ライフサイエンスコーパス: Pacific

1 , Europe, Eastern Mediterranean, and Western Pacific).

2 rage of 0.13 (+/-0.05, n = 8) in the central Pacific.

3 haped the history of human settlement in the Pacific.

4 ficant threats to other parts of the western Pacific.

5 part by changes in heat flux from the North Pacific.

6 b-Saharan Africa and 17.1% from Asia and the Pacific.

7 on around New Caledonia in the western South Pacific.

8 undances than similar species in the western Pacific.

9 iance measurements over the tropical Eastern Pacific.

10 l generally greater in the Atlantic than the Pacific.

11 d mounding corals that form reefs across the Pacific.

12 nd detect a cryptic Acroporid species in the Pacific.

13 with the phasing of human dispersal into the Pacific.

14 future, especially in the eastern equatorial Pacific.

15 mation on N(2)O variability across the South Pacific.

16 abyssicola-the voracious predator from North Pacific.

17 cale of a temperate reef in the northeastern Pacific.

18 resenting the whole of the Central Indo-West Pacific.

19 alth risks in developing regions of the Asia-Pacific.

20 entral Asia (3.2%), Africa (2.1%), East Asia/Pacific (1.1%), and the Middle East (0.6%).

21 as as follows: Africa-Middle East 3.0%, Asia-Pacific 21.4%, Europe 48.2%, Latin America 12.1%, and No

22 orth Africa, 9.9% (6.0%-14.6%); Asia and the Pacific, 9.8% (8.7%-11.0%); Eastern and Southern Africa,

23 Pacific acroporids can also be genotyped using a subset

24 in the upper ocean in the eastern equatorial Pacific across different scenarios of biological iron up

25 c El Nino events, and weakening of the North Pacific Aleutian Low Circulation.

26 ue-like bias in the central-eastern tropical Pacific and a warm bias beneath the marine stratocumulus

27 a Holocene teleconnection between the North Pacific and Arctic.

28 fied water vapor transport from the tropical Pacific and Atlantic increased high-altitude atmospheric

29 st decades, associating with warmer northern Pacific and Atlantic oceans, leading mostly to global su

30 PSH due to suppressed warming in the western Pacific and enhanced land-sea thermal contrast, leading

31 Despite these reductions, only the Western Pacific and European regions and 25 countries (most of w

32 ilar high-resolution records from across the Pacific and in the Southern Ocean.

33 pper-mantle depths, the boundary between the Pacific and North American plates is off-centered from t

34 ons in the tropical North Atlantic and North Pacific and significantly correlated to the variability

35 onal-interannual variability in the tropical Pacific and substantial efforts have been dedicated to p

36 tality and hospital admission between Maori, Pacific, and European patients with type 2 diabetes in A

37 se-specific clinical outcomes between Maori, Pacific, and European people remain unclear.

38 malies in global oceans outside the tropical Pacific, and significant anomalies of land surface air t

39 , and notably in the northern and equatorial Pacific, and the sub-polar gyre south of Greenland.

40 Asia-Pacific (APAC) has been the world's most dynamic emergin

41 argest decrease occurred in high-income Asia Pacific (APC = -2.88% [-3.58 to -2.18%]).

42 -control study conducted in New Caledonia, a Pacific archipelago with one of the highest recorded thy

43 es, using a long-term experimental test in a Pacific archipelago.

44 Ice Sheet retreat and instead implicates the Pacific as an early part of a cascade of dynamic climate

45 undisturbed waters (for example, the Central Pacific Basin) or in cold waters subject to high human p

46 rsors into the decadal-scale variance of the Pacific basin, accounting for the largest fraction of th

47 stward propagating mesoscale eddies from the Pacific basin.

48 gh long-read sequencing technologies such as Pacific Biosciences (PacBio) and Oxford Nanopore Technol

49 y using accurate Illumina data and long-read Pacific Biosciences (PacBio) data from all related indiv

50 The recently introduced Pacific Biosciences (PacBio) HiFi sequencing technology

51 t-read Illumina RNA sequencing and long-read Pacific Biosciences (PacBio) isoform sequencing (Iso-seq

52 cancer patients using Illumina/10x Genomics, Pacific Biosciences (PacBio), and Oxford Nanopore Techno

53 Long-read sequencing from Pacific Biosciences and NGS barcoding from 10x Genomics

54 In this study, we applied LRS platforms from Pacific Biosciences and Oxford Nanopore Technologies to

55 the set of recently generated long accurate Pacific Biosciences HiFi reads.

56 mparison of Oxford Nanopore Technologies and Pacific Biosciences phased assemblies identified 154 reg

57 icated species, fig (Ficus carica L.), using Pacific Biosciences single-molecule, real-time sequencin

58 whole genome sequencing was performed using Pacific Biosciences SMRT sequencing to determine the gen

59 Pacific Biosciences SMRT sequencing was used to investig

60 A decrease in the frequency of two southeast Pacific blue whale song types was examined over decades,

61 mechanism of foraging behaviors in the Indo-Pacific bottlenose dolphin (Tursiops aduncus) population

62 oxygen minimum zones (OMZs) of the tropical Pacific but the impacts of El Nino cycles on this key so

63 reviously been reported in the central South Pacific but we have identified a distinct lineage from t

64 soon and typhoon activities over the western Pacific, but future projections of its changes remain hu

65 ropean theaters of World War II, that of the Pacific campaign remains undescribed.

66 ics across marine ecosystem in the Northeast Pacific can help elucidate the magnitude of assemblage s

67 Longer telomeres in indigenous Maori and Pacific children may reflect the heritability of telomer

68 ations declined by 79% and 67% for Maori and Pacific children, respectively, between 2006 and 2015.

69 mphibian hosts representing two species (the Pacific chorus frog, Pseudacris regilla and the Californ

70 coincident with a documented shift in North Pacific circulation involving the Aleutian Low at ~4 ka,

71 IOD variability and persistent tropical Indo-Pacific climate coupling-may have implications for impro

72 es apparently began around a 1988/1989 North Pacific climate shift that was marked by abrupt northeas

73 coast flooding 500 km alongshore the Mexican Pacific coast and up to 6 km inland.

74 t great tsunamis do not occur on the Mexican Pacific coast cannot be sustained.

75 ndividuals from 17 island populations and 15 Pacific coast Native American groups.

76 ty located in the town of Guapi in the South Pacific Coast of Colombia.

77 at earthquakes and tsunamis have whipped the Pacific coast of Mexico in the past.

78 o a United States seaport from a port on the Pacific coast of South America.

79 Along the Pacific coast, upwelling brings subsurface waters with l

80 nths in 2013 along the entire North American Pacific coast.

81 species distributed along the North American Pacific coast.

82 al drivers are statistically significant for Pacific cod and walleye pollock recruitment, (c) separat

83 8.5), end-of-century (2075-2100) pollock and Pacific cod fisheries collapse in >70% and >35% of all s

84 We screened an Asian-Pacific cohort for CANVAS and identified a novel RFC1 re

85 also modulates the strength of the tropical-Pacific cold tongue.

86 etabolic immune response of WS-infected Indo-Pacific corals.

87 nean and Africa, southeast Asia, and western Pacific), country income (low, middle, high) and income

88 Indo-Pacific coupling was characterized by weak interannual v

89 Although, the Pacific crabapple, Malus fusca, is a hardy and disease r

90 Bindin in the East Pacific D. mexicanum, the West Atlantic D. antillarum, t

91 the East Atlantic D. africanum, and the Indo-Pacific D. paucispinum also evolves slowly under purifyi

92 oling in Eurasia is likely influenced by the Pacific Decadal Oscillation (PDO) and Siberian high (SH)

93 l and ecological conditions mapping onto the Pacific Decadal Oscillation (PDO) index and North Pacifi

94 w frequency climate variability, such as the Pacific Decadal Oscillation (PDO), are poorly understood

95 ENSO), North Atlantic Oscillation (NAO), and Pacific Decadal Oscillation (PDO).

96 ecadal shifts were found to be driven by the Pacific Decadal Oscillation (PDO).

97 The Pacific Decadal Oscillation index showed a positive corr

98 such as the El Nino/Southern Oscillation and Pacific Decadal Oscillation, and recently unprecedented

99 , the impacts of ENSO precursors on Tropical Pacific Decadal-scale Variability (TPDV) is still not we

100 ern Ocean deep mixing and enhanced influx of Pacific Deep Water into UCDW, inducing a water mass stru

101 are of high management concern in the North Pacific due to the active recreational fishery and their

102 de-wind anomalies in the Central and Eastern Pacific during boreal winter.

103 nlinear thermal damping cools the equatorial Pacific during El Nino but warms it during La Nina(15,16

104 devastating marine impacts in the Northeast Pacific during winter 2013/2014.

105 t to the modern/Holocene pattern, when South Pacific dust fluxes are thought to be primarily supporte

106 ndent skill as indices of regional northeast Pacific ecosystem variability.

107 ew sediment core from the Eastern Equatorial Pacific (EEP) Ocean spanning the last 180,000 years and

108 al Pacific trade winds, emergence of Central Pacific El Nino events, and weakening of the North Pacif

109 ITCZ air-sea column may also trigger Central Pacific El Nino events.

110 of El Nino (EN) events after ~11 ka: eastern Pacific EN, La Nina, coastal EN (COA), and central Pacif

111 ) events originating in the Eastern Tropical Pacific (ETP).

112 from the ETNP and the Eastern Tropical South Pacific (ETSP) ODZ, indicating arsenotrophy is a metabol

113 mumol/l O(2) ) in the Eastern Tropical South Pacific (ETSP) OMZ.

114 a, the Americas, Southeast Asia, the Western Pacific, Europe, and the Eastern Mediterranean) were ref

115 fishes from the Caribbean (Belize) and Indo-Pacific (Fiji) were attracted to cues from mangroves lea

116 ssroads of human population movements in the Pacific for the past three millennia.

117 ving eastward and northward toward the Great Pacific Garbage Patch.

118 e period 1918-2018 (across 23 different Asia-Pacific geopolitical entities).

119 ting oxic sediment of the oligotrophic South Pacific Gyre (SPG).

120 ic Decadal Oscillation (PDO) index and North Pacific Gyre Oscillation (NPGO) index have changed over

121 Regionally, the Western Pacific had the highest need of rehabilitation services

122 yptic lineages within Dall's, spectacled and Pacific harbor porpoises suggest a richer evolutionary h

123 ults from a prolonged weakening of the North Pacific High-Pressure System.

124 cific Ocean contribute to the weakened North Pacific High.

125 located on Axial Seamount in the North-East Pacific, in the Urashima field on the southern Mariana b

126 tly southern hemisphere species found in the Pacific, Indian and southern South Atlantic Oceans, comp

127 e in the SST power spectra in the equatorial Pacific is 1.9 K(2) on 1-5 year timescales, dominated by

128 We suggest that the deep Pacific is a site of respired carbon storage associated

129 y 13(th) and January 22(nd), 2017, the South Pacific Island of Moorea, French Polynesia experienced a

130 New Zealand, a geographically remote Pacific island with easily sealable borders, implemented

131 2.05-2.26) or American Indian/Alaska Native/Pacific Islander (aOR 1.26, 95% CI 1.05-1.52) vs. White

132 r these groups and the non-Hispanic Asian or Pacific Islander (NHAPI) population.

133 Hispanic (odds ratio [OR], 1.58), Asian or Pacific Islander (OR, 3.51), and Native American (OR, 5.

134 panics (n = 106), Blacks (n = 50), Asian and Pacific Islander Americans (API, n = 27) and Other (n =

135 African American, white, Hispanic, and Asian/Pacific Islander health plan members who were 51-56 year

136 Conversely, Asian or Pacific Islander race was associated with progression fr

137 sk factors for surgeon suicide include Asian/Pacific Islander race/ethnicity, older age, history of m

138 nfidence interval (CI): 0.06-3.16] and Asian/Pacific Islander were 438% more likely (OR = 5.38, 95% C

139 Asian or Pacific Islander, better socioeconomic status, lived in

140 ic, Native American, Bi- or Multi-racial and Pacific Islander.

141 Latina/Hispanic > Non-Hispanic White > Asian/Pacific Islander/Other; p < 0.01), with higher levels of

142 /Black, Hispanic/Latino, and Native Hawaiian/Pacific Islander; 2) discuss measurement challenges rela

143 is B (CHB) screening among at-risk Asian and Pacific Islanders (API).

144 ican Americans, whites, Hispanics, and Asian/Pacific Islanders who were 51-56 years old.

145 ng Black/African Americans, Hispanic/Latinx, Pacific Islanders, and American Indians, diminishes as i

146 rity was observed with Hispanics, Asians and Pacific Islanders, and Native Americans at a higher risk

147 A higher proportion of Asians/Pacific Islanders/Hawaiians carried the ADH1B*2 allele (

148 nd tempo of human dispersal to the far-flung Pacific Islands has been a source of fascination for cen

149 r, such as countries in Africa and Asia, the Pacific Islands, and parts of South America, often becom

150 in the tropical Americas and on Atlantic and Pacific Islands.

151 astal basins of the Japan Sea, and the North Pacific Islands.

152 nts in other PICTs or regions outside of the Pacific islands.

153 nal timescales from both the North and South Pacific, known as "precursors" of the El Nino Southern O

154 In the Northeast Pacific, large-scale climate patterns such as the El Nin

155 ), beyond simple vicariance of Caribbean and Pacific lineages, are needed to better understand the ev

156 Invasive Indo-Pacific lionfish Pterois volitans/miles have become well

157 f TUTTs between the North Atlantic and North Pacific makes the TC activity indices over the two basin

158 res of the unprecedented 2014-2016 northeast Pacific marine heatwave to understand the potential caus

159 intensity and longevity of summertime North Pacific marine heatwaves.

160 and secondarily to the positive phase of the Pacific Meridional Mode (PMM).

161 nstraints on the displacement process of the Pacific mid-ocean ridge basalt (MORB)-type mantle by the

162 how that dissolved iron is cycled rapidly in Pacific mode and intermediate water and accumulates at a

163 individuals sampled across the tropical Indo-Pacific, morphological information, and three newly asse

164 The arms race between tetrodotoxin-bearing Pacific newts (Taricha) and their garter snake predators

165 In U.S. Pacific Northwest coho salmon (Oncorhynchus kisutch), st

166 In 2013, the Pacific Northwest National Laboratory led a geologic car

167 lowed for the adaptation of the virus to the Pacific Northwest of the USA.

168 navirus SARS-CoV-2 was first detected in the Pacific Northwest region of the United States in January

169 ow-dependent Yakima River Basin (YRB) in the Pacific Northwest United States.

170 n stocks of major tidal wetland types in the Pacific Northwest, United States.

171 the drought sensitivity of vegetation in the Pacific Northwest, USA, as the percent reduction in vege

172 s of an integrated health care system in the Pacific Northwest.

173 U.S. Interior West and smallest in the mesic Pacific Northwest.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

188 ed heterotrophic unicellular eukaryotes from Pacific Ocean samples.

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

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

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

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

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

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

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

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

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

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

199 many marine mammal species in the Northeast Pacific Ocean.

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

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

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

203 amination in white sharks from the Northeast Pacific Ocean.

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

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

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

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

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

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

210 ical crossroads between the Arctic and North Pacific Oceans.

211 e interconnectedness of the Arctic and North Pacific on multimillennial timescales, and are consisten

212 c EN, La Nina, coastal EN (COA), and central Pacific or Modoki EN (CP).

213 he cleaner shrimp A. longicarpus in the Indo-Pacific, our study highlights that although cleaning int

214 pth profiles from the Eastern Tropical North Pacific Oxygen Deficient Zone (ETNP ODZ) where Prochloro

215 ng particles from the eastern tropical North Pacific oxygen-deficient zone and that some microbially

216 g four shell colors full-sib families of the Pacific oyster Crassostrea gigas, we systematically iden

217 e of a full-length TIR-STING fusion from the Pacific oyster Crassostrea gigas.

218 Specimens of the Pacific oyster Magallana gigas, an oyster well known for

219 nt findings of mud blisters on the shells of Pacific oysters (Crassostrea gigas Thunberg) in Washingt

220 lychaete causing these blisters, we obtained Pacific oysters from two locations in Puget Sound and ex

221 herpesvirus 1 (OsHV-1) cause high losses of Pacific oysters globally, including in Tomales Bay, Cali

222 d heat transport from low latitudes in North Pacific paleoclimate.

223 report aerodynamic forces and kinematics of Pacific parrotlets (Forpus coelestis) during short, fora

224 ehensive and Progressive Agreement for Trans-Pacific Partnership'.

225 s) across the three ethnic groups, Maori and Pacific patients had consistently higher hospital admiss

226 Maori but not Pacific patients had higher adjusted IRRs for all-cause

227 the associated differences between Maori and Pacific patients is also needed.

228 (15.7%) were Maori, and 12 044 (26.7%) were Pacific patients.

229 gov NCT02960230.FUNDINGThe V Foundation, the Pacific Pediatric Neuro-Oncology Consortium Foundation,

230 Within the Pacific Pediatric Neuro-Oncology Consortium, we assessed

231 alth outcomes have persisted among Maori and Pacific people with type 2 diabetes for more than 20 yea

232 Details of Pacific plate subduction under the Japan Sea and associa

233 from foraging to migration in the Northeast Pacific population.

234 ercial significance in their native northern Pacific range and in regions to which they have been int

235 dances from four ecoregions in the Northeast Pacific ranging from subarctic to subtropical: the Gulf

236 In the eastern North Pacific, recovering sea otters are transforming coastal

237 ease COVID-19 restrictions: five in the Asia Pacific region (ie, Hong Kong [Special Administrative Re

238 studies were conducted in the East Asia and Pacific region (n = 20) followed by South Asia (n = 7).

239 In 2015, the Western Pacific region had the largest share of global cases of

240 The Asia-Pacific region represents the largest share (93.8%) of g

241 y in a middle-income country in the Asia and Pacific region to show the effect of PCV on pneumonia, f

242 i, is a major cause of fever across the Asia Pacific region with more than a billion people at risk.

243 ne grasslands-that are unmatched in the Asia-Pacific region(4,5), it is a globally recognized centre

244 trongly with high certainty (all in the Indo-Pacific region) and seven were declining strongly but wi

245 patients (94.8%) were enrolled from the Asia-Pacific region, 684 (4.5%) from the Americas, and 120 (0

246 ast decade has spread into Europe, Asia, the Pacific Region, and the Americas.

247 ma abdominalis in the poorly known Southeast Pacific region, with samples spanning an ocean gradient

248 America, South America, Europe, and the Asia-Pacific region.

249 America, South America, Europe, and the Asia-Pacific region.

250 970 000; 5%) of whom resided in the Asia and Pacific region.

251 ain a panoptic view of scattering across the Pacific region.

252 es of adverse pregnancy outcomes in the Asia-Pacific region.

253 scarce for the effect of PCV in the Asia and Pacific region.

254 Here we show for the Pacific Rim an international approach how to data mine a

255 warms, as on the Gofar transform of the East Pacific Rise and the Blanco Ridge in the northeast Pacif

256 The ecosystems supporting Pacific salmon (Oncorhynchus spp.) are changing rapidly

257 We highlight widespread declines in Pacific salmon size based on 60 years of measurements fr

258 Here, using industrial-era Indo-Pacific sea surface temperature (SST) as training data,

259 -term chlorophyll enhancements around 17% of Pacific seamounts and 45% of shallow (< 100 m) seamounts

260 ignificant ice mass loss acceleration in the Pacific sector and deceleration in the Atlantic-Indian S

261 ions may mask El Nino warming at our central Pacific site, potentially obscuring a volcano-El Nino co

262 achine learning model using data from 2 Asia-Pacific sites (Singapore and New Zealand; n = 399).

263 a frequency decline in the scarcer southeast Pacific song type n.1 between 1970 to 2014, revealing th

264 ers for the more common song type (southeast Pacific song type n.2) between 1997 to 2017.

265 s from 14 European, North American, and Asia-Pacific study groups of the Ponte di Legno group were in

266 orth American study groups, and 20 from Asia-Pacific study groups).

267 to ~80% of the dust deposition in the South Pacific Subantarctic Zone via efficient circum-Antarctic

268 higher for longlines fished inside the North Pacific Subtropical Convergence Zone (versus outside) an

269 of metatranscriptomes collected in the North Pacific Subtropical Gyre (NPSG) to examine how in situ p

270 es of populations of E. huxleyi in the North Pacific Subtropical Gyre to shifts in the nutrient envir

271 of 16S rRNA genes in the oligotrophic North Pacific Subtropical Gyre.

272 coastal upwelling to the oligotrophic South Pacific Subtropical Gyre.

273 a into the nutrient-poor waters of the North Pacific Subtropical Gyre.

274 The western North Pacific Subtropical High (WNPSH) is a key circulation sy

275 c carbon (DIC) concentration, surmising that Pacific surface-ocean DIC increased by [Formula: see tex

276 cribed species plus an unknown central South Pacific taxon.

277 dynamical heating (NDH) along the equatorial Pacific thermocline.

278 ated fossil corals from the central tropical Pacific to gauge ENSO's response to large volcanic erupt

279 Ventilation of the intermediate-depth North Pacific tracks strength of the Asian monsoon, supporting

280 the 21st-century intensification of Central Pacific trade winds, emergence of Central Pacific El Nin

281 " has been historically endorsed by the Asia-Pacific treatment algorithm as well as by the recent Ita

282 rates in the control arm are similar to the PACIFIC trial.

283 bay in American Samoa, namely the 2009 South Pacific Tsunami and the 1960 Great Chilean Earthquake Ts

284 kness and both El Nino amplitude and central Pacific variability.

285 The Pacific Walker Circulation (PWC) fluctuates on interannu

286 rogressive orbitally-driven weakening of the Pacific Walker Circulation as contributing to this chang

287 hows that El Nino-likeness of the equatorial-Pacific warming pattern is linearly related to ENSO ampl

288 te shift that was marked by abrupt northeast Pacific warming, declining temporal variance in the Aleu

289 tentially increasing transport of warm North Pacific water to the Arctic through the Bering Strait.

290 W), toward Nd isotope values more typical of Pacific waters.

291 ng on a natural experiment in the equatorial Pacific, we track individual coral colonies at sites spa

292 ion in the wild (Chiloe Island, Southeastern Pacific), where populations of the two parents exist sym

293 yield and oxidative stability of lipids from Pacific white shrimp (Litopenaeus vannamei) cephalothora

294 20%-80%) on quality and melanosis in chilled Pacific white shrimp (Litopenaeus vannamei) under O(2) c

295 Inhibition of Pacific white shrimp polyphenoloxidase (PPO) with Chamua

296 When Pacific white shrimp were treated with GLE-S at differen

297 Pacific white shrimp with prior pulsed electric field (P

298 n or toxicity was observed when L. vannamei (Pacific whiteleg shrimp) were fed mealworm biomass grown

299 l cyclone (TC) season over the western North Pacific (WNP) underwent two extreme situations: 18 TCs o

300 sum and D. savignyi overlap in the Indo-West Pacific, yet their bindins show no evidence of positive