ライフサイエンスコーパス: yr

1 yr BP and maize (Zea mays) at about 6,850 cal.

2 yr BP) that coincide with markedly increased mollusc col

3 yr BP), manioc (Manihot sp.) at about 10,350 cal.

4 yr BP, in the Llanos de Moxos (Bolivia).

5 yr BP, inhabitants of this region began to create a land

6 yr BP, primarily driven by increasing frequency and stre

7 Here we present a 12,000 yr continuous U/Th-dated precipitation record from a Gua

8 n of a human pathogen over a period of 5,000 yr.

9 alaeolithic (MP) occupation dates to >51,000 yr BP.

10 tients (0.72 +/- 0.02 yr/yr vs 0.03 +/- 0.01 yr/yr; p < 0.0001).

11 equates to a linear rate of less than 0.01%/yr.

12 eath: 0.10% +/- 0.02%/yr vs -0.21% +/- 0.01%/yr; p < 0.0001).

13 r study period (adjusted relative risk, 1.01/yr; 0.96-1.06) nor did the proportion of acute respirato

14 1]; nonelective, nontrauma: odds ratio 1.014/yr [1.012-1.016/yr; p < 0.0001]; interaction: p < 0.0001

15 nontrauma: odds ratio 1.014/yr [1.012-1.016/yr; p < 0.0001]; interaction: p < 0.0001).

16 nelective, nontrauma patients (0.72 +/- 0.02 yr/yr vs 0.03 +/- 0.01 yr/yr; p < 0.0001).

17 d New Zealand risk of death: 0.10% +/- 0.02%/yr vs -0.21% +/- 0.01%/yr; p < 0.0001).

18 yr, p = 0.04), and RRMS (INL:-0.10 +/- 0.04%/yr, p = 0.01; ONL:-0.13 +/- 0.05%/yr, p = 0.01), whereas

19 as compared to controls (INL:-0.09 +/- 0.04%/yr, p = 0.03; ONL:-0.12 +/- 0.06%/yr, p = 0.04), and RRM

20 discharge care (adjusted relative risk, 1.04/yr; 0.97-1.11).

21 +/- 0.04%/yr, p = 0.01; ONL:-0.13 +/- 0.05%/yr, p = 0.01), whereas they were similar in RRMS and con

22 tle admixture event dated to circa 750-1,050 yr ago, which has shaped the genome of today's cattle in

23 +/- 0.04%/yr, p = 0.03; ONL:-0.12 +/- 0.06%/yr, p = 0.04), and RRMS (INL:-0.10 +/- 0.04%/yr, p = 0.0

24 9%/yr, p < 0.001) and GCIPL (-0.27 +/- 0.07%/yr, p < 0.001) thinning, as compared to RRMS.

25 ssociated with faster pRNFL (-0.34 +/- 0.09%/yr, p < 0.001) and GCIPL (-0.27 +/- 0.07%/yr, p < 0.001)

26 gle year of exacerbations) and recurrent (>1 yr) exacerbation patterns, using logistic regression.

27 n of minimal residual disease (MRD) within 1 yr after ASCT at the previously validated threshold of >

28 est is in the range 70-117 t CO(2) eq ha(-1) yr(-1) (95% confidence interval, CI), with CO(2) and N(2

29 ting, increasing to ~7.99 +/- 0.95 Mg ha(-1) yr(-1) when a 'perfect' plantation was modelled.

30 tter (15.6 +/- 1.4 vs 14.8 +/- 2.2 Mg ha(-1) yr(-1)) and slightly lower estimated ethanol energy yiel

31 aried much more (-3.4 to 9.8 Mg CO(2) ha(-1) yr(-1)), indicating that the latter dominates biogenic C

32 across cities (-2.1 to -0.87 Mg CO(2) ha(-1) yr(-1)), while emissions from the carbon stock change du

33 , the meadow now offsets 0.42 tCO(2)e ha(-1) yr(-1), which is roughly equivalent to the seagrass sequ

34 e will be depleted by between 4-19 kg ha(-1) yr(-1), with average losses of P due to erosion by water

35 a, Mexico (GOC), we collected a continuous 1-yr temperature time series at ~5 m water depth at 16 sit

36 ffer significantly between the two groups (1-yr survival = 85.5% and 80.7% in extracorporeal membrane

37 l plants flower a single time during their 1-yr life cycle, investing much of their energy into rapid

38 ents (male:female, 32:7; mean age, 53 +/- 10 yr [range, 29-79 yr]; Black and minority ethnic, n = 25

39 At 10 yr after the last nutrient application we quantified lon

40 the timing of annual severe bleaching >= 10 yr (>= 20 yr) for 38% (9%), 15% (1%), and 1% (0%) of cor

41 Over the last 10 yr there have been major advances in documenting and und

42 LRR than were those with margins >=2 mm (10-yr LRR rate, 30.9% vs 5.4%, respectively; hazard ratio,

43 gs of intention-to-treat and per-protocol 10-yr cancer-free survival differences were -0.5% (95% conf

44 provide reasonable bounds for the actual 100 yr warming impact.

45 For the 100 yr GWP, other model uncertainties (e.g., static GWP valu

46 y is to assess the implications of using 100 yr and 20 yr static and dynamic global warming potential

47 median annualized impact exceeds pound 100m.yr(-1).

48 e analysed tree-ring chronologies across 109 yr of monthly climatic variation (1901-2009) for 14 spec

49 re availability and site conditions over 111 yr.

50 hy volunteers across infancy/childhood (2-12 yr), maturity (20-50 yr), and older adulthood (>50 yr).

51 = 3.18; p = 0.001) in both adults (age > 12 yr) and children (age <= 12 yr), increasing by 9-100% pe

52 of lumacaftor-ivacaftor in adolescents (>=12 yr) and adults (>=18 yr) in a real-life postapproval set

53 adults (age > 12 yr) and children (age <= 12 yr), increasing by 9-100% per year since 2008.

54 egion has not increased significantly for 13 yr.

55 An analysis of a 1300-yr control integration of a comprehensive climate model

56 Data from 354 patients (mean age 55 +/- 14 yr, 28.5% male, median admission Glasgow Coma Scale 14 [

57 0 patients (65% male; mean +/- SD, 60 +/- 14 yr old) with septic shock (30%), hemorrhagic shock (15%)

58 red by Southern blotting at baseline and ~14 yr thereafter.

59 th, unmanaged Fagus sylvatica forest over 14 yr, including six mast years.

60 respiratory distress syndrome (age 64 +/- 15 yr, body mass index 26 +/- 6 kg/m, PaO2/FIO2 147 +/- 42,

61 patients were analyzed (mean age, 69 +/- 15 yr; 23% female; 12% of hospital admission survival): cap

62 .44-0.79; P trend < 0.0001] higher FVC at 15 yr than boys in the lowest trajectory).

63 We established a 15-yr gradient of old-field succession to examine the herbi

64 at has fascinated researchers for almost 150 yr.

65 in children (>5 yr old), adolescents (12-17 yr old), and adults with asthma were included.

66 or in adolescents (>=12 yr) and adults (>=18 yr) in a real-life postapproval setting.Methods: The stu

67 Pediatric patients (< 18 yr old) with a severe isolated traumatic brain injury we

68 nd dated between 31210-33103 and 18334-19860 yr cal BP (2sigma).

69 7 included patients was 56.1 years (SD, 16.2 yr), 61% of whom were male.

70 eter on microcores sampled weekly during a 2 yr period.

71 ulation: n = 141,937), matched on age (+/- 2 yr), sex, region of residence, and hospitalization year.

72 or Pediatric Quality of Life Inventory (>=2 yr old).

73 Toddler Quality of Life Questionnaire-97 (<2 yr old) or Pediatric Quality of Life Inventory (>=2 yr o

74 positively related to summer precipitation 2 yr before (R(2) = 0.85), and negatively to precipitation

75 s measured in two cohorts of children aged 2 yrs (N = 487) and 7-9 yrs (N = 218).

76 ow that the mean CAR is 161.8 +/- 6 g Cm(-2 )yr(-1), and the conterminous US tidal wetlands sequestra

77 We project 0.6-6.0 GtCO(2 )yr(-1) in global mitigation by 2055 at costs of 2-393 bi

78 sole (PCA) at Lomonosovfonna (23.5 pg cm(-2) yr(-1)) and Kongsvegen (14.1 pg cm(-2) yr(-1)).

79 d OCP flux at Lomonosovfonna (81.7 pg cm(-2) yr(-1)) and Kongsvegen (60.6 pg cm(-2) yr(-1)), and at A

80 f sediment mass accumulation rates (g cm(-2) yr(-1)) and sediment accumulation rates (cm yr(-1)) more

81 m(-2) yr(-1)) and Kongsvegen (60.6 pg cm(-2) yr(-1)), and at Austfonna, but not at Holtedahlfonna whe

82 m(-2) yr(-1)) and Kongsvegen (14.1 pg cm(-2) yr(-1)).

83 pite tripling the N(2)O flux to 0.06 g m(-2) yr(-1) and increasing CH(4) 8-fold to 0.8 g m(-2) yr(-1)

84 ined global warming potential of 264 g m(-2) yr(-1) CO(2)-e over 100 years, and it increased to 351 g

85 -1), our study-wide average of 340 g C m(-2) yr(-1) indicated that L. hyperborea forests are highly p

86 r 100 years, and it increased to 351 g m(-2) yr(-1) with the removal of extreme rain events.

87 ields (10.6 +/- 1.0 vs 11.8 +/- 2.9 MJ m(-2) yr(-1)) as corn grain with 75% stover collection.

88 re the playa source was dominant (89 g m(-2) yr(-1)) were less than, but approaching the scale of, th

89 estimates of APPP from 300 to 500 g C m(-2) yr(-1), corresponding to "eutrophic" to "hypertrophic" c

90 een sites, ranging from 166 to 738 g C m(-2) yr(-1), our study-wide average of 340 g C m(-2) yr(-1) i

91 ) and increasing CH(4) 8-fold to 0.8 g m(-2) yr(-1), the meadow now offsets 0.42 tCO(2)e ha(-1) yr(-1

92 average DACCS scale-up rates of 1.5 GtCO(2)/yr would require considerable sorbent production and up

93 entury carbon removal goals of 10-20 GtCO(2)/yr.

94 ng facilities (i.e., producing >=100 ktCO(2)/yr).

95 45Q for the power sector, e.g., 500 ktCO(2)/yr, the tax credit incentivizes the capture of roughly 3

96 decline by 1.11 (0.23-1.98) ml/min/1.73 m(2)/yr in patients with CKD and by 2.41 (1.49-3.32) ml/min/1

97 CKD and by 2.41 (1.49-3.32) ml/min/1.73 m(2)/yr in patients without CKD.

98 lead to the avoidance of roughly 195 MtCO(2)/yr (188 MtCO(2)/yr qualifying for 45Q).

99 entivizes the capture of roughly 397 MtCO(2)/yr at a 90% capture efficiency or 75% of the emissions i

100 the potential to avoid roughly 68.5 MtCO(2)/yr at costs below $40/tCO(2) delivered.

101 (2) collection hubs, emissions of 40 MtCO(2)/yr can be avoided within 100 miles of the existing Louis

102 dance of roughly 195 MtCO(2)/yr (188 MtCO(2)/yr qualifying for 45Q).

103 d with an opportunity to scale to 19 MtCO(2)/yr.

104 sess the implications of using 100 yr and 20 yr static and dynamic global warming potential (GWP) app

105 g of annual severe bleaching >= 10 yr (>= 20 yr) for 38% (9%), 15% (1%), and 1% (0%) of coral reef si

106 ne therapy has been shown within the last 20 yr to correct the T cell immunodeficiency caused by gamm

107 s increased substantially during the last 20 yr.

108 ate and atmospheric change over the past 200 yr (including Pinus strobus, Platycladus orientalis, Pop

109 al American rainfall increased within a 2000 yr period from a persistently dry state to an active con

110 We examined a cohort (0-21 yrs.) who have undergone esophagogastroduodenoscopy and

111 We revisited a 23-yr-old field experiment where N and P had been applied t

112 In the 25 yr since the gene encoding the microphthalmia-associated

113 median follow-up of 11 years (range 1 mo-25 yrs), symptomatic recurrence was observed in 61%: 15 pat

114 ronosequence (1, 2, 8, 14, 30, 49 and c. 260 yr) in cold-temperate forests of the Great Khingan Mount

115 Senegalese adults aged 18-50 yr (average, 29 yr) were vaccinated with the Ebola vaccine candidate chi

116 However, they only emerge 1-3 yr after infection, and show a number of highly unusual

117 On 5 separate visits, 12 young (23 +/- 3 yr, 7 M/5F) and 12 older (67 +/- 6 yr, 5 M/7F) subjects

118 eight locations across the central USA for 3 yr and conducted quantitative trait locus (QTL) mapping

119 S plants in a glasshouse common garden for 3 yr.

120 ciated with increased dialysis duration (> 3 yr) and phosphatemia (> 2.5 mmol/L), with lower albumine

121 er age (adjusted odds ratio for 13-17 vs < 3 yr, 2.1; 95% CI, 1.5-3.1) and male gender (adjusted odds

122 ric and torpedo models have been used for 30 yr to explain how transcription terminates on protein-co

123 ction of DMSP has remained enigmatic for >30 yr.

124 s 67%, with 1,058 respondents (median age 33 yr; 71% women; 68% nursing staff).

125 ia like early-onset breast cancer (age 20-35 yr) provides a condition for an unbiased estimate of the

126 Most were young (38 yrs) males (84%) with blunt injuries (51%).

127 age was 27 years (interquartile range, 15-39 yr); 52.5% were male.

128 hms, these children were younger (0.4 vs 1.4 yr; p = 0.005) and more likely to have a respiratory eti

129 ed monthly ground-based LiDAR surveys over 4 yr at an Amazon forest site.

130 odified floral phenotypes were stable over 4 yr of study.

131 art turgor-driven growth model to simulate 4 yr of hourly stem radial increment from Picea abies (L.)

132 ions from China rose by 1.1 +/- 0.4 Tg CH(4) yr(-1) from 2010 to 2015, culminating in total anthropog

133 er heaters emitted 1400 [1240, 1560] g CH(4) yr(-1) on average, 0.39% [0.34%, 0.43%] of their natural

134 rs emitted 2390 [95% CI: 2250, 2540] g CH(4) yr(-1) on average, 0.93% [0.87%, 0.99%] of their natural

135 tted an estimated 82.3 [73.2, 91.5] Gg CH(4) yr(-1), 0.40% [0.35%, 0.44%] of all natural gas consumed

136 l oceanic CH(4) emissions between 6-12TgCH(4)yr(-1), narrowing the range adopted by recent atmospheri

137 ed by recent atmospheric budgets (5-25TgCH(4)yr(-1)) by a factor of three.

138 y estimates total emissions of 0.53 Tg CH(4)/yr [0.40-0.71 Tg CH(4)/yr, 95% CI] and corresponds to a

139 ions of 0.53 Tg CH(4)/yr [0.40-0.71 Tg CH(4)/yr, 95% CI] and corresponds to a loss rate of 2.9% [2.2-

140 ate uptake and assimilation rates in four 40-yr-old monoculture coniferous plantations (Pinus koraien

141 ility patients were older (mean age 53 vs 44 yr; p < 0.001) and had longer hospital durations (length

142 was older (median 62 yr treated pooled vs 46 yr placebo), and a greater percentage had more than 2 or

143 egnant women of reproductive age (WRA; 15-49 yr) and preschool children (PSC; 6-59 mo).

144 ]; p < 0.0001 and cost range $147,548 [18-49 yr] to $105,350 [80-90 yr]; p < 0.0001).

145 group (length of stay range from 17 d [18-49 yr] to 9 d [80-90 yr]; p < 0.0001 and cost range $147,54

146 With a 1.5 yr time-series of 2324 in situ measurements of daily pre

147 The mean age was 69.3 years (10.5 yr), 119 were men (66.1%).

148 ecutive patients (62% male; median age, 58.5 yr) underwent endoscopic examination after extubation.

149 eneration (at an average parental age of 7.5 yr), much lower than found in direct estimates from grea

150 The new model was tested using a 5 yr drought/heat field experiment on an established pinon

151 /systemic corticosteroid use in children (>5 yr old), adolescents (12-17 yr old), and adults with ast

152 In the past 5 yr or so, and with the advent of superresolution microsc

153 infants (<18 mo) and children (>=18 mo to 5 yr) during AVB and after convalescence.

154 to diagnosis of 10.3 years (range, 6.4-15.5 yrs).

155 this, dCLKT exhibited improved 1-, 3-, and 5-yr patient and kidney survival (p=0.02) and decreased le

156 The survey based on 36 RCTs (median 5-yr citation index 85 (24-474), from 21 different countri

157 vs 3.1%, P = 0.31), and overall survival (5-yr survival: 48.6% vs 48.7%, P = 0.76; multivariable-adj

158 TAM) macrophages that were associated with 5-yr disease-free survival rates of 27.8% and 0.2%, respec

159 healthy UK and Senegalese adults aged 18-50 yr (average, 29 yr) were vaccinated with the Ebola vacci

160 infancy/childhood (2-12 yr), maturity (20-50 yr), and older adulthood (>50 yr).

161 most of the world's coral reefs within 30-50 yr.

162 ed enigmatic since its initial discovery >50 yr ago, but our understanding of the mechanisms involved

163 aturity (20-50 yr), and older adulthood (>50 yr).

164 sts in western Eurasia that were up to 6,500 yr old.

165 ually a disease of adulthood (median age: 51 yrs).

166 tructive sleep apnea (75% male; mean age, 52 yr; apnea-hypopnea index, 49/h; baseline sleepiness scor

167 management 33 degrees C were older (57 vs 52 yr; p < 0.05) and had more arrests of cardiac etiology (

168 age was 56 years (interquartile range, 43-56 yr), 75% (n = 54) were men.

169 than males and had worse OS (median OS 2.56 yrs vs 2.08; P = 0.034).

170 9% of the population, were younger (39 vs 57 yr old, respectively; p < 0.0001), Hispanic (83%; p < 0.

171 Fourteen patients (median age, 58 yr [interquartile range, 56-62 yr]; Sequential Organ Fai

172 was obtained from 40 patients (mean age, 58 yr [SD, 10], hemoglobin A1c 36.8 mmol/mol [4.9 mmol/mol]

173 age was 56 years (interquartile range, 52-59 yr), 3,933 were male (63%), 3,019 had out-of-hospital ca

174 62% men, median [interquartile range] age 59 yr [48-67 yr]) were included in the study.

175 ients, the mean age was 61.0 years (+/- 17.6 yr), 281 were females (52.9%), and 164 (30.9%) were acti

176 es were similar (fire return interval of 4-6 yr), seeders were restricted to regions with more freque

177 ad been randomized (57% male; mean age, 53.6 yr).

178 (23 +/- 3 yr, 7 M/5F) and 12 older (67 +/- 6 yr, 5 M/7F) subjects consumed 1 L of distilled water, G-

179 ect soil fungal community development over 6 yr along a manipulated pH gradient in a large-scale expe

180 Thirty-eight patients (mean 12 +/- 6 yrs) were identified; median (IQR) follow-up was 19 (5-3

181 15 men, 38 +/- 6 yrs, n = 10 women, 32 +/- 6 yrs, mean +/- SD).

182 ve healthy crewmembers (n = 15 men, 38 +/- 6 yrs, n = 10 women, 32 +/- 6 yrs, mean +/- SD).

183 ubjects [mean (standard deviation): age 44.6 yrs (13.0), body mass index 25.4 kg/m2 (3.6), 60.1% fema

184 Here we conducted a 6-yr field experiment in a high-altitude (4600 m asl) alpi

185 s shifted to be 6 d earlier over the last 60 yr, while their flight period length decreased by 2 d.

186 , the odds of death increased with age (>=60 yrs.), admission from a nursing facility, Charlson score

187 three strongest regional droughts over a 60-yr period.

188 edian age, 58 yr [interquartile range, 56-62 yr]; Sequential Organ Failure Assessment score, 14 [12-1

189 The treated group was older (median 62 yr treated pooled vs 46 yr placebo), and a greater perce

190 railty in older (>=65 yr) and younger (18-64 yr) candidates.

191 tients (median [interquartile range] age: 64 yr [53-71 yr] and Acute Physiology and Chronic Health Ev

192 and function) measures recorded at age 60-64 yrs in a British birth cohort study.

193 Older adults (>= 65 yr) had significantly higher mortality compared with you

194 Rationale: Older adults (>=65 yr old) account for an increasing proportion of patients

195 red the prevalence of frailty in older (>=65 yr) and younger (18-64 yr) candidates.

196 rtality compared with younger patients (< 65 yr) (54.7% vs 36.5%; p < 0.0001).

197 ty-four patients (693 < 65 yrs and 281 >= 65 yrs) were included.

198 Nine hundred seventy-four patients (693 < 65 yrs and 281 >= 65 yrs) were included.

199 n electricity prices range from pound 29-66m.yr(-1) GBP2018, whilst in 20% of cases from pound 66-95m

200 ere 57 years old (interquartile range, 47-67 yr old).

201 edian [interquartile range] age 59 yr [48-67 yr]) were included in the study.

202 epsis patients were younger (median 66 vs 68 yr) but had more comorbidities (median Elixhauser score

203 lable in 164 patients (average 58.6 +/- 18.7 yr old, 45% females).

204 were younger (49.0 +/- 21.6 vs 60.6 +/- 18.7 yr; p < 0.0001), predominantly male (73.1% vs 53.9%; p <

205 B surveillance records (median follow-up 4.7 yr).

206 (interquartile range) of 61 years old (51-70 yr old) with a high severity of illness (Acute Physiolog

207 educed vaccine responses in the elderly (>70 yr).

208 dian [interquartile range] age: 64 yr [53-71 yr] and Acute Physiology and Chronic Health Evaluation I

209 edian [25th-75th percentile] age, 71 [64-72] yr; 55% male; body mass index, 24 [21-29]; FEV(1)% predi

210 91 women (40.7%); median age 63 years (49-74 yr); median Simplified Acute Physiology Score II 28 (19-

211 age was 66 years (interquartile range, 56-75 yr).

212 nts was 67 years (interquartile range, 60-75 yr).

213 continued expansion into central Europe 788 yr ago (1227 AD).

214 , 32:7; mean age, 53 +/- 10 yr [range, 29-79 yr]; Black and minority ethnic, n = 25 [64%]), there was

215 (50% female; mean +/- SD: age, 63.7 +/- 6.8 yr; FEV(1), 41.6 +/- 7.3% predicted; modified Medical Re

216 ults showed our sample of gamers (24 +/- 2.8 yrs; 88.64% Male), 30% were addicted, 30% were problemat

217 FEV(1)% predicted over a range of ages (6-82 yr).

218 four age bands (16-64, 65-74, 75-84, and 85+ yr) admitted to ICUs contributing to the Case Mix Progra

219 rts of children aged 2 yrs (N = 487) and 7-9 yrs (N = 218).

220 n age, 34.7 [interquartile range, 29.4-41.9] yr), 30-day mortality was 14.6% (64/439) and associated

221 pients was 54.8 +/- 15.4 years (range, 18-90 yr).

222 tay range from 17 d [18-49 yr] to 9 d [80-90 yr]; p < 0.0001 and cost range $147,548 [18-49 yr] to $1

223 range $147,548 [18-49 yr] to $105,350 [80-90 yr]; p < 0.0001).

224 state to an active convective regime at 9000 yr BP and has remained strong thereafter.

225 7 patients [F:M 1:1; median age = 41 (12-95) yrs], through laparotomy (n = 157, 34%) or laparoscopy (

226 1]; nonelective, nontrauma: odds ratio 0.957/yr [0.955-0.959/yr; p < 0.0001]; interaction p < 0.0001)

227 nontrauma: odds ratio 0.957/yr [0.955-0.959/yr; p < 0.0001]; interaction p < 0.0001).

228 18, whilst in 20% of cases from pound 66-95m.yr(-1).

229 ng trauma patients (trauma: odds ratio 0.976/yr [0.968-0.984/yr; p < 0.0001]; nonelective, nontrauma:

230 ts (trauma: odds ratio 0.976/yr [0.968-0.984/yr; p < 0.0001]; nonelective, nontrauma: odds ratio 0.95

231 an annual increase (trauma: odds ratio 0.986/yr [0.981-0.990/yr; p < 0.0001]; nonelective, nontrauma:

232 se (trauma: odds ratio 0.986/yr [0.981-0.990/yr; p < 0.0001]; nonelective, nontrauma: odds ratio 1.01

233 sumption of the EU is estimated at ~4000 t B yr(-1), which could be sustained by the B currently inst

234 nts providing benefits beyond US$4.3 billion yr(-1).

235 g (on-farm) benefits of US$14.6-19.5 billion yr(-1).

236 ees by the radiative equivalent of 0.77 Pg C yr(-1) under nitrogen deposition rates projected for 203

237 ux of atmospheric CO(2) as 26.2 +/- 4.7 Tg C yr(-1) over the open NW European shelf.

238 s US tidal wetlands sequestrate 4.2-5.0 Tg C yr(-1).

239 om L. hyperborea is estimated at ~ 7.61 Tg C yr(-1).

240 gan only ~15,935 +/- 75 to 15,130 +/- 20 cal yr B.P., suggesting that our estimation of ~16,560 to 15

241 that our estimation of ~16,560 to 15,280 cal yr B.P. is unsupported.

242 ion dated to the YD onset (12,785 +/- 58 cal yr BP).

243 pening of an ice-free corridor (<=14,800 cal yr B.P.), which supports the hypothesis that initial hum

244 on ages show that between ~ 2185 and 965 cal yr B.P. the drinking water in the Corriental reservoir w

245 -fold more EC (299 +/- 45 mg EC m(-2) canopy yr(-1)) compared to live oak trees (160 +/- 31 mg EC m(-

246 ive oak trees (160 +/- 31 mg EC m(-2) canopy yr(-1)).

247 treating at a steady rate of 4.5 +/- 0.63 cm yr(-1), whilst maintaining a similar profile form.

248 yr(-1)) and sediment accumulation rates (cm yr(-1)) more than doubled after 1950 in coastal depocent

249 n production in nearly 1000 Midwest counties yr(-1) over 9 years.

250 rapid directional changes reaching 1 degrees yr(-1), although the observations are controversial and

251 ates of directional change reach ~10 degrees yr(-1), typically during times of decreasing field stren

252 an ecosystem potentially accumulate 3.5 t EC yr(-1), equivalent to ~32% of annual vehicular EC emissi

253 iderable sorbent production and up to 300 EJ/yr of energy input by 2100.

254 tration potential to over 2.6 Gt CO(2)-C(eq) yr(-1), thus boosting the efficiency of utilisation of l

255 - 18.34 g/m at the rate of 10.03 +/- 12.79 g/yr and 6.25 +/- 10.28 g/m/yr, whereas in control patient

256 (7.4-10.4) Gg yr(-1) and 0.80 (0.64-1.04) Gg yr(-1), respectively.

257 South African emissions of 8.9 (7.4-10.4) Gg yr(-1) and 0.80 (0.64-1.04) Gg yr(-1), respectively.

258 ess CO(2) fixed in crop biomass, and 52.6 Gg yr(-1) of more reactive N in the environment.

259 a net atmospheric Se sink, with around 7 Gg yr(-1) of Se transferred from land through the atmospher

260 ble, and sustainable with a very large (Gton yr(-1) ) source.

261 rate at the far-downgradient plume (0.048 kg/yr compared to the near-source area (3.6 kg/yr)).

262 /yr compared to the near-source area (3.6 kg/yr)).

263 are projected to accelerate from ~2 to 6 km/yr by 2050.

264 al evidence of high basal melt rates (7-16 m yr(-1)) beneath an East Antarctic ice shelf, Shirase Gla

265 ted into the Quaternary Ice Age around 2.6 M yr ago.

266 10.03 +/- 12.79 g/yr and 6.25 +/- 10.28 g/m/yr, whereas in control patients LV characteristics did n

267 and isoetalean lycophytes, has a 400-million-yr evolutionary history that involves considerably broad

268 breast height) increased from 0.81 to 2.1 mm yr(-1) along a soil texture gradient from 0 to 67% clay,

269 predictions, the Midway data suggest ~13 mm yr(-1) of African LLSVP motion since the Oligocene.

270 of southward Hawaiian hotspot drift (~47 mm yr(-1)), and excludes true polar wander as a relevant fa

271 an mass trends are smaller by 0.63-0.88 mm . yr(-1) compared to the ocean mass trend estimated throug

272 to derive an average slip rate of 4.5-9.0 mm.yr(-1) on the master fault over the past ~610 ka and an

273 AR and control patients increased at 0.58 mm/yr.

274 ents increased at a rate of 0.60 +/- 0.80 mm/yr, which was 2.4-fold faster than in controls.

275 4 +/- 3.6 Mt/yr (or 0.62 +/- 0.08.10(12) mol/yr), our results constrain the time-averaged (2005-2015)

276 7 +/- 2.9 Mt/yr (or 0.88 +/- 0.06.10(12) mol/yr).

277 the measured CO(2) output of 27.4 +/- 3.6 Mt/yr (or 0.62 +/- 0.08.10(12) mol/yr), our results constra

278 d that ISWs could induce and suspend 78.7 Mt/yr of sediment from shelf to deep-sea areas of the north

279 ssing subaerial volcanoes at 38.7 +/- 2.9 Mt/yr (or 0.88 +/- 0.06.10(12) mol/yr).

280 jor reactive N losses amount to 1.7-9.4 Tg N yr(-1) , which corresponds to 3%-14% of the global cropl

281 s (slopes, -1.53 versus -2.41% predicted per yr; difference: 0.88; 95% confidence interval [CI], 0.30

282 re we show that a decline of 0.2 +/- 0.1 PgC yr(-1) in fire emissions during 2008-2014 relative to 20

283 l carbon sink enhancement of 0.4 +/- 0.2 PgC yr(-1) attributable to carbon cycle feedbacks, amounting

284 ined sink increase comparable to the 0.6 PgC yr(-1) budget imbalance.

285 sinks requires an additional sink of 0.6 PgC yr(-1) in the last decade to explain the observed airbor

286 ated net flux into the oceans by 0.8-0.9 PgC yr(-1), at times doubling uncorrected values.

287 xcess of 2 petagrams of carbon per year (PgC yr(-1)).

288 ontinued to decline (-0.23 discrepant-points/yr), reaching anosognosia 3.2 years before dementia onse

289 progression to MCI (-0.08 discrepant-points/yr).

290 SE) decline of 0.57 (0.25) percent predicted/yr.

291 < 0.010), MM (P < 0.001), and <45 procedures/yr (P = 0.002).

292 ) are considered high volume (>10 resections/yr), 33% offer a minimally-invasive approach, and 50% of

293 of Surgery In-Training Exam (~3750 residents/yr; response rate 99%).

294 were notably smaller (960 +/- 500 tonnes SOA yr(-1)).

295 national total for 2010 is 1,653 +/- 30 TgC yr(-1) with an uncertainty ([Formula: see text]) that ta

296 impact of $536M USD yr(-1), 4.0 million tons yr(-1) of less CO(2) fixed in crop biomass, and 52.6 Gg

297 er range of trends (-0.023 to 0.023 pH units yr(-1)) and are as likely to show long-term increase as

298 n acidification (-0.0004 to -0.0026 pH units yr(-1)) driven by increased atmospheric CO(2), coastal e

299 aggregated economic loss impact of $536M USD yr(-1), 4.0 million tons yr(-1) of less CO(2) fixed in c

300 gation by 2055 at costs of 2-393 billion USD yr(-1), with avoided tropical deforestation comprising 3