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Monodon monoceros Linnaeus,
1756
English: Narwhal
Germa: Narwal
Spanish: Narval
French: Narval

Monodon monoceros © Würtz-Artescienza (see "links")
1. Description
Narwhals are completely mottled on the back with white ventral
and lateral fields that increase with age. Old males only maintain
a narrow dark spotted pattern on the top of the back, whereas the
rest of the body is white. Newborns are grey to brownish and develop
the mottled pattern after 2 years. The rear margin of the tail flukes
is markedly convex and the fin is replaced by a low ridge. Average
Body length is 400 cm and 450 cm in adult males and females, respectively,
and mass reaches 1000 kg and 1600 kg, respectively (Heide- Jørgensen,
2009).
In males, usually the left one of two elongated maxillary teeth
grows and protrudes through the maxillary bones and skin of the
rostrum. Some males lack the tusk whereas others may develop two.
Females may sometimes have a tusk as well. The largest tusk measured
was 267cm long, normal size is 200 cm. The tusk is believed to be
a secondary sexual character determining social rank among males
(Heide- Jørgensen, 2009). During growth, the tusk spirals
and grooves to the left. However, the tusk as a whole does not seem
to revolve during growth (Heide-Jørgensen et al. 2008).
2. Distribution
The narwhal is discontinuously circumpolar and arctic. It is observed
very infrequently south of 65°N in Greenland. However, during
spring, when distributional ranges may overlap north of Greenland,
its range may become circumpolar (Born, 1994). The main part of
the population occurs in the eastern Canadian Arctic and west Greenland.
Observations by Gjertz (1991) suggest that off Svalbard narwhals
concentrate in the north-west area of Spitzbergen.
Narwhal Monodon monoceros distribution
in the Arctic Ocean and adjacent Greenland Sea,
Baffin Bay, Davis and Hudson Strait (Jefferson et al. 2008; ©
IUCN; enlarge
map).
Narwhals are vagrant south to the coast of Labrador
(Rice, 1998), rare to accidental south to Iceland, the Norwegian
Sea, the North Sea (south to the British Isles, The Netherlands
and Germany), the White Sea, and the arctic coast of mainland Eurasia,
and east into the Chukchi Sea and the Bering Sea, as far south as
Komandorskiye Ostrova and the north side of the Alaska peninsula
(Rice, 1998).
3. Population size
The most recent population estimates come from Nunavut waters in
Canadian Arctic waters, where the highest narwhal concentrations
are found (Jefferson et al. 2008). Abundance estimates for Somerset
(45,358; CV = 0.35; Innes et al. 2002); Admiralty (5,362; CV = 0.5);
Eclipse (20,225; CV = 0.36); East Baffin Bay (10,0073; CV=0.31)
and North Hudson Bay (5,053; CV = 0.4) sum up to a total of 86,000
individuals (DFO, 2008).
Abundance in Inglefield Bredning and adjacent fjords in northwest
Greenland was estimated using aerial digital photographic techniques
in August 2001 and 2002, resulting in abundance estimates of 2,297
(95% CI: 1,472-3,122) and 1,478 (95% CI 1,164-1,793) in these two
years, respectively (Heide-Jørgensen, 2004). This corresponds
to a 10% decline as opposed to line- transect surveys conducted
in 1985 and 1986 (Born et al.1994)
In the Eurasian sector of the Arctic the only known estimate of
narwhal numbers is from Scoresby Sound and King Oscar Fjord in eastern
Greenland. A conservative figure of only 176 was obtained from an
aerial line-transect survey carried out in September 1983 by F.
Larsen (cited in Hay and Mansfield, 1989). Born (1994) confirms
that more detailed data is lacking. He suggests that in this sector,
narwhals prefer areas distant from the coast and may number at most
a few thousand individuals. There is no recent data available for
any of the north-east Atlantic waters (Jefferson et al. 2008; Heide-Jørgensen,
2009).
4. Biology and Behaviour

Narwhal and kayak © Don McMichael (see "links")
Habitat: Narwhals are considered deep-water cetaceans, associated
with the pack ice (Hay and Mansfield, 1989). Other investigators,
however, dispute their characterization as deep-water species, noting
that they occur in waters of different depths. Born (1994) suggests
that the occurrence of narwhals and belugas (Delphinapterus
leucas) is mutually exclusive, since summering and wintering
grounds differ both in location and time, which seems to exclude
competition for food. When both species do occur in the same areas,
they seem to reduce competition by foraging at different depths.
Schooling: Most pods consist of 2-10 individuals but they
may aggregate to form larger herds of hundreds or even thousands
of individuals (Jefferson et al. 1993).
Reproduction: The gestation period is estimated to be 15.3
months. The season of conceptions is March to May and calving occurs
during July and August. Since the lactation period exceeds 12 months,
the interval between successive conceptions is usually three years,
but about 20% of females conceive at the first breeding season following
birth of their calves. The annual population birth rate is calculated
to be about 0.07. The basic life history features of the narwhal
are similar to those of other medium-sized toothed whales (Hay,
1985). Narwhals can reach very high ages: Age estimates based on
the racemization of l-aspartic acid to d-aspartic acid in the nucleus
of the eye lens yield a maximum estimated age of 115 years in a
female specimen. Age at sexual maturity is estimated to be 6-7 years
for females and 9 years for males (Garde et al. 2007).
Food: Narwhals feed heavily during migrations, but very
little during the open water season (Hay and Mansfield, 1989; Reyes,
1991 and refs. therein). Consequently, stomachs collected from narwhal
summer harvests were mostly empty with little evidence of recent
feeding. Stomachs collected in late fall and winter harvests had
considerable amounts of undigested material with evidence of recent
feeding. In summer, Arctic cod (Arctogadus glacialis), polar
cod (Boreogadus saida), and Gonatus squid spp. constituted
the narwhal diet.
In the fall, Gonatus fabricii was the only prey item observed.
In late fall and winter, Greenland halibut (Reinhardtius hippoglossoides)
and G. fabricii were the dominant prey items, observed in
51% and 73% of stomachs collected, respectively. Greenland halibut
taken by narwhals were on average 39 cm and 556 g and G. fabricii
were on average 23 g with mean mantle lengths of 85 mm. The low
diversity of prey species indicates narwhals have a restricted diet
across all seasons (Laidre and Heide-Jørgensen, 2005).
Further prey items include the shrimps Pasiphaea tarda and
Hymenodora glacialis (Hay and Mansfield, 1989; Reyes, 1991
and refs. therein). In Baffin Bay, narwhals fitted with satellite-linked
time-depth recorders selected bottom temperature ranges and gradients
in their wintering grounds which often coincided with areas of concurrent
high density of Greenland halibut and predictable open water in
winter pack ice (Laidre et al. 2004). Stomach content analyses suggest
that they feed over a wide range of depths, at least in the Baffin
Bay area (Hay and Mansfield, 1989). Whales occupying one wintering
ground spent most of their time diving to between 200 and 400 m
whereas narwhals in a separate wintering ground spent less time
at shallow depths and most of their time diving to at least 800
m (Laidre et al. 2003). The deepest recorded diving depth was 1,864m,
and dive times usually amounted to 25-30 min (Heide-Jørgensen,
2009).
5. Migration
Throughout the year, narwhals live in close contact
to the Arctic pack ice (Born, 1994). They follow the distribution
of the ice and move towards coastal areas when these are ice free.
During freeze-up, the coastal areas are abandoned and the narwhals
move offshore (Heide-Jørgensen, 2002). Observations from
airplanes suggest that narwhals overwinter in small groups within
heavy pack ice, whereas only a few animals were observed in loose
pack ice and open water (Koski and Davis, 1994).
Narwhals instrumented with satellite transmitters in Tremblay Sound,
northeast Canada went northwest visiting adjacent fjords before
moving south, along the east coast of Baffin Island. The narwhals
arrived on the wintering ground in northern Davis Strait in late
October. Speed and range of movements declined once the wintering
ground was reached. Late summer and winter kernel home ranges were
approximately 3,400 km² and 12,000 km², respectively.
(Heide-Joergensen et al. 2002). Female narwhals tracked by satellite
from their summering ground near Somerset Island in the Canadian
High Arctic went to wintering grounds in central Baffin Bay which
are spatially discrete from another narwhal wintering ground located
earlier. The area of the summering ground was approximately 9,464
km² and the area of the wintering ground was 25,846 km²
(Heide-Jørgensen et al. 2003). Resighting of a tagged narwhal
10 years after tagging confirms evidence for site fidelity and for
the same migratory schedule and route over large time periods (Heide-Jørgensen
et al. 2008).
At summering grounds in West Greenland and Canada, narwhals moved
back and forth between glacier fronts, offshore areas and neighbouring
fjords (Dietz et al. 2001). When fast ice formed, the whales moved
out to deeper water, usually up to 1,000m water depth. In October,
the whales moved southward toward the edge of the continental shelf
where water depth increases over a short distance from 1,000 to
2,000m. This slope in central Baffin Bay was also used as a wintering
ground, and even though the whales seemed stationary in this area,
they still conducted shorter movements along the steep continental
slope. Narwhals satellite-tracked from Canada and West Greenland
were within a few kilometres from each other at these wintering
grounds. The importance of this wintering ground in central Baffin
Bay has also been confirmed by aerial surveys (Heide-Jørgensen,
2002).
The regular occurrence of narwhals at Repulse Bay in north-western
Hudson Strait suggests that they may overwinter there as well, or
possibly in Hudson Strait where they were also observed by McLaren
and Davis (Hay and Mansfield, 1989).
The migratory cycle in east Greenland waters is not well known.
Apparently narwhals migrate to the north and north-east into the
ice fields of the Greenland Sea during May-July. Some whales migrate
eastwards to the vicinity of Franz Josef Land and as far east as
the new Siberian Islands. A few whales also visit the fjords of
north-western Greenland. Their southward migrations in autumn lead
them to the southern Greenland Sea, Barents Sea and Denmark Strait
(Hay and Mansfield, 1989).
Genetic data shows that narwhals from the eastern Canadian Arctic
have little contact with animals from eastern Greenland, and even
between geographically close areas, which is attributed to their
fidelity to specific summer and autumn feeding grounds (Born, 1994;
Palsboll et al. 1997). 
6. Threats

Drawing of M. monoceros by courtesy of North
West Territories PAS (see "Links")
Direct catch: The narwhal has been hunted since the earliest
times by the Inuit (Reyes, 1991), with an annual take in the order
of 1,000 animals. Recent data confirms that these levels are still
maintained today, with annual catch rates at 535 and 433 between
2000-2004 in West Greenland and Canada, respectively (Heide-Jørgensen
2009). However, while male narwhals compose most of the landed catch,
annual harvest statistics underestimate total numbers of narwhals
killed due primarily to the non-reporting of struck-and -killed
but lost whales. The estimated total kill of narwhals may exceed
the reported landed catch by 40% (Roberge and Dunn, 1990).
The North Atlantic Marine Mammal Commission (NAMMCO) has repeatedly
expressed grave concern on the apparent decline of stocks in West
Greenland, and while commending Greenland for the recent introduction
of quotas, there is still serious concern that present takes of
narwhals in West Greenland, according to the advice of both the
NAMMCO Scientific Committee and the Canada/Greenland Joint Commission
on Narwhal and Beluga Scientific Working Group are not sustainable
and will lead to further depletion of the stocks. The quota for
Greenland was 385 animals in the 2006/2007 season, again well above
the recommended level of 135. In east Greenland, around 100 are
assumed to be taken annually, without quotas nor harvest sustainability
assessment (NAMMCO, 2006).
Narwhals supply various staples in the traditional subsistence economy.
Today the main products are muktaaq and ivory. The large tusks of
adult males are sold in the speciality souvenir market both inside
Canada and in the global marketplace. The price of narwhal ivory
has increased substantially over the past years. Canadian narwhal
ivory traditionally was exported to the United Kingdom, then often
re-exported. The EEC ban closed the direct link with the United
Kingdom. Consequently, new markets developed in Japan and Switzerland.
Narwhal hunting remains an important source of food and cash income
for residents of some coastal communities in the eastern Canadian
Arctic and Greenland. The international ivory trade provided an
incentive to procure large tusks, and this may have strongly influenced
the nature and intensity of the hunt (Reeves, 1992). However, international
trade is now regulated through the Convention on International Trade
in Endangered Species (CITES), requiring national permits for import
and export (all Cetacea are listed in either CITES Appendix I or
II). Furthermore, Greenland installed a ban on all narwhal product
exports in 2006 (Heide-Joergensen, 2009).
Natural enemies: Natural enemies include Greenland sharks
(Somniosus microcephalus), orcas, polar bears and walrus,
although the mortality rates inflicted by these species do not seem
to be very high (Born, 1994). The same author reports that narwhals
do occasionally become trapped in fast forming ice and may die during
the winter because of exhaustion in an attempt to keep the breathing
hole open.
Habitat degradation: Because of their prevalence for high-density
pack-ice, narwhals are susceptible to man-made as well as natural
climatic changes influencing the water currents and ice formation
in the Arctic (Heide-Jørgensen, 2002).
Pollution: Anthropogenic threats include pollution via heavy
metals and organochlorines (Heide-Jørgensen, 2009). Cadmium
concentrations seem to be significantly higher in narwhals than
in other cetaceans (Born, 1994 and references therein). Highest
Cadmium concentrations were reported from narwhals living along
the Canadian coast, whereas lead concentrations were higher in west
Greenland animals. Narwhal skin as a whole (in Inuktitut known as
"muktuk") is considered to be a delicacy by native Canadian
and Greenland people. However, concentrations and patterns of polychlorinated
biphenyls (PCBs), chlorinated pesticides, and polybrominated diphenyl
ethers (PBDEs) in narwhal blubber from Svalbard, Norway showed a
broad range of pollutants in relatively high concentrations. PCBs
and pesticide levels in lipid were approximately 9 µg/g 24
µg/g, respectively, while PBDEs 47 levels were approximately
170 ng/g. Compared with other marine mammals from the same area,
contaminant levels are among the highest ever measured, indicating
a low capacity for contaminant metabolism. These high levels are
further explained by substantially high contaminant levels in the
benthic diet of narwhals (Wolkers et a. 2006). While PCB and DDT
concentrations in West Greenland narwhals were half those found
in East Greenland and Svalbard (Dietz et al. 2004), the concentration
of total mercury is 0.59 µg/g (wet wt) in narwhal skin as
a whole (muktuk), exceeding Canadian Government's Guideline (0.5
µg/g wet wt) for fish export and consumption (Wagemann and
Kozlowska, 2005). To conclude, human consumption of narwhal muktuk
seems to bear health risks.
7. Remarks
Range states (Jefferson et al. 2008) :
Canada; Greenland; Russian Federation; Svalbard (Norway) and Jan
Mayen (Norway).
The species is included in Appendix II of CMS and in Appendix II
of CITES. The narwhal is categorized as "Near Threatened"
by the IUCN (Jefferson et al. 2008), because there is clear evidence
for the ongoing decline of several sub-populations of the species,
also attributed to intensive hunting of the species in Canada and
Greenland.
The IWC Scientific Committee (2000) recommended that genetic and
telemetric studies are needed to identify stocks, and improved catch-reporting
(including estimation of hunting loss) should be conducted in Canada
and Greenland.
Information on life history, distribution, abundance and actual
hunting loss rates are needed to assess and manage the stocks. The
probable effects of pollution, industrial development and climatic
change should be fully studied, since these may represent a potential
threat.
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© Illustrations by Maurizio Würtz, Artescienza.
© Maps by IUCN.

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