ARCTIC ECOSYSTEMS IN PERIL: REPORT OF THE ARCTIC GOOSE HABITAT WORKING
GROUP
GREATER SNOW GEESE IN BREEDING, STAGING AND WINTERING AREAS
The single population of this sub-species breeds from northern Baffin
Island and northwards and birds feed predominantly on sedges and grasses
growing in moss-covered fens and in uplands during the summer. There is
evidence of changes in habitat use by snow goose families, possibly in
response to food depletion in the grass and sedge fens which are their
preferred habitat. These are habitats where there is a well developed
organic substratum, unlike the situation on the intertidal flats of the
Hudson Bay coast. Parallels can be made between the two subspecies and
their effects on vegetation, but there are also differences, primarily
related to the use of different species as a prime source of forage.
Damage to Coastal Habitats in the Wintering and Staging Areas
Prior to the 1960s the geese fed almost exclusively in freshwater tidal
marshes dominated by the bulrush, Scirpus americanus, particularly
in the marshes of the St. Lawrence River (Giroux and Bédard 1987,
Reed 1989). Smith (1983) reported that greater snow geese altered the
species composition of salt marshes on the wintering grounds in North
Carolina. The birds grazed intensively on Spartina alterniflora and on Spartina patens and the above-ground biomass was severely
reduced (Smith and Odum 1981, Fig. 2.20).
However, the vegetation was not eliminated and full recovery of the latter
species occurred in exclosures which were protected for two growing
seasons after grazing ceased. Scirpus robustus invaded heavily
grazed patches of Spartina alterniflora. Stands of Scirpus
americanus were unaffected by grazing, the percentage cover in grazed
and ungrazed areas was not significantly different. Eleocharis species were only present in grazed sites. Of course, the geese grazed
only during the period when the marsh plants were dormant, hence the
effects of grazing and rhizome grubbing were not likely to be as severe as
when active growth was occurring. Nevertheless, grazing/grubbing led to a
decrease in net below-ground production and a change in species
composition.
Formerly, staging in the St. Lawrence estuary occurred almost
exclusively in the Scirpus americanus marshes, and even today,
with many more geese and an expanded range, those marshes are of critical
importance. Vigorous grubbing by the geese removed an estimate 74% of the
underground biomass of Scirpus in one year in a major marsh area,
however, no long term trend in abundance of the plant occurred (Reed
1989). In another marsh, it was demonstrated that net above ground primary
production of Scirpus was lower in areas exposed to heavy grubbing
by geese than in areas protected from grubbing (Giroux and Bédard
1987) but the heavily grubbed areas were maintaining their production
(albeit at a lower-than-potential level) over the long term (Reed and
Giroux, unpublished data). Expansion of the staging area downstream led to
geese feeding on salt-marsh vegetation, including Spartina
alterniflora and Spartina patens. Although marshes continue to
be used as roost sites (Gauthier et al. 1988), the low abundance
of Scirpus americanus and the high extraction cost and low energy
return associated with Spartina roots has led to the birds feeding
in agricultural land (Bédard and Gauthier 1989). The rhizomes of
bulrush (S. americanus) are still an important component of the
diet, but there are indications that demand is outstripping the regrowth
potential of stands of bulrush, and that soft mudflats are replacing
former stands of bulrush. A similar situation exists in the Fraser Delta
in British Columbia, where lesser snow geese eat a substantial proportion
of the total rhizome of each plant of Scirpus (Burton 1977). In
addition, the geese there are increasingly foraging for waste crops on
agricultural land (potato fields, corn and wheat stubble fields).
Damage to Agricultural Crops
Most of the reported damage to agricultural land in the USA by greater
snow geese is associated with small grain crops, particularly winter
wheat. Damage can result from a variety of causes but it includes removal
of seedlings, grazing of plants, and the loss of seed heads (Anonymous
1981, Hindman and Ferrigno 1990). In some areas, the persistent foraging
by geese has led to reduced wheat yields. The birds also glean grain from
old fields of corn (Zea mays) and soybean (Glycine max)
(Reed 1991). A crop damage insurance program began in Québec in
1992. Costs of reported damage to hay crops by GSGO in Québec from
1992-1995 are shown in Table 2.1.
Most agricultural land adjacent to the marshes in the St. Lawrence River
is managed for hay production based on a 4-6 year rotation system with
oats/barley, Phleum pratense, Trifolium pratense and Medicago
sativa. In spring, geese graze the new green growth which is mostly Phleum (timothy grass). Heavy grazing on this growth and that of
other forage species can significantly reduce hay yields at first harvest
(Bédard et al. 1986, Reed and Cloutier 1990) which occurs
from mid- to late-June (Reed 1991). This is approximately 3 to 6 weeks
after the northward migration of geese from the area. In the Montmagny
area where the grazing is particularly intensive, a mean loss of 14% in
hay yield was recorded in old and new hay fields in 1980. By 1985 goose
usage had tripled and hay losses at harvest had doubled (Bédard and
Lapointe 1991). Yield loss is not uniform across the entire area but is
concentrated in a few individual fields, hence the loss is
disproportionately high for a small group of farmers. Gauthier and Bédard
(1991) have experimented with forage mixtures which are less palatable to
the geese. Among legumes, Trifolium pratense ranked highest and Lotus corniculatus lowest in preference. Among grasses, Phalaris arundinacea (canary grass) was the preferred species followed
by Dactylis glomerata, Bromus inermis and Phleum
pratense. They conclude that the substitution of Trifolium with Lotus would reduce the attractiveness of hay fields to snow
geese.
Table 2.1. Crop damage by greater snow geese in Québec (data
courtesy of Michel Lepage, Ministère de l'Environnement et de la
Faune du Québec).
|
1992 |
1993 |
1994 |
1995 |
Claims for goose damage |
$ 466,600 |
$ 211,500 |
$ 500,000 |
$700,000 |
Compensation paid |
$ 373,270 |
$ 169,200 |
$400,000 |
$ 560,000 |
Administrative cost |
$ 139,200 |
$ 72,700 |
$ 193,200 |
$ 186,600 |
Preferred Forage Species on the High Arctic Breeding Grounds
Much of the information discussed below is based on the results of G.
Gauthier and his group working on Bylot Island, NWT, where there is a
large breeding colony of greater snow geese numbering 27,500 breeding
pairs in 1993 (Reed and Chagnon 1987; Reed et al. 1992, and A.
Reed, unpublished data).
Grazing by geese has had a major impact on the above-ground biomass of
forage graminoid species and the effect of the geese on the vegetation has
increased in recent years (Gauthier et al. 1995). Although Dupontia
fisheri is the dominant plant in moss covered fens in which family
groups of greater snow geese feed, the impact of goose grazing was more
severe on Eriophorum scheuchzeri/angustifolium than on Dupontia. Peak above-ground biomass in ungrazed areas averaged 33
g dwt/sq m. In all years of a three-year study, it was estimated that
geese consumed from 65-113% of the cumulative net above- ground primary
production (NAPP) of Eriophorum species and 30- 78% of the
cumulative NAPP of Dupontia. Grazed plants were able to grow new
foliage, but grazing did not enhance NAPP, unlike at La Pérouse Bay
where swards of Puccinellia phryganodes show increased NAPP
following defoliation (Cargill and Jefferies 1984).
It is likely that this pattern of grazing is common in the high Arctic.
Again, there are indications that with the increasing number of birds the
swards may not be able to regenerate and foraging areas will become moss
carpets. On the Tundra of the Academy on Wrangel Island this has occurred
in the vicinity of shallow, thermokarst lakes (R. Jefferies, per. obs.).
However, in general, there does not appear to be the level of damage in
the high arctic that characterizes the coastal areas of the subarctic
Hudson Bay lowland.
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