plants in a grassland Some relatively fast-growing herbaceous plants (especially annuals) are
pioneers, or early-successional species. Others form the main vegetation of many stable habitats, occurring for example in the ground layer of
forests, or in naturally open
habitats such as
meadow,
salt marsh or
desert. Some habitats, like
grasslands and
prairies and
savannas, are dominated by herbaceous plants along with aquatic environments like
ponds, streams and
lakes. The age of some herbaceous perennial plants can be determined by
herbchronology, the analysis of annual growth rings in the secondary root
xylem. Herbaceous plants do not produce perennializing above-ground structures using
lignin, which is a complex phenolic polymer deposited in the secondary cell wall of all vascular plants. The development of lignin during vascular plant evolution provided mechanical strength, rigidity, and hydrophobicity to secondary cell walls creating a woody stem, allowing plants to grow tall and transport water and nutrients over longer distances within the plant body. Since most woody plants are perennials with a longer life cycle because it takes more time and more resources (nutrients and water) to produce persistently living lignified woody stems, they are not as able to colonize open and dry ground as rapidly as herbs. The surface of herbs is a catalyst for dew, which in arid climates and seasons is the main type of precipitation and is necessary for the survival of vegetation, i.e. in arid areas, herbaceous plants are a generator of precipitation and the basis of an ecosystem. Most of the water vapor that turns into dew comes from the air, not the soil or clouds. The taller the herb (
surface area is the main factor though), the more dew it produces, so a short cut of the herbs necessitates watering. For example, if you frequently and shortly cut the grass without watering in an arid zone, then
desertification occurs. ==Types of herbaceous plants==