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1 ed along the Malaspina 2010 Circumnavigation Expedition.
2 obtained during the Deepsea Challenge (DSC) Expedition.
3 out of 109 metagenomes from the Tara Oceans expedition.
4 zo in 2012, precisely 210 y after Humboldt's expedition.
5 e oceans during the circumglobal Tara Oceans expedition.
6 a primary goal of the Global Ocean Sampling Expedition.
7 d during the famous second Galathea deep-sea expedition.
8 have been reported following mountaineering expeditions.
9 ts genetic architecture and for gene-hunting expeditions.
10 fects occurred only for group, but not solo, expeditions.
11 S-ADL score (95% CI, -2.3 to 1.4; P=0.64) in EXPEDITION 1 and -1.3 points (95% CI, -2.5 to 0.3; P=0.0
14 a from EXPEDITION 1, the primary outcome for EXPEDITION 2 was revised to the change in scores on the
15 ase 3, double-blind trials (EXPEDITION 1 and EXPEDITION 2), we randomly assigned 1012 and 1040 patien
18 eef development from cores recovered by IODP Expedition 310 to Tahiti, and show that a fringing reef
19 ted during Integrated Ocean Drilling Program Expedition 336 to 'North Pond' on the western flank of t
20 gin during Integrated Ocean Drilling Program Expedition 339 provide constraints on Mediterranean Outf
21 g Project (Integrated Ocean Drilling Program Expedition 343 and 343T) installed a borehole temperatur
25 sis of metagenomic data from the Tara Oceans expedition (7) shows that phages carrying PSI gene casse
28 nomic samples from the Global Ocean Sampling expedition acquired in the Atlantic, Pacific, and Indian
29 d during the Malaspina 2010 circumnavigation expedition, and analyzed for 14 ionizable PFASs, includi
33 uring the Tara Oceans and Malaspina research expeditions, and analyse the resulting 'global ocean vir
34 of a bryozoan collected on Scott's Antarctic expeditions, and subsequently, provide clear evidence of
35 ssigned to International Space Station (ISS) expeditions between Sept 18, 2006, and March 16, 2011.
36 omposition was assessed before and after the expedition by using a 4-component model including fat ma
37 gate body composition during a high-altitude expedition by using non-empirically derived methods, exp
38 EGULATOR9 (PRR9), PRR7, PRR5 and CCA1 HIKING EXPEDITION (CHE), activators of CCA1 remain elusive.
39 rs (TFs), NTM1-like 9 (NTL9) and CCA1 hiking expedition (CHE), as activators of ICS1 during specific
40 ock feedback loop, consisting of CCA1 HIKING EXPEDITION (CHE), CIRCADIAN CLOCK ASSOCIATED1 (CCA1), an
43 t results of the 2001 Arctic Mid-Ocean Ridge Expedition divided the Gakkel ridge into three tectonic
44 mountain climbers from 56 countries on 5,104 expeditions found that hierarchy both elevated and kille
46 with remote sensing and used analyses of ~60 expeditions from 1850-1925 to represent baseline conditi
47 y both elevated and killed in the Himalayas: Expeditions from more hierarchical countries had more cl
50 on at La Isabela seemed to indicate that the expedition had located and tested deposits of silver-bea
51 l mapping system during the submarine SCICEX expedition in 1999 provided the opportunity to perform s
55 gists with no illness and people who went on expeditions in other parts of the world did not have ant
58 gaging in deep space missions such as a Mars expedition is exposure to radiations that put them at ri
60 for environmental factors, risk preferences, expedition-level characteristics, country-level characte
62 World, was established in 1494 by the second expedition of Christopher Columbus but was abandoned by
63 nal activator which is required not only for expedition of virus multiplication but also for blocking
66 nce databases from the Global Ocean Sampling Expedition provide an opportunity to address this questi
68 that provided greater agility in allocating expedition resources resulting in new scientific insight
69 DNA metagenome samples from the Tara-Oceans expedition reveals that populations of Bathycoccus that
70 morphological data sets from 43 Tara Oceans expedition samples to assess viral community patterns an
76 genomic data gathered during the Tara Oceans expedition to improve our understanding of carbon export
79 hnologies during an International Polar Year expedition to the Gakkel ridge in the Arctic Basin at 85
80 mplished during an international ice-breaker expedition to the high Arctic and North Pole in summer 2
82 00 m of sediment core from a recent drilling expedition to the Lomonosov ridge in the Arctic Ocean.
83 Museum of Natural History (AMNH)'s Explore21 expedition to the Solomon Islands in September 2013.
85 y and related parameters from several recent expeditions to the Atlantic, Pacific, Southern and Arcti
87 rom 2075 to 4250 m below the surface on five expeditions to the western and central Arctic Ocean betw
88 99 International Trans-Antarctica Scientific Expedition traverse in East Antarctica at sites located
91 Using plankton samples from the Tara Oceans expeditions, we validate its applicability to taxonomic
92 rica between 1832 and 1833 during the Beagle expedition were examples of the large, heavily armored h
93 ater samples taken during the Malaspina 2010 expedition which covered all the tropical and subtropica
94 Net deposition was shown for ENDO-I on all expeditions, while the net exchange direction of other C
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