- Key People:
- William Starling Sullivant
Bryophytes generate their nutrient materials through the photosynthetic activity of the chlorophyll pigments in the chloroplasts. In addition, most bryophytes absorb water and dissolved minerals over the surface of the gametophore. Water retention at the surface is assisted by the shape and overlapping of leaves, by an abundance of rhizoids, or by capillary spaces among these structures. Water loss through evaporation is rapid in most bryophytes.
A few bryophytes possess elaborate internal conducting systems (see below Form and function) that transfer water or manufactured nutrients through the gametophore, but most conduction is over the gametophore surface. In most mosses, water and nutrient transfer from the gametophore to the developing sporangium takes place along the seta and also via an internal conducting system. A protective cuticle covers the seta, reducing water loss. The calyptra that covers the developing sporangium prevents water loss in this fragile immature structure. In liverworts the sporangium remains close to the gametophore until it is mature; thus, a conducting system is not formed in the seta. In most hornworts there is also an internal conducting system within the developing horn-shaped sporangium. The internal movement of fluid in all parts of the bryophyte is extremely slow. Storage products include starch and lipids.
Ecology and habitats
Some bryophytes are unusually tolerant of extended periods of dryness and freezing, and, upon the return of moisture, they rapidly resume photosynthesis. The exact mechanism involved remains controversial.
Many bryophytes grow on soil or on the persistent remains of their own growth, as well as on living or decomposing material of other plants. Some grow on bare rock surfaces, and several are aquatic. The main requirements for growth appear to be a relatively stable substratum for attachment, a medium that retains moisture for extended periods, adequate sunlight, favourable temperature, and, for richest luxuriance, a nearly constantly humid atmosphere.
Unusual habitats include decomposing animal waste (many species in the moss family Splachnaceae), somewhat shaded cavern mouths (the liverwort Cyathodium and the mosses Mittenia and Schistostega), leaf surfaces (the moss Ephemeropsis and the liverwort genus Metzgeria and many species of the liverwort family Lejeuneaceae), salt pans (the liverwort Carrpos), bases of quartz pebbles (the moss Aschisma), and copper-rich substrata (the moss Scopelophila).
In humid temperate or subtropical climates, bryophytes often grow profusely, forming deep, soft carpets on forest floors and over rock surfaces, sheathing trunks and branches of trees and shrubs, and festooning branches. In broad-leaved forests of temperate areas, trees and boulders often harbour rich bryophyte stands, but it is near watercourses that bryophytes tend to reach their richest luxuriance and diversity.
In Arctic and Antarctic regions, bryophytes, especially mosses, form extensive cover, especially in wetlands, near watercourses, and in sites where snowmelt moisture is available for an extended part of the growing season. There they can dominate the vegetation cover and control the vegetation pattern and dynamics of associated plants. The same is true for alpine and subalpine environments in which many of the same species are involved.
Bryophytes, especially mosses, are important in nutrient cycling, in some cases making use of limited precipitation and airborne minerals that are thus made unavailable to the seed plant vegetation. Rapid evaporation from the moss mat is probably critical to some vegetation types by impeding moisture penetration to the root systems of seed plants and therefore indirectly controlling the vegetational composition of some forests.
Bryophytes are fundamental to the development of wetland habitats, especially of peatland. The moss genus Sphagnum leads to the development of waterlogged masses of highly acid peatland, in which decomposition is relatively slow. The formation of extensive bogs can control the hydrology of much of the surrounding landscape by behaving like a gigantic sponge that absorbs and holds vast quantities of water and influences the water table. Extension of this saturated living moss mat into living forest can drown the root systems of the forest trees, killing the forest and replacing it with bog. Peatland can also develop on calcareous terrain through the growth of other mosses, including species of the genera Drepanocladus and Calliergon. These mosses also build up a moss mat that, through organic accumulation of its own partially decomposed remains, alters the acidity of the site and makes it attractive to the formation of Sphagnum peatland.
Mosses colonize bare rock surfaces, leading ultimately to the initiation of soil formation. This in turn produces a substratum attractive to seed plant colonists that invade these mossy sites and, through their shading, eliminate the pioneer mosses but create a shaded habitat suitable for other bryophytes. These new colonists, in turn, are important in nutrient cycling in the developing forest vegetation.
