Abstract
We ascertained a high evolutionary variability in vegetation and climate in the northeastern part of the Lena-Angara plateau during the Mid–Late Holocene. The dynamical successions are dated and correlated with the available time series of changes in natural environment in temperate and high-latitudes of the northern hemisphere. It is established that the intervals of reorganization of the natural environment in the northeastern part of the Lena-Angara plateau were proceeding in the quasi-millennial regime obeying global climate rearrangement.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
