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1 m the Levant (Natufians) than other mainland Arabians.
2 on events in the histories of: 1) Indian and Arabian ancestries, 2) Kalash ancestry, and 3) Native Am
3 s a mixture of ancestries closely related to Arabian ancestry and Nilo-Saharan or Omotic ancestry.
4 an and 1 Arabian-pony cross), and 2 foals (1 Arabian and 1 Arabian-pony cross) with severe combined i
5 ult Arabian horses, two 1-month-old foals (1 Arabian and 1 Arabian-pony cross), and 2 foals (1 Arabia
6 respect to nearby populations: Yemeni, other Arabian and Bedouin samples form a continuum towards the
8 Turkmen) and west/southwest breeds (Persian Arabian and Kurdish) into two phylogeographic clades ref
9 en studied in the context of Asian, Saharan, Arabian, and Australian storms, but there has been no re
11 es suggestive of selective sweeps across the Arabian breed contain candidate genes for combating oxid
12 t no significant genomic contribution of the Arabian breed to the Thoroughbred racehorse, including Y
13 tember 2012 in samples obtained from a Saudi Arabian businessman who died from acute respiratory fail
14 abia, over an almost 2-year period and local Arabian camels over 2 months in the year after surveilla
15 yalipithecus) deep within the otherwise Afro-Arabian clade Parapithecoidea and indicates that transat
17 y characterised haplogroups, one observed in Arabian/Coldblooded and the other in Turkoman/Thoroughbr
19 time, the sources of DNA became increasingly Arabian, consistent with evidence of growing interaction
20 the progressive aridification of the Saharo-Arabian desert and the fluctuations of savannah habitats
21 en monsoonal Asia to the east and the Saharo-Arabian desert belt to the west, making it a key thresho
23 ests the episodic presence within the Saharo-Arabian Desert interior of water-dependent fauna (for ex
27 ed early modern humans to surpass the Saharo-Arabian deserts or if climatic changes triggered punctua
31 ne was performed with individuals from Saudi Arabian families with multiple, clinically confirmed, mo
35 d a positional candidate approach in a Saudi Arabian family affected with autosomal recessive SCAN1,
37 is c.1028C>T (p.Thr343Met), while in a Saudi Arabian family the variant is c.962G>A (p.Arg321Gln).
38 affected siblings in a consanguineous Saudi Arabian family we performed genome-wide linkage and mapp
39 quencing in a multiplex consanguineous Saudi Arabian family with a pallido-pyramidal syndrome, iron d
42 ly that the genetic SCID disease observed in Arabian foals is explained by a defect in V(D)J recombin
44 ntaneous genetic immunodeficiencies in mice, Arabian foals, and recently in Jack Russell terriers hav
48 ns in the world's warmest reefs, the Persian/Arabian Gulf (PAG), represent an ideal model system to u
50 atal Neonatal Outcomes Research Study in the Arabian Gulf (PEARL-Peristat Study) between April 2017 a
51 om reefs both inside and outside the Persian/Arabian Gulf across temperatures of 27.0 degrees C, 31.5
52 ine systems of the northeastern Arabia area (Arabian Gulf and Sea of Oman) and of these which ones ar
53 st, most extreme coral reefs in the southern Arabian Gulf and the nearby, but more environmentally be
54 measurements of high mixing ratios over the Arabian Gulf are adequately simulated, strong underpredi
61 New Caledonia, the northern Red Sea, and the Arabian Gulf, should become part of a judicious global s
65 of polymorphism on the Y chromosome of Saudi-Arabian hamadryas baboons, Papio hamadryas hamadryas.
66 discussed, as well as characterization of an Arabian heavy vacuum gas oil in terms of the ring number
68 importantly, there was no evidence that the Arabian horse breed has clear subdivisions depending on
70 Overall, our data support an origin of the Arabian horse in the Middle East, no evidence for reduce
71 aternal inheritance is an essential point in Arabian horse population genetics and strains classifica
73 ed (OR = 1.9, 95% CI 1.2-2.8, P = 0.005) and Arabian horses (OR = 1.9, 95% CI 1.2-2.8, P = 0.005) wer
75 s of oxidative status in 3 years old, racing Arabian horses during long term observation and the chan
80 We sequenced the whole mtDNA D-loop of 251 Arabian horses to study the genetic diversity and phylog
81 this region identified one SNP found only in Arabian horses, located in exon 4 of TOE1 and approximat
82 xperimentally transmit EHCV to 4 young adult Arabian horses, two 1-month-old foals (1 Arabian and 1 A
89 al at least five hominin expansions into the Arabian interior, coinciding with brief 'green' windows
92 disease processes, HHV-8 derived from Saudi Arabian KS lesions were shown to have a distinct nucleot
94 ain phase of silicic volcanism from the Afro-Arabian large igneous province preserves some of the lar
97 ng 15-20 kya, when Levantines expanded while Arabians maintained smaller populations that derived anc
98 r gap exists in the Oligocene record of Afro-Arabian mammal evolution is now limited primarily to a p
103 on in Jeddah that were reported to the Saudi Arabian Ministry of Health from January 1 through May 16
105 llele frequencies between 1% and 5% in Saudi Arabians (n = 1,061), Vietnamese (n = 1,264), Thai (n =
106 oms the diverging plate dynamics between the Arabian, Nubian, and Somalian plates along the Red Sea,
107 from Africa to Spain during the long-lasting Arabian occupation that started in the seventh century,
109 pothesis that crown Strepsirrhini is of Afro-Arabian origin and that lemuriforms likely colonized Mad
110 support to the hypothesis of an ancient Afro-Arabian origin for crown Strepsirrhini and an Eocene div
111 human population samples is consistent with Arabian origin, a more eastern or Persian origin, and in
112 other species, such as African elephants and Arabian oryx, may alter their potential to experience RE
113 onstrable crown strepsirrhines from the Afro-Arabian Palaeogene--a galagid and a possible lorisid fro
114 or approximately 85% of the alleles in Saudi Arabian patients, the S379P, R441X, R474W, and F480L mut
115 U.S. (-0.39 +/- 0.10 mug m(-3) yr(-1)), the Arabian Peninsula (0.81 +/- 0.21 mug m(-3) yr(-1)), Sout
118 identify wild dromedaries from the southeast Arabian Peninsula among the founders of the domestic dro
123 st, MERS is primarily a camel disease on the Arabian Peninsula and in Africa, with clinical disease i
124 dispersal to West Africa, and across to the Arabian Peninsula and Indian subcontinent, from source p
125 ation occurred in the eastern portion of the Arabian Peninsula and reveal substantial subsequent gene
127 corridors from northeastern Africa into the Arabian Peninsula and the Levant and expanding further i
128 prominent glacial migration waves across the Arabian Peninsula and the Levant region around 106-94, 8
131 ive distribution of the wild ancestor on the Arabian Peninsula and to the brief coexistence of early-
132 tire genomes of 104 unrelated natives of the Arabian Peninsula at high coverage, including 56 of indi
133 a zoonotic disease endemic in Africa and the Arabian Peninsula caused by the highly infectious Rift V
134 kable genetic homogeneity across most of the Arabian Peninsula coastline, with a genetic break toward
137 the presence of early cercopithecines on the Arabian Peninsula during the late Miocene reinforces the
138 ecoregions such as the Sahara desert and the Arabian Peninsula during various 30-year periods, pointi
139 ious world-wide biogeographical regions, the Arabian Peninsula exhibits the highest intra-population
144 gical and paleoenvironmental research in the Arabian peninsula is transforming our understanding of a
145 circulates widely in dromedary camels in the Arabian Peninsula leading to zoonotic transmission.
147 nd complex Structure profiles are seen among Arabian Peninsula populations underscoring the high gene
149 nto Arabia by this time, suggesting that the Arabian Peninsula was a potential filter for cross-conti
152 A new coronavirus emerged in 2012 on the Arabian Peninsula with a clinical syndrome of acute resp
153 ds which ancestors colonized Africa from the Arabian peninsula) and tested to what extent historical
155 inct ancestry groups: general Arab, Persian, Arabian Peninsula, Admixture Arab, African, and South As
156 nce of human and dromedary MERS-CoV from the Arabian peninsula, and genetically diverse dromedary vir
157 ving resided in or recently travelled to the Arabian peninsula, and is a global concern for public he
158 , zoonotic disease endemic to Africa and the Arabian Peninsula, and its spread outside of the endemic
159 d the Tibetan Plateau, Central Asia, and the Arabian Peninsula, and Western Siberia, respectively.
160 ations inhabiting the Levant rather than the Arabian Peninsula, but the principal route for the expan
161 espiratory illness with recent travel to the Arabian Peninsula, especially among healthcare workers.
162 st to all other genotyped populations of the Arabian Peninsula, genome-level analysis of the medieval
163 r An. stephensi across its full range (Asia, Arabian Peninsula, Horn of Africa) and a set of spatial
164 ated at the southeastern most portion of the Arabian Peninsula, in the tri-continental crossroads con
165 mmon with the rest of the populations in the Arabian Peninsula, it is unique in terms of its relative
166 number of families from three tribes of the Arabian Peninsula, Persia, and Oman, with indications of
167 nsively managed herds, ubiquitous across the Arabian Peninsula, present a major potential source of p
168 One high-frequency region-encompassing the Arabian Peninsula, southern Mesopotamia, and the souther
169 ile pastoralism in the desert regions of the Arabian Peninsula, the history of the Jews, and the spre
170 y Holocene ~ 9500 years ago somewhere in the Arabian Peninsula, the Levant, and southern Mesopotamia.
171 tial spreading of mice first to the southern Arabian Peninsula, thence eastward and northward into so
172 malaria vector native to South Asia and the Arabian Peninsula, was detected in Djibouti's seaport, f
173 rus widely distributed across Africa and the Arabian Peninsula, which causes devastating epidemics af
174 drocarbon measurements, performed around the Arabian Peninsula, with global model simulations that in
204 rporting to explain Druze history that posit Arabian, Persian or mixed Near Eastern-Levantine roots.
206 an incipient suture zone that separates the Arabian plate from in situ Gulf of Oman oceanic crust an
209 triple junction, between Nubian, Somali and Arabian plates, and for hosting environments at the very
210 the regional simple mantle flow beneath the Arabian Platform and eastern Turkey deflects as a circul
212 an-pony cross), and 2 foals (1 Arabian and 1 Arabian-pony cross) with severe combined immunodeficienc
213 rses, two 1-month-old foals (1 Arabian and 1 Arabian-pony cross), and 2 foals (1 Arabian and 1 Arabia
215 ade, and mainly female assimilation into the Arabian population as a result of miscegenation and manu
216 ficantly different between an African and an Arabian population, suggesting that loss of variation du
220 diversity and phylogenetic relationships of Arabian populations and to examine the traditional strai
224 ed along 13 degrees of latitude in the Saudi Arabian Red Sea, from shallow-water reefs to deep-sea ha
228 at as is the case in C.B-17 SCID mice and in Arabian SCID foals, the defective factor in these SCID p
230 clustering the cyclogenesis over the Eastern Arabian Sea (EAS) next to the Indian West coast in recen
231 sed delta(11)B record from the north-eastern Arabian Sea (NEAS) covering the mid-late Holocene (~ 8-1
233 ion of moist, westerly monsoon flow from the Arabian Sea across India, resulting in a smaller flux of
234 ent between the Middle East and the southern Arabian Sea and drives the changes of low-level jet (LLJ
235 na bulloides abundance in box cores from the Arabian Sea and found that monsoon wind strength increas
237 e way to the development of upwelling in the Arabian Sea and possibly led to a strengthening of South
238 stern and southeastern coasts, adjoining the Arabian Sea and the Bay of Bengal, were assessed with el
240 ear, average sea surface temperatures in the Arabian Sea are warm enough to support the development o
242 ing stratification of the upper layer of the Arabian Sea at a much faster rate than predicted by glob
243 African-descent Makranis, who reside on the Arabian Sea coast of Pakistan, as well that of four neig
244 es from three major mangrove sites along the Arabian Sea coast of Pakistan, Indus Delta, Sandspit and
245 substantial millennial-scale variability in Arabian Sea denitrification and productivity during the
247 s rapid, century-scale reorganization of the Arabian Sea ecosystem in response to climate excursions,
248 -pressure systems that traverse the northern Arabian Sea every winter and spring disrupt winter conve
252 oration, driving the convective formation of Arabian Sea High Salinity Water (ASHSW) during the winte
253 ution of denitrification to N(2) loss in the Arabian Sea indicates the global significance of denitri
255 pproach in practice, nitrogen cycling in the Arabian Sea oxygen minimum zone (OMZ) was modeled to exa
257 an increase in the intensity of pre-monsoon Arabian Sea tropical cyclones during the period 1979-201
259 the Northeast Atlantic and tropical Western Arabian Sea with new data from the Northeast Pacific.
262 of the monsoon circulation over the northern Arabian Sea, as revealed by a compilation of proxy recor
263 d affect tropical cyclone intensity over the Arabian Sea, but so far no such linkage has been shown.
264 of the low-level monsoon westerlies over the Arabian Sea, driving surges of moisture supply, leading
266 otable increase in extreme cyclones over the Arabian Sea, particularly in post-monsoon cyclones (Sept
267 wn independently of the Indus River into the Arabian Sea, perhaps along courses of now defunct rivers
269 hich involves in-phase fluctuations over the Arabian Sea, the Bay of Bengal, and the South China Sea,
270 anammox dominates the N(2) loss term in the Arabian Sea, the largest and most intense OMZ in the wor
271 f data from the equatorial Pacific Ocean and Arabian Sea, we show that the relative direct and indire
272 cation dominates over anammox in the central Arabian Sea, which has important implications for the lo
273 eover, the trend in aerosol loading over the Arabian Sea, which is located downwind to Central India,
274 of Kachchh (Kutch), an infilled gulf of the Arabian Sea, which must have received input from the Sar
275 munities differentiated strongly moving from Arabian Sea-influenced high salinity (southerly; prasino
286 retion complexes occupying almost the entire Arabian Shield and much of Egypt and parts of the small
288 tiated during this period, which we term the Arabian Standstill, include loci involved in the regulat
291 ere performed based on two independent Saudi Arabian studies comprising 3950 MI patients and 2324 non
293 aximize levels of heterozygosity and include Arabian, Thoroughbred, Welsh Cob, and Icelandic Horse br
296 Data regarding the vitamin D status of Saudi Arabian women and its relation to breast cancer risk are