BIO 412 Principles of Ecology Phil Ganter 301 Harned Hall 963-5782 |
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Alligator at Canaveral National Seashore (taken at a safe distance) |
Life Table/Demography Laboratory
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Introduction:
Within a population of a species, not all individuals are the same. We have already spoken of differences due to sex and genetic makeup. Today, we will examine the differences due to age. The age of an organism can strongly affect both the rate of mortality and natality. Just think of humans. It is very obvious that not all humans have the ability to reproduce as some are too young and some too old. It may be less obvious, but no less true, that mortality is also dependent on age, with the very young and old more likely to die. When considering a population of mixed ages, an ecologist needs to be able to predict the composition of the population in the future based on the population of today. To do this, we must have a means of taking the proportions of the population in various age classes into account. We can do this with a life table: a schedule of the probabilities of death and reproduction that covers the potential life span of an individual organism. The rates (= probabilities) of dying and reproduction in a life table are referred to as age-specific mortality and fecundity.
How do we get such a schedule? There are two general ways. One can take a snap-shot of the population at a single time and look at the proportions occurring in each age class. However, this method assumes that the population has reached a equilibrium value, called the Stable Age Distribution. A better way, but more difficult, is to follow a group of individuals born at the same time (called a cohort) until all are dead and record when each female reproduces (and how many offspring are produced). From the life table, we can calculate other ecological parameters such as expected life span (adjusted for age), the eventual stable age distribution for the population if the life table does not change with time, and the growth rate of the population.
The techniques used were developed for animal populations and are most highly developed for human populations. For that reason, the science of life tables is called demography (demos is the Greek root for people). Now the term is used for life tables for any organisms, and you often see the phrase "human demography" which is a bit redundant. Recently, plant ecologists have made good use of demographic techniques, which makes good sense if you consider that it should be easier to follow a cohort of plants due to their sessile (fixed in one place) life style.
The Life Table:
The first column of the table gives the ages into which the lifespan of the organisms will be broken.
lx = age specific survivorship -- fraction of cohort alive at the START OF THE INTERVAL
dx = age specific mortality -- number dying in the interval
qx = age specific mortality rate -- death rate for individuals of a specific age
ex = age specific life expectancy - number of years left for an organism of a particular age. IT IS NOT ALWAYS MAXIMAL AT BIRTH!!
bx = age specific natality -- number born in the interval
mx = age specific birth rate - the per female rate of offspring production for females of a particular age.
R0 = net replacement rate = the number of females alive in the next generation for each female alive in the present generation.
Tc = generation time
Calculations from the life table:
First, lets start with a life table that has no births in it, so we can work with life expectancy exclusively. We gather nx and calculate lx, qx, and ex from it! First, I should mention that, by convention, the first age inerval has the notation 0, so the number in the cohort at the start is n0.
To calculate ex, we will need to tack on another pair of columns to make it easier to do. This column is Lx, the average number alive in interval x. This is simple to do:
From this column, we can get Tx, which is the sum of all of the Lx values from x until the age that the last member of the cohort dies (this is symbolized by L°). We will use this to calculate life expectancy. To understand how this is done, one must consider the units we are using (Tx and Lx will have the same units). Remember that we defined Lx as the average number of individuals alive in an age class. You might wonder how we can reconcile these units with life expectancy, as Lx seems to be in the units "individuals" and life expectancy (ex) is in time units. However, Lx is the sum of individuals that live a particular period of time (= the duration of an age class), and so the units are actually "individuals-age class." This is not obvious from the way we calculate Lx, but it is necessary for calculating life expectancy, as we will see below.
Now, we can calculate the age specific life expectancy. This is the total
What are the units of life expectancy? Tx is in "individuals-age class" and nx is in "individuals". Dividing Tx by nx cancels out "individuals" and we are left with "age class". Thus, you will get an answer in terms of age classes. If you want to use a more universal unit, you have to convert between age class and, say, years. A life expectancy of 10 age classes is 50 years if one age class is ten years long.
If we eliminate the males and add a column containing births (total number of births by mothers in each age class), then we can calculate the net replacement rate (R0).
Mx, the age-specific birth rate is the number of births from mothers in the x age class divided by the total number of individuals in that age class
R0, the net replacement rate, is the sum over all age classes of the product of the age-specific survivorships times the age-specific birth rate. Thus, the population growth rate depends on the number of offspring each age class produces reduced by the probability of surviving to that age (remember that lx will be between 0 and 1).
The net replacement rate is a measure of population growth rate.
Before we go on, it is best if we take a second look at what we have calculated to see why the calculation results in the net replacement rate.
.
"R0 is the net replacement rate or the number of individuals in the next generation per individual in the current generation."
- You can see how this is true from the above analysis of the dimensions of the terms that contribute to the calculation of R0. If the sum is less than one, there is less than one in the next generation for each alive in the current generation, and the population is shrinking. Try dimensional analysis to further your understanding of the calculation of Tc below.
We can also calculate the approximate generation time from the same data that gave us the net replacement rate.
Gathering the Data:
Data from a local cemetary
Your first consideration should be just that: consideration. We are visiting a graveyard, which is consecrated ground and must be afforded due respect. No walking on graves, no disturbing memorials, and a serious demeanor is expected.
We want to work with a cohort that is old enough so that it is most likely that all in that cohort are dead. You will work in pairs pick a random starting point far enough from others that you will not overlap and resample data already collected by other pairs. Walk along the tombstones and record the sex of the individual, his or her birth and death dates, and calculate the age at death from 100 tombstones. If a date is missing, skip that tombstone. Skip any tombstone later than 1930.
Back in the lab, we will organize the data from the entire class by year of birth. When that is done, we will assign you a cohort to work with. We may have to combine sequential years, as we want at least 50 individuals in each cohort
In-lab data
If we can not go to the cemetery, we will use data from an old cemetery located just outside of Philadelphia, PA. The instructor will assign two sets of years to you. The first set are two to three years of data from the earliest graves and the second set are from the newest graves. You will do the calculations below on both sets of data and compare them for changes in demography.
Data Analysis:
Construct a separate life table for each cohort-by-sex combination. Use the headings below:
Make 5 year age classes, so that the age class column should read 0, 0-4, 5-9, 10-14, etc. until the last of the cohort died. X will be the number of the age class, starting with 0 and going up to 15 or so (depending on how old the oldest person in the cohort was when he or she died).
Separate the data by sex (a separate table for each sex) and calculate the death rates, survival rates, and life expectancies for each sex from your cohorts.
When you have completed the above, look to the table below for the mx data. This data comes from two populations taken during mid-century censuses. One is an island and the other is a large, industrial country. We will use both of these to see how both mortality and natality contribute to population growth. Use both sets of mx data and the survivorship data from the females in your cohorts to calculate R0 and Tc. If you are using a spreadsheet, this is easy to do.
Age Class |
Island |
Continental |
mx |
mx |
|
0-14 |
0 |
0 |
15-19 |
0.150 |
0.070 |
20-24 |
0.650 |
0.175 |
25-29 |
0.750 |
0.325 |
30-34 |
0.520 |
0.335 |
35-39 |
0.250 |
0.285 |
40-44 |
0.125 |
0.075 |
45-49 |
0.025 |
0.10 |
50+ |
0 |
0 |
Data Presentation and Interpretation:
First, present you dimensional analysis of the calculation of Tc.
Second, present the life tables for your cohort, by sex. Title each table and make sure it includes the years in which they were born in some prominent place.
Third, make two graphs:
On each graph, all four datasets should be presented (one line for females from the early cohort, one for females from the later cohort, one line for males from the early cohort, one for males from the later cohort ). Be sure that a legend is presented and that all lines look different enough to make reading the graph easy.
Fourth, present the calculations for R0 and Tc for both island and continent data.
Fifth, answer the questions below.
Thinking about the experiment:
Last updated September 9, 2006