There is a conspicuous gradient in the proportion of passerine breeding communities contributed by tropical migrants (PPM) in Europe, with communities located in the northernmost areas showing the greatest percentages and those located to the south the smallest. I used multiple stepwise regression and regression on principal components to investigate the effects of a set of ecological, climatic, and geographical variables on migrant percentages in a sample of 55 European censuses distributed from northern Fennoscandia through southern Spain. When the main habitat types are considered individually, this geographic pattern is still significant. The best single predictor of PPM as revealed by multiple regression analyses is latitude, but when this variable is removed, the temperature of the coldest month provides almost equivalent predictions of PPM. Habitat type per se apparently does not influence substantially the percent of migrants in European breeding passerine communities.
These results contrast with those reported by MacArthur (1959) for North America, although they are consistent with some suggestions derived from the recent reanalysis of North American data carried out by Willson (1976). Intercontinental differences are perhaps due to sampling deficiencies in the North American areas studied, mainly derived from the restricted latitudinal range.
To explain the European pattern of PPM, I suggest that the percentage of migrants in a community during the breeding season depends on both the harshness of adverse winter conditions faced by the resident populations and on the total resource availability during the breeding period. Carrying capacity of the habitat during the severe season will to some extent regulate the size of resident populations in the following breeding period, which in turn must affect the abundance of migrants that may successfully colonize the habitat. Very harsh winters coupled to very productive breeding seasons favor the largest percentage of migrants. Received 29 June 1977, accepted 31 August 1977.
Biological Station of Dogana, Paraguay Street 1-2, Sevilla (12), Spain
IN analysing the contribution to North American breeding bird communities by
neotropical, long distance migrants, R. H. MacArthur (1959) was able to show the
existence of a pattern on a continental scale relating migrant percentages to habitat
seasonality. No apparent geographical trend was found, however, and interhabitat
differences alone appeared to account for the largest part of the variation in neo-
tropical migrant proportions. Recently, MacArthur's analysis has been reinterpreted
and some of his results questioned (Willson 1976). European breeding bird com-
munities, as those in North America, are composed of a variable fraction of species
(hereafter named "migrants") that migrate south in the autumn to spend the winter
in the African tropics south of the Sahara Desert (Moreau 1952). They thus provide
the opportunity for an analysis similar to that of MacArthur (1959); such intercon-
tinental comparisons of geographical patterns may contribute substantially to our
understanding of )rocesses that configure breeding bird communities.
A preliminary investigation into this theme (Herrera 1977) revealed that, inde-
pendently of structural quality of habitats, there is a strong geographical pattern in
European percentages of migrant birds. The proportion of migrants increases north-
wards and reaches its highest values in Scandinavian communities, regardless of
whether these are located in arctic tundra, boreal forests, or peatland bogs. Lowest
values are displayed by southern European breeding communities. These latitudinal
changes contrast with the results of MacArthur (1959) for North America. Are there
in fact different mechanisms underlying migrant percentages in Europe and North
America or, alternatively, are the same causal factors operating differentially in both
continents to give contrasting patterns? This paper aims to provide an answer to
this question.
METHODS
The present study differs from MacArthur's analysis in two ways (which I believe to be unimportant).
Owing to the relative scarcity of accurate census results for nonpasserine species, I have been concerned
throughout only with passerine breeding communities. Normally, nonpasserines constitute only a small
fraction of the total number of individuals, so I think any decrease in generality caused by ignoring them
will be compensated largely by an increase in censuses available for analysis. This point will be further
discussed in the final section of this paper. On the other hand, no special care has been taken in selecting
censuses from undisturbed, natural habitats since, after some thousand years of heavy human landscape-
use, pristine habitats are unfortunately very rare throughout Europe, especially in the southern half of
the continent.
To eliminate possible irregularities derived from unusual spring conditions in single years, census data
were preferentially chosen from studies over several consecutive breeding seasons. However, for the sake
of geographical completeness, one-season censuses were used if neglecting them would have meant leaving
a large area unrepresented. Hereafter, both one-season and several-seasons average censuses will be
indiscriminately termed "censuses."
A total of 55 censuses was considered (Appendix 2) and three sets of data were recorded for each,
related to the census itself (1-4 below), geographical features of the census locality (5-8), and climatic
characteristics (9-16). Values for the last data set were obtained from the nearest station reported in
Walter and Lieth (1960). Variables and symbols used are as follows.
1. Total passerine breeding density (TPD), in individuals/10 ha.
2. Migrant breeding density (birds/10 ha) (MD). Species considered as migrants were those which,
according to Moreau (1952), do not winter to any extent in the Western Palearctic, their winter areas
extending exclusively over the African and/or Asian continents, mainly south of 15øN (southern border
of the Sahara Desert). This criterion eliminates some species that winter in Africa but also occupy large
areas in the southern Palearctic (e.g. Sylvia atricapilla, Phylloscopus collybita, Motacilla alba). The
migrant species are listed in Appendix 1.
3. Percentage of migrant individuals (PPM), equal to (MD/TPD) x 100.
4. Structural quality of the habitat (SQH) scored from 1 to 5: herbaceous fields, tundra, etc. (1);
shrubland (2); coniferous (3); deciduous (4); and mixed (5) forests.
5. Latitude (LATITU), expressed to the nearest half degree.
6. Altitude above sea level (AASL) in meters.
7. Shortest distance to the nearest coast (DISNEC) in km.
8. Shortest distance to the Atlantic coast, facing west (DISWFC) in km.
9,10. Monthly mean temperature of coldest (MTCM) and hottest (MTHM) month in øC.
11. Absolute yearly range of monthly mean temperatures (YRMT) in øC, obtained as the difference
between MTHM and MTCM.
12. Relative range of temperatures (RRT) (YRMT divided by MTHM).
13,14. Monthly precipitation of driest (MPDM) and wettest (MPWM) month in mm.
15. Absolute yearly range of monthly precipitation (YRMP), obtained as the difference between MPWM
and MPDM.
16. Relative range of precipitation (RRP) (YRMP divided by MPWM).
Climatic data were chosen to consider seasonal aspects of the annual cycle in an objective fashion. It
is reasonable to assume that climatic indices of seasonality must be related in some way to ecological
seasonality, the causal factor argued by MacArthur (1959) to explain the North American pattern of
PPM. As the degree of seasonality is modified by altitude and continentality (KiSppen 1923, Jansa 1969),
several variables (6-8) were employed to measure such effects.
I used multivariate methods that have been shown useful in the analysis of geographical patterns
(Vuilleumier 1970, Brown 1971, Ketterson and Nolan 1976). Multiple stepwise regression analyses were
performed on census data using the BMD02R computer routine (Dixon 1968). In this program, one
variable is added to the regression equation at each step. The variable added is the one that makes the
greatest reduction in the error sum of squares; equivalently, the added variable has the highest partial
correlation with the dependent variable partialed on the variables already included and is the variable
2
I I
0 I 0 20 30 40 50
PPM
Fig. 1. Geographical pattern exhibited by the percentage of migrant individuals (PPM, black sectors
of circles) in 55 European breeding passerine communities. Frequency distributions of PPM values within
each latitudinal zone are shown to the left. Latitudinal areas were arbitrarily chosen.
that would have the highest F-value (Dixon 1968). Original data were used throughout with no trans-
formation since there is no a priori reason to expect nonlinear dependences. Analyses were run taking as
the dependent variable TPD, MD, and PPM, either deleting or not some of the independent ones.
In addition, a regression of PPM on the principal components resulting from the correlation matrix of
the 13 environmental variables was carried out using the BMD02M computer program (Dixon 1968).
This type of analysis provides a somewhat different view of the relationships between the dependent and
independent variables. Whereas in stepwise regression variables are added one at each time and the
relationships are assessed on the basis of individual variables, principal component analysis provides
uncorrelated sets of related, linearly combined variables against which to regress the dependent ones.
This procedure is particularly useful when dealing with independent variables among which there exist
some highly correlated ones, such a the climatic variables under consideration.
To save space ! omit the complete list of raw data, but it can be obtained from the author upon
request. A list of localities, habitat types, and source references is given in Appendix 2.
RESULTS
A geographical pattern of PPM values is readily appreciated in Fig. 1. Passerine
communities located to the northeast on the European continent contain a larger
fraction of migrant individuals than those situated to the southwest. The frequency
distributions of PPM values show a dependence upon latitude, although a rather
slight longitudinal trend could perhaps be observed in Fig. 1 as well. Longitude was
not considered among the geographical variables used in this study as, due to the
peculiar distribution of land masses in western Europe, distance to the Atlantic coast
¸
PPM - 9.375 PC.I * 18.80
50 R2= 0.485 0
o
30
20-
¸
¸
/ o P.C.I
-2 -1 O +1 +2
Fig. 2. Regression of PPM (percenge of migrant individuals) against P.C. I (first principal com-
ponent). High values of P.C. I are associated with high latitude, low extreme temperatures (both coldest
and hottest ones), and high seasonality in temperature, both in absolute and relative terms (Table 2). It
can be seen that the proportion of migrants increases with the increasing values of P.C.I. Correlation
is highly significant (t = 7.07, n = 55, P 0.001).
appeared to be a better estimate of climatic continentality. Nevertheless, DISWFC
does not appear to be significantly related to PPM (see below, Table 3).
Very distinct habitat types are pooled and intermixed in Fig. 1. However, no
apparent relationship between habitat characteristics and geographical location of
samples could be detected (correlation between LATITU and SQH, r = -0.113,
P > 0.4). Furthermore, each habitat type taken separately exhibited a strong cor-
relation between LATITU and PPM (Table 1). A test of homogeneity among the
three correlation coefficients (Sokal and Rohlf 1969) revealed no significant differ-
ences (X 2 = 1.81, df = 2, P > 0.3), thus indicating that the relationship between
migrant percentages and latitude is independent of the habitat type considered.
Is only latitude responsible for PPM variation or are there further associated
environmental variables that contribute to the main sources of PPM changes? Prin-
cipal component analysis reveals that, in addition to LATITU, there are four cli-
matic variables that could potentially affect the percentage of migrant individuals
in a significant way (Table 2, Fig. 2). They are MTCM, MTHM, YRMT, and
TABLE 1. Correlations a between PPM and LATITU when the main habitat types are individually
considered
r N Significance
Coniferous forests 0.794 15 P < 0.001
Deciduous forests 0.626 21 P < 0.01
Grassland and shrubland 0.842 13 P < 0.001
a Pearson product-moment correlation coefficient, r
TABLE 2. Principal component analysis of the correlation matrix of 13 environmental variables
Principal component loadings a
P.C. I P.C. II P.C. III
LATITU 0.895 DISNEC 0.895 MPDM 0.914
MTCM -0.958 DISWFC 0.905
MTHM -0.869
YRMT 0.558
RRT 0.930
Eigenvalues 4.920 2.946 2.493
Proportion of environmental variance 0.378 0.227 0.192
Correlation coefficient with PPM b 0.697*** -0.097 -0.215
a Only loadings greater than 0.4 are shown
RRT, which together with LATITU, gave the highest loadings on the first principal
component (P.C.) (Table 2). Localities showing high scores on P.C. I are charac-
terized by high latitude, low MTCM and MTHM values, and large values of YRMT
and RRT. Percentage of migrants is highly and positively correlated with P.C. I
scores (Fig. 2), and thus increases with increasing latitude, absolute and relative
ranges of temperatures, and with decreasing values of extreme annual temperature,
both coldest and hottest ones. It must be stressed that the relationship just described
is between PPM and the combination of all the variables contributing to P.C. I in
a significant way, but it tells us nothing on the possible relations between PPM and
any of them considered individually.
No variable related to rainfall appears to account for any substantial amount of
environmental variation in the set of localities studied. This was not unexpected,
since except for four localities with a Mediterranean climate, rainfall is very evenly
TABLE 3. Results from multiple stepwise regression analyses
Dependent variable
PPM MD TPD
Order Order Order
en- en- en-
Inde- tered tered tered
pendent in Increase in Increase in Increase
vari- equa- in R- equa- in R- equa- in R-
abies tion F-value a square b tion F-value square tion F-value square
TPD -- -- -- 1 13.42'** 0.202 -- -- --
MD 7 2.36 0.011 -- -- -- 2 15.35'** 0.164
PPM -- -- -- 6 2.19 0.026 -- -- --
SQH 6 13.96'** 0.064 8 1.30 0.015 1 20.49*** 0.279
LATITU 1 70.33'** 0.570 -- -- -- 6 1.28 0.013
AASL 3 2.32 0.016 5 1.87 0.023 4 1.26 0.013
DISNEC 10 0.60 0.003 10 0.38 0.004 10 0.29 0.003
DISWFC 9 0.56 0.003 4 2.57 0.032 7 2.93 0.030
MTCM 4 4.86* 0.030 -- -- -- 8 0.89 0.009
MTHM 12 0.07 0.000 9 0.56 0.007 -- -- --
YRMT -- -- -- 12 0.77 0.009 -- -- --
RRT 5 4.32* 0.025 7 3.22 0.037 5 0.64 0.007
MPDM 2 10.89'* 0.074 ......
MPWM -- -- -- 11 0.78 0.009 9 0.47 0.005
YRMP 11 0.60 0.003 3 2.69 0.035 -- -- --
RRP 8 1.10 0.005 2 7.71'* 0.103 3 1.96 0.021
Only F-values greater than 0.05 are shown. Significance levels: * = P < 0.05; ** = P < 0.01; *** = P < 0.001
Increases below 0.001 are not shown
TABLE 4. Results of stepwise regression of PPM when TPD, MD, and LATITU are removed
Increase Coefficient
in in
Variable a R-square F-value b regression
MTCM 0.460 45.15'** -4.373
AASL 0.155 20.97*** -0.009
DISNEC 0.058 9.06*** -0.006
RRT 0.017 2.74* -39.327
SQH 0.039 7.14'** -2.763
RRP 0.017 3.19'* 14.146
a Only significant variables are shown, listed in the order they enter the equation
b Significance levels as in Table 3
distributed in time and space for the localities studied, all of which have a temperate
climate (correlations between LATITU and either MPDM or MPWM are nonsig-
nificant, r -- -0.020 and r = 0.069, respectively, P > 0.5). A slight, negative cor-
relation exists between PPM and P.C. III (Table 2), but statistical significance is
not achieved (0.1 < P < 0.2).
Results of the stepwise regression analyses are shown in Table 3. Firsfly, it must
be noted that whereas PPM is very strongly influenced by geographical and climatic
variables, this is not so for absolute measures of abundance (TPD and MD), whose
variation is not substantially accounted for by any of the environmental variables
I included in the analysis. If TPD were omitted from the list of independent vari-
ables, RRP would be the first variable entering equation with MD as dependent
variable. This suggests some relationship between seasonality of precipitation (and
thus seasonality of productivity), and abundance of migrant individuals. In any
case, the relationships between either TPD or MD and environmental variables
appear to be rather weak, since while 80.3% of PPM variation is related to these
variables, they account for only about 35% of either TPD or MD variation. On the
other hand, no close relationships exist between PPM and either TPD or MD. The
percentage of migrant individuals (PPM) appears rather as a community-specific
ratio which does not depend to any extent on absolute abundance of individuals.
Migrant density (MD) and total passerine density (TPD) are, however, slightly in-
terrelated, quite likely through a third, unknown variable, presumably of an envi-
ronmental nature. It must be noted that TPD is significantly correlated with SQH,
which is the first variable entering the equation (Table 3); this is not an unexpected
result, as more complex habitats generally support denser passerine populations (e. g.
Jones 1972, Blondel et al. 1973, Herrera 1977).
LATITU, MPDM, MTCM, RRT and SQH enter significantly into the regression
equation of which PPM is the dependent variable (Table 3). Of these, LATITU is
the best single predictor of migrant percentages and the first variable entering the
equation, accounting for 57% of the total R 2. The remaining four significant vari-
ables account altogether for an increase in R 2 of 0.193. The simultaneous effect of
all five accounts for 76.4% of total PPM variation in the sample. The addition of
the remaining 10 nonsignificant variables to the regression increases R 2 up to only
0.803, and unknown factors account for the rest of the variation (0.197).
The simplest predictive equation is
PPM = -47.795 + 1.285LATITU (r = 0.755, df = 1,53, F = 70.33, P 0.001)
Up to the sixth step, the regression receives the five significant variables plus the
nonsignificant AASL (in brackets):
PPM-- 38.777 - 3.647SQH + 0.878LATITU(-0.005AASL)
- 3.587MTCM- 43.946RRT - 0.152MPDM
(r = 0.883, df = 6,48, F = 28.27, P < 0.001)
According to this equation, the greater proportion of migrant individuals held by a
community, the greater its latitude and the lower the monthly mean temperature of
the coldest month (MTCM), rainfall of the driest month (MPDM), relative range of
temperature (RRT), and structural quality of the habitat (SQH). As it is nonsig-
nificant, AASL must be disregarded. Breeding communities located in northern
localities with cold winters, relatively dry springs and/or summers, and inhabiting
simple habitats are most likely to have a large proportion of migrant individuals.
At first glance, these results appear to differ slightly from those obtained with
principal component analysis as, for instance, P.C. III (mainly influenced by
MPDM) was there nonsignificantly correlated with PPM whereas MPDM emerges
as a significant variable in stepwise regression. This discrepancy must be attributed
to the fact that scores on any principal component result from the combination of
several variables and when low-loading variables predominate on a given component
(e.g.P.C. III), they may obscure correlations at certain times despite their small
individual loadings.
As principal component analysis showed that several climatic parameters
(MTCM, MTHM, YRMT and RRT) were associated with LATITU and strongly
correlated with PPM, a stepwise regression was run taking PPM as the dependent
variable and deleting LATITU from the set of independent ones. TPD and MD
were removed as well. In this way, the influence of climatic variables alone could
be assessed. Results are shown in Table 4.
Mean temperature of the coldest month (MTCM) alone explains 46% of PPM
variation and it is the first variable entering the equation. It accounts for only a
slightly smaller fraction of PPM variation than did LATITU alone when this latter
variable was included in the analysis (Table 3), thus indicating that MTCM is almost
as good a predictor of PPM as LATITU. After the first step, the resulting equation
is
PPM= 17.335 - 1.711MTCM (r = 0.678, df-- 1,53, F = 45.15, P < 0.001)
thus revealing that communities facing the coldest winters hold the larger propor-
tions of migrant individuals during next breeding season. This is an interesting
result, since it suggests that PPM variation in Europe can be satisfactorily explained
in climatic terms alone, disregarding the latitudinal location of communities. Al-
though one must be well aware of the fact that correlation does not necessarily imply
causation, it is tempting to assume that mean temperature of the coldest month is
the critical parameter which largely regulates the proportion of migrant individuals
in European breeding passerine communities.
DISCUSSION
Prior to comparing my results with MacArthur's (1959) and Willson's (1976) for
North America, it is necessary to verify that my neglect of nonpasserines has not
invalidated intercontinental comparisons. The absolute difference between the per-
centage of migrants computed according to MacArthur's criterion (PPM, nonpas-
serines included) and mine (PPM2, only passerines), were obtained for individual
censuses (I PMM, - PPM I). This was done for 18 North American censuses (Stewart
and Aldrich 1949, 1951; Odum 1950; Speirs 1972; Shugart and James 1973) and 17
European censuses chosen from those analysed in this paper--the only ones that
provided adequate nonpasserine data. Mean absolute differences between figures
yielded by the two methods were 1.86 _+ 0.39 and 1.10 _+ 0.29%, for North America
and Europe respectively (intercontinental comparison nonsignificant, P > 0.05).
When the signs of differences are taken into consideration (PPM - PPM2), respective
means for America and Europe are -1.79 -+ 0.41 and +0.59 -+ 0.37%, which in
this case does differ significantly (P < 0.001). Although the latter result suggests
some sort of intercontinental difference with regard to the degree of migratoriousness
among nonpasserines, the small absolute differences found between figures arrived
at by the two methods (ca. 1%) indicates that migrant percentages remain nearly
unaltered by either deleting or including nonpasserines in the analysis.
The above results have revealed several important differences between Europe
and North America in the geographical pattern of the percentage of tropical migrants
(PPM). Whereas in Europe PPM values show a strong geographical component, this
is lacking in North America, where migrant percentages vary according to habitat
types (MacArthur 1959). Structural quality of the habitat (SQH) has a moderate
negative influence on European PPM figures (Tables 3, 4), while according to
MacArthur's results, wooded habitats of North America hold the highest percentages
and simple habitats (prairie, desert) the lowest ones. A recent reanalysis of data
covering part of the area dealt with by MacArthur suggests that his conclusions
deserve some reassessment (Willson 1976). The clear-cut relations between habitat
type and PPM that MacArthur found seem to be not too clear when examined using
somewhat different criteria (e.g. differences between grasslands and northeastern
deciduous forests appear nonexistent). When all migrants (not only tropical ones)
are considered, average percent of migrant individuals is about the same in grassland
(73%) and in deciduous forests (75%) and, as MacArthur found, is significantly
greater in coniferous forests (94%) (Willson 1976). Although the criterion I have
chosen to select migrant species is closer to MacArthur's, my European results are
in fair agreement with Willson's suggestions for North America, as she pointed out
(p. 585) that latitudinal differences in seasonality could be more a function of climate
than of habitat type. My results demonstrate that in European breeding commu-
nities, geographical location with respect to latitude is the most important factor in
determinating the relative importance of tropical migrants and this relation continues
to hold when the different habitat types are considered individually. However,
latitude is not the only factor involved, as SQH, MPDM, RRT, and MTCM have
significant effects on PPM as well (Table 3).
Neither MacArthur's nor Willson's contributions have revealed as strong an in-
fluence of latitude as my European results, but this fact must be related to the shape
of the geographical area sampled by those authors. Of the 29 breeding communities
analysed by MacArthur, only 2 came from Canada, and of 37 censuses handled by
Willson only 9 were of Canadian origin. In both cases a relatively narrow range of
latitude was sampled and under these circumstances it would be difficult to dem-
onstrate a significant relationship to latitude. On the other hand, the range of hab-
itats is much greater and more sharply defined in North America, and therefore
American authors pay more attention to inter-habitat differences that can mask
purely geographical patterns. Presumably, a restricted sampling design coupled to
a well-defined habitat mosaic may have been responsible for the observed differences
between North American and European results, although these are perhaps only
superficial. It is reasonable to expect that if more Canadian censuses were included
in large enough numbers and latitude were equitably sampled, latitudinal trends
would surely appear in North America.
In her discussion, Willson (1976) suggests the possibility of latitude affecting PPM
values within a given habitat type, acting through variables such as length of sum-
mer growing season. Although this hypothesis remained untested in her paper, my
results firmly support it. Despite the facts that many habitat types have been con-
sidered in the European analysis and that all of them are geographically intermixed,
the effect of latitude on PPM is still clear whether habitats are combined or are
considered separately, thus indicating that habitat type per se affects migrant per-
centages secondarily or not at all.
I have not considered length of summer growing season among the variables
analysed. However, mean temperature of the coldest month emerges as a factor
strongly affecting migrant percentages and this result has a fairly reasonable eco-
logical meaning. Assuming that a breeding community is composed of two kinds of
species only, namely migrants and strict residents, PPM values will be large when,
given a total passerine density (supposedly regulated by the carrying capacity of the
environment), migrants are relatively more abundant with respect to resident spe-
cies. The latter are forced to live throughout the annual cycle in the same environ-
ment and successfully persist from one breeding season to the next. If breeding takes
place only one time each year, population levels of resident species during a given
breeding season depend not only on the success of reproduction during the previous
summer, but also on the intervening successive carrying capacities of the habitat
from summer to summer. Adverse seasons during this off-breeding period will im-
pose a "bottleneck" to the "flow" of a resident population from summer to summer.
If no substantial immigration from neighboring areas takes place, then lowered
population levels will persist until the next breeding season, when migrant species
will come in temporarily to colonize the habitat again. In this case, the latter will
successfully appropriate a larger part of total available resources and reach higher
densities. According to this reasoning, the narrower the bottleneck, the larger the
fraction of migrants during the next breeding season. However, the percentage of
migrant individuals should depend also on the total abundance of resources during
the breeding season, which imposes a second constraint on PPM: the greater the
total resource availability, the greater the total bird density exploiting it, and for a
given narrowness of the bottleneck, the larger PPM as well. Seasonal "blooms" of
insect prey are characteristic of environments with short summer growing seasons
and these environments are usually found in high latitudes, just those having the
greatest percentage of migrants in Europe.
It must be noted that it is not necessary to assume that populations of resident
species are exclusively regulated during the non-breeding season, but only that this
period plays at least part in regulation. Although this has been a traditionally con-
troversial subject, recent studies suggest that this point may be essentially correct
in some instances (e.g. Lack 1966, Fretwell 1972, Slagsvoid 1975).
In Fig. 3 I propose that PPM values depend not only on total abundance of
resources during the breeding season, but also on the severity of the winter season
faced by resident birds. Relative magnitude of resource availability and/or accessi-
bility during winter with respect to summer would be most closely related to PPM,
as is suggested in Fig. 3. The absence of any significant correlation between PPM
and either total passerine (TPD) or migrant (MD) density (demonstrated above) tends
PM :3-. ... PPM 1
Fig. 3. A simple idealized graphical model to explain the observed differences in migrant percentages
between communities under differing regimes of seasonality. It is assumed that communities are composed
of year-round residents and summer migrants only. P(t) describes the annual variations in carrying
capacity of the environment to the birds, the peak (D) corresponding to the breeding season and the
minimum (d) to the adverse season. The area under the curve is divided into two sections, corresponding
to utilization by migrants (stippled area) and residents (shaded area), respectively. According to this
model, PPM will depend simultaneously on D and d. A: For a given degree of severeness during the
adverse season (d), PPM increases with increasing D; ii: For a given resource abundance level during
breeding season (D), PPM will decrease with increasing d; C: When D and d vary simultaneously, the
final outcome will depend on the relative magnitude of D and d changes. In the case shown the curves
are parallel to each other.
to support this hypothesis, as PPM appears rather as a community-specific ratio
unrelated to the absolute magnitude of resource availability during the breeding
season (which presumably affects TPD directly), but linked to the ratio between
summer and winter conditions. Maximum figures of PPM are likely to be found in
environments characterized by very harsh winters and summers with relatively high
productivity. My results are concerned with the first aspect; assuming that ecological
severeness of the adverse season must be related in some way to winter climatic
harshness, the correlation found between PPM and MTCM tends to support the
former hypothesis. Mean temperature of the coldest month explains by itself 46%
of PPM variation in the European sample when the effects of latitude are removed.
On the other hand, evidence exists relating winter climatic features to community
parameters such as bird species diversity (Tramer 1974, Kricher 1975), bird density
(Shields and Grubb 1974), and foraging behaviour (Grubb 1975).
Length of the summer growing season was not considered in the above analysis
and some of the unexplained variation of PPM may be attributable to this neglected
variable. In any case, coldest climates in extreme latitudes are characterized by a
short growing season and both variables should be correlated to some undetermi-
nated extent. Another source of unexplained variation may be the consideration of
only tropical migrants instead of all migrant species, regardless of distance from
breeding to wintering grounds. As Willson (1976) pointed out, there is no reason
why seasonality should be reflected by tropical migrants only, and Fig. 3 is con-
structed taking account of this fact.
Obviously, I have made some simplifying assumptions that must be explicitly
recognized. It is a common feature among temperate bird communities to contain
in winter a variable fraction of non-resident birds that come in to overwinter there,
and this fact was not considered at all when constructing Fig. 3. The effects of this
neglected factor on model predictions must be especially noticeable in southern
communities and less so in mid-latitude and northern areas. The study of geograph-
ical patterns of wintering passerines in temperate regions and their ecological cor-
relates will undoubtedly modify our understanding of breeding bird community
structure (Herrera 1977). Another critical aspect to be considered is why European
tropical migrants exhibit a distributional pattern apparently similar to that shown
in North America by all migrant species combined, as revealed by Willson (1976),
whereas European-tropical (present study) versus North American-tropical
(MacArthur 1959) comparisons show contrasting patterns. Keeping in mind these
and perhaps other limitations, the above results must only serve to call attention to
the significance that the non-breeding season can have in affecting the configuration
of breeding communities. Further studies are needed before substantial conclusions
can be drawn.
ACKNOWLEDGMENTS
I express my sincere thanks to Prof. J. M. Rubio for helpful suggestions on climatic patterns, and Mrs.
Laura Fisher for kindly checking the English. Computer time was generously provided by the Centro de
C/tlculo, Universidad de Sevilla. Delia Balbontin, Paco Garcia, and other members of the staff at the
Centro de C/dculo helped in many ways. Comments of anonymous referees were most useful in improving
the paper. This work was supported by a predoctoral grant from the Consejo Superior de Investigaciones
CientJficas, Spain.
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Appendix 1
Breeding passefine species considered as migrants in this study. Only species occurring in any of the
censuses are listed.
Alaudidae: Calandrella brachydactyla.
Hirundinidae: Hirundo rustica, H. daurica.
Motacillidae: Anthus trivialis, A. cervinus, Motacilla fiava.
Laniidae: Lanius senator, L. collurio.
Muscicapidae: Locustella naevia, Hippolais icterina, Sylvia hortensis, S. borin, S. communis, S. curruca,
S. cantillans, Phylloscopus trochilus, P. bonelli, P. sibilatrix, Ficedula hypoleuca, F. albicollis,
F. parva, Muscicapa striata.
Turdidae: Saxicola rubetra, Oenanthe oenanthe, Phoenicurus phoenicurus, Luscinia megarhynchos, Cy-
anosylvia svecica.
Oriolidae: Oriolus oriolus.
Appendix
Summary of census material used in the present study.
Number
of
Location Habitat type censuses Reference
NORWAY
Nordm0re Temperate and 4 R0v 1975
boreal deciduous
Hardangervidda Mountain tundra 4 Lien et al. 1974
Trondheim Mixed forest 1 Hogstad 1967
Tran0y Island Boreal deciduous 1 Myrberget et al.
1976
Appendix 2
Continued
Number
of
Location Habitat type censuses Reference
FINLAND a
SW Finland Peatland bogs 1
Suomenselk Peatland bogs 1
Tornio-Kainuu Peatland bogs 1
Forest Lapland Peatland bogs 1
Fell Lapland Peatland bogs 1
ENGLAND
Chiltern Hills Shrubland 1
Mid-Argyll Temperate 1
deciduous
Sussex Yew woodland 1
DENMARK
AIs Temperate 1
Deciduous
POLAND
Niezgody Floodplain 1
deciduous
Radziadza Floodplain 1
deciduous
Niezgody Mixed forest 1
Borowiny Temperate 1
deciduous
Rudy Milickiej Coniferous 1
forest
CZECHOSLOVAKIA
near Brno Spruce forest 1
near Brno Temperate 4
deciduous
SWITZERLAND
Cossonay Mixed forest 1
FRANCE
Briangon Mountain 3
coniferous
Rambouillet Temperate 1
deciduous
Paimpont Lowland 4
coniferous
Vende Herbaceous 1
field
Camargue Mediterranean 1
shrubland
Jura Coniferous 4
forests
Dijon Deciduous 5
forests
SPAIN
Pyrenees Spruce dominated 1
forests
Pyrenees Pine forests 2
Almerla Coastal 1
shrubland
Huelva Evergreen-oak 2
woodlands
Jiirvinen and
Sammalisto 1976
Jirvinen and
Sammalisto 1976
Jiirvinen and
Sammalisto 1976
Jiirvinen and
Sammalisto 1976
Jirvinen and
$ammalisto 1976
Williamson 1975
Williamson 1974
Williamson and
Williamson 1973
Joensen in
Cody 1974
Mrugasiewicz 1974
Mrugasiewicz 1974
Mrugasiewicz 1974
Mrugasiewicz 1974
Mrugasiewicz 1974
Pikula 1968
Pikula 1968
Zollinger 1976
Le Louarn 1968
Le Louarn 1971
Constant etal.
1973
Thiollay 1968
Blondel 1969
Frochot 1971
Frochot 1971
Purroy 1972
Purroy 1974
Garcia and
Purroy 1973
Herrera 1977
a Each of the five Finnish censuses is the average from a certain number of nearby localities