ライフサイエンスコーパス: creek

1 , RMSE = 43.8315, MAPE = 7.6029 for Barratta Creek).

2 everal decades contaminated nearby Coldwater Creek.

3 gtime 15-min rainfall extremes in Mahantango Creek.

4 ater at two downstream locations in a single creek.

5 the headwater and downstream regions of the creek.

6 re recalcitrant during P transport along the creek.

7 arily agricultural and suburban Little Rouge Creek.

8 ites, including a beach scour pond and tidal creek.

9 and 91%, depending on the snorkel survey and creek.

10 -edge marsh evolving into mudflats and wider creeks.

11 to their role in energy cycling within tidal-creeks.

12 osquitofish Gambusia hubbsi inhabiting tidal creeks.

13 , and 1900 +/- 1200 ng/L in roadway-impacted creeks.

14 food source for predators in small, forested creeks.

15 usly established plots located along a tidal creek; 10 plots are on forest islands surrounded by salt

16 cted in McLean Creek (30.1 mug/L) and Beaver Creek (190 mug/L), two tributaries that are physically i

17 men-derived organics were detected in McLean Creek (30.1 mug/L) and Beaver Creek (190 mug/L), two tri

18 9.3 h during the spring, and to the Fourmile Creek 8.4 km downstream site times were 18 and 8.8 h, re

19 for simulation of MWCNTs transport in Brier Creek, a coastal plain river located in central eastern

20 of 5-min precipitation data from Mahantango Creek, a long-term experimental agricultural watershed i

21 genus Cupriavidus isolated from Tim's Branch Creek, a second-order stream that eventually serves as a

22 g 17 storm events over three years in Miller Creek, a small roadway-impacted watershed in the Puget S

23 amined nutrient spatial patterns in Sycamore Creek, an intermittent desert stream in Arizona that exp

24 d 2.5 1 millimeters per year for the Mission Creek and Banning strands, respectively.

25 racts of the Channeled Scabland-Telford-Crab Creek and Cheney-Palouse-near 18 ka, whereas glacial iso

26 ng units (CFU) per 100 mL every year in Camp Creek and occasionally elsewhere, with exceedances trend

27 and common shiner (Luxilus cornutus)) in the creek and partitioning coefficients demonstrated that se

28 R) and 95% CIs between living near Coldwater Creek and several self-reported cancer outcomes were est

29 Four streams-Clear Fork, Lost Creek, Camp Creek and Still Creek-in northwestern Oregon's Sandy Riv

30 aze and Clean Air pattern, except at Bonanza Creek and Yakutsk, where anthropogenic pollution alters

31 m the coeval Tyrannosaurus rex and that Hell Creek (and equivalent) ecosystems supported a diverse as

32 mbers of the complex: the Highlands J, Buggy Creek, and Fort Morgan viruses.

33 ed nitrate removal was lower in the impacted creek, and higher chlorophyll levels were observed in a

34 ed through a tripartite division of the Hell Creek, and preservational biases were corrected for by c

35 the Athabasca River-Beaver River and McLean Creek-as possibly receiving OSPW seepage.

36 Sampling a salt marsh creek at high temporal resolution allowed assessment of

37 xides forming in the hyporheic zone of Pinal Creek, AZ, was investigated using extended X-ray absorpt

38 and slope-driven transport processes such as creek bank slumping.

39 s reduced geomorphic stability, resulting in creek-bank collapse with significant areas of creek-bank

40 reek-bank collapse with significant areas of creek-bank marsh converted to unvegetated mud.

41 shed in spatially equivalent positions along creek banks in monospecific stands of Spartina alternifl

42 ing to the loss of cordgrass from salt marsh creek banks.

43 sediment accretion in the agricultural Coon Creek Basin for the period 1975-93 was only about 6 perc

44 ydrologic simulations in the Ichawaynochaway Creek basin of Southwest Georgia.

45 intermediate in the middle drainage, Bishop Creek (BC).

46 xyhydroxides forming in inflow waters and on creek beds have V K-edge XANES spectra exhibiting E1/2 p

47 m populations to sparse tree lines along the creek beds.

48 ds during the 2014-2019 fall runs in Whatcom Creek, Bellingham, Washington, USA, and recorded visitat

49 d organism from the late Carboniferous Mazon Creek biota (approximately 309-307 million years ago) of

50 ler than the southernmost drainage, Big Pine Creek (BPC), where PGI allele 4 predominated.

51 Four streams-Clear Fork, Lost Creek, Camp Creek and Still Creek-in northwestern Oregon

52 Black Creek Canal (BCC) virus is a newly identified hantavirus

53 Black Creek Canal virus (BCCV) is a New World hantavirus which

54 letal proteins in the morphogenesis of Black Creek Canal virus (BCCV), a New World hantavirus.

55 -21.8% and from Sin Nombre, Bayou, and Black Creek Canal viruses by 23.8%-26.5%.

56 within samples collected from the Hazeltine Creek catchment affected by the August 2014 Mount Polley

57 Within groundwater of the Archer Creek Catchment in the Adirondack Mountains (New York) t

58 e analyzed in 3741 samples from 18 river and creek catchments between 2011 and 2016.

59 t moves downstream, was conducted at Boulder Creek, Colorado and Fourmile Creek, Iowa to determine in

60 The Buttermilk Creek Complex confirms the emerging view that people occ

61 15,528 artifacts that define the Buttermilk Creek Complex, which stratigraphically underlies a Clovi

62 eystone sea otter, burrowing crabs and marsh creeks, demonstrating the spatial generality of predator

63 nivore: Peromyscus maniculatus) in the Smoke Creek Desert of northwestern Nevada using (13) C and (15

64 n laurel leaves and seed-plant stems at Rose Creek document a diverse guild of piercing-and-sucking i

65 rhyodacite eruption, the ~650-y-old Deadman Creek Dome eruption, and several mafic subvolcanic orbic

66 sotope signatures of sediments in San Carlos Creek downstream of the former Hg mine New Idria, CA, US

67 hing the distribution of nds within the Bull Creek drainage of the Beaver River basin in the Oklahoma

68 vered along a small tributary of Last Chance Creek during hydraulic thawing that exposed the permafro

69 ak (Quercus spp.) savanna ecosystem at Cedar Creek Ecosystem Science Reserve in Minnesota, USA.

70 and during a 40 h time series in a mangrove creek (ecosystem scale).

71 d genetic and phenotypic data from beach and creek ecotypes of sockeye salmon (Oncorhynchus nerka) in

72 ly nutrient-enriched marshes worldwide, with creek-edge and bay-edge marsh evolving into mudflats and

73 he circumneutral pH environment of Hazeltine Creek, elevated V concentrations are likely naturally at

74 fication rates were observed in the impacted creek, especially near the wastewater discharge, and den

75 rted away from the mine with runoff into the creek, eventually affecting ecosystems downstream.

76 rgence of marsh surfaces, particularly where creeks exhibit morphologies that are unable to efficient

77 ture) in a complex landscape of the Reynolds Creek Experimental Watershed (RCEW) in southwest Idaho,

78 sensed environmental data from the Reynolds Creek Experimental Watershed in SW Idaho, USA.

79 In 2017, the Eagle Creek Fire burned 200 km(2) of the CRG, prompting concer

80 phenotypic differentiation between beach and creek fish was high and significant in all sampling year

81 a mealybug - from the Lower Cretaceous Rose Creek Flora of the Dakota Formation (c.

82 f macroalgal fossils from the Tonian Dolores Creek Formation (ca. 950 Ma) of northwestern Canada (Yuk

83 phic framework for the Upper Cretaceous Hell Creek Formation (HCF) of Montana reveals the evolutionar

84 latitude for the clade-the Cretaceous Prince Creek Formation (PCF) of northern Alaska.

85 illion-year-old sandstones from the Mosquito Creek Formation (Pilbara, Australia) using a suite of ad

86 l crocodylian from the Upper Cretaceous Hell Creek Formation and assess its origin, formation, and pa

87 While the 1.64-billion-year-old Barney Creek Formation contains chemical fossils of the earlies

88 rid collected from the Upper Cretaceous Hell Creek Formation in 2001 is identified as Pachycephalosau

89 hore surge deposit from the terrestrial Hell Creek Formation in Montana.

90 ial skull from the lower part of the Lincoln Creek Formation in Washington State, USA, we describe th

91 The Prince Creek Formation of Alaska, a rock unit that represents l

92 de Arctic avialan assemblage from the Prince Creek Formation of Alaska-the northernmost Late Cretaceo

93 cological diversity of dinosaurs in the Hell Creek Formation of Montana and North Dakota show no evid

94 g a T. rex tooth were discovered in the Hell Creek Formation of South Dakota.

95 osaur Edmontosaurus from the Cretaceous Hell Creek Formation previously found to exhibit low REE conc

96 annosaur skeleton (NCSM 40000) from the Hell Creek Formation that shares autapomorphies with the holo

97 type locality of the upper Maastrichtian Owl Creek Formation, offering an excellent opportunity to co

98 aurid from the Liscomb Bonebed of the Prince Creek Formation.

99 r Cretaceous strata of the South Dakota Hell Creek Formation.

100 high-latitude Late Cretaceous Arctic Prince Creek Formation.

101 Western Australian approximately 1.8-Ga Duck Creek Formation.

102 e WEE antigenic complex, including the Buggy Creek, Fort Morgan, Highlands J, Sindbis, Babanki, Ockel

103 egularly and are abundant in estuarine tidal creeks (from 0.3 to 6.3 individuals per km of creek, n =

104 latipinnis) migrating to a tributary, McElmo Creek, from the mainstem San Juan River for spawning.

105 ed by published geochemical data on the Kidd Creek gas, including the distribution of alkane abundanc

106 pproximately 2.3-Ga Western Australian Turee Creek Group opened a new window to life's early history.

107 opulation inhabiting the warmer stream, Piru Creek, had higher critical thermal maxima and higher fun

108 g and burrowing fronts at the heads of tidal creeks (hereafter, creekheads).

109 n (HTN), Seoul (SEO), Puumala (PUU), Convict Creek (HN107), and SN.

110 The lack of hexagonal nds suggests Bull Creek I is not near any impact site.

111 ort of an abundance spike of nds in the Bull Creek I Younger Dryas boundary soil is confirmed, althou

112 0 km), but beach catchment variables (drains/creeks, impervious surface, urban land cover) influenced

113 estuarine waterways and in a mangrove tidal creek, implying that submarine groundwater discharge was

114 ent, water, and freshwater biota in an urban creek in Canada.

115 ve association between living near Coldwater Creek in childhood and risk of cancer.

116 During field deployment at Muddy Creek in North Liberty, Iowa, optimal ENM-CNTs (PAN with

117 al daily sampling campaigns at Conococheague Creek in Pennsylvania.

118 designed to simulate conditions in Abraham's Creek in Quantico, Virginia.

119 For San Diego Creek in southern California, measurements from 1983 to

120 m the top 5 cm of sediment in a saline tidal creek in the estuary at Murrell's Inlet, South Carolina

121 Clear Fork, Lost Creek, Camp Creek and Still Creek-in northwestern Oregon's Sandy River Basin were mo

122 +/- 5% over the past <25 y and, by tripling creek-incision rates relative to nongrazed creekheads, h

123 cted at Boulder Creek, Colorado and Fourmile Creek, Iowa to determine in-stream transport and attenua

124 upport the idea that Zn attenuation in Pinal Creek is largely controlled by sorption to microbial Mn

125 eth River, Virginia with PAH-sensitive Kings Creek (KC) fish.

126 t-bodied fossil from the Carboniferous Mazon Creek Lagerstatte (Illinois, USA).

127 We revisit the 2017 Mud Creek landslide in California using radar interferometry

128 cterize 8 years of stable sliding of the Mud Creek landslide, California, USA, prior to its rapid acc

129 odiscid shells may have only reached the Owl Creek locality by drifting seaward after death.

130 ission came from a single surface mine (Hail Creek) located in a methane-rich coal basin.

131 imately one year, and daily U discharge to a creek, located approximately 50 m from the injection wel

132 In other samples from the same creek, loss of HuNoV infectivity could not be attributed

133 Residential proximity to Coldwater Creek (<=1, >1 to 5, >5 to 20, and >20 km) in childhood

134 eks to beaches were deeper bodied than other creek males.

135 , with beach males having deeper bodies than creek males.

136 We find that alkane gases from the Kidd Creek mines in the Canadian Shield are microbial product

137 to the fracture fluids in Birchtree and Kidd Creek mines within the Canadian Precambrian crust.

138 Comparable results from Cedar Creek (MN) support both hypotheses and suggest that sens

139 nontargeted data was collected from the Fall Creek Monitoring Station (Ithaca, NY), where daily sampl

140 We established the Fall Creek Monitoring Station in March 2017 and collected dai

141 ons in daily composite samples from the Fall Creek Monitoring Station over 18 months.

142 iculate matter from estuarine sources at the creek mouth region and importing it upstream.

143 reeks (from 0.3 to 6.3 individuals per km of creek, n = 45 surveys).

144 31 dogs and 32 horses that reside in Gray's Creek NC at households with documented PFAS contaminatio

145 characterized bacterial aerosols at Newtown Creek (NTC), a public waterway and Superfund site in a d

146 Piru Creek O. mykiss, however, had higher resting metabolic r

147 abrupt nanoparticle release event to a tidal creek of a Spartina -dominated estuary.

148 ative roadway runoff and stormwater-affected creeks of the U.S. West Coast indicated widespread occur

149 ative roadway runoff and stormwater-affected creeks of the U.S. West Coast indicated widespread occur

150 osquitofish (Gambusia spp.) inhabiting tidal creeks on six different Bahamian islands.

151 uman serum and natural creek water (Highland Creek, ON) with good recovery.

152 stal corridors in the Paleoproterozoic Halls Creek Orogen, a rheologically-weak rift zone adjacent to

153 flooding considering the lower part of Darby Creek, PA, USA.

154 adult Bahamas mosquitofish from seven tidal-creek populations across Andros Island, The Bahamas that

155 Multi-creek surveys comparing marsh creeks pre- and post-sea otter colonization confirmed th

156 source in samples collected from four local creeks, presence probabilities were low for all sources,

157 ominated faunal structure as in the Careless Creek Quarry of the USA that was also deposited under a

158 dominated in the northernmost drainage, Rock Creek (RC), which was also significantly cooler than the

159 The typical northern California creek receiving urban stormwater runoff contains fiproni

160 Predator-exclusion experiments in five marsh creeks revealed that sea otters suppress the abundance o

161 s and springs, discharging directly to urban creeks, reveals high concentrations of TDS, sulfate, Cd,

162 atch is for an age of 1.186 Ma for the Alder Creek Rhyolite sanidine and 28.201 Ma for the Fish Canyo

163 In this study, creek sediment samples were collected in the stream bed

164 Creek sediments carry an integrated isotope signature of

165 Overall, our results suggest that analyzing creek sediments downstream of former Hg mines can provid

166 nal arxA-like sequences in Mono Lake and Hot Creek sediments, both arsenic-rich environments in Calif

167 ould not be ruled out as source of Hg to the creek sediments.

168 et sp. nov., from the Francis Creek Shale (309-307 million years ago) of Illinois, Uni

169 s extracted from ground stone tools at North Creek Shelter, southern Utah.

170 upstream creek water, which decreased after creek-side residences were educated about proper pet was

171 April and July of 2009 in a reach at McTier Creek, South Carolina to determine the relative importan

172 regional hydraulic gradient from from Spring Creek Spring Complex (SCSC), a group of submarine spring

173 These data establish the Mission Creek strand as the primary fault bounding the Pacific a

174 n 224 2-y-old children residing near the Tar Creek Superfund Site.

175 of rGO-1h and rGO-2h remain stable in Call's Creek surface water, while effluent wastewater readily d

176 Multi-creek surveys comparing marsh creeks pre- and post-sea o

177 tudied for water samples taken from an urban creek system (Duck Creek Watershed, Cincinnati, OH) impa

178 two PAH-contaminated sediments: Chattanooga Creek (Tennessee) and Lake Erie (western basin).

179 e industrially contaminated East Fork Poplar Creek, Tennessee (EFPC) were measured during 2014-2016 u

180 ribing the origin and fate of V in Hazeltine Creek that is applicable to other river systems is prese

181 s and edge erosion have declined markedly in creeks that have high levels of sea otter recolonization

182 City of Boulder Colorado's WWTF and Boulder Creek, the receiving stream.

183 ace runoff, are observed in the Little Rouge Creek throughout storm hydrographs, with an occasional f

184 le Technology (TAST) was deployed at Whatcom Creek to deter harbor seals from preying on fall runs of

185 eriment in an impacted and a reference tidal creek to investigate the impacts of wastewater discharge

186 than other beach fish, and male strays from creeks to beaches were deeper bodied than other creek ma

187 mortality when adult salmon migrate to urban creeks to reproduce.

188 ptomyces sp. AD-23-14 isolated from the Rock Creek underground coal mine acid drainage site.

189 eries of grassland community data from Cedar Creek, USA, to examine the joint effects of pulse soil d

190 rm follow-up of the survivors of the Buffalo Creek (W.Va.) flood.

191 Surface water from a freshwater creek was filter-sterilized, inoculated with HuNoV (GII.

192 centration of [Ca(2+)] and [K(+)] in a local creek was found to be 257 +/- 7.3 and 28.1 +/- 1.1 muM,

193 Australian rivers (Albert River and Barratta Creek) was forecasted for up to 10 days using a novel de

194 cal matrixes such as human serum and natural creek water (Highland Creek, ON) with good recovery.

195 were exposed for 28 days to upstream Boulder Creek water and WWTF effluent under controlled condition

196 CNTs were present predominantly in the Brier Creek water column, while downstream MWCNT surface and d

197 In one creek water sample, genome damage was likely a dominant

198 to determine the K(+) and Ca(2+) contents in creek water samples.

199 load of 0.1 kg d(-1) in the uppermost Brier Creek water segment showed that MWCNTs were present pred

200 isotope values of particulate P pools in the creek water suggested that the NaHCO(3)-P pool was bioav

201 , and denitrification inhibition by impacted creek water was clearly observed in the microcosm experi

202 hree real water samples including tap water, creek water, and river water were analyzed and yielded r

203 Canine sources included input via upstream creek water, which decreased after creek-side residences

204 ncentrations of Hg(I) (4.4-6.1 mug L(-1)) in creek waters from a heavily Hg-polluted area, accounting

205 thods to extract DBPs in 10 L of chlorinated creek waters.

206 historical releases of BTs within the Mimico Creek watershed have likely led to elevated summation op

207 10 times higher in the more urbanized Mimico Creek watershed relative to the primarily agricultural a

208 speciation of Bacteroidales within the Duck Creek Watershed using next-generation sequencing technol

209 mples taken from an urban creek system (Duck Creek Watershed, Cincinnati, OH) impacted by combined se

210 y across multiple stream orders in Frenchman Creek watershed, USA.

211 of DRWH and ARWH systems adapted to the Back Creek watershed, Virginia.

212 collected from stream habitats of the French Creek watershed, which is renowned for its unique and ri

213 the most downstream (7.4 km) site in Boulder Creek were 6.2 h during the summer and 9.3 h during the

214 Potential hexagonal nds at Bull Creek were found to be more consistent with graphene/gra

215 Male strays from beaches to creeks were shallower bodied than other beach fish, and

216 treams, except the sites in the Little Rouge Creek with low levels of vehicle traffic.

217 e duration (min) individuals remained at the creek with TAST on, and a significant 43.8% reduction in

218 The samples were collected from the Gorjak creek (Zagreb, Croatia), a recipient of wastewater efflu