ライフサイエンスコーパス: Pacific

1 g corals in shallow exposed reefs across the Pacific.

2 ty Provinces (LLSVPs) beneath Africa and the Pacific.

3 tions over other remote oceanic areas beyond Pacific.

4 s reports across 4 countries in Asia and the Pacific.

5 at enables anomalous warm SST in the central Pacific.

6 e in feedback occurring in the tropical East Pacific.

7 g rapidly the surface warming in the eastern Pacific.

8 mmercial fish catch across the pelagic North Pacific.

9 n HSV-2 in the Americas, Europe, and Western Pacific.

10 tent atmospheric ridging system in the North Pacific.

11 ial westerly wind anomalies over the western Pacific.

12 the LGM in the New Zealand sector of the SW Pacific.

13 e worldwide, especially in the western North Pacific.

14 ll -induced climate feedback in the tropical Pacific.

15 ry Study on Men and Violence in Asia and the Pacific.

16 d, a remote, uninhabited island in the South Pacific.

17 ncurrent super El Nino event in the tropical Pacific.

18 ersal in three general directions: (1) South Pacific, (2) eastern Atlantic and Mediterranean Sea and

19 ate iron (measured in the eastern equatorial Pacific(30)) is bioavailable.

20 Our results suggest that the equatorial Pacific acts as a nonlinear amplifier that allows global

21 berian air mass was greater than that of the Pacific air mass during geomagnetic reversals in marine

22 ad trends were less evident across the North Pacific, although regions were identified across the Sal

23 t effect of local oxygenic photosynthesis on Pacific AMZ biogeochemical cycling.

24 ed water from 5 m depth in the central North Pacific and amended duplicate 20 liter polycarbonate car

25 and the timing of meltwater discharge to the Pacific and Arctic oceans.

26 urface temperatures (SSTs) over the tropical Pacific and Atlantic are used to assess the role of trop

27 ed precipitation over the western equatorial Pacific and Atlantic.

28 n rates suggests that splits between eastern Pacific and Caribbean biota, dated on the assumption of

29 The most recent separation between eastern Pacific and Caribbean extant clades occurred at 4.90 Ma,

30 olume (WWV) variability along the equatorial Pacific and El Nino-Southern Oscillation (ENSO) variabil

31 hronous with the warming of western tropical Pacific and Indian Ocean sea surface temperatures.

32 microbial loads over the tropical Atlantic, Pacific and Indian oceans and propose islands as steppin

33 is 60-90 years.Deep waters of the Atlantic, Pacific and Indian Oceans upwell in the Southern Oceanbu

34 trations found in the open-ocean OMZs of the Pacific and Indian Oceans.

35 usally linked to the warming of the tropical Pacific and Indian Oceans.

36 severity, a full-latitude section of the mid-Pacific and near-equatorial region of the east Pacific w

37 e of deep water mass properties in the North Pacific and North Atlantic Ocean.

38 per 100000 person-years were 52 in the Asia-Pacific and ranged between 180 and 280 in the other regi

39 s that will be most impacted by shoaling are Pacific and southern bluefin tunas-habitat compression i

40 institutions in 14 countries in Europe, Asia-Pacific, and North America.

41 d to cause outbreaks in the Americas and the Pacific, and the first outbreaks were reported in contin

42 ergence of double-track volcanism across the Pacific; and finally, secondary pyroxenite, which is for

43 This topic has not been investigated for Pacific Arctic beluga whales (Delphinapterus leucas) tha

44 in the context of their rapidly transforming Pacific Arctic ecosystem, suggesting flexible responses

45 In the Pacific-Arctic domain, fungal parasitism is linked to li

46 Cooler SSTs in the northeast Pacific are also associated with more summertime heatwav

47 ons spanning from the western to the eastern Pacific are captured by the coupled model.

48 7)Cs levels in seawater in the eastern North Pacific are equivalent to fallout background levels of (

49 geographic scenario that shows the Indo-West Pacific as the probable ancestral area of the genus Hipp

50 on samples from the tropical and subtropical Pacific, Atlantic and Indian Oceans were collected durin

51 a tropic-ward flow on the ocean floor of the Pacific, Atlantic and Indian Oceans.

52 mperature, located in the central equatorial Pacific, based on oxygen isotopic time series from Taiwa

53 mergence at northern Shatsky Rise, Northwest Pacific, based on the integration of unique micropalaeon

54 ng laminated sediments and compare them with Pacific basin-scale and regional indices of ocean climat

55 tivity by coupling the DNA walking system to Pacific Bioscience(R) Next-generation sequencing technol

56 ombines strand-specific Illumina RNA-seq and Pacific Biosciences (PacBio) full-length cDNAs to identi

57 We generated Pacific Biosciences (PacBio) long-read data of the genom

58 complete eukaryotic chromosomes using either Pacific Biosciences (PacBio) or Oxford Nanopore technolo

59 e single-molecule sequencing long reads from Pacific Biosciences (PacBio) to determine the detailed s

60 real-time (SMRT) sequencing technology from Pacific Biosciences (PacBio) to sequence eight Bacterial

61 Pacific Biosciences and Oxford Nanopore increase through

62 Long-read sequencing technologies such as Pacific Biosciences and Oxford Nanopore MinION are capab

63 read depth of 31X, the assemblies from both Pacific Biosciences and Oxford Nanopore MinION show exce

64 rid assembly strategy utilizing Illumina and Pacific Biosciences sequencing technologies produced a d

65 Using Pacific Biosciences single-molecule long-read isoform se

66 n whole-genome sequencing using Illumina and Pacific Biosciences technologies, and compared with publ

67 Many successful assembly applications of the Pacific Biosciences technology have been reported rangin

68 amplified isoform sequencing technique from Pacific Biosciences to characterize the lytic transcript

69 of Taxol linked to the drug-like fluorophore Pacific Blue (PB).

70 projected for the entire geographic range of Pacific bluefin tuna and for the spawning region of sout

71 tially influence resource partitioning among Pacific bluefin, bigeye, yellowfin, and skipjack tunas i

72 city provinces (LLSVPs) under Africa and the Pacific, but is much smaller.

73 een detected in some regions, e.g. the North Pacific, but there is no agreed global signal.

74 a highly disconnected distribution (Eastern Pacific, Caribbean, Atlantic, Mediterranean, Madagascar,

75 nd East South Central census regions (aOR vs Pacific census region = 5.57, P < .001; aOR = 3.58, P <

76 (lower in West South Central, Mountain, and Pacific census regions), and receptor status (lower in p

77 ity of eight parasite taxa observed in 3,571 Pacific chorus frogs (Pseudacris regilla) surveyed from

78 ter pressure patterns over the Central North Pacific (CNP) imparts a significant signature upon the s

79 habitat shift from the oceanic central North Pacific (CNP) to the neritic east Pacific region near th

80 Native to the Pacific coast of Asia, it is now well-established in Nor

81 The Pacific coast of North America is an excellent test case

82 Rickettsia philipii, in a population of the Pacific Coast tick, Dermacentor occidentalis in Mendocin

83 s, Ostreococcus maxima occurred in the North Pacific coastal upwelling for OI (36 713 +/- 1485 copies

84 entification of Atlantic cod (Gadus morhua), Pacific cod (Gadus macrocephalus), Alaska pollock (Gadus

85 gadoid species: Atlantic cod (Gadus morhua), Pacific cod (Gadus macrocephalus), Alaska pollock (Thera

86 ractinian reefs in the Central and Northeast Pacific, combined with the shallow aragonite saturation

87 e amount of iAs as a mean Tribal, Asian, and Pacific consumer is exposed to from rice.

88 st 21 shark species, from both Caribbean and Pacific Coral Sea water samples, whose geographical patt

89 cean acts as a key pacemaker for the western Pacific decadal climate variability.

90 is modulated by variability relating to the Pacific Decadal Oscillation (PDO) and the Arctic Oscilla

91 tial for more powerful typhoons) in negative Pacific Decadal Oscillation (PDO) years, as well as with

92 ts during positive or negative phases of the Pacific Decadal Oscillation (PDO), as well as highlight

93 ds from North China, plausibly driven by the Pacific Decadal Oscillation (PDO).

94 id is strongly related to warm phases of the Pacific Decadal Oscillation and the Oceanic Nino Index,

95 trusions into the South China Sea echoed the Pacific Decadal Oscillation, the intrusion northeast of

96 overturning and the loss of the modern North Pacific Deep Water (NPDW) mass in climate models of the

97 faster change in Pb isotope ratios of North Pacific deep water below the WSAG versus the NPSG.

98 Similarly, mantle beneath the Pacific does not spread to surrounding regions of the pl

99 gtime zonal winds in the high latitude South Pacific drive western Ross Sea autumn sea ice conditions

100 ces in child development using the East Asia-Pacific Early Child Development Scales (EAP-ECDS) in six

101 tory, upper trophic level predators in North Pacific ecosystems.

102 last deglaciation in the eastern equatorial Pacific (EEP) using benthic and planktonic foraminiferal

103 Central Pacific El Nino events may become more frequent in comin

104 orcing may be driving an increase in central Pacific El Nino-Southern Oscillation variability and/or

105 by 2 degrees C in response to the developing Pacific El Nino.

106 cal cyclones (TCs) pose in the eastern North Pacific (ENP) and the importance of improving our unders

107 odel's natural modulations; however, central Pacific ENSO amplitude significantly decreases, to an ex

108 Changes in eastern Pacific ENSO SST metrics due to climate change are secon

109 ific teleconnection - the East Pacific/North Pacific (EP/NP) pattern - and United States (US) tempera

110 co, but will increase over the western North Pacific, especially that hits Korea and Japan.

111 The indigenous populations of the South Pacific experience a high burden of rheumatic heart dise

112 ry Study on Men and Violence in Asia and the Pacific, exploring the pathways between different forms

113 ca and drives westerly wind anomalies in the Pacific favouring an El Nino response.

114 her amplified by air-sea interactions in the Pacific, favouring an El Nino-like response.El Nino tend

115 r with a primary colonization in the eastern Pacific followed by a radiation into the western Atlanti

116 h its emergence in Yap Island in the western Pacific, followed in 2013-14 by a larger epidemic in Fre

117 trials) conducted in Africa and the Western Pacific from 1996-2015.

118 nteraction over the tropical central eastern Pacific from a new perspective, climate network.

119 e western Indian Ocean, but also the western Pacific from Japan to Australia is constantly increasing

120 winds converge towards the subtropical North Pacific from the tropics, leading to anomalous cyclonic

121 In addition, the Indo-West Pacific genus Alcyonohippolyte was included.

122 and marine sedimentation rates in the South Pacific Gyre (SPG) provide a unique opportunity to exami

123 rotectant ability between FPHs produced from Pacific hake muscle within the range of conditions studi

124 Sardinops sagax and Merluccius productus (Pacific hake) exhibited an unprecedented early and north

125 Ecosystem dynamics in the Northeast Pacific have been suggested to be predominately bottom-u

126 butions of sperm whale cultural clans in the Pacific have likely changed mitochondrial genetic geogra

127 ythm Association, Heart Rhythm Society, Asia-Pacific Heart Rhythm Society, and Sociedad Latinoamerica

128 North Pacific hydroclimate is dominated by the Aleutian Low, a

129 ficiency of iron recycling in the equatorial Pacific implies the evolution of ecosystem-level mechani

130 n thermocline conditions in tropical western Pacific in early 2015, reigniting rapidly the surface wa

131 epted multiple snapshots of BC profiles over Pacific in various seasons, and revealed a 2 to 5 times

132 pacemaker of the biennial variability in the Pacific including that in ENSO and the PSHs during recen

133 that warmer-than-usual SSTs in the Tropical Pacific (including El Nino events) and Atlantic were the

134 perton Zone (CCZ, abyssal eastern equatorial Pacific) is the focus of a major research effort linked

135 pporting data for young lavas from southwest Pacific island arcs, Eyjafjallajokull, Iceland, and Terc

136 tal cities and the habitability of low-lying Pacific island nations.

137 %), 2310 black (30.9%), 233 Asian (3.1%), 93 Pacific Islander (1.2%), and 40 American Indian/Alaskan

138 .5) patients but remained elevated for Asian/Pacific Islander (106.4) and "other" (104.7; p < 0.001)

139 confidence interval [CI], 1.14-1.75), Asian/Pacific Islander ethnicity (RR to white, 1.7; 95% CI, 1.

140 erican Indian/Alaskan Native/Native Hawaiian/Pacific Islander fellows decreased from 15 (1.0%) to sev

141 for all cancer sites, and Asian American and Pacific Islander patients had the highest, compared with

142 For Asian/Pacific Islander women, the hospitalization rate was 24%

143 6.5 [0.73] years), of whom 2 (3%) were Asian/Pacific Islander, 23 (29%) were black/African American,

144 (6.6%) were Hispanic, 424 (5.3%) were Asian/Pacific Islander, 63 (0.8%) were Native American, and 22

145 Hispanic black, Hispanic, Asian American and Pacific Islander, and separately each for Chinese, Japan

146 panic, and 90.7% (95% CI 87.0-93.5) in Asian/Pacific Islander/American Indian/Alaska Native patients.

147 R rates in white, black, Hispanic, and Asian/Pacific Islander/American Indian/Alaska Native patients;

148 ] black, 1,187 [6%] Hispanic, 348 [2%] Asian/Pacific Islander/American Indian/Alaska Native, and 2,36

149 iduals (up to 3.9% per year), and Asians and Pacific Islanders (up to 2.6% per year), mainly because

150 duals, and 34 000 fewer deaths in Asians and Pacific Islanders aged 25-64 years.

151 pitalization rates among Hispanics and Asian/Pacific Islanders is needed.

152 cancer incidence remains highest among Asian/Pacific Islanders likely due to gene-environment interac

153 PCNSL incidence was higher in Asians/Pacific Islanders than non-Hispanic whites (aIRR = 2.09)

154 blacks, 1.57 (95% CI: 1.17, 2.09) for Asians/Pacific Islanders, 2.33 (95% CI: 0.93, 5.83) for America

155 an that among non-Hispanic blacks, Asians or Pacific Islanders, and Native Americans (P<0.05 for all

156 bal variation in susceptibility to T2D, with Pacific Islanders, Asian Indians, and Native Americans b

157 er cancer has been most frequent among Asian/Pacific Islanders, chiefly due to hepatitis B vertical t

158 dividuals, black individuals, and Asians and Pacific Islanders.

159 al reef fish communities at 38 US-affiliated Pacific islands that ranged in human presence from near

160 ntries (mostly in sub-Saharan Africa and the Pacific Islands) since a review in 2008.

161 Zika virus (ZIKAV) has spread throughout the Pacific islands, the Americas and Southeast Asia.

162 on-associated nitrogen inputs to the western Pacific, it has been suggested that even the open ocean

163 In North-eastern Pacific kelp forests, the starfish Pycnopodia helianthoi

164 e wind response to forcing over the tropical Pacific, leading to errors in thermocline feedback.

165 Subsequent viral spread in the Pacific led to a large outbreak in French Polynesia comm

166 We used humeri from juvenile North Pacific loggerhead turtles (Caretta caretta), animals th

167 ic conditions and coastal response along the Pacific margin, exposing many heavily populated regions

168 The northwest Pacific marginal seas are a primary center of phylogeogr

169 ridization of marine groups in the northwest Pacific marginal seas.

170 cross their broad range in the eastern North Pacific (NEP) and identified key environmental factors t

171 duration and rainstorm events related to the Pacific North American pattern (PNA) using a 2100-year-l

172 pical Pacific Ocean temperatures through the Pacific-North American (PNA) teleconnection pattern.

173 ces varying consistently with the springtime Pacific/North American (PNA) index.

174 tant North Pacific teleconnection - the East Pacific/North Pacific (EP/NP) pattern - and United State

175 in epidermal xenomas from flatfish from the Pacific Northwest [1].

176 ime series of genetic data, we show that the Pacific Northwest Coast exhibits genetic continuity for

177 The Pacific Northwest Coast proves an intriguing focus for t

178 from the Prince Rupert Harbour region of the Pacific Northwest region of British Columbia, Canada.

179 Here we examine CH4 emission dynamics in six Pacific Northwest U.S. reservoirs of varying trophic sta

180 Principal actors in the Pacific NW region of the U.S. (representing a progressiv

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

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

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

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

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

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

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

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

189 1-4 degrees C above normal) in the northeast Pacific Ocean during 2015-2016, we documented shifts in

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

213 oactivity tracer plume through the northeast Pacific Ocean.

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

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

216 rements along 137 degrees E in the northwest Pacific of 2004-2016, we show that the observed upper oc

217 Here we show in the Eastern Tropical North Pacific OMZ 70% of POC remineralization is due to microb

218 y the Tapes philippinarum, a species of Indo-Pacific origin.

219 near-surface winds associated with the North Pacific Oscillation (NPO) serve as a significant extratr

220 unlikely to be explained by the Interdecadal Pacific Oscillation.

221 e did two cross-sectional PET studies at the Pacific Parkinson's Research Centre in Vancouver, BC, Ca

222 r, a number of typhoons in the western North Pacific pass through the Luzon Strait into South China S

223 rance of other double volcanic tracks on the Pacific plate and a recent azimuthal change in the motio

224 ions; second, the recent azimuthal change in Pacific plate motion exposes high- and low-pressure melt

225 irst, mantle flow beneath the rapidly moving Pacific plate strongly tilts the Hawaiian plume and lead

226 The Tribal, Asian, and Pacific population exhibited the highest mean daily expo

227 The Tribal, Asian, and Pacific population exhibited the highest mean daily expo

228 us (ZIKV) outbreak in the Americas and South Pacific poses a significant burden on human health becau

229 330 families collected by the Stanford Asian Pacific Program in Hypertension and Insulin Resistance (

230 rapid deglacial radiocarbon changes in these Pacific records are coeval with changes in the Atlantic

231 ble to rates reported for other inshore Indo-Pacific reefs.

232 The World Health Organization (WHO) Western Pacific Region (WPR) has maintained its polio-free statu

233 ntibiotic resistance to H pylori in the Asia-Pacific region and to examine the relation between resis

234 The Asia-Pacific region has disparate hepatitis C virus (HCV) epi

235 HCV in the Asia-Pacific region is challenging because of the disparate e

236 tral North Pacific (CNP) to the neritic east Pacific region near the Baja California Peninsula (BCP)

237 uality across six countries in the east Asia-Pacific region were associated with improved performance

238 e main challenges encountered in the Western Pacific Region with both IPV introduction and the tOPV-b

239 ntres in Europe, North America, and the Asia Pacific region, aged 16 years or older and with newly di

240 s located in North America, Europe, the Asia-Pacific region, and Latin America.

241 ral encephalitis in children across the Asia-Pacific region, including in Vietnam, which has experien

242 cally dominated by the Indian Ocean-Southern Pacific region, marking a transition from lower-than-ave

243 , North America, South America, and the Asia-Pacific region.

244 efficacy of first-line regimens in the Asia-Pacific region.

245 Europe to 21% (95% CI, 9-35) in the Western Pacific region.

246 ainly in Europe, North America, and the Asia-Pacific region.

247 esistance in Helicobacter pylori in the Asia-Pacific region.

248 nd their use is highly prevalent in the Asia-Pacific region.

249 cation in six countries across the east Asia-Pacific region.

250 pora damicornis on fringing reefs around two Pacific remote islets with large seabird colonies.

251 gers an anticyclonic response over the North Pacific, resulting in significant drying over California

252 smically in the D'' layer beneath the circum-Pacific rim.

253 tions of the melting regime beneath the East Pacific Rise with our experimental results requires that

254 culturally and economically important group, Pacific salmon (Oncorhynchus spp.), experience site-spec

255 ation and heritable phenotypic plasticity in Pacific salmon embryos, we measured the developmental ra

256 ood size could alter stream habitats used by Pacific salmon for reproduction, with negative consequen

257 rdax (northern anchovy) and Sardinops sagax (Pacific sardine) larvae, which are normally summer spawn

258 be traced back to variations of the Atlantic/Pacific sea surface temperature gradient, external radia

259 s: warm tropical Atlantic and cold northeast Pacific sea surface temperatures (SSTs), as well as posi

260 ls, we further show that warming of tropical Pacific sea surface temperatures accounts for these chan

261 articularly based on variability in tropical Pacific Sea Surface Temperatures.

262 rise, but the instrumental record of central Pacific sea-surface temperatures is too short to detect

263 we show that the lack of coastal ice in the Pacific sector of Antarctica leads to major reductions i

264 ican Society for Reproductive Medicine, Asia Pacific Society of Human Genetics, British Society for G

265 antiretroviral therapy (ART) across the Asia-Pacific, South Africa, Europe, Latin, and North America.

266 The wind changes induce a subtropical North Pacific SST warming through wind-evaporation-SST effect,

267 ese results suggest that projected shifts of Pacific storm tracks over the 21st century would likely

268 rives during the cool season via midlatitude Pacific storm tracks, which may experience future shifts

269 of Crocosphaera over eight days in the North Pacific Subtropical Gyre (NPSG).

270 kg(-1)) extended throughout the entire North Pacific Subtropical Gyre (NPSG).

271 scillation (ENSO) and the variability in the Pacific subtropical highs (PSHs) have major impacts on s

272 Nitrate persists in eastern equatorial Pacific surface waters because phytoplankton growth fuel

273 ning relationship between an important North Pacific teleconnection - the East Pacific/North Pacific

274 Ocean conditions in the northeast Pacific that are associated with warm phases of these in

275 rise to enhanced biennial variability in the Pacific that may increase the occurrence frequency of se

276 eakened Walker circulation over the tropical Pacific that transports less moisture to the ASM region

277 n some mangrove forests in parts of the Indo-Pacific that will exacerbate other pressures.

278 from five previous studies in the equatorial Pacific to document the nonlinear relationship between c

279 reas), spring peepers (Pseudacris crucifer), Pacific treefrogs (P. regilla), leopard frogs (Lithobate

280 length in western toads, American toads, and Pacific treefrogs.

281 and women, aged 18-49 years, in Asia and the Pacific, using standardised population-based household s

282 ispheres are strongly influenced by tropical Pacific variability associated with the El Nino/Southern

283 amine several characteristics of the Western Pacific Warm Pool (WP) in the past thirty years of mixed

284 that depends on the strength of the western Pacific warm pool in a simple and effective fashion.

285 last 360,000 years from the southern Western Pacific Warm Pool with records from five previous studie

286 hypothesis that reef formation in the North Pacific was improbable.

287 rtion of Thaumarchaeota (4-54%) in temperate Pacific waters.

288 cific and near-equatorial region of the east Pacific were identified as representative regions for pr

289 akens the Aleutian low and subtropical North Pacific westerlies.

290 a larger epidemic in French Polynesia, south Pacific, where the first severe complications and non-ve

291 per ocean temperature bias in the equatorial Pacific, which becomes more intense with increasing lead

292 diative Forcing by current models over North Pacific, which further suggests that large uncertainties

293 increase in TC activity in the western North Pacific, which is owing to enhanced subtropical deep con

294 s an atmospheric teleconnection to the North Pacific, which weakens the Aleutian low and subtropical

295 The Pacific whiteleg shrimp, Litopenaeus vannamei, is the mo

296 polymetallic nodules in the Central Tropical Pacific will generate plumes of suspended sediment which

297 rd is consistent with intensification of the Pacific winter storm track in response to North Atlantic

298 gtime zonal winds in the high latitude South Pacific, with a lead-time of 5 months.

299 ariability of sBC* is seen over the Northern Pacific, with abundances varying consistently with the s

300 analysis suggests that the western tropical Pacific (WTP) sea surface temperature (SST) shows predom