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Equations
   Defining
Metapopulations
The variables
    Time: best measured in generations but most convenient for us
             to measure time in years. Tm=1/emin

       pe = probability of local Extinction
    1" pe = probability of local Persistence
       pc = probability of local colonization
!      x = number of patches
      Px = probability of regional persistence
       f = fraction of sites occupied
!      i = effect of increasing patch occupancy
       r = intensity of rescue
       N e = effective (breeding) population size
!
df
 Levins (1969) equation was basically                    dt
                                                              = cf (1" f ) " ef
  Note that C " E # $ is analogous to G = B " D

  Bottom line, df = C ! E , and !
               dt
                                there are four typical models
  for estimating C and E:
  !                           !
                                                     Extinction
                                   Independent                     Rescue
Colonization




                          df                            df
               External   dt
                               = pc (1" f ) " pe f      dt
                                                             = pc (1" f ) " e(1" f ) f


               Internal   df
                               = if (1" f ) " pe f      df
                                                             = if (1" f ) " e(1" f ) f
               !          dt               !            dt




               !                          !
The method
Persistence of one patch over time
                       1" pe
Persistence of one patch over two time periods is:
                                           2
             (1" pe )(1" pe ) = (1" pe )
Persistence of one patch over n time periods is:
          !                      n
                      (1" pe )
Persistence of two patches over time is:
!
                     1" pe1 pe 2
Persistence of many patches over time is:
         !                           x
                   Px = 1" ( pe )
         !
Assumptions
    Patches are homogenous in size, distance from
      each other, habitat quality, food, CC

    All patches have same pc and pe over all time
      periods

    pc and pe are independent of patch occupation
                !      !
    Instantaneous response to !

    No diffusion effect and no spatial structure
!
f = fraction of occupied patches
    (1" f ) = fraction of unoccupied patches
    C = pc (1" f )
!      rate of colonization in one time period thru
       immigration. We use it as though it were a
       probability. C is dependent on patch suitability
       (area, critical habitat, food, predators,
       competitors, disease, distance from other
       occupied patches) & proportion of unoccupied
       patches.
    E = pe f
       rate of extinction in one time period (we must use
       as though it’s a probability).
                   df
                   dt   = pc ( ! f )! pe f
                             1
One External Source (Propagule Rain)

A source that is outside the metapopulation

pc is constant

             df
If stable,   dt   = 0 then solve equation for zero


                     0 = pc (1" f ) " pe f
                      ˆ          pc
                      f =
                            ( pc + pe )
      !
Multiple Internal Sources

    Each occupied internal site produces an excess of
    propagules that can colonize unoccupied patches

       i = effect of increasing patch occupancy
    pc = if because C depends only on patch occp’ncy

!   If stable,   df
                 dt   = 0 then solve equation for zero
            !
                           0 = if (1" f ) " pe f
                              ˆ = 1" pe
                              f
                                       i
             !
Rescue

If propagules land in occupied sites, they can "Ne
which # pe. If more sites are occupied then more
propagules will be available for rescue

  r = combination of Ne and migration rate
pe = r(1" f ) because E depends on breeding pop’n

             df
If stable,   dt   = 0 then solve equation for zero

                   0 = pc (1" f ) " r(1" f ) f
                           ˆ = pc
                           f
                                r
    !
Closed
Propagules arise only from w/in the metapop’n
& patches rescue each other
             df
If stable,   dt   = 0 then solve equation for zero
                  0 = if (1" f ) " r(1" f ) f
Oops, can’t solve for f so we must weigh possible
results based on likely values of i and r. Barbour &
Pugliese ’05 show that there are thresholds, below
   !
which all solutions indicate total extinction of the
metapop’n. Thus, in the end, most closed
metapopulations will expire without a stabilizing
influence from outside.
Making models realistic

All metapop’n models begin with these
fundamental equations and then add
procedures for modeling the variables and
factors affecting the variables.
  b = per capita birth rate
 d = per capita death rate
 ! = P of catastrophic destruction of a patch
 ! = P of migrant making it to a patch
 ! (x )= lacunarity (index of l’scape texture)
 µij = enemy-victim relationship

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Metapop Equations

  • 1. Equations Defining Metapopulations
  • 2. The variables Time: best measured in generations but most convenient for us to measure time in years. Tm=1/emin pe = probability of local Extinction 1" pe = probability of local Persistence pc = probability of local colonization ! x = number of patches Px = probability of regional persistence f = fraction of sites occupied ! i = effect of increasing patch occupancy r = intensity of rescue N e = effective (breeding) population size !
  • 3. df Levins (1969) equation was basically dt = cf (1" f ) " ef Note that C " E # $ is analogous to G = B " D Bottom line, df = C ! E , and ! dt there are four typical models for estimating C and E: ! ! Extinction Independent Rescue Colonization df df External dt = pc (1" f ) " pe f dt = pc (1" f ) " e(1" f ) f Internal df = if (1" f ) " pe f df = if (1" f ) " e(1" f ) f ! dt ! dt ! !
  • 4. The method Persistence of one patch over time 1" pe Persistence of one patch over two time periods is: 2 (1" pe )(1" pe ) = (1" pe ) Persistence of one patch over n time periods is: ! n (1" pe ) Persistence of two patches over time is: ! 1" pe1 pe 2 Persistence of many patches over time is: ! x Px = 1" ( pe ) !
  • 5. Assumptions Patches are homogenous in size, distance from each other, habitat quality, food, CC All patches have same pc and pe over all time periods pc and pe are independent of patch occupation ! ! Instantaneous response to ! No diffusion effect and no spatial structure !
  • 6. f = fraction of occupied patches (1" f ) = fraction of unoccupied patches C = pc (1" f ) ! rate of colonization in one time period thru immigration. We use it as though it were a probability. C is dependent on patch suitability (area, critical habitat, food, predators, competitors, disease, distance from other occupied patches) & proportion of unoccupied patches. E = pe f rate of extinction in one time period (we must use as though it’s a probability). df dt = pc ( ! f )! pe f 1
  • 7. One External Source (Propagule Rain) A source that is outside the metapopulation pc is constant df If stable, dt = 0 then solve equation for zero 0 = pc (1" f ) " pe f ˆ pc f = ( pc + pe ) !
  • 8. Multiple Internal Sources Each occupied internal site produces an excess of propagules that can colonize unoccupied patches i = effect of increasing patch occupancy pc = if because C depends only on patch occp’ncy ! If stable, df dt = 0 then solve equation for zero ! 0 = if (1" f ) " pe f ˆ = 1" pe f i !
  • 9. Rescue If propagules land in occupied sites, they can "Ne which # pe. If more sites are occupied then more propagules will be available for rescue r = combination of Ne and migration rate pe = r(1" f ) because E depends on breeding pop’n df If stable, dt = 0 then solve equation for zero 0 = pc (1" f ) " r(1" f ) f ˆ = pc f r !
  • 10. Closed Propagules arise only from w/in the metapop’n & patches rescue each other df If stable, dt = 0 then solve equation for zero 0 = if (1" f ) " r(1" f ) f Oops, can’t solve for f so we must weigh possible results based on likely values of i and r. Barbour & Pugliese ’05 show that there are thresholds, below ! which all solutions indicate total extinction of the metapop’n. Thus, in the end, most closed metapopulations will expire without a stabilizing influence from outside.
  • 11. Making models realistic All metapop’n models begin with these fundamental equations and then add procedures for modeling the variables and factors affecting the variables. b = per capita birth rate d = per capita death rate ! = P of catastrophic destruction of a patch ! = P of migrant making it to a patch ! (x )= lacunarity (index of l’scape texture) µij = enemy-victim relationship