ライフサイエンスコーパス: gulf

1 Western Hemisphere, the Gulf of Mexico (the Gulf).

2 in migration timing or intensity through the Gulf.

3 ulf of Mexico coast before flying across the Gulf.

4 ope with extreme temperatures in the Persian Gulf.

5 o discrete groups corresponding with Persian Gulf and Sea of Oman sites.

6 ems of the northeastern Arabia area (Arabian Gulf and Sea of Oman) and of these which ones are potent

7 extreme coral reefs in the southern Arabian Gulf and the nearby, but more environmentally benign, Gu

8 belonged to ITS2 rDNA type C3 in the Persian Gulf and type D1a in the Sea of Oman contradicting patte

9 l, results indicate the Ohio, South Atlantic Gulf, and Missouri Regions are the most likely to see ef

10 ments of high mixing ratios over the Arabian Gulf are adequately simulated, strong underprediction by

11 We show that assemblages in the Arabian Gulf are half as diverse and less than 25% as abundant a

12 ound discontinuously along the length of the Gulf at elevations of 3 to 26 m.

13 ses of RAD-Seq datasets resolved the classic Gulf-Atlantic coastal phylogeographic break, which was n

14 ational models that serve to bridge the wide gulf between a descriptive analysis and a formal theory

15 s hypothesis in humans is lacking, leaving a gulf between animal and human studies of the condition.

16 Despite the evolutionary gulf between plant and vertebrate genomes and encoded an

17 ies is less important in urban areas and the Gulf, but it is similar in importance to the uncertainty

18 stributions of benthic microorganisms in the Gulf can be constrained, and moreover, deviations from t

19 antial fraction of the East Coast (>18%) and Gulf Coast (>17%), and also parts of the West Coast wher

20 he 10 largest extreme events, whereas at the Gulf Coast and Caribbean TCs dominate.

21 ural details of an ancient settlement on the Gulf Coast of Florida without parallel in the Southeaste

22 spill in U.S. history, negatively impacting Gulf Coast residents and the surrounding ecosystem.

23 y shown in all inversion results include the Gulf Coast states, the San Francisco Bay Area in Califor

24 ome of an FLE, termed FLE-Am, present in the Gulf Coast tick, Amblyomma maculatum.

25 ocations, whereas along the Mexican Southern Gulf coast, the average contribution of tides over the l

26 (SCSC), a group of submarine springs at the Gulf Coast.

27 h and 12-month mortality were studied in the GULF-COAST, a prospective multicenter cohort of acute co

28 the late Cretaceous to Eocene strata on the Gulf Coastal Plain (United States).

29 the generic diversity nor composition of the Gulf Coastal Plain molluscan communities.

30 ntal conditions did not devastate the entire Gulf Coastal Plain, allowing molluscs to rapidly recolon

31 Beads and other objects made from gulf coastal shell were integral to the political econom

32 w that along the North American Atlantic and Gulf coasts the meridional distributions of dissolved in

33 t the county level along the US Atlantic and Gulf Coasts.

34 In the Gulf Cooperation Council states (United Arab Emirates, B

35 Persian Gulf corals had higher rates of survival at elevated tem

36 e compared sound levels produced by spawning Gulf Corvina (Cynoscion othonopterus) with simultaneous

37 Reports from Arabian Gulf countries have demonstrated emergence of novel meth

38 oration and low precipitation in the Persian Gulf, discharges from desalination plants (DPs) can lead

39 p plate boundary, the faulted margins of the Gulf display largely dip-slip extensional movement and a

40 The daily capacity of DPs in the Persian Gulf exceeds 11 million m(3) per day, which is approxima

41 Additionally, Persian Gulf hosts had fixed greater potential to mitigate oxida

42 large (63,000 km(2)), partially ice-covered gulf in the Canadian Arctic.

43 uture destructive earthquakes in the central Gulf is greater than in the sub-basins to the north and

44 samples from elsewhere, indicating that the Gulf is primed for oil biodegradation.

45 al-reef fish (50 specimens) from the Persian Gulf, Kharg Island (Iran), specifically Lethrinus microd

46 particles (NPs) and their bioavailability to Gulf killifish (Fundulus grandis) embryos, with the aim

47 e toxicant resistance has rapidly evolved in Gulf killifish (Fundulus grandis) that occupy polluted h

48 Gulf killifish embryos were exposed to dissolved Cu and

49 ustralis stands from native, introduced, and Gulf lineages to determine lineage-specific controls on

50 wer exposure to enemy attack than native and Gulf lineages.

51 Using data from detailed Gulf Long-term Follow-up ( GuLF) Study enrollment interv

52 We used data from the Gulf Long-term Follow-up Study, a cohort of workers and

53 ong 24,375 oil spill workers enrolled in the Gulf Long-Term Follow-up Study.

54 To minimize energetic costs, trans-Gulf migrants should stop over when they encounter cross

55 with regions in the Indian Ocean (e.g., the Gulf of Aden) than with the northern part of the basin.

56 c ranging from subarctic to subtropical: the Gulf of Alaska (1981-2017), British Columbia (2001-2017)

57 .7 nmol L(-1) d(-1) , p = 0.026) but not the Gulf of Alaska (8.8 +/- 4.0 versus 1.5 +/- 0.6, p > 0.05

58 lows since the beginning of sampling in the Gulf of Alaska and British Columbia, while in Oregon and

59 carbon and sedimentological results from the Gulf of Alaska document recurrent millennial-scale episo

60 ly half of the freshwater discharge into the Gulf of Alaska originates from landscapes draining glaci

61 ear history of human presence in the western Gulf of Alaska, but little understanding of how human fo

62 , and suspended and sinking particles in the Gulf of Aqaba (GOA), Red Sea.

63 The Gulf of Aqaba transform plate boundary is a source of de

64 netic shift at a barrier to dispersal in the Gulf of Bejaia, Eastern Algeria.

65 pth in Monterey Canyon and at 1,722 m in the Gulf of California (Mexico).

66 and the more marginal hotspots, such as the Gulf of California and the Equatorial area which are not

67 ated systems in the arid environments of the Gulf of California and Yemen.

68 Using the Gulf of California as case study, we assess the benefits

69 The analyses revealed that the Gulf of California fin whale population was founded ~2.3

70 d very low levels of genetic diversity among Gulf of California fin whales and a significant level of

71 ze and high degree of isolation implied that Gulf of California fin whales are vulnerable to the nega

72 ss the degree and timing of the isolation of Gulf of California fin whales in a population genetic an

73 outhern California and from 2004-2010 in the Gulf of California using autonomous acoustic recorders.

74 sin spreading center, at 2000 m depth in the Gulf of California, is overlain by a thick sedimentary c

75 dy of the biogeography of rocky reefs in the Gulf of California, Mexico (GOC), we collected a continu

76 The Gulf of California, Mexico is home to many cetacean spec

77 long and short triplets were dominant in the Gulf of California.

78 ed carbonate-hosted hydrothermal vent in the Gulf of California.

79 ~10 cm long) also occurred at 1,722 m in the Gulf of California.

80 the large-scale dieback of mangroves in the Gulf of Carpentaria in northern Australia.

81 n of iron monosulfides to iron oxides in the Gulf of Finland in spring, possibly explaining why botto

82 The highest densities were observed at Gulf of Finland sites with high rates of sulfate reducti

83 cubation of an intact sediment core from the Gulf of Finland with aerated overlying water.

84 miting oceanographic features, including the Gulf of Honduras gyre.

85 In the Gulf of Honduras, we use video observations to analyze >

86 Further downstream, in the Gulf of Lion, the intermediate heat and salt content wer

87 e of both rapid ocean warming throughout the Gulf of Maine and apparent changes in right whale migrat

88 y pronounced in the spring and summer in the Gulf of Maine and Georges Bank.

89 perature in the assessment and management of Gulf of Maine Atlantic cod caused overfishing.

90 howed that blue mussels have declined in the Gulf of Maine by >60% (range: 29-100%) at the site level

91 ed States, the iconic groundfish fishery for Gulf of Maine cod has endured several dramatic reduction

92 d that warming waters reduce growth rates in Gulf of Maine cod.

93 tic oceanographic processes that link to the Gulf of Maine ecosystem.

94 past decade, sea surface temperatures in the Gulf of Maine increased faster than 99% of the global oc

95 ank National Marine Sanctuary (SBNMS) in the Gulf of Maine is a historic fishing ground renowned for

96 owhere are those impacts greater than in the Gulf of Maine where North America's most valuable marine

97 together comprise one of seven areas in the Gulf of Maine where right whales seasonally congregate.

98 In the Gulf of Maine, the copepod Calanus finmarchicus co-occur

99 idal habitats, over the past 40 years in the Gulf of Maine, USA, one of the fastest warming regions i

100 tructure in response to rapid warming in the Gulf of Maine.

101 sel population abundance and dynamics in the Gulf of Maine.

102 and a simultaneous decrease in the northern Gulf of Maine.

103 Northeast Channel, Shelf Break, and Central Gulf of Maine.

104 lls and weathered crude oil samples from the Gulf of Mexico (collected after the Deepwater Horizon oi

105 rangian dynamics in a region occupied by the Gulf of Mexico (GoM) and adjacent portions of the Caribb

106 The northern Gulf of Mexico (GoM) is a region strongly influenced by

107 intense hurricane landfalls in the northern Gulf of Mexico (GOM) is within or outside the natural ra

108 baselines for petroleum contamination in the Gulf of Mexico (GoM) prior to this study.

109 mperature, and carbon dioxide (CO(2)) in the Gulf of Mexico (GoM) were compiled from the Surface Ocea

110 Mexican exclusive economic zone (EEZ) of the Gulf of Mexico (GoM), ranging between 1000 and > 3500 m

111 birds in eastern North America negotiate the Gulf of Mexico (GOM), where inclement weather coupled wi

112 five monitoring sites over two years in the Gulf of Mexico (GOM).

113 isease, such as the states located along the Gulf of Mexico (Gulf States), may be disadvantaged by li

114 seawater samples obtained from the northern Gulf of Mexico (NGoM) before, during, and after the 2010

115 We examined changes in northern Gulf of Mexico (nGOM) lionfish populations following the

116 eepwater Horizon Oil Spill (DWH) on northern Gulf of Mexico (nGoM) reef fish communities.

117 w formed in the water column of the northern Gulf of Mexico (nGoM), settled rapidly, and ultimately a

118 ion corridors in the Western Hemisphere, the Gulf of Mexico (the Gulf).

119 tive to coastal regions and estuaries of the Gulf of Mexico - habitats that routinely experience pron

120 bony fish and marine reptiles, from northern Gulf of Mexico - located about 500 km from the Chicxulub

121 is used to estimate hypoxia in the northern Gulf of Mexico across summers from 1985 to 2017.

122 Billfishes and tunas moved throughout the Gulf of Mexico and all species investigated (blue marlin

123 50% SPR during spring and autumn through the Gulf of Mexico and Atlantic coasts of the south-eastern

124 cal, biological, and economic aspects of the Gulf of Mexico and find that an ecosystem-wide reorganiz

125 tems in north Florida and across much of the Gulf of Mexico and south Atlantic coasts of the United S

126 n Hemisphere Warm Pool (WHWP) centred on the Gulf of Mexico and the Caribbean Sea.

127 s) inhabits the eastern equatorial Atlantic, Gulf of Mexico and western North and South Atlantic.

128 Salt domes of the Gulf of Mexico Basin typically exhibit extensive deposit

129 sand patties deposited in the swash zone on Gulf of Mexico beaches following the Deepwater Horizon o

130 a) forms nearly every summer in the northern Gulf of Mexico because of nutrient inputs from the Missi

131 ere detectable in non-oiled samples from the Gulf of Mexico but not in comparable samples from elsewh

132 column in the hypoxic region of the northern Gulf of Mexico by conducting on-deck incubation experime

133 ainson's Thrushes often stop on the northern Gulf of Mexico coast before flying across the Gulf.

134 Louisiana oyster harvesting areas along the Gulf of Mexico coast, USA.

135 ediction of oyster norovirus outbreaks along Gulf of Mexico coast.

136 PAHs) and 22 oxygenated PAHs (OPAHs) at four Gulf of Mexico coastal sites prior to, during and after

137 level rise rate of 1.10 mm +/- 0.19/a in the Gulf of Mexico during 1909-1992 and its acceleration of

138 f surface PAH concentrations reported in the Gulf of Mexico during the Deepwater Horizon spill.

139 Louisiana continental shelf in the northern Gulf of Mexico experiences bottom water hypoxia in the s

140 of crude oil were released into the northern Gulf of Mexico from the Deepwater Horizon disaster, expo

141 The Gulf of Mexico has experienced two of the largest accide

142 ills like the Deepwater Horizon (DWH) in the Gulf of Mexico have the potential to drastically impact

143 The Deepwater Horizon blowout in the Gulf of Mexico in 2010, one of the largest marine oil sp

144 llion barrels of crude oil into the northern Gulf of Mexico in 2010, overlapping spatially and tempor

145 oil and gas facilities were conducted in the Gulf of Mexico in February 2018.

146 il and gas platforms collected over the U.S. Gulf of Mexico in January 2018.

147 ypothesized period of increased transport of Gulf of Mexico moisture northward into the continental i

148 tions for eastern Texas was 10-11 ppb in the Gulf of Mexico near Galveston and 7-8 ppb in much of the

149 uld need to be reduced by 69% to achieve the Gulf of Mexico Nutrient Task Force Action Plan target hy

150 For the full U.S. Gulf of Mexico our inventory estimates total emissions o

151 lycyclic aromatic hydrocarbons (TPAH) in the Gulf of Mexico over time and space.

152 arine vertebrates already disappeared in the Gulf of Mexico prior to the latest Maastrichtian, the Ch

153 of freshwater and nutrients to the northern Gulf of Mexico promoting the development of a large hypo

154 d every 1-30 years in southeast Atlantic and Gulf of Mexico regions in the late 21st century.

155 heatwave) in coastal waters of the northern Gulf of Mexico resulted from compounding effects of a tr

156 Gulf of Mexico saltmarsh sediments were heavily impacted

157 ced dispersed plumes of fine oil droplets in Gulf of Mexico seawater and successfully replicated the

158 e southeast during winter and spring, in the Gulf of Mexico southwards of the Texas and Louisiana coa

159 predict habitat use and oil exposure within Gulf of Mexico spawning grounds.

160 rrent life history model, which assumes only Gulf of Mexico spawning, overestimates age at maturity f

161 characteristics of a hydrocarbon seep in the Gulf of Mexico to its footprint on the sea surface.

162 2010 Deepwater Horizon oil spill exposed the Gulf of Mexico to substantial amounts of oil that also i

163 ion of a 30-year or longer recovery time for Gulf of Mexico water quality is highly uncertain, and th

164 e outside any area of active seepage) of the Gulf of Mexico were investigated and compared.

165 from 7 orders and 11 families native to the Gulf of Mexico were successfully identified.

166 of lionfish in the Atlantic, Caribbean, and Gulf of Mexico will likely remain at or above current le

167 at achieving nitrogen reduction goals in the Gulf of Mexico will take decades as a result of legacy n

168 cleanup of the Deepwater Horizon oil spill (Gulf of Mexico) and heart attack risk among 24,375 oil s

169 e the effects of the 2010 Deepwater Horizon (Gulf of Mexico) disaster on the mental health of individ

170 (The 2010 Deepwater Horizon oil spill in the Gulf of Mexico).

171 ion, with larger individuals spawning in the Gulf of Mexico, and smaller individuals spawning in the

172 lease of millions of barrels of oil into the Gulf of Mexico, and some marsh shorelines experienced he

173 nd, mid-Atlantic, southeast Atlantic, to the Gulf of Mexico, and the effect of TC climatology change

174 behavior in a gregarious fish native to the Gulf of Mexico, Atlantic croaker (Micropogonias undulatu

175 over the North Atlantic, particularly in the Gulf of Mexico, but will increase over the western North

176 on strategies for coastal communities in the Gulf of Mexico, especially those affected by subsidence.

177 f oil and 10(10) mol of natural gas into the Gulf of Mexico, forming deep-sea plumes of dispersed oil

178 olate profusely through the sediments of the Gulf of Mexico, leading to numerous seeps at the seafloo

179 owing the Deepwater Horizon oil spill in the Gulf of Mexico, natural marine snow interacted with oil

180 Here, we demonstrate that in the Gulf of Mexico, Thaumarchaeota use urea and cyanate both

181 e Yucatan to productive coastal areas in the Gulf of Mexico, the Caribbean Sea and along the South Am

182 However, in the Gulf of Mexico, the loss of marsh vegetation because of

183 hore deep bank pinnacles in the northwestern Gulf of Mexico, the present study opens the door to asse

184 Along the Spartina marshes of the northern Gulf of Mexico, the sympatric species P. marginata and P

185 for this knowledge for the U.S. Atlantic and Gulf of Mexico, we integrated 23 years of aerial and shi

186 For lesser-known taxa, and in the Gulf of Mexico, where seasonal movements were less well

187 n the Orca Basin brine pool in the deepwater Gulf of Mexico, which contains numerous landslide deposi

188 SSA are reported at a site >320 km from the Gulf of Mexico, with transport times of 7-68 h.

189 leum seeps (3 km water depth) in the Eastern Gulf of Mexico.

190 uction in non-seep sediments of the northern Gulf of Mexico.

191 ected in thaumarchaeal genomic data from the Gulf of Mexico.

192 ied in the sandy beaches of the northeastern Gulf of Mexico.

193 cause of the persistent hypoxic zone in the Gulf of Mexico.

194 SLR for over 40% of coastal counties in the Gulf of Mexico.

195 .5 to 3.0 kg) diving waterbird common in the Gulf of Mexico.

196 bons (PAHs), in the coastal sediments of the Gulf of Mexico.

197 oil seeps at Campeche Knolls in the southern Gulf of Mexico.

198 ne life and spill responders in the northern Gulf of Mexico.

199 unprecedented discharge of oil into the deep Gulf of Mexico.

200 astern United States, the Caribbean, and the Gulf of Mexico.

201 -maturing western stock, which spawns in the Gulf of Mexico.

202 ts sampled at two localities in the northern Gulf of Mexico.

203 se of millions barrels of crude oil into the Gulf of Mexico.

204 st Plain (WKP), Florida and connected to the Gulf of Mexico.

205 derived carbon (petrocarbon) as oil into the Gulf of Mexico.

206 in foraging habitat quality in the northern Gulf of Mexico.

207 response to natural hydrocarbon seeps in the Gulf of Mexico.

208 ed inventory of CH(4) emissions for the U.S. Gulf of Mexico.

209 tion and growth of Nitrospinae to AOA in the Gulf of Mexico.

210 eposits extended up to 10-km inland from the Gulf of Mexico.

211 011, often extending from West Africa to the Gulf of Mexico.

212 The Gulf of Naples is an example of the most beautiful and b

213 hat separates the Arabian plate from in situ Gulf of Oman oceanic crust and mantle presently subducti

214 try of the ophiolite, its extension into the Gulf of Oman, and the nature of the crust that underlies

215 iotic algae across >5,000 km of the PAG, the Gulf of Oman, and the Red Sea coastline, we show thatS.

216 erse and less than 25% as abundant as in the Gulf of Oman, despite comparable benthic composition and

217 the nearby, but more environmentally benign, Gulf of Oman.

218 The elasmobranch bycatch of the Gulf of Papua Prawn Fishery is investigated in detail fo

219 a total of 403 trawl sets (1,273 hrs) in the Gulf of Papua.

220 Bluefin tuna tagged in the Gulf of St.

221 t of these predation events occurring in the Gulf of St.

222 In the upper Gulf of Thailand, Bryde's whales, which feed on small fi

223 e Great Rann of Kachchh (Kutch), an infilled gulf of the Arabian Sea, which must have received input

224 -enclosed and highly dynamic coastal system (Gulf of Trieste, northern Adriatic Sea, NE Mediterranean

225 cological impacts of DP discharge on Persian Gulf organisms.

226 Coral communities in the Persian/Arabian Gulf (PAG) withstand unusually high salinity levels and

227 We explored the genome of the Gulf pipefish (Syngnathus scovelli), which belongs to fa

228 genome, condensed into chromosomes, for the Gulf pipefish.

229 anguinity, variably practiced in the Persian Gulf region, North Africa, and Central Asia, has resulte

230 donia, the northern Red Sea, and the Arabian Gulf, should become part of a judicious global strategy

231 The western region of the Gulf showed a mean rate of passage 5.4 times higher than

232 = 45 years of age), male (80.8%), lived in a Gulf state (82.3%), and worked at least 1 day on the oil

233 Although Gulf State DSAs have lower expected donation rates, thes

234 On unadjusted analyses, Gulf State DSAs were associated with 3.52 fewer expected

235 nsecurity, and uninsurance were higher among Gulf State DSAs.

236 Participants from Gulf states completed a home visit in which biological a

237 istics and expected kidney donation rates by Gulf States location.

238 the states located along the Gulf of Mexico (Gulf States), may be disadvantaged by limited local supp

239 dney donors per 100 eligible deaths than non-Gulf States.

240 eficiency is endemic in people living in the Gulf states.

241 formation of Warm Core Rings (WCRs) from the Gulf Stream (GS) between 75 degrees and 55 degrees W.

242 nalyze the position, speed, and width of the Gulf Stream (GS) from 80 degrees W-50 degrees W using sa

243 xistence of a surface current connecting the Gulf Stream (GS) to the subpolar gyre (SPG) and have cas

244 pawning ground in the Slope Sea, between the Gulf Stream and northeast United States continental shel

245 A captivating facet of the Gulf Stream as a large-scale ocean climate phenomenon is

246 e Florida Current marks the beginning of the Gulf Stream at Florida Straits, and plays an important r

247 boundary currents, such as the Kuroshio and Gulf Stream Extensions, and have difficulty simulating t

248 Along the Gulf Stream front in the North Atlantic, these observati

249 The Gulf Stream front separates the North Atlantic subtropic

250 ional evidence of enhanced mixing across the Gulf Stream front.

251 Although the Gulf Stream has been vigorously explored over many decad

252 The Gulf Stream is the upper-ocean limb of a powerful curren

253 w study where the decadal variability of the Gulf Stream north wall (defined by the 15 degrees C isot

254 derstanding the long-term variability of the Gulf Stream path is critical for resolving how the ocean

255 C isotherm at 200 m)-the major marker of the Gulf Stream pathway-is analyzed using in situ observatio

256 ve dye released within the north wall of the Gulf Stream provides direct observational evidence of en

257 olving meso-scale oceanic variability in the Gulf Stream region strongly affects mid-latitude interan

258 or, the blue shark (Prionace glauca), in the Gulf Stream region using electronic tags, earth-observin

259 ported by ocean currents associated with the Gulf Stream System from Sargasso Sea breeding grounds to

260 locations would increase entrainment in the Gulf Stream system.

261 crease entrainment of juvenile eels into the Gulf Stream System.

262 Geostrophic flow of the Gulf Stream through the narrow Florida Straits causes an

263 m observations whether anomalous heat in the Gulf Stream's northern extension provides predictability

264 misphere western boundary currents, like the Gulf Stream, are key regions for cyclogenesis affecting

265 ch oceanic regions, such as the Kuroshio and Gulf Stream, highlighting the importance of meso-scale o

266 The Gulf Stream, the main heat-carrier from low to high lati

267 e present a mechanism, in the context of the Gulf Stream, where energy is transferred from the geostr

268 The GuLF STUDY provides a unique opportunity to study potent

269 The GuLF STUDY was designed to investigate relationships bet

270 ata from detailed Gulf Long-term Follow-up ( GuLF) Study enrollment interviews, we determined potenti

271 winds are consistently supportive across the Gulf, thereby avoiding the potentially lethal consequenc

272 purified from Penaeus vannamei from Persian Gulf to homogeneity level using ammonium sulfate precipi

273 ntral and South America and from the Persian Gulf to south Asia.

274 with the intestinal precipitates produced by Gulf toadfish (Opsanus beta).

275 ion rates of isolated intestinal tissue from Gulf toadfish acclimated to control or 1900 muatm CO2 (p

276 poxia, we hypothesized that treatment of the Gulf toadfish, Opsanus beta, with FLX would interfere wi

277 Superior thermal tolerance of Persian Gulf vs. Sea of Oman corals was maintained after 6-month

278 n Veterans who served in the 1990-91 Persian Gulf War and diagnosed with Gulf War Illness (GWI).

279 tary personnel who served during the Persian Gulf War and is notable for cognitive deficits, depressi

280 osure experienced by veterans of the Persian Gulf War contributes to long-lasting pathophysiology by

281 Gulf War illness (GWI) afflicts military personnel who s

282 Gulf War Illness (GWI) and Chronic Fatigue Syndrome (CFS

283 Gulf War Illness (GWI) is a chronic health condition tha

284 Gulf War illness (GWI) is a chronic multisymptom disorde

285 Pain is a diagnostic criterion for Gulf War Illness (GWI), Chronic Fatigue Syndrome (CFS),

286 1990-91 Persian Gulf War and diagnosed with Gulf War Illness (GWI).

287 l neuroimmune disruption in a mouse model of Gulf War illness.

288 e, and time frame of exposure experienced by Gulf War veterans and assessed the acute and chronic imp

289 Because the majority of Gulf War Veterans are overweight, a second objective was

290 c multisymptom disorder that is prominent in Gulf War veterans.

291 ed in Veterans after returning home from the Gulf War.

292 two formulations effectively controlled the Gulf wedge clam Rangia cuneata, an IAS currently spreadi

293 ponses following the early detection of both Gulf wedge clams and many other filter-feeding IAS, and

294 efore, on a breeding/resting ground, Exmouth Gulf, Western Australia, we used animal-borne DTAGs to q

295 atygyra daedalea corals from the hot Persian Gulf where summer temperatures reach 36 degrees C were c

296 shorelines (predators present) was exhibited gulf-wide by all tracked bowheads during the entire 3-wk

297 eepwater Horizon (DWH) spill, we implemented Gulf-wide fish surveys extending over seven years (2011-

298 Planned commercial infrastructure in Exmouth Gulf will cause a substantial increase in shipping traff

299 nt departure winds were predictive of future Gulf winds, and tested whether birds responded to predic

300 extensive declines occurring in the Western Gulf, Wooramel Bank and Faure Sill.