ライフサイエンスコーパス: Pacific Ocean

1 anian Gateway, which connects the Indian and Pacific oceans).

2 n carcharias and squids in the eastern North Pacific Ocean.

3 ish that feed at ~500-m depth in the central Pacific Ocean.

4 e marine ligand pool in the eastern tropical Pacific Ocean.

5 sment of the effects of lake drainage on the Pacific Ocean.

6 from a range of depths in the eastern North Pacific Ocean.

7 i Nuclear Power Plant (FDNPP) and across the Pacific Ocean.

8 olite in a diatom bloom in the eastern North Pacific Ocean.

9 housand kilometres westward across the South Pacific Ocean.

10 tal to open ocean waters in the Northeastern Pacific Ocean.

11 several, distinct Fe sources to the central Pacific Ocean.

12 with low iron content collected in the North Pacific Ocean.

13 o the day/night cycle across the subtropical Pacific Ocean.

14 many marine mammal species in the Northeast Pacific Ocean.

15 both hemispheres of the mid-latitude western Pacific Ocean.

16 m the 1980s to present time in the northeast Pacific Ocean.

17 ty following thermonuclear bomb tests in the Pacific Ocean.

18 fish from coral reef communities across the Pacific Ocean.

19 ng material from Fukushima Prefecture to the Pacific Ocean.

20 ecently found near hydrothermal vents in the Pacific Ocean.

21 ast from Asia across the vast expanse of the Pacific Ocean.

22 across a meridional transect in the central Pacific Ocean.

23 a cruise along a latitudinal transect in the Pacific Ocean.

24 ansion of Humboldt squid in the northeastern Pacific Ocean.

25 f DOC at an oligotrophic site in the central Pacific Ocean.

26 y of mantle upwelling beneath Africa and the Pacific Ocean.

27 on earth are U.S. National Monuments in the Pacific Ocean.

28 ears from a depth transect in the equatorial Pacific Ocean.

29 conserve bigeye tuna in the Western Central Pacific Ocean.

30 agenomes, including new metagenomes from the Pacific Ocean.

31 s) in highly migratory marine species in the Pacific Ocean.

32 erived radionuclides across the entire North Pacific Ocean.

33 i-ichi nuclear power plants to the Northwest Pacific Ocean.

34 usta symbiont and the first from outside the Pacific Ocean.

35 no and Endeavour Segment in the northeastern Pacific Ocean.

36 ding a 39-day controlled experiment over the Pacific Ocean.

37 m isolated from surface coastal water of the Pacific Ocean.

38 nitrate-poor coastal waters of the Northeast Pacific Ocean.

39 ish species distributed throughout the North Pacific Ocean.

40 long an 8000-kilometer transect in the South Pacific Ocean.

41 ic level prey sampled from the central North Pacific Ocean.

42 is the sediment at a depth of 1050 m in the Pacific Ocean.

43 ioluminescent Vibrio fischeri from the North Pacific Ocean.

44 ial assemblage collected in the oligotrophic Pacific Ocean.

45 sites spanning the breadth of the equatorial Pacific Ocean.

46 ation of large reefs unique to the Northeast Pacific Ocean.

47 urbation responses in the warm waters of the Pacific Ocean.

48 al structure and circulation of the tropical Pacific Ocean.

49 amination in white sharks from the Northeast Pacific Ocean.

50 rs and minor impacts on the ecosystem in the Pacific Ocean.

51 a relatively narrow corridor in the central Pacific Ocean.

52 ly to be an important Fe source to the North Pacific Ocean.

53 ur in deeply buried sediments of the eastern Pacific Ocean.

54 annual insolation in the eastern equatorial Pacific Ocean.

55 c Rise and the Blanco Ridge in the northeast Pacific Ocean.

56 cal stepping-stones for dispersal across the Pacific Ocean.

57 test in the Arctic and smallest in the South Pacific Ocean.

58 oactivity tracer plume through the northeast Pacific Ocean.

59 multiple wood falls in the deep ( 1600 m) NE Pacific Ocean.

60 Caledonia is a French territory in the South Pacific Ocean.

61 iously reported (129)I concentrations in the Pacific Ocean.

62 ea corals from the low-latitude Atlantic and Pacific Oceans.

63 n to susceptible species in the Atlantic and Pacific Oceans.

64 ss refugia for reef corals in the Indian and Pacific Oceans.

65 tic shipping routes linking the Atlantic and Pacific Oceans.

66 es to distant regions of the North and South Pacific Oceans.

67 4) at multiple locations in the Atlantic and Pacific Oceans.

68 d bipolar asymmetry between the Atlantic and Pacific Oceans.

69 different deep-sea areas of the Atlantic and Pacific oceans.

70 ical crossroads between the Arctic and North Pacific Oceans.

71 trace-metal concentrations across the North Pacific Ocean (158 degrees W from 25 degrees to 42 degre

72 e plankton net data collected in the eastern Pacific Ocean (17.4 degrees S to 61.0 degrees N; 85.0 to

73 mperature, salinity, and productivity in the Pacific Ocean (20 degrees N-15 degrees S).

74 en reported from cod in the Atlantic [2] and Pacific Oceans [3].

75 which are centred in the equatorial central Pacific Ocean(7-9).

76 reduced zonal gradient in the tropical Indo-Pacific Ocean, a change consistent with subsurface tempe

77 ar (DFG) is abundant across the remote North Pacific Ocean, accumulating in convergence zones that co

78 In the Pacific Ocean, air and ocean temperatures, atmospheric c

79 during two song revolutions across the South Pacific Ocean, allowing fine-scale analysis of compositi

80 Oscillation (ENSO) events in the equatorial Pacific Ocean alter precipitation across the tropics.

81 stal and oligotrophic regions of the eastern Pacific Ocean, amphibactins were replaced with lower con

82 Using analyses of data from the equatorial Pacific Ocean and Arabian Sea, we show that the relative

83 many wild Pacific salmon stocks in the North Pacific Ocean and Bering Sea, apparently through bottom-

84 coral holobiont and its ecosystem across the Pacific Ocean and for various oceanographically distinct

85 he area from the western Great Plains to the Pacific Ocean and from the Oregon border to southern Mex

86 r salinities are low in the western tropical Pacific Ocean and increase towards the eastern part of t

87 vealed that the Fe-Mn crust samples from the Pacific Ocean and Indian Ocean were dominated by low coe

88 vironments such as the Southern Ocean, North Pacific Ocean and North Atlantic Ocean.

89 with dry climatic conditions (Playa Grande, Pacific Ocean and Sandy Point, Caribbean Sea), but the e

90 Here, we survey 152 tide gauges in the Pacific Ocean and South China Sea and statistically eval

91 sotopic composition from the Subarctic North Pacific Ocean and the Southern Ocean.

92 climate teleconnections between the tropical Pacific Ocean and the western Antarctic Peninsula streng

93 the two broad low-velocity regions under the Pacific Ocean and under Africa, often referred to as "su

94 ent in Japan spread rapidly across the North Pacific Ocean and was first observed at the westernmost

95 ity of aeolian iron supply to the equatorial Pacific Ocean and, more generally, on the potential cont

96 has been transferred across the Atlantic and Pacific Oceans and between the Northern and Southern hem

97 along transects in the Arctic, Atlantic, and Pacific oceans and during three time series in the North

98 otrophic gyres of the Indian and the western Pacific Oceans and minima at higher latitudes.

99 d viruses from locations in the Atlantic and Pacific Oceans and the Mediterranean Sea.

100 sheets.Warming of the tropical Atlantic and Pacific oceans and the Southern Hemisphere also began at

101 rine air masses in the open ocean (Southeast Pacific Ocean) and coastal sites at northern Alaska (Bar

102 oral reef accumulation occurs in the Western Pacific Ocean, and 80% of coral reef, 63% of carbonate s

103 and diversity in the eastern tropical North Pacific Ocean, and highlight the sensitivity of key bact

104 sition layer (TTL) over the tropical eastern Pacific Ocean, and may reflect a missing inorganic bromi

105 stimates from the Miocene mid-latitude North Pacific Ocean, and show that oceanic warmth persisted th

106 inhabiting the California coast, the central Pacific Ocean, and waters offshore the Antarctica Penins

107 in the North Pacific, Indian, and Southwest Pacific Oceans, and the smallest percentage increase occ

108 pospheric equatorial westerly ducts over the Pacific Ocean are the preferred location for Rossby wave

109 rofiles of the delta18Op in the Atlantic and Pacific Oceans are near a temperature-dependent isotopic

110 Nino, which occur in the equatorial eastern Pacific Ocean, are larger than the maximum cold anomalie

111 urrence of three tuna species in the eastern Pacific Ocean as a model system, we used cardiac gene ex

112 arating marine organisms in the Atlantic and Pacific oceans at ca. 23 and 7 Ma.

113 Interdecadal modes of tropical Pacific ocean-atmosphere circulation have a strong influ

114 ohabiting species from opposite sides of the Pacific Ocean, barnacle abundance had a positive effect

115 f interannual climate variability across the Pacific Ocean basin, with influence on the global climat

116 at correspond to the South Atlantic and Indo-Pacific ocean basins that have similar effective breeder

117 e to and infection with PDV across the North Pacific Ocean beginning in 2003 with a second peak of PD

118 being the primary influence and the tropical Pacific Ocean being the most dominating larger-scale cli

119 rface chlorophyll concentration in the North Pacific Ocean between 2003 and 2010.

120 Located in the Pacific Ocean between Australia and New Zealand, the uni

121 bution of 12 coral species in the Indian and Pacific Oceans, between the latitudes 37 degrees N and 3

122 O) is a climate event that originates in the Pacific Ocean but has wide-ranging consequences for weat

123 d peaks in the ITCZ of both the Atlantic and Pacific Oceans but underestimate its magnitude, likely d

124 nkton fauna along the coast of the Northeast Pacific Ocean, but impacts differed between marine ecosy

125 de and terrigenous dust flux in the tropical Pacific Ocean, but not in global ice volume.

126 ns (in the Mediterranean Sea, the Indian and Pacific Oceans) by a submarine floating seismograph, and

127 helf of Washington State in the Northeastern Pacific Ocean, characterized by a species-rich community

128 obally, with more substantial changes in the Pacific Ocean compared to the Atlantic and Indian Oceans

129 gene cassettes are abundant in the tropical Pacific Ocean, composing up to 28% of T4-like cyanomyoph

130 and a relatively more-rounded pile under the Pacific Ocean, consistent with seismic observations.

131 ial and, surprisingly, the subtropical North Pacific Ocean contribute to the weakened North Pacific H

132 ce the global average, whereas the northwest Pacific Ocean cooled by an amount equal to the global av

133 surface temperatures (SSTs) of the tropical Pacific Ocean could have played important roles in produ

134 Us codominated in iron-depleted areas of the Pacific Ocean, CRD1 and the yet-to-be cultured EnvB were

135 long-standing differences between Indian and Pacific Ocean crust.

136 We compared Pacific Ocean data to lake levels from the interior west

137 O2 observations to confirm that the tropical Pacific Ocean does play an early and important role in m

138 temic approach on coral reefs throughout the Pacific Ocean, drawing an east-west transect from Panama

139 st) overturning of air across the equatorial Pacific Ocean--driven by convection to the west and subs

140 rd shift in the intrusion frequency over the Pacific Ocean, due to the climate regime shift in SST pa

141 1-4 degrees C above normal) in the northeast Pacific Ocean during 2015-2016, we documented shifts in

142 arth's hum originates mainly in the northern Pacific Ocean during Northern Hemisphere winter, and in

143 t sea-level pressure gradients over the Indo-Pacific Ocean during solar maxima and the following 1-2

144 fifteenth century in the central and eastern Pacific Ocean, during the seventeenth century in northwe

145 Tropical Pacific Ocean dynamics during the Medieval Climate Anoma

146 hree global carbonate hot spots: the Western Pacific Ocean, Eastern Indian Ocean, and Caribbean Sea.

147 o the PDO, different indicators of northeast Pacific Ocean ecosystem productivity.

148 This tracer requires that all western Pacific Ocean emigrants acquire the (134)Cs signal, a ra

149 nce of Mobula mobular species in the eastern Pacific Ocean (EPO).

150 The total flux of radiocesium into the Pacific Ocean estimated at the outlet station (basin are

151 five stations in the eastern tropical North Pacific Ocean (ETNP), we captured systematic variations

152 rential mortality rates develop in the North Pacific Ocean for reasons unrelated to dam passage.

153 rannual climate fluctuations in the tropical Pacific Ocean for the period 1857 to 2003, using a coupl

154 s opening routes connecting the Atlantic and Pacific Oceans for longer periods each year.

155 , and sea otter species sampled in the North Pacific Ocean from 2001-2016, we investigated the timing

156 medirostris), which is found in the eastern Pacific Ocean from Baja California to the Bering Sea, te

157 ug' inhibits the warm surface water from the Pacific Ocean from flowing southward into the Indian Oce

158 ischarge of radioactivity into the northwest Pacific Ocean from the 2011 Fukushima Dai-ichi nuclear r

159 lastic debris in the eastern North and South Pacific Oceans from more than 2500 plankton net tows con

160 warm temperate latitudes of the Atlantic and Pacific oceans from shallow coastal waters to the open o

161 volcano on the Juan de Fuca Ridge in the NE Pacific Ocean, from 2013 to 2015 at three different vent

162 ea to Indonesia, from the Eastern to Western Pacific Ocean, from the Caribbean to Canary Islands.

163 Methylmercury cycling in the Pacific Ocean has garnered significant attention in rece

164 ium ((90)Sr and (89)Sr) on the western North Pacific Ocean has not been well established, although (9

165 and the adjacent islands of the southwestern Pacific Ocean, has an insect diversity approximately pro

166 ype 36 (ST36) strains that are native to the Pacific Ocean have recently caused multistate outbreaks

167 er Island), a remote island in the southeast Pacific Ocean, have been debated for generations.

168 The persistence of deeply sourced Fe in the Pacific Ocean illustrates that multiple sources contribu

169 ued lead (Pb) contamination of the Northwest Pacific Ocean in 2002 and present the first comprehensiv

170 ls, was confirmed in sea otters in the North Pacific Ocean in 2004, raising the question of whether r

171 the Fukushima nuclear plant incident in the Pacific Ocean in 2011.

172 eveal that shearwaters fly across the entire Pacific Ocean in a figure-eight pattern while traveling

173 Recent drilling in the eastern Pacific Ocean in Hole 1256D reached gabbro within seismi

174 chemical cycle of iodine in the northwestern Pacific Ocean in the future.

175 f increasing deep convective clouds over the Pacific Ocean in winter from long-term satellite cloud m

176 and has been reported from the Atlantic and Pacific oceans in both hemispheres, and the Arabian Sea.

177 he 100- to 300-meter layer of the Indian and Pacific Oceans in the past decade since 2003.

178 by small diazotrophs in various parts of the Pacific Ocean, including the waters off Hawaii where the

179 e temperature contrast across the equatorial Pacific Ocean increased, which might have had a signific

180 imatic effects propagating from the adjacent Pacific Ocean, indexed by the North Pacific Gyre Oscilla

181 ndonesian throughflow (ITF) linking the Indo-Pacific oceans, influencing global ocean circulation, cl

182 eye tuna (BET) landed in the Western Central Pacific Ocean is caught incidentally in the purse seine

183 ecadal sea level variability centered in the Pacific Ocean is closely tied to low frequency variabili

184 ozone distribution over the central-eastern Pacific Ocean is mainly driven by convective activity re

185 er circulation, whereas the influence of the Pacific Ocean is minimal.

186 The equatorial Pacific Ocean is one of the major high-nutrient, low-chl

187 ella species from deep waters of the eastern Pacific Ocean is reported here.

188 veillance of artificial radionuclides in the Pacific Ocean is still required.

189 tudy, regional application over Northwestern Pacific Ocean is taken as an example.

190 e salinity of surface waters in the tropical Pacific Ocean is thought to be controlled by a combinati

191 yse the geochemical record and timing of the Pacific Ocean Large Igneous Provinces and preserved accr

192 duces stratification of the upper equatorial Pacific Ocean, leading to a smaller increase in ENSO var

193 mong the diverse marine mammals in the North Pacific Ocean linked to change in Arctic sea ice extent.

194 In coastal waters of the northeast Pacific Ocean, marine mammals have increased in abundanc

195 increase in tropospheric ozone flux over the Pacific Ocean may affect the radiative processes and cha

196 measurements of [Formula: see text] using a Pacific Ocean meridional transect crossing all major sur

197 strong correlation between eastern tropical Pacific Ocean mixed-layer thickness and both El Nino amp

198 , sea-surface temperatures in the equatorial Pacific Ocean modulate rainfall variability in the outer

199 meters at Station ALOHA in the central North Pacific Ocean near Hawaii.

200 tion over the extensive regions of the North Pacific Ocean (NPO) have led to a detectable increase in

201 hat undergo long migrations across the North Pacific Ocean (NPO), using multiple discrete regions as

202 ecent large-scale warming event in the North Pacific Ocean of unprecedented magnitude and duration al

203 at ~1.5 to 2.5 km below the seafloor in the Pacific Ocean off Japan.

204 nstrain phytoplankton growth in the tropical Pacific Ocean on an unprecedented spatial scale.

205 gest that climate variations in the tropical Pacific Ocean on millennial as well as orbital timescale

206 plankton community composition in the North Pacific Ocean over the past millennium.

207 among 49 islands in the western and central Pacific Ocean over the period 2001-2017.

208 r of Antarctica leads to major reductions in Pacific Ocean overturning and the loss of the modern Nor

209 the outer tropical (10-25 degrees N) central Pacific Ocean, particularly during La-Nina conditions.

210 ake from the atmosphere) of the Atlantic and Pacific oceans, particularly with regard to a central bu

211 tuna and other top-level predators from the Pacific Ocean pelagic ecosystem since 1950, leading to c

212 Nano CT-scans of selected equatorial Pacific Ocean planktonic foraminifera, have revealed tha

213 y of four hydrogenetic Fe-Mn crusts from the Pacific Ocean (PO-01), South China Sea (SCS-01, SCS-02)

214 and its ontogeny in a highly migratory North Pacific Ocean predator, the northern fur seal (Callorhin

215 ncomitant with the abnormal warming over the Pacific Ocean, prevalently known as "El Nino".

216 p waters of the South Atlantic, Southern and Pacific oceans, probably as a result of the incorporatio

217 killer whale population of the northeastern Pacific Ocean provides a data-rich case to explore anthr

218 f the Tonga subduction zone in the southwest Pacific Ocean provides evidence suggesting significant m

219 rom several different sources in the eastern Pacific Ocean ranging between the Equator and Chilean Pa

220 refugia, and seven areas were identified as Pacific Ocean refugia for reef corals under climate chan

221 in the Hawaiian-Emperor hotspot track in the Pacific Ocean remains enigmatic.

222 eating anomaly in the eastern Indian/western Pacific Ocean, representing the record positive precipit

223 ing mixed-layer waters from the northeastern Pacific Ocean resulted in increased proportions of diato

224 ployed 4,306 tags on 23 species in the North Pacific Ocean, resulting in a tracking data set of unpre

225 ed heterotrophic unicellular eukaryotes from Pacific Ocean samples.

226 strumental record implicates both Indian and Pacific ocean sea surface temperatures (SSTs) as possibl

227 cted to decrease SIE in the Indian Ocean and Pacific Ocean sectors.

228 tofossils were chemically extracted from two Pacific Ocean sediment drill cores.

229 of individual trichomes sampled in the South Pacific Ocean, showed significant (13)C-enrichments afte

230 nthaster starfish, across the tropical north Pacific Ocean since 1980.

231 Here we present results from two Pacific Ocean sites, margin and open ocean, both of whic

232 s consistent with the recent findings in the Pacific Ocean, Southern Ocean, and Mediterranean Sea.

233 tion was observed between the Indian and the Pacific Ocean specimens (F(ST) = 0.145***).

234 Prochlorococcus isolate from the equatorial Pacific Ocean (strain MIT9215) through a series of growt

235 cid and metal concentrations in northeastern Pacific Ocean stratocumulus cloudwater samples collected

236 stress-tolerant "zooxanthella" from the Indo-Pacific Ocean, Symbiodinium trenchii, has rapidly spread

237 GSWS involved extensive changes to the Indo-Pacific ocean teleconnection system, characterized by su

238 re conditions that is influenced by tropical Pacific Ocean temperatures through the Pacific-North Ame

239 ut the observed SSTs in the tropical eastern Pacific Ocean (TEP) are applied for 1871-2012.

240 Earth's lower mantle beneath Africa and the Pacific Ocean that are not easily explained by temperatu

241 gy to isolate a cyanophage from the tropical Pacific Ocean that carries a PSI gene cassette with seve

242 istent evidence for a poorly ventilated deep Pacific Ocean that could have released its radiocarbon-d

243 ygen isotopic compositions from the tropical Pacific Ocean that cover the Eocene/Oligocene boundary.

244 of neodymium isotopes from two cores in the Pacific Ocean that indicate a shift in deep-water produc

245 the upper-ocean circulation in the tropical Pacific Ocean that may have been essential for maintaini

246 n stretching from East Africa to the western Pacific Ocean that persisted for 2 mo.

247 ions of key physical variables for the North Pacific Ocean that seem to show these behaviours are not

248 profiles from airborne measurements over the Pacific Ocean that show significant IO up to 9.5 km alti

249 ked by a La Nina-like decadal cooling in the Pacific Ocean that subsequently generated an increase in

250 nomes from four biogeographic regions in the Pacific Ocean that vary by season, depth, and proximity

251 e Izu-Bonin-Mariana subduction zone forearc (Pacific Ocean) that contain complex organic matter and n

252 resolution simulation of the realistic North Pacific Ocean, that ocean eddies are instead sustained b

253 c overturning circulation above the tropical Pacific Ocean (the Walker circulation) over the twentiet

254 he northern subtropical and eastern tropical Pacific Ocean, the Arabian Sea, and the Bay of Bengal.

255 that the major subtropical WBC of the South Pacific Ocean, the East Australian Current (EAC), transp

256 In the Pacific Ocean, the identification of such a mode has led

257 he silicate and borate depth profiles in the Pacific Ocean; the silicate results show an excellent ma

258 ein-like substances in the open Atlantic and Pacific oceans, though often significantly aged, compris

259 an receives warm, saline water from the Indo-Pacific Ocean through Agulhas leakage around the souther

260 e junction region, in the eastern equatorial Pacific Ocean, thus consists of two counter-rotating mic

261 imal impacts from closing large parts of the Pacific Ocean to fishing.

262 deposition at 10 sites from the coast of the Pacific Ocean to Great Basin National Park.

263 ensitive uranium from the central equatorial Pacific Ocean to identify intervals associated with resp

264 ears will soon reduce the BET biomass in the Pacific Ocean to less than that capable of producing max

265 emporal bioenergetics model of the Northeast Pacific Ocean to quantify how predation by three species

266 three sediment cores in the western tropical Pacific Ocean to reconstruct Holocene sea surface temper

267 m marine sediments in the eastern equatorial Pacific Ocean to reconstruct sea surface temperatures an

268 sites spanning the breadth of the equatorial Pacific Ocean to test the dust fertilization hypothesis.

269 Pacific bluefin tuna (PBFT) that crossed the Pacific Ocean to the California Current Large Marine Eco

270 traveled thousands of kilometers across the Pacific Ocean to the shores of North America and Hawai'i

271 and between populations in the Atlantic and Pacific Oceans, to begin to understand the selective pre

272 rface blooms of Trichodesmium from the South Pacific Ocean triggered PCD under Fe-limitation and high

273 es, the world's largest suboxic zone, in the Pacific Ocean, varies in size by a factor of 2.

274 ent millennial-scale episodes of reorganized Pacific Ocean ventilation synchronous with rapid Cordill

275 Application to 32 viromes from the Pacific Ocean Virome dataset identified clusters of samp

276 In a single experiment, we screened 10(7) Pacific Ocean viruses against a single strain of Synecho

277 th century, the North Atlantic and northeast Pacific oceans warmed by twice the global average, where

278 Two distinctly different forms of tropical Pacific Ocean warming are shown to have substantially di

279 at cooling in the top 100-meter layer of the Pacific Ocean was mainly compensated for by warming in t

280 ence between populations in the Atlantic and Pacific Oceans was more common than subdivisions among p

281 The warmth of the Indian and west Pacific oceans was unprecedented and consistent with gre

282 ure of glacial carbon storage and equatorial Pacific Ocean watermass structure.

283 core, n = 1000) from the Western and Central Pacific Ocean (WCPO).

284 iron enrichment experiment conducted in the Pacific Ocean, we propose that iron-limited cells in the

285 ssuming Pb isotope compositions in the North Pacific Ocean were homogeneous prior to large-scale 20th

286 most mantle (D'' region) beneath the central Pacific Ocean were inferred from the observation of a ra

287 The individual impact of North Atlantic and Pacific Ocean Western Boundary Currents (OWBCs) on the t

288 Pacific Ocean western boundary currents and the interlin

289 n tuna sampled at three locations across the Pacific Ocean (western, central, and eastern) via analys

290 ange, with the highest rates in the tropical Pacific Ocean where many of the world's low-lying atolls

291 nts from the abyssal southeast and southwest Pacific Ocean, where dFe of 1.0-1.5 nmol/kg near 2,000 m

292 n path exists in the northwest corner of the Pacific Ocean, where enhanced vertical mixing, perhaps d

293 et the cobalt distribution in the equatorial Pacific Ocean, where surface concentrations are among th

294 t nitrogen fixation rates are highest in the Pacific Ocean, where water column denitrification rates

295 ear, all birds from Kerguelen migrate to the Pacific Ocean, whereas most from Crozet are sedentary.

296 n compared with the Sargasso Sea and Eastern Pacific Ocean, which may be related to the nitrogen avai

297 pical convection over the Indian and western Pacific Oceans, which resulted in a wave-3 circulation p

298 fragments cloned from the subtropical North Pacific Ocean with <1% sequence divergence even in inter

299 eamounts are the only seamount trails in the Pacific Ocean with a sharp 60 degrees bend, similar to t

300 lantic Ocean by snoek from the South-Eastern Pacific Ocean, with a potential impact on the landings o