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1 the distal supply of iron to the equatorial Pacific Ocean).
2 (they could take tens of years to cross the Pacific Ocean).
3 anian Gateway, which connects the Indian and Pacific oceans).
4 oactivity tracer plume through the northeast Pacific Ocean.
5 both hemispheres of the mid-latitude western Pacific Ocean.
6 m the 1980s to present time in the northeast Pacific Ocean.
7 ty following thermonuclear bomb tests in the Pacific Ocean.
8 fish from coral reef communities across the Pacific Ocean.
9 ng material from Fukushima Prefecture to the Pacific Ocean.
10 ecently found near hydrothermal vents in the Pacific Ocean.
11 ast from Asia across the vast expanse of the Pacific Ocean.
12 across a meridional transect in the central Pacific Ocean.
13 a cruise along a latitudinal transect in the Pacific Ocean.
14 ansion of Humboldt squid in the northeastern Pacific Ocean.
15 f DOC at an oligotrophic site in the central Pacific Ocean.
16 y of mantle upwelling beneath Africa and the Pacific Ocean.
17 ears from a depth transect in the equatorial Pacific Ocean.
18 conserve bigeye tuna in the Western Central Pacific Ocean.
19 agenomes, including new metagenomes from the Pacific Ocean.
20 s) in highly migratory marine species in the Pacific Ocean.
21 erived radionuclides across the entire North Pacific Ocean.
22 i-ichi nuclear power plants to the Northwest Pacific Ocean.
23 usta symbiont and the first from outside the Pacific Ocean.
24 no and Endeavour Segment in the northeastern Pacific Ocean.
25 m isolated from surface coastal water of the Pacific Ocean.
26 nitrate-poor coastal waters of the Northeast Pacific Ocean.
27 ish species distributed throughout the North Pacific Ocean.
28 long an 8000-kilometer transect in the South Pacific Ocean.
29 ic level prey sampled from the central North Pacific Ocean.
30 is the sediment at a depth of 1050 m in the Pacific Ocean.
31 ioluminescent Vibrio fischeri from the North Pacific Ocean.
32 ial assemblage collected in the oligotrophic Pacific Ocean.
33 sites spanning the breadth of the equatorial Pacific Ocean.
34 iously reported (129)I concentrations in the Pacific Ocean.
35 urbation responses in the warm waters of the Pacific Ocean.
36 al structure and circulation of the tropical Pacific Ocean.
37 rs and minor impacts on the ecosystem in the Pacific Ocean.
38 a relatively narrow corridor in the central Pacific Ocean.
39 multiple wood falls in the deep ( 1600 m) NE Pacific Ocean.
40 ur in deeply buried sediments of the eastern Pacific Ocean.
41 annual insolation in the eastern equatorial Pacific Ocean.
42 confined to a few islets in the northwestern Pacific Ocean.
43 udies of oceanic islands have focused on the Pacific Ocean.
44 ese small islands over a long stretch of the Pacific Ocean.
45 e of the decadal variability observed in the Pacific Ocean.
46 mal vents located on the ridge crests in the Pacific ocean.
47 complex in Australia and the islands of the Pacific Ocean.
48 r (TOMS) data between the high Andes and the Pacific Ocean.
49 e marine ligand pool in the eastern tropical Pacific Ocean.
50 sment of the effects of lake drainage on the Pacific Ocean.
51 from a range of depths in the eastern North Pacific Ocean.
52 i Nuclear Power Plant (FDNPP) and across the Pacific Ocean.
53 olite in a diatom bloom in the eastern North Pacific Ocean.
54 housand kilometres westward across the South Pacific Ocean.
55 tal to open ocean waters in the Northeastern Pacific Ocean.
56 several, distinct Fe sources to the central Pacific Ocean.
57 with low iron content collected in the North Pacific Ocean.
58 o the day/night cycle across the subtropical Pacific Ocean.
59 tic shipping routes linking the Atlantic and Pacific Oceans.
60 es to distant regions of the North and South Pacific Oceans.
61 4) at multiple locations in the Atlantic and Pacific Oceans.
62 d bipolar asymmetry between the Atlantic and Pacific Oceans.
63 temperatures, especially over the Indian and Pacific Oceans.
64 ea corals from the low-latitude Atlantic and Pacific Oceans.
65 n to susceptible species in the Atlantic and Pacific Oceans.
66 ss refugia for reef corals in the Indian and Pacific Oceans.
67 e plankton net data collected in the eastern Pacific Ocean (17.4 degrees S to 61.0 degrees N; 85.0 to
71 reduced zonal gradient in the tropical Indo-Pacific Ocean, a change consistent with subsurface tempe
74 tions between the Caribbean Sea and tropical Pacific Ocean about 3.5 million years ago, began to stim
76 during two song revolutions across the South Pacific Ocean, allowing fine-scale analysis of compositi
77 stal and oligotrophic regions of the eastern Pacific Ocean, amphibactins were replaced with lower con
78 eneath regions of upwellings centered on the Pacific Ocean and Africa that are characterized by slow
79 Using analyses of data from the equatorial Pacific Ocean and Arabian Sea, we show that the relative
80 many wild Pacific salmon stocks in the North Pacific Ocean and Bering Sea, apparently through bottom-
81 he area from the western Great Plains to the Pacific Ocean and from the Oregon border to southern Mex
82 ad in tropical surface waters of the eastern Pacific Ocean and in temperate coastal waters of the nor
83 r salinities are low in the western tropical Pacific Ocean and increase towards the eastern part of t
84 vealed that the Fe-Mn crust samples from the Pacific Ocean and Indian Ocean were dominated by low coe
86 with dry climatic conditions (Playa Grande, Pacific Ocean and Sandy Point, Caribbean Sea), but the e
88 apsed over large areas of the northern North Pacific Ocean and southern Bering Sea during the last se
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 sequences were widely distributed across the Pacific Ocean and were shared between recognized species
96 ity of aeolian iron supply to the equatorial Pacific Ocean and, more generally, on the potential cont
99 sheets.Warming of the tropical Atlantic and Pacific oceans and the Southern Hemisphere also began at
100 rine air masses in the open ocean (Southeast Pacific Ocean) and coastal sites at northern Alaska (Bar
101 and diversity in the eastern tropical North Pacific Ocean, and highlight the sensitivity of key bact
102 sition layer (TTL) over the tropical eastern Pacific Ocean, and may reflect a missing inorganic bromi
103 stimates from the Miocene mid-latitude North Pacific Ocean, and show that oceanic warmth persisted th
104 inhabiting the California coast, the central Pacific Ocean, and waters offshore the Antarctica Penins
105 cal profiles (0-250 m) from the Atlantic and Pacific Oceans, and in discrete (monthly) time series (O
106 in the North Pacific, Indian, and Southwest Pacific Oceans, and the smallest percentage increase occ
109 l vents on mid-ocean ridges of the northeast Pacific Ocean are known to respond to seismic disturbanc
110 pospheric equatorial westerly ducts over the Pacific Ocean are the preferred location for Rossby wave
111 rofiles of the delta18Op in the Atlantic and Pacific Oceans are near a temperature-dependent isotopic
112 urrence of three tuna species in the eastern Pacific Ocean as a model system, we used cardiac gene ex
114 in the outgassing of CO2 from the equatorial Pacific Ocean-at present the largest oceanic source of c
116 ical findings shed light on how the tropical Pacific ocean-atmosphere system may respond to exogenous
117 nity variations imply shifts in the tropical Pacific ocean/atmosphere system analogous to modern El N
118 ohabiting species from opposite sides of the Pacific Ocean, barnacle abundance had a positive effect
119 f interannual climate variability across the Pacific Ocean basin, with influence on the global climat
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
125 ns (in the Mediterranean Sea, the Indian and Pacific Oceans) by a submarine floating seismograph, and
126 helf of Washington State in the Northeastern Pacific Ocean, characterized by a species-rich community
127 gene cassettes are abundant in the tropical Pacific Ocean, composing up to 28% of T4-like cyanomyoph
128 and a relatively more-rounded pile under the Pacific Ocean, consistent with seismic observations.
129 surface temperatures (SSTs) of the tropical Pacific Ocean could have played important roles in produ
130 Us codominated in iron-depleted areas of the Pacific Ocean, CRD1 and the yet-to-be cultured EnvB were
133 O2 observations to confirm that the tropical Pacific Ocean does play an early and important role in m
134 st) overturning of air across the equatorial Pacific Ocean--driven by convection to the west and subs
135 rd shift in the intrusion frequency over the Pacific Ocean, due to the climate regime shift in SST pa
136 1-4 degrees C above normal) in the northeast Pacific Ocean during 2015-2016, we documented shifts in
137 arth's hum originates mainly in the northern Pacific Ocean during Northern Hemisphere winter, and in
142 0,000 years, which shows that the equatorial Pacific Ocean exhibits higher-frequency variations than
143 rential mortality rates develop in the North Pacific Ocean for reasons unrelated to dam passage.
144 rannual climate fluctuations in the tropical Pacific Ocean for the period 1857 to 2003, using a coupl
146 medirostris), which is found in the eastern Pacific Ocean from Baja California to the Bering Sea, te
147 ug' inhibits the warm surface water from the Pacific Ocean from flowing southward into the Indian Oce
148 ischarge of radioactivity into the northwest Pacific Ocean from the 2011 Fukushima Dai-ichi nuclear r
149 lastic debris in the eastern North and South Pacific Oceans from more than 2500 plankton net tows con
150 warm temperate latitudes of the Atlantic and Pacific oceans from shallow coastal waters to the open o
151 volcano on the Juan de Fuca Ridge in the NE Pacific Ocean, from 2013 to 2015 at three different vent
152 ea to Indonesia, from the Eastern to Western Pacific Ocean, from the Caribbean to Canary Islands.
153 shelves of the western Atlantic and eastern Pacific Oceans, from the tropics to the Arctic Ocean.
155 ium ((90)Sr and (89)Sr) on the western North Pacific Ocean has not been well established, although (9
156 and the adjacent islands of the southwestern Pacific Ocean, has an insect diversity approximately pro
157 Decadal temperature fluctuations in the Pacific Ocean have a significant effect on marine ecosys
158 ype 36 (ST36) strains that are native to the Pacific Ocean have recently caused multistate outbreaks
160 The persistence of deeply sourced Fe in the Pacific Ocean illustrates that multiple sources contribu
161 ued lead (Pb) contamination of the Northwest Pacific Ocean in 2002 and present the first comprehensiv
163 eveal that shearwaters fly across the entire Pacific Ocean in a figure-eight pattern while traveling
165 pboard air sampling transect made across the Pacific Ocean in July 2000 and are part of an ongoing at
167 f increasing deep convective clouds over the Pacific Ocean in winter from long-term satellite cloud m
168 and has been reported from the Atlantic and Pacific oceans in both hemispheres, and the Arabian Sea.
171 by small diazotrophs in various parts of the Pacific Ocean, including the waters off Hawaii where the
172 e temperature contrast across the equatorial Pacific Ocean increased, which might have had a signific
173 imatic effects propagating from the adjacent Pacific Ocean, indexed by the North Pacific Gyre Oscilla
174 roxies we find evidence for intensified deep Pacific Ocean inflow and ventilation during the glacial
175 10 million m3 x s(-1) of water flow from the Pacific Ocean into the Indian Ocean through the Indonesi
176 eye tuna (BET) landed in the Western Central Pacific Ocean is caught incidentally in the purse seine
177 ecadal sea level variability centered in the Pacific Ocean is closely tied to low frequency variabili
178 ozone distribution over the central-eastern Pacific Ocean is mainly driven by convective activity re
180 ut 60% of the global ocean uptake, while the Pacific Ocean is neutral because of its equatorial sourc
187 e salinity of surface waters in the tropical Pacific Ocean is thought to be controlled by a combinati
188 kelberg seamount chain beneath the northeast Pacific Ocean, is a locus of volcanic activity thought t
189 Africa to southeast Asia and across the many Pacific Ocean island chains is the most likely explanati
190 en isotope marine record in the Atlantic and Pacific Oceans just before the late Pliocene deteriorati
191 yse the geochemical record and timing of the Pacific Ocean Large Igneous Provinces and preserved accr
192 increase in tropospheric ozone flux over the Pacific Ocean may affect the radiative processes and cha
193 , sea-surface temperatures in the equatorial Pacific Ocean modulate rainfall variability in the outer
194 from station ALOHA in the subtropical North Pacific Ocean near Hawaii, and find a significant decrea
196 tion over the extensive regions of the North Pacific Ocean (NPO) have led to a detectable increase in
197 hat undergo long migrations across the North Pacific Ocean (NPO), using multiple discrete regions as
198 ecent large-scale warming event in the North Pacific Ocean of unprecedented magnitude and duration al
201 gest that climate variations in the tropical Pacific Ocean on millennial as well as orbital timescale
202 bility-for example, in the subtropical North Pacific Ocean-our observations suggest that marine nitro
204 r of Antarctica leads to major reductions in Pacific Ocean overturning and the loss of the modern Nor
205 the outer tropical (10-25 degrees N) central Pacific Ocean, particularly during La-Nina conditions.
206 ake from the atmosphere) of the Atlantic and Pacific oceans, particularly with regard to a central bu
207 tuna and other top-level predators from the Pacific Ocean pelagic ecosystem since 1950, leading to c
208 y of four hydrogenetic Fe-Mn crusts from the Pacific Ocean (PO-01), South China Sea (SCS-01, SCS-02)
209 p waters of the South Atlantic, Southern and Pacific oceans, probably as a result of the incorporatio
210 killer whale population of the northeastern Pacific Ocean provides a data-rich case to explore anthr
211 f the Tonga subduction zone in the southwest Pacific Ocean provides evidence suggesting significant m
212 refugia, and seven areas were identified as Pacific Ocean refugia for reef corals under climate chan
215 ing mixed-layer waters from the northeastern Pacific Ocean resulted in increased proportions of diato
216 ployed 4,306 tags on 23 species in the North Pacific Ocean, resulting in a tracking data set of unpre
217 During the 1997-98 El Nino, the equatorial Pacific Ocean retained 0.7 x 10(15) grams of carbon that
218 strumental record implicates both Indian and Pacific ocean sea surface temperatures (SSTs) as possibl
220 of individual trichomes sampled in the South Pacific Ocean, showed significant (13)C-enrichments afte
221 a pH profile for the middle Eocene tropical Pacific Ocean shows that atmospheric pCO2 was probably s
225 s consistent with the recent findings in the Pacific Ocean, Southern Ocean, and Mediterranean Sea.
226 cid and metal concentrations in northeastern Pacific Ocean stratocumulus cloudwater samples collected
227 stress-tolerant "zooxanthella" from the Indo-Pacific Ocean, Symbiodinium trenchii, has rapidly spread
228 re conditions that is influenced by tropical Pacific Ocean temperatures through the Pacific-North Ame
230 on sampled over 7000 kilometers of the South Pacific Ocean that appear indicative of iron-limiting gr
231 Earth's lower mantle beneath Africa and the Pacific Ocean that are not easily explained by temperatu
232 gy to isolate a cyanophage from the tropical Pacific Ocean that carries a PSI gene cassette with seve
233 istent evidence for a poorly ventilated deep Pacific Ocean that could have released its radiocarbon-d
234 ygen isotopic compositions from the tropical Pacific Ocean that cover the Eocene/Oligocene boundary.
235 of neodymium isotopes from two cores in the Pacific Ocean that indicate a shift in deep-water produc
236 the upper-ocean circulation in the tropical Pacific Ocean that may have been essential for maintaini
238 ions of key physical variables for the North Pacific Ocean that seem to show these behaviours are not
239 profiles from airborne measurements over the Pacific Ocean that show significant IO up to 9.5 km alti
240 nomes from four biogeographic regions in the Pacific Ocean that vary by season, depth, and proximity
241 e Izu-Bonin-Mariana subduction zone forearc (Pacific Ocean) that contain complex organic matter and n
242 resolution simulation of the realistic North Pacific Ocean, that ocean eddies are instead sustained b
243 c overturning circulation above the tropical Pacific Ocean (the Walker circulation) over the twentiet
244 he northern subtropical and eastern tropical Pacific Ocean, the Arabian Sea, and the Bay of Bengal.
246 he silicate and borate depth profiles in the Pacific Ocean; the silicate results show an excellent ma
247 ein-like substances in the open Atlantic and Pacific oceans, though often significantly aged, compris
248 an receives warm, saline water from the Indo-Pacific Ocean through Agulhas leakage around the souther
249 e junction region, in the eastern equatorial Pacific Ocean, thus consists of two counter-rotating mic
250 and ocean may limit the SST in the tropical Pacific Ocean to below 305 kelvin even in the absence of
252 ensitive uranium from the central equatorial Pacific Ocean to identify intervals associated with resp
253 ears will soon reduce the BET biomass in the Pacific Ocean to less than that capable of producing max
254 records from Palmyra Island in the tropical Pacific Ocean to provide 30-150-year windows of tropical
255 emporal bioenergetics model of the Northeast Pacific Ocean to quantify how predation by three species
256 three sediment cores in the western tropical Pacific Ocean to reconstruct Holocene sea surface temper
257 m marine sediments in the eastern equatorial Pacific Ocean to reconstruct sea surface temperatures an
258 sites spanning the breadth of the equatorial Pacific Ocean to test the dust fertilization hypothesis.
259 Pacific bluefin tuna (PBFT) that crossed the Pacific Ocean to the California Current Large Marine Eco
260 traveled thousands of kilometers across the Pacific Ocean to the shores of North America and Hawai'i
261 and between populations in the Atlantic and Pacific Oceans, to begin to understand the selective pre
264 In a single experiment, we screened 10(7) Pacific Ocean viruses against a single strain of Synecho
265 Two distinctly different forms of tropical Pacific Ocean warming are shown to have substantially di
266 at cooling in the top 100-meter layer of the Pacific Ocean was mainly compensated for by warming in t
267 ence between populations in the Atlantic and Pacific Oceans was more common than subdivisions among p
270 iron enrichment experiment conducted in the Pacific Ocean, we propose that iron-limited cells in the
271 ssuming Pb isotope compositions in the North Pacific Ocean were homogeneous prior to large-scale 20th
272 most mantle (D'' region) beneath the central Pacific Ocean were inferred from the observation of a ra
274 n tuna sampled at three locations across the Pacific Ocean (western, central, and eastern) via analys
275 ange, with the highest rates in the tropical Pacific Ocean where many of the world's low-lying atolls
276 nts from the abyssal southeast and southwest Pacific Ocean, where dFe of 1.0-1.5 nmol/kg near 2,000 m
277 n path exists in the northwest corner of the Pacific Ocean, where enhanced vertical mixing, perhaps d
278 t nitrogen fixation rates are highest in the Pacific Ocean, where water column denitrification rates
279 ear, all birds from Kerguelen migrate to the Pacific Ocean, whereas most from Crozet are sedentary.
280 n compared with the Sargasso Sea and Eastern Pacific Ocean, which may be related to the nitrogen avai
281 fragments cloned from the subtropical North Pacific Ocean with <1% sequence divergence even in inter
282 eamounts are the only seamount trails in the Pacific Ocean with a sharp 60 degrees bend, similar to t
283 ean currents connecting the western tropical Pacific Ocean with the eastern tropical Pacific Ocean ar
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