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Cryogenian (∼720-635 Ma) global glaciations (the snowball Earth) represent the most extreme ice ages in Earth's history. The termination of these snowball Earth glaciations is marked by the global precipitation of cap carbonates, which are interpreted to have been driven by intense chemical weathering on continents. However, direct geochemical evidence for(More)
We present the first steps in applying transverse relaxation-optimized spectroscopy (TROSY) techniques to the study of allosterism. Each beta-chain of the hemoglobin (Hb) tetramer has 17 valine residues. We have (15)N-labeled the beta-chain Val residues and detected 16 of the 17 (1)H-(15)N correlation peaks for beta-chain Val of the R state CO-Hb structure(More)
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