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leHierarchical modelling of population growth rate from
individual capture-recapture data
Simone Tenan1,2,∗, Roger Pradel3, Giacomo Tavecchia1, Jose Manuel Igual1, Ana Sanz-Aguilar1,4,
Meritxell Genovart1, Daniel Oro1
1 Population Ecology Group, IMEDEA (CSIC-UIB), Miquel Marques 21, 07190 Esporles
(Mallorca), Spain;
2 Sezione Zoologia dei Vertebrati, MUSE - Museo delle Scienze, Corso del Lavoro e della Scienza
3, 38123 Trento, Italy (current address);
3 Biostatistics and Population Biology Group, Centre d’Ecologie Fonctionelle et Evolutive
(Campus CNRS) 1919 Route de Mende, F-34293 Montpellier, France;
4 Estacion Biologica de Donana (CSIC), Americo Vespucio s/n, E-41092 Sevilla, Spain;
∗ E-mail: Corresponding [email protected]
Running title: Hierarchical Bayesian temporal symmetry model
This article has been accepted for publication and undergone full peer review but has not been
through the copyediting, typesetting, pagination and proofreading process, which may lead to
differences between this version and the Version of Record. Please cite this article as doi:
10.1111/2041-210X.12194
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leAbstract
1. Estimating rates of population change is essential to achieving theoretical and applied goals
in population ecology, and the Pradel (1996) temporal symmetry method permits direct esti-
mation and modelling of the growth rate of open populations, using capture-recapture data
from marked animals.
2. We present a Bayesian formulation of the Pradel approach that permits a hierarchical mod-
elling of the biological and sampling processes. Two parametrisations for the temporal sym-
metry likelihood are presented and implemented into a general purpose software in BUGS
language.
3. We first consider a set of simulated scenarios to evaluate performance of a Bayesian variable
selection approach to test the temporal linear trend on survival and seniority probability,
population growth rate and detectability. We then provide an example application on indi-
vidual detection information of three species of burrowing nesting seabirds, whose populations
cannot be directly counted. For each species we assess the strength of evidence for temporal
random variation and the temporal linear trend on survival probability, population growth
rate and detectability.
4. The Bayesian formulation provides more flexibility, by easily allowing the extension of the
original fixed time effects structure to random time effects, an option that is still impractical
in a frequentist framework.
Key-words
Bayesian analysis, Balearic shearwater, Gibbs variable selection, mark-recapture, population dy-
namics, rate of population change, Scopoli’s shearwater, Storm petrel, survival, temporal symmetry
model.
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leIntroduction
The rate of change of population size over time is a process of great interest in population ecology.
Much has been written about the importance of this metric to assess the viability of a population
and the effects of management actions (e.g. Morris & Doak 2002). Different approaches exist to
estimate and model population growth and associated vital rates using capture-recapture data from
open populations, and many are implemented in freely available software such as MARK (White &
Burnham 1999) and POPAN (Arnason & Schwarz 1999). All represent multiple ways of writing the
likelihood first introduced by Jolly (1965) and Seber (1965), and differ in the way that the arrival
of new individuals into the population (i.e., local recruitment along with immigration) is modelled.
The frameworks among which animal ecologists can choose include the superpopulation approach
(Crosbie & Manly 1985; Schwarz & Arnason 1996), the temporal symmetry approach (Pradel 1996),
the parametrisation of Link & Barker (2005) and the restricted occupancy formulation of Royle &
Dorazio (2008).
The Pradel method, i.e., the temporal symmetry approach, has the unique characteristic of
combining in the same likelihood the standard-time and the reverse-time approach, simultaneously
incorporating survival and recruitment parameters and thus allowing inference on population growth
rate. The conceptual basis of the temporal symmetry of capture-recapture data derives from the
observation that the proportion of individuals that are already members of the population in the
previous sampling occasion, is the analogue of the survival rate when capture history data are
considered in reverse time order (Pollock et al. 1974; Nichols et al. 1986). Pradel (1996) termed
that proportion the ‘seniority’ parameter, reflecting the relative contribution of survivors from the
previous occasion to the population growth rate (Nichols et al. 2000).
Among the three parametrisations presented for the temporal symmetry likelihood, one uses
population growth rate ρ as a model parameter and thus allows testing of biological hypotheses
directly on ρ. Population growth rate integrates environmental effects on different vital rates and
the possibility of directly modelling ρ can be useful to investigate overall environmental influences,
especially when an environmental covariate influences multiple vital rates (Nichols & Hines 2002).
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leNichols & Hines (2002) also highlighted that temporal variance of ρ, estimated using a random
effect perspective, is highly relevant to extinction probability and ‘emphasizes the potential utility
of the direct estimation and modelling of ρ for population viability analyses’.
Here we present a Bayesian formulation of the Pradel temporal symmetry approach in which
parameter estimates are derived from the sampling of posterior distributions by MCMC methods.
The Bayesian formulation permits the hierarchical modelling of the biological and sampling pro-
cesses, allowing the extension of the original fixed time effects structure to random time effects, an
option that is still impractical in a frequentist framework. We illustrated the modelling approach
with real data on detection histories of individuals belonging to three species of burrowing nesting
seabirds, whose populations cannot be directly censused. In addition to the estimation of unex-
plained temporal variance we tested for temporal trends in model parameters. Our study species
suffer from additive mortality from longline fishing gears and alien predators at sea and at the
colonies, respectively, and it has been suggested that this mortality is causing a decline in their
populations (Barcelona et al. 2010; Cooper et al. 2003). For this reason, population trends for these
seabirds are of particular conservation interest.
Previous evidence suggested that placing constraints on some model parameters may impose
unintended constraints on others, with ρ being defined as a function of survival probability, that
in turn appears in the model (Nichols & Hines 2002). Furthermore, spurious trends in ρ can arise
from changes in the relative number of marked and unmarked animals in the population through
time (Hines & Nichols 2002). We therefore preceded the application with an investigation of the
effectiveness of detecting a temporal trend, and assigned it to the correct parameter, through the
Gibbs variable selection procedure (Dellaportas et al. 2000) applied to simulated data. Finally, we
provided supplementary material to facilitate understanding of likelihood implementation in BUGS
language (Lunn et al. 2009).
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leMethods
The Pradel temporal symmetry approach
Pollock et al. (1974) first pointed out that considering capture histories in reverse time order allows
inference about the recruitment process. By adopting this approach, Pradel (1996) developed a full
likelihood that permits the direct modelling of population dynamics by incorporating survival and
recruitment parameters. We briefly describe the Pradel temporal symmetry approach, to which we
also refer for general notation, by focusing on single-age populations sampled at a single study site.
Consider a sampling scheme of capture-mark-recapture (CMR) data on individuals sampled during
s successive occasions. From the ensemble of capture histories we can derive, for each occasion i,
the number of animals observed (ni), and among them, those observed for the first time (ui), for
the last time (vi), and those removed from (i.e., not released back into) the population (di).
The likelihood of Pradel (1996) includes the following parameters:
φi the survival probability from just after i to just before i+ 1;
pi the probability of being captured at time i when present just before i;
γi the probability that an animal present just before i was already present just after i− 1 (also
called seniority probability);
ri the probability of being captured at time i when present just after i;
µi the probability of being released for an individual captured at i;
ξi the probability of not being seen before i when present just before i;
χi the probability of not being seen after time i when present just after i.
Note that the parameters γi, ri, and ξi are the reverse-time analogue of φi, pi, and χi used
in the Cormack-Jolly-Seber (CJS) model. When neither removals nor introductions derive from
the capture-recapture procedure, as in our study, the statement “just before” and “just after” can
be replaced with “at”, and the forward- and reverse-time capture probabilities are equal (pi =
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leri). The temporal symmetry models use both forward- and reverse-time modelling simultaneously,
conditioning on the number of animals in the population at the beginning of the study (N−1 ). More
generally we can define N−i and N+
i as the abundances just before and just after sampling occasion
i. The expected number of animals in the population at successive occasions is determined by
means of the population growth rate (ρi), which can be expressed by considering the forward- and
reverse-time manner of writing the expected number of animals alive, i.e. N+i φi = N−
i+1γi+1. The
expected rate of population growth can be derived, from the following approximate equality, as:
ρi = E(N−i+1/N
+i ) ≈ φi/γi+1. (1)
Note that eqn 1 does not account for sampling-related mortality, i.e. for animals captured but not
released back into the population. Trap mortality can easily be taken into account and we refer to
Nichols & Hines (2002, eqn 8) and Hines & Nichols (2002, eqn 6) for further details.
The expected number of animals with a specific capture history can be written conditional on
the initial population size N−1 . As an instance, under the temporal symmetry model the expected
number of animals exhibiting capture history ‘011’ can be written as:
E(x011|N−1 ) = N−
1 λ′
1 ξ2 p2 µ2 φ2 p3 µ3, (2)
where N−1 λ
′1 gives the expected number of animals in the population just before sampling occasion 2.
Note that the initial population size N−1 in Eqn 2 is an unknown random variable. The probability
of each capture history conditional on the total number of animals captured (P (h)), can be derived
by dividing the expected number of animals with a specific capture history (E(xh)) by the expected
total number of animals caught (E(M)). E(M) can be written as the sum of the expected number
of animals seen for the first time at each sampling occasion, i.e. E(M) =∑s
i=1 ξiN−i pi (for i =
1, . . . , s). The unknown initial population sizes N−i cancel in the ratio P (h) = E(xh)/E(M), leaving
the conditional probabilities expressed in terms of estimable model parameters. The likelihood, for
the set of observed animals, is thus the product of the conditional probabilities of all individual
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lecapture histories, i.e. L =
∏h P (h)xh .
Pradel (1996) proposed three different parametrisations of his original likelihood, which are all
implemented in program MARK (White & Burnham 1999). They all maintain detection and sur-
vival probability as model parameters: (i) one parametrisation uses the reverse-time parameter, or
seniority probability (φt,γt,pt, where t denotes time-variant parameters), (ii) another parametrisa-
tion incorporates population growth rate as a parameter (φt,ρt,pt), and (iii) a third one is based on
a measure fi of recruitment rate, defined as the expected number of new individuals at time i + 1
per animal alive and in the population at i (φt,ft,pt). We focused on the first two parametrisations,
denoted (γ, φ) and (ρ, φ) respectively, whose likelihoods differ in the way by which seniority prob-
ability is expressed. In fact, the second parametrisation can be derived from the first original one
(eqn 2 in Pradel 1996) by substituting γi with the ratio φi−1
ρi−1derived from eqn 1 (see Appendix S1
for further details). Note that this model formulation, with seniority probability γi as a derived
parameter, allows values of γ greater than 1.
Data simulation
We used simulated data to investigate the capability of detecting simulated trends in model param-
eters (φi, γi, pi). We also examined whether spurious trends could not be selected in any parameter,
including ρi. For each scenario, we generated 100 data sets of individual capture histories from a
population size N=100, for ten sampling occasions. Population size was assumed constant over
time (i.e. ρi=1), and thus each time we added to the population the number of new individuals
needed to compensate for the number of deaths. A total of six scenarios were considered (see Table
1 in Appendix S2). The first three scenarios had in common a constant survival and seniority prob-
ability (denoted as φ(.)γ(.)) with φi=γi=0.85, and thus a constant population growth rate (ρ(.)),
but differed in the values defined for detectability p. The latter parameter was considered constant
(p(.)=0.5) in the first scenario, and with a temporal logit-linear trend in the other two scenarios
(with trend coefficient βp,time = 0.3 in the second scenario, denoted as p(trend03), and βp,time = 0.5
in the third scenario, p(trend05)) along with a mean value p=0.5. Time was standardized to have
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lemean zero and unit variance. Detectability ranged between 0.39 and 0.61 in the scenario p(trend03),
and between 0.32 and 0.68 in the scenario p(trend05).
A second group of scenarios included an equal temporal logit-linear trend for survival and
seniority probability (φ(trend)γ(trend)) that led again to a constant ρ. We used a mean survival (φ)
and seniority (γ) rate of 0.8, whereas trend coefficients on the logit scale βφ,time and βγ,time were set
to 0.5. Simulated survival and seniority probabilities ranged between 0.66 and 0.89. Detectability
was assumed either constant or with two different temporal trends as in the previous scenarios.
Scenario-specific settings for each parameter are summarized in Table 1 of Appendix S2. Each
simulated data set was analysed using the (γ, φ) and (ρ, φ) parametrisation of the Pradel temporal
symmetry model, under two sets of priors (see section ‘Bayesian analysis’).
Case study
The application we present is based on individual data collected for three seabird species of Procel-
lariiformes during s successive occasions (years), with s equals 12, 8, and 20 for Scopoli’s shearwater
(Calonectris diomedea), Balearic shearwater (Puffinus mauretanicus), and Storm petrel (Hydrobates
pelagicus), respectively. More specifically, data were collected during the breeding period at three
Mediterranean colonies: Pantaleu Islet (Mallorca, Balearic Archipelago, Spain) for Scopoli’s shear-
water (period 2002-2013, n=699), Sa Cella (Mallorca, Balearic Archipelago) for Balearic shearwater
(1997-2004, n=443), and Benidorm Island cave 1 (Alicante, Spain) for European storm petrel (1993-
2012, n=889). The number of individuals recaptured at least once was 475 in Scopoli’s shearwater,
251 in Balearic shearwater, and 590 in Storm petrel. All individuals were caught at nests while
incubating or when feeding chicks, and thus the sample was made up only of breeding adults. Since
all study burrows are marked and monitored over the years, and the goal has been to capture the
two members of the pair of each burrow during the breeding season, field effort has been kept rather
constant. More details of fieldwork procedures can be found in Genovart et al. (2013a), Oro et al.
(2004), and Sanz-Aguilar et al. (2011). The two shearwaters are mainly threatened by mortality
at sea from fishing gears, a factor that does not affect storm petrels, which are affected by alien
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leterrestrial predators such as rats and carnivores (e.g. Barcelona et al. 2010; Cooper et al. 2003).
Scopoli’s shearwater and Storm petrel include Mediterranean sub-species with vulnerable popula-
tions, whereas the Balearic shearwater has the highest IUCN category of threat for a taxon in the
wild, Critically Endangered, and is an endemic species of the Balearic archipelago (IUCN 2013).
The study colonies were all free of alien terrestrial predators and only the storm petrel colony was
affected by adult predation from yellow-legged gulls (Sanz-Aguilar et al. 2009a).
Bayesian analysis
Temporal symmetry models were fitted using a Bayesian formulation and the Markov chain Monte
Carlo (MCMC) framework (Robert & Casella 2004). Since the Pradel model involves likelihoods
not directly available in BUGS, we used the “zeros trick” (Spiegelhalter et al. 2007) that allows the
creation of an arbitrary likelihood. We refer to Appendix S1 for a detailed description of likelihood
specification.
Simulated data were analysed using both the (γ, φ) and (ρ, φ) parametrisation of the Pradel
model, under two sets of priors (see below). Given the conditions assumed for each scenario, we
calculated posterior probability of detecting trends in model parameters or, in other words, the
strength of evidence for temporal trends. This degree of support for a trend in a specific parameter
can be assessed by calculating the posterior variable inclusion probability, i.e. the probability
that a variable (‘TIME’ in this case) is “in” the model, using a Bayesian variable selection approach
(O’Hara & Sillanpaa 2009). Following Dellaportas et al. (2000) and Ntzoufras (2002), each temporal
slope βη,time (present in each linear predictor) was multiplied by an “inclusion parameter” ωη (for
η ∈ {φ, γ, p} in the (γ, φ) parametrisation, and η ∈ {φ, ρ, p} in the (ρ, φ) parametrisation), a latent
binary variable with a Bernoulli prior distribution with parameter 0.5, indicating no constraints on
the probability that a given covariate is included in the model. Taking the example of the (ρ, φ)
parametrisation, testing for a temporal trend in each parameter by means of the Gibbs variable
selection approach involved the calculation of the probability that the covariate ‘TIME’ was included
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lein the model. The corresponding ‘full’ linear predictors, and related constraints, are as follows:
logit(φi) = αφ + ωφ βφ,timeTIMEi
log(ρi) = αρ + ωρ βρ,timeTIMEi
logit(pi) = αp + ωp βp,timeTIMEi
(3)
where αφ, αρ, and αp are the overall means of survival probability (on logit scale), population
growth rate (on log scale) and capture probability (on logit scale), respectively. ωφ, ωρ, and ωp are
the inclusion parameters (in each linear predictor) for covariate TIMEi, which was standardized to
have mean zero and unit variance (for sampling occasion i from 1 to 10). If ωη=1 the linear predictor
includes trend variable ‘TIME’, whereas if ωη=0 the linear predictor does not include ‘TIME’. For
each scenario and model parametrisation, we derived the mean across 100 replicates of the Bayesian
point estimate of the mean inclusion probability, i.e the probability that ωη=1, associated with a
trend in each linear predictor.
In the application with real data, we extended the model applied on simulations to a hierarchical
formulation in order to estimate the temporal random variance, unexplained by the deterministic
trend term, for each parameter in the (ρ, φ) parametrisation (φ,ρ,p). Consequently, the extended
‘full’ linear predictors used in the Gibbs variable selection were the following:
logit(φi) = αφ + εφ,i + ωφ βφ,timeTIMEi, εφ,i ∼ N(0, σ2φ)
log(ρi) = αρ + ερ,i + ωρ βρ,timeTIMEi, ερ,i ∼ N(0, σ2ρ)
logit(pi) = αp + εp,i + ωp βp,timeTIMEi, εi ∼ N(0, σ2p)
(4)
where εφ,i, ερ,i, and εp,i is the deviation from the overall mean of each parameter, whereas σ2φ, σ
2ρ,
and σ2p is the temporal variance of each parameter (on logit scale for φ and p, on log scale for ρ).
From this mixture model, we derived not only the posterior inclusion probabilities ωη, but also
model-averaged estimates (averaged across the different models included in the posterior sample)
for φi, ρi, pi, the related overall means (αφ, αρ, αp) and standard deviations (σφ, σρ, σp). These
estimates take into account both parameter and model uncertainty, with respect to trend covariate
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ledependence. Model-averaged estimates were also obtained for covariate coefficients (βφ,time, βρ,time,
βp,time) by averaging across posterior samples where the corresponding ωη=1 ( i.e., conditional on
the covariate ‘TIME’ being present in the model) (Royle & Dorazio 2008).
Posterior distributions, for both parameter estimates and variable inclusion probabilities, were
assessed for prior sensitivity (e.g. King 2009) by using two sets of priors for the intercepts (αs)
and slopes (βs) in the linear predictors (prior set 1: Normal(0, 100) distributions; prior set 2:
Uniform(−5, 5) distributions). The hierarchical priors were specified by assuming each σ in eqn 4
drawn from a Uniform(0, 2) distribution.
Summaries of the posterior distribution were calculated from one Markov chain (in the simulation
study) and from three independent chains (in the application) initialized with random starting
values, run 500,000 times after a 50,000 burn-in and re-sampling every 20 draws. Chain length
was increased to 1,000,000 (after burn-in) iterations in the application with real data, in order to
improve sampling of the parameters associated with low inclusion probabilities. The models were
implemented in program JAGS (Plummer 2003), that we executed from R (R Core Team 2012)
with the package R2jags (Su & Yajima 2012). An R script with the model specification in BUGS
language is provided in Appendix S1.
Results
Simulation study
In the presence of constant survival and seniority probability, and thus constant population growth
rate, the probability of detecting a spurious trend was generally very low (average posterior inclusion
probability ω < 0.17 for φ, < 0.09 for γ, and < 0.01 for ρ, across 100 replicate data sets; Appendix
S2, Table 2). Under the same conditions, the probability of including in model a real trend on
detectability ranged, on average, from 0.40 to 0.56 for a logit-linear trend coefficient βp,time = 0.3,
and from 0.84 to 0.95 for βp,time = 0.5.
When a temporal trend was imposed on survival and seniority probability, but not on the
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lepopulation growth rate, the probability of detecting a real trend in φ and γ was always > 0.25
(Appendix S2, Table 3). The related posterior inclusion probabilities ranged, on average, as follows:
for φ: 0.40 – 0.77 (no trend in p), 0.39 – 0.74 (βp,time = 0.3), 0.33 – 0.68 (βp,time = 0.5); for γ:
0.40 – 0.52 (no trend in p), 0.38 – 0.45 (βp,time = 0.3), 0.26 – 0.42 (βp,time = 0.5). Under the last
two scenarios, the average probability of including in the model a real trend in detectability was
0.40 – 0.63 (βp,time = 0.3) and 0.75 – 0.81 (βp,time = 0.5). In addition, the probability of detecting
a spurious trend in ρ was always low (< 0.02) and not affected by the simulated conditions on p.
Interestingly, (ρ, φ) parametrisation models performed better than (γ, φ) parametrisation models in
the presence of trend in φ and γ (last three scenarios; Table 3 in Appendix S2). In general, posterior
inclusion probabilities were slightly higher under the Uniform(−5, 5) priors, even if estimates did
not substantially differ under the two sets of priors.
Case study
Posterior probabilities for the inclusion of temporal trends in model parameters (ωη with η ∈
{φ, ρ, p}) showed good agreement for the two sets of priors, even though ωη estimates were slightly
higher with the Uniform(−5, 5) priors (Table 1). The degree of support for trends in model param-
eters was very low (i.e. < 0.2, Ntzoufras 2009) in all species, except for the probability of a trend in
Scopoli’s shearwater detectability (ωp=0.25, under prior set 2). The two sets of priors yielded sim-
ilar posterior distributions for the parameters (Appendix S3). We thus discussed model-averaged
posterior estimates obtained under the set of Normal(0, 100) priors.
Mean survival probability (φ = expit(αφ)) was the lowest for Balearic shearwater (0.773, 0.672 –
0.863, 95%CRI), the highest for Storm petrel (0.824, 0.785 – 0.861), and intermediate for Scopoli’s
shearwater 0.810 (0.784 – 0.838; Table 2, Fig. 1). In all three species, 95% credible interval for
the estimate of the survival trend coefficient (βφ,time) encompassed zero, in agreement with the low
inclusion probabilities for temporal trends in φ. However, Balearic shearwater and Storm petrel
survival probabilities were characterized by substantial unexplained temporal random variation (σφ;
0.526, 0.055 – 1.368, and 0.494, 0.281 – 0.808 respectively) compared to Scopoli’s shearwater (0.193,
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le0.019 – 0.445).
On average, Scopoli’s shearwater and Storm petrel populations are both estimated to slightly
increase (i.e. ρ > 1, where ρ = exp (αρ)) over the whole study period, by 0.2 and 0.4% per year,
respectively. In contrast, Balearic shearwater showed an average decreasing trend of 4.9% per year.
Nevertheless, credible intervals of mean population growth rates encompassed one (i.e. population
stability) in all three species (Fig. 2), and the probability of a mean growth > 1 was 0.55 for both
Scopoli’s shearwater and Storm petrel, whereas the probability of a mean growth < 1 was 0.86
in Balearic shearwater. Temporal random variation of population growth rate (σρ) was generally
quite small, with the largest in Storm petrel (0.115, 0.068 – 0.182), intermediate values in Balearic
shearwater (0.095, 0.003 – 0.324), and the lowest in Scopoli’s shearwater (0.043, 0.003 – 0.105).
Detectability (p) of Scopoli’s shearwater showed a clear positive relationship with time (βp,time
= 0.233, 0.024 – 0.441), while a sizeable temporal random variability characterized p in Balearic
shearwater and Storm petrel (Table 2).
Recruitment, in the form of seniority probability (γ), was estimated by deriving it from survival
probability and population growth rate. In Scopoli’s shearwater γ was almost constant, varying
from 0.785 (0.732 – 0.832, γ7) to 0.846 (0.795 – 0.901, γ9), whereas in Balearic shearwater values
ranged from a minimum of 0.701 (0.469 – 0.932, γ2) to a maximum of 0.874 (0.800 – 0.954, γ6), and
in Storm petrel from 0.696 (0.582 – 0.810, γ12) to 0.935 (0.814 – 1.055, γ11).
Discussion
Simulation study
The interest in the temporal symmetry method, compared to other open population modelling
approaches for CMR data, lies in the possibility of directly testing covariate effects on population
growth rates (e.g. Hunter et al. 2010; Ozgul et al. 2010; Tenan et al. 2012). However, a legitimate
concern is that a trend in capture probability may be mistaken for a trend in some other parameter.
Similarly, wrongly modelling parameters as functions of some time-variant covariates may induce
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lecompensatory patterns in other parameters. In this paper, we investigated the efficiency of detecting
the correct linear trends under the (γ, φ) and (ρ, φ) parametrisations in a Bayesian implementation
of the temporal symmetry model. More specifically, we evaluated the performance of a well-known
Bayesian variable selection procedure, the Gibbs variable selection (Dellaportas et al. 2000), in
terms of probability of detecting real trends and avoiding spurious trends under scenarios with
three degrees of trend in detection probability p (no trend, a moderate trend βp,time = 0.3, and a
strong trend βp,time = 0.5). Results showed very low probabilities of detecting spurious trends in
model parameters (< 0.02 for ρ) under all simulated conditions for p. In addition, trend strength in
p (i.e. the βp,time value) only weakly affected the probability of correctly assigning a trend to survival
φ and seniority γ probability. Directly testing for a trend in ρi, by means of a variable selection
procedure, showed good performance in terms of a low probability of selecting spurious trend in
population growth rates, at least under the limited range of scenarios considered. On the other
hand, simulation results showed probabilities of including a real trend (ωη, with η ∈ {φ, ρ, γ, p})
were often < 0.5. Thus, regarding population growth rate, the approach appears conservative:
trends may not be detected, but if they are, they are highly likely to be real. If the approach is
to select the best model, i.e. the more probable combination of covariates in the model, then one
has to define a threshold inclusion probability (values of 0.2 and 0.5 have been proposed in the
literature; Ntzoufras 2009; Barbieri & Berger 2004). As an alternative, model-averaged estimates
can be derived, as done here in the application, taking into account both parameter and model
uncertainty and avoiding the awkward definition of threshold inclusion probabilities. Although a
certain amount of trend will always pass in the average estimates with the latter alternative, this
effect, being weighted by small inclusion probabilities, should be small if no actual trend was present.
This is what we observed in the range of scenarios considered (see Tables 4 to 7 in Appendix S2).
In particular, robust estimates of population growth rate parameters were obtained even in the
presence of trends in other demographic parameters.
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leCase study
Our application focused on testing for linear trends in survival probability, population growth rate,
and detection probability, as well as estimating unexplained temporal random variation in these
parameters, for three species of burrowing nesting seabirds. Testing temporal trends in survival
was initially motivated by evidence for additive causes of anthropogenic mortality (e.g. Laneri
et al. 2010) that affect Scopoli’s and Balearic shearwater (longline by-catch) potentially inducing
a decreasing trend in survival. Furthermore, inbreeding depression (Hogg et al. 2006) and density
dependence (both positive and negative; Ehrlen & Groenendael 1998; Stephens & Sutherland 1999)
can generate temporal trends in population growth rate, which can be even larger in social species,
like our study species. Finally, a trend in detection probability can be induced by an array of
factors, such as an increase in skills in fieldwork procedures or a variation of resource availability
over time (e.g. Williams et al. 2002).
In our case, only a trend in Scopoli’s shearwater detectability was supported by the data, and
temporal random variation was generally small in the population growth rates of all species. The
estimated mean survival probability for Scopoli’s shearwater (0.810) was generally low compared to
other estimates from the same colony but referred to a shorter time series (newly marked individuals
0.83 (0.76 – 0.88, 95%CI) and 0.78 (0.71 – 0.83), residents 0.87 (0.83 – 0.91) and 0.87 (0.82 – 0.90)
in Genovart et al. 2013a and Sanz-Aguilar et al. 2011, respectively) or from other Mediterranean
islands (ranging from 0.74 to 0.96; Igual et al. 2009; Jenouvrier et al. 2008, 2009). This low level
of adult survival has been strongly associated to the large-scale Southern Oscillation index (SOI)
influencing the frequency of strong hurricanes (Genovart et al. 2013a), and to other non-climatic
factors such as long-line incidental bycatch (Barcelona et al. 2010; Laneri et al. 2010; Ramos et al.
2012). Furthermore, the presence of transients in our sample (e.g. Jenouvrier et al. 2009) and the
impossibility of discerning them in the analyses, is known to negatively bias survival estimates
for residents (Pradel et al. 1997). The annual percentage in the number of transients at the two
colonies considered by Genovart et al. (2013a) varied from 0% to 21%. Low survival rates in
this species might be compensated for by recruitment, which was here estimated in the form of
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leseniority probability and encompasses not only local recruitment but also immigration. Previous
studies already suggested that even if the species is mostly philopatric (97%), there is non-negligible
dispersal (particularly natal dispersal) between colonies (Genovart et al. 2013b).
It is known that adult survival in Balearic shearwater is unusually lower than the typical values
observed in Procellariform seabirds (Oro et al. 2004). Our results confirmed a low mean survival
probability (0.773), very close to the estimate of 0.780 (0.02, SE) reported by Oro et al. (2004),
higher than 0.662 (0.04, SE) estimated by Tavecchia et al. (2008), and characterized by a remarkable
temporal random variation. The population is estimated to decline on average by 4.9% per year,
matching the 4.8% value reported by Oro et al. (2004) using population age-class matrix models
that incorporated both demographic and environmental stochasticity. Note that even if we used
two more years of data than Oro et al. (2004), inference of trend might be limited by the relatively
short study period.
Inference for the vulnerable Storm petrel was based on data from the same colony studied by
Sanz-Aguilar et al. (2009a) but using a time-series that is five years longer. Sanz-Aguilar et al.
(2009a) showed that predation by yellow-legged gulls negatively affected survival probability of
syntopic petrels, whose values soared from 0.75 (0.71–0.78, 95%CI) to 0.89 (0.82–0.94) after the
removal of specialist predatory gulls. The average survival probability estimated here (0.824) was
consistent with these values, but lower than estimates from predator-free colonies (0.90–0.95, Biar-
ritz, Atlantic France, Hemery 1980; 0.88 (0.85–0.91 95%CI), Marettimo, Italy, Sanz-Aguilar et al.
2009b). As a very interesting result, clearly reflected in Fig. 2, population growth rates were es-
timated to be positive after the beginning, in 2004, of a program of culling specialist gulls. The
unexplained temporal variation in survival we found here may be due to gull predation as numbers
of predated petrels were highly variable during the study period (Sanz-Aguilar et al. 2009a).
The modelling approach
We implemented in a Bayesian framework the temporal symmetry approach of Pradel (1996) that
permits direct modelling of ρi, the rate of change in population size between sampling occasion i
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leand i + 1. We showed how a Bayesian variable selection approach (O’Hara & Sillanpaa 2009) can
be used to test hypotheses directly on different model parameters, even though more investigation
is needed to explore potential biases in the estimation of model parameters (and related effects)
under other specific sampling situations. Moreover, by adopting a Bayesian approach we were able
to test for temporal random variation in the population growth rate, an option that is not available
in other computer software in which this modelling approach is implemented (e.g. MARK). A
Bayesian implementation of the temporal symmetry approach can help to make this underused
method more accessible, a method that has already been applied to other ecological themes, such
as characterizing the realized growth of host populations in relation to disease effects (Lachish et al.
2007), or estimating stopover duration (Chernetsov 2012).
Acknowledgements
We thanks Robert B. O’Hara and the anonymous referees for constructive comments on previous
versions of this manuscript. We also thanks Aaron Lemma for IT assistance. Funds were partially
provided by FEDER – Balearic Government and Fundacion Biodiversidad. We are grateful to
the Ward and Environmental Monitoring Service of Benidorm Island (Serra Gelada Natural Park,
Generalitat Valenciana), Ciudadanos por la Ciencia, Dr. E. Minguez, Dr. A. Martınez-Abraın and
B. Sarzo. Roger Pradel received a research stay grant from Universitat de les Illes Balears.
Data accessability
• The R and BUGS script for running the model is included in supplementary material (Ap-
pendix S1).
• Input data for the BUGS model: http://dx.doi.org/10.6084/m9.figshare.977874.
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leTables
Table 1: Posterior probabilities (ωη with η ∈ {φ, ρ, p}) of including a linear trend for the modelparameters of the (ρ, φ) parametrisation. Estimates are reported for two prior sets for the intercepts(αs) and slopes (βs) in the linear predictors in eqn 4 (prior set 1: Normal(0, 100) distributions; priorset 2: Uniform(−5, 5) distributions).
Inclusion probabilitySpecies prior set ωφ ωρ ωp
Scopoli’s shearwater 1 0.019 0.005 0.1162 0.054 0.012 0.253
Balearic shearwater 1 0.037 0.012 0.0392 0.086 0.028 0.093
Storm petrel 1 0.074 0.018 0.0302 0.166 0.047 0.074
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leTable 2: Model-averaged parameter estimates obtained under the set of Normal(0, 100) priors forthe intercepts (αs) and slopes (βs) in the linear predictors of eqn 4. Mean survival (φ) and detection(p) probabilities are given on probability scale, i.e., φ = expit(αφ) and p = expit(αp) where expit isthe inverse-logit function, and the related βs and σs on logit scale. Population growth rate-relatedparameters (βρ and σρ) are on log scale, whereas mean population growth rate ρ = exp(αρ). Median,2.5 and 97.5 percentiles are also reported.
Species Parameter mean SD 2.5% 50% 97.5%
Scopoli’s shearwater φ 0.810 0.013 0.784 0.810 0.838ρ 1.002 0.018 0.965 1.002 1.038p 0.792 0.017 0.758 0.792 0.826σφ 0.193 0.110 0.019 0.181 0.445
βφ,time -0.111 0.104 -0.306 -0.114 0.100σρ 0.043 0.027 0.003 0.039 0.105
βρ,time -0.021 0.024 -0.067 -0.021 0.027σp 0.245 0.122 0.033 0.234 0.520
βp,time 0.233 0.105 0.024 0.233 0.441
Balearic shearwater φ 0.773 0.046 0.672 0.774 0.863ρ 0.951 0.059 0.839 0.950 1.068p 0.468 0.079 0.311 0.467 0.629σφ 0.526 0.327 0.055 0.465 1.368
βφ,time 0.179 0.440 -0.713 0.162 1.128σρ 0.095 0.091 0.003 0.071 0.324
βρ,time -0.069 0.136 -0.367 -0.050 0.155σp 0.845 0.287 0.443 0.789 1.582
βp,time 0.144 0.399 -0.700 0.153 0.892
Storm petrel φ 0.824 0.019 0.785 0.824 0.861ρ 1.004 0.029 0.947 1.003 1.062p 0.709 0.038 0.632 0.710 0.780σφ 0.494 0.136 0.281 0.477 0.808
βφ,time 0.247 0.139 -0.025 0.245 0.532σρ 0.115 0.029 0.068 0.111 0.182
βρ,time 0.054 0.030 -0.006 0.055 0.113σp 0.763 0.151 0.524 0.743 1.113
βp,time 0.179 0.188 -0.193 0.181 0.556
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leFigures
Year
Sur
viva
l pro
babi
lity
2003 2005 2007 2009 2011
0.7
0.8
0.9
(a)
Year
1998 2000 2002
0.5
0.6
0.7
0.8
0.9
(b)
Year
Sur
viva
l pro
babi
lity
1993 1995 1997 1999 2001 2003 2005 2007 2009 2011
0.6
0.7
0.8
0.9
1.0
(c)
Figure 1: Model-averaged annual estimates (with 95%CRI) of survival probability (φi) for Scopoli’sshearwater (a), Balearic shearwater (b), and Storm petrel (c).
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Year
Pop
ulat
ion
grow
th r
ate
2003 2005 2007 2009 2011
0.85
0.95
1.05
1.15
(a)
Year
1998 2000 2002
0.7
0.9
1.1
1.3
(b)
Year
Pop
ulat
ion
grow
th r
ate
1993 1995 1997 1999 2001 2003 2005 2007 2009 2011
0.8
1.0
1.2
1.4
(c)
Figure 2: Model-averaged estimates (with 95%CRI) of population growth rate (ρi) for Scopoli’sshearwater (a), Balearic shearwater (b), and Storm petrel (c). The dotted line indicates populationstability.
Supporting Information
Additional Supporting Information may be found in the online version of this article.
Appendix S1. R and BUGS script.
Appendix S2. Simulation study.
Appendix S3. Bayesian learning plots.
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