Abstract
The paper presents the dynamics of the natural environment of the Sea of Azov under the different-scale and multidirectional changes of the climate during the last macrocycle, the epoch from the last interglacial to the modern one, including the Mikulino interglacial and Valdai glacial epochs, their development stages and phases.It has been shown that the paleogeographic development of the Sea of Azov is closely related to global climate changes and is dependent on the functioning of the Mediterranean–Pont–Caspian system.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
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 call
