ライフサイエンスコーパス: gulf

1 ulf of Mexico coast before flying across the Gulf.

2 in their ability to acquire fat to cross the Gulf.

3 erns, favored southward departure across the Gulf.

4 rom any other ITS2 C3 type found outside the Gulf.

5 's hottest sea, the southern Persian/Arabian Gulf.

6 Strait, and (4) the eastern Joseph Bonaparte Gulf.

7 ope with extreme temperatures in the Persian Gulf.

8 ermophilum, sp.nov. from the Persian/Arabian Gulf, a thermally tolerant coral symbiont.

9 eus from summer and winter from the Amundsen Gulf and measured their alpha-HCH concentrations, enanti

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

11 cies from the Canadian High Arctic (Amundsen Gulf and the Canadian Beaufort Sea) in relation to ambie

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

13 tion investments on nutrient delivery to the Gulf and use an evolutionary algorithm to solve the opti

14 subcategories are recognised, i.e. Vostizza, Gulf, and Provincial.

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

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

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

18 In the gulf between genotype and phenotype exists proteins and,

19 ng Made Easy color plates (Home Vision Care, Gulf Breeze, FL), and diagnostic confirmatory testing wa

20 orating Centre for Mass Gatherings Medicine, Gulf Co-operation Council states, UK universities, and p

21 nt of ecosystem goods and services along the Gulf Coast (USA) demonstrates the need to include both t

22 from representative potable aquifers in the Gulf Coast area.

23 antified in water and oysters from Florida's Gulf Coast by plating on mCPC agar, enrichment and plati

24 of individuals sampled from the Southeastern Gulf Coast drainages were characterized by the presence

25 s comprised of samples from the Southeastern Gulf Coast drainages.

26 esulted in crude oil contamination along the Gulf coast in sensitive estuaries.

27 erae non-O1/O139 gastroenteritis in the U.S. Gulf Coast is reported here.

28 owland Maya civilization and the role of the Gulf Coast Olmec.

29 well as from the drainages of the Southwest Gulf Coast region, lack this tandem repeat.

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

31 rn (LOC) established jointly by the NOAA/FDA/Gulf Coast states under the protocol to reopen state and

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

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

34 s in organic aerosol concentration along the Gulf Coast were likely due to the DWH spill.

35 a compound that displayed strong ties to the Gulf Coast where cotton cloth was made.

36 tion, or about 30% more than Florida and the Gulf Coast, the highest deposition areas within the U.S.

37 utaries and rivers draining to the Southwest Gulf Coast, the other lineage is comprised of samples fr

38 y Mountains and the highest emissions in the Gulf Coast.

39 Chiapas, the Pacific Coast, and the southern Gulf Coast.

40 quality issue for populated areas along the Gulf Coast.

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

42 increased southwards along the Atlantic and Gulf coasts as fire and hurricane disturbances became pr

43 ion Council for the Arab States of the Gulf (Gulf Cooperation Council [GCC]), namely, Saudi Arabia, U

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

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

46 nium associations of 6 species (5 genera) of Gulf corals, we demonstrate that S. thermophilum is the

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

48 ing Colwellia, which also bloomed in situ in Gulf deep waters during the discharge.

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

50 the background-subtracted SOA spectra in the Gulf (for short, "Gulf SOA") showed higher contribution

51 operation Council for the Arab States of the Gulf (GCC), and these trends are set to continue.

52 operation Council for the Arab States of the Gulf (Gulf Cooperation Council [GCC]), namely, Saudi Ara

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

54 t in the spring and early summer critical to Gulf hypoxia formation, with the largest differences (un

55 ient loading reduction is required to reduce Gulf hypoxia to the Action Plan goal of 5000 km(2), to t

56 s on a limited mostly deep-water area of the Gulf, include a conservative estimate of thickness of th

57 the intertidal zones of Lengeh Port, Persian Gulf, Iran, to survey whether heavy metals are within th

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

59 ects of Deepwater Horizon crude oil on fish, Gulf killifish ( Fundulus grandis ) were collected from

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

61 Furthermore, laboratory exposures of Gulf killifish embryos to field-collected sediments from

62 Gulf killifish embryos were exposed to dissolved Cu and

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

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

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

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

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

68 c study in the United Arab Emirates (UAE), a Gulf nation in the Middle East, with an inter-disciplina

69 The calcification rate of the Gulf of Aden was estimated by the Rayleigh model to be a

70 .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

71 oraminiferal oxygen isotope records from the Gulf of Alaska (GOA) reveal sudden shifts between interv

72 ability across two North Pacific ecosystems (Gulf of Alaska and Bering Sea).

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

74 ne palaeotemperature reconstruction from the Gulf of Alaska that reveals two abrupt warming events of

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

76 iple islands in Prince William Sound and the Gulf of Alaska.

77 ing steep population declines in the central Gulf of Alaska.

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

79 in surface water of the northern Baltic Sea (Gulf of Bothnia, consisting of Bothnian Bay and Bothnian

80 ediments collected in different areas of the Gulf of Cadiz and subjected to several pH treatments to

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

82 nd may explain SAR324's ubiquity in the deep Gulf of California and in the global marine biosphere.

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

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

85 n hydrothermal plumes and deep waters of the Gulf of California enabled detailed population-specific

86 mal plume and surrounding waters in the deep Gulf of California to gain insight into the genetic capa

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

88 In the Gulf of California, these animals mature at large size (

89 GB) and nearby background waters in the deep Gulf of California.

90 nd Atlantis ecosystem model for the Northern Gulf of California.

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

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

93 ~10 cm long) also occurred at 1,722 m in the Gulf of California.

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

95 hin the Baltic Sea (Baltic Main Basin (BMB), Gulf of Finland (GoF), and Bothnian Sea (BS)) during mar

96 of the Finnish oil combating vessels in the Gulf of Finland (GoF), Eastern Baltic Sea.

97 growth of maritime oil transportation in the Gulf of Finland (GoF), North-Eastern Baltic Sea, increas

98 Oil transport has greatly increased in the Gulf of Finland over the years, and risks of an oil acci

99 er quality elements from 1970 to 2010 in the Gulf of Finland, a eutrophied sub-basin of the Baltic Se

100 ctive (WFD) in Finnish coastal waters in the Gulf of Finland, one of the most eutrophicated areas of

101 trade wind blowing from the Sahara into the Gulf of Guinea.

102 oss sub-Saharan Africa and on islands in the Gulf of Guinea.

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

104 in between thermally stratified water in the Gulf of Maine and mixed water on the bank.

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

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

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

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

109 k is a large, shallow feature separating the Gulf of Maine from the Atlantic Ocean.

110 The experience in the Gulf of Maine highlights the need to incorporate environ

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

112 ura 2000 in Europe, lobster fisheries in the Gulf of Maine, North America, and fisheries in Europe.

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

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

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

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

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

118 absent by December 2010 in the Northeastern Gulf of Mexico (3 of 8 cruises with one positive station

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

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

121 vated methylmercury (MeHg) concentrations in Gulf of Mexico (GOM) fish, we quantified fluxes of total

122 ic monitoring data collected at sites in the Gulf of Mexico (GOM) from the period during and followin

123 yed offshore demersal fishes in the northern Gulf of Mexico (GoM) in 2011-2013, to assess polycyclic

124 s groups (i.e. functional groups) across the Gulf of Mexico (GoM) using a large fisheries independent

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

126 the Deepwater Horizon (DWH) oil spill in the Gulf of Mexico (GOM).

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

128 gree, sediment porewater of the Northeastern Gulf of Mexico (NEGOM) and west Florida shelf (WFS) at t

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

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

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

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

133 osts are most favorable for the coast of the Gulf of Mexico and Florida peninsula, where evaporation

134 portant for predicting summer hypoxia in the Gulf of Mexico and targeting nutrient reduction within t

135 rge from the BP Macondo Prospect well in the Gulf of Mexico are calculated using a physically based m

136 ht weathered oil samples collected from four Gulf of Mexico beaches 12-19 months after the Deepwater

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

138 slicks on surface waters and tar balls from Gulf of Mexico beaches.

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

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

141 d (RFS) and reducing hypoxia in the northern Gulf of Mexico by reducing riverine nitrate-N loads repr

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

143 Along the northern Gulf of Mexico coast, USA, subtropical black mangrove (A

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

145 demonstrated maximum productivity along the Gulf of Mexico coast, with the highest values on the Flo

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

147 to sediments from oiled locations along the Gulf of Mexico coast.

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

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

150 e report on a voluntary testing program with Gulf of Mexico commercial fishermen to ensure the safety

151 Standard Reference Material (NIST SRM) 2779 Gulf of Mexico crude oil by GC coupled to vacuum ultravi

152 st known deep-water coral communities in the Gulf of Mexico do not appear to have been acutely impact

153 The irruption of gas and oil into the Gulf of Mexico during the Deepwater Horizon event fed a

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

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

156 Horizon incident, crude oil flowed into the Gulf of Mexico from 1522 m underwater.

157 estimate the hypoxic extent in the northern Gulf of Mexico from data collected during midsummer, qua

158 samples collected on beaches in the northern Gulf of Mexico from July 2010 until August 2012, hopanoi

159 ntrations in air flowing into Texas from the Gulf of Mexico have not changed significantly over this

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

161 ed by the Deepwater Horizon oil spill in the Gulf of Mexico in 2010 and the Fukushima nuclear plant i

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

163 the Deepwater Horizon (DWH) oil spill in the Gulf of Mexico in June 2010 indicated the presence of hi

164 The Gulf of Mexico is one of the most ecologically and econo

165 water Horizon oil spill (DWH) in 2010 in the Gulf of Mexico is the largest accidental marine oil spil

166 er hypoxic (low oxygen) zone in the northern Gulf of Mexico is the second largest in the world.

167 The sinking of the Deepwater Horizon in the Gulf of Mexico led to uncontrolled emission of oil to th

168 gnatures among coastal fish consumers in the Gulf of Mexico likely reflects both differences in envir

169 These results suggest that Gulf of Mexico marsh sediments have considerable biodegr

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

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

172 deployed during the Deepwater Horizon (DWH) Gulf of Mexico oil spill to track the subsea oil plume.

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

174 tween consumed seafood and hair samples from Gulf of Mexico recreational anglers who are exposed to l

175 Gulf of Mexico saltmarsh sediments were heavily impacted

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

177 Tar balls collected from the Gulf of Mexico shores of Louisiana and Florida after the

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

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

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

181 boratory incubations of deep waters from the Gulf of Mexico stimulated Colwellia's growth.

182 s a 5-y running average) set by the national Gulf of Mexico Task Force's Action Plan.

183 The oil spill in the Gulf of Mexico that followed the explosion of the explor

184 rface plumes of dispersed oil and gas in the Gulf of Mexico that stimulated growth of psychrophilic,

185 oxygen isotope (delta(18)O) records from the Gulf of Mexico using a water mixing model.

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

187 Two oil-degrading cultures from the Gulf of Mexico were isolated, one from the surface (meso

188 of 12.8 +/- 2.6 ppm in tissue collected from Gulf of Mexico whales in the wake of the crisis.

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

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

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

192 We found an extinct spreading ridge in the Gulf of Mexico, a major propagating rift in the South At

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

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

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

196 (DWH) disaster that occurred in 2010 in the Gulf of Mexico, could severely affect fish at impacted s

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

198 ndo Well on the water surface throughout the Gulf of Mexico, including deposition on the shorelines.

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

200 he Deepwater Horizon oil well blowout in the Gulf of Mexico, the application of 7 million liters of c

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

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

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

204 ow the AMO may drive physical changes in the Gulf of Mexico, thus altering higher-level ecosystem dyn

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

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

207 has or has not been affected in the Northern Gulf of Mexico, which when put in context with oil spill

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

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

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

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

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

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

214 l(-1)) zone occurs annually in the northern Gulf of Mexico.

215 ss is unknown for pelagic predators from the Gulf of Mexico.

216 oeukaryotic phytoplankton) in the P-depleted Gulf of Mexico.

217 alyze wells penetrating salt deposits in the Gulf of Mexico.

218 -top, and downcore samples from the northern Gulf of Mexico.

219 frequent exposure to K. brevis blooms in the Gulf of Mexico.

220 urface velocity fluctuations in the Northern Gulf of Mexico.

221 636 million L of crude oil into the northern Gulf of Mexico.

222 lcifying depth habitat or seasonality in the Gulf of Mexico.

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

224 dominant toxic red tide algal species in the Gulf of Mexico.

225 ted 760 million liters of crude oil into the Gulf of Mexico.

226 contamination of coastal environments in the Gulf of Mexico.

227 ical storms to the south of Florida into the Gulf of Mexico.

228 that threaten coastal regions throughout the Gulf of Mexico.

229 regional P-limitation of algal growth in the Gulf of Mexico.

230 s used as an oil spill countermeasure in the Gulf of Mexico.

231 and long-term effects of the disaster on the Gulf of Mexico.

232 ogic pathways for hydrocarbon release to the Gulf of Mexico.

233 , even in energetic environments such as the Gulf of Mexico.

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

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

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

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

238 tion (R (2) = 0.49) between ice cover in the Gulf of St.

239 e conducted for the month of February in the Gulf of St.

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

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

242 vers of seabird habitat selection within the Gulf of the Farallones and Cordell Bank National Marine

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

244 The Gulf oil spill resulted in an isolated source of seconda

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

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

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

248 At six monitoring sites (Persian/Arabian Gulf, Red Sea, northern and southern Galapagos, Easter I

249 se military members who have deployed to the Gulf region in support of more recent contingency operat

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

251 health services some of the countries in the Gulf region, the burden of non-communicable diseases is

252 are not among the most common cancers in the Gulf region.

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

254 Processes that led to the observed Gulf SOA characteristics are also likely to occur in pol

255 a gradient in the degree of oxidation of the Gulf SOA was observed: more oxidized SOA (oxygen/carbon

256 tracted SOA spectra in the Gulf (for short, "Gulf SOA") showed higher contribution of C(x)H(y)O(+) re

257 = 45 years of age), male (80.8%), lived in a Gulf state (82.3%), and worked at least 1 day on the oil

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

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

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

261 plume, and in samples characteristic of the Gulf Stream and the U.S. East Coast.

262 hich was related to a northward shift in the Gulf Stream and to changes in the Atlantic Multidecadal

263 -depth ocean temperature associated with the Gulf Stream are rapidly destabilizing methane hydrate al

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

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

266 locations would increase entrainment in the Gulf Stream system.

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

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

269 Samples taken in the Gulf Stream were below detection limit for all parent PA

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

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

272 In the midnorthwest Atlantic/Gulf Stream, sum PFAA concentrations ( summation operato

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

274 The GuLF STUDY provides a unique opportunity to study potent

275 The GuLF STUDY was designed to investigate relationships bet

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

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

278 In the Arabian/Persian Gulf, this situation has already occurred and population

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

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

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

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

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

284 ss in the Millennium Cohort than in the 1991 Gulf War cohort, a higher prevalence of reported CMI was

285 d illnesses reported by veterans of the 1991 Gulf War era are a cause of potential concern for those

286 This Gulf War era multiple sclerosis cohort provides a unique

287 the military between 1990, the start of the Gulf War era, and 2007 and who were service-connected fo

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

289 are the key brain abnormalities observed in Gulf war illness (GWI), a chronic multisymptom health pr

290 tigated the effect of 4 weeks of exposure to Gulf war illness-related (GWIR) chemicals in the absence

291 those in a cohort of subjects from the 1991 Gulf War to gain context for the present report.

292 rgic autonomic deficits in the population of Gulf War veterans.

293 study population of US Seabees from the 1991 Gulf War, as well as from deployed and nondeployed subgr

294 thesis that symptoms in veterans of the 1991 Gulf War, such as chronic diarrhea, dizziness, fatigue,

295 ly 25% of veterans who served in the Persian Gulf War-1.

296 ater off the bank during flood tide and cool gulf water onto the bank during ebb tide.

297 A considerable portion of Gulf water samples collected during the spill had PAH co

298 ning" of trapped crude oil on the surface of Gulf waters during the 2010 Deepwater Horizon (DWH) oil

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

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

301 ubwatersheds that deliver nutrients into the Gulf with a hypoxic zone model.