Late Quaternary paleoenvironmental reconstructions from sediments of Lake Emanda (Verkhoyansk Mountains, East Siberia)

• Published in: Journal of Quaternary Science
• Main Authors: Andreev, Andrei A., Nazarova, Larisa B., Lenz, Marlene M., Böhmer, Thomas, Syrykh, Ludmila, Wagner, Bernd, Melles, Martin, Pestryakova, Ludmila A., Herzschuh, Ulrike
• Other Authors: European Research Council, Deutsche Forschungsgemeinschaft
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2022
• Subjects: Dwarf birch; Tundra; Yakutia; Siberia
• Online Access: http://dx.doi.org/10.1002/jqs.3419; https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3419; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3419

ABSTRACT Continuous pollen and chironomid records from Lake Emanda (65°17′N, 135°45′E) provide new insights into the Late Quaternary environmental history of the Yana Highlands (Yakutia). Larch forest with shrubs (alders, pines, birches) dominated during the deposition of the lowermost sediments suggesting its Early Weichselian [Marine Isotope Stage (MIS) 5] age. Pollen‐ and chironomid‐based climate reconstructions suggest July temperatures ( T July ) slightly lower than modern. Gradually increasing amounts of herb pollen and cold stenotherm chironomid head capsules reflect cooler and drier environments, probably during the termination of MIS 5. T July dropped to 8 °C. Mostly treeless vegetation is reconstructed during MIS 3. Tundra and steppe communities dominated during MIS 2. Shrubs became common after ~14.5 ka bp but herb‐dominated habitats remained until the onset of the Holocene. Larch forests with shrub alder and dwarf birch dominated after the Holocene onset, ca. 11.7 ka bp. Decreasing amounts of shrub pollen during the Lateglacial are assigned to the Older Dryas and Younger Dryas with T July ~ 7.5 °C. T July increased up to 13 °C. Shrub stone pine was present after ~7.5 ka bp. The vegetation has been similar to modern since ca. 5.8 ka bp. Chironomid diversity and concentration in the sediments increased towards the present day, indicating the development of richer hydrobiological communities in response to the Holocene thermal maximum.