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From Momo, F.R., Doyle, S.R., Ure, J.E., 2012. Hierarchical Energy Dissipation in
Populations. In: Jordán, F., Jørgensen, S.E. (Eds), Models of the
Ecological Hierarchy: From Molecules to the Ecosphere. Elsevier B.V., pp. 533–543.
ISBN: 9780444593962
Copyright © 2012 Elsevier B.V. All rights reserved
Elsevier
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31
Hierarchical Energy Dissipation
in Populations
Fernando R. Momo*, **, Santiago R. Doyle*, José E. Ure*
*
INSTITUTO DE C IENCIAS, UNIVERSIDAD NACIONAL DE GENERAL SARMIENTO, J.M. GUTIÉRR EZ
1 15 0, LO S P O L V O RI N E S , ARGE NT I N A; C O N I C ET , AR G ENT I NA, * * INEDES, UNIVERS IDAD
NACIONAL DE LUJÁN, ARGENTINA
This chapter is devoted to three great ecologists: Leonardo Malacalza, Eduardo
Rapoport and Ramón Margalef (in memoriam). They all have been a guide, an
inspiration and an example.
31.1 Introduction to Populations as Thermodynamic
Systems
Biological populations are characterized by structural and demographic magnitudes such
as density, age or stage structure, and growth and mortality rates. These are the typical
magnitudes that are studied by ecologists, who analyze the relationships among them in
terms of population dynamics. There is, however, another point of view to study biological populations, which consider them as open thermodynamic systems, i.e., systems
that interchange matter and energy with their environment, and are, moreover, the units
of entropy production and entropy exchange (Michaelian, 2005).
Populations are constituted by individuals, which are complex dissipative systems that
remain far from thermodynamic equilibrium (Ulanowicz and Hannon, 1987). But the
population is a system of a higher order of complexity: in a population, individuals born and
die, also grow, and, eventually, suffer metamorphosis or changes in their reproductive stage.
The set of all interacting individuals constitute the system that we call population. It is
a complex dissipative system, which is capable to regulate certain emergent properties.
If we adopt this point of view, it is clear that populations are also far from its thermodynamic equilibrium. Populations are, in general, in some stationary state characterized by a given biomass, density, age (or stage) structure, and a specific regime of
energy and entropy fluxes.
In order to formalize these concepts, we must carefully define the different terms in stake.
We will focus animal populations, and start with a very imperfect analogy, considering
the population like a sort of “turbine” activated by a “fall” of energy, which is sourced by
Models of the Ecological Hierarchy. DOI: http://dx.doi.org/10.1016/B978-0-444-59396-2.00031-6
ISSN 0167-8892, Copyright Ó 2012 Elsevier B.V. All rights reserved
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food. Because populations are open systems, they dissipate low-quality energy (heat) and
pour degraded matter to the environment. Of course, food is not the sole energy that
population receives; however, we assume here that it is at thermal equilibrium and other
forms of energy such as heat or light are in a stationary regime. Then, the biological work
made by individuals (that is translated as demographic changes at the population level)
will be supported by the chemical energy in the food.
The energetic gradient under which populations work is given by the difference of free
energy between source and sink (i.e., between foods and waste). We will call this gradient
DESourSink (see Fig. 31.1), that is, the free energy contained in the food (ESo) minus the
energy contained in the detritus (ESi). The flux of energy running throughout a population
is directly proportional to this gradient.
According to Prigogine (1978), in nonequilibrium stationary states, the perturbation in
the produced entropy is given by
X
1d 2
d S ¼
ðdJp dXp Þ:
2 dt
(1)
Here, dS is the perturbation in entropy production, the terms dJp are the deviation in
the rates of various irreversible processes, and dXp are the deviations in the generalized
forces (affinities, gradients of temperature, etc.).
The question is what happens when the system (i.e., the population) is far from
equilibrium and, moreover, far from the stationary regime?
In order to tackle this problem, we propos to follow the previous analogy and consider
that, like in another physical systems, when a flux that is proportional to a given gradient
exists, entropy dissipation is proportional to the square of that gradient (it is non linear).
We can synthesize these as follows:
dE
fk1 DESourSink
dt
de S
fk2 ðDESourSink Þ2 :
dt
(2)
Source
(food)
Energy flux
(dE/dt)
Population (biomass)
Storage
D E = ESo - ESi
Dissipation
(deS/dt)
Sink
(detritus)
FIGURE 31.1 Conceptual representation of biological populations as dissipative systems.
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Chapter 31 • Hierarchical Energy Dissipation in Populations
535
de S
represents the amount of entropy dissipated by the population to its
dt
environment per unit of time.
Energy flows (Fig. 31.1) can be associated to population dynamics and to different
demographic phenomena: inputs or energy are transformed basically in work and
biomass. The biological work is measurable throughout the metabolic rate of the individuals in the population and, due to the second law of thermodynamics it is in a direct
correlation with a fraction of the entropy exchange between organisms and environment.
The other fraction of the entropy exportation is measured by mortality.
The amount of energy that is not spent is stored as new biomass.
Finally, egestion, excretion, and other matter exchange phenomena are responsible of
the remainder flux of energy (and entropy) to the detritus (the sink).
When DE varies abruptly, the regime of the system becomes far from the stationary
state; the rapid (nonlinear) increase of the dissipated entropy allows the system to
recovery the stationary regime but in a new state. In a population, this new state will be
defined by a given age and size structure.
In Eqn (2),
31.2 Demography and Thermodynamics
In a recent work, we have shown that several modifications in the population demography can be interpreted in a thermodynamic way (Momo et al., 2010). In fact, we can say
that populations are dissipative systems because they maintain their age structure and
biomass by pumping entropy to their environment.
Assuming that if populations make some kind of mechanical work, this work will be
transformed finally to heat, and by analogy with other thermodynamic systems, we can
postulate the following relationship:
dS
1
¼
dU
T
(3)
where S is the entropy, U is the internal energy, and T is temperature. However, this
relationship is incomplete for ecological purposes because dissipative systems maintain
their organization by mean of fluxes of entropy and energy, and it is more accurate to
write:
dS=dt
1
¼ :
T
dU=dt
(4)
Equation (4) represents the relationship between entropy expulsion, and the energy
exchange between the system and its environment. If both fluxes are calculated, the
1
magnitude s ¼ may be interpreted as a demographic sensitivity.
T
Two demographic tools can be used to this approach: the first are the Leslie matrices,
which represent populations divided into age classes of the same length as the time step,
and that can be used to simulate the population dynamics; the second are the survival
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curves, which show the percent of a cohort that survives until a given age, and can be
associated to different demographic traits suggesting how population allocate the
available energy.
In Momo et al. (2010), we have also shown that Leslie matrices contain information
about the way in which a population dissipates energy and pumps entropy outside the
system, and have also shown that r-selected populations have higher entropic costs than
K-selected populations, whereas populations having Type I survival curves (high survival
of immature and low survival of adults) have lower entropic costs than populations with
Type IV (high larvae mortality) survival curves.
Consider now a Leslie matrix (A) with three age classes, where only the last age class
reproduces
2
0
A ¼ 4 s1
0
0
0
s2
3
f
0 5;
s3
(5)
where f is the fertility and si are survival rates.
In this demographic model, we can represent different trade-off, as we will show in
a moment. In that work, authors assumed that f ¼ 1/(s1s2) in order to have a l1 > 1
(growing populations); then, numerical simulations were performed considering
different cases having more or less fertility combined with more or less survivals (i.e., the
r–K trade-off). In addition, the relationship between s1 and s2 was changed in order to
simulate the shift between different survival curves (from type I to IV).
Computing the demographic entropy (H ¼ Spi log(pi)) for each gradient, authors
observed that both trade-offs are not equivalent and K-selected populations maximize
their demographic entropy (Fig. 31.2).
Despite the interest of this approximation, it is strongly limited because the relationship shown in Eqn (3) is only true under linear and near to equilibrium conditions,
and the demographic entropy considered in the model is only a measurement of the
relative abundance of individuals of different ages; so, it is not a true entropy in a thermodynamic sense, and it does not represent a flux. In consequence, it is necessary to
deepen in the problem in order to catch the complete picture including nonlinear and far
from equilibrium regimes and energy and entropy fluxes.
31.3 Body Size and Metabolic Rate
The metabolic rate is the fundamental biological rate, because it is a measure of energy
uptake, transformation, and allocation (Brown et al., 2004). Metabolic rate is linked to the
rates of many other biological activities at various hierarchical levels of organization
(Brown et al., 2004; Glazier, 2005). Moreover, studies of metabolism are useful tools for
understanding the patterns of energy flow in populations and ecosystems (Glazier, 1991;
Doyle and Momo, 2009; Doyle et al., 2012).
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Chapter 31 • Hierarchical Energy Dissipation in Populations
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FIGURE 31.2 Phase space of populations following r–K or Type IV—Type I trade-offs. Horizontal axis are percent of
ages 2 and 3; the vertical axis indicates the entropy. Points indicate the level of demographic entropy.
Several variables influence the metabolic rate of organisms; among these, temperature
and body size (generally understood as body weight) are the most important (Gillooly
et al., 2001).
Temperature is the dominant abiotic factor that affects metabolic rate in ectothermic
organisms, and its effect on metabolic rate is due to the thermodynamic nature of the
kinetics of chemical reactions and enzyme conformational changes (Hill et al., 2004). In
ectothermic animals, metabolic rate increases exponentially with temperature within
a certain range up to a maximum value, and further increase in temperature produces
a decrease in metabolic rate (Schmidt-Nielsen, 1997). The acute response of metabolic
rate to temperature is due to the thermodynamic nature of the kinetics of chemical
reactions and enzyme conformational changes (Hill et al., 2004).
Body size is the most biotic factor that regulates metabolic rate, and it has been
recognized like that since the seminal work of Kleiber (1932). More recently, the books by
Peters (1983) and Schmidt-Nielsen (1984) have summarized some regularities relating the
body size with the physiological and population parameters, including metabolic rate.
Knowledge of the relationship between body size and metabolic rate has multiple
applications in ecology; for instance, it is possible to estimate the whole respiration of
a population from its body size distribution. In an animal population, size distribution is
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a measure that can be obtained easily, and thus the whole respiration of the population can be estimated with a relatively low survey effort (LaBarbera, 1989; Han and
Straskraba, 2001).
The expected relationship between metabolic rate (MR) and body weight (W) is an
allometric scaling:
MR ¼ a$W b :
(6)
The constant a is a proportionality parameter whose value is equal to the metabolic rate
of an individual having a unit body weight; the parameter b is known as the scaling
exponent. The metabolic rate per unit of biomass or specific metabolic rate (SMR) can be
similarly calculated as:
SMR ¼ a$W b
1
:
(7)
It is clear that the metabolism of a given size class in the population can be calculated by
multiply Eqn (7) by the abundance of the class.
31.4 Going Further: Thermodynamic Regime of
Populations
Let us go back to the Prigogine (1978) approximation: if a population is in a stationary
state, its amount of internal (structural) entropy remains roughly constant. If it is
assumed that the system is near the equilibrium, we can expand the function of entropy
as follows:
1
S ¼ S þ dS þ d2 S;
2
(8)
were S* denotes the entropy in the stationary state, and dS is the fluctuation in entropy
around that stationary value. Because d2S can be considered a Lyapunov function of the
system (Jørgensen and Svirezhev, 2004), a given state will be stable (in both the thermodynamics sense and the Lyapunov sense) if it is verified that dS ¼ 0, d2 S < 0, and
d 2
ðd SÞ > 0. In this condition, biomass, density, and age structure of the population
dt
di S
de S
¼
, and the total amount of internal entropy of the popremain constant, while
dt
dt
ulation remains constant. Hence, the mortality rate, integrated through all ages, equals
the birthrate of the population.
However, populations rarely are near to the equilibrium and therefore these relationships ought to be different, because the entropy pumping to the environment grows
nonlinearly with the energy gradient as is shown in Eqn (2). The distance from equilibrium can be measured by mean of one of the classic magnitudes used in the literature,
among which exergy is one which has been most widely used (Jørgensen and Svirezhev,
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Chapter 31 • Hierarchical Energy Dissipation in Populations
539
2004). Meysman and Bruers (2007) have proposed the use of the disequilibrium between
resource and waste products as a meaningful measure of the distance from equilibrium of
an ecological system. In the context of this chapter, this last approximation is a good way
to relate the forcing variable (the energetic cascade) with the response variable (the rate of
entropy exportation) and, moreover, the state variable of the population (its structural
entropy). We will assume that, under realistic conditions, the energetic distances between
food and detritus are large, and the population has a very low probability to be near to the
thermodynamic equilibrium.
In a far from equilibrium condition, populations fight against the Second Law in order
to maintain not only their biomass, but their organization. In this regime, higher-order
interaction terms in the relationship between forces and fluxes are not negligible.
31.5 Symmetry Breaking and Hierarchical Responses of
Population
We postulate that, when the difference of free energy between the source (food) and the
sink (detritus) starts to grow, the exportation of entropy to the environment (deS/dt) starts
to vary according to the power relation shown in Eqn (2). One might ask, however, what is
exactly deS/dt? We consider here that this rate is composed by two terms: the first
represents the metabolic dissipation of all individuals in the population, and the second
represents the mortality of every age or stage class.
The metabolic rate of a given individual, as previously exposed, is mainly determined
by its body size and environmental temperature. As a consequence, the amount of
entropy exchanged by each size class in the population will be given by the product
between the mean body size of the class, the SMR for that size, and the relative abundance of the stage; all these magnitudes are multiplyed by a constant to adjust units and
divided by T, the absolute temperature.
Mortality rates are also determined by the body size, but affect the relative abundance
of each stage.
Briefly, we can write the following:
m
m
X
de S
k3 n X
SMRi pi Bi þ k4 n
mi pi ;
¼
dt
T i¼1
i¼1
(9)
where pi ¼ ni/n is the relative abundance of the i-stage, Bi is the mean body biomass of the
i-stage, and mi is its mortality rate.
Considering that DE is growing, the flux of entropy must vary over time and we can
write:
m
m
X
d de S
d k3 n X
mi pi Þ:
SMRi pi Bi þ k4 n
ð
Þ ¼
ð
dt dt
dt T i ¼ 1
i¼1
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If we expand Eqn (10), under isothermal conditions and assuming that Bi are constant,
we obtain the following expression:
!
m
m
X
d2e S
dn k3 X
¼
SMRi pi Bi þ k4
m i pi þ
dt 2
dt T i ¼ 1
i¼1
( "
X
#
m
m
k3 X
dpi
dSMRi
þn
pi Bi
SMRi Bi þ
þ k4
T i ¼ 1 dt
dt
i¼1
X
!)
m
m
X
dpi
dmi
m þ
p1
dt
dt i
i¼1
i¼1
(11)
We can see that the first term in Eqn (11) represents the effect of the population density
variation. In the second term, we have the effect of the whole population metabolism
"
#
m
k3 X
dpi
given by the variation in the relative abundances of stages:
SMRi Bi .
T i ¼ 1 dt
Similarly, the whole population metabolism can be modified by changes in the specific
"
#
m
k3 X
dSMRi
p i Bi
. The remaining terms indicate
metabolic rate of each size class:
T i¼1
dt
the variations in the flux of entropy that depend on total mortality, influenced by relative
abundances and group mortalities variations. All these effects are summarized in
Table 31.1.
As the difference between source and sink is increasing (dDE/dt > 0), the flux of
entropy to the environment also increases. When the ratio between this rate and the
energy flow rises the critical values, symmetry can break, in consequence the population
rises a new stationary state (i.e., it becomes a new dissipative structure) characterized by
a particular amount of structural entropy.
However, the different terms of Eqn (11) change with a particular timing. The first
effect in be apparent is the physiological one (term C of Table 31.1) because individuals
Table 31.1 Mean of the Components of the Eqn (11) (Changes in the Rate of Entropy
Exchange Between Population and Environment)
A
B
C
D
E
m
m
X
dn k3 X
mi p i
SMRi pi B i þ k4
dt T i ¼ 1
i¼1
"
#
m
k3 X
dpi
SMRi B i
n
T i ¼ 1 dt
"
#
m
k3 X
dSMRi
n
pi Bi
T i¼1
dt
#
dpi
mi
dt
#
Pm
dmi
nk4
i ¼ 1 p1
dt
nk4
Pm
i¼1
!
Is the global effect produced by the change in the population density
Represents the changes in the total metabolism of the population given
by changes in the relative abundances of the different size classes
Is the change in metabolism produced by the variation in the SMR of each
size class. It represents the physiological effect of modifying the energetic
quality and quantity of food
Is the change in total mortality given by the modification of the relative
abundances of size classes
Is the change in the mortality effect due to the modification in stagespecific rates of mortality
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Chapter 31 • Hierarchical Energy Dissipation in Populations
+
↑Δ E SoSi
SMR i
+
541
Total
population
metabolism
n
(Total
population
Density)
µi
∑
modify
(Stage-specific
mortality rates)
modify
modify
pi
(i-stages
relative abundance)
FIGURE 31.3 Conceptual relationships between the different components of the entropy flux variation.
respond to a better input of food. The well-known effect of food on metabolic rates is the
reason by which standard measurement of metabolism are made in fasted animals, and
has a characteristic time scales of hours to days. Moreover, a trend to higher metabolic
rate with increasing potential food availability, a related but different phenomenon
operating at larger time scales, has been observed in several invertebrates (Brockington,
2001; Brockington and Peck, 2001; Fraser et al., 2002; Doyle et al., in press).
This change produces in a second instance a modification in the survival probability
for each size class; if the food is better, all stages have lower mortality rates but the effect is
mediated by the allometric dependence of the size. In consequence, term E is the second
in be modified and causes a shift in relative abundances of stages (term D). Changes in
relative abundances produce modifications in the total metabolism of the population
(term B).
Finally, the population density (term A) changes until the biomass rises a new state
stage. These phenomena are summarized in Fig. 31.3.
In this way, a sort of “cascade” of effects is caused by a change in energy flow
throughout the population. This succession of changes can be detected experimentally by
the measurement of the metabolic rate of the population and the Shannon entropy of size
classes (stages or ages), that is, the demographic entropy sensu (Demetrius et al., 2004,
2009). If we plot these magnitudes versus the energetic difference between food and
detritus, the phase transitions will be apparent by abrupt changes in the slope of each
curve (Fig. 31.4).
31.6 Concluding Remarks
Ecological populations involve a set of nested biological phenomena, from physiological
to demographic ones. This hierarchical structure constraints and determinates the
thermodynamic response to changes in the flux of energy. Each biological process has
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H’
TMR
(demographic
entropy)
(total
metabolic
rate)
Second
symmetry
breaking
First
symmetry
breaking
ΔE
ΔE
FIGURE 31.4 Phase diagrams of the symmetry breaking in metabolism and size structure. When the energetic skip
is high, the final stable state of the population is given by a higher metabolic rate and a lower diversity of sizes.
a characteristic velocity of response to environmental changes, so there is a successive
group of responses in the population.
The consideration of nonlinear effects in thermodynamic processes allows us to
predict some general timing in the responses and, in this way, it is possible to test
experimentally the validity of our model and hypotheses. First of all, the metabolic rate of
individuals should show changes under an increment of energy availability. In a second
phase, we should see differential changes in the mortality rates of the different size
classes. Finally, the size structure of the population should change together with its
density.
Experiments that investigate these predictions will be very important in order to
continue building a strong thermodynamic theory of ecological systems.
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