Abstract
Landscape-bionomic zoning reveals the effect of hydrological and geomorphological links of the physical-geographical process on the bionomic differentiation of the Barents Sea floor. The polar front separates the Arctic water masses and communities from the subarctic ones; under the influence of warm Atlantic Current branches, extrazonal boreal biomes are formed. The geomorphological structure represents the lithogenic basis that determines the formation of bionomic types of the Barents Sea floor. It was established that each geomorphological region corresponds to one macrozoobenthos group.
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.
