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1 n of the uterus and spiral arteries is often shallow.
2 dominate, even when gradients are relatively shallow.
3 could arise because of ocean warming and DSL shallowing.
4 ng the four subgroups, LS displayed the most shallow ACD (p = 0.01).
5 face litter material and accumulated in both shallow and deep soil, perhaps through mixing by earthwo
6  concentrations occurred in shallower wells, shallow and deep wells were virus-positive at similar ra
7 ecule ligand discovery due to the relatively shallow and featureless binding surfaces.
8 northwards, opening an equatorial gateway to shallow and intermediate circulation.
9 nuous increase during the Ordovician in both shallow- and deep-marine environments.
10                                           At shallow anoxic depths, PA taxa were primarily affiliated
11    Risk factors for increased EC loss were a shallow anterior chamber depth (ACD) (P </= 0.005) and a
12 perative complications, an increased risk of shallow anterior chamber was observed in the limbal-base
13 ce was detected in the risk of postoperative shallow anterior chamber, which was increased in the lim
14 xpression during development and resulted in shallow anterior chambers.
15 ed, in situ bacterial communities inhabiting shallow aquifers (<30 m) at two sites in Araihazar, Bang
16 e sources of Mo in drinking-water wells from shallow aquifers in a region of widespread CCR disposal
17  in the case of any unplanned migration into shallow aquifers or to the surface.
18 Mitigation of the widespread As-pollution in shallow aquifers through exploitation of deep Pleistocen
19 h potential leakage of reservoir fluids into shallow aquifers, in particular the possible environment
20 ral and Northeast Pacific, combined with the shallow aragonite saturation horizon (ASH) and high carb
21 he tidal range changes most significantly in shallow areas, whereas both, notch geometry and models r
22 haviors performed by fruit flies moving in a shallow arena.
23 en reported to detect pheromone gradients as shallow as 0.1 nM/mum.
24 .1 mm/s were realized in separation ducts as shallow as 300 nm using our current design for a maximum
25                       This angle could be as shallow as the approach angle of a patch-clamp pipette b
26 n depth; in waterlogged lowlands, roots stay shallow, avoiding oxygen stress below the water table; i
27 cts that have been addressed have focused on shallow back reef habitats.
28 polymerase I (Pol I) and Pol II recover from shallow backtracks by 1D diffusion, use RNA cleavage to
29       The southern habitat, characterised by shallow banks and channels, may be marginal relative to
30                                              Shallow basal root growth angle (BRGA) increases phospho
31        Given the combination of wetlands and shallow bays as landscape components that determine the
32                                           In shallow beds, however, reduced visibility exacerbates th
33 oncentrated CO2, provides direct evidence of shallow benthic CO2 accumulations originating from sub-s
34 heir x-z dimension, but preferentially adopt shallow beta angles between spindle pole axis and substr
35 tors typically engage these sites using very shallow binding modes.
36 nd non-cognate Galpha peptides show deep and shallow binding, respectively, and in distinct orientati
37 n of the south arm and the existence of oxic shallow brine and anoxic deep brine layers.
38 te equilibrium oxygen isotope values implies shallow calcification depths for H. inflatus (75 m).
39 e cell rear perturbs efficient chemotaxis in shallow cAMP gradients, without affecting the abundance
40 we demonstrate the presence of both deep and shallow carrier traps.
41 ess rhythmic at depth (50-140 m) relative to shallow-caught animals (0-50 m).
42 eme while its aliphatic chain snakes along a shallow cavity making hydrophobic interactions in the "s
43 erium Escherichia coli is well understood in shallow chemical gradients, but its swimming behavior re
44  framework of how cells sense and respond to shallow chemical gradients.
45 strain the aerosol-cloud radiative effect in shallow clouds through a combination of routine process
46 onditions influencing the biogeochemistry in shallow CO2-rich hydrothermal systems and the importance
47 ane was microbially generated, likely within shallow coal seams.
48 ing and multivariate statistics to show that shallow coastal areas are extremely sensitive to changin
49 of methane from thawing subsea permafrost on shallow continental shelves and dissociation of methane
50 c system with strong electronic stopping and shallow core level states.
51 the current ice core record beyond 800 ka by shallow coring in Antarctic blue ice areas.
52 The complex is organized as a double-layered shallow corkscrew, with the AAA+ and AAA+-like domains f
53  immobilized and the 2.3% of shelf which are shallows could be as productive as all the remaining con
54 ight the importance of the representation of shallow cumulus convection.
55 cal oceans, and the prevailing cloud type is shallow cumulus.
56               When ELM is intact, there is a shallow decline in acuity with increasing subretinal flu
57 itive to surface heat fluxes in regions with shallow (deep) mixed layer.
58                                          The shallow defects, which are situated at about 20 meV belo
59 rties demonstrates a continuously accreting, shallow-deforming, bed and invariant basal conditions.
60 ested that the B26 side chains pack within a shallow depression at the solvent-exposed periphery of t
61 e calculate the amount of magma contained at shallow depth beneath Santorini volcano, Greece.
62 amplification methods, and sequenced them at shallow depth.
63 ppropriate method to detect contamination at shallow depths at sites with VI.
64 ystal-poor, silicic magma that are stored at shallow depths in the crust, and to obtain theoretical b
65          Traditionally heavy oil in sands at shallow depths is accessed by large scale mining activit
66 ore abundant and larger in mesophotic versus shallow depths, which remains particularly suggestive of
67 tion of centuries-old colonies, even at very shallow depths.
68 ntrast, and (iii) measurements taken at very shallow depths.
69 ng all subsurface behaviour as deep dives or shallow dives discounts a significant amount of importan
70  complex than a simple dichotomy of deep and shallow diving states, and labelling all subsurface beha
71 ation, and that the defect energy level is a shallow donor to the conduction band rendering the mater
72 to Ga2O3 Schottky diodes containing only the shallow donor.
73 wly developed highly biocompatible magnesium shallow doped gamma-Fe2 O3 (Mg0.13 -gammaFe2 O3 ) SPNPs
74 nuous sea-air gas flux data collected over a shallow ebullitive methane seep field on the Svalbard ma
75 ctories that frequently involve movements up shallow energy gradients prior to the "downhill" folding
76 sensing enables detection of and response to shallow epidermal growth factor (EGF) gradients that are
77  find that the final stage of wave growth in shallow estuaries can be presented by a product of water
78      We demonstrate that wave growth rate in shallow estuaries is a function of wind fetch to water d
79  deterioration of wetland ecosystems in many shallow estuaries raises concerns about the contributing
80 pelling palaeobiological evidence for a very shallow, euphotic setting.
81 sphorus (P) behavior underneath the ice of a shallow eutrophic freshwater bay.
82 spp., the dominant habitat-forming corals in shallow exposed reefs across the Pacific.
83                   Our results imply that the shallow extent of the seismogenic zone of a subducting i
84 isms that can amplify its sensitivity in the shallow external gradients typical of chemotaxis experim
85 f SAWs into other modes, even for relatively shallow features.
86  they are therefore relatively immune to the shallow flapping amplitude.
87 ogen, oxygen, iron, sulfur, and uranium in a shallow floodplain.
88  Most critically we report major declines in shallow fore-reef carbonate budgets, these shifting from
89                                   Thus these shallow fore-reef habitats are now in a phase of net ero
90                 POP formation was highest in shallow-fried potatoes with PS liquid margarine (64.44mg
91 (NMOG) emissions from boiling, charbroiling, shallow frying, and deep frying of various vegetables an
92                               Emissions from shallow frying, deep frying and charbroiling are dominat
93 amounts of biogenic methane originating from shallow gas accumulations in the overburden of deep rese
94                                              Shallow gas migration along hydrocarbon wells constitute
95  hydrocarbon-prolific provinces of the world shallow gas pockets are frequently observed in the sedim
96 e, we identify numerous wells poking through shallow gas pockets in 3-D seismic data of the CNS indic
97                                         In a shallow gradient of chemoattractant, local Ras activatio
98                               In response to shallow gradients of chemotactic stimuli recognized by G
99 ome cells are capable of detecting extremely shallow gradients, even in the presence of significant m
100 ical linear-response theory of chemotaxis in shallow gradients, limits in drift due to steep gradient
101 F showed the most dramatic improvements with shallow gradients, which is particularly useful for biol
102 w yeast cells filter fluctuations and detect shallow gradients.
103 g armed insurrection of 1916 and buried in a shallow grave on Cork prison's grounds.
104 dues make additional interactions in a wide, shallow groove adjacent to the primary binding site.
105                      However, there are only shallow grounds for finding Darwinian concepts or popula
106 he Agricultural Water Productivity Model for Shallow Groundwater (AWPM-SG) for calculating capillary
107 organic arsenic to receiving waters and very shallow groundwater after precipitation.
108                          Capillary rise from shallow groundwater can decrease the need for irrigation
109 seeps and surface water from seven sites and shallow groundwater from 15 sites in five states (Tennes
110 e microbially mediated release of arsenic to shallow groundwater in Bangladesh remain poorly understo
111 to outlying areas where arsenic-contaminated shallow groundwater is pervasive and has potential to mi
112 PM-SG) for calculating capillary fluxes from shallow groundwater using readily available data.
113 coal ash ponds to adjacent surface water and shallow groundwater.
114 from surface water via the hyporheic zone to shallow groundwater.
115  beneficial to save more water in areas with shallow groundwater.
116 deeper living corals will likely increase as shallow habitats further degrade due to climate change a
117 thermally polluted and undisturbed (control) shallow hard bottom habitats.
118       Employing EG, we observe its role as a shallow hole trap, or as an intermediate hole transport
119 thermore, there is increasing awareness that shallow hydrate-related methane seeps have appeared due
120 tail anchor of MT-WQ-IDL also binds with the shallow hydrophobic pocket outside the groove of the NHR
121 onductance (n gate) showed a longer peak and shallow hyperpolarization; for power-law activation of t
122 requency range was 1.2-8.0 kHz to simulate a shallow insertion depth and the input frequency range wa
123 raction because nanoscale roughness produced shallow interactions that were susceptible to removal.
124 ia was induced in healthy male volunteers by shallow intracutaneous injection of low millimolar conce
125 band emission and radiative recombination at shallow intrinsic defect sites.
126 with pachychoroid features, the finding of a shallow irregular pigment epithelial detachment on OCT h
127      We report the creation of an ultimately-shallow junction at the surface of n-type silicon with e
128  The impact of climate warming on the GWP of shallow lakes is a more complex interplay of phytoplankt
129 t]wt % that is typical for concentrations in shallow lakes on early Earth.
130 cture analogous to the regime shifts seen in shallow lakes.
131                          The hazard posed by shallow landslides depends on the availability and stren
132                                              Shallow landslides, triggered by extreme rainfall, are a
133 a linguistic architecture involving a single shallow level of syntax connected to a semantic level co
134 logical processes, affecting the atmosphere, shallow lithosphere, hydrosphere, and biosphere.
135 of bridgmanite and magnesiowustite under the shallow lower mantle conditions.
136 s and deflection of rising plumes in Earth's shallow lower mantle have been suggested to result from
137 cating chemical homogeneity of the upper and shallow lower mantle.
138   A high Fe(3+)/Fe(2+) ratio of about two in shallow-lower-mantle bridgmanite is required to match se
139                          They are biased for shallow, lowest common denominator information, at the e
140      These palaeo-subglacial lakes comprised shallow (&lt;10 m) lenses of water perched behind ridges or
141 bicolor damselfish (Stegastes partitus) from shallow (&lt;10 m), deep shelf (20-30 m), and mesophotic re
142        How much magma needs to be added to a shallow magma chamber to cause rupture, dyke injection,
143 , and accumulate in voluminous but ephemeral shallow magma chambers.
144                                              Shallow magma intrusion builds subsurface reservoirs tha
145 onnect subduction-induced ascending melts to shallow magma reservoirs.
146 the Monte Nuovo eruption and investigate the shallow magma transfer.
147 nsition in crystal-bearing magmas at certain shallow magmatic conditions.
148 e transport high-(3)He/(4)He material to the shallow mantle beneath plume-fed hotspots.
149                                              Shallow marine calcifiers play an important role as mari
150 omatolites demonstrates the establishment of shallow marine carbonate production with biotic CO2 sequ
151 nnovations in herbivore function have shaped shallow marine ecosystems from kelp forests to coral ree
152 ack species, Caranx ignobilis, which inhabit shallow marine ecosystems.
153              The ISB stromatolites grew in a shallow marine environment, as indicated by seawater-lik
154 rolling biodiversity through availability of shallow marine environments and via allopatric speciatio
155 latively low authigenic phosphorus burial in shallow marine environments until about 800 to 700 milli
156 and foraminiferal assemblages showing marked shallow-marine preferences.
157              Detection was best explained by shallow marsh plant species identity (34.8%) and surroun
158 r, a down-shifted pattern of ICN maturation (shallow maturation), rather than a right-shifted pattern
159 test path to a goal in novel mazes with one (shallow maze) or two (deep maze) choice points.
160                                          The shallow MeHg maxima just below the productive surface la
161 r ferrofluids of different concentrations in shallow microchannels.
162 summer relate positively to a combination of shallow mixed layer depth and increased wind in spring,
163 versus stimulus level function would predict shallow MPI since the amount of current reduction necess
164  the enteroviruses and cardioviruses, with a shallow, narrow depression bounded by the prominent VP0
165 tates generated by quantum dynamics, while a shallow network representation with a restricted Boltzma
166 rizes the representational power of deep and shallow neural networks, which is of fundamental interes
167                     Coherent manipulation of shallow nitrogen-vacancy (NV) color centers enables the
168 chnique to extend the spin coherence time of shallow nitrogen-vacancy centers, we demonstrate magneti
169 n described by two states; deep foraging and shallow, non-foraging dives.
170 nd groups such as the Bahamas, surrounded by shallow oceans, Quaternary glacial-interglacial changes
171 considered a single PC embedded epidermally (shallow) or dermally (deep) to model the PC's location w
172 ified the susceptibility of DOM draining the shallow organic mat and the deeper permafrost layer of a
173                                          The shallow overturning circulation of the oceans transports
174                                     Overall, shallow P. astreoides exhibited high gene flow between F
175 ether the earthquake rupture extended to the shallow part of the plate boundary near the trench remai
176 lip near the surface is poorly understood as shallow parts of thrust faults are considered to be fric
177 persal of water vapour is constrained by the shallow PBL, leading to an increase in relative humidity
178 essing of aerosol and water vapour in a very shallow PBL.
179 chanism only weakly amplifies signaling in a shallow PDGF gradient, but it synergizes with other feed
180 ded deep deposits but mainly to extended but shallow peat in the Amazon Basin.
181 hen compared between taxa, even at this very shallow phylogenetic level.
182  pollutants and water vapour accumulate in a shallow planetary boundary layer (PBL).
183 PFC increases during sequential (deep versus shallow) planning and is higher before correct versus in
184 s to ca. 6 km depth, which we interpret as a shallow plumbing system comprising a fractured hydrother
185                       First, we identified a shallow pocket adjacent to the groove in the N-terminal
186                              We identified a shallow pocket adjacent to the groove in the NHR trimer
187                    However, contamination of shallow potable aquifers by HVHF at depth has never been
188 t MeC3Me ((3)3), but they also reveal a very shallow potential energy surface.
189 , and N2O in CO2 equivalents) emitted from a shallow productive lake during an average versus a heat-
190 ayed a major role in driving tropical marine shallow reef biodiversity dynamics.
191 itigate high temperature bleaching for 9% of shallow reef habitat (to 30 m depth) - habitat that was
192  horizontal dispersal of propagules from one shallow reef to another.
193  lower bleaching threshold temperatures than shallow reefs.
194 ssible hot zone, linking ascending melts and shallow reservoirs.
195 ihydrofuran that leads to the formation of a shallow resorcinarene framework; condensation with aroma
196 r breath in a suite of aquatic habitats from shallow rivers to deep oceans.
197 n excess supply of 20 mM Pi (P20) produces a shallow root system architecture (RSA), reduces primary
198  when surface waters cooled, fish moved into shallow seagrass and macroalgae beds that were previousl
199 s has led to the additional assumptions that shallow search slopes (at most a few tens of millisecond
200 sults show that while benthic communities in shallow seas generally show higher biomass in a warmed w
201 supply due to sea level-driven variations in shallow sediment denitrification associated with the cyc
202  MCG Archaea in clone libraries decreased at shallow sediment depths (27% of the total MCG).
203 n of DEH showed populations may establish in shallow sediments (i.e. upper centimetres), although as
204 s associated with potential CO2 leakage into shallow sediments at carbon sequestration sites.
205 rthermore, larger changes (>50%) occurred in shallow sediments, a few meters away from the injection,
206 H2-rich vapor phase to form, suggesting that shallow serpentinization environments where a separate g
207  only temporally but also spatially from the shallow shelf to deep-water environments in tandem with
208                           Using conventional shallow shell theory in combination with equilibrium sta
209                                       On the shallow shelves (<100 m water depth), methane released f
210  of coral dominance at chronically disturbed shallow sites is likely due to an abundance of coral tax
211 they generally do not deal specifically with shallow slip features.
212 quake produced an unexpected large amount of shallow slip greatly contributing to the ensuing tsunami
213                                              Shallow slip offshore Sumatra appears driven by diagenet
214  soil dwelling animals and microorganisms in shallow soil are affected as well.
215 drought events, particularly in regions with shallow soil depths.
216 f CO2 leakage from storage reservoirs on the shallow soil property and vegetation.
217      Under semiarid conditions, hydrology of shallow soils is expected to decouple from plant hydrolo
218       However, the active site of PPIases is shallow, solvent-exposed, and well conserved between fam
219 Precipitation reduction alters the uptake of shallow sources following extended droughts for pinon.
220 ns four Apaf-1/pc-9 CARD pairs arranged in a shallow spiral with the fourth pc-9 CARD at lower occupa
221 DOM samples along a salinity gradient from a shallow STE on Spiekeroog Island, North Sea, Germany, an
222  y, which affects biota by strengthening and shallowing stratification of the water column.
223 ins are commonly present in the mantle above shallow subducting slabs and play key roles in controlli
224 ce, are part of the largest arsenic-CO2-rich shallow submarine hydrothermal ecosystem on Earth.
225                  We present newly discovered shallow subsea pools located within the Santorini volcan
226 ace-elevation change, vertical accretion and shallow subsidence rates.
227 sium Planitia show distinct chemistry in the shallow subsurface (down to several decimeters) relative
228   Hydrochemical solute concentrations in the shallow subsurface can be spatially highly variable with
229  reduction at Von Damm occurs rapidly during shallow subsurface mixing of the same fluids, which may
230          Here we present a 135-kyr record of shallow subsurface pCO2 and nutrient levels from the Nor
231 gas accumulations known to be present in the shallow subsurface were reached.
232 ntial volatile occurrence in the surface and shallow subsurface.
233 ated control plots in the low intertidal and shallow subtidal zone.
234 lfide droplets, followed by degassing of the shallow, sulfide-saturated, and exceptionally volatile a
235 Utah, we asked where and when groundwater vs shallow surface water inputs controlled stream discharge
236 rier of Ea =4.8 kcal mol(-1) and with only a shallow temperature dependence, the results are interpre
237 firmed that the axonal guidance is caused by shallow temperature-gradient, eliminating the role of an
238 l of 3700 kg of coal tar over 12 days in the shallow test and 860 kg over 11 days in the deep test wa
239 uenced the front propagation geometry in the shallow test.
240 cific and the eastern Pacific cooling with a shallow thermocline are all captured by this simple coup
241  sponge found on Caribbean coral reefs along shallow to mesophotic depth gradients where multiple abi
242  contrasting with weakening proposed for the shallow Tohoku-Oki 2011 rupture, but our results are app
243 istinct Eu-Mg defect configurations with the shallow transient and deep ground states of the Mg accep
244  observed in the first hour, probably due to shallow traps, followed by subsequent fading of 6-7% ove
245 y forming a Cd-S bond, while maintaining the shallow traps.
246 strongly modified the global distribution of shallow tropical seas reshaping the geographic configura
247 ), deep tubewells (DTWs) (n = 107; 17%), and shallow tubewells (STWs) (n = 96; 19%) during the 2012 a
248 oral population from a previously unexplored shallow underwater cave in Corsica (France) harbouring t
249 l to differentiate properly, contributing to shallow uterine invasion and deficient spiral artery rem
250 tial leaky integrate-and-fire models using a shallow voltage-dependence for the exponential term that
251 s for understanding sedimentary processes in shallow warm-water carbonate provinces.
252     Arctic gas hydrate reservoirs located in shallow water and proximal to the sediment-water interfa
253 des prevalent at all depths, but sharing the shallow water benthos with the copepods.
254                    Males that call from very shallow water bodies (few mm depth) benefit from reduced
255                                We argue that shallow water CO2 bubble stripping should be considered
256 , favoured deposition of thick evaporites in shallow water of the Brazilian-Angolan margins.
257 reefs are as vulnerable to climate change as shallow water reefs.
258 ing-induced gas hydrate dissociation in this shallow water seep site.
259 juniper responded to warming with a shift to shallow water sources, whereas pinon pine responded to p
260              Constraints on the timescale of shallow water storage after precipitation events are inc
261 cant stress changes were associated with the shallow water table before or during the earthquake sequ
262 ged system is approximately 100 m(2), with a shallow water table.
263 gely corroborated patterns documented during shallow water underwater visual censuses, with up to an
264 reased deep water uptake and pinon increased shallow water uptake.
265 ed reciprocal transplant experiments along a shallow water volcanic pCO2 gradient to assess the impor
266 a combination of large ecosystem metabolism, shallow water, and long residence times.
267 ave radiated to occupy habitats ranging from shallow water, to near shore to the open ocean and the d
268 inates the visual acuity in these animals in shallow water.
269 and leading to the subsequent development of shallow-water anoxia, the hallmark of the T-OAE.
270 high productivity, principally the extensive shallow-water banks covered in seagrass meadows [2], whe
271 6 h) copper and cadmium exposures, using the shallow-water ecophysiological model organism Palaemon v
272  species has promoted interest in developing shallow-water ecotoxicological proxy species.
273  held perception that areas characterized by shallow-water methane seeps and/or strongly elevated sea
274                                Indeed, these shallow-water nearshore reefs may share many characteris
275 Here, we show by field observation that in a shallow-water octopus, Octopus tetricus, a range of visi
276 by tropical cyclone waves and currents, in a shallow-water or terrestrial setting.
277 gy framework, with kinetic energy predicting shallow-water richness, while chemical energy (export pr
278                            Subsequently, two shallow-water specialists expanded their population size
279 xicants differs across biogeographic ranges, shallow-water species may be suitable ecotoxicological p
280           In our experiments, fish swim in a shallow-water tunnel with controlled velocity, and stere
281 e report the first analyses that distinguish shallow-water zooxanthellate and deep-water azooxanthell
282 y derived from underwater visual censuses in shallow waters (</=30 m).
283 ort appears to remain resident year-round in shallow waters (<50 m depth) in a relatively fixed area.
284  substrate for in-situ incubation studies in shallow waters of Catalina Island, CA to investigate the
285  to the true CH4 emission estimates from all shallow waters, be them lakes, reservoirs, or coastal oc
286 tion, with no untouched populations known in shallow waters.
287              One strategy for mitigating the shallow wave penetration is to exploit eigenchannels wit
288 zation, might promote fecal contamination of shallow well water, thus increasing the risk of diarrhea
289      The data demonstrate the existence of a shallow well-ventilated northern-sourced cell overlying
290              A three-well design scheme with shallow-well GaAs/Al0.10Ga0.90As superlattices is develo
291                             It is shown that shallow-well heterostructures lead to optimal quantum-tr
292 ulic fractures can propagate 2000 ft upward, shallow wells may warrant special safeguards, including
293 ce and concentration in groundwater from 125 shallow wells, a dominant drinking water resource in rur
294 red seabed was hit each year, and just 7% of shallows were not hit.
295  in the world, containing millions of small, shallow wetlands.
296 rations in mutDNA using Tagged-Amplicon- and shallow Whole Genome- Sequencing.
297                                              Shallow whole-genome sequencing was performed on an Illu
298        Although the peat layer is relatively shallow (with a maximum depth of 5.9 metres and a median
299 g antibiotic administration and in simulated shallow wounds conditions.
300                              By exploiting a shallow zero-crossing of a Feshbach resonance, we charac

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