Hemoglycin

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Hemoglycin
(Glycine-containing space polymer of amino acids found in meteorites)
Hemoglycin was found in Acfer 086, an Allende meteorite similar to that pictured.
Functionunknown, although possibly able to split water to hydroxyl and hydrogen moieties[1]

Hemoglycin (previously termed hemolithin) is a space polymer that is the first polymer of amino acids found in meteorites.[2][3][4]

Structural work has determined that its 1,494-dalton core unit (glycine18 / hydroxy-glycine4 / Fe2O4) contains iron, but not lithium, leading to the more general term hemoglycin for these molecules.[1][5] The hemoglycin core contains a total of 22 glycine residues in an anti-parallel beta-sheet chain that is terminated at each end by an iron atom plus two oxygens. Four of these glycine residues are oxidized to hydroxy-glycine with hydroxy groups (−OH) on the alpha carbon. This structure was determined by mass spectrometry of meteoritic solvent extracts[1][2][5] and has been confirmed in X-ray scattering by crystals of hemoglycin,[6] and also by optical absorption.[3] Crystals show a 480 nm characteristic absorption that can only exist when hydroxy-glycine residues have R chirality and are C-terminal bonded to iron.[6]

History

Because hemoglycin has now been found to be the dominant polymer of amino acids in 6 different meteorites (Allende,[7] Acfer 086, Efremovka, Kaba, Orgueil and Sutter's Mill), each time with the same structure, it has been proposed[3][6] that it is produced by a process of template replication. The measured 480 nm absorbance is larger than expected for a racemic distribution of R and S chirality in the hydroxy-glycine residues, indicating an R chirality excess in the polymer. Modeling of template replication that is assumed to depend on 480 nm absorption leads to an excess of R chirality and thus is consistent with this finding.

Significance

See also

References

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