Изменения размеров ледникового купола Беллинсгаузена (остров Кинг-Джордж, Антарктика) в позднем голоцене

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Рассмотрено изменение ледникового купола Беллинсгаузен на острове Кинг-Джордж (Ватерлоо) в позднем голоцене по имеющимся геоморфологическим и биологическим признакам, а также по данным радиоуглеродного датирования органических остатков, обнаруженных в моренах с ледяным ядром или вне них (мертвые мхи, ракушки и кости кита). Выделено два этапа активизации ледникового купола Беллинсгаузена – 600–800 и 300 лет назад.

Об авторах

Б. Р. Мавлюдов

Институт географии РАН

Автор, ответственный за переписку.
Email: bulatrm@bk.ru
Россия, Москва

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