Диатомовые водоросли как показатель динамики формирования поверхностных донных осадков южной части моря Скоша
DOI:
https://doi.org/10.15587/2313-8416.2015.42246Słowa kluczowe:
осадконакопление, донные отложения, диатомит, диатомовые водоросли, средний миоцен, море СкошаAbstrakt
Изучение диатомовых из осадков нижнего интервала колонки К97-18 в море Скоша выявило в комплексах сочетание позднеплейстоцен-голоценовых и миоценовых видов, что объясняется обилием в породе включений среднемиоценового диатомита. Были установлены время переотложения, агенты и пути транспортировки, а также предложены возможные места локализации коренных слоев диатомита
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