ライフサイエンスコーパス: open ocean

1 gic thaumarchaeon CN25, originating from the open ocean.

2 for understanding archaeal adaptation to the open ocean.

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

4 oorganisms occupying surface seawater in the open ocean.

5 cumulation of floating plastic debris in the open ocean.

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

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

8 mical events and biological responses in the open ocean.

9 and modeling polarization camouflage for the open ocean.

10 vigation towards settlement habitat from the open ocean.

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

12 their goal before reorienting, often in the open ocean.

13 gnificant source of bioavailable iron in the open ocean.

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

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

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

17 eutrophication and nitrogen pollution of the open ocean.

18 n many aquatic environments particularly the open ocean.

19 nd/or rapidly degraded before it reaches the open ocean.

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

21 d ocean surface elevations observed over the open ocean.

22 1.7 x 10(30) cells/yr and is highest in the open ocean.

23 representatives of this phylum occur in the open ocean.

24 e most important source of fixed N(2) in the open ocean.

25 e greater remineralization of this OC in the open ocean.

26 hot springs and deserts to glaciers and the open ocean.

27 epods may shape microbial communities in the open ocean.

28 processes of iceberg degradation towards the open ocean.

29 dification in coastal waters compared to the open ocean.

30 of magnitude greater than those observed in open ocean.

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

32 across strong thermal gradients found in the open ocean.

33 tion and microbial community dynamics in the open ocean.

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

35 se dynamic microhabitats in the oligotrophic open ocean.

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

37 but considerably less so in the oligotrophic open ocean.

38 nal coastal location and those picked in the open ocean.

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

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

41 system stability across vast expanses of the open ocean.

42 , where PFAAs are predicted to accumulate in open oceans.

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

44 on rates at ammonium concentrations found in open oceans.

45 he most impactful planktonic predator in the open oceans.

46 appears common among estuaries, coasts, and open oceans.

47 nt contributors to primary production in the open oceans.

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

49 s that, in contrast to the uniform trends of open-ocean acidification (-0.0004 to -0.0026 pH units yr

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

51 lic acid showed higher concentrations in the open ocean air.

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

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

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

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

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

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

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

59 xide (CO(2)) and exporting carbon (C) to the open ocean and sediments.

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

61 +/- 2700 Mg a(-1)), of which 28% reaches the open ocean and the rest is deposited to ocean margin sed

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

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

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

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

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

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

68 cant control on biogeochemical fluxes in the open ocean, and eddies may trap distinctive plankton com

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

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

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

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

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

74 olved record of sea-salt sodium (a proxy for open-ocean area) and non-sea salt calcium (a proxy for c

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

76 ebrate species in the world's coastal and/or open ocean areas.

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

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

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

80 rom human sources away from the coast to the open ocean before eutrophication develops.

81 but also are abundant and widespread in the open ocean, benefiting from a previously overlooked func

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

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

84 ort pathway for land-derived plastics to the open ocean but are relatively understudied compared to c

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

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

87 a turtles, for an ability to reorient in the open ocean, but only at a crude level.

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

89 turtles use a true navigation system in the open ocean, but their map sense is coarse scale.

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

91 ecies with planktonic dispersal, invasion of open ocean coastlines is impaired by the physical advers

92 orical sea-level-driven coastal recession on open ocean coasts is often outpaced by wave-driven chang

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

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

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

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

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

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

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

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

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

102 by the rim current forced by the basin-scale open-ocean convection over the subpolar North Atlantic.

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

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

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

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

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

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

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

110 ing through the shutdown of the Labrador Sea open-ocean deep convection, our results reveal a differe

111 e, i.e., a strengthening of the Labrador Sea open-ocean deep convection, which is not a cause of the

112 er Weddell Polynya associated with intensive open-ocean deep convection.

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

114 nd its subsequent impact on the Labrador Sea open-ocean deep convection.

115 Broadly ranging nearshore and open-ocean delphinids are likely reservoir populations t

116 sed geography likely limits the nearshore or open-ocean delphinids that carry DMV from interacting wi

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

118 t behavior of a demersal fish species in the open ocean, despite our study occurring in deeper water

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

120 n, do not reflect the composition of ancient open-ocean DIC.

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

122 rface DOM from Southern California (USA) and open-ocean DOM from the central North Pacific (Hawaii),

123 However, not many studies focus on the open ocean due to logistical restraints.

124 yi blooms and in samples collected during an open-ocean E. huxleyi bloom, indicating that resistant c

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

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

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

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

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

130 In open ocean ecosystems, competition for low availability

131 ktonic organisms underpin the functioning of open ocean ecosystems.

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

133 al impacts of future anthropogenic change on open ocean ecosystems.

134 lability to predator resource utilization in open-ocean ecosystems.

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

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

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

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

139 t water management is now transitioning from open ocean exchange to a ballast water performance stand

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

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

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

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

144 can be put to complex uses - navigating the open oceans, finding prey, and coordinating herds or col

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

146 Open-ocean fish species exhibited camouflage that was su

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

148 nds of kilometers from reproductive sites to open ocean foraging areas (Figure 1A), yet return within

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

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

151 In the open ocean genetically diverse clades of the unicellular

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

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

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

155 we explore the morphology and behavior of an open-ocean Halobates germanus and a related coastal spec

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

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

158 Bacteria living in the oligotrophic open ocean have various ways to survive under the pressu

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

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

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

162 plankton species originate and evolve in the open ocean, in the absence of apparent geographic barrie

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

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

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

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

167 er pCO(2) in the northwest and southeast GoM open ocean is increasing (1.63 +/- 0.63 uatm year(-1) an

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

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

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

171 sulfonates support growth requirements of an open-ocean isolate of the SAR11 clade, the most abundant

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

173 tion (SIO Pier; San Diego) and UCYN-A3 in an open ocean location (Station ALOHA; Hawaii).

174 )(7)(,)(8)(,)(9) However, cyclone impacts on open ocean marine life remain poorly understood.

175 anthropogenic climate changes are affecting open-ocean marine ecosystems from phytoplankton to top p

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

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

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

179 s Arctic sea ice diminishes, the exposure of open ocean may increase aerosolization rates of marine b

180 , Al, Fe, Ti) far exceed global riverine and open ocean mean values and highlight the importance of s

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

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

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

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

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

186 Here we combine SAR and AIS for large-scale open ocean monitoring, developing methods to match vesse

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

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

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

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

191 This unique dataset provides four seasons of open-ocean observations of wind speed, sea surface tempe

192 ytoplankton bloom spanning 9000 km(2) in the open ocean of the eastern Weddell Gyre.

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

194 constraints on microbial nitrogen cycling in open ocean oligotrophic sediments from seafloor to basem

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

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

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

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

199 -22% of the aerosol PM(1) mass originated in open ocean (OO) and sea ice (SI) regions, respectively.

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

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

202 In the open ocean, our models reveal a significant relationship

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

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

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

206 tion into Earth System Models that represent open ocean pelagic CaCO(3) production and deep-sea prese

207 on variability when modeling the response of open ocean pelagic ecosystems under future climate chang

208 in the biological iron cycle cascade through open ocean pelagic ecosystems, from plankton to fish, af

209 d with their differential use of coastal and open ocean pelagic ecosystems.

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

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

212 e first to confirm a significant increase in open ocean plastics in recent decades.

213 An open-ocean polynya is a large ice-free area surrounded b

214 the GOA is faster than that reported for the open ocean possibly due to higher particle scavenging an

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

216 n, despite their significant contribution to open ocean primary production and other biogeochemical p

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

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

219 organisms is still poorly understood in the open ocean realm.

220 the homogenous W isotope composition of the open ocean (refined d(186/184)W of +0.543 0.046 %).

221 acterial diazotrophs commonly found in other open ocean regions.

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

223 and ultraoligotrophic conditions typical of open ocean regions.

224 ected to intensify the oligotrophic state of open-ocean regions that are far from land-based nutrient

225 patterns of fragile gelatinous fauna in the open ocean remain scarcely documented.

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

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

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

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

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

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

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

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

234 interval, sharks virtually disappeared from open-ocean sediments, declining in abundance by >90% and

235 are the dominant source of cyclized GDGTs in open ocean settings, addressing a major source of uncert

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

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

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

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

240 correlates differ between shallow marine and open-ocean settings.

241 overies of persistent coastal species in the open ocean shift our understanding of biogeographic barr

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

243 pical planktic foraminifer diversity at this open-ocean site during the PETM.

244 d daily production of HCN-sensitive CO at an open-ocean site near Bermuda.

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

246 h electroactive humic substances at multiple open ocean sites, with the ratio of iron to humics incre

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

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

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

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

251 The four open ocean stations in the Indian Ocean had similar comm

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

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

254 of freshwater from the Arctic Ocean into the open ocean such that the freshwater input has a limited

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

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

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

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

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

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

261 Across coastal and open ocean systems, the biomass of autotrophs scales non

262 rogen fixation estimates for terrestrial and open ocean systems, yet other aquatic systems in between

263 s on material cycles over broad areas of the open ocean than previously considered.

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

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

266 ct species) have succeeded at colonizing the open ocean - the largest biome on Earth.

267 contrasting environments: the Canada Basin (open ocean), the Mackenzie Trough (river-influenced), th

268 In the open ocean, the AR generates prominent changes of mixed

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

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

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

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

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

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

275 From shallow waters to the deep sea, the open ocean to rivers and lakes, numerous terrestrial and

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

277 waters of coastal seas, the Great Lakes, and open oceans to examine temporal and geospatial trends.

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

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

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

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

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

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

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

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

286 , reaching remarkably high concentrations in open ocean waters (1200 km offshore of the American Coas

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

288 mparison with freshwaters, Hg methylation in open ocean waters appears less restricted to anoxic envi

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

290 our findings unveil the UCYN-A3 symbiosis in open ocean waters suggesting that the different UCYN-A s

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

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

293 ive to autotrophic nutrition in oligotrophic open ocean waters.

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

295 rasinophyte contributions in mesotrophic and open-ocean waters.

296 tween land, freshwater environments, and the open ocean where plastic debris accumulates.

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

298 Here, we show that compared with open oceans, where the annual RI counts do not show sign

299 soil environments to the abyssal zone of the open ocean with important implications for ecosystem fun

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