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1  Moon has shifted: the hydrogen deposits are antipodal and displaced equally from each pole along opp
2 a, rotation of the kDNA disk relative to the antipodal attachment sites results in distribution of pr
3 ic quakes and ejecta fallout produced by the antipodal Caloris basin impact.
4 ing internal pyridine motifs and two crucial antipodal carboxylic acid groups.
5 maintain cylindrical cell shape and strictly antipodal cell growth.
6 sacs have smaller central cells and abnormal antipodal cells that are larger, more vacuolated, and fe
7 , 11 genes were expressed exclusively in the antipodal cells, 11 genes were expressed exclusively or
8 d two synergids, one central cell, and three antipodal cells.
9  synergid cells, one central cell, and three antipodal cells.
10       Our examination of the Caloris basin's antipodal chaotic terrain reveals multi-kilometer surfac
11 yrrole-imidazole dimers is the production of antipodal congeners without the corresponding enantiomer
12 ode is probably responsible for the observed antipodal decline in magnetic field strength.
13  one predominant and a second, less frequent antipodal direction.
14 blages are strongly magnetized in two nearly antipodal directions.
15 r hypothesis provides an explanation for the antipodal distribution of lunar polar hydrogen, and conn
16  these receptors could have such diverse and antipodal effects are considered here.
17 red from one enantiomer of nopinone, provide antipodal enantiofacial selectivity in the dialkylzinc a
18  (1)H and (11)B NMR tracing the reciprocally antipodal endocyclic open face H(ec) and B(1).
19                   In addition, synergid- and antipodal-expressed genes are ectopically expressed in a
20               The Tharsis-induced trough and antipodal high were largely in place by the end of the N
21 identified multiple chaotic terrains with no antipodal impact basins; hence a new geological explanat
22                                          The antipodal introduction of two bromine atoms on the 2,12
23 relationship of the described compounds, the antipodal isomers (3aR)-N1,N8-bisnorcarbamates (+)9 and
24 ors of BChE, particularly (-)19, whereas the antipodal isomers lacked activity.
25                                   Two nearly antipodal large low-shear-velocity provinces in the deep
26 lation over the past 1 Gyr, we find that two antipodal LLVPs develop naturally as a consequence of Ea
27 ously remagnetized the meteorite in a nearly antipodal local field.
28 tereomerically distinct and enantiomerically antipodal metabolites, have remained largely uncharacter
29 f CD43 was necessary and sufficient for this antipodal movement.
30 tization directions were defined with nearly antipodal normal and reversed polarities for samples PO-
31 NA displayed the flipped sugar moiety in the antipodal north conformation, we suggest that conversion
32 ng destabilization of the aptamer, while the antipodal North/anti-dG nucleoside was less destabilizin
33 a carbocyclic nucleoside into one of the two antipodal (north or south) conformations typical of conv
34                                              Antipodal paleomagnetic directions determined from the c
35 we observed propagating for four (plus three antipodal) passages around Earth over 6 days.
36 ocalization site, forming the characteristic antipodal pattern.
37                                              Antipodal plasma membranes were prepared from isolated c
38 lpha subunits in rat colonocytes, colonocyte antipodal plasma membranes, and colonic neoplasms.
39 mpared with brush border fraction of colonic antipodal plasma membranes.
40 on in the T cell-APC contact zone and at the antipodal pole of the cell.
41 t negative charge for the C12 carbon atom in antipodal position, in agreement with the proposed elect
42  signify large-scale mantle upwelling in two antipodal regions of the mantle.
43  that catalyze the same aldol reactions with antipodal selectivity were analyzed by comparing their a
44 mapped two global-scale organized concentric antipodal sets of arcuate troughs up to hundreds of kilo
45 s with the other replication proteins at the antipodal sites and also at the two faces of the kDNA di
46 ision or G1, but is abruptly detected in the antipodal sites at the onset of kDNA replication.
47 specific endonuclease have been localized to antipodal sites flanking the kDNA disk along with nascen
48 II and DNA polymerase beta colocalize in two antipodal sites flanking the kDNA during replication, th
49 r with the localization of the enzyme in two antipodal sites flanking the kDNA, show that a function
50 A topoisomerase and a DNA polymerase beta at antipodal sites flanking the kinetoplast disc.
51 ma brucei, showing it to be localized in the antipodal sites flanking the kinetoplast DNA disk, as pr
52 ication proteins and a possible role for the antipodal sites in removal of RNA primers and the repair
53 mmunofluorescent localization of SSE1 to the antipodal sites is only observed during kinetoplast repl
54 The replicating minicircles then move to two antipodal sites that flank the disk-shaped network.
55  the localization of the endonuclease to the antipodal sites varies in a cell cycle-dependent manner
56 ell cycle stages; usually it is found in two antipodal sites, but during cytokinesis each postscissio
57 brucei kinetoplast does move relative to the antipodal sites.
58 iphery, are thought to take place within the antipodal sites.
59 n accumulation of the protein at or near the antipodal sites.
60 acial selectivity at the new center for each antipodal substrate, indicating that the enzyme also is
61  enzyme catalyzes the hydroxylation of small antipodal substrates with distinct stereochemistries and
62  were employed to assess the contribution of antipodal sugar conformations on the stability of the ca
63 terrestrial sites in southern Pangea, nearly antipodal to contemporaneous STLIP activity, providing i
64            Most of these regions are located antipodal to large basins, leading to the hypothesis tha
65 ws that the lunar magnetic fields are strong antipodal to Mare Imbrium and Mare Serenitatis and has d
66 ols and aminoalkanediols with configurations antipodal to that found in mammalian D-erythro-sphingosi
67      Electron reflection maps of the regions antipodal to the Imbrium and Serenitatis impact basins,
68 hat crustal magnetic fields fill most of the antipodal zones of those basins.