Роль вакуумного ультрафиолетового излучения и других видов энергии открытого космоса в абиогенном синтезе нуклеотидов и дипептидов
Диссертация
Геологические данные неопровержимо свидетельствуют, что уже 3.5 млрд лет назад на планете существовали достаточно сложные фотоавтотрофные микроорганизмы, сходные с современными цианобактериями (Schopf, 1993). Более того, изотопный анализ углерода из осадочных пород, имеющих возраст около 3.8 млрд лет говорит о том, что и в это время протекали фотоавтотрофные биохимические процессы (Schidlowski… Читать ещё >
Содержание
- Список принятых сокращений
- Глава I. Обзор литературы
- 1. 1. Краткий обзор теорий возникновения жизни
- 1. 2. Возможные места космической химической эволюции
- 1. 2. 1. Межзвездная среда
- 1. 2. 2. Межзвездные пылевые облака
- 1. 2. 3. Метеориты
- 1. 2. 4. Кометы
- 2. 1. Объекты исследования
- 2. 2. Методы исследования
- 2. 2. 1. Абиогенный синтез нуклеотидов
- 2. 2. 2. Абиогенный синтез дипептидов
- 2. 2. 3. Полетные эксперименты на спутнике «Бион-11»
- 2. 3. Аналитические методы
- 2. 4. Определение радиационно-химического и квантового выходов реакции
- 2. 5. Статистическая обработка результатов
- 3. 1. 1. Абиогенный синтез нуклеотидов под действием вукуумного ультрафиолетового излучения
- 3. 1. 1. 1. Абиогенный синтез пуриновых нуклеотидов под действием ВУФ-излучения
- 3. 1. 1. 2. Абиогенный синтез пиримидиновых нуклеотидов под действием ВУФ-излучения
- 3. 1. 1. 3. Распад исходных нуклеозидов под действием ВУФ-излучения
- 3. 1. 2. Абиогенный синтез нуклеотидов под действием биологически-значимого УФ-излучения
- 3. 1. 3. Абиогенный синтез нуклеотидов под действием у-излучения
- 3. 1. 4. Абиогенный синтез природных нуклеотидов в условиях космического полета спутника «Бион-11»
- 3. 2. Абиогенный синтез дипептидов под действием различных источников энергии космического пространства
- 3. 2. 1. Абиогенный синтез дипептидов под действием ВУФ-излучения
- 3. 2. 2. Абиогенный синтез дипептидов под действием у-радиации
- 3. 2. 3. Абиогенный синтез дипептдов под действием потока заряженных частиц
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