ライフサイエンスコーパス: Atlantic Ocean

1 istinct prymnesiophyte partners in the South Atlantic Ocean.

2 raltar and continue their migration into the Atlantic Ocean.

3 of new nutrients in the euphotic zone of the Atlantic Ocean.

4 widespread, peaking at 4.2 mW m(-2) over the Atlantic Ocean.

5 outhern Ocean, North Pacific Ocean and North Atlantic Ocean.

6 mechanisms in two contrasting regions of the Atlantic Ocean.

7 n the mode of overturning circulation in the Atlantic Ocean.

8 0 years) temperature changes in the northern Atlantic Ocean.

9 III) compounds in the western tropical North Atlantic Ocean.

10 ritis linked to shellfish harvested from the Atlantic Ocean.

11 pine Abyssal Plain site in the eastern North Atlantic Ocean.

12 pply on phytoplankton iron status across the Atlantic Ocean.

13 This is similar to observations from the Atlantic Ocean.

14 subpolar gyre (SPG) circulation of the North Atlantic Ocean.

15 nutrient concentrations of the (sub)tropical Atlantic Ocean.

16 trations ([Fe]) along a section of the North Atlantic Ocean.

17 hout the extremely Pi-depleted western North Atlantic Ocean.

18 eature separating the Gulf of Maine from the Atlantic Ocean.

19 but frequency was depressed elsewhere in the Atlantic Ocean.

20 h was forced by AMOC variations in the North Atlantic Ocean.

21 pical gyres and the Equatorial Region of the Atlantic Ocean.

22 ntal shelf, slope, and rise of the northwest Atlantic Ocean.

23 Shanghai, China to Cape Verde in the Central Atlantic Ocean.

24 served sea surface temperatures in the North Atlantic Ocean.

25 er in remote regions of the Indian and South Atlantic Ocean.

26 this time was solely eastward into the North Atlantic Ocean.

27 eridional overturning circulation within the Atlantic Ocean.

28 projections (RCP8.5 scenario) for the North Atlantic Ocean.

29 hy this reservoir has only been found in the Atlantic Ocean.

30 has previously been suggested for the North Atlantic Ocean.

31 alcium carbonate content from the equatorial Atlantic Ocean.

32 er and 1.3 x 10(15) W of heat into the North Atlantic ocean.

33 nd basin-wide environmental gradients in the Atlantic Ocean.

34 st percentage increase occurred in the North Atlantic Ocean.

35 gh krill densities observed in the southwest Atlantic Ocean.

36 leased from 12 rivers flowing into the North Atlantic Ocean.

37 21 to 32% of it to be exported to the North Atlantic Ocean.

38 st decade in the mid- to high-latitude North Atlantic Ocean.

39 de in the multidecadal behavior of the North Atlantic Ocean.

40 n a sediment core from the subtropical North Atlantic Ocean.

41 breed sympatrically at South Georgia, South Atlantic Ocean.

42 and Chain transform faults in the equatorial Atlantic Ocean.

43 ounts of fresh water into the northern North Atlantic Ocean.

44 V methods and was tested on samples from the Atlantic Ocean.

45 cold and fresh water into the northern North Atlantic Ocean.

46 entricity--in the tropical and extratropical Atlantic Ocean.

47 ting the routing of fresh water to the North Atlantic Ocean.

48 mal isolation of the Southern Ocean from the Atlantic Ocean.

49 ra Poisoning is an emerging risk in the east Atlantic Ocean.

50 n overseas French territory in the northwest Atlantic Ocean.

51 o oligotrophic stations in the western North Atlantic Ocean.

52 coast, shelf, and slope of the Northwestern Atlantic Ocean.

53 driven by the transbasin influence from the Atlantic Ocean.

54 with a contemporary range spanning the North Atlantic Ocean.

55 is vital to pelagic ecosystems in the North Atlantic Ocean.

56 c herring populations from both sides of the Atlantic Ocean.

57 via the denitrification pathway in the open Atlantic Ocean.

58 ion of dissolved organic sulfur (DOS) in the Atlantic Ocean.

59 agoes such as the Faroe Islands in the North Atlantic Ocean.

60 mospheric Observatory in the remote tropical Atlantic Ocean.

61 ss properties in the North Pacific and North Atlantic Ocean.

62 9 organizations throughout the western North Atlantic Ocean.

63 collected from 100- to 5,000-m depth in the Atlantic Ocean.

64 irginia (USA) following voyages in the North Atlantic Ocean.

65 by a large and growing anomaly in the South Atlantic Ocean.

66 munities of 68 species were simulated in the Atlantic Ocean.

67 kton across diverse sites from the Northwest Atlantic Ocean.

68 of truly dissolved POPs at two sites in the Atlantic Ocean.

69 colonizing Greenland from both sides of the Atlantic Ocean.

70 east (toward the Tyrrhenian) and toward the Atlantic Ocean.

71 ir entire lifecycle without migrating to the Atlantic Ocean.

72 onsumes 72% of the DOC exported by the whole Atlantic Ocean.

73 malies in the tropical Pacific and the North Atlantic oceans.

74 the variability of the tropical Pacific and Atlantic Oceans.

75 n-atmosphere conditions over the Pacific and Atlantic Oceans.

76 ated to direct advection from the Indian and Atlantic oceans.

77 ctivity in the west Indian and the southwest Atlantic Oceans.

78 cal convective regions over both Pacific and Atlantic oceans.

79 are also present in the tropical Indian and Atlantic Oceans.

80 ation and divergence; (1) the opening of the Atlantic Ocean, (2) the breakup of Gondwana, and (3) the

81 ic to the volcanic island of Sao Tome in the Atlantic Ocean, 280 km west of Gabon.

82 ollected along a latitudinal transect in the Atlantic Ocean (31 degrees N to 38 degrees S).

83 a significant amount of HCB is stored in the Atlantic Ocean (4.8-26% of the global HCB environmental

84 particulate heme b distributions across the Atlantic Ocean (59.9 degrees N to 34.6 degrees S).

85 DOC to the carbon sequestration in the North Atlantic Ocean (62 Tg-C.yr(-1)) is considerable and repr

86 ntrations showed subsurface maxima (tropical Atlantic Ocean -800 m, North Atlantic -500 m).

87 By contrast, the North Atlantic Ocean-a major conduit for atmospheric CO(2) tra

88 exico, a major propagating rift in the South Atlantic Ocean, abyssal hill fabric on slow-spreading ri

89 Our findings suggest that the Atlantic Ocean acts as a key pacemaker for the western P

90 the Mediterranean, but two eels reached the Atlantic Ocean after six months and at distances greater

91 d salt transfer from the Indian Ocean to the Atlantic Ocean (Agulhas leakage) has an important effect

92 iculty of females locating mates in the vast Atlantic Ocean (Allee effect).

93 dicate that the mid-depth North and tropical Atlantic Ocean almost always has lower SigmaCO2 levels t

94 to (15 +/- 12) x 10(6) m3 s(-1) in the North Atlantic Ocean and (21 +/- 6) x 10(6) m3 s(-1) in the So

95 ibuted to a meltwater outflow into the North Atlantic Ocean and a slowdown of North Atlantic Deep Wat

96 pulse, which predominantly entered the North Atlantic Ocean and accounted for about 70 per cent of th

97 content at the surface of the western North Atlantic Ocean and Caribbean Sea from 1986 to 2008.

98 ntifiable PE packaging were collected in the Atlantic Ocean and compared to new PE boxes.

99 o an increase in ocean temperatures over the Atlantic Ocean and elsewhere.

100 oid copepod crustaceans in the eastern North Atlantic Ocean and European shelf seas.

101 aircraft measurement campaign over the North Atlantic Ocean and find evidence for rapid recycling of

102 r rivers that discharge to the western North Atlantic Ocean and find that these rivers are sources of

103 iability and bloom timing over the Northeast Atlantic Ocean and North Sea.

104 ions ([CO3(2-)]) during three cruises in the Atlantic Ocean and one in the Mediterranean Sea were use

105 ation-the strongest oceanic pacemaker of the Atlantic Ocean and perhaps the entire Earth's climate.

106 nditions are found during warm states of the Atlantic Ocean and positive phases of the North Atlantic

107 xpressing nosZ in samples taken from the mid-Atlantic Ocean and Red Sea implying that Trichodesmium c

108 d phytoplankton community composition in the Atlantic Ocean and show that the distribution of diatoms

109 ts of emerging concern to the tropical North Atlantic Ocean and suggest that medium-/long-range conta

110 n of solid-phase extractable DOS in the East Atlantic Ocean and the Atlantic sector of the Southern O

111 water-exchange region between the North Sea-Atlantic Ocean and the Baltic Sea.

112 g and autumn-spawning populations across the Atlantic Ocean and the Baltic Sea.

113 adal variability is a notable feature of the Atlantic Ocean and the climate of the regions it influen

114 The water mass structure of the glacial deep Atlantic Ocean and the mechanism by which it may have se

115 m the closure of marine gateways between the Atlantic Ocean and the Mediterranean Sea, the causes of

116 d mesopelagic waters in both the Pacific and Atlantic oceans and has the unusual property of producin

117 most abundant cephalopods in the Pacific and Atlantic Oceans and is an important prey species for a v

118 sium-137 was deposited mostly in Pacific and Atlantic Oceans and North Pole (80%), whereas the rest i

119 d from two major populations, South Georgia (Atlantic Ocean) and the Prince Edward Islands (Indian Oc

120 n based on seawater measurements made in the Atlantic Ocean, and the resultant fluxes suggest that th

121 (-1)) than those previously reported for the Atlantic Ocean, and which are within the range of the hi

122 Cape Agulhas, which separates the Indian and Atlantic Oceans, and across the Drake Passage between th

123 of (129)I in shallow seawater from the South Atlantic Ocean are presented and discussed.

124 rbon isotope excursion from Maud Rise (South Atlantic Ocean) are controversial, as they seem to indic

125 ses biological productivity in the Subarctic Atlantic Ocean as increasing ocean surface buoyancy supp

126 ginal salmon populations had migrated to the Atlantic Ocean as part of their lifecycle (anadromy), st

127 The North Atlantic ocean/atmosphere environment exhibits pronounce

128 ly anisotropic model of Europe and the North Atlantic Ocean based on adjoint seismic tomography.

129 cetacean species/groups in the western North Atlantic Ocean based on generalized additive models, to

130 Here we use macrostratigraphic data from the Atlantic Ocean basin to show that changes in global spec

131 Reconnection of the Pacific and Atlantic Ocean basins will present both challenges to ma

132 rds and mammals move between the Pacific and Atlantic Ocean basins.

133 ion in which they gradually circle the north Atlantic Ocean before returning to the North American co

134 distribution during six cruises in the West Atlantic Ocean between 2008 and 2010 and examined enviro

135 degrees N) through the western basins of the Atlantic Ocean between the 1950s and the 1990s.

136 and velocity fluctuations in the Pacific and Atlantic oceans between 42 degrees N and 2 degrees S to

137 on photochemical ozone loss in the tropical Atlantic Ocean boundary layer.

138 mpact on climate variability in the tropical Atlantic Ocean, but a robust influence is found only in

139 on the climate and circulation of the North Atlantic Ocean, but their influence beyond that region r

140 recolonization of the southern South-Western Atlantic Ocean by snoek from the South-Eastern Pacific O

141 carbonate-ion concentrations in the glacial Atlantic Ocean, by roughly 20 micromolkg-1, while little

142 sts that the provenance of deep water in the Atlantic Ocean can be decoupled from ventilation state o

143 pleted glacial delta(13)C values in the deep Atlantic Ocean cannot be explained solely by water mass

144 e remaining fraction was exported toward the Atlantic Ocean, Central Asia, Northern, and Tropical Afr

145 nity, suggesting a tight linkage between the Atlantic Ocean circulation and hydrologic cycle during t

146 sent) have been linked with changes in North Atlantic Ocean circulation.

147 ensive compilation of data from the subpolar Atlantic Ocean, clear evidence of a marked pre-bloom sil

148 temperature and salinity in the Pacific and Atlantic oceans close to the gauges.

149 cent equatorial and temperate regions of the Atlantic Ocean, collected on three Atlantic Meridional T

150 nd in the Pacific, Indian and southern South Atlantic Oceans, comprising five previously allopatric s

151 these cycles coincides with changes in North Atlantic Ocean conditions, indicating a connectivity bet

152 nts were detected in the Pacific, Indian and Atlantic oceans, confined to a strip along the equator (

153 ored by a uranium-lead chronology with North Atlantic ocean data to show that the first two deglaciat

154 idional overturning circulation in the North Atlantic Ocean does not lead to a net cooling in Europe.

155 titude ~36 degrees S) and western equatorial Atlantic Ocean Drilling Project Site 929 (paleolatitude

156 involve changes in circulation of the North Atlantic Ocean due to the closing of the Isthmus of Pana

157 pecies that breed in North America cross the Atlantic Ocean during autumn migration when travelling t

158 eak decrease over the U.S. Southeast and the Atlantic Ocean during summer.

159 The circulation of the deep Atlantic Ocean during the height of the last ice age app

160 position of ice-rafted detritus in the North Atlantic Ocean during the last glacial period interprete

161 ion of passive continental margins along the Atlantic Ocean during the opening phase of the current W

162 changes in the tropical rainbelt across the Atlantic Ocean during the past two millennia are linked

163 peratures of the deep Pacific, Southern, and Atlantic oceans during the LGM were relatively homogeneo

164 ficant debate as to the role played by North Atlantic Ocean dynamics in previous climate transitions

165 ti-decadal timescales, indicating that North Atlantic Ocean dynamics played an active role in modulat

166 te and sustainable system for monitoring the Atlantic Ocean exists.

167 stadial salinities preconditioned the North Atlantic Ocean for a rapid return to deep overturning ci

168 er clouds, separately in four regions of the Atlantic Ocean, for June through August 2002: marine aer

169 During one of his many voyages across the Atlantic Ocean, Franklin observed that oil had a calming

170 have been a swarming locust that crossed the Atlantic Ocean from Africa to America approximately 6 mi

171 Despite receiving unpolluted air off the Atlantic Ocean from northeasterly trade winds, during tw

172 ntrations were investigated in the Northwest Atlantic Ocean from September to October 2016.

173 tion depth in the tropical Pacific and South Atlantic oceans from approximately 42 million years ago,

174 water to the Arctic and high-latitude North Atlantic oceans from lows in the 1960s to highs in the 1

175 on of water masses in the northeastern North Atlantic Ocean has a strong influence on global climate

176 Samples from the Atlantic Ocean have been analyzed using the parabactin b

177 IBRD records from the North Atlantic Ocean have been widely used to reconstruct vari

178 ation taken from sediment cores in the South Atlantic Ocean have yielded conflicting interpretations

179 culation response at only a few sites in the Atlantic Ocean, however, and the phase of circulation re

180 cal sea surface temperature anomalies in the Atlantic Ocean (i.e., Atlantic Multidecadal Oscillation,

181 on an east-west transect across the tropical Atlantic Ocean in 2009 and analyzed for PBDEs.

182 of 772 Atlantic bluefin tuna in the western Atlantic Ocean in an effort to identify population struc

183 e lead isotope composition of the deep North Atlantic Ocean in response to chemical weathering, we fi

184 in the euphotic layer of the temperate North Atlantic Ocean in summer.

185 of the bottles floating in the central South Atlantic Ocean, in contravention of International Conven

186 amine the timing of dust fluxes to the North Atlantic Ocean, in relation to climate records from the

187 d air during three cruises in the Arctic and Atlantic Oceans, in/over generally oligotrophic waters.

188 ame depth, 1800 meters, in the western North Atlantic Ocean increased by as much as 670 years during

189 Scotland, immediately downwind of the North Atlantic Ocean, indicating that the Scottish ice cap dis

190 variations of the surface temperature of the Atlantic Ocean induce shifts in the non-stationary effec

191 rier from low to high latitudes in the North Atlantic Ocean, influences the climate and weather in th

192 undary (CMB) region beneath the southeastern Atlantic Ocean into the upper mantle beneath eastern Afr

193 size-class suspended in the top 200 m of the Atlantic Ocean is 11.6-21.1 Million Tonnes.

194 to abrupt climate change events in the North Atlantic Ocean is contentious.

195 The Atlantic Ocean is the most important CO2 sink, providing

196 nd the Faroe Shetland channel into the North Atlantic Ocean is the principal means of ventilating the

197 mixing in the deep Brazil Basin of the South Atlantic Ocean is weak at all depths above smooth abyssa

198 The Atlantic Ocean is well ventilated, and unlike the major

199 deep-water flow between the Arctic and North Atlantic oceans is critical for modelling climate change

200 m 531A, isolated from a diseased fish in the Atlantic Ocean, is a mixture composed of about 95 and 5%

201 out the entire Southern Hemisphere and North Atlantic Ocean, is the main source of nutrients for the

202 s in the Southwestern Pacific and equatorial Atlantic oceans, it came to our attention that misannota

203 associating with warmer northern Pacific and Atlantic oceans, leading mostly to global supply shortag

204 rgs through the Hudson Strait into the North Atlantic Ocean, leaving behind distinct layers of ice-ra

205 s: Extensive iceberg influxes into the North Atlantic Ocean linked to global impacts on climate and b

206 Thus, sea salts from seven north-east Atlantic Ocean locations (France, Portugal, Continental

207 asis of detailed observations from the North Atlantic Ocean, mantle temperature was identified as the

208 ation, it is plausible that the entire North Atlantic Ocean may vary in concert, resulting in a varia

209 ginate lyases were predominantly detected in Atlantic Ocean metagenomes.

210 For large swaths of the tropical Atlantic Ocean, neither PCB nor organochlorine pesticide

211 anariensis, a coral species collected in the Atlantic Ocean never described as a PLTX-producer before

212 results of an experiment conducted over the Atlantic Ocean, off the coast of France, confirming the

213 c samples were collected across the tropical Atlantic Ocean on a transect of the R/V Endeavor in summ

214 nresolved, with tectonic restrictions to the Atlantic Ocean or glacio-eustatic restriction of flow du

215 n the island of Bermuda in the western North Atlantic Ocean over 18 mo.

216 inental breakup and the opening of the North Atlantic Ocean over a period from 62 to 54 Ma.

217 ense hurricane activity in the western North Atlantic Ocean over the past 5,000 years based on sedime

218 The total heat gained by the North Atlantic Ocean over the past 50 years is equivalent to a

219 nthic microfaunal record from the equatorial Atlantic Ocean over the past four glacial-interglacial c

220 in scale (50 degrees S-36 degrees N) for the Atlantic Ocean over two decades (1993-2013).

221 Occurrence in animals from the Pacific and Atlantic oceans over 111 years made a pathophysiological

222 The Atlantic Ocean overturning circulation is important to t

223 123 linear paths of subsurface water of the Atlantic Ocean, passing by Cape Verde, the east coast of

224 Across the entire tropical Atlantic Ocean, phenanthrene displayed on average highes

225 uesas Islands or between southern Indian and Atlantic Oceans-pointing to a tight correlation between

226 ing a targeted metagenome from an uncultured Atlantic Ocean population.

227 The Atlantic Ocean presented on average the highest PCDD/F a

228 The Atlantic Ocean presented the broader range in concentrat

229 e of heat from warm waters in the deep North Atlantic Ocean probably triggered the Bolling-Allerod wa

230 new evidence that basin-scale changes in the Atlantic Ocean, probably related to the thermohaline cir

231 sages on the Mid-Atlantic Ridge in the North Atlantic Ocean produce as much buoyancy flux as has prev

232 levels of fisheries exploitation across its Atlantic Ocean range.

233 The Atlantic Ocean receives warm, saline water from the Indo

234 ted from the bipolar seesaw behaviour of the Atlantic Ocean related to changes in the ocean circulati

235 e same latitude but on opposite sides of the Atlantic Ocean, responded by swimming in different direc

236 We suggest that stratification of the North Atlantic Ocean resulted in amplified seasonality that, p

237 tration in deep-sea cores from the southeast Atlantic Ocean reveal millennial-scale pulses of IRD del

238 Measurements of [CO3(2-)] along the Atlantic Ocean showed high consistency with the [CO3(2-)

239 ral phytoplankton community in the southeast Atlantic Ocean showed no significant toxic response at a

240 connected with the broad southern Indian and Atlantic Oceans, showing that the AC system is pivotal f

241 water have been added to the northern North Atlantic Ocean since the mid-1960s.

242 systems in the Gulf of Mexico (GOM) and U.S. Atlantic Ocean south of Chesapeake Bay were deemed to be

243 fects, in seagrass ecosystems of the western Atlantic Ocean spanning 30 degrees of latitude from the

244 n isotope (delta(18)O) record from the South Atlantic Ocean spanning an interval between 30.1 My and

245 Here we reconstructed an index of the South Atlantic Ocean SST (SASD-like) for the past twelve thous

246 h groups detected on the eastern and western Atlantic Ocean suggest that these associations are a gen

247 he surface waters of the tropical North-East Atlantic Ocean, suggesting the global significance of mi

248 These observations imply that Atlantic Ocean surface water circulation was radically d

249 roductivity in the Amazon Basin and Tropical Atlantic Ocean (TAO), leading to sequestration of carbon

250 pass-filtered variance, in northern tropical Atlantic Ocean temperatures.

251 tion of ferromanganese crusts from the North Atlantic Ocean that cover the past 550,000 years.

252 ralline algal time series from the northwest Atlantic Ocean that exhibits multidecadal variability ex

253 ote, uninhabited island in the central South Atlantic Ocean that has a very high macrodebris load (~5

254 Mid-Atlantic Ridge in the subtropical North Atlantic Ocean that suggest that passages in rift valley

255 However, in the north and tropical Atlantic Ocean, the Atlantic Multidecadal Oscillation (a

256 In the northwest Atlantic Ocean, the depletion of large coastal sharks wa

257 geographically isolated ocean provinces (the Atlantic Ocean, the Red Sea and the Indian Ocean) were s

258 with changes in a major climate mode in the Atlantic Ocean: the Atlantic Multidecadal Oscillation (A

259 Variations in the strength of the North Atlantic Ocean thermohaline circulation have been linked

260 of hurricane activity in the tropical North Atlantic Ocean threatens the sustainability of modern pi

261 s freshwater outburst delivered to the North Atlantic Ocean through the Lake Huron-North Bay-Ottawa R

262 s deep-water exchange between the Arctic and Atlantic oceans throughout the past 35,000 years.

263 trophic marine species from the southwestern Atlantic Ocean, tissue from bottlenose dolphins (Tursiop

264 9/11 on mental disorders extended across the Atlantic Ocean to Denmark.

265 , a distance of 5000 to 10,000 km across the Atlantic Ocean to the Sargasso Sea.

266 e transition regions of the North Sea to the Atlantic Ocean, to the Baltic Sea, and upstream the Elbe

267 ediate depths (500-2,000 m) across the North Atlantic Ocean, to the south and to the east of the Labr

268 sses (Diomedeidae) do not occur in the North Atlantic Ocean today except as vagrants, although five s

269 lation from the Norwegian Sea into the North Atlantic Ocean took place much earlier than is currently

270 itrate in seawater and air samples along two Atlantic Ocean transects provide the first direct eviden

271 of the Equator arises primarily because the Atlantic Ocean transports energy northward across the Eq

272 enriched in the Mediterranean Sea and North Atlantic Ocean, two regions that feature sustained perio

273 re of surface waters in the western tropical Atlantic Ocean underwent pronounced variability about 10

274 s the biomass of deep-pelagic shrimps in the Atlantic Ocean using data collected between 40 degrees N

275 hat, during 1955-2017, up to one-half of the Atlantic Ocean warming and thermosteric sea-level rise a

276 he temperature of deep water in the tropical Atlantic Ocean was 4°C colder during the last glacia

277 time, the diet of sunfish in the north-east Atlantic Ocean was characterised.

278 of plants of any volcanic archipelago in the Atlantic Ocean, was performed to examine patterns of pla

279 e is enough heat contained in inflowing warm Atlantic Ocean water to melt all Arctic sea ice within a

280 d from the Last Glacial Maximum in the North Atlantic Ocean we found that past temperatures reconstru

281 In the North Atlantic Ocean, we found that natural populations of Pro

282 ated with gas hydrates at Blake Ridge in the Atlantic Ocean were dated by measuring their iodine-129/

283 icate that the marine resources of the North Atlantic Ocean were used to sustain an international dem

284 here form four groups, corresponding to the Atlantic Ocean, West pacific, mid-Pacific, and east Paci

285 emained in deep water until they reached the Atlantic Ocean, when they recommenced DVM.

286 ed during a 15,000-kilometer transect in the Atlantic Ocean where iron concentrations are relatively

287 the South China Sea, Indian Ocean and South Atlantic Ocean where the relative wind direction matched

288 America and over the east Pacific and North Atlantic oceans where July wind anomalies, averaged betw

289 ose uptake by Prochlorococcus in the central Atlantic Ocean, where glucose concentrations were 0.5-2.

290 essfully made a 2-4 month migration into the Atlantic Ocean, where they utilised well-defined core ar

291 he water mass that fills the mid-depth North Atlantic Ocean, which had been believed to be formed ent

292 ponent of the overturning circulation of the Atlantic Ocean, which helps regulate global climate.

293 n intermediate and deep water in the glacial Atlantic Ocean, which indirectly points to an increase i

294 ays (Mobula tarapacana) in the central North Atlantic Ocean, which provide movement patterns of indiv

295 DZs) in both the Northeast Pacific and North Atlantic Oceans, which we attribute to Cd sulfide (CdS)

296 hanges in oceanic characteristics across the Atlantic Ocean will result in remarkable vulnerability o

297 year-round habitat use of the western North Atlantic Ocean, with a decrease in detections in waters

298 ical evolution of air masses in the tropical Atlantic Ocean, with a focus on halogen chemistry.

299 ndergoing net deposition across the tropical Atlantic Ocean, with conditions closer to equilibrium of

300 ies are found in the temperate western North Atlantic Ocean, with limited information existing on the