Abstract
The information about the sources of organic mat� ter (OM) in suspended matter (SM) of the boundary river–sea geosystems, conditions of its mobilization, and water migration, peculiarities of transformation, and scales of spatiotemporal variability are needed for solution of applied and fundamental problems of bio� geochemistry, sedimentology, ecology, and others. The system of the Amur River and the Sea of Okhotsk and the Sea of Japan (further on—the system, which is specific due to many causes, has remained unstudied from this standpoint. Landscapes of plains and moun� tains as well as rocks of different geological formations are drained in the watershed of the river, while prepa� ration of the sedimentary material to water migration occurs in the conditions of the continental and mon�
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.
