Ecology. Michael Begon

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Ecology - Michael  Begon


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factor that converts one population size to another population size, one generation later, i.e. T time intervals later. Thus:

      (4.9)equation

      But we can see from Equation 4.8 that:

      (4.10)equation

      Therefore:

      or, if we take natural logarithms of both sides:

      (4.12)equation

      r, the intrinsic rate of natural increase

      The term ln R is usually denoted by r, the intrinsic rate of natural increase. It is the rate at which the population increases in size – the change in population size per individual per unit time. Clearly, populations will increase in size for r > 0, and decrease for r < 0; and we can note from the preceding equation that:

      Summarising so far, we have a relationship between the average number of offspring produced by an individual in its lifetime, R0, the increase in population size per unit time, r (= ln R), and the generation time, T. Previously, with discrete generations (see Section 4.5.2), the unit of time was a generation. It was for this reason that R0 was the same as R.

      4.7.2 Estimating the variables from life tables and fecundity schedules

      The most precise way to calculate r is from the equation:

      We can estimate r from Equation 4.15 if we know the value of the cohort generation time Tc, which is the average length of time between the birth of an individual and the birth of one of its own offspring. This, being an average, is the sum of all these birth‐to‐birth times, divided by the total number of offspring, i.e.:

equation

      or

      This is only approximately equal to the true generation time T, because it takes no account of the fact that some offspring may themselves develop and give birth during the reproductive life of the parent.

Age (years) x ax lx mx lxmx xlxmx
0 1 000 000 1.000 0 0
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