ライフサイエンスコーパス: Atlantic

1 edge kelp forests on both sides of the North Atlantic.

2 influences on hydroclimate over the tropical Atlantic.

3 n the upper Porcupine Bank Canyon (uPBC), NE Atlantic.

4 whales (Megaptera novaeangliae) in the North Atlantic.

5 austion of excess carbonate in the Northeast Atlantic.

6 res the multidecadal variability seen in the Atlantic.

7 , Gulf of Mexico and western North and South Atlantic.

8 iction of ISOW pathways throughout the North Atlantic.

9 iological productivity in the tropical North Atlantic.

10 termining the salinity of the subpolar North Atlantic.

11 uth of Greenland, cooling the subpolar North Atlantic.

12 curately the temperature change in the North Atlantic.

13 nnected to lower latitudes through the North Atlantic.

14 onized the already existing rookeries of the Atlantic.

15 Sharks were collected from the North-East Atlantic.

16 ic diversity within a major ocean basin (the Atlantic), a regional rookery (Cabo Verde Archipelago) a

17 duals in the Americas and populations across Atlantic Africa, yielding a more comprehensive understan

18 nucleotide polymorphisms clearly resolved an Atlantic and a Norwegian group within P. maximus as well

19 Atlantic herring is widespread in North Atlantic and adjacent waters and is one of the most abun

20 bility that recurrent blooms in the tropical Atlantic and Caribbean Sea may become the new norm.

21 6 times larger to protect the same number of Atlantic and Caribbean species, which occur at lower abu

22 ortion of MeHg sources between western North Atlantic and eastern Arctic regions.

23 Here, we show that along the North American Atlantic and Gulf coasts the meridional distributions of

24 It compares methods on either side of the Atlantic and highlights challenges and solutions.

25 als AESs around sub-Antarctic islands in the Atlantic and Indian Oceans and over the Antarctic contin

26 changes in the Pacific Ocean compared to the Atlantic and Indian Oceans.

27 lankton populations in the Subtropical South Atlantic and Irminger Basin.

28 ch is critically endangered in the Northeast Atlantic and landings have been prohibited (although the

29 sly two species) is distributed in the North Atlantic and Mediterranean Sea.

30 s of potential teleconnections between North Atlantic and mid-to-low latitudes at the transition from

31 eef fish trophic interactions in the Western Atlantic and modeled projections of changes in fish occu

32 [Cl] is increasing at nearly all Mid-Atlantic and New England sites with the largest increase

33 In the Mid-Atlantic and New England, [Cl] and [Cl] exceedances stro

34 vironmental conditions in the tropical North Atlantic and North Pacific and significantly correlated

35 e anticorrelation of TUTTs between the North Atlantic and North Pacific makes the TC activity indices

36 alysis of surge extremes covering the entire Atlantic and North Sea coasts of Europe for the period 1

37 nonmigrants in the tropical Americas and on Atlantic and Pacific Islands.

38 15%-30% (+/-12%-17%) in the North and South Atlantic and Pacific, and the Indian Ocean by 2100, wher

39 d habitat quality and resourcefulness of Mid-Atlantic and possibly other USA coastal regions.

40 in the eastern United States: Southeast, Mid-Atlantic, and New England.

41 red laminarin along transects in the Arctic, Atlantic, and Pacific oceans and during three time serie

42 The ocean and atmosphere in the North Atlantic are coupled through a feedback mechanism that e

43 This, in turn, supports the South Atlantic as a locus of unusual geomagnetic behavior aris

44 s across the Falkland Plateau into the South Atlantic as a series of high-velocity jets.

45 ported from the Norwegian Sea into the North Atlantic as part of the global Meridional Overturning Ci

46 on (the leading mode of variability in North Atlantic atmospheric circulation) by an order of magnitu

47 . counties for all land-falling or near-land Atlantic basin storms, covering 1996-2011 for all metric

48 ropical cyclone intensification rates in the Atlantic basin that are highly unusual compared to model

49 ng subsurface warming throughout much of the Atlantic basin(9,12,17).

50 cyclone ecology is biased towards the North Atlantic Basin, because cyclone effects do differ across

51 southeast trade winds in the tropical South Atlantic Basin.

52 tal mercury in muscle tissue from 268 reared Atlantic bluefin tuna in the Mediterranean Sea, detects

53 ies investigated (blue marlin, white marlin, Atlantic bluefin tuna, yellowfin tuna) frequently crosse

54 encephalitis virus has been detected in wild Atlantic bottlenose dolphins, and captive orcas have bee

55 p boundary current around the subpolar North Atlantic, but this single-boundary-following pathway is

56 mited climate refugia locations in the North Atlantic by 2100 for scleractinian corals (30%-42% of pr

57 Capitalizing on Atlantic Canada's largest freshwater wetland, the Grand

58 a substantial warming over much of the North Atlantic, caused by increasing greenhouse gases over the

59 Mid-Atlantic chronic [Cl] exceedances occur primarily in Dec

60 Northeast Atlantic climate shifted into the Quaternary Ice Age aro

61 ons are in agreement with multidecadal North Atlantic climate variability derived from independent pr

62 blue crab (Callinectes sapidus) along the US Atlantic coast and found that their intrinsic dynamics w

63 extinct Tupi branch that used to settle the Atlantic Coast of Brazil.

64 Scotia to Georgia winter exclusively on the Atlantic coast of northern South America and share commo

65 n endemic species of the dune systems of the Atlantic coast of the Iberian Peninsula.

66 the northern Amazon and then directly to the Atlantic coast, or heading south into the continent and

67 ecognized across the Southeast, Midwest, and Atlantic Coast, with many providers in this area managin

68 Atlantic coastal, semirural site, with comparative urban

69 ted 12.5 million people from ports along the Atlantic coastline of Africa between the 16th and 19th c

70 ng and autumn through the Gulf of Mexico and Atlantic coasts of the south-eastern US, the most promin

71 across much of the Gulf of Mexico and south Atlantic coasts of the United States.

72 Along the US Atlantic coasts the contribution of tides can be signifi

73 Atlantic cod (Gadus morhua) has recently emerged as a mo

74 different functional specializations of the Atlantic cod Ahr's.

75 lyses revealed two Ahr-encoding genes in the Atlantic cod genome, gmahr1a and gmahr2a.

76 ransformation limits and the central role of Atlantic cod, which is the main target species but canno

77 These results suggest that within a Mid-Atlantic cohort, patient subgroups can be identified usi

78 Samples from the NE Atlantic contained this anthropogenic imprint at distanc

79 ta, ruggedness, and backscatter from a trans-Atlantic corridor along the Vema Fracture Zone, covering

80 regarious fish native to the Gulf of Mexico, Atlantic croaker (Micropogonias undulatus).

81 circulation, including slowing of the North Atlantic Current and diversion of Arctic freshwater from

82 importantly, we show evidence that the North Atlantic current and its variability shape the spatial d

83 reveal an increase, up to two-fold, in North Atlantic current surface velocities over the last 24 yea

84 ep-reaching eddies and meanders of the North Atlantic Current.

85 m, the West Atlantic D. antillarum, the East Atlantic D. africanum, and the Indo-Pacific D. paucispin

86 n in the East Pacific D. mexicanum, the West Atlantic D. antillarum, the East Atlantic D. africanum,

87 emperature (SST) estimates from southwestern Atlantic Deep Sea Drilling Project Site 516 (paleolatitu

88 Disrupting North Atlantic Deep Water (NADW) ventilation is a key concern

89 Here we present a detailed record of North Atlantic deep-ocean temperature, global sea-level, and i

90 ant wave directions in the Subtropical South Atlantic during the last ~ 3000 years.

91 imply a larger fraction of NADW in the deep Atlantic during the LGM and deglaciation than reconstruc

92 urce, as well as a crucial part of the North Atlantic ecosystem.

93 ter properties in the eastern subpolar North Atlantic (ENA).

94 warmer, higher-salinity water from the North Atlantic entering the Arctic (260 +/- 20 pg/L versus 190

95 Over the past century, the subpolar North Atlantic experienced slight cooling or suppressed warmin

96 In Brazil's Atlantic Forest (AF) biodiversity conservation is of key

97 We extrapolated our findings to the entire Atlantic Forest and found that just 19.4% of the total e

98 ted in October 2017 in Aloutta monkeys in an Atlantic Forest area.

99 uence, An. cruzii moves to the border of the Atlantic Forest nearing urban areas seeking resources, i

100 eshy fruit plants in six sites in continuous Atlantic forest of Brazil.

101 by northern (lowland) and southern (montane) Atlantic Forest species, triggered by the joint impact o

102 focused on the globally threatened Brazilian Atlantic Forest, where commitments have been made to res

103 The Brazilian Atlantic Forest, which has been undergoing an intense pr

104 ~30% of endemic species richness of primary Atlantic forest.

105 malaria-elimination efforts in the Brazilian Atlantic Forest.

106 especially in the northeastern Andes and the Atlantic Forest.

107 nderstorey epiphytic plants in the Brazilian Atlantic Forest.

108 y 11%-30% and spread over lowland Amazon and Atlantic forests.

109 (2) of rock habitats potentially occur along Atlantic fracture zones alone, significantly increasing

110 ted using plankton nets in the western North Atlantic from 1986 to 2015.

111 d to much greater depths than those at Trans-Atlantic Geotraverse and Logachev-1 hydrothermal fields

112 metabolomes of five mother and pup pairs of Atlantic grey seals, Halichoerus grypus, from birth to w

113 two species) inhabits the eastern equatorial Atlantic, Gulf of Mexico and western North and South Atl

114 ries Study (BATS) in the Sargasso Sea (North Atlantic gyre) provides a unique opportunity to explore

115 During the larval period, Atlantic haddock (Melanogrammus aeglefinus) are transpor

116 Here, we exposed Atlantic haddock embryos to 10 and 80 mug oil/L (0.1 and

117 modeling experiments to show that the North Atlantic has also strongly influenced the Extratropical

118 etic models suggests the colonization of the Atlantic has occurred in two distinct waves, each corres

119 Atlantic herring has an estimated total breeding stock o

120 Atlantic herring is widespread in North Atlantic and adj

121 n hurricane-associated rainfall in the North Atlantic highlight the need to consider how such shifts,

122 This suggests that spatial heterogeneity in Atlantic hurricane activity since 1850 CE could have per

123 ing examples from Hawaiian volcanic and West Atlantic hurricane interactions, this work illustrates h

124 ined the effects of the most energetic North Atlantic hurricane season in 50 years on the genetic div

125 The 2017 North Atlantic hurricane season induced record-breaking econom

126 shear (VWS), a metric that strongly controls Atlantic hurricanes.

127 ucted climate variables characterizing North Atlantic: i.e. sea surface temperatures (SST) from the t

128 ikely linked to eruptive phases of the North Atlantic Igneous Province.

129 ast geological events spanning the Northeast Atlantic inception of an Ice Age.

130 apor transport from the tropical Pacific and Atlantic increased high-altitude atmospheric humidity an

131 n the Pacific sector and deceleration in the Atlantic-Indian Sectors, forming a bi-polar spatial patt

132 r taxa under a future scenario of increasing Atlantic influence, but the eukaryote response is more c

133 and slow) have different frequencies across Atlantic intertidal zones due to selection on postsettle

134 The high salinity of the subpolar North Atlantic is a prerequisite for overturning circulation,

135 Here, the chemical status of the Northeast Atlantic is examined by means of a high-quality database

136 ayer, the carbonate content in the Northeast Atlantic is maintained by the interplay between the nort

137 elected Tropic Seamount in the North-Eastern Atlantic is representative for the majority of isolated

138 e may be having a larger impact on the North Atlantic jet stream than previously thought. The increas

139 neys often share the same production area in Atlantic landscapes.

140 g this deep water cycle because hydration in Atlantic lithosphere, produced by slow spreading, is exp

141 shelf-life of mechanically filleted well-fed Atlantic mackerel during frozen storage at -25 degrees C

142 Afterwards, films were used on Atlantic mackerel stored at -18 degrees C for 4 months a

143 et molecules from the most abundant species (Atlantic mackerel) both in real-time and from the archiv

144 lavour and odour in complex matrixes such as Atlantic mackerel.

145 was linked to diel migration patterns of the Atlantic mackerel.

146 ns are linked to the eruption of the Central Atlantic Magmatic Province (CAMP) flood basalts.

147 w PGE data for volcanic rocks of the Central Atlantic Magmatic Province (CAMP) in Morocco and show th

148 The Central Atlantic Magmatic Province (CAMP) is the most aerially e

149 The Central Atlantic magmatic province (CAMP), the end-Triassic mass

150 basaltic rocks from the end-Triassic Central Atlantic Magmatic Province (CAMP), through investigation

151 have become well-established in many western Atlantic marine habitats and regions.

152 prioritization strategies, the Northeastern Atlantic marine terebellid Eupolymnia nebulosa was selec

153 re, continued ocean warming in the northeast Atlantic may reduce primary productivity of this foundat

154 ttribute to invigoration or weakening of the Atlantic meridional overturning circulation (AMOC) and a

155 The change in the Atlantic Meridional Overturning Circulation (AMOC) and o

156 ep convection, affecting the strength of the Atlantic Meridional Overturning Circulation (AMOC) and t

157 limate anomalies in response to slow-down of Atlantic meridional overturning circulation (AMOC) durin

158 y effective during glacial periods, when the Atlantic Meridional Overturning Circulation (AMOC) exper

159 mportant diagnostic for the stability of the Atlantic Meridional Overturning Circulation (AMOC).

160 Indian Ocean warming acts to strengthen the Atlantic meridional overturning circulation (AMOC).

161 planktonic stocks in response to a weakened Atlantic Meridional Overturning Circulation(6-8).

162 k Channel and supplies the lower limb of the Atlantic Meridional Overturning Circulation, a critical

163 ordic Seas comprises the deepest limb of the Atlantic Meridional Overturning Circulation, yet questio

164 n in accordance with stronger (weaker) South Atlantic mid- to high-latitudes mean sea-level pressure

165 equent records from other parts of the North Atlantic, minke whales have never been acoustically reco

166 s they provide, under predicted increases of Atlantic mixing and warming within the Arctic region.

167 highlight the potential role of other North Atlantic modes of variability (i.e., East Atlantic patte

168 ISM rainfall appears to be modulated by the Atlantic Multi-decadal Oscillation (AMO) via changes in

169 Nino-Southern Oscillation (ENSO), the North Atlantic Multidecadal Oscillation (AMO), and tropical cy

170 Predictions of Atlantic multidecadal variability are also improved, sug

171 Atlantic which vary on a multidecadal scale (Atlantic multidecadal variability, AMV).

172 Atlantic Oscillation is not driven solely by Atlantic multidecadal variability.

173 g dominated the distribution of deep glacial Atlantic Nd isotopes, our results would imply a larger f

174 sharks, Cetorhinus maximus, in the Northeast Atlantic (NEA) affords an opportunity to resolve individ

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

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

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

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

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

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

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

182 The Atlantic Ocean overturning circulation is important to t

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

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

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

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

187 pply on phytoplankton iron status across the Atlantic Ocean.

188 but frequency was depressed elsewhere in the Atlantic Ocean.

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

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

191 n overseas French territory in the northwest Atlantic Ocean.

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

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

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

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

196 teleconnections to regions beyond the North Atlantic offer the prospect of reconstructing AMV from h

197 In the eastern eropical North Atlantic, OMZ expansion in the course of global climate

198 tic field behavior is anomalous in the South Atlantic on timescales of millions of years.

199 The North Atlantic Oscillation (NAO) is the major atmospheric mode

200 ance from the coast, elevation and the North Atlantic Oscillation (NAO) using PEP725 leafout data for

201 g El Nino Southern Oscillation (ENSO), North Atlantic Oscillation (NAO), and Pacific Decadal Oscillat

202 ction of the total variability) of the North Atlantic Oscillation (the leading mode of variability in

203 (a) negatively associated with lagged North Atlantic Oscillation for seals at NR and (b) positively

204 just the variance of the ensemble-mean North Atlantic Oscillation forecast to match the observed vari

205 closely related to enhancement of the North Atlantic Oscillation index.

206 are also improved, suggesting that the North Atlantic Oscillation is not driven solely by Atlantic mu

207 antic Ocean and positive phases of the North Atlantic Oscillation on decadal scales.

208 d use only the ensemble members with a North Atlantic Oscillation sufficiently close to the variance-

209 The North Atlantic Oscillation was closed related to the opposite

210 ssociated with a positive phase of the North Atlantic Oscillation.

211 riance-adjusted ensemble-mean forecast North Atlantic Oscillation.

212 Extrapolating to the whole Atlantic, over 260,000 km(2) of rock habitats potentiall

213 We suggest Antarctic sea ice and Atlantic overturning conditions favoured abyssal ocean v

214 an upwelling, likely promoted by rejuvenated Atlantic overturning.

215 th Atlantic modes of variability (i.e., East Atlantic pattern) on the non-stationary behaviour of the

216 nce of the predicted(5) collapse of northern Atlantic planktonic stocks in response to a weakened Atl

217 to distinct assemblages across a gradient of Atlantic-Polar Water influence in the Norwegian Sea.

218 ent OSNAP (Overturning in the Subpolar North Atlantic Program) data with respect to estimates from cl

219 th high spatial resolution in the North-East Atlantic provides a unique opportunity to assess the abi

220 We observed 2 Atlantic puffins at their breeding colonies, one in Wale

221 ures were widely dispersed through the North Atlantic reducing their overlap with breeding adults.

222 m 1982 to 2004 for Chesapeake Bay in the mid-Atlantic region of the United States supported estimates

223 ariability has repeatedly affected the North Atlantic region with predictable consequences.

224 of sea-surface pressure changes in the North Atlantic region, whose waters are among the world's fast

225 rmation on their acoustic behaviour in a mid-Atlantic region.

226 whales had higher acoustic occurrence in mid-Atlantic regions after 2010.

227 ture alkaline hydrothermal vents off the Mid-Atlantic Ridge axis nearly 20 y ago, the observation tha

228 mantle wedge peridotite dredged from the Mid-Atlantic Ridge near 16 degrees 30'N.

229 n created during 26 Ma at a 11 degrees N Mid-Atlantic Ridge segment, and exposed along the Vema Trans

230 nd Logachev-1 hydrothermal fields on the Mid-Atlantic Ridge.

231 y of ISOW along the western flank of the Mid-Atlantic Ridge.

232 The North Atlantic right whale (Eubalaena glacialis) is one of the

233 detect the vocalizations of endangered North Atlantic right whales (Eubalaena glacialis).

234 minke (Balaenoptera acutorostrata) and North Atlantic right whales (NARW; Eubalaena glacialis).

235 iated with probabilities of endangered North Atlantic right whales Eubalaena glacialis migrating to a

236 , we derived thermal affinities for European Atlantic rocky intertidal species by matching their know

237 and report 15,483 high-confidence SVs in 492 Atlantic salmon (Salmo salar L.) sampled from a broad ph

238 despread decline in marine survival rates of Atlantic salmon (Salmo salar) over the last four decades

239 s disease causing severe economic losses for Atlantic salmon aquaculture.

240 investigated the genetic basis of growth in Atlantic salmon by exploiting the high level of genetic

241 ates the potential for production of further Atlantic salmon clonal lines, potentially with distinct

242 Atlantic salmon eggs fertilized with UV irradiated sperm

243 ice abundance after 38 EMB treatments on six Atlantic salmon farms, in a small archipelago in British

244 The Atlantic salmon is one of the best studied fish species

245 ave now produced the first documented cloned Atlantic salmon lines.

246 he differences between wild and domesticated Atlantic salmon may provide insights into some of the ge

247 Functional divergence of tshbeta paralogs in Atlantic salmon supports a specific role of tshbetab in

248 me of the offspring of wild and domesticated Atlantic salmon were compared using a common-garden expe

249 ach was used to distinguish fresh and thawed Atlantic salmon.

250 tion of epistasis in a quantitative trait in Atlantic salmon.

251 es, and from these the first clonal lines in Atlantic salmon.

252 North Atlantic sea surface temperatures have large climate imp

253 ts can occur within a single year (e.g., the Atlantic seaboard due to tropical cyclones and atmospher

254 ication of megalithic architecture along the Atlantic seaboard, culminating in the great passage tomb

255 earliest farming communities of the European Atlantic seaboard.

256 -ice and the ice-associated ecosystem in the Atlantic Sector lasts far beyond their short lifespan.

257 ntimately links conditions on the North West Atlantic shelf and slope region with the eastern subpola

258 However, across the Northeast Atlantic shelves, there has been an ongoing summertime d

259 Episodes of reduced NADW in the deep Atlantic, similar in magnitude to glacial events, have b

260 o large climate-induced changes in the North Atlantic simultaneously impacting populations from dista

261 ane impacts than almost anywhere else in the Atlantic since 1850 CE.

262 n flows surround the edges of the Rivera and Atlantic slabs, while escape flows are inferred through

263 ese refugia, the Cantabrian region (northern Atlantic Spain), was intensively occupied throughout the

264 High-Arctic proxy and other highly resolved Atlantic SST proxies demonstrate that it shares the mult

265 eric-only model, that anomalously warm North Atlantic SSTs enhance heatwave activity through an assoc

266 recedented time resolution, indicating North Atlantic SSTs were coldest from ~1400-1800 CE, while cur

267 uctions in the East North Central and Middle Atlantic states.

268 ences in pstS between the ETNP and the North Atlantic stations were consistent with differences in ph

269 establish baseline information on endangered Atlantic Sturgeon in the New York Wind Energy Area (NY W

270 Atlantic subduction zones are a valuable endmember when

271 The north Atlantic subpolar gyre (SPG) has been widely implicated

272 The Gulf Stream front separates the North Atlantic subtropical and subpolar ocean gyres, water mas

273 In contrast to the ETNP, in the oxic North Atlantic T4-like cyanophages encoded psbA and pstS throu

274 Thus, explaining the North Atlantic temperature trends and particularly the NAWH re

275 ion factors are all generally greater in the Atlantic than the Pacific.

276 tuce, is a fast growing seaweed in the North Atlantic that chefs are bringing into the local cuisine.

277 Along the Gulf Stream front in the North Atlantic, these observations further suggest that shear

278 In this respect, the Bermuda Atlantic Time-series Study (BATS) in the Sargasso Sea (N

279 o synchronize ocean sediments from the North Atlantic to correlate major climate events in a common t

280 experiments were performed in the northwest Atlantic to elucidate connectivity among areas closed to

281 anistic path by which a climatic driver, the Atlantic trade winds, determines the viability of a bird

282 A common North Atlantic trend explains 37% of the temporal variability

283 This timing precludes an Atlantic trigger for Cordilleran Ice Sheet retreat and i

284 es because they are known to influence North Atlantic tropical cyclone activity and because their und

285 t the cross-currents of the Tropical Western Atlantic (TWA).

286 We show that the eastern subpolar North Atlantic underwent extreme freshening during 2012 to 201

287 In the Mid-Atlantic United States, two Asian species of mason bee (

288 Using pan-trap records from the Mid-Atlantic US, we examined catch abundance of two exotic a

289 The second lineage entered the Atlantic via the Cape of Good Hope, establishing colonie

290 e temperature trends, often dubbed the North Atlantic warming hole (NAWH).

291 observations, we show that the recent North Atlantic warming hole is of anthropogenic origin.

292 ng at midlatitudes, referred to as the North Atlantic warming hole.

293 Increasing influence of Atlantic water in the Arctic Ocean has the potential to

294 % of in- and outflow takes place), the North Atlantic Waters transport most of the ocean heat, but al

295 sea surface temperatures (SSTs) in the North Atlantic which vary on a multidecadal scale (Atlantic mu

296 ideo transects in the eastern tropical North Atlantic, which features a mild but intensifying midwate

297 of AChE in the hippocampal formation of the Atlantic white-sided dolphin (AWSD) with the view to und

298 es and show that decadal variations in North Atlantic winter climate are highly predictable, despite

299 tending from the Bering Sea to the northwest Atlantic, with high levels of genetic diversity in the e

300 7% of the adults which remained in the North Atlantic year-round.