MARINE ECOLOGY PROGRESS SERIES
Mar Ecol Prog Ser
Vol. 277: 263–274, 2004
Published August 16
Seasonal distribution of minke whales
Balaenoptera acutorostrata in relation to physiography and prey off the Isle of Mull, Scotland
Kelly Macleod1, 2,*, Richard Fairbairns3, Alison Gill3, Brenan Fairbairns3,
Jonathan Gordon1, 2, Chris Blair-Myers4, Edward C. M. Parsons1
1
Hebridean Whale and Dolphin Trust, Main Street, Tobermory, Isle of Mull PA75 6NU, UK
2
Sea Mammal Research Unit, University of St. Andrews, St. Andrews, Fife KY16 8LB, UK
3
Sea Life Surveys, Ledaig, Tobermory, Isle of Mull PA75 6NU, UK
4
Kent County Council, Maidstone, Kent ME14 1XQ, UK
ABSTRACT: Sightings of minke whales Balaenoptera acutorostrata were recorded in waters off the
Isle of Mull between March and November each year from 1992 to 1999. Survey effort amounted to
42 342.5 km, and 850 minke whale encounters were recorded. Data were analysed in relation to
undersea topography and seabed sediment type using multiple logistic regression. The effect of
potential minke whale prey distribution was inferred from maps predicting suitable habitats for the
lesser sandeel Ammodytes marinus and herring Clupea harengus constructed using a Geographical
Information System (GIS). Whale distribution changed with season, and this may be a response to a
shift in prey preferences. In spring, sediment type was a significant predictor of whale presence and
sightings predominated over mixtures of gravel/sand seabed sediments. This distribution closely
matched that of the sandeel, which is dependent on suitable winter settlement grounds. Throughout
summer, the distribution of the minke whale underwent considerable change. In June, minke whales
were predominately distributed over the sandeel habitat, but in July they dispersed to the predicted
pre-spawning herring habitat, clustering in that area by August. In the waters around Mull, shifts in
prey distribution and abundance occur between March and November and are the most likely factor
governing the distribution and abundance of the minke whale.
KEY WORDS: Minke whale · Bathymetry · Seabed sediment · Herring · Sandeel · Geographical
Information System
Resale or republication not permitted without written consent of the publisher
INTRODUCTION
In the NE Atlantic, minke whales Balaenoptera
acutorostrata range from the Barents Sea to Portugal,
and east into the western Mediterranean during summer. The wintering range is poorly known but includes
waters from the southern North Sea to the Straits of
Gibraltar (Rice 1998). The feeding season of baleen
whales generally occurs during summer and breeding
during winter. Seasonal migrations may occur between
the feeding and breeding grounds. There is considerable overlap between summering and wintering ranges
*Present address: St. Andrews.
Email: km53@st-andrews.ac.uk
of NE Atlantic minke whales, and some individuals
reside year-round in temperate waters.
The current population estimate for the North Atlantic
minke whale is thought to be in excess of 100 000 (Sigurjonsson 1995). Whilst the minke whale is not an endangered species (Reeves & Leatherwood 1994), annual
losses occur from NE Atlantic stocks through direct (e.g.
Bjorndal & Conrad 1998) and indirect takes in fisheries
(IWC 2003). Competition between minke whales and
fishermen for commercial fish species (e.g. Schweder et
al. 1998) has led to proposals for reducing the size of
minke whale stocks. Additionally, chemical and acoustic
© Inter-Research 2004 · www.int-res.com
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Mar Ecol Prog Ser 277: 263–274, 2004
pollution, and other forms of habitat degradation and loss,
are potential threats to most cetaceans, including the
minke whale (Parsons et al. 2000, Gill et al. 2001).
Effective management and conservation of cetaceans can be assisted through an understanding of the
effects of environmental factors, including physical,
chemical and biological factors, on their distribution
and abundance. Knowledge of species habitat preferences can aid the establishment of protected areas
(Hooker et al. 1999), improvement of population abundance estimates, interpretation of population trends
(Forney 1999) and understanding the consequences of
environmental shifts for long-term management. Many
factors may influence the temporal and spatial distribution and abundance of cetaceans but few studies
have investigated such links for minke whales. Water
depth (Skov et al. 1995, Hooker et al. 1999), seabed
sediment type (Naud et al. 2003), oceanographic fronts
(Kasamatsu et al. 2000), sea-surface temperature
(Kasamatsu et al. 2000, Hamazaki 2002) and the extent
of sea ice (Kasamatsu et al. 2000) are known to influence minke whale distribution, although their relative
importance varies geographically. Minke whale distribution and abundance on the feeding grounds will
ultimately depend on the distribution of their prey, as
has been demonstrated for other baleen whales
(Whitehead & Carscadden 1985, Payne et al. 1990,
Woodley & Gaskin 1996). Significant correlations
between whale distribution and environmental factors
may be indirect due to their influence on prey distribution. Many benthic and pelagic fishes show habitat
associations throughout or during parts of their life
cycle that can directly influence their survivorship
and recruitment (Reay 1970, Lindholm et al. 2001,
Maravelias 2001, Borja et al. 2002).
Minke whales have been described as the most
icthyophagous of the Balaenoptera (Gaskin 1982). In
the North Atlantic, they are known to take a range of
pelagic shoaling and demersal fish species, in particular sandeel Ammodytes sp., herring Clupea harengus,
mackerel Scomber scombrus, capelin Mallotus villosus, cod Gadus morhua and haddock Melanogrammus
aeglefinus (Jonsgård 1982, Nordøy & Blix 1992, Haug
et al. 1995a,b). The feeding habits of most baleen
whales can be categorised as skimming, swallowing or
both (Hoelzel et al. 1989). Minke whales are a typical
swallowing species and engulf prey concentrated in
shoals, which they chase and herd from below (Hoezel
et al. 1989) or locate below feeding birds (Hoezel et al.
1989, Gill et al. 2000). The lesser sandeel A. marinus
and herring are prey of the minke whale in British
waters (Nørdoy & Blix 1992) and these species are
known to exhibit habitat preferences in terms of
bathymetry and seabed sediment type. Sandeel prefer
shallow waters and seabed sediments of coarse sand
and fine gravel (Macer 1966, Reay 1970, Wright &
Begg 1997). The relative abundance of herring is influenced by temperature, seabed substrate, depth and by
boundaries between water masses that enhance local
production and food availability (Maravelias 1997,
2000). Maravelias et al. (2000) showed that aggregations of pre-spawning herring in the northern North
Sea preferred zooplankton-rich waters at depths between 100 and 150 m. Spawning herring favour gravel
beds, generally within 30 to 50 km of the coast (Saville
& Bailey 1980, Blaxter 1990).
Waters surrounding the Inner Hebrides off the west
coast of Scotland, UK, accommodate a minke whale
population in which most individuals are seasonally
resident (Gill 1994) and in which some may reside
year-round. Data collected by a tour operator in coastal
waters of the Isle of Mull, Coll and the Small Isles off
western Scotland (Fig. 1) between 1992 and 1999 were
analysed to investigate the seasonal and spatial distribution of the minke whale in relation to depth, slope
and seabed sediment type. In the absence of fisheries
data, the influence of sandeel and herring distribution,
inferred from maps of potential distribution predicted
from known associations of these species with bathymetry and sediment type, is also discussed.
Part of these data (1993 to 1995) collected by the
same tour operator were previously analysed by Leaper
et al. (1997) to assess the relative abundance and distribution of minke whales. The potential for bias in such
data sets is strong because tour operators tend to travel
to areas thought to have high densities of whales.
Leaper et al. (1997) divided the survey area into blocks
for analysis. The purpose of the stratification was to determine the largest block size such that prior knowledge of the locations in which the whales were last
found did not allow them to be found more easily in the
block on subsequent trips. With a 4 km-square block,
overdispersion caused by clumping of sightings was evident in only 3% of all blocks surveyed; this was considered the maximum size of block free of bias due to prior
knowledge of whale locations. This study further
showed that minke whale distribution changed significantly with season. These results form the basis of the
temporal and spatial stratification for this analysis.
MATERIALS AND METHODS
Data collection. Data were collected in coastal waters
off the Isle of Mull, the Small Isles and Coll (~56° 20’ to
57° N and 6° to 6° 40’ W) (Fig. 1) between March and
November each year from 1992 to 1999. The data were
collected on board the 12 m motor vessel ‘Alpha Beta’
run by an experienced tour operator, who had been
running cetacean sighting trips in the area since 1989.
MacLeod et al.: Seasonal distribution of minke whales off Scotland
265
Cetacean sightings, search effort (measured as distance travelled by the boat)
and environmental variables were
recorded by the tour operator (the vessel skipper) using Logger software
(IFAW 1994) run on a personal computer in the wheelhouse. The skipper
made observations from the wheel
house (2 m eye height), an additional
trained observer was on the flying
bridge (4.5 m eye height) and a varying
number of passengers observed from
seats on the observation deck (3 m eye
height). Surveying was carried out in
Beaufort sea states of ≤ 4.
Data on survey effort was collected
and included the position of the vessel
(NMEA 0183 serial interface between
the laptop computer and the vessel
Global Positioning System, GPS), start
and end time of trips, and the search
Fig. 1. Research area off Isle of Mull and wider Inner Hebrides, Scotland
status throughout each trip. The
search status detailed whether the obfined as shallow waters (20 to 60 m) and sediments of
servers were actively searching for whales (on effort) or
coarse sand and fine gravel (Macer 1966, Reay 1970,
not (off effort). The GPS position was updated every
Wright & Begg 1997). Pre-spawning herring habitat
5 min so that the cruise track of the vessel could be plotwas defined as water depths of 100 to 150 m (Marated. Environmental data, including wind speed, wind divelias et al. 2000) and spawning herring habitat as
rection and Beaufort sea state, were recorded in Logger
areas of gravel seabed sediments (Saville & Bailey
by the skipper. Logger data were updated at regular in1980, Blaxter 1990). Using this information, the digital
tervals (environment) or as they changed (effort and enbathymetry and sediment data were queried using
vironment). The program provided an audible prompt
ArcView, and 3 further coverages of potential sandeel
when the input of the environmental data was due.
habitat and attractive areas to pre-spawning and
When a cetacean was sighted, the time of the first
spawning herring were produced.
sighting cue, the GPS position and visual estimates of
Data analysis. All data from 1992 to 1999 were used
sighting angle and bearing were recorded in Logger.
in the analysis, with the exception of that collected
The skipper entered additional information on species
in 1996, which were considered unreliable due to
and certainty of identification, group size and composiproblems with the GPS and Logger.
tion (such as the presence of calves), behaviour and
Only positive identifications of minke whales and
associations between species and sea birds.
sightings recorded during survey effort were used in
Environmental data. Admiralty charts of the survey
the analysis. The sightings and survey effort data were
area were digitised using the Geographical Informapooled over years and stratified both spatially and temtion System (GIS) ArcInfo 8 to produce digital terrain
porally. We defined 3 seasons: (1) spring (March, April
models of seabed slope and bathymetry. A digital
and May), (2) summer (June, July and August), and
map of sediment classes in the survey area was
(3) autumn (September, October and November). Spaobtained from the British Geological Survey. The sedtial stratification of the survey area was used to aid visiment types were reclassified: (1) S1 = gravelly sand,
sandy gravel, (2) S2 = mud/sand/gravel, gravel/mud/
ual identification of ‘high use’ areas by minke whales
sand, (3) S3 = mud, sandy mud, (4) S4 = mud/sand,
and limit bias caused by the searching behaviour of the
sand and (5) S5 = rock. All data were imported into a
tour operator (Leaper et al. 1997). For this study, a 2 kmGIS, ArcView 3.2 (ESRI 1999) to form the basic envisquare grid (4 km2) was created throughout the survey
ronmental coverages on which analyses with the
area and the data were analysed on this spatial scale. A
minke whale sighting data were based.
smaller grid than suggested by Leaper et al. (1997) was
The environmental coverages were used to make
used so that relationships between minke whales and
maps of potential habitat for sandeel and pre-spawnenvironmental features on a finer scale could be invesing and spawning herring. Sandeel habitat was detigated. Changes in seasonal distribution of the minke
266
Mar Ecol Prog Ser 277: 263–274, 2004
whale were investigated through the estimation of an
encounter rate (number of sightings km–1 surveyed,
n km–1) within each 2 km square-grid and for each
season, and was mapped using ArcView.
To investigate the relationship between minke whale
distribution and environmental parameters, each
square of the 2 km grid was assigned a value for the following parameters: MD = mean depth (m); MIND = minimum depth (m); MAXD = maximum depth (m); SDD =
standard deviation depth (m) (a measure of variability
within a grid square); MS = mean slope (%); MINS =
minimum slope (%); MAXS = maximum slope (%); SDS
= standard deviation slope (%); and S1– 5 = dominant
seabed sediment type. The survey effort (E) in each grid
square was also included in the analysis as a continuous
variable to account for the varying survey effort.
General linear models (GLMs) can be used to fit nonnormally distributed data by expression of an appropriate link function (McCullagh & Nelder 1989). Logistic
regression (Collet 1991) was used to examine the importance of the environmental parameters on the distribution of minke whales. The encounter rate for each
grid square was categorised as either 0 or 1, signifying
absence or presence of whales, respectively. Logistic
regression models the probability of whale presence in
a grid square given the environmental parameters. The
logistic transformation (the link function) of a success
probability p is log(p/[1 – p]), written as:
logit(p) = β0 + β1x1i + β2x2i + … + βkxki
for k explanatory variables (x1i, x2i … xki) associated
with that observation. On rearrangement of this equation and given hi = ∑jbjxji …
pi =
e hi
1 + e hi
normal standardised deviance residuals and index plots
of Cook’s statistic (Collet 1991) were used to assess the
adequacy of the link function and to detect outliers in
the data. The analysis was carried out using Genstat 5
(Lawes Agricultural Trust 1998).
RESULTS
Between 1992 and 1999 (excluding 1996), 42 342.5 km
was surveyed on effort (Fig. 2). The total number of
minke whale encounters was 850 (Table 1), comprising
1285 individuals. Whales tentatively identified as juveniles (half to three-quarter adult size) accounted for
40.5% of individuals and 5.1% of whales encountered
were calves (less than half adult size). The proportion of
juveniles and calves in relation to the total number of
whales encountered increased from spring to autumn.
The mean group size over all seasons was 1.5 (SE = 0.9).
Mean group sizes differed significantly with season
(Kruskal-Wallis, p < 0.001), tending to be larger during
autumn than in the previous seasons. In spring and
summer, 71.3 and 77.2% of encounters, respectively,
were with single minke whales. In autumn, 55.7% of
encounters were with single individuals, the remainder
being pairs or larger groups of up to 10 individuals.
The effect of varying numbers of observers on the
number of whales sighted was not considered in this
analysis. Over all years, only 17% of sightings were
recorded as first seen by passengers, and variation in
the number of observers did not vary systematically.
Survey effort was carried out in Sea States 0 to 4, but
the greatest proportion of effort and minke whale
sightings occurred during Sea State 2 or below. For
data pooled over the years, the effect of sea state was
not significant (p > 0.05) and whale counts were not
adjusted prior to the calculation of encounter rates.
The highest mean seasonal encounter rate occurred
during autumn (Table 1) and the difference between
seasons was significant (Kruskal-Wallis, p < 0.001).
The trend for the highest encounter rates during late
summer and autumn was consistent within years.
A change in distribution and relative abundance
appeared to occur between spring and autumn (Fig. 3),
The data were overdispersed and a scale parameter
was estimated for each model. Each environmental predictor variable was modelled in turn, and the significant
variables were used to build a full model using forward
selection procedures. The significance of additional
variables was assessed using an analysis of deviance
(Collet 1991) against the critical values of a χ2 distribution (α = 0.05). Single variables significant at the 10%
level were also initially retained in the
model. The residual deviance was used
Table 1. Balaenoptera acutorostrata. Summary of minke whale sightings each
as a measure of model fit; the smaller
season pooled over years. Na: number of adults; Nj: number of juveniles;
the deviance the better the fit of the
Nc: number of calves; Nt: total number of whales; n: number of encounters;
L: total survey effort; n/L: encounter rate (n km–1); s: mean group size
model. The residual deviance of the final model, scaled for the estimated dispersion parameter, was tested against a
Season
Na
Nj
Nc
Nt
n
L (km)
n/L
s (SE)
χ2 distribution (α = 0.05), where H0 =
Spring
089
038
02
129
087
05 890.3
0.015 1.5 (0.10)
model correct, H1 = model not correct.
Summer
463
339
36
838
596
28 769.3
0.021 1.4 (0.04)
The fit of the final model was also ex07 682.9
0.022 1.9 (0.11)
Autumn
146
144
28
318
167
amined using diagnostic plots. Half-
MacLeod et al.: Seasonal distribution of minke whales off Scotland
Fig. 2. Balaenoptera acutorostrata. Survey effort, as distance
travelled (on a 2 km grid) in study area during spring (top),
summer (middle) and autumn (bottom)
267
Fig. 3. Balaenoptera acutorostrata. Encounter rates (sightings
km–1) of minke whales during spring (top), summer (middle)
and autumn (bottom)
Mar Ecol Prog Ser 277: 263–274, 2004
268
Table 2. Significant environmental variables predicting presence of minke whales Balaenoptera acutorostrata (logistic regression).
D: residual deviance; S1 to S5: seabed types (see second subsection of ‘Materials and methods’ for details)
Variable
—————— Spring ——————
Antilog β
df
D
p-value
Constant
0.072
299
250.1
Effort (E)
1.004
298
178.1
Sediment (S)
S1
S2
S3
S4
S5
1.000
0.300
0.000
0.000
0.105
295
188.3
—————— Summer ——————
Antilog β
df
D
p-value
0.436
447
550.0
0.000
1.018
446
409.9
0.000
1.000
0.877
0.360
0.629
0.059
443
486.0
0.259
286
290.6
0.000
1.025
285
244.0
0.000
0.000
1.000
0.001
2.678
2.604
0.212
282
261.4
0.000
1.014
284
282.8
0.012
1.010
284
279.9
0.003
0.039
284
282.0
0.008
1.040
285
288.2
0.065
Mean depth (MD)
1.014
441
529.6
0.002
Min. depth (MIND)
1.012
441
537.4
0.050
Max. depth (MAXD)
1.006
441
539.3
0.098
Standard deviation
depths (SDD)
Mean slope (MS)
0.853
298
244.5
0.018
Min. slope
Max. slope
2.962
0.948
298
243.8
0.012
Standard deviation 0.779
slope (SDS)
298
244.5
0.018
446
—————— Autumn ——————
Antilog β
df
D
p-value
538.9
0.001
E × MD
1.001
433
328.4
0.000
E × MIND
1.001
433
351.1
0.000
E×S
S1
S2
S3
S4
S5
1.000
1.015
1.017
1.050
0.992
430
346.3
0.000
S × MD
S1
S2
S3
S4
S5
1.000
0.962
0.961
0.977
1.042
430
359.3
0.019
SDD × MS
0.987
276
202.4
0.010
MAXD × MS
0.997
276
203.9
0.024
MAXD × SDD
0.999
276
204.4
0.032
with a noticeable shift in distribution from the area
between North Coll and Ardnamurchan in spring to
the channel between Ardnamurchan headland and the
Small Isles (Rhum, Muck and Eigg) in autumn. Environmental factors and ultimately prey distribution may
be influencing this. Behaviour consistent with feeding
activity, such as lunges through fish shoals, was observed during 27.5% of the minke whale encounters.
During all seasons, the variable that on its own had the
greatest predictive power was the amount of survey
effort in each grid square (E). Subsequent environmental parameters were fitted allowing for the effects
of survey effort. Sediment type was also significant in
all seasons (Table 2).
During spring, a further 3 variables, MAXS, MS and
SDS were, singly, significant predictors of the presence
of whales (Table 2). However, a 2-term model containing just E and S was the best fit of the data (χ2,
p = 0.492):
logit(p)MWspring = β + β1E + β2S
where β is a constant and β1 and β2 are parameter estimates for survey effort and sediment class. The parameter estimates (Table 3) show that S1, gravelly sand,
seabed sediment, is the strongest predictor of the presence of a minke whale within any grid square compared to other sediments. Sediments of mud/sand/
gravel (S2) are also an important predictor, but to a
lesser extent than S1. Seabed sediment is likely to have
an indirect influence on minke whale distribution, possibly through its influence on sandeel distribution.
Fig. 4 shows the distribution of minke whale sightings
MacLeod et al.: Seasonal distribution of minke whales off Scotland
during spring in relation to predicted sandeel habitat.
The majority of the sightings are within a single sediment type (gravelly sand) and within depths of less
than 60 m.
A number of environmental variables were, singly,
significant predictors of minke whale occurrence during the summer (Table 2). In addition to E and S, MINS,
MD, MIND and MAXD were significant. MAXD and
MD were strongly correlated (p < 0.001) and, as the
less significant predictor variable, MAXD was therefore eliminated from further analysis. At the 5% level,
3 interaction terms, E with S, MD and MIND, were also
significant. The interaction between E and MD was the
most significant and only the interaction between E
and S was significant when added to this. The final
model (χ2, p = 0.504) was:
269
August (Fig. 5) could be explained in terms of a shift in
prey preference from sandeel at the beginning of summer to herring towards the end of the season.
logit(p)MWsummer =
β + β1E + β2S + β3MD + β4E × MD + β5E × S
Of the dominant sediment types, the probability of
minke whale presence was greatest in areas of
mud/sand/gravel mixtures (S2). Deeper waters also increased the probability of whale occurrence (Table 3).
During summer, particularly July, a number of known
prey species, such as sprat Sprattus sprattus and mackerel, are abundant in the survey area. The range of
environmental variables which, used singly, were significant predictors of whale presence may indicate that
minke whales do not have a strong habitat (and therefore prey) preference during summer. Alternatively,
the patterns of whale distribution between June and
Table 3. Summary of parameter estimates for final multiple logistic regression models of significant variables for each season
Variables
Spring (SE)
Summer (SE)
Autumn (SE)
Constant
0.106 (0.258)
0.311 (0.352)
0.015 (0.618)
Effort
1.029 (0.004)
0.991 (0.004)
1.025 (0.004)
Dominant sediment
S1
S2
S3
S4
S5
1.000
0.700 (0.579)
0.000 (10.2)
0.000 (13.3)
0.164 (0.520)
1.000
2.754 (0.679)
1.112 (0.461)
0.801 (0.544)
0.121 (0.550)
1.000
0.001 (9.33)
2.863 (0.373)
1.481 (0.464)
0.215 (0.707)
Mean depth
0.987 (0.069)
SDD
1.142 (0.036)
Mean slope
1.271 (0.143)
SDD × MS
0.987 (0.005)
E × MD
1.001 (0.000)
E×S
S1
S2
S3
S4
S5
1.000
0.980 (0.015)
0.990 (0.010)
1.024 (0.014)
1.010 (0.004)
Fig. 4. Balaenoptera acutorostrata. Minke whale sightings
during spring as a function of predicted sandeel habitat
270
Mar Ecol Prog Ser 277: 263–274, 2004
During autumn, SDD, MAXD, MD and MS were significant predictors of minke whale presence in addition to E and S. There were 3 significant interactions:
MAXD and both SDD and MS, and SDD and MS
(Table 2). The interaction between SDD and MS was
the most significant and the 2 other interactions did not
reduce the deviance significantly when added to the
model, and were thus eliminated. The final model
(χ2, p = 0.488) was:
logit(p)MWautumn =
β + β1E + β2S + β3SDD + b4MS + b5SDD × MS
The parameter estimates (Table 3) indicate that the
probability of encountering a minke whale was increased in areas with mud or sandy mud sediments (S3)
and where SDD and MS was greater, perhaps indicative of areas of variable seabed topography. Most
autumn sightings with minke whales were in areas
predicted to be suitable for pre-spawning herring
(Fig. 6) and thus predation by minke whales on this
species in autumn is a possible explanation for the spatial distribution of whales. Feeding on bait balls of
juvenile herring has been observed during September
in the survey area (A. Gill pers. comm.).
DISCUSSION
A shift in the spatial and temporal distribution of the
minke whale was apparent in the Hebridean waters off
the Isle of Mull (Fig. 3). In spring, minke whales were
distributed predominantly between Ardnamurchan
and Coll. During summer, the whales appeared to disperse over a wider area extending as a ‘corridor’ of
higher encounter rates between the north of Coll and
the east of Muck and Eigg. Finally, a concentration of
whales southeast of Muck and Eigg predominated in
Fig. 5. Balaenoptera acutorostrata. Changes in distribution of
sightings during summer months (June, July and August) as a
function of predicted sandeel and herring habitats
Fig. 6. Balaenoptera acutorostrata. Minke whale sightings during autumn as a function of predicted herring pre-spawning
and spawning habitats
MacLeod et al.: Seasonal distribution of minke whales off Scotland
the autumn, with a few scattered areas of high encounters in the southern region of the Treshnish Isles. The
encounter rates suggest that the relative abundance of
the minke whale reaches a peak during the end of
summer and beginning of autumn annually.
Minke whales are present off the Island of Mull and
wider Inner Hebrides throughout summer, the main
feeding season for baleen whales. During this period,
their distribution changes, and this may be a response
to changing prey availability. The minke whale diet is
flexible, varying spatially and temporally. A strong correlation exists between prey availability and minke
whale diet (Haug et al. 1995, Tamura & Fujise 2002).
In spring, the environmental variable with the most
influence on the presence of minke whales was sediment type, in particular gravel/sand mixtures, with
small quantities of mud and rock. The distribution of
whale sightings compared well with the expected
inferred distribution of sandeels during the spring
(Fig. 4). Sandeels are a schooling fish, are of high
calorific value (Hislop et al. 1991) and are eaten by a
range of marine predators. Sandeels burrow into the
seabed from October to early April, with the exception
of a short period between December and January
when they emerge to spawn. Sandeel distribution is
restricted by their dependence on suitable settlement
grounds and the most favourable sediments include
clean, coarse sands or fine gravel (Reay 1970). In the
North Sea, Ammodytes marinus is most abundant in
depths of 20 to 40 m (Macer 1966). During April and
May, 1-group and older sandeels emerge from the
seabed to feed in the water column. They retreat to the
sediment as a form of defence, which binds them to the
sediments from which they emerged. The 0-group
sandeels disperse over wider areas than the older age
classes (P. J. Wright pers. comm.). Therefore, during
spring, sandeels are available in the water column as
prey to minke whales. The local sandeel fishery coincides with this timing, starting in April and finishing in
mid-July (H. Allen pers. comm.). Minke whales off the
Mingan Islands in the Gulf of St. Lawrence were
sighted more frequently over sand dunes, where their
2 main prey items, sandeels and spawning capelin,
were abundant (Naud et al. 2003). A link between
sandeel distribution and other marine predators has
been established, including the common guillemot
Uria aalge (Wright & Begg 1997), the humpback whale
Megaptera novaeangliae (Payne et al. 1986) and the
fin whale Balaenoptera physalus (Overholtz & Nicolas
1979).
The summer distribution of minke whales may represent a shift in dietary preference from one prey to
another as the season progresses. The whales are distributed widely in the research area; this may be a
response to increased prey availability, with 2 abun-
271
dant species, sandeels and herring, dominating the
diet in early and late summer, respectively. Stockin et
al. (2001) noted significant differences in the surfacing
intervals of minke whales off Mull between April and
October. This was interpreted as a result of changes in
the foraging strategies of minke whales during this
period. The spatial distribution of whale sightings
appears to correlate with the likely sandeel distribution in June and the pre-spawning herring habitat in
August (Fig. 5). During July, many prey species are
abundant and minke whales may not have strong prey
preferences at this time, as reflected in the range of
single environmental predictor variables significant for
the summer season.
The distribution of whales during August, southeast
of the islands of Muck and Eigg, is maintained into
the autumn (September to November) and is possibly
linked to a continuation of feeding on pre-spawning
herring. The waters of the Inner Hebrides are nursery
grounds for herring, but minke whales target certain
age classes (Haug et al. 2003) and may only feed on
schools that have reached a certain threshold density.
Small prey that occurs in dense schools is probably
easier to catch. The energy density of herring, like
other fish species, varies seasonally but reaches a peak
in September (Mårtensson et al. 1996). Off Mull, herring form large schools and spawn during late August
through October, but begin to congregate near the
spawning grounds about 2 mo before this time. They
move to deeper, cooler waters below the thermocline
and undertake diurnal vertical migrations. Their daily
migration may be a response to that of Calanus finmarchicus, their main food, which also moves into
deeper, cooler waters beneath the thermocline during
summer and autumn (Maravelias & Reid 1997). This
may explain the preference of minke whales for
deeper waters east of Muck during late summer and
autumn (Fig. 6). Herring also school in areas of
increased productivity (Maravelias et al. 2000).
Increased mixing in the vicinity of the Small Isles
occurs due to the confluence of fresher coastal water
north of Ardnamurchan and close to the south coast of
Skye, with the coastal current as this travels northward. Additionally, the surrounding islands, headlands
and channels increase mixing and may enhance productivity in this area (Pingree & Maddock 1985). Topographic fronts can also form in the lee of islands and
headlands and are often the location of enhanced primary and secondary production (Simpson et al. 1982).
The final model of the autumn data highlighted the
significance of areas of high topographic relief. Varied
seabed topography can also enhance productivity. The
predominance of herring in the minke whale diet in
areas of the NE Atlantic is well known (Nordøy & Blix
1992, Mårtensson et al. 1996, Lindstrøm et al. 1999).
272
Mar Ecol Prog Ser 277: 263–274, 2004
The apparent increase in group sizes in autumn may
be a response to the abundant prey and large school
sizes of herring.
The searching behaviour of the tour boat is a potential source of bias in these data. As a commercial venture, the boat tends to search areas where cetaceans
have been encountered before. The importance of this
variable was reflected in the significance of survey
effort in each grid square in all models. Attempts to
limit this bias were made by modelling environmental
variables to allow for the effects of survey effort. The
index of abundance was also chosen such that survey
effort was the denominator of the encounter rate;
thereby relative abundance between grid squares
would be comparable. Finally, the data were spatially
stratified on the basis of the results presented in
Leaper et al. (1997) to minimise bias caused by searching behaviour of the tour operator.
This study suggests that 2 areas contained concentrations of minke whales for most of the tour operator’s
season. The area north of Coll had relatively high
encounter rates throughout spring and summer. It did
not seem to be of importance in autumn; however survey effort was low in this season. The area between
Muck and Ardnamurchan was used throughout summer, but in particular during autumn. On this basis,
these 2 areas may be considered as being of particular
importance to minke whales in this area, a conclusion
also drawn by Leaper et al. (1997). Evidence of territoriality in minke whales was proposed by Dorsey (1983)
from studies of identified minke whales in the coastal
waters of Washington State. The whales formed 3 distinct groups and each occupied a ‘home-range’ which
adjoined but did not overlap with the ranges of the
other groups of whales. Future research of the habitat
use of identified minke whales in the Mull area could
be used to investigate whether the 2 high-use areas
identified represent core ranges for different, but consistent, groups of minke whales during the tour operator’s season. However, the photo-identification catalogue for this area is relatively small, with few resightings, and currently does not allow such analysis.
Alternatively, differences in the arrival time and usage
of the area around Mull for feeding may vary with
changing proportions of age and sex classes from
spring to autumn, explaining the observed changes in
distribution. The results from marking experiments off
Svalbard and Norway have shown that females arrive
at the feeding grounds before males (Christensen &
Rørvik 1980). In the Antarctic, females generally occur
at higher latitudes than males during the feeding
season (Ohsumi & Masaki 1975).
At present there are limited threats to minke whales
in these waters, but increased understanding of this
species ecology could be important in the future. Com-
parable studies on minke whales and environmental
variables in the wider Hebridean waters would be of
use in determining on a wider geographical scale the
stability of those environmental parameters identified
as important in this study.
Acknowledgements. This work was funded by a grant from
the Worldwide Fund for Nature (UK) and was part of a PhD
study at the University of Greenwich, London. We thank Dr.
D. Jeffries, Natural Resources Institute and Dr. P. Hammond,
Sea Mammal Research Unit, for advice on the analysis
of these data. Thanks to reviewers of previous drafts of
this paper — Professor J. Mathews and F. Hansen of the
Hebridean Whale and Dolphin Trust and Professor D.
Thomas, Natural Resources Institute. Thanks to H. Allen,
Northwest Fisheries Association, for specific details on local
fish distributions and to Dr. P. Wright for information on
sandeel distribution. The Logger program was funded and
developed by the International Fund for Animal Welfare.
Admiralty charts were digitised by permission of the Controller of Her Majesty's Stationary Office and the UK Hydrographic Office. Helpful comments on the manuscript were
given by 3 anonymous reviewers.
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Editorial responsibility: Otto Kinne (Editor),
Oldendorf/Luhe, Germany
Submitted: October 17, 2003; Accepted: May 11, 2004
Proofs received from author(s): July 30, 2004