ライフサイエンスコーパス: tidal

1 The end-tidal alveolar dead space fraction ((PaCO2-PETCO2)/PaCO2

2 a site with continuous permafrost and small tidal amplitudes, fluxes are mostly affected by seasonal

3 Using the ratio between the estimated tidal and geostrophic current velocities and comparing t

4 re carved by grounded icebergs influenced by tidal and geostrophic ocean currents.

5 orientation of Sputnik Planitia arising from tidal and rotational torques can explain the basin's pre

6 0 degrees with respect to the rotational and tidal axes.

7 cated very close to the longitude of Pluto's tidal axis and may be an impact feature, by analogy with

8 e moved the feature towards the Pluto-Charon tidal axis, on the far side of Pluto from Charon.

9 large feature is very near the Pluto-Charon tidal axis.

10 in the city, they must find their way to the Tidal Basin where the Japanese trees grow.

11 -0.449; 95% CI, -0.664 to -0.234; p < 0.001; tidal: beta = -0.267; 95% CI, -0.423 to -0.111; p = 0.00

12 ) pressure during end-inspiratory pause of a tidal breath and tidal stress as the transpulmonary pres

13 ns receiving the greatest deformation from a tidal breath, thus ensuring ventilation-perfusion matchi

14 esponse to length oscillations equivalent to tidal breathing and deep inspirations.

15 althy term infants aged 5 weeks during quiet tidal breathing in unsedated sleep.

16 Testing during quiet natural sleep included tidal breathing, exhaled nitric oxide, and multiple brea

17 Once locked, Charon raises a permanent tidal bulge on Pluto, which greatly enhances the gravity

18 ins locked in place because of the permanent tidal bulge raised by Charon.

19 d in real time during the PPV, including end-tidal carbon dioxide (ETCO2), oxygen saturation (SaO2),

20 ger photoplethysmographic arterial pressure, tidal carbon dioxide concentrations and volumes, and per

21 of stations exhibit a greater than +/-50 mm tidal change per meter sea-level fluctuation.

22 s that control the formation of an efficient tidal channel network remain unclear.

23 Tidal channel networks mediate the exchange of water, nu

24 m Pleistocene fluvial systems reactivated as tidal channels during the post- Last Glacial Maximum tra

25 espiratory rate and resulting changes in end-tidal cO2 ( big up tri, openPetCO2) as well as between c

26 al volume ratio (Vd/Vt), and arterial to end-tidal CO2 difference were all higher (P<0.05) in patient

27 , semidiurnal, terdiurnal and quarterdiurnal tidal components.

28 zed to receive either inhaled xenon (40% end-tidal concentration) combined with hypothermia (33 degre

29 lly evaluate how the sum of the four largest tidal constituents, a proxy for the highest astronomical

30 each sites, including a beach scour pond and tidal creek.

31 previously established plots located along a tidal creek; 10 plots are on forest islands surrounded b

32 than the mean current and comparable to the tidal currents near the bottom.

33 The tidal cycle is important in controlling the biogeochemic

34 the persistence of the eruptions through the tidal cycle, the phase lag, and the total power output o

35 bility to measure residence time over single tidal cycles in estuaries will be useful for evaluating

36 ations in nitrogen components over flood-ebb tidal cycles, and tidal simulation experiments.

37 Regions of tidal decrease and/or amplification highlight the non-li

38 in high-resolution X-ray spectra of a nearby tidal disruption event, ASASSN-14li in the galaxy PGC 04

39 gravitational wave emission by observing two tidal disruption events that are separated by more than

40 sient events, including gamma-ray bursts and tidal disruption events.

41 low-up observations of known thermal stellar tidal disruption flares (TDFs) have not yet produced a c

42 The tidal disruption of a star by a supermassive black hole

43 mal long-duration gamma-ray bursts or in the tidal disruption of a star.

44 sional hydrodynamic simulations to study the tidal disruption of stars by such a binary in the final

45 Here we show that tidal dissipation due to lunar obliquity was an importan

46 by orbital decay and circularization due to tidal dissipation in the stars.

47 The tidal effect is supported further by nutrient profiles,

48 ation has led to constraints being placed on tidal energy generation developments.

49 a variety of environments, from low wave and tidal energy lagoons, to high energy tidal reef flats, b

50 Wave and tidal energy plants are upcoming, potentially green tech

51 his study supports the potential of wave and tidal energy plants as alternative green technologies.

52 We present a tidal evolution model starting with the Moon in an equat

53 Our tidal evolution model supports recent high-angular-momen

54 ty was an important effect during the Moon's tidal evolution, and the lunar inclination in the past m

55 ) denitrification to the atmosphere, and (3) tidal export.

56 osphere, but DMS emission from corals during tidal exposure is not well quantified.

57 nt experiment to directly test the effect of tidal exposure on the microbiome of H. heliophila, using

58 Peak plume flux lags peak tidal extension by approximately 1 rad, suggestive of re

59 as accelerated in both areas, the decline in tidal flat area has been much greater in Jiangsu than in

60 developed an automatic algorithm to estimate tidal flat areas based on the Land Surface Water Index a

61 ter coastal planning and management based on tidal flat dynamics.

62 which differ in riverine sediment supply and tidal flat management patterns.

63 AH degradation capability in seasonally cold tidal flat might be reflected in elevated expression of

64 llular responses to environmental variables (tidal flat, seawater, naphthalene, and pyruvate) and exh

65 s that either added naphthalene or pyruvate; tidal flat-naphthalene (TF-N), tidal flat-pyruvate (TF-P

66 or pyruvate; tidal flat-naphthalene (TF-N), tidal flat-pyruvate (TF-P), seawater-naphthalene (SW-N),

67 ts ecophysiological behavior in contaminated tidal flats and seawater.

68 The total area of tidal flats in the Yangtze Estuary has decreased by 36%

69 Tidal flats play a critical role in supporting biodivers

70 We used estuarine tidal flats to study the effects of changes in herbivore

71 value that exceeds the area of the remaining tidal flats.

72 eplaced forest understory vegetation along a tidal flooding gradient.

73 Between 1992 and 2014, tidal flooding of forest islands increased by 22%-117%,

74 tudies found that salt stress from increased tidal flooding prevented tree regeneration in frequently

75 Frequencies of tidal flooding, rates of tree mortality, and understory

76 d through restoration of disconnected saline tidal flows.

77 was a strong coupling between turbidity and tidal fluctuations.

78 sible for spewing briny water into space, no tidal forces are acting on Ceres.

79 icy satellites of Jupiter and Saturn, where tidal forces are responsible for spewing briny water int

80 ormation of the Earth's crust as a result of tidal forces.

81 with ocean water causes erupted flux to lag tidal forcing and helps to buttress slots against closur

82 supply or where migration upwards within the tidal frame is constrained.

83 tion capital (i.e., relative position in the tidal frame) to survive.

84 ich tidal marshes become perched high in the tidal frame, decreasing their vulnerability to accelerat

85 al being more diverse than the subtidal, and tidal height differentiation being modest but significan

86 drying cycles simulating low-, mid- and high-tidal height periodicity.

87 Differences among tidal heights within Bodega Bay were also remarkably con

88 y cyclical processes such as seasonality and tidal hydrology.

89 s well as hyperaerated lung compartments and tidal hyperaeration.

90 Tidal volume, static compliance, tidal impedance variation, end-expiratory lung impedance

91 hetics during surgery (derived from mean end-tidal inhalational anesthetic concentrations).

92 ur binary evolution model, it was spun-up by tidal interaction in a close binary and is likely to be

93 n circular, aligned orbits because of strong tidal interactions with the stellar convective envelope.

94 Tidal inundation at the upper border of this migration z

95 e', consisting of elevations that experience tidal inundation with frequencies ranging from 20% to 0.

96 vel during 1970-2005 to 4.0-5.1 m above mean tidal level by 2080-2100 and ranges from 5.0-15.4 m abov

97 0-2100 and ranges from 5.0-15.4 m above mean tidal level by 2280-2300.

98 flood event increases from 3.4 m above mean tidal level during 1970-2005 to 4.0-5.1 m above mean tid

99 luto that always faces Charon as a result of tidal locking.

100 wer V(RM) predicted high end-inspiratory and tidal lung stress (end-inspiratory: beta = -0.449; 95% C

101 EEP can improve arterial oxygenation, reduce tidal lung stress and strain, and promote more homogenou

102 se findings are applicable to large areas of tidal marsh along the U.S. Atlantic coast and in other u

103 provides the most comprehensive estimates of tidal marsh blue carbon in Australia, and illustrates th

104 owing down along natural stress gradients in tidal marsh ecosystems.

105 ion using a nine-year CO2 xN experiment in a tidal marsh.

106 e assessed the three primary fates of N in a tidal marsh: (1) retention in plants and soil, (2) denit

107 l organic carbon (OC) storage in Australia's tidal marshes (323 cores).

108 equestration is the primary process by which tidal marshes become perched high in the tidal frame, de

109 agement practices at the upland periphery of tidal marshes can facilitate or impede ecosystem migrati

110 Australia's 1.4 million hectares of tidal marshes contain an estimated 212 million tonnes of

111 sediment elevation dynamics in mangroves and tidal marshes has been gained by monitoring a wide range

112 Tidal marshes have a large capacity for producing and st

113 n N retention on a decadal timescale because tidal marshes have a relatively open N cycle and can acc

114 Australia's tidal marshes have suffered significant losses but their

115 To thrive in a time of rapid sea-level rise, tidal marshes will need to migrate upslope into adjacent

116 other 'blue carbon' habitats (mangroves and tidal marshes) seagrasses are thought to provide coastal

117 n experiments in European and North American tidal marshes.

118 her ecosystem services provided by Australia tidal marshes.

119 imed at facilitating ecosystem migration for tidal marshes.

120 gy of prominent features that do not fit the tidal model.

121 ment width by itself, the combined effect of tidal movement and temperature had a greater negative ef

122 Although tidal movement was not a significant driver of increment

123 Turbidity, temperature, tidal movement, and wave action were recorded every 10 m

124 ten shorebird taxa that refuel on Yellow Sea tidal mudflats, a threatened ecosystem that has shrunk b

125 Palaeo tidal notches are considered as one of the most precise

126 n and palaeo (Marine Isotope Stage (MIS) 5e) tidal notches on Bonaire (southern Caribbean Sea) and re

127 hic cascade emerged because reef topography, tidal oscillations, and shark hunting behaviour interact

128 discharge is tidal pumping, due to the large tidal oscillations, whereas at Point Barrow, a site with

129 nt an 8-h isocapnic exposure to hypoxia (end-tidal P(O2)=55 Torr) in a purpose-built chamber.

130 nse to a standardized step change in the end-tidal partial pressure of carbon dioxide.

131 Elevation of the end-tidal partial pressure of CO2 (PETco2) increases cerebra

132 different blood gas conditions, with the end-tidal partial pressure of oxygen (PETCO2) ranging from 4

133 This pattern suggests that tidal pumping may sustain dissimilatory nitrate reductio

134 driver of submarine groundwater discharge is tidal pumping, due to the large tidal oscillations, wher

135 ng and facies analysis suggest that elevated tidal range and bed shear stress optimized mangrove deve

136 ests that mangrove forests at sites with low tidal range and low sediment supply could be submerged a

137 Our models show that the tidal range changes most significantly in shallow areas,

138 of Bonaire, are less affected to changes in tidal range in conditions of MIS 5e sea levels.

139 ies to assess whether, in a particular area, tidal range might have been different in MIS 5e with res

140 Three tidal stream devices, one tidal range plant and one wave energy harnessing device

141 The impacts of the tidal range plant were on average 1.6 times higher than

142 hese two tools to investigate changes in the tidal range since MIS 5e.

143 uss the importance of considering changes in tidal range while reconstructing MIS 5e sea level histor

144 gy) to 20 (tidal stream), or even 115 times (tidal range) lower impact than electricity generated fro

145 their formation is closely tied to the local tidal range.

146 when collected during periods with increased tidal range: spring ebb and flood tides.

147 presence and location of regions of presumed tidal recruitment (i.e., elastance decrease during infla

148 ation by minimizing the probability of local tidal recruitment and/or overdistension.

149 cent of total gas content in lower lung) and tidal recruitment as the difference in the percent mass

150 piratory pressure indicate that, expectedly, tidal recruitment increases in dependent regions with de

151 ved: electrical impedance tomography-derived tidal recruitment with poorly aerated regions (r = 0.43;

152 gible regions of presumed overdistension and tidal recruitment.

153 poorly and nonaerated lung compartments, and tidal recruitment.

154 ave and tidal energy lagoons, to high energy tidal reef flats, but remain dependent upon suitable sub

155 Modeled climatic forcing indicates that tidal restoration to reduce emissions has a much greater

156 xtent, hold nearly ten-fold more carbon than tidal saltwater sites-indicating their importance in reg

157 In contrast, the signature of the tidal signal on pore-water temperature persisted for lon

158 alinity had a relatively short memory of the tidal signal when inland freshwater recharge was large.

159 components over flood-ebb tidal cycles, and tidal simulation experiments.

160 southern Caribbean Sea) and results from two tidal simulations, using the present-day bathymetry and

161 ound when comparing the results of the three tidal stream devices to offshore wind power plants (with

162 Three tidal stream devices, one tidal range plant and one wave

163 lants have on average 8 (wave energy) to 20 (tidal stream), or even 115 times (tidal range) lower imp

164 end-inspiratory pause of a tidal breath and tidal stress as the transpulmonary pressure difference b

165 The response to the tidal stress carries otherwise inaccessible information

166 , which modulates the amplitude of the daily tidal stress over a 14-d cycle.

167 tly associated with both end-inspiratory and tidal stress.

168 ynamics of CO2 for MBF using prospective end-tidal targeting to precisely control arterial Pco2 and P

169 Here we use tidal tomography to constrain Earth's deep-mantle buoyan

170 ward-dipping caldera ring fault, with strong tidal triggering indicating a critically stressed system

171 Tidal variability was higher during neurally adjusted ve

172 e treated with low tidal volume ventilation (tidal volume < 6.5 mL/kg predicted body weight) at some

173 3%; 95% CI, 1.01-1.05; P = 0.004), decreased tidal volume (-1.7 ml; 95% CI, -3.3 to -0.2; P = 0.03),

174 001), whereas we detected no association for tidal volume (1.05, 0.98-1.13; p=0.179).

175 Low tidal volume (2.9-4 ml/kg ideal body weight) and poor co

176 mL/kg), and mechanical ventilation with high tidal volume (20 mL/kg).

177 trol group), mechanical ventilation with low tidal volume (6 mL/kg), and mechanical ventilation with

178 variation obtained by transiently increasing tidal volume (tidal volume challenge) are superior to pu

179 , and estimate the respiration rate (RR) and tidal volume (TV) from analysis of electrocardiographic

180 y driving pressure (DP(AW)), the quotient of tidal volume (V(T)), and respiratory system compliance (

181 ion of the RTN to breathing frequency (FR ), tidal volume (VT ) and minute volume (VE ) by inhibiting

182 increased both breathing frequency (fR ) and tidal volume (VT ) whereas, in REM sleep, hypercapnia in

183 hypocapnic; central CO2 response slopes for tidal volume (VT ), breathing frequency (fb ) and rate o

184 The protective role of a small tidal volume (VT) has been established, whereas the adde

185 Baseline corresponded to tidal volume 6 mL/kg of predicted body weight without ex

186 ariation, and cardiac index were recorded at tidal volume 6 mL/kg predicted body weight and 1 minute

187 nd-expiratory occlusion test obtained during tidal volume 6 mL/kg predicted body weight did not predi

188 two-thirds of patients with ARDS received a tidal volume 8 of mL/kg or less of predicted body weight

189 generated tidal volume values (n = 600; mean tidal volume = 6 mL/kg), with a 30% coefficient of varia

190 n minutes]: OR, 1.14, 95% CI, 1.05-1.24; and tidal volume [in milliliters per kilogram of predicted b

191 s included ventilatory management (including tidal volume [VT] expressed as mL/kg predicted bodyweigh

192 th moderate-to-severe hypoxemia, the expired tidal volume above 9.5 mL/kg predicted body weight accur

193 In these patients, the expired tidal volume above 9.5 mL/kg predicted body weight predi

194 m H2O) were noted, with significantly higher tidal volume and compliance at PEEP10 and PEEP5 than PEE

195 ECCO2R enables reductions in tidal volume and driving pressure, key determinants of v

196 urs with matched lung strains (ratio between tidal volume and functional residual capacity) but diffe

197 We assessed expired tidal volume and its association with noninvasive ventil

198 ammation than atelectrauma at comparable low tidal volume and lower driving pressure, suggesting that

199 pressure, respiratory carbon dioxide levels, tidal volume and peroneal nerve muscle sympathetic activ

200 Tidal volume and positive end-expiratory pressure had no

201 sis was to determine the association between tidal volume and the occurrence of pulmonary complicatio

202 2 patients with ARDS with 11,558 twice-daily tidal volume assessments (evaluated in milliliter per ki

203 The median (interquartile range) expired tidal volume averaged over all noninvasive ventilation s

204 /kg predicted body weight and after reducing tidal volume back to 6 mL/kg predicted body weight.

205 ing a simple algorithm targeting the expired tidal volume between 6 and 8 mL/kg of predicted body wei

206 A low or moderate expired tidal volume can be difficult to achieve during noninvas

207 ined by transiently increasing tidal volume (tidal volume challenge) are superior to pulse pressure v

208 to 8 mL/kg predicted body weight, that is, "tidal volume challenge," the changes in pulse pressure v

209 redicted body weight and 1 minute after the "tidal volume challenge." The tidal volume was reduced ba

210 ptor activity (major breathing frequency and tidal volume changes did not alter vagal tone or sympath

211 gnificant dynamic hyperinflation and greater tidal volume constraints (P<0.05).

212 atory lung volume increased (P < 0.001), and tidal volume did not change (P = 0.44); the ratio of tid

213 8 mL/kg predicted body weight, and the mean tidal volume during the first 72 hours after acute respi

214 and stroke volume variation after increasing tidal volume from 6 to 8 mL/kg predicted body weight pre

215 and stroke volume variation after increasing tidal volume from 6 to 8 mL/kg predicted body weight wer

216 hypothesized that with transient increase in tidal volume from 6 to 8 mL/kg predicted body weight, th

217 here was a reduction in emergency department tidal volume from 8.1 mL/kg predicted body weight (7.0-9

218 bution due to the change in lung height with tidal volume inflation are probably bigger contributors

219 A low expired tidal volume is almost impossible to achieve in the majo

220 emic respiratory failure, and a high expired tidal volume is independently associated with noninvasiv

221 In total, 54.4% of patients received a tidal volume less than 8 mL/kg predicted body weight, an

222 The current study elucidated the effects of tidal volume lung inflation [functional residual capacit

223 Tidal volume lung inflation results in structural change

224 hesion molecule-1 protein levels in the high-tidal volume lungs (p < 0.0001).

225 High tidal volume mechanical ventilation and the resultant ex

226 DS with lung-protective ventilation, using a tidal volume of 6 mL per kg of predicted bodyweight and

227 lavage, the LTVV group was ventilated with a tidal volume of 6 mL/kg and progressively higher positiv

228 prototypical patient receiving 8 days with a tidal volume of 6 ml/kg PBW, the absolute increase in IC

229 t (ventilator-induced lung injury) lung with tidal volume of approximately 3 mL/kg and 1) high positi

230 mechanical ventilation strategies using low tidal volume or high levels of positive end-expiratory p

231 text]e/[Formula: see text]co2, dead space to tidal volume ratio (Vd/Vt), and arterial to end-tidal CO

232 0.80 to -0.84; P < 0.001) but not dead space/tidal volume ratio.

233 ed with mechanical ventilation using the low tidal volume strategy as per the Acute Respiratory Distr

234 lume did not change (P = 0.44); the ratio of tidal volume to DeltaPes (an estimate of dynamic lung co

235 d Hering-Breuer mechanoreflex, and increased tidal volume under normal conditions.

236 th basis as a sequence of randomly generated tidal volume values (n = 600; mean tidal volume = 6 mL/k

237 venty patients (19.3%) were treated with low tidal volume ventilation (tidal volume < 6.5 mL/kg predi

238 The entire cohort received low tidal volume ventilation 11.4% of the time patients had

239 Interventions that improve adoption of low tidal volume ventilation are needed.

240 her evidence for early implementation of low tidal volume ventilation as well as new insights into th

241 bal lung stress varies considerably with low tidal volume ventilation for acute respiratory distress

242 zed mice were ventilated with injurious high tidal volume ventilation for periods up to 180 minutes.

243 Previous studies reported poor low tidal volume ventilation implementation.

244 d 34% waited more than 72 hours prior to low tidal volume ventilation initiation.

245 ely recognition of ARDS and adherence to low tidal volume ventilation is important for reducing morta

246 Low tidal volume ventilation lowers mortality in the acute r

247 years after publication of the landmark low tidal volume ventilation study, use remains poor.

248 % were associated with increased odds of low tidal volume ventilation use.

249 ine the rate, quality, and predictors of low tidal volume ventilation use.

250 ur attending physicians (6.2%) initiated low tidal volume ventilation within 1 day of acute respirato

251 as 34 physicians (52.3%) never initiated low tidal volume ventilation within 1 day of acute respirato

252 that compared low with high PEEP during low tidal volume ventilation, an increase in the level of PE

253 Among patients who received low tidal volume ventilation, the mean (SD) percentage of ac

254 Women were less likely to receive low tidal volume ventilation, whereas sepsis and FIO2 greate

255 ably predict fluid responsiveness during low tidal volume ventilation.

256 pressure greater than 30 cm H2O received low tidal volume ventilation.

257 put monitoring, and receiving controlled low tidal volume ventilation.

258 n predicting fluid responsiveness during low tidal volume ventilation.

259 uent tidal volumes compared with the initial tidal volume was associated with a 15% increase in morta

260 Expired tidal volume was averaged and respiratory and hemodynami

261 y weight [7.6-10.2]; p = 0.001), and expired tidal volume was independently associated with noninvasi

262 nute after the "tidal volume challenge." The tidal volume was reduced back to 6 mL/kg predicted body

263 Tidal volume was set at 8 ml/kg, and respiratory rate wa

264 At the end of recruitment, tidal volume was significantly higher (p = 0.002) and ox

265 The mean expired tidal volume was significantly higher in patients who fa

266 nation, heart rate, transcutaneous PCO2, and tidal volume were simultaneously recorded at each airway

267 ransfected mice during inspiration increased tidal volume without altering inspiratory duration, wher

268 ninvasive ventilation sessions (mean expired tidal volume) was 9.8 mL/kg predicted body weight (8.1-1

269 identified by prior work: 1) lung-protective tidal volume, 2) appropriate setting of positive end-exp

270 ventilation settings (i.e. plateau pressure, tidal volume, and positive end-expiratory pressure) on I

271 e, positive end-expiratory pressure, DeltaP, tidal volume, Cdyn, and PaO2/FIO2 were collected at acut

272 xpiratory pressure, DeltaP [PIP minus PEEP], tidal volume, dynamic compliance [Cdyn]) or oxygenation

273 g for PaO2/FIO2 and either driving pressure, tidal volume, or plateau pressure and positive end-expir

274 risk of hospital death based on quantiles of tidal volume, positive end-expiratory pressure, plateau

275 th significant changes (p < 0.01 for all) in tidal volume, positive end-expiratory pressure, respirat

276 ger photoplethysmographic arterial pressure, tidal volume, respiratory carbon dioxide concentrations

277 Secondary outcomes included tidal volume, respiratory rate, minute volume, dynamic l

278 Tidal volume, static compliance, tidal impedance variati

279 We investigated the association of tidal volume, the level of PEEP, and driving pressure du

280 d by a wide variety of changes in the depth (tidal volume, VT ) and number of breaths (respiratory fr

281 by titration of the respiratory rate and/or tidal volume.

282 Mechanical ventilation with low tidal volume.

283 ceiving mechanical ventilation with very low tidal volume.

284 trong for mechanical ventilation using lower tidal volumes (4-8 ml/kg predicted body weight) and lowe

285 Lower tidal volumes (Vts) attenuate extrapulmonary organ injur

286 d-expiratory occlusion test was performed at tidal volumes 6 and 8 mL/kg predicted body weight and af

287 ect harmful forms of OTV including excessive tidal volumes and common forms of patient-ventilator asy

288 Protective mechanical ventilation with lower tidal volumes and PEEP reduces compounded postoperative

289 igh respiratory drive and breathe with large tidal volumes and potentially injurious transpulmonary p

290 reover, a 1 ml/kg PBW increase in subsequent tidal volumes compared with the initial tidal volume was

291 aphragmatic stimulation generated sufficient tidal volumes in all STIM animals.

292 High stress despite low tidal volumes may worsen lung injury and increase risk o

293 proved in the intervention group (use of low tidal volumes, avoidance of heavy sedation, use of centr

294 rial abundances are enhanced at the sediment-tidal water interface and at the tide-induced groundwate

295 encapsulated from higher-level cognition, a tidal wave of recent research alleges that states such a

296 of soils across a total of 24 945.9 km(2) of tidal wetland area, twice as much carbon as the most rec

297 Tidal wetlands contain large reservoirs of carbon in the

298 estuarine emergent wetlands with freshwater tidal wetlands holding about 19%.

299 The average density across all tidal wetlands was 0.071 g cm(-3) across 0-15 cm, 0.055

300 If this result applies more generally to tidal wetlands, it has important implications for models