Abstract
The composition of the primary pollen changes during pollen transfer and redistribution over the Earth's surface and fossilization. These processes are particularly pronounced in the tundra zone. Patterns of pollen spectra formation in the subaerial and subaqueous deposits of the tundra zone were considered and the differences in the content of palynomorphs with exine rupture were revealed. The changes in the effect of regional and local taphonomic factors on Arctic tundra slopes were traced. Pollen conservation in the deposits of the tundra zone, snowfields, and wedge ice was considered.
Sign-in/Register to access full text options 
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.
