Lithophyte

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Nepenthes sp. Misool growing as a lithophyte in Raja Ampat, New Guinea RajaAmpatNep13.jpg
Nepenthes sp. Misool growing as a lithophyte in Raja Ampat, New Guinea

Lithophytes are plants that grow in or on rocks. They can be classified as either epilithic (or epipetric) or endolithic; epilithic lithophytes grow on the surfaces of rocks, while endolithic lithophytes grow in the crevices of rocks (and are also referred to as chasmophytes). [1] Lithophytes can also be classified as being either obligate or facultative. Obligate lithophytes grow solely on rocks, while facultative lithophytes will grow partially on a rock and on another substrate simultaneously. [2]

Contents

Nutrients

Lithophytes that grow on land feed off nutrients from rain water and nearby decaying plants, including their own dead tissue. It is easier for chasmophytes to acquire nutrients because they grow in fissures in rocks where soil or organic matter has accumulated.

For most lithophytes, nitrogen is only available through interactions with the atmosphere. The most readily available form of nitrogen in the atmosphere is the gaseous state of ammonia (NH3). Lithophytes consume atmospheric ammonia through a concentration gradient that allows the compound to traverse the plants' apoplast. Once free in the apoplast, gaseous ammonia is absorbed into metabolic cells by the enzyme glutamine synthetase. [3]

To be able to absorb the few nutrients available on rocks or rocky substrates efficiently, lithophytes have evolved certain adaptations. They possess decreased numbers of root hairs and larger root diameters in comparison to other plant species. To add to this nutrient uptake efficiency, lithophytic plants have increased their relationship with arbuscular mycorrhizal fungi and dark septate endophyte fungi. These two types of fungi live inter- and intracellularly with the roots of lithophytes and a wide variety of other plant species. They increase the uptake of nutrients and water and have been found in greater concentrations in lithophytes. [2]

Walls colonised as artificial cliffs by lithophytes

Asarina procumbens, the trailing snapdragon, colonising a crevice in a Berwickshire sandstone church wall - just as it would a siliceous inland cliff in its native Pyrenees Asarina procumbens cascading down wall beside Paxton church gatepost.jpg
Asarina procumbens , the trailing snapdragon, colonising a crevice in a Berwickshire sandstone church wall - just as it would a siliceous inland cliff in its native Pyrenees
Erysimum cheiri, the wallflower, growing out of the (brick) city wall of Louvain Erysimum cheiri02.jpg
Erysimum cheiri, the wallflower, growing out of the (brick) city wall of Louvain

Walls, and other exposed stonework, are colonised by plants in a similar way to the colonisation of cliffs and scree. These natural features are uncommon, especially in the lowlands, so walls are important for the conservation of plants which might otherwise be very isolated. Some wall plants even have 'wall' or 'muralis' as part of their common or scientific name such as wall-flower ( Erysimum cheiri ) or ivy-leaved toadflax ( Cymbalaria muralis ), which shows their long established relationship with these man-made structures.

English Heritage
Landscape Advice Note: Vegetation on Walls [4]

Examples

Examples of lithophytes include many orchids such as Dendrobium and Paphiopedilum , bromeliads such as Tillandsia , as well as many ferns, algae and liverworts. Lithophytes have also been found in many other plant families, such as, Liliaceae, Amaryllidaceae, Begoniaceae, Caprifoliaceae, Crassulaceae, Piperaceae and Selaginellaceae. [5]

Carnivorous plants

As nutrients tend to be rarely available to lithophytes or chasmophytes, many species of carnivorous plants can be viewed as being pre-adapted to life on rocks. By consuming prey, these plants can gather more nutrients than non-carnivorous lithophytes. [6] Examples include the pitcher plants Nepenthes campanulata and Heliamphora exappendiculata , many Pinguicula and several Utricularia species.

Tennyson poem inspired by lithophyte

In the year 1863, Alfred, Lord Tennyson was moved to write his short and pithy poem of metaphysical speculation Flower in the Crannied Wall upon contemplating an unnamed lithophyte growing out of the masonry of the wishing well at Waggoners Wells. [7]

National Trust plaque displayed on the wall of the wishing well at Waggoners Wells commemorating the composition of the poem "Flower in the Crannied Wall" National Trust wishing well sign, Waggoners Wells, Grayshott.jpg
National Trust plaque displayed on the wall of the wishing well at Waggoners Wells commemorating the composition of the poem "Flower in the Crannied Wall"

Flower in the crannied wall,
I pluck you out of the crannies,
I hold you here, root and all, in my hand,
Little flower—but if I could understand
What you are, root and all, and all in all,
I should know what God and man is. [8]

See also

Related Research Articles

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Canopy soils, also known as arboreal soils, exist in areas of the forest canopy where branches, crevices, or some other physical feature on a tree can accumulate organic matter, such as leaves or fine branches. Eventually, this organic matter weathers into some semblance of a soil, and can reach depths of 30 cm in some temperate rainforests. Epiphytes can take root in this thin soil, which accelerates the development of the soil by adding organic material and physically breaking up material with their root system. Common epiphytes in the canopy soils in temperate rainforests include mosses, ferns, and lichens. Epiphytes on trees in the temperate zone are often ubiquitous and can cover entire trees. Some host trees house up to 6.5 tons dry weight of epiphytic biomass, which can equate to more than 4x of its own foliar mass. This massive presence means their dynamics need to be better understood in order to fully understand forest dynamics. The nutrients that become stored within canopy soils can then be utilized by the epiphytes that grow in them, and even the tree that the canopy soil is accumulating in through the growth of canopy roots. This storage allows nutrients to be more closely cycled through an ecosystem, and prevents nutrients from being washed out of the system.

Seventeen elements or nutrients are essential for plant growth and reproduction. They are carbon (C), hydrogen (H), oxygen (O), nitrogen (N), phosphorus (P), potassium (K), sulfur (S), calcium (Ca), magnesium (Mg), iron (Fe), boron (B), manganese (Mn), copper (Cu), zinc (Zn), molybdenum (Mo), nickel (Ni) and chlorine (Cl). Nutrients required for plants to complete their life cycle are considered essential nutrients. Nutrients that enhance the growth of plants but are not necessary to complete the plant's life cycle are considered non-essential, although some of them, such as silicon (Si), have been shown to improve nutrent availability, hence the use of stinging nettle and horsetail macerations in Biodynamic agriculture. With the exception of carbon, hydrogen and oxygen, which are supplied by carbon dioxide and water, and nitrogen, provided through nitrogen fixation, the nutrients derive originally from the mineral component of the soil. The Law of the Minimum expresses that when the available form of a nutrient is not in enough proportion in the soil solution, then other nutrients cannot be taken up at an optimum rate by a plant. A particular nutrient ratio of the soil solution is thus mandatory for optimizing plant growth, a value which might differ from nutrient ratios calculated from plant composition.

References

  1. Christy, Arun; Thomas, Binu (June 26, 2020). "Phytodiversity of Chasmophytic Habitats at Olichuchattam Waterfalls, Kerala, India". Journal of Threatened Taxa. 12 (9): 16099–16109. doi:10.11609/jott.4554.12.9.16099-16109.
  2. 1 2 Muthukumar, Thangavelu; Chinnathambi, Marimuthu; Priyadharsini, Perumalsamy (July 11, 2016). "Root fungal associations in some non-orchidaceous vascular lithophytes". Acta Botanica Brasilica. 30 (3): 407–421. doi: 10.1590/0102-33062016abb0074 .
  3. Tozer, W.C.; Hackell, D.; Miers, D.B.; Silvester, W.B. (2005). "Extreme Isotopic Depletion of Nitrogen in New Zealand Lithophytes and Epiphytes; the Result of Diffusive Uptake of Atmospheric Ammonia?". Oecologia. 144 (4): 628–635. doi:10.1007/s00442-005-0098-0. PMID   15891815.
  4. English Heritage Landscape Advice Note: Vegetation on Walls https://www.english-heritage.org.uk/siteassets/home/learn/conservation/gardens-and-landscapes/lan_-_vegetation_on_walls.pdf Retrieved at 14.55 on Thursday 21/7/22
  5. Angalan, Norbert; Reyes, Gaudelia; Gomez, Romeo (2014). "Ture Measure of Lithophytes Diversity Across Microclimates". Journal of Natural Studies. 13.
  6. McPherson, S.R. (2010). Carnivorous Plants and their Habitats. Volume 1. Redfern Natural History Productions, Poole. pp. 176–180.
  7. Fiske, John (1899). Through Nature to God. Houghton, Mifflin.
  8. Poems of Alfred Lord Tennyson. Eugene Parsons (Introduction). New York: Thomas Y. Crowell Company, 1900.