geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-179710.31857/S2949178923040059GMLYYXgeomorf-3269Research ArticleСтатьиArticleОсадочная летопись ранней стадии развития Канозера (ЮЗ часть Кольского полуострова): новые данные для реконструкций дегляциации региона и изменений уровня моряSediment record of the earliest stage of the evolution of Lake Kanozero (SW Kola Peninsula): new data for regional deglaciation reconstructions and relative sea-level studieshttps://orcid.org/0000-0001-6022-2455ЛудиковаА. В.LudikovaA. V.

Лаборатория географии и гидрологии, с.н.с.

ellerbeckia@yandex.ruhttps://orcid.org/0000-0003-0933-7091СапелкоТ. В.SapelkoT. V.

Лаборатория географии и гидрологии, с.н.с.

tsapelko@mail.ruhttps://orcid.org/0000-0001-8864-9936КузнецовД. Д.KuznetsovD. D.

Лаборатория географии и гидрологии, н.с.

dd_kuznetsov@mail.ruШихиринаК. А.ShikhirinaK. A.

магистрант

kristinashikhirinaa@gmail.comИнститут озероведения РАН – СПб ФИЦ РАН, Санкт-ПетербургРоссияInstitute of Limnology of the RAS, St. Petersburg Federal Research Center of the RAS, St. PetersburgRussian FederationРГПУ им. А.И. Герцена, Санкт-ПетербургРоссияHerzen State Pedagogical University, St. PetersburgRussian Federation20231812202354490104Copyright © Лудикова А.В., Сапелко Т.В., Кузнецов Д.Д., Шихирина К.А., 20232023Лудикова А.В., Сапелко Т.В., Кузнецов Д.Д., Шихирина К.А.Ludikova A.V., Sapelko T.V., Kuznetsov D.D., Shikhirina K.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/3269

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.

The multi-proxy study of the lowermost part of the sediment sequence of Lake Kanozero (south-western part of the Kola Peninsula, ca. 53 m a.s.l.) revealed the evidences for marine waters penetration into the basin during the earliest stage of its evolution. The diatom analysis inferred the conditions of a large brackish-water basin. Sediments composition and very low organic content also supported large-basin and low-productivity environments. Based on the pollen study, this stage covers a cooling period preceding the Allerød (tentatively assigned to the Older Dryas) and the onset of the Allerød. Periglacial vegetation typical of the cold and dry climate prevailed in the area for the most of the period. The subsequent transition to the freshwater conditions inferred from the diatom study took place in the Allerød, according to the pollen data. Except for a minor decrease in the fine sand fraction, no other corresponding changes were observed in the sediment record suggesting no major shifts in sedimentary environments. In the late Allerød and throughout the Younger Dryas, Lake Kanozero remained a large, low-productive freshwater basin. Our results indicate that ice-free conditions with aquatic sedimentation in the Kanozero depression had already existed in the Older Dryas. This assumes earlier deglaciation of the study area than it was previously thought. The study also suggests that brackish conditions in the White Sea basin established earlier than reported before. While the previous studies found no signals of marine transgression above ca. 41 m a.s.l., our results indicate that the local marine limit in the study area exceeds ca. 53 m a.s.l.

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The authors declare that there are no conflicts of interest present.