Геологический вестник

В статье выполнен краткий обзор представлений о климате докембрия, присутствующих как в капитальных монографиях и университетских учебниках, опубликованных с середины 1960-х гг. до настоящего времени, так и в многочисленных статьях, увидевших свет в зарубежных и отечественных рецензируемых журналах. Показано существование двух парадигм (жаркий и умеренный архей), основанных примерно на одной и той же совокупности изотопно-геохимических данных, но исходящих из разных представлений об эволюции изотопного состава морской воды далекого геологического прошлого и разного понимания процессов трансформации/сохранения “первичного сигнала” в кремнях, карбонатных и фосфатных минералах и других носителях информации. Отмечено, что данных о палеотемпературах и других параметрах палеоклимата для позднего докембрия все еще существенно меньше, чем для докембрия раннего, и эта ситуация нуждается в исправлении.

палеоклимат, палеотемпература, методы реконструкции, представления, докембрий, обзор

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