The problem of the 11th marine isotope stage from the viewpoint of the new conception of the orbital theory of the paleoclimate

It is shown that the so-called MIS-11 problem is not a problem of the Milankovitch theory but is a problem of his followers. The existence of this problem points out the drawbacks of the corresponding theoretical notions that associate the insolation variations with the global climate changes in the Pleistocene. The conclusion is reached that the MIS 11 problem is a particular case of the more common problem of the disparity of the orbital induced insolation variations and global climate changes in geological time intervals.