Осадочная летопись ранней стадии развития Канозера (ЮЗ часть Кольского полуострова): новые данные для реконструкций дегляциации региона и изменений уровня моря
- Авторы: Лудикова А.В.1, Сапелко Т.В.1, Кузнецов Д.Д.1, Шихирина К.А.2
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Учреждения:
- Институт озероведения РАН – СПб ФИЦ РАН
- РГПУ им. А.И. Герцена
- Выпуск: Том 54, № 4 (2023)
- Страницы: 90-104
- Раздел: Палеолимнологические исследования в России: от Калининграда до Камчатки
- URL: https://cardiosomatics.ru/2949-1789/article/view/660695
- DOI: https://doi.org/10.31857/S2949178923040059
- EDN: https://elibrary.ru/GMLYYX
- ID: 660695
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Аннотация
Комплексное исследование нижней части толщи донных отложений Канозера (юго-западная часть Кольского п-ова, 53 м над у. м.) выявило свидетельства проникновения соленых вод в его бассейн на ранней стадии его эволюции. По результатам диатомового анализа реконструированы условия крупного солоноватоводного водоема. Литологический состав донных отложений и крайне низкое содержание органического вещества свидетельствуют об обстановках большого низкопродуктивного бассейна. По данным спорово-пыльцевого анализа этот этап охватывает период похолодания среднего дриаса и начало аллереда. На данном этапе в основном преобладала перигляциальная растительность, типичная для холодного и сухого климата. Переход к пресноводным условиям, о котором свидетельствуют изменения состава диатомовых комплексов, произошел в аллереде. Помимо незначительного уменьшения содержания песчаной фракции, в составе донных отложений никаких изменений отмечено не было, что свидетельствует об отсутствии заметных изменений в обстановках осадконакопления в ходе изоляции. С конца аллереда и в течение всего позднего дриаса озеро Канозеро оставалось крупным низкопродуктивным пресноводным бассейном. Наши результаты свидетельствуют о том, что котловина Канозера была свободна от ледникового льда уже в среднем дриасе, когда здесь происходило субаквальное осадконакопление. Это предполагает, что дегляциация района исследования произошла раньше, чем считалось прежде. Полученные данные также указывают на более раннее установление солоноватоводных условий в беломорской котловине. Тогда как предыдущие исследования не выявили свидетельств морской трансгрессии на отметках >41 м над у. м., наши результаты показывают, что верхняя морская граница в районе исследования превышает 53 м над у. м.
Ключевые слова
Об авторах
А. В. Лудикова
Институт озероведения РАН – СПб ФИЦ РАН
Автор, ответственный за переписку.
Email: ellerbeckia@yandex.ru
Россия, Санкт-Петербург
Т. В. Сапелко
Институт озероведения РАН – СПб ФИЦ РАН
Email: ellerbeckia@yandex.ru
Россия, Санкт-Петербург
Д. Д. Кузнецов
Институт озероведения РАН – СПб ФИЦ РАН
Email: ellerbeckia@yandex.ru
Россия, Санкт-Петербург
К. А. Шихирина
РГПУ им. А.И. Герцена
Email: ellerbeckia@yandex.ru
Россия, Санкт-Петербург
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