ライフサイエンスコーパス: open ocean

1 processes of iceberg degradation towards the open ocean.

2 and modeling polarization camouflage for the open ocean.

3 of magnitude greater than those observed in open ocean.

4 vigation towards settlement habitat from the open ocean.

5 ndant in the water column of the coastal and open ocean.

6 gnificant source of bioavailable iron in the open ocean.

7 eshwater systems and coastal margins, to the open ocean.

8 ic oceans from shallow coastal waters to the open ocean.

9 ed search at the large spatial scales of the open ocean.

10 eutrophication and nitrogen pollution of the open ocean.

11 n many aquatic environments particularly the open ocean.

12 asing DFe throughout the water column in the open ocean.

13 ide on the surface of ponds, rivers, and the open ocean.

14 d ocean surface elevations observed over the open ocean.

15 across strong thermal gradients found in the open ocean.

16 1.7 x 10(30) cells/yr and is highest in the open ocean.

17 representatives of this phylum occur in the open ocean.

18 tion and microbial community dynamics in the open ocean.

19 n on the atmospheric microbial load over the open ocean.

20 se dynamic microhabitats in the oligotrophic open ocean.

21 rogue waves that appear from nowhere in the open ocean.

22 but considerably less so in the oligotrophic open ocean.

23 trophic regions, which constitute 30% of the open ocean.

24 water off Changjiang Estuary and 0.19 in the open ocean.

25 system stability across vast expanses of the open ocean.

26 gic thaumarchaeon CN25, originating from the open ocean.

27 for understanding archaeal adaptation to the open ocean.

28 dification in coastal waters compared to the open ocean.

29 ression patterns of the UCYN-A1 clade in the open ocean.

30 oorganisms occupying surface seawater in the open ocean.

31 cumulation of floating plastic debris in the open ocean.

32 nitrogen removal in the anoxic zones of the open ocean.

33 serves as a novel ecological habitat in the open ocean.

34 mical events and biological responses in the open ocean.

35 ion for confronting the iron scarcity of the open oceans.

36 on rates at ammonium concentrations found in open oceans.

37 nt contributors to primary production in the open oceans.

38 turbulence levels >10,000 times that in the open ocean, (3) determine that the Kuroshio western boun

39 seawater effects are a worldwide increase in open-ocean acidity and large-scale declines in calcium c

40 ) a dispersal barrier of at least 3900 km of open ocean and (ii) the breeding barrier of self-incompa

41 totrophic bacteria are abundant in the upper open ocean and comprise at least 11% of the total microb

42 be exported to the continental shelf and the open ocean and could shift the effect of anthropogenic n

43 on of the vocal behaviour of penguins in the open ocean and discuss the function of their vocal commu

44 s encompassing lakes, rivers, estuaries, the open ocean and forested and non-forested terrestrial eco

45 lankton causes isotopic fractionation in the open ocean and in culture.

46 sition of anthropogenic atmospheric N on the open ocean and its incorporation into plankton and, in t

47 ing from shallow water, to near shore to the open ocean and the deep sea.

48 +/- 2700 Mg a(-1)), of which 28% reaches the open ocean and the rest is deposited to ocean margin sed

49 tions characteristic of large regions of the open ocean and thus have consequences for ecological nic

50 esiding throughout the euphotic zones in the open oceans and are major contributors to the global car

51 numerically dominant photoautotrophs in the open oceans and contributors to the global carbon cycle.

52 ultivated unicellular prymnesiophyte alga in open-ocean and coastal environments.

53 2)S) in seawater sulphate through oxygenated open-ocean and OMZ-bearing water columns.

54 natural waters (apart from the oligotrophic open ocean), and the device was deployed in an estuarine

55 breaking waves in the laboratory and in the open ocean, and provide a quantitative description of bu

56 be still dominated by large inputs from the open ocean, and there is little evidence of anthropogeni

57 However, the relevance of these sources in open-ocean anoxic zones is debated.

58 Superficially, the open ocean appears homogeneous, with few clear barriers

59 ndensable iodine-containing vapours over the open ocean are sufficient to influence marine particle f

60 Significantly higher %Hg(0) observed in open ocean areas (15.8 +/- 3.9%) may reflect lower disso

61 eneration rates may be sustainable over some open ocean areas.

62 Similar to other open ocean basins, Arctic MeHg concentration maxima also

63 ic understanding of food web function in the open ocean, because plastidic protists should now be con

64 d 5.2% decrease in future (2091-2100) global open ocean benthic biomass under RCP8.5 (reduction of 5.

65 lts from two Pacific Ocean sites, margin and open ocean, both of which have deep, subsurface stimulat

66 s panmictic species, which reproduces in the open ocean but spends most of its prereproductive life i

67 dicated a crucial role of olfaction over the open ocean, but left open the question of whether birds

68 ry production in oligotrophic regions of the open ocean, but recent studies have showed that biologic

69 Invasion of the open ocean by tetrapods represents a major evolutionary

70 ed for a significant fraction of coastal and open ocean communities, respectively, and members of the

71 s were more dissimilar from their respective open ocean communities.

72 cial stagnation event appears decoupled from open ocean conditions and may have resulted from coastal

73 machinery (consistent with the fact that the open ocean constitutes a far more constant and buffered

74 re the relatively stable temperatures of the open ocean constrain temperature-dependent sex determina

75 Labrador Sea Water (LSW), formed by open ocean convection in the subpolar North Atlantic, is

76 ring cold intervals, we infer a reduction in open-ocean convection and an associated incursion of an

77 re by northeast Atlantic convection, reduced open-ocean convection in both the northwest and northeas

78 Deepwater formation in the North Atlantic by open-ocean convection is an essential component of the o

79 small Rossby deformation radius typical for open-ocean convection sites, the most probable states th

80 eostrophic models for the spreading phase of open-ocean convection.

81 ic anthropogenic fixed nitrogen entering the open ocean could account for up to about a third of the

82 nd that production of these compounds in the open ocean could increase CCN there too.

83 We tested open-ocean crypsis in nature by collecting more than 150

84 microbial species, including the ubiquitous open ocean cyanobacterium, Prochlorococcus marinus.

85 Open-ocean deep convection, one of the processes by whic

86 been suggested as an additional location for open-ocean deep convection.

87 uced biological differences that result from open-ocean depth gradients.

88 p-sea-core isotopes, and by the discovery of open-ocean diatoms in subglacial sediments.

89 TR-antagonist, as well as relocation to the open-ocean, disturb A. triostegus larvae transformation

90 sources and to exert top-down control in the open ocean ecosystem.

91 he mass extinction, but the structure of the open-ocean ecosystem did not fully recover for more than

92 azotrophs) are a major source of nitrogen to open ocean ecosystems and are predicted to be limited by

93 ardines, and the productivity of coastal and open ocean ecosystems have varied over periods of about

94 nvironments, but the influence of plastic on open ocean ecosystems is poorly understood, particularly

95 In open ocean ecosystems, competition for low availability

96 host cell abundance seem to be a feature of open ocean ecosystems.

97 ktonic organisms underpin the functioning of open ocean ecosystems.

98 ion for effective concealment in the complex open ocean environment.

99 indings are consistent with the existence of open-ocean environmental conditions earlier in the Prote

100 the importance of camouflage in near-surface open ocean environments and (ii) the use of a Stokes con

101 aters to coastal systems and ultimately into open ocean environments.

102 and extinction in epicontinental seas versus open-ocean-facing coastal regions in the Permian through

103 xed, indicating that epicontinental seas and open-ocean-facing coastlines carry distinct macroevoluti

104 d differently in epicontinental seas than in open-ocean-facing habitats of comparable depth.

105 formation to guide their return from distant open-ocean feeding areas.

106 e surface-reflectance Mueller matrix of live open ocean fish (lookdown, Selene vomer) and seagrass-dw

107 Open-ocean fish species exhibited camouflage that was su

108 orage over thousands of square kilometers of open ocean for patchily distributed live prey and carrio

109 Globally, the source of Hg to the open ocean from rivers amounts to 30% of atmospheric inp

110 ironmental sequences from an estuary and the open ocean generated with high throughput sequencing and

111 In the open ocean genetically diverse clades of the unicellular

112 e markedly different between the coastal and open ocean genomes and suggest a more prominent role for

113 teria are often abundant in the oligotrophic open ocean gyres.

114 eriod of glaciation that resulted in loss of open-ocean habitat south of the polar front, driving non

115 and microscopic evidence indicates that the open ocean harbors a diverse range of novel free-living

116 Pacific, it has been suggested that even the open ocean has been affected.

117 as much as 20% of prokaryotic biomass in the open ocean, have been linked to environmentally relevant

118 in vast regions of the modern ocean, such as open-ocean, high nutrient low chlorophyll areas and coas

119 Most of the earth's prokaryotes occur in the open ocean, in soil, and in oceanic and terrestrial subs

120 hemical cycles by supplying nutrients to the open ocean, in turn stimulating ocean productivity and c

121 t low-frequency, ambient noise levels in the open ocean increased approximately 3.3 dB per decade dur

122 In large regions of the open ocean, iron is a limiting resource for phytoplankto

123 spite appearing featureless to our eyes, the open ocean is a highly variable environment for polariza

124 cription of the scope of this problem in the open ocean is lacking.

125 ntering an extremely large rogue wave in the open ocean is much larger than expected from ordinary wa

126 n in the aquatic ecosystems-particularly the open oceans-is sufficiently low to limit photosynthetic

127 jor contributors to nitrogen fixation in the open ocean, lives in symbiosis with single-celled phytop

128 rden through bromine and iodine emitted from open-ocean marine sources has been postulated by numeric

129 ine this problem by combining long-distance, open-ocean marine turtle movements (obtained via long-te

130 n (N) and phosphorus (P) availability in the open ocean may favor the loss of Fe response genes when

131 cal evidence of ocean acidification (OA) via open-ocean measurements for the past several decades, it

132 Here we perform the first synthesis of open-ocean measurements of the specific rate of surface

133 ns, however, has been difficult to test with open ocean microbes because sampling methods commonly ha

134 es associated with key metabolic pathways in open ocean microbial species-including genes involved in

135 marine environments ranging from sea ice to open ocean mixed layer to tropical coral reefs, and in e

136 istribution of plastic on the surface of the open ocean, mostly accumulating in the convergence zones

137 ered to be the most important contributor to open-ocean N2 fixation.

138 and 2.7 Tmol/yr nitrogen to the coastal and open ocean near major source regions in North America, E

139 might make a substantial contribution to the open ocean nitrogen budget.

140 Animals inhabiting the open ocean often conceal themselves by being highly tran

141 thylsulfoniopropionate (DMSP) degradation in open-ocean, oligotrophic regions were investigated durin

142 e of the highest concentrations found in the open-ocean OMZs of the Pacific and Indian Oceans.

143 ard impingements of cyclonic eddies from the open ocean on the Kuroshio main stream in place of antic

144 ally more highly productive and dynamic than open ocean ones.

145 ral larvae to navigate to reefs while in the open-ocean, or to settlement sites while on reefs is ext

146 of a coastal current, bringing warm water of open ocean origin through the Filchner Depression and in

147 al pattern in the delta(13)C measured in the open oceans over the same time period.

148 Moreover, I contend that open-ocean particle production and cloud enhancement do

149 In the vast and barren open ocean, partnership with photosymbionts that have ex

150 similar, but not identical, to profiles for open-ocean pelagic fishes, suggesting that in both setti

151 ycles, symbioses are poorly characterized in open ocean plankton.

152 or Levy search patterns across 14 species of open-ocean predatory fish (sharks, tuna, billfish and oc

153 ubsurface metabolic activity: a sulfate-rich open-ocean province, and an ocean-margin province where

154 er Columbia River were introduced for salmon open-ocean ranching in the late 1970s and 1980s, and wer

155 ds the magnitude of long-term projections in open ocean regions.

156 and ultraoligotrophic conditions typical of open ocean regions.

157 acterial diazotrophs commonly found in other open ocean regions.

158 these three sources to the Fe budget of the open ocean remains contentious.

159 th no object to hide behind in 3D space, the open ocean represents a challenging environment for camo

160 rger than the changes of the global mean and open ocean, resulting in a fast increase of extremely ho

161 both in near-shore coastal water and in the open ocean, rising coastal nitrogen levels, and widespre

162 variability of dominant dsDNA viruses in the open ocean's euphotic zone over daily and seasonal times

163 ion varied in natural waters, from 352 pM in open ocean seawater (mean, 779 pM +/- 15.0%, RSD) to 58.

164 diverse bacteria are abundant in coastal and open-ocean seawater samples.

165 arcian Oceanic Anoxic Event or T-OAE from an open ocean sedimentary succession from western North Ame

166 igination rates were significantly higher in open-ocean settings for a protracted interval from the L

167 xtinction rates were significantly higher in open-ocean settings than in epicontinental seas during m

168 o generally sparse biological communities in open-ocean settings, seamounts and ridges are perceived

169 n of organic carbon burial to terrestrial or open-ocean settings.

170 At the open ocean site, increases in numbers of prokaryotes at

171 lk water column nitrification at coastal and open ocean sites with sub-micromolar ammonia/ammonium co

172 At open-ocean sites, nitrate and oxygen are supplied to the

173 lar to particles in marine air masses in the open ocean (Southeast Pacific Ocean) and coastal sites a

174 e reef flat, normally indistinguishable from open-ocean SST, exceeded 6 degrees C above normal summer

175 ers of viral community structure at a single open ocean station, whereas variability along onshore-of

176 the West African continental shelf and four open ocean stations, including the CVOO time series site

177 CC9311, has significant differences from an open ocean strain, Synechococcus sp. strain WH8102, and

178 ation modifications for polarocrypsis in the open ocean, suggesting a mechanism for natural selection

179 e also observed high diatom diversity in the open ocean, suggesting that diatoms may be more relevant

180 However, the global load of plastic on the open ocean surface was estimated to be on the order of t

181 ropogenic carbon dioxide (CO2) has acidified open-ocean surface waters by 0.1 pH units since preindus

182 y flexible species actively grows within the open-ocean surface waters, thus occupying both planktic

183 of the latter hypothesis that focuses on the open ocean surrounding Antarctica, involving both the bi

184 t there are unicellular cyanobacteria in the open ocean that are expressing nitrogenase, and are abun

185 source of nutrients and trace metals to the open ocean that can enhance ocean productivity and carbo

186 rophic prokaryotes in the upper 200 m of the open ocean, the ocean below 200 m, and soil are consiste

187 d to phototrophic living in the oligotrophic open ocean-the most extensive biome on Earth.

188 Pelagic seabirds wander the open oceans then return accurately to their habitual nes

189 Rogues form in the open ocean through the addition of elemental wave trains

190 r, that tidal dissipation also occurs in the open ocean through the scattering by ocean-bottom topogr

191 ns at ocean margins but are too small in the open ocean to explain observed declines of seawater conc

192 r home river, but how they navigate from the open ocean to the correct coastal area has remained enig

193 the inaccessibility of the foraging site-the open ocean-to researchers.

194 Our results are based on an open-ocean tracer release of trifluoromethyl sulphur pen

195 A model of iodine chemistry in the open ocean tropical boundary layer, which incorporates t

196 ary productivity, often dominate coastal and open-ocean upwelling zones.

197 er end of estimated fluxes are comparable to open ocean values, but higher end of estimates are two o

198 egion near the ridge is 10 times larger than open-ocean values.

199 he 'Belgica' trough, which today routes warm open-ocean water back to the ice front to reinforce dyna

200 tions of lambdaDOC/lambdaI representative of open ocean waters (0.5-1).

201 tor to the oceanic dry deposition of O3 over open ocean waters and has also recently been shown to pr

202 a physico-chemical gradient from coastal to open ocean waters in the Northeastern Pacific Ocean.

203 se communities inhabit range from coastal to open ocean waters, how the biological dynamics vary betw

204 edict the impact of Fe-containing dusts into open ocean waters.

205 ive to autotrophic nutrition in oligotrophic open ocean waters.

206 In open-ocean waters, AQY(330) generally ranged between 1 a

207 rasinophyte contributions in mesotrophic and open-ocean waters.

208 They decreased sharply toward the open oceans where they remained relatively stable.

209 North Sea and much higher than several other open oceans worldwide.