The
Flow of Energy: Higher Trophic Levels
Three
hundred trout are needed to support one man for a year.
The
trout, in turn, must consume 90,000 frogs, that must consume 27 million
grasshoppers
that live off of 1,000 tons of grass.
-- G.
Tyler Miller, Jr., American Chemist (1971)
In this lesson, we will answer the
following questions:
-
What is the efficiency with which energy
is converted from trophic level to trophic level?
-
What are the differences between assimilation
efficiency, net production efficiency, and ecological efficiency?
-
How do ecosystems differ in the amount
of biomass or number of organisms present at any point in time, and generated
over time, at each trophic level?
-
How much energy is available to humans,
and how much do we use?
-
What are the main controls on ecosystem
function?
Introduction
In our last lecture we examined the
creation of organic matter by primary producers. Without autotrophs, there
would be no energy available to all other organisms that lack the capability
of fixing light energy. However, the continual loss of energy due to metabolic
activity puts limits on how much energy is available to higher trophic
levels (this is explained by the Second Law of Thermodynamics). Today we
will look at how and where this energy moves through an ecosystem once
it is incorporated into organic matter.
Most of you are now familiar with
the concept of the trophic level (see Figure 1). It is simply
a feeding level, as often represented in a food chain or food web. Primary
producers comprise the bottom trophic level, followed by primary consumers
(herbivores), then secondary consumers (carnivores feeding on herbivores),
and so on. When we talk of moving "up" the food chain, we are speaking
figuratively and mean that we move from plants to herbivores to carnivores.
This does not take into account decomposers and detritivores (organisms
that feed on dead organic matter), which make up their own, highly important
trophic pathways.
Figure 1: Trophic levels.
The Transfer
of Energy to Higher Trophic Levels
What happens to the NPP that is produced
and then stored as plant biomass? On average, it is consumed or decomposed.
You already know the equation for aerobic respiration:
C6H12O6
+ 6 O2 -------- 6 CO2 + 6 H2O
In the process, metabolic work is
done and energy in chemical bonds is converted to heat energy. If NPP was
not consumed, it would pile up somewhere. Usually this doesn't happen,
but during periods of earth history such as the Carboniferous and Pennsylvanian,
enormous amounts of NPP in excess of consumption accumulated in swamps.
It was buried and compressed to form the coal and oil deposits that we
mine today. When we burn these deposits (same chemical reaction as above
except that there is greater energy produced) we release the energy to
drive the machines of industry, and of course the CO2 goes into
the atmosphere as a greenhouse gas. This is the situation that we have
today, where the excess CO2 from burning these deposits (past
excess NPP) is going into the atmosphere and building up over time.
But let's get back to an ecosystem
that is balanced, or in "steady state" ("equilibrium"), where annual total
respiration balances annual total GPP. As energy passes from trophic level
to trophic level, the following rules apply:
-
Only a fraction of the energy available
at one trophic level is transferred to the next trophic level. The rule
of thumb is 10%, but this is very approximate.
-
Typically the numbers and biomass of
organisms decrease as one ascends the food chain.
An Example: The Fox and the Hare
To understand these rules, we must examine
what happens to energy within a food chain. Suppose we have some amount
of plant matter consumed by hares, and the hares are in turn consumed by
foxes. The following diagram (Figure 2) illustrates how this works
in terms of the energy losses at each level.
A hare (or a population of hares)
ingests plant matter; we'll call this ingestion. Part of this material
is processed by the digestive system and used to make new cells or tissues,
and this part is called assimilation. What cannot be assimilated,
for example maybe some parts of the plant stems or roots, exits the hare's
body and this is called excretion. Thus we can make the following
definition: Assimilation = (Ingestion - Excretion). The efficiency
of this process of assimilation varies in animals, ranging from 15-50%
if the food is plant material, and from 60-90% if the food is animal material.
The hare uses a significant fraction
of the assimilated energy just being a hare -- maintaining a high, constant
body temperature, synthesizing proteins, and hopping about. This energy
used (lost) is attributed to cellular respiration. The remainder goes into
making more hare biomass by growth and reproduction. The conversion of
assimilated energy into new tissue is termed secondary production
in consumers, and it is conceptually the same as the primary production
or NPP of plants. In our example, the secondary production of the hare
is the energy available to foxes who eat the hares for their needs. Clearly,
because of all of the energy costs of hares engaged in normal metabolic
activities, the energy available to foxes is much less than the energy
available to hares.
Just as we calculated the assimilation
efficiency above, we can also calculate the net production efficiency
for any organism. This efficiency is equal to the production divided by
the assimilation for animals, or the NPP divided by the GPP for plants.
The "production" here refers to growth plus reproduction. In equation form,
we have net production efficiency = (production / assimilation), or
for plants = (NPP / GPP). These ratios measure the efficiency with
which an organism converts assimilated energy into primary or secondary
production.
These efficiencies vary among organisms,
largely due to widely differing metabolic requirements. For instance, on average vertebrates
use about 98% of assimilated energy for metabolism, leaving only 2% for
growth and reproduction. On average, invertebrates use only ~80% of assimilated
energy for metabolism, and thus exhibit greater net production efficiency
(~20%) than do vertebrates. Plants have the greatest net production efficiencies,
which range from 30-85%. The reason that some organisms have such low net
production efficiencies is that they are homeotherms, or animals
that maintain a constant internal body temperature. This requires much
more energy than is used by poikilotherms, which are organisms that do not regulate their temperatures internally.
Just as we can build our understanding
of a system from the individual to the population to the community, we
can now examine whole trophic levels by calculating ecological efficiencies.
Ecological
efficiency is defined as the energy supply available to trophic level
N + 1, divided by the energy consumed by trophic level N. You might think
of it as the efficiency of hares at converting plants into fox food. In
equation form for our example, the ecological efficiency = (fox production
/ hare production).
Thinking about ecological efficiency
brings us back to our first rule for the transfer of energy through trophic
levels and up the food chain. In general, only about 10% of the energy
consumed by one level is available to the next. For example, If hares consumed
1000 kcal of plant energy, they might only be able to form 100 kcal of
new hare tissue. For the hare population to be in steady state (neither
increasing nor decreasing), each year's consumption of hares by foxes should
roughly equal each year's production of new hare biomass. So the foxes
consume about 100 kcal of hare biomass, and convert perhaps 10 kcal into
new fox biomass. In fact, this ecological efficiency is quite variable,
with homeotherms averaging 1- 5% and poikilotherms averaging 5-15%. The
overall loss of energy from lower to higher trophic levels is important
in setting the absolute number of trophic levels that any ecosystem can
contain.
From this understanding, it should
be obvious that the mass of foxes should be less than the mass of hares,
and the mass of hares less than the mass of plants. Generally this is true,
and we can represent this concept visually by constructing a pyramid of
biomass for any ecosystem (see Figure 3).
Figure 3. A pyramid of biomass showing
producers and consumers.
Pyramids of Biomass,
Energy, and Numbers
A pyramid of biomass is a representation
of the amount of energy contained in biomass, at different trophic levels
for a given point in time (Figure 3, above, Figure 4b below). The
amount of energy available to one trophic level is limited by the amount
stored by the level below. Because energy is lost in the transfer from
one level to the next, there is successively less total energy as you move
up trophic levels. In general, we would expect that higher trophic levels
would have less total biomass than those below, because less energy is
available to them.
We could also construct a pyramid
of numbers, which as its name implies represents the number of organisms
in each trophic level (see Figure 4a). For the oceans as shown in
Figure 4, the bottom level would be quite large, due to the enormous number
of small algae. For other ecosystems, the pyramid of numbers might be inverted:
for instance, if a forest's plant community was composed of only a handful
of very large trees, and yet there were many millions of insect grazers
which ate the plant material.
Just as with the inverted pyramid
of numbers, in some rare exceptions, there could be an inverted pyramid
of biomass, where the biomass of the lower trophic level is less than the
biomass of the next higher trophic level. The oceans are such an exception
because at any point in time the total amount of biomass in microscopic
algae is small. Thus a pyramid of biomass for the oceans can appear inverted
(see
Figure 4b). You should now ask "how can that be?" If the amount of
energy in biomass at one level sets the limit of energy in biomass at the
next level, as was the case with the hares and foxes, how can you have
less energy at the lower trophic level? This is a good question, and can
be answered by considering, as we discussed in the last lecture, the all
important aspect of "time". Even though the biomass may be small, the RATE
at which new biomass is produced may be very large. Thus over time it is
the amount of new biomass that is produced, from whatever the standing
stock of biomass might be, that is important for the next trophic level.
We can examine this further by constructing
a pyramid of energy, which shows rates of production rather than
standing crop. Once done, the figure for the ocean would have the characteristic
pyramid shape (see Figure 4c). Algal populations can double in a
few days, whereas the zooplankton that feed on them reproduce more slowly
and might double in numbers in a few months, and the fish feeding on zooplankton
might only reproduce once a year. Thus, a pyramid of energy takes into
account the turnover rate of the organisms, and can never be inverted.
Figure 4: Pyramids of numbers, biomass,
and energy for the oceans.
We see that thinking about pyramids
of energy and turnover time is similar to our discussions of residence
time of elements. But here we are talking about the residence time of "energy".
The residence time of energy is equal to the energy in biomass divided
by the net productivity, Rt = (energy in biomass / net productivity).
If we calculate the residence time of energy in the primary producers of
various ecosystems, we find that the residence times range from about 20-25
years for forests (both tropical rainforests and boreal forests), down to ~3-5 years for grasslands, and finally down
to only 10-15 days for lakes and oceans. This difference in residence time
between aquatic and terrestrial ecosystems is reflected in the pyramids
of biomass, as discussed above, and is also very important to consider
in analyzing how these different ecosystems would respond to a disturbance
or what scheme might best be used to manage the resources of the ecosystem.
Humans and Energy
Consumption
All of the animal species on earth are
consumers, and they depend upon producer organisms for their food. For
all practical purposes, it is the products of terrestrial plant productivity
that sustain humans. What fraction of the terrestrial NPP do humans use,
or, "appropriate"? It turns out to be a surprisingly large fraction. Let's
use our knowledge of ecological energetics to examine this very important
issue. (Why NPP? Because only the energy "left over" from plant metabolic
needs is available to nourish the consumers and decomposers on Earth.)
We can start by looking at the Inputs
and Outputs:
Inputs: NPP, calculated as
annual harvest. In a cropland NPP and annual harvest occur in the same
year. In forests, annual harvest can exceed annual NPP (for example, when
a forest is cut down the harvest is of many years of growth), but we can
still compute annual averages.
Outputs: 3 Scenarios
-
How much NPP humans use directly, as
food, fuel, fiber, timber. This gives a low estimate of human appropriation
of NPP.
-
Total productivity of lands devoted
entirely to human activities. This includes total cropland NPP, and also
energy consumed in setting fires to clear land. This gives a middle
estimate.
-
A high estimate is obtained by
including lost productive capacity resulting from converting open land
to cities, forests to pastures, and due to desertification and other overuse
of land. This is an estimate of the total human impact on terrestrial productivity.
Units: We will use the Pg
or Pedagram of organic matter (= 1015 g, = 109 metric
tons, = 1 "gigaton") (1 metric ton = 1,000 kg).
Table 1 provides estimates of
total NPP of the world. There is some possibility that below-ground NPP
is under-estimated, and likewise marine NPP may be underestimated because
the contribution of the smallest plankton cells is not well known. Total
= 224.5 Pg
Table 1: Surface area
by type of cover and total
(from Atjay et al. 1979 and De
Vooys 1979).
Ecosystem Type
|
Surface area
(x 106 km2)
|
NPP
(Pg)
|
Forest |
31 |
48.7 |
Woodland,
grassland, and savanna |
37 |
52.1 |
Deserts |
30 |
3.1 |
Arctic-alpine |
25 |
2.1 |
Cultivated
land |
16 |
15.0 |
Human
area |
2 |
0.4 |
Other
terrestrial
(chapparral, bogs, swamps, marshes) |
6 |
10.7 |
Subtotal
terrestrial |
147 |
132.1 |
Lakes
and streams |
2 |
0.8 |
Marine |
361 |
91.6 |
Subtotal
aquatic |
363 |
93.4 |
Total |
510 |
224.5 |
1. The Low Calculation: (See Table 2)
(a) Plant material directly
consumed = 5 billion people X 2500 kcal/person/day X 0.2 (to convert
kcal -- organic matter) = 0.91 Pg organic matter. If we assume that 17%
of these calories derive from animal products, humans directly consume
0.76 Pg of plant matter. Estimate of human harvest of grains and other
plant crops is 1.15 Pg annually. This implies loss, spoilage, or wastage
of 0.39 Pg, or 34% of the total harvest.
(b) Consumption by livestock:
estimates range from 2.8 to 5 Pg, and there seems to be some uncertainty
here. Our low estimate uses 2.2 Pg.
(c) Forests: harvest of wood
for construction and fiber is well known. Amount used for firewood, especially
in tropics, is not. The table gives a low estimate.
(d) Fish harvest: 0.075 Pg
wet weight = 0.02 Pg dry wt. If we assume the average fish is two trophic
transfers (@ 10% each) above primary producers, the NPP to produce those
fish was 2 Pg annually.
Total: Humans
consume 7.2 Pg of organic matter directly each year. This is about 3 %
of the biosphere's total annual NPP.
Table 2: Amount
of NPP used directly by
humans and domestic animals
Source
|
NPP used
(Pg)
|
Cultivated
land, food |
0.8 |
Domestic
animal fodder |
2.2 |
Wood
products Construction,
FiberFirewood |
1.2
1.0 |
Fisheries
(0.020 dry wt. Harvested) |
2.0 |
Total |
7.2 |
Percent
NPP (7.2/224.5) |
3.2 |
2. The Intermediate Calculation:
(See Table 3)
We add to the low calculation
the amount of NPP co-opted by humans. This is:
(a) All cropland NPP
(b) All pastureland that was converted
from other ecosystem types, NPP consumed by livestock on natural grazing
land, and human-set fires
(c) A number of forest land uses
(d) Human occupied areas including
lawns, parks, golf courses, etc.
Total is 42.6 Pg
of NPP per year, or 19% of world NPP.
Table 3:
Intermediate calculation of NPP
co-opted by humans
Source
|
NPP
Co-opted
(Pg)
|
Cultivated
land |
15.0 |
Grazing
land:
Converted pastures
Consumed on natural grazing lands
Burned on natural grazing land
Subtotal |
9.8
0.8
1.0
11.6 |
Forest
land:
Killed during harvest, not used
Shifting cultivation
Land clearing
Forest plantation productivity
Forest harvests
Subtotal |
1.3
6.1
2.4
1.6
2.2
13.6 |
Human-occupied
areas |
0.4 |
SUBTOTAL
TERRESTRIAL |
40.6 |
Aquatic
ecosystems |
2.0 |
TOTAL |
42.6 |
Percent
terrestrial co-opted
(40.6/132.1) |
30.7 |
Percent
aquatic co-opted
(2.0/92.4) |
2.2 |
3. The High Calculation: (See
Table 4)
For the high estimate we now include
both co-opted NPP and potential NPP lost as a consequence of human activities:
(a) Croplands are likely
to be less productive than the natural systems they replace. If we use
production estimates from savanna-grasslands, it looks like cropland production
is less by 9 Pg.
(b) Forest conversion to pasture:
the roughly 7 million km2 of forest converted to pasture represents
a loss of 1.4 Pg.
(c) Overuse: Some 35 million
km2 of land has been made more arid and less productive as a
result of human overuse, some 15 million km2 severely so. Using
dry savanna estimates of NPP, global NPP has been reduced by 4.5 Pg.
(d) Land conversion: Assuming
the 2 million km2 of land in cities, highways, etc. had a productivity
equivalent to natural forests, 2.6 Pg of NPP is foregone.
The total for the high
estimate is 58.1 Pg of NPP used, co-opted, or lost. We also must add the
potential NPP to the world estimated NPP before we compute the fraction
appropriated by humans. This gives us 58.1/149.6, or nearly 40% of potential
terrestrial production (about 25 % of terrestrial + aquatic production).
Caveat: These estimates are based on best available data and are approximate.
They probably give the correct order of magnitude.
Table 4: High calculation
of NPP co- opted by humans.
Additions to Table 3 from processes
that co-opt or degrade NPP.
Process
|
Amount
(Pg)
|
Previous
terrestrial total (Table 3) |
40.6 |
Decreased
NPP in agriculture |
9 |
Conversion
of forest to pasture |
1.4 |
Desertification |
4.5 |
Loss
to human areas |
2.6 |
Total
terrestrial |
58.1 |
Percent
terrestrial co-opted or lost
(58.1/149.8) |
38.8 |
Percent
terrestrial plus aquatic co-opted
or lost [60.1/(149.8+92.4)] |
24.8 |
Inferences:
What can we conclude from the above
analysis of the fate of net primary production in our world?
(a) Human use of marine
productivity is relatively small. Moreover, although major fish stocks
are heavily fished, and many coastal areas are severely polluted, human
impact on the seas is less than on land.
(b) On land, one species, Homo
sapiens, commands about 40% of the total terrestrial NPP. This has
probably never occurred before in earth's history.
(c) There are many consequences of
this co-option of NPP by humans. The consequences include environmental
degradation, species extinctions, and altered climate.
(d) Human "carrying capacity" on
earth is hard to estimate, because it depends upon affluence of a population
and the technology supporting that population. But at present levels of
affluence and technology, a population 50 to 100% larger than we have today
would push our use of terrestrial NPP to well over 50% of the available
production, and the attending degradation of ecosystems on earth (e.g.,
air and water pollution) would be of major concern. Thus the limits to
unchecked growth must be very near. Notice that the lower we "feed" on
the trophic chain, the more efficient the web of life becomes -- eating
animals that eat animals that eat plants is a very inefficient use of solar
energy.
Controls on Ecosystem Function
Now that we have learned something
about how ecosystems are put together and how materials and energy flow
through ecosystems, we can better address the question of "what controls
ecosystem function"? There are two dominant theories of the control of
ecosystems. The first, called bottom-up control, states that it
is the nutrient supply to the primary producers that ultimately controls
how ecosystems function. If the nutrient supply is increased, the resulting
increase in production of autotrophs is propagated through the food web
and all of the other trophic levels will respond to the increased availability
of food (energy and materials will cycle faster).
The second theory, called
top-down
control, states that predation and grazing by higher trophic levels
on lower trophic levels ultimately controls ecosystem function. For example,
if you have an increase in predators, that increase will result in fewer
grazers, and that decrease in grazers will result in turn in more primary
producers because fewer of them are being eaten by the grazers. Thus the
control of population numbers and overall productivity "cascades" from
the top levels of the food chain down to the bottom trophic levels.
So, which theory is correct? Well,
as is often the case when there is a clear dichotomy to choose from, the
answer lies somewhere in the middle. There is evidence from many ecosystem
studies that BOTH controls are operating to some degree, but that NEITHER
control is complete. For example, the "top-down" effect is often very strong
at trophic levels near to the top predators, but the control weakens as
you move further down the food chain. Similarly, the "bottom-up" effect
of adding nutrients usually stimulates primary production, but the stimulation
of secondary production further up the food chain is less strong or is
absent.
Thus we find that both of these controls
are operating in any system at any time, and we must understand the relative
importance of each control in order to help us to predict how an ecosystem
will behave or change under different circumstances, such as in the face
of a changing climate.
Summary
-
Only a fraction of the energy available
at one trophic level is transferred to the next trophic level; the fractions
can vary between 1-15%, with an average value of 10%.
-
Typically the numbers and biomass of
organisms decreases as one ascends the food chain.
-
We can construct pyramids of biomass,
energy, and numbers to represent the relative sizes of trophic levels in
ecosystems. Pyramids can often be "inverted" as a consequence of high production
rates at lower trophic levels.
-
The human diet is derived from plant
material. Humans may consume, co-opt or make unavailable as much as 40%
of the earth's total terrestrial NPP for food, land, and other uses.
-
Ecosystem function is controlled mainly
by two processes, "top-down" and "bottom-up" controls.
Review
Suggested Readings
-
Wessells, N.K. and J.L. Hopson. 1988.
Biology.
New York: Random House, ch. 44
- Townsend, C.R., J.L. Harper, and M.
Begon. 2000. Essentials of Ecology. Blackwell Science.
All materials © the Regents of
the University of Michigan unless noted otherwise.
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