ライフサイエンスコーパス: creek

1 arily agricultural and suburban Little Rouge Creek.

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

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

4 food source for predators in small, forested creeks.

5 -edge marsh evolving into mudflats and wider creeks.

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

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

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

9 9.3 h during the spring, and to the Fourmile Creek 8.4 km downstream site times were 18 and 8.8 h, re

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

33 -21.8% and from Sin Nombre, Bayou, and Black Creek Canal viruses by 23.8%-26.5%.

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

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

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

37 15,528 artifacts that define the Buttermilk Creek Complex, which stratigraphically underlies a Clovi

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

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

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

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

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

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

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

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

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

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

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

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

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

51 Western Australian approximately 1.8-Ga Duck Creek Formation.

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

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

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

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

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

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

58 0 km), but beach catchment variables (drains/creeks, impervious surface, urban land cover) influenced

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

82 Creek sediments carry an integrated isotope signature of

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

106 10 times higher in the more urbanized Mimico Creek watershed relative to the primarily agricultural a

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

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

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

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

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

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

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

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