The 11,800-year pollen-based vegetation (biome) reconstruction obtained from Razlomnoe Peat in the Lake Onega region (Eastern Fennoscandia) ...

• Main Authors: Krikunova, Aleksandra I, Savelieva, Larisa A, Long, Tengwen, Leipe, Christian, Kobe, Franziska, Kostromina, Natalia A, Vasilyeva, Aleksandra V, Tarasov, Pavel E
• Format: Dataset
• Language: unknown
• Published: PANGAEA 2024
• Subjects: biome reconstruction; Fennoscandia; Holocene; Karelia; Lateglacial; Event label; DEPTH, sediment/rock; AGE; Pollen, affinity scores, tundra; Pollen, affinity scores, cold deciduous forest; Pollen, affinity scores, taiga; Pollen, affinity scores, cool coniferous forest; Pollen, affinity scores, cool mixed forest; Pollen, affinity scores, cold steppe; Pollen, affinity scores, landscape openness; Dominant biome; Hand-held Peat Corer; Age, 14C; Onega; taiga; Tundra
• Online Access: https://dx.doi.org/10.1594/pangaea.971601; https://doi.pangaea.de/10.1594/PANGAEA.971601

The 885-cm-long sediment core RZ19 (62°27′53′′N, 34°26′4′′E) was retrieved in 2019 from Razlomnoe Peat (northern shore of Lake Onega), radiocarbon-dated and analysed for pollen and cryptogam spores. The age-depth model suggests continuous sedimentation since ca. 11,800 a BP. A total of 97 sediment s...