Savidge William B, Blair Neal E
Skidaway Institute of Oceanography, 10 Ocean Science Circle, Savannah, GA 31411, USA.
Oecologia. 2004 Apr;139(2):178-89. doi: 10.1007/s00442-004-1500-z. Epub 2004 Feb 24.
A survey of the intramolecular C isotopic composition of a variety of organisms was conducted to investigate the potential of intramolecular isotopic measurements as a tracer of biological or geochemical processes. Based on a consideration of inorganic C sources and enzymatic fractionations, contrasting predictions were made for the relative (13)C enrichments of the alpha-carboxyl carbons fixed by the anapleurotic (beta)-carboxylation pathway during amino acid synthesis by photoautotrophs and heterotrophs. To test the model predictions, the stable C isotopic compositions of the acid hydrolyzable C fraction, the total amino acid alpha-carboxyl C fraction and the alpha-carboxyl C of glutamate from a variety of autotrophic and heterotrophic organisms were compared. The relative (13)C enrichments of carboxyl carbons in the bulk amino acid fraction and in glutamate conformed qualitatively to model predictions. Macroalgal taxa possessed a significantly less enriched carboxyl C fraction than did either C3 or C4 vascular plants, indicating the presence of a different beta-carboxylation pathway operating in these organisms. In most multicellular heterotrophs, the isotopic composition of the amino acid carboxyl carbons closely resembled that of their food sources. Amino acids are apparently assimilated into tissue proteins directly from their diets without significant metabolic modification. However, shifts in the isotopic composition of the carboxyl C fractions in some organisms were detected that were consistent with the occurrence of significant resynthesis of amino acids from non-amino acid precursors. Comparison of plant leaves and roots provided evidence of environmentally controlled assimilate partitioning. Intramolecular isotopic measurements of biological molecules provide unique insights into the origins and transformations of bio-molecules.
对多种生物体的分子内碳同位素组成进行了调查,以研究分子内同位素测量作为生物或地球化学过程示踪剂的潜力。基于对无机碳源和酶促分馏的考虑,对光合自养生物和异养生物在氨基酸合成过程中通过回补(β)-羧化途径固定的α-羧基碳的相对(13)C富集情况做出了对比预测。为了检验模型预测,比较了来自多种自养和异养生物的酸可水解碳组分、总氨基酸α-羧基碳组分以及谷氨酸的α-羧基碳的稳定碳同位素组成。大量氨基酸组分和谷氨酸中羧基碳的相对(13)C富集在质量上符合模型预测。大型藻类分类群的羧基碳组分的富集程度明显低于C3或C4维管植物,这表明这些生物体中存在不同的β-羧化途径。在大多数多细胞异养生物中,氨基酸羧基碳的同位素组成与其食物来源非常相似。氨基酸显然是直接从它们的饮食中被同化到组织蛋白中,而没有明显的代谢修饰。然而,在一些生物体中检测到羧基碳组分的同位素组成发生了变化,这与从非氨基酸前体大量重新合成氨基酸的情况一致。对植物叶片和根系的比较提供了环境控制同化产物分配的证据。生物分子的分子内同位素测量为生物分子的起源和转化提供了独特的见解。