More info for the terms:
cover,
fen,
minerotrophic,
organic soilsBeaked spikerush is an obligate wetland species [
28]. It occurs in many
types of alkaline wetlands including salt and brackish marshes, tidal
flats, alkaline seeps, bogs, stream margins, hot spring edges, and
swamps [
12,
13,
21,
23]. Beaked spikerush occurs near springs and seeps in
desert areas of the Southwest [
24,
39]. The depth to the water table
averages 2.2 inches (5.5 cm) for beaked spikerush sites in New York
[
29]. In Ohio, beaked spikerush forms solid mats in meadows where the
water table is at or above the soil surface [
8]. In northern Minnesota,
beaked spikerush occurs 4 inches (10 cm) above the water table in
spring-fen channels with peaty soil [
10,
11].
In a fen in New York, beaked spikerush occurs on wet minerotrophic
sites, nutrient-poor marl beds, and organic soils. (Marl beds are soils
formed from calcium carbonate precipitates.) Average soil pH for all
sites in New York was greater than 7.0 [
30]. In the Minnesota
spring-fen, groundwater discharge from calcareous till maintains a pH
greater than 7.0 and calcium concentrations between 20 and 45 milligrams
per liter [
10,
11]. Brotherson [
3] studied soil characteristics of a
common spikerush community in Utah in which beaked spikerush averaged
0.6 percent cover. Soil pH averaged 7.7, soluble salts averaged 4,003
parts per million, and organic matter averaged 32.7 percent. The
mineral fraction averaged 13 percent sand, 48 percent silt, and 39
percent clay [
3].
Beaked spikerush occurs from sea level in Atlantic, Gulf, and Pacific
coast salt marshes and tidal flats [
13,
16,
23] to nearly 9,000 feet
(2,700 m) elevation in Colorado [
6]. In Montana, it primarily occurs in
valley and foothill zones from 3,200 to 5,500 feet (915-1,675 m)
elevation [
22].