Sphagnum moss is strikingly different from all other mosses in its
structure and its influence on the growth of other plants. Both its
leaves and its stems contain many large "hyaline" cells, which consist
of cell walls only, and have no living contents when mature. The walls
of these cells have pores which facilitate the entrance of water, and
large quantities of it are thus taken in and retained by this moss. When
Sphagnum forms a dense mat, it tends to encourage the growth of certain
plants (e. g. some heath shrubs) and to discourage the growth of many of
the plants common in the region. Its presence thus tends to produce a
"bog flora". This is very striking where Sphagnum moss has formed a
thick continuous mat over a considerable area, but is less evident where
the lay of Sphagnum is thin and where it occurs in small patches
only.
Sphagnum flourishes in cool places which are very wet during the
growing season, and is most common on flat areas from which there is
little or no drainage. When it once gets a start in such a place it
encroaches rapidly on other vegetation. It forms extensive bogs with
very characteristic flora in the low lands of the Puget Sound region and
occasionally up to 3000 feet elevation, or even a little higher, in the
Cascade mountains. In the Olympics its occurrence is somewhat similar to
that in Mt. Rainier National Park.
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A-Surface view of portion of sphagnum leaf. x 300.
B-Reservoir cells from the epidermis of sphagnum branch. x 225.
g- green cells contain ing chlorophyll.
h - hoop-like bands.
p - pores or openings in the reservoir cells.
r - reservoir cell.
(Sketches from "Sphagnum as a Surgical Dressing" - Hotson.)
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Sphagnum moss is known to occur in Mt. Rainier National Park in the
following places: Berkley Park, Mystic Lake, Lake James, Windy Gap,
Mowich Lake, Eunice Lake, and Mountain Meadows. It probably occurs in
other places also, but it seems evident that the places listed show
representative habitats for Sphagnum in the Park.
In Berkley Park two small species of Sphagnum (S. teres and S.
robustum) are growing vigorously in small patches 5 to 15 feet in
diameter on a flat sedge meadow (elevation about 5700 feet) having an
area of about 2 acres. Some of these patches are flat on the meadow,
some have grown into low hummocks and some extend along the margins of
small rivulets. The rugged slopes of Berkley Park rise abruptly on the
east and west sides of this meadow and a small stream flows through it
to the north fork of the White River. This meadow is very cool and wet
since it lies immediately north of Mt. Rainier and Burroughs Mountain
where it receives much drainage water and comparatively little
sunshine.
The living Sphagnum has about 8 inches of dead Sphagnum under it,
indicating that it has flourished there for a good many years. Under the
dead Sphagnum are sedge peat and muck. The Sphagnum is everywhere
encroaching on the sedge meadow and if nature is allowed to take its
course it will probably in time form a continuous Sphagnum bog. At
present the only plant growing in the Sphagnum and not in the sedge
meadow is a small variety of swamp laurel (Kalmia microphylla). Plants
common in the living Sphagnum and also in the sedge meadow are two
heathers (Phyllodoce empetriformis and Cassiope Mertensiana), a small red
spiraea (S. densiflora), a huckleberry (Vaccinium sp), a small blue
gentian (Gentiana calycosa), a bright yellow Potentilla (P.
flabellifolia), a lousewart (Pedicularis surrecta), a pink fleabane
(Erigeron salsuginosus), a white flowered lovage (Ligusticum purpureum),
a marsh marigold (Caltha leptosepala), a small sedge (Carex sp), an
unidentified grass, an unidentified moss, and two unidentified toadstool
fungi. These patches of bog thus represent a very early stage in bog
succession, and the selective influence of the Sphagnum on their flora
extends to only one species.
The occurrence of Sphagnum at Mytic Lake is similar to that in
Berkley Park. It grows in patches on a swampy flat bordering the south
side of the lake which is on the north side of Mount Rainier at an
elevation of about 5300 feet. There are, however, the following
differences. (1) The individual patches are larger. (2) The total area
of Sphagnum on the flat is larger. (3) The layer of dead Sphagnum is a
little thicker. (4) There is a little more evidence of selective
influence of the Sphagnum on the plant society occurring in it. This
selective influence includes four species. The swamp laurel is common in
the Sphagnum and within a few feet of it, but not elsewhere in the
swampy meadow. The crowberry (Empetrum nigrum) is abundant in the
Sphagnum, but not outside of it in the immediate vicinity. When seen
elsewhere in this portion of the Park (e. g. on Tyee Peak) it was on
rocky, drier places and was bearing berries abundantly, though no
berries were found on it in the Sphagnum. A small fireweed (Epilobium
sp) was much more abundant in the Sphagnum than elsewhere. Very small
stunted specimens of the lodge pole pine (Pinus contorta) were found in
the Sphagnum, but this species was not found elsewhere in wet places,
though it was abundant on nearby higher places. It thus appears that the
Sphagnum succession on the wet sedge meadow has reached a little later
stage at Mystic Lake than it has in Berkley Park.
The Sphagnum in Mountain Meadows like that in the two cases just
described is an early stage of succession on a very wet sedge meadow.
These meadows are crossed by the old Grindstone Trail and lie between
Mowich Lake and Grindstone. The patches of Sphagnum occur in the margins
of the meadows. Two plants (Kalmia microphylla and Gaultheria humifusa)
occur in the Sphagnum but not elsewhere in the meadow, though the latter
is in the woods nearby.
The Sphagnum at Windy Gap is less than an acre in extent and is
fairly continuous. It occupies a rather poorly drained area at an
elevation of about 5700 feet. The occurrence of swamp laurel and
crowberry here in Sphagnum but not elsewhere in the immediate vicinity
is like that at Mystic Lake.
The Sphagnum at Lake James, Mowich Lake, Eunice Lake, and along the
trail between Mowich Lake and Mountain Meadows is small in amount. It
grows over soil, logs, and stumps and exercises no selective influence
on the plants growing with it. The Sphagnum in Berkley Park was studied
in August, 1934. In the other locations it was studied in 1922 and
preceding summers.
-oOo-
Dr. Geo. B. Rigg,
Department of Botany,
University of Washington.
Frog - his spring song resounds in park marshes now.