ライフサイエンスコーパス: riverine

1 ilica, respectively, which are comparable to riverine and atmospheric inputs.

2 ecological phase involves a transition from riverine and deltaic environments to marine ones, concom

3 ation change experiment, and also applied to riverine and marine DOC.

4 radiogenic (Delta(14) C) isotopes that trace riverine and marine organic matter sources as they are p

5 onriverine sites was high in comparison with riverine and mixed geomorphic settings, with sites close

6 ological system, with major implications for riverine and near-shore marine environments.

7 atively high variation in OC storage between riverine and nonriverine geomorphic settings indicates t

8 Direct comparison of riverine and reservoir reaches, where sedimentation in t

9 Also, wetlands experiencing more (riverine and tidal) hydrologic exchange recovered more r

10 lerae, an autochthonous member of estuarine, riverine, and marine habitats and the causative agent of

11 s and small mammals indicate that a putative riverine barrier (the Jurua River) does not relate to pr

12 ocene marine incursion, Pliocene/Pleistocene riverine barriers and Pleistocene refugia.

13 has systematically evaluated the impact that riverine barriers might have on structuring whole Amazon

14 The riverine bicarbonate flux originates mainly from the dis

15 es are a key, but understudied, component of riverine biogeochemical function.

16 Riverine biological processes could potentially be respo

17 Riverine bluff areas also appeared less heavily occupied

18 f some elements contributed significantly to riverine budgets (e.g., 24% for Zn, 50% for P, and 83% f

19 termediate reservoir, then the importance of riverine carbon in the ocean carbon cycle has been under

20 Our estimates of riverine carbon storage represent a previously undocumen

21 the implications of temporal changes in the riverine chemical weathering flux for oceanic geochemica

22 ogeographical evidence suggesting that these riverine cichlids are products of a recent adaptive radi

23 conducted between May and July 2015 in four riverine communities in Mazan district.

24 support a "nodal" or heterogeneous model of riverine community organization across a particularly ex

25 in carbon storage; and historical changes in riverine complexity have likely reduced carbon storage.

26 ics, which is reflected in the delta(15)N of riverine consumer tissues.

27 ne deposition rate is overestimated, whereas riverine deposition is underestimated by at least an ord

28 fluents made only a moderate contribution to riverine discharge (21% for PFOA, 6% for PFOS), while at

29 ivity maxima and increased precipitation and riverine discharge from northern South America are close

30 d polyfluoroalkyl substances (PFASs) through riverine discharge into coastal waters.

31 Global riverine discharge of organic matter represents a substa

32 Inputs (from riverine discharge, atmospheric deposition, coastal wast

33 be equal or larger by a factor of 16 to the riverine discharge.

34 estrial and marine net primary productivity, riverine dissolved and suspended matter fluxes to the oc

35 ssolved carbon and nitrogen, indicating that riverine dissolved components could be used to scale GHG

36 Riverine dissolved sulfate (SO4(2-)) flux and sulfur sta

37 ue can be successfully applied to marine and riverine DOC without further sample pretreatment.

38 ic input will drive substantial variation in riverine DOM and, thus, estuarine optics and photochemis

39 Determining the molecular composition of riverine DOM is essential for understanding its source,

40 at the genetic structure would correspond to riverine drainage basins.

41 historic as well as present-day patterns of riverine drainages.

42 underappreciated interannual variability of riverine DSi fluxes.

43 zone biogeochemistry and its influence over riverine ecosystem function.

44 though the importance of these subsidies for riverine ecosystems is increasingly recognized, little i

45 onal forest ecosystems and here in dendritic riverine ecosystems suggests the possible application of

46 namic way to create spatial heterogeneity in riverine ecosystems, and provides a means to detect spat

47 Past shifts in connectivity in riverine environments (for example, sea-level changes) a

48 In general, rotifers were more abundant in riverine environments than lakes and reservoirs.

49 Riverine environments, such as streams and rivers, have

50 semiaquatic and lived in freshwater swamp or riverine environments, where they grazed on freshwater v

51 atterns of fish distributions in schools and riverine environments.

52 at modifying the supply of organic matter to riverine, estuarine, and coastal food webs need to incor

53 lerae, has been shown to be autochthonous to riverine, estuarine, and coastal waters along with its h

54 Riverine export of particulate organic carbon (POC) to t

55 cation has resulted in increased base-cation riverine exports (Ca(2+), Mg(2+), Na(+), K(+)) correlate

56 lthough local and basin-scale differences in riverine fish diversity have been analysed as functions

57 Here, we derive a gridded global map of riverine fisheries and assess its implications for biodi

58 ent, which commonly occurs as contaminant in riverine floodplains and associated wetlands affected by

59 ated by an increase in the Fe:S ratio of the riverine flux after Sturtian glacial removal of a long-l

60 We contend that the riverine flux obtained from observations of modern river

61 n tons per year, which is ~10% of the global riverine flux of dissolved organic carbon (DOC).

62 we quantify the global impact of dams on the riverine fluxes and speciation of the limiting nutrient

63 consideration of the temporal variability in riverine fluxes largely ameliorates long-standing proble

64 tes of terrestrial organic C, which supports riverine food webs and is a source of CO2, are lacking.

65 ncorporation of allochthonous subsidies into riverine food webs.

66 ks, our framework facilitates predictions of riverine [Formula: see text] emissions globally using wi

67 (EEA), reveal centennial-scale variations of riverine freshwater input that are synchronous with nort

68 tion within nonriverine settings, but not in riverine geomorphic settings.

69 Predicted increases in riverine hypoxia via eutrophication and increased temper

70 erine settings along with those with reduced riverine influence located on tide-dominated sand island

71 The riverine input of fine particles played an important rol

72 mercury observed in atmospheric deposition, riverine input, seawater, freshwater lakes, and freshwat

73 sea ice-modified atmospheric deposition and riverine input.

74 spheric deposition while CH is influenced by riverine input.

75 Riverine inputs of Hg to the North Atlantic have decreas

76 is, values on the same order of magnitude as riverine inputs of P and N to the MS.

77 e observed in coastal waters receiving major riverine inputs of terrestrial CDOM (0.06-0.5 m(3) (mol

78 hese clones were from sites far removed from riverine inputs, suggesting a wide diffusion of pathogen

79 astal and shelf areas that are influenced by riverine inputs.

80 cosystems, our results clearly indicate that riverine iron fluxes need to be accounted for as the vol

81 mates of global silicate fluxes derived from riverine measurements.

82 Results show a projected 10-fold increase in riverine MeHg levels and a 2.6-fold increase in estuarin

83 Riverine mercury export to AO is estimated at 50 Mg yr(-

84 (3) The alloy exhibits an unusual riverine microstructure of martensite not seen in other

85 U.S. watersheds and tested against available riverine N flux estimates.

86 Riverine N2 O emission estimates will be further enhance

87 Previous studies may overestimate global riverine N2 O emission rates (300-2100 Gg N2 O-N yr(-1)

88 de the best fit between modeled and observed riverine N2 O emission rates (EF(a): R(2) = 0.92 for bot

89 from published literature to estimate global riverine N2 O emission rates and emission factors.

90 Global riverine N2 O emission rates are forecasted to increase

91 ads for 6400 rivers, models estimated global riverine N2 O emission rates of 29.6-35.3 (mean = 32.2)

92 Riverine N2 O flux was significantly correlated with NH4

93 ture of [Formula: see text] production along riverine networks, our framework facilitates predictions

94 tions of [Formula: see text] emissions along riverine networks.

95 allows examination of the impact of imposing riverine nitrate-N load limits on the biofuel production

96 a in the northern Gulf of Mexico by reducing riverine nitrate-N loads represent two such cases that o

97 l agricultural activities strongly influence riverine nitrogen (N) dynamics, which is reflected in th

98 ANI has been shown to be a good predictor of riverine nitrogen export.

99 r networks and improving estimates of global riverine nitrogen loads.

100 Estimates of global riverine nitrous oxide (N2 O) emissions contain great un

101 trations on the shelf in response to varying riverine nutrient and organic carbon loads, boundary flu

102 Sea surface warming and reduced riverine nutrient inputs are found to be likely contribu

103 dsummer hypoxic areas were most sensitive to riverine nutrient loads and sediment oxygen demand from

104 kes up much of the DOC and particulate OC of riverine OC (along with soil OC), why do we not see more

105 enzymatic processes in the mineralization of riverine OM: (i) the role of phenol oxidase activity in

106 For example, riverine organic matter assimilation by the glacier-nest

107 r runoff, but the influence of the influx of riverine organic matter on the trophodynamics of coastal

108 issues of marine consumers, estimates of the riverine organic matter source contribution to upper tro

109 We quantified the ecological impact of riverine organic matter subsidies to glacier-marine habi

110 Riverine organic matter supports of the order of one-fif

111 found in the open lake is not simply diluted riverine organic matter.

112 ed geomorphic settings, with sites closer to riverine outflow from the east and south of Moreton Bay

113 to calculate PFAA atmospheric inputs to and riverine outputs from the catchments.

114 ogeneity in controlling processes, including riverine particulate material loads, historically changi

115 tional genes also showed clear backwater and riverine patterns.

116 This riverine population of approximately 5000 individuals is

117 netic structure and demographic processes in riverine population of fishes.

118 understanding of basal resources supporting riverine productivity.

119 thin paleodrainages can be explained by past riverine properties (i.e., area and number of rivers in

120 Our findings extend the influence of current riverine properties on genetic diversity to those associ

121 the order of hours, days, and a week for the riverine, river-impacted, and open lake waters, respecti

122 based on their absorbance properties (a300): riverine, river-impacted, or open lake sites.

123 Atmospheric deposition and riverine runoff have been traditionally considered the m

124 t worldwide coastal eutrophication fueled by riverine runoff of fertilizers and the burning of fossil

125 Shanghai and Jiangsu areas, which differ in riverine sediment supply and tidal flat management patte

126 t geomorphological settings (wetlands within riverine settings along with those with reduced riverine

127 indicators of N loading might be accurate in riverine settings, but could be inaccurate when consider

128 ) groups involved in nitrogen cycling in the riverine sites, suggesting a higher level of bacterial a

129 functionally different between backwater and riverine sites, which represent communities with and wit

130 pristine preindustrial natural baselines of riverine SO4(2-) flux and delta(34)S cannot be directly

131 lable dissolved organic carbon from external riverine sources supports a large component of ecosystem

132 MeHg in two riparian spiders is derived from riverine sources while approximately 45% of MeHg origina

133 , Lake Victoria), and Astatotilapia burtoni (riverine species around Lake Tanganyika).

134 palis gambiensis (Diptera: Glossinidae) is a riverine species that is still present as an isolated me

135 fy coastal evacuations by otherwise resident riverine striped bass in the Hudson River Estuary, New Y

136 Riverine sul1 correlated with upstream capacities of ani

137 However, the direction of range shifts in riverine systems is less clear.

138 Cores collected from large-scale riverine systems with many wastewater sources recorded i

139 hin grid cells and the potential C export to riverine systems, in a way to be conservative in a mass

140 Riverine systems, where groundwater mixes with surface w

141 large-scale spatial biodiversity patterns in riverine systems.

142 one will substantially increase (19 +/- 14%) riverine total nitrogen loading within the continental U

143 Riverine transport of iron (Fe) and arsenic (As) is affe

144 e focused on Glossina palpalis gambiensis, a riverine tsetse species representing the main vector of

145 , and appeared similar to small terrigenous (riverine) UDOM even in marine water.

146 rates were relatively high when compared to riverine uptake, especially during the spring and summer

147 and plant CO2 fertilization to increases in riverine water and carbon export from this large region

148 sis of certified reference materials (SLRS-4 Riverine water and NIST SRM 1515 Apple leaves).

149 ngs highlight the degree to which changes in riverine water and sediment discharge can be related wit

150 h-to-north advection and dilution with fresh riverine water enroute, and/or lower production in the n