MICRO-GEOGRAPHICAL GENETIC STRUCTURE OF INIA GEOFFRENSIS IN THE NAPO-CURARAY RIVER BASIN BY MEANS OF CHESSER´SMODELS - Biology, Evolution and Conservation of River Dolphins Within South America and Asia - page 138

 mmt+1 = (F t )/8) + (( mmt )/4) + (( mft )/2) + (((2 (1-

 t and the T matrix to estimate S t + 1 is now

(2 - )/2 0 /2 /2

T = 1 -  0 0 

(2(1 - ) + (1 - ) (2 - ))/4 /8 (2 - )/4 /2

(2n(1 - ) + (n - 1) (1 - ) (1 - ))/4n ((n - 1) + 2)/8n ((n - 1)(1 + (1 - ))/4n /2

To estimate the asymptotic F-statistics, only  mm = (/(8 - 2(2 - )) needs to be
modified.
A third model that I used was for the case where both sexes could simultaneously migrate
with different migration rates (Chesser, 1991b). Then, the relevant equations were as follows:
       mmt )/4 + (         mft )/2 + ((4 -
             t /4), where   is the male migration rate and   is
the female migration rate, respectively;
2- F t + 1 =          mft +          t ;
3-  mmt+1 = (F t )/8) + ((2 -  (1 -    mmt )/4) + (1 - (1 -
         mft )/2) + (((4 - 2              t 
 mft+1 = (F t )((n - 1) + 2)/8n) + ((n - 1)(2 -
     mmt )/4n + ((1 - (1 -          mft )/2 + ((2n (1 -
        n     t /4n, where all the terms were
previously explained. With these equations, a new transition T matrix was constructed to
obtain S t+1 = TS t + C,

(4 -     )/4 0     /4 /2

T = (1 -  0 0 1- (1 -A

((2(1 - ) A) + B)/4 /8 (2 - B)/4 (1- (1 -A)/2

(2n(1 - )A + (n - 1) B)/4n ((n - 1) + 2)/8n ((n - 1)(2- B))/4n (1- (1 -A)/2