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1 rgence in new territories (e.g., the Arabian Peninsula).
2 adapted moss commonly found in the Antarctic Peninsula.
3 solated populations in Italy and the Iberian Peninsula.
4 four NS populations from across the Iberian peninsula.
5 erennially cold waters of the west Antarctic Peninsula.
6 oast, with the highest values on the Florida peninsula.
7 Center or hCoV-EMC), emerged in the Arabian Peninsula.
8 explains the observed trend over the Arabian Peninsula.
9 wider geographical region beyond the Arabian peninsula.
10 auna in a submerged cave on Mexico's Yucatan Peninsula.
11 focus, and the third in the southern Arabian Peninsula.
12 livestock throughout Africa and the Arabian Peninsula.
13 the ecology and appearance of the Antarctic Peninsula.
14 terranean waters of the north-western Balkan Peninsula.
15 oncurrently in at least two locations on the peninsula.
16 applied to seven watersheds on the Delmarva Peninsula.
17 ry disease in humans, emerged in the Arabian Peninsula.
18 d, off the northeastern tip of the Antarctic Peninsula.
19 croach farther southward along the Antarctic Peninsula.
20 rently most likely for the Western Antarctic Peninsula.
21 eration of several glaciers on the Antarctic Peninsula.
22 livestock throughout Africa and the Arabian Peninsula.
23 hroughout Africa and portions of the Arabian Peninsula.
24 e eastern and western sides of the Antarctic Peninsula.
25 tive of the climate history of the Antarctic Peninsula.
26 tal environment off Mexico's Baja California peninsula.
27 as, and atmospheric warming on the Antarctic Peninsula.
28 ed across sub-Saharan Africa and the Arabian Peninsula.
29 re disease throughout Africa and the Arabian Peninsula.
30 mainly in sub-Saharan Africa and the Arabian Peninsula.
31 roughout Africa, Madagascar, and the Arabian Peninsula.
32 depths in Marguerite Bay, western Antarctic Peninsula.
33 oughout Africa and more recently the Arabian peninsula.
34 /epidemics throughout Africa and the Arabian peninsula.
35 ic Ocean, and waters offshore the Antarctica Peninsula.
36 hesis of vascular plants along the Antarctic Peninsula.
37 els in sediment communities of the Antarctic Peninsula.
38 termediate to both species found on the Baja peninsula.
39 curring much earlier than on the rest of the peninsula.
40 of the total regional CH4 flux of the Barrow Peninsula.
41 ded throughout the last 100 y in the Iberian Peninsula.
42 of the total regional CH4 flux of the Barrow Peninsula.
43 e in Macedonia and other countries of Balkan peninsula.
44 s repeatedly caused outbreaks in the Arabian Peninsula.
45 disease outbreaks in Africa and the Arabian Peninsula.
46 livestock illness in Africa and the Arabian Peninsula.
47 Applied Health Research and Care South West Peninsula.
48 n at Palmer station in the Western Antarctic Peninsula.
49 of latitude from Patagonia to the Antarctic Peninsula.
50 their spatial distribution across the Barrow Peninsula.
51 y entered from what would become the Arabian Peninsula.
52 0.39 +/- 0.10 mug m(-3) yr(-1)), the Arabian Peninsula (0.81 +/- 0.21 mug m(-3) yr(-1)), South Asia (
53 hundreds of glaciers draining the Antarctic Peninsula (63 degrees to 70 degrees S) have undergone sy
56 specimens archived from participants in the Peninsula AIDS Research Cohort Study (PARC) demonstrated
57 n the muskox population occupying the Seward Peninsula, Alaska during 2002-2012, we formulated the hy
58 Recent findings showed that some of the Kii Peninsula ALS cases had pathogenic C9orf72 repeat expans
59 wild dromedaries from the southeast Arabian Peninsula among the founders of the domestic dromedary g
61 he virus is endemic in camels in the Arabian Peninsula and Africa and thus poses a consistent threat
62 (-3)) in the Kara Strait, Kara Sea, and Kola Peninsula and an extremely high concentration (1000 ng m
63 t trends in 244 marine glacier fronts on the peninsula and associated islands over the past 61 years.
65 introductions were observed within the Malay Peninsula and between countries bordered by the Mekong R
66 century transfer of cattle from the Iberian Peninsula and Canary Islands to the Caribbean laid the f
67 the Classic Maya civilization in the Yucatan Peninsula and Central America was a complex process that
69 arts of South America as well as the Iberian Peninsula and Eastern Australia, and over 60% in most of
72 al to West Africa, and across to the Arabian Peninsula and Indian subcontinent, from source populatio
74 y to the observed warming over the Antarctic Peninsula and Patagonia and to the cooling over eastern
75 curred in the eastern portion of the Arabian Peninsula and reveal substantial subsequent gene flow wi
76 rast between strong warming of the Antarctic Peninsula and slight cooling of the Antarctic continenta
77 Eurasian populations were established on the Peninsula and that contemporary indigenous Arabs are dir
79 present geochemical data from the Kamchatka peninsula and the Aleutian islands that reaffirms the sl
80 rs from northeastern Africa into the Arabian Peninsula and the Levant and expanding further into Eura
81 t glacial migration waves across the Arabian Peninsula and the Levant region around 106-94, 89-73, 59
82 aled two main clades confined to the Iberian Peninsula and the rest of Europe but showing incongruent
83 ea, a deep ocean basin between the Antarctic peninsula and the tip of South America, showing a high i
84 ribution of the wild ancestor on the Arabian Peninsula and to the brief coexistence of early-domestic
85 trol animals, VM202-treated animals revealed peninsulas and/or islands of viable myocardium in infarc
86 locations (highest in the Arctic and Alaska Peninsula) and among years in tundra swans (Cygnus colum
87 ancestors colonized Africa from the Arabian peninsula) and tested to what extent historical coloniza
88 ure (presently occurring along the Antarctic Peninsula), and may serve as a leading indicator of immi
89 uman and dromedary MERS-CoV from the Arabian peninsula, and genetically diverse dromedary viruses fro
90 ided in or recently travelled to the Arabian peninsula, and is a global concern for public health.
93 pancies between observations at Tahiti, Huon Peninsula, and Sunda Shelf during Lateglacial time (appr
94 ayment of West Antarctica, and the Antarctic Peninsula are changing quite rapidly as a result of proc
95 , refugia in the Italian, Balkan and Iberian peninsulas are believed to be the main sources of specie
96 estern Mediterranean Sea, south-west Iberian Peninsula) are global PCB "hotspots" for marine mammals.
99 d arcs, continental fragments and the Papuan Peninsula, as well as recolonization of the central orog
100 omes of 104 unrelated natives of the Arabian Peninsula at high coverage, including 56 of indigenous A
101 ographic location in the heart of the Balkan Peninsula at the intersection of Central and Southeaster
102 east Pacific region near the Baja California Peninsula (BCP) (42.7 +/- 7.2 vs. 68.3 +/- 3.4 cm carapa
103 though warming of the northeastern Antarctic Peninsula began around 600 years ago, the high rate of w
105 constituted nearly 20% of isolates from the peninsula but were virtually absent in East Malaysia.
106 nhabiting the Levant rather than the Arabian Peninsula, but the principal route for the expansion out
107 Unlike participants with ALS from the Kii Peninsula, C9orf72 expansions do not cause ALS-PDC in Ch
108 ic disease endemic in Africa and the Arabian Peninsula caused by the highly infectious Rift Valley fe
109 tarctica, West Antarctica, and the Antarctic Peninsula changed in mass by -142 +/- 49, +14 +/- 43, -6
111 ent during peak growing season on the Barrow Peninsula, CO2 uptake occurs at -902.3 10(6) gC-CO2 day(
112 netic homogeneity across most of the Arabian Peninsula coastline, with a genetic break towards the so
113 es (OCPs) were measured in Western Antarctic Peninsula continental shelf sediments, porewater, and be
114 continental margin of the western Antarctic Peninsula cooled by 3-4 degrees C over the past 12,000 y
115 pidly warming seas off the western Antarctic Peninsula could now facilitate their return to the conti
117 s collected at selected areas from Antarctic Peninsula (Deception and Livingstone Islands, Southern S
118 vity near the shelf in the Western Antarctic Peninsula despite a short growing season and cold temper
119 istribution of North African ancestry in the peninsula does not reflect the initial colonization and
121 ence of early cercopithecines on the Arabian Peninsula during the late Miocene reinforces the probabi
122 ns such as the Sahara desert and the Arabian Peninsula during various 30-year periods, pointing to de
123 eltwater on the hydrography of the Antarctic Peninsula ecosystem has been largely ignored, and the re
125 de the well-documented refuge in the Iberian Peninsula, evidence for a cryptic refuge in northwest Fr
127 ld-wide biogeographical regions, the Arabian Peninsula exhibits the highest intra-population variance
130 storic population responses in the Antarctic Peninsula, favoring generalist gentoo penguins as climat
131 steini off Marguerite Bay, western Antarctic Peninsula for environmental or trophic impediments to sh
132 The CCM of diatoms in the Western Antarctic Peninsula functions with a relatively small expenditure
133 al separation of Jeju Island from the Korean peninsula has allowed Jeju black pigs not only to acquir
134 a California indicates that sea level in the peninsula has been rising at a mean rate of 0.70 mm/y (+
135 nued retreat of ice shelves on the Antarctic Peninsula has been widely attributed to recent atmospher
136 pact of climatic change along the Antarctica Peninsula has been widely debated in light of atmospheri
138 a, of the Larsen ice shelf off the Antarctic Peninsula has led to a refocus toward the implications o
140 lar, recent climate changes on the Antarctic Peninsula have been dramatic, yet the Holocene climate v
141 nges in penguin populations on the Antarctic Peninsula have been linked to several environmental fact
142 he 1950s, research stations on the Antarctic Peninsula have recorded some of the largest increases in
143 lgae at their southern limits in the Iberian Peninsula have shown shifts in geographical range and a
144 ear-old Nuvvuagittuq Greenstone Belt (Ungava peninsula) have been investigated to track the early ori
147 Larsen A and B ice shelves on the Antarctic Peninsula in 1995 and 2002 confirm the impact of southwa
154 Coast in North America and the Mediterranean peninsulas in Europe during the Pleistocene glaciations;
155 the southeastern most portion of the Arabian Peninsula, in the tri-continental crossroads connecting
156 in small, isolated populations on the Balkan peninsula, initially by pollination experiments and iden
158 ming over the past 50 years on the Antarctic Peninsula is associated with the collapse of a number of
164 by prehistoric people on Michigan's Keweenaw Peninsula is one of the oldest examples of metalworking.
166 h the rest of the populations in the Arabian Peninsula, it is unique in terms of its relative high As
167 al time resolution from the temperate Korean Peninsula (KP) for the last 5500 years in order to compa
169 Summer temperature on the Cape Churchill Peninsula (Manitoba, Canada) has increased rapidly over
170 Ocean temperatures at the western Antarctic Peninsula margin were tied to changes in the position of
171 ilicic acid [Si(OH)4] on the west Antarctica Peninsula margin, a region in which the modern phytoplan
173 a preliminary analysis of benthic Antarctic Peninsula meiofauna using high throughput sequencing whi
175 nalyzed lake-sediment cores from the Yucatan Peninsula, Mexico, to reconstruct the climate history of
176 and aboveground carbon stocks in the Yucatan Peninsula, Mexico-a region with a long history of habita
178 rred at a high incidence on Guam, in the Kii peninsula of Japan, and in southern West New Guinea more
180 alt at cities in the interior of the Yucatan peninsula of Mexico, Belize, and Guatemala in an area wh
183 Recent studies have shown that the Nicoya Peninsula of northwestern Costa Rica is moving northwest
185 o species of Cnemidophorus occur on the Baja peninsula, one relatively large (Cnemidophorus tigris) a
186 of families from three tribes of the Arabian Peninsula, Persia, and Oman, with indications of African
187 ex Structure profiles are seen among Arabian Peninsula populations underscoring the high genetic dive
190 ISH) in coastal waters of the west Antarctic Peninsula region during two austral summers and one aust
191 n polar regions, as observed in Antarctica's peninsula region over the second half of the 20th centur
192 ises (SHALDRIL I and II) in the northernmost Peninsula region yield a record that, when combined with
193 prolonged period of warming in the Antarctic Peninsula region, in combination with the long-term thin
194 statistically increasing along the Antarctic Peninsula region, the presence of glacial meltwater is l
195 ankton, and krill samples from the Antarctic Peninsula region, which questions previous claims that t
198 uth, becoming distributed among the isolated peninsulas represented by Anatolia, Italy and Iberia.
200 ate change, risks will grow in the Antarctic Peninsula, Ross Sea, and East Antarctic coastal regions.
201 owever, two lakes located closer to the Kola Peninsula (Russia) have recorded increasing SBC fluxes f
202 thwest Pacific, and Elovy Island in the Kola Peninsula, Russia, indicate transport times of hours to
203 Ardley Island, home to one of the Antarctic Peninsula's largest breeding populations of gentoo pengu
205 es of PCBs (63-94%) in the Western Antarctic Peninsula sediments were bound to black carbon or recalc
206 e la Boella" site (north-east of the Iberian Peninsula) seem to indicate that an earlier introduction
207 Sustained observations at the West Antarctic Peninsula show that in this region, rapid environmental
208 renowned archaeological caves of the Iberian Peninsula spanning the last million years of human evolu
210 ew areas around the Scotia Sea and Antarctic Peninsula suitable for growth of the largest krill (>60
211 data from Seymour Island, near the Antarctic Peninsula, that provides well-constrained evidence for a
212 g recent centuries in the northern Antarctic Peninsula, the most rapidly warming region of the Southe
213 ' as they are now declining in the Antarctic Peninsula, the opposite of their response to post-LGM wa
214 eading of mice first to the southern Arabian Peninsula, thence eastward and northward into south-cent
216 ing and multi-trophic interactions along the peninsula to be increasingly regulated by glacial discha
217 nt warming extends well beyond the Antarctic Peninsula to cover most of West Antarctica, an area of w
221 t future nitrogen delivery from the Delmarva Peninsula to the Bay given different scenarios of nitrog
222 climate changes extending from the Antarctic Peninsula to the subtropics-similar to those associated
223 and 6 Korean pigs (which live on the Korean peninsula) to compare and identify putative signatures o
224 cted by ice per year (Hangar Cove, Antarctic Peninsula) to those protected by virtually permanent sea
226 aplogroups H1, H3, V, and U5b1), the Italian Peninsula (U5b3), and the East European Plain (U4 and U5
230 ntense diatom bloom in the Western Antarctic Peninsula (WAP) and in laboratory cultures of a psychrop
232 limate of the western shelf of the Antarctic Peninsula (WAP) is undergoing a transition from a cold-d
234 8-year time-series in the Western Antarctic Peninsula (WAP) with an approximately weekly sampling fr
235 n export potential at the Western Antarctica Peninsula (WAP), a region which has experienced rapid wa
238 ty, but none explains the observed Antarctic Peninsula warming or the sea-ice redistribution in austr
240 ia by this time, suggesting that the Arabian Peninsula was a potential filter for cross-continental f
244 t the elevated interior areas of the Yucatan Peninsula were more susceptible to system collapse and l
245 64 rivers that drain 84% of Michigan's Lower Peninsula were sampled under baseflow conditions for Esc
246 the most pronounced along the West Antarctic Peninsula where there has been a rapid warming event dur
247 f this expansion will occur in the Antarctic Peninsula, where a threefold increase in ice-free area c
248 the coast of the Gulf of Mexico and Florida peninsula, where evaporation relative to precipitation i
249 wth frequency of speleothems from the Korean peninsula, which we compare to Southern Hemisphere equiv
250 ancestry are seen in the Italian and Iberian peninsulas, which may indicate different effects of hist
252 w coronavirus emerged in 2012 on the Arabian Peninsula with a clinical syndrome of acute respiratory
253 ing along the southern half of the Kamchatka peninsula with a region of transcurrent motion along the
254 rsity for the butterfly fauna of the Iberian Peninsula with unprecedented resolution (3502 DNA barcod
256 talagmite delta(18)O record from the Yucatan Peninsula (YP) that spans the interval between 26.5 and
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