Yanagawa H, Ogawa Y, Kojima K, Ito M
Mitsubishi-Kasei Institute of Life Sciences, Tokyo, Japan.
Orig Life Evol Biosph. 1988;18(3):179-207. doi: 10.1007/BF01804670.
We have developed experimental approaches for the construction of protocellular structures under simulated primitive earth conditions and studied their formation and characteristics. Three types of envelopes; protein envelopes, lipid envelopes, and lipid-protein envelopes are considered as candidates for protocellular structures. Simple protein envelopes and lipid envelopes are presumed to have originated at an early stage of chemical evolution, interaction mutually and then evolved into more complex envelopes composed of both lipids and proteins. Three kinds of protein envelopes were constructed in situ from amino acids under simulated primitive earth conditions such as a fresh water tide pool, a warm sea, and a submarine hydrothermal vent. One protein envelope was formed from a mixture of amino acid amides at 80 degrees C using multiple hydration-dehydration cycles. Marigranules, protein envelope structures, were produced from mixtures of glycine and acidic, basic and aromatic amino acids at 105 degrees C in a modified sea medium enriched with essential transition elements. Thermostable microspheres were also formed from a mixture of glycine, alanine, valine, and aspartic acid at 250 degrees C and above. The microspheres did not form at lower temperatures and consist of silicates and peptide-like polymers containing imide bonds and amino acid residues enriched in valine. Amphiphilic proteins with molecular weights of 2000 were necessary for the formation of the protein envelopes. Stable lipid envelopes were formed from different dialkyl phospholipids and fatty acids. Large, stable, lipid-protein envelopes were formed from egg lecithin and the solubilized marigranules. Polycations such as polylysine and polyhistidine, or basic proteins such as lysozyme and cytochrome c also stabilized lipid-protein envelopes.
我们已经开发出了在模拟原始地球条件下构建原细胞结构的实验方法,并研究了它们的形成和特性。三种类型的包膜,即蛋白质包膜、脂质包膜和脂蛋白包膜,被视为原细胞结构的候选者。简单的蛋白质包膜和脂质包膜被推测起源于化学进化的早期阶段,相互作用,然后进化成由脂质和蛋白质组成的更复杂的包膜。在模拟原始地球条件下,如淡水潮池、温暖的海洋和海底热液喷口,由氨基酸原位构建了三种蛋白质包膜。一种蛋白质包膜是在80摄氏度下,使用多个水合-脱水循环由氨基酸酰胺混合物形成的。在富含必需过渡元素的改良海洋介质中,在105摄氏度下,由甘氨酸与酸性、碱性和芳香族氨基酸的混合物产生了marigranules,即蛋白质包膜结构。在250摄氏度及以上,由甘氨酸、丙氨酸、缬氨酸和天冬氨酸的混合物也形成了耐热微球。微球在较低温度下不形成,由硅酸盐和含有酰亚胺键以及富含缬氨酸的氨基酸残基的肽样聚合物组成。形成蛋白质包膜需要分子量为2000的两亲性蛋白质。由不同的二烷基磷脂和脂肪酸形成了稳定的脂质包膜。由卵磷脂和溶解的marigranules形成了大的、稳定的脂蛋白包膜。聚赖氨酸和聚组氨酸等聚阳离子,或溶菌酶和细胞色素c等碱性蛋白质也使脂蛋白包膜稳定。