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Finally, in series C of Table 1, (S)- and (R)- sensitive reaction for recognizing and amplify-
phenyl-1,2,3,4,5,6-13C6-phenylmethanol 3 were ing the extremely small chiral influence be-
used as chiral initiators of asymmetric autocatal- tween 12C and 13C. The method described above
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enantioselective addition of i-Pr2Zn to pyrimidine- tope chirality in organic molecules in nature (33).
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References and Notes
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formation of the zinc alkoxide of the isotopically
chiral alcohol tips the enantiomeric balance of
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5 is induced. After this step, the subsequent auto-
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therefore in the final production of 5.
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Materials and Methods
SOM Text
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Include this information when citing this paper.
A Global View of the
Lithosphere-Asthenosphere Boundary
Catherine A. Rychert* and Peter M. Shearer
meric excess. It is therefore impossible to disclose a The lithosphere-asthenosphere boundary divides the rigid lid from the weaker mantle
structural reason for the difference in frequency of and is fundamental in plate tectonics. However, its depth and defining mechanism are not
these initial enantiotopic face selectivities. The well known. We analyzed 15 years of global seismic data using P-to-S (Ps) converted phases and
“cooperation–amplification” effect, which has been imaged an interface that correlates with tectonic environment, varying from 95 T 4 kilometers
discussed regarding the structural effect of hy- beneath Precambrian shields and platforms to 81 T 2 kilometers beneath tectonically altered
drogen deuterium chiral substitution in a helical regions and 70 T 4 kilometers at oceanic island stations. High-frequency Ps observations
polymer (15), finds reactive analogy in this auto- require a sharp discontinuity; therefore, this interface likely represents a boundary in
catalytic system. The product handedness is en- composition, melting, or anisotropy, not temperature alone. It likely represents the
tirely predictable, but the absolute value of the ee lithosphere-asthenosphere boundary under oceans and tectonically altered regions, but
varies from run to run. This observation indicates it may constitute another boundary in cratonic regions where the lithosphere-asthenosphere
a stochastic influence in the initiation phase bi- boundary is thought to be much deeper.
ased by the chiral additive. The locally induced
enantiomeric excess of zinc alkoxide is then am-
plified by the normal asymmetric autocatalytic
process (32).
apping the depth and character of the to be a challenge. Global surface-wave studies
lithosphere-asthenosphere boundary with (1–4) image rigid lithospheres that increase in
existing seismic methods has proven thickness from oceans to continents at broad
M
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