 Spin-orbit coupling (SOC) is the key to realizing time-reversal-invariant top

87 ic insulator and a high spin-orbit coupling (SOC) metal coated over a non-magnetic substrate.

88 ction parameter (U) and spin-orbit coupling (SOC) were not properly accounted for in the calculations

89 with colossal intrinsic spin-orbit coupling (SOC), theoretically give rise to giant Rashba-type SOC.

90 ombined with the strong spin-orbit coupling (SOC).

91 rtificially generated spin-orbital coupling (SOC).

92 eristic suggests self-organized criticality (SOC), a statistical property that has been identified in

93 valuate virus tropism in skin organ culture (SOC) and skin xenograft mouse models.

94 mpensate such decline (i.e. maintain current SOC stocks), a 3% increase of NPP is required.

95 We used subtype signatures to deconvolute SOC expression data and found substantial intra-tumor NG

96 natural pasture to perennial crop decreased SOC stocks by 1% over 0-30 cm (-2.5 +/- 4.2 Mg/ha) and 1

97 ng root and litter inputs, which may deplete SOC pools despite greater SOC formation rates.

98 through the soil food web and into distinct SOC pools.

99 This vital role of downward SOC movement in controlling whole-soil profile SOC dynam

100 Without the downward SOC movement, global SOC declines by 15%, while a 20% in

101 parent paradox has emerged where roots drive SOC stabilization causing SOC accrual, but also SOC dest

102 more holistic approach to study root-driven SOC dynamics.

103 eat AML sub-studies versus those who elected SOC.

104 hmark sites in global frameworks to estimate SOC change.

105 We evaluated SOC simulated from an ensemble of 26 process-based C mod

106 should be the standard method for evaluating SOC stock changes in mineral soils, but we further sugge

107 luable metrics for future studies evaluating SOC storage under alternative management in changing cli

108 ) or evolocumab 420 mg monthly (evolocumab + SOC) for year 1.

109 l-evolocumab period and receive evolocumab + SOC for an additional 4 years.

110 We found that evolutionarily SOC appears in animals conquering the land - amniotes.

111 ng in regions with considerable pre-existing SOC stocks will have the intended policy and climate cha

112 4 hours after injection were 1.6 +/- 0.4 for SOC and 1.2 +/- 0.5 in the combined -10 degrees C arms (

113 nge in SOC and examine the MRV platforms for SOC change already in use in various countries/regions.

114 ing anesthesia versus 395 +/- 40 seconds for SOC (P < 0.0001).

115 ral soils, but ESM remains underutilized for SOC stocks and has rarely been used for other soil prope

116 URY, MIMICS more accurately estimates forest SOC concentrations and the sensitivities of SOC to varia

117 the primacy of living root inputs in forming SOC.

118 orthern part of the region is likely to gain SOC while the southern part of the region is predicted t

119 long-term data (r(2) = 0.92; n = 90), global SOC distribution (rmse = 4.7 +/- 0.6 kg C m(-2)), and to

120 Without the downward SOC movement, global SOC declines by 15%, while a 20% increase in NPP is need

121 We predict that global SOC stocks (down to 2 m) will decline by 4% (~80 Pg) on

122 = 4.7 +/- 0.6 kg C m(-2)), and total global SOC in the top 0.3 m (822 Pg C) accurately.

123 which may deplete SOC pools despite greater SOC formation rates.

124 ffusion along (003) layers dominates at high SOC.

125 Rather, the PROMISE concept considers how SOC cycling rates are governed by the stochastic process

126 I(SOC) is a cation current permeating the ISOC channel.

127 Global calcium entry and I(SOC) are decreased by S100A6 in a PPP5C-dependent manner

128 In pulmonary endothelial cells, I(SOC) activation leads to formation of inter-endothelial

129 Following I(SOC) activation, cytosolic S100A6 translocates to the pl

130 y role in the PPP5C-FKBP51 axis to inhibit I(SOC) and protect the endothelial barrier against calcium

131 e protein phosphatase 5C (PPP5C), inhibits I(SOC) .

132 onary endothelial cells and contributes to I(SOC) inhibition by the PPP5C-FKBP51 axis.

133 il organic carbon (SOC) pool but also impact SOC stability through soil aggregation.

134 rovides rich genetic resources for improving SOC and valuable insights toward understanding the compl

135 In SOC, VZV infected the epidermis and HCMV infected the de

136 eligible subjects, 81 (38%) and 132 (62%) in SOC and early corticosteroid groups, respectively.

137 an be used to simulate and project change in SOC and examine the MRV platforms for SOC change already

138 However, model projections of changes in SOC due to climate warming depend on microbially-driven

139 soil surveys are used to estimate changes in SOC over time, and how long-term experiments and space-f

140 r errors than FD when quantifying changes in SOC stocks and other soil properties.

141 crops and the subsequent temporal changes in SOC stocks during the perennial crop cycle.

142 ended in lieu of FD for assessing changes in SOC stocks in mineral soils, but ESM remains underutiliz

143 Gen proved adequate in describing changes in SOC, with MMM equal to average SOC (and standard deviati

144 The decline in SOC cancelled out the increment in C stocks in tree biom

145 consistent in reflecting the differences in SOC decomposition or accumulation among four vegetation

146 as the main driver explaining differences in SOC dynamics, followed by crop age, soil bulk density, c

147 nial crops led to an average 20% increase in SOC at 0-30 cm (6.0 +/- 4.6 Mg/ha gain) and a total 10%

148 e data indicated that while a 2% increase in SOC was observed at 0-30 cm (16.81 +/- 55.1 Mg/ha), a de

149 that translate into the observed increase in SOC.

150 phasizes the active role of soil microbes in SOC storage by integrating the continual microbial trans

151 perature relationships have been proposed in SOC models.

152 g-term parameters, respectively, resulted in SOC loss (-8.2 +/- 5.1% or -3.9 +/- 2.8%), and minor SOC

153 riming' of soil organic matter, resulting in SOC loss, constraining the benefits of tree planting for

154 However, there are differences spatially in SOC trends.

155 ant surface trends and spatial structures in SOC and TN in both croplands, and the fertilization effe

156 er the genetic basis of natural variation in SOC of Brassica napus by genome- and transcriptome-wide

157 nce aggregate stability, as well as increase SOC concentration in bulk soils and all soil aggregate s

158 rrier to implementing programmes to increase SOC at large scale, is the need for credible and reliabl

159 re humid regions are more likely to increase SOC only, while some colder regions have yield losses an

160 the climate mitigation induced by increased SOC storage is generally overestimated if associated N(2

161 et the climate change benefit from increased SOC storage.

162 Finally, PSR increased SOC content via its positive influence on microbial biom

163 ), a powerful greenhouse gas, and increasing SOC may influence N(2) O emissions, likely causing an in

164 ricultural management options for increasing SOC stocks.

165 amounts of (14) C-CO(2) are assimilated into SOC (74.3-175.8 mg (14) C kg(-1) ) and microbial biomass

166 the conversion of plant organic matter into SOC, yet the relationship between plant diversity, soil

167 hern part of the region is predicted to lose SOC.

168 on diffusion is kinetically favorable at low SOC and planar diffusion along (003) layers dominates at

169 trees had greater soil respiration and lower SOC in organic soil horizons than heather control plots.

170 e review methods and challenges of measuring SOC change directly in soils, before examining some rece

171 in combination with defective STIM1-mediated SOC channel activation, while Ca2+ store content and ago

172 The microbial SOC model based on this concept reproduces long-term dat

173 (-8.2 +/- 5.1% or -3.9 +/- 2.8%), and minor SOC gain (1.8 +/- 1.0%) in response to 5 degrees C warmi

174 o the protection afforded to downward-moving SOC by depth, indicated by much longer residence times o

175 Patients received neoadjuvant SOC chemotherapy (FOLFIRINOX or gemcitabine/nab-paclitax

176 on due to the priming of downward-moving new SOC from upper layers on native old SOC in deeper layers

177 We evaluate the amount of SOC that can be stored as well as resulting changes in N

178 The GP had the greatest amounts of SOC, total N (TN), and microbial biomass carbon (MBC) an

179 nitiative and the FAO's Global assessment of SOC sequestration potential (GSOCseq) programme.

180 n pool-based models, which assume classes of SOC with internally homogenous physicochemical propertie

181 lthough they are widely used, comparisons of SOC stocks at fixed depth (FD) intervals are subject to

182 al associations based on the coordination of SOC particles to metal-(hydr)oxide cores.

183 The decay of SOC in these plots has been monitored for decades since

184 tended to decrease and the decomposition of SOC tended to increase leading to a loss of SOC with cli

185 ators are essential to unravel the degree of SOC decomposition and accumulation, and a combination of

186 vature when the entire vertical dimension of SOC is measured and fine-resolution (3 m) digital elevat

187 In natural watersheds, the flux of SOC transformation is mainly driven by the flux of SOC t

188 ansformation is mainly driven by the flux of SOC transport; but in the consolidated gully, the transp

189 es with or without spin-up initialization of SOC.

190 SOC tended to increase leading to a loss of SOC with climate change compared to a baseline scenario

191 The magnitude of SOC can be tuned by the substituent groups (e.g. heavy a

192 enhanced carbon sink, where the magnitude of SOC increase rate (1.0 [Formula: see text]) is about twi

193 IMICS can resolve the dominant mechanisms of SOC decomposition and stabilization and that it can be a

194 Changes in the multi-model median (MMM) of SOC were used as descriptors of the ensemble performance

195 the globe, we find that downward movement of SOC along the soil profile reduces SOC loss under warmin

196 veals the vital role of downward movement of SOC in reducing SOC loss under global warming.

197 new vision for a global framework for MRV of SOC change, to support national and international initia

198 e collected a set of in situ observations of SOC, litterfall and soil properties from 206 sites cover

199 ithelium (FTE) cells, the cells of origin of SOC.

200 rease confidence in long-term predictions of SOC dynamics by reducing the uncertainty in model estima

201 Previous regional predictions of SOC trends under climate change often ignore or do not e

202 sing in situ observations of a wide range of SOC stocks over large spatial scales before their introd

203 SOC concentrations and the sensitivities of SOC to variation in soil temperature, clay content and l

204 carbon sequestration and the sensitivity of SOC stocks to climate and land-use changes.

205 understanding of temperature sensitivity of SOC under long-term agricultural management is very limi

206 es might be unfavorable for the stability of SOC in N-rich and P-poor tropical forests.

207 on the source, decomposition, and storage of SOC in estuarine wetlands with four vegetation types, in

208 prognostic and therapeutic stratification of SOC.

209 neously re-established spatial structures of SOC and TN in bioenergy croplands, which little varied w

210 indicated by much longer residence times of SOC in deeper layers.

211 scale the rapidly evolving understanding of SOC formation and stabilization based on laboratory and

212 aining paired-comparison empirical values of SOC and different types of perennial crops (perennial gr

213 ving new SOC from upper layers on native old SOC in deeper layers.

214 d-localization nuclei in the superior olive (SOC) as well as other computationally important centers.

215 model to examine the effect of adaptation on SOC for corn and soybean production in the U.S. Corn Bel

216 erceived beneficial effects of N addition on SOC storage in tropical forest soils.

217 ntations) the physicochemical constraints on SOC deprotection and microbial turnover in MIMICS, the e

218 ricultural land use has a profound impact on SOC dynamics, and few studies have explored how agricult

219 inputs exert a disproportionate influence on SOC formation, but few field studies have explicitly tes

220 of climate, soil properties, and landform on SOC dynamics.

221 onments, evaluated the effect of each QTL on SOC, and analyzed selection in QTL regions during breedi

222 r >=3 months, or had completed dabigatran or SOC treatment in the DIVERSITY trial (NCT01895777) and h

223 The overall SOC content and CMI in arable land were almost the lowes

224 To date, efforts to predict SOC dynamics have rested on pool-based models, which ass

225 C movement in controlling whole-soil profile SOC dynamics in response to warming is due to the protec

226 cts of agricultural land use on soil profile SOC dynamics varied with soil characteristics and topogr

227 of the fine-scale variation in total profile SOC within a 1.8 km(2) semi-arid catchment in Idaho, U.S

228 sceptible to errors not only for quantifying SOC stocks but also for soil mass-based properties such

229 velopments that show promise for quantifying SOC.

230 prominent expression of alpha7 nAChRs in rat SOC, suggesting possible engagement of ACh-mediated modu

231 7 US institutions with the intent to receive SOC axi-cel.

232 anesthesia were compared with eyes receiving SOC.

233 tion were 2.3 +/- 0.4 for patients receiving SOC and 2.2 +/- 0.6 in patients receiving -10 degrees C

234 anesthesia versus 44% of patients receiving SOC.

235 locally advanced unresectable PDAC receiving SOC neoadjuvant chemotherapy and chemoradiation.

236 the Beat AML sub-studies and those receiving SOC (induction with cytarabine + daunorubicin (7 + 3 or

237 vement of SOC along the soil profile reduces SOC loss under warming.

238 role of downward movement of SOC in reducing SOC loss under global warming.

239 mentally demonstrated to negatively regulate SOC.

240 rved year), indicating sufficiently reliable SOC estimates.

241 ification methods included each laboratory's SOC, which included matrix-assisted laser desorption ion

242 the adaptation scenarios, leading to similar SOC stocks under different climate change scenarios.

243 turnover in MIMICS, the errors of simulated SOC concentrations across sites were further decreased.

244 Simutaneously, SOC in WSA(>5 mm) affected SOC concentration in bulk soi

245 Since SOC content of soils cannot be easily measured, a key ba

246 provides the first estimation of whole-soil SOC changes under warming and additional NPP required to

247 s, which ultimately contribute to the stable SOC pool.

248 Here, the strong SOC from topological insulators (TIs) is utilized to pro

249 Subsoil SOC decreases were more likely to occur in high relief a

250 arable projections to the observed long-term SOC changes under warming only on 480- and 729-day.

251 ost the accuracy and confidence of long-term SOC projections.

252 reliable tool for predictions of terrestrial SOC dynamics under future climate change.

253 The results indicated that SOC change caused by agricultural land use was depth dep

254 emities (whales, bats, jerboa) revealed that SOC development correlates with the extent of mechanical

255 Mathematical modeling revealed that SOC reduces mechanical stress within the growth plate.

256 rocytes to mechanical stress and showed that SOC protects these cells from apoptosis caused by extens

257 Altogether, these findings suggest that SOC has evolved to protect the hypertrophic chondrocytes

258 The SOC is capped by six interstitial sulfur atoms, giving a

259 The SOC, TN, SOC/TN (C: N), delta(13)C and delta(15)N were q

260 Besides the SOC induced ISC pathway, triplet excited states are also

261 43/57) was significantly higher than in the SOC arm (34%, 18/53; P < .001; relative risk [RR] 2.48,

262 in the primary care arm, compared to in the SOC arm (49% [28/57] and 30% [16/53], respectively; P =

263 Women in the SOC arm reported that 17.4% (71/408) of their partners t

264 n empirical model to estimate changes in the SOC content under crops as a function of time, land use,

265 Ts, and cryoprecipitate) versus 87.2% in the SOC group (P < 0.001).

266 nsfusion, there were no such patients in the SOC group (P = 0.012).

267 The safety and efficacy of axi-cel in the SOC setting in patients with relapsed/refractory LBCL wa

268 1980s and 2010s, this study investigated the SOC changes of the soil profile caused by agricultural l

269 rmula: see text]) is about twice that of the SOC decrease rate (- 0.5 [Formula: see text]) in the sur

270 The results showed that the SOC content increased by 3.78 g C/kg in the topsoil (0-2

271 Our theory reveals that the SOC-modified interference, immiscibility, and interactio

272 36: 70 to the primary care arm and 66 to the SOC arm.

273 in yields and associated carbon input to the SOC pool counteracted the increased decomposition in the

274 cipitate) in the TEG group compared with the SOC group.

275 nal ZUMA-1 trial, 129 patients (43%) in this SOC study would not have met ZUMA-1 eligibility criteria

276 The SOC, TN, SOC/TN (C: N), delta(13)C and delta(15)N were quantified

277 ulting in comparable levels of anesthesia to SOC with a reduction in procedure time.

278 Compared to SOC NAATs, the positive agreement of the Xpert test was

279 At 8 months, compared to SOC, the YPT group demonstrated increased LDKT readiness

280 microbial residues and their contribution to SOC accumulation in a tropical coastal forest.

281 es and the microbial residue contribution to SOC is still not well understood.

282 microbial residues and their contribution to SOC were presumably due to enhanced recycling of microbi

283 microbial residues and their contribution to SOC, whereas N addition had no significant effect.

284 e in soil and be the dominant contributor to SOC accrual in diversified perennial bioenergy crops.

285 he ePlex BCID-GP Panel compares favorably to SOC and targeted molecular methods for the identificatio

286 d the contribution of microbial necromass to SOC, respectively, that should serve as valuable metrics

287 k reshapes dialogue around issues related to SOC management in a changing world.

288 tions strengthen agroecosystem resistance to SOC loss.

289 The ratios of microbial biomass to total SOC predicted by MIMICS agree well with independent obse

290 theoretically give rise to giant Rashba-type SOC.

291 For each agricultural land use, SOC decreases in deep soils only occurred in high relief

292 ations were also identified among variables (SOC > TN > delta(15)N > C: N > delta(13)C).

293 will decline by 4% (~80 Pg) on average when SOC reaches the steady state under 2 degrees C warming,

294 decreases in the 20-60 cm soil layers, while SOC decreases only occurred in the 40-60 cm soil layer f

295 ated, 22 with cooling anesthesia and 22 with SOC.

296 ass turnover) was negatively associated with SOC content and microbial respiration rates.

297 r gene modules significantly associated with SOC were identified by analyzing population transcriptom

298 In combination with SOC, CMI and soil physical properties, we argued that al

299 lower use of blood components compared with SOC (transfusion guided by INR and PLT count), without a

300 tential benefit for eculizumab compared with SOC in preventing acute AMR in recipients sensitized to