ライフサイエンスコーパス: tidal

1 that the Cryogenian ocean hosted diminished tidal amplitudes and associated energy dissipation rates

2 we studied the combined effect of seasonal, tidal and diel cycles on the occurrence of bottlenose do

3 minant physiographic forcings in the system (tidal and fluvial influence levels, channel connectivity

4 lood risk associated with sea-level rise and tidal and/or meteorological changes alone.

5 lar expiratory time constants, and 3) reduce tidal atelectasis, preventing hyperinflation.Methods: Th

6 imize lung mechanics and limit tidal-EFL and tidal atelectasis, without increasing hyperinflation.

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

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

9 ed to mimic the shear stress associated with tidal breathing.

10 entilatory response to arousal and nadir end-tidal carbon dioxide were determinants of the apnea-hypo

11 al change in esophageal pressure (DeltaPes), tidal change in dynamic transpulmonary pressure (DeltaPl

12 Clinical features, tidal change in esophageal pressure (DeltaPes), tidal ch

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

14 Doppler ultrasound), BP (Finometer) and end-tidal CO(2) ( PETCO2 , capnography) were performed durin

15 (CBFV; transcranial Doppler ultrasound), end-tidal CO(2) (capnography) and heart rate (ECG) were perf

16 End-tidal CO(2) (EtCO(2)) is used to monitor cardiopulmonary

17 ation, time to glottis passage and first end-tidal CO2 measurement, degree of glottis visualization,

18 onally collected mean arterial pressure, end-tidal CO2, and temperature.

19 , semidiurnal, terdiurnal and quarterdiurnal tidal components.

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

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

22 sm experiment in an impacted and a reference tidal creek to investigate the impacts of wastewater dis

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

24 grazing and burrowing fronts at the heads of tidal creeks (hereafter, creekheads).

25 ness repeatedly over time and in response to tidal cycle (high vs. low, an index of risk) and daily t

26 inflation characteristics of the individual tidal cycle (plateau pressure, positive end-expiratory p

27 wimming speed and direction to vary over the tidal cycle and (ii) that, in some instances, larval swi

28 ions could vary by a factor of 1000 within a tidal cycle at our sample locations.

29 g ice sheet grounding line during successive tidal cycles.

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

31 antly on the equation of state (EoS)-related tidal deformability parameter Lambda, but at late times

32 Tidal disruption and subsequent accretion of planetesima

33 nd x-ray quasi-periodic oscillation from the tidal disruption event ASASSN-14li.

34 osity gamma-ray burst at high redshift, or a tidal disruption event involving an intermediate-mass bl

35 since 2010, possibly indicating a long-lived tidal disruption event(5).

36 Our findings demonstrate that tidal disruption events can generate quasi-periodic osci

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

38 dormant galaxies and often attributed to the tidal disruption of a star by the central black hole(1,2

39 ciated with a variety of phenomena including tidal effects during the inspiral.

40 esistances optimize lung mechanics and limit tidal-EFL and tidal atelectasis, without increasing hype

41 Rationale: Tidal expiratory flow limitation (tidal-EFL) is not completely avoidable by applying posit

42 ratory diaphragmatic contraction counteracts tidal-EFL.

43 tion, external expiratory resistances reduce tidal-EFL.Objectives: To assess whether external expirat

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

45 Ordovician reveals amphibious locomotion in tidal environments and fills a gap between molecular est

46 ces for movement and self-defense in aqueous tidal environments.

47 promising intervention is through restoring tidal exchange to impounded coastal wetlands for reduced

48 Rationale: Tidal expiratory flow limitation (tidal-EFL) is not comp

49 ure was associated with reduced time to peak tidal expiratory flow to expiratory time (beta = -0.004;

50 s were particularly vulnerable (time to peak tidal expiratory flow to expiratory time: beta = -0.003,

51 ncluding the ratio of the time to reach peak tidal expiratory flow to the total expiratory time (tpte

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

53 t II), single S. salsa (S, habitat III), and tidal flat (TF, habitat IV) across a salinity gradient.

54 signal a continuing negative trajectory for tidal flat ecosystems around the world.

55 About 70% of the global extent of tidal flats is found in three continents (Asia (44% of t

56 that maps the global extent of and change in tidal flats over the course of 33 years (1984-2016).

57 % (15.62-16.47%, 95% confidence interval) of tidal flats were lost between 1984 and 2016.

58 We find that tidal flats, defined as sand, rock or mud flats that und

59 l-resolution dataset delivers global maps of tidal flats, which substantially advances our understand

60 eas globally, the distribution and status of tidal flats-one of the most extensive coastal ecosystems

61 eplaced forest understory vegetation along a tidal flooding gradient.

62 density of vulnerable assets and present-day tidal flooding issues.

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

64 d through restoration of disconnected saline tidal flows.

65 n seagrass meadows, whilst accommodating for tidal fluctuations.

66 bandoned ponds over time in areas exposed to tidal flushing.

67 n oiled sediments contaminated via simulated tidal flux.

68 th pole, even though the expected pattern of tidal forced deformation should be symmetric between the

69 The tidal forces close to massive black holes can rip apart

70 Although it has long been suspected that tidal forces(10,11) and ram-pressure stripping(12,13) co

71 as restored to normothermic values using end-tidal forcing.

72 for high marsh, and 1,064 +/- 38 Mg C/ha for tidal forest (high elevation/low salinity).

73 eagrass and marsh communities and 78% in the tidal forest.

74 eagrasses and marshes and 34% of the TECS in tidal forests.

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

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

77 Internal waves at tidal frequencies can regularly flush reefs with cooler

78 ons to propagate along the pycnocline with a tidal frequency (i.e. internal tides).

79 fibular microneurography) when clamping end-tidal gases at baseline levels.

80 nces among these groups were found along the tidal gradient and seasonally when observed at a finer t

81 of three different mats developing along the tidal gradient of the North Sea beach of the Dutch barri

82 he subsurface wave is likely driven by lunar tidal gravitational force.

83 y cyclical processes such as seasonality and tidal hydrology.

84 time to re-extend tentacles after simulated tidal immersion.

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

86 uctures of all dimensions, the components of tidal inflation that relate to power (which include freq

87 ing mooring, in a seagrass meadow under high tidal influence.

88 nomical units, except at periapse, where the tidal interaction with the black hole stretches them alo

89 Proteus has migrated outwards because of tidal interactions with Neptune.

90 the thermochemical history of Mars, through tidal interactions-we can gain insight into the thermal

91 hat long-term sea-level rise effects such as tidal inundation and increased porewater salinity will l

92 Tidal inundation at the upper border of this migration z

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

94 sand, rock or mud flats that undergo regular tidal inundation(7), occupy at least 127,921 km(2) (124,

95 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

96 0-2100 and ranges from 5.0-15.4 m above mean tidal level by 2280-2300.

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

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

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

100 Coastal wetlands (mangrove, tidal marsh and seagrass) sustain the highest rates of c

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

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

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

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

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

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

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

108 Here we show that tidal marshes on coastlines that experienced rapid RSLR

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

110 preserve vegetated coastal ecosystems (VCE; tidal marshes, mangroves and seagrasses) to mitigate gre

111 n experiments in European and North American tidal marshes.

112 her ecosystem services provided by Australia tidal marshes.

113 imed at facilitating ecosystem migration for tidal marshes.

114 is contrasts with the northeast where strong tidal mixing prevents thermal stratification and recent

115 examine how the interplay of ocean warming, tidal mixing, and larval behavior results in a brighter

116 show, using an established numerical global tidal model and paleogeographic reconstructions, that th

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

118 counted for dynamic physical drivers such as tidal non-linearity, storms, short-term climate variabil

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

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

121 no differences in arterial CO2 tension or in tidal or minute ventilation between the groups.

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

123 = 0.665), consistent with the unchanged end-tidal PCO2 (P = 0.327); whereas, Q(VA) was higher throug

124 ry blood flow, independent of changes in end-tidal PCO2 and blood pressure External carotid artery bl

125 End-tidal PCO2 and PO2 were effectively clamped to resting v

126 ssive heat stress during isocapnia (i.e. end-tidal PCO2 was held constant) Submaximal cycling exercis

127 ionospheric sporadic E layer with a downward tidal phase is observed followed by a subsequent intensi

128 We argue that the near-absence of Cryogenian tidal processes may have been one contributor to the pro

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

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

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

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

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

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

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

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

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

138 during inspiration in the setting of minimal tidal recruitment/derecruitment and that this mismatchin

139 Tidal recruitment/derecruitment with fractional atelecta

140 In experimental atelectasis with minimal tidal recruitment/derecruitment, mechanical inspiratory

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

142 surface forces, lung stress relaxation, and tidal reexpansion/collapse.

143 riods of intensified SOM decay; (c) changing tidal regimes in mangroves due to sea level rise might a

144 Determine the intra-tidal regional gas and blood volume distributions at dif

145 infall trends when assessing the efficacy of tidal reinstatement for GHG emission control.

146 lux (CO(2) and CH(4)) prior to and following tidal reinstatement.

147 s the non-linear interaction of tide and non-tidal residual in order to quantify its contribution to

148 e the surrounding ocean is too large to host tidal resonances.

149 nstrated during a three-week deployment in a tidal river.

150 nd dissolved oxygen (DO) conditions on diel, tidal, seasonal and interannual timescales.

151 The high tidal sensitivity at Axial Volcano results from the shal

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

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

154 The main tidal signature depends predominantly on the equation of

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

156 om the salt marsh, and its relationship with tidal state and bulk suspended sediment concentrations (

157 onforms to triggering theory over the entire tidal stress range.

158 gma chamber inflates/deflates in response to tidal stresses, producing Coulomb stresses on the faults

159 utpaced marsh vertical accretion, increasing tidal submergence of marsh surfaces, particularly where

160 idal waters to traverse intertidal and upper tidal surfaces.

161 he orbital period, indicating star spots and tidal synchronization.

162 The morphological development of fluvial and tidal systems is forecast more and more frequently by mo

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

164 Dust tides-tidal transport of dust in this way-rapidly transport he

165 lk modulus is sufficiently low, the phase of tidal triggering is inverted.

166 The strong tidal triggering of mid-ocean ridge earthquakes has rema

167 nd farms and marine energy converters (e.g., tidal turbines).

168 uring at 0.1 Hz) elucidated the influence of tidal variation, rain events, diurnal effects, and anthr

169 ion and flow of human red blood cells during tidal ventilation and distension of a proximate airway.

170 Gradual aeration with tidal ventilation and PEEP produced the least lung injur

171 ion (SI) until full aeration (n = 26); or 3) tidal ventilation with an initial escalating/de-escalati

172 th current ventilation practice that employs tidal ventilation with limited driving pressure.

173 ion) were randomized at birth to receive: 1) tidal ventilation without an intentional recruitment (no

174 ional injury patterns that affect subsequent tidal ventilation.

175 Median end-tidal volatile anesthetic concentration was significantl

176 idal volumes less than 6.5 mL/kg (51% use of tidal volume <= 6.5 mL/kg if acute respiratory distress

177 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),

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

179 d ventilation (control group) with identical tidal volume (7 mL/kg) and positive end-expiratory press

180 postoperative increases in all components of tidal volume (left and right chest wall and diaphragm, a

181 se for left lung tidal volume and right lung tidal volume (P < .001 for both), respectively.

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

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

184 utamate (10 mm/100 nL) in the PPTg decreased tidal volume (V(T) ) but otherwise increased respiratory

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

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

189 health record data, we examined patterns of tidal volume administration, the effect on clinical outc

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

191 mechanical power was achieved by increasing tidal volume and decreasing respiratory rate.

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

193 ecruitment maneuvers (a stepwise increase of tidal volume and eventually PEEP) or to the low level of

194 um driving pressure was achieved by reducing tidal volume and increasing respiratory rate and positiv

195 breath, bins them according to frequency or tidal volume and plots the results against bin means.

196 was a 43.8% and 55.3% increase for left lung tidal volume and right lung tidal volume (P < .001 for b

197 al of Philadelphia (n = 77) and from the low tidal volume arm of the Acute Respiratory Distress Syndr

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

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

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

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

202 surgery, intraoperative ventilation with low tidal volume compared with conventional tidal volume, wi

203 es, and alternate metrics for evaluating low tidal volume compliance in clinical practice.

204 d provide a unique window for evaluating low tidal volume delivery and targets for improvement.

205 idal volume with alternative measures of low tidal volume delivery ranged from 0.38 to 0.66.

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

207 The theoretical basis for minimizing tidal volume during high-frequency oscillatory ventilati

208 rable changes in response to the increase in tidal volume during mechanical ventilation.

209 atio, 1.82; 95% CI, 1.20-2.78), whereas mean tidal volume exposure was not (odds ratio, 0.87/1 mL/kg

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

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

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

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

214 32 of 590 patients (39%) in the conventional tidal volume group (difference, -1.3% [95% CI, -6.8% to

215 rred in 231 of 608 patients (38%) in the low tidal volume group compared with 232 of 590 patients (39

216 6 mL/kg predicted body weight (n = 614; low tidal volume group) or a tidal volume of 10 mL/kg predic

217 predicted body weight (n = 592; conventional tidal volume group).

218 distress syndrome was associated with lower tidal volume in multivariate analysis.

219 Despite low mean tidal volume in the cohort, a significant percentage of

220 anical ventilation during surgery, the ideal tidal volume is unclear.

221 eight (n = 614; low tidal volume group) or a tidal volume of 10 mL/kg predicted body weight (n = 592;

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

223 Patients were randomized to receive a tidal volume of 6 mL/kg predicted body weight (n = 614;

224 eceived volume-controlled ventilation with a tidal volume of 7 mL/kg of predicted body weight.

225 rpin RNA (shRNA) progressively decreased the tidal volume of breaths yet surprisingly increased breat

226 e, but it was stable on the average: average tidal volume ranged between 524.8 and 607.0 mL (p = 0.33

227 0.80 to -0.84; P < 0.001) but not dead space/tidal volume ratio.

228 Initial tidal volume settings strongly predicted exposure to vol

229 ol ventilation with only 50% achieving a low tidal volume strategy (plateau pressure <= 30 cm H2O) wi

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

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

232 Acute Respiratory Distress Syndrome Network tidal volume trial (n = 100).

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

234 ble Ventilation (VV), in which frequency and tidal volume vary from breath-to-breath.

235 , we found that the protective effect of low tidal volume ventilation against lung injury caused by l

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

237 sociated with a high mortality rate, and low tidal volume ventilation improves mortality.

238 ratory distress syndrome recognition and low tidal volume ventilation use have increased over time, t

239 The main management strategy, low tidal volume ventilation, can be associated with the dev

240 nificant improvement include use of targeted tidal volume ventilation, use of caffeine therapy, oxyge

241 lness and is also associated with use of low tidal volume ventilation.

242 We assumed patients received low tidal volume ventilation.

243 differential diagnosis, or treated with low tidal volume ventilation.

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

245 n predicting fluid responsiveness during low tidal volume ventilation.

246 Although mean tidal volume was 6.8 mL/kg predicted body weight, 40% of

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

248 lipopolysaccharides and ventilation at high tidal volume was suppressed in Rap1 knockout mice.

249 Across ICUs, correlation of mean tidal volume with alternative measures of low tidal volu

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

251 ally ventilated in pressure-controlled mode (tidal volume, 6 mL/kg; respiratory rate, 40; FIO2, 0.6;

252 e positive end-expiratory pressure, baseline tidal volume, and hospital site.

253 taset had limited scope for further reducing tidal volume, but driving pressure was still significant

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

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

256 n commonly used respiratory variables (i.e., tidal volume, minute ventilation, and respiratory rate).

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

258 entilator-induced lung injury, including low tidal volume, prone position, and neuromuscular blockers

259 ot only accurately measure respiratory rate, tidal volume, respiratory minute volume, and peak flow r

260 istance and elastance as a function of time, tidal volume, respiratory rate, and positive end-expirat

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

262 Tidal volume, static compliance, tidal impedance variati

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

264 low tidal volume compared with conventional tidal volume, with PEEP applied equally between groups,

265 chanically ventilated swine by adjusting the tidal volume.

266 ventilatory rate rather than an increase in tidal volume.

267 anical power led to significant increases in tidal volume.

268 eased despite unchanged respiratory rate and tidal volume.

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

270 umbar Cobb angle were poor predictors of MRI tidal volumes (chest wall, diaphragm, and left and right

271 l capacity showed moderate correlations with tidal volumes (chest wall, diaphragm, and left and right

272 Lower tidal volumes (Vts) attenuate extrapulmonary organ injur

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

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

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

276 patient level, exposure to 24 total hours of tidal volumes greater than 8 mL/kg predicted body weight

277 body weight, 40% of patients were exposed to tidal volumes greater than 8 mL/kg predicted body weight

278 The average lung tidal volumes increased after operation for TIS; there w

279 Mechanical ventilation with low tidal volumes is recommended for all patients with acute

280 differential diagnosis were associated with tidal volumes less than 6.5 mL/kg (51% use of tidal volu

281 Use of tidal volumes less than 6.5 mL/kg also increased (p < 0.

282 Tidal volumes were analyzed across 1,905 hospitalization

283 were exposed to a prolonged duration of high tidal volumes which was correlated with higher mortality

284 wall and diaphragm, and left and right lung tidal volumes) measured at MRI.

285 quency or resonant frequency despite reduced tidal volumes, especially in adults, due to regional amp

286 airway pressure release ventilation with low tidal volumes, positive end-expiratory pressure was set

287 ot demonstrate improvements in postoperative tidal volumes.

288 All participants received low tidal volumes.

289 rlying water and is the first part of rising tidal waters to traverse intertidal and upper tidal surf

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

291 The tidal wetland CAR is projected to increase in this centu

292 le data exist for the carbon stocks of major tidal wetland types in the Pacific Northwest, United Sta

293 osition on CH(4) emissions from an estuarine tidal wetland.

294 p explain elevated zooplankton abundances in tidal wetlands and other detrital-dominated regions.

295 Tidal wetlands contain large reservoirs of carbon in the

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

297 We synthesized C accumulation rate (CAR) in tidal wetlands of the conterminous United States (US), u

298 s a baseline assessment of C accumulation in tidal wetlands of US, and indicate a significant C sink

299 - 6 g Cm(-2 )yr(-1), and the conterminous US tidal wetlands sequestrate 4.2-5.0 Tg C yr(-1).

300 nservation and restoration of temperate zone tidal wetlands through climate change mitigation strateg

301 in seagrass, emergent marshes, and forested tidal wetlands, occurring along increasing elevation and