Orchids mycorrhiza (OM) are found in approximately 10% of the botanical diversity of earth and have unique and specialized mycorrhizal nutrient transfer interactions which define the fitness and diversity of the orchid family. Orchid mycorrhizal associations involve a plethora of unique nutrient transport systems, structures and phenomena which have only been observed in the family Orchidaceae. These interactions are formed between basidiomycete fungi and all Orchidaceae species. The way and degree to which different orchid species exploit these interactions varies. Orchid mycorrhizal interactions can range from wholly parasitic on the fungal partner, to a mutualistic interaction involving bidirectional nutrient transfer between the plant and mycorrhizal fungus. Orchid plants have an obligatory parasitic life stage at germination where all of their nutrients must be supplied by a fungus. After germination, the orchid mycorrhizal interactions will become specialized to utilize the carbon and nutrients available in the environment surrounding the interaction. These associations are often thought to be dictated by the plant.
Nutrient transfer interfaces and mechanisms At infection of an orchid by a mycorrhizal fungus both partners are altered considerably to allow for nutrient transfer and symbiosis. Nutrient transfer mechanisms and the symbiotic mycorrhizal peloton organs start to appear only shortly after infection around 20–36 hours after initial contact. The surrounding plant membrane essentially becomes rough
endoplasmic reticulum with high amounts of ribosomes and a plethora of transporter proteins, and aquaporins. Additionally there is evidence from electron microscopy that indicates the occurrence of exocytosis from the plant membrane. Pelotons are not permanent structures and are readily degraded and digested within 30 to 40 hours of their formation in orchid mycorrhiza. This happens in all endomycorrhizal associations but orchid plants readily digest fungal pelotons sooner after formation and more often than is seen in arbuscular mycorrhizal interactions. but orchid mycorrhizal nutrient transfer is less specific (but no less regulated) and there is often bidirectional flow of carbon between the fungus and plant, as well as flow of nitrogen and phosphorus from the fungus to plant. In around 400 species of plants there is no flow of carbon from plant and all of the nutrients of the plant are supplied by the fungus. Nitrogen is significantly easier to obtain than phosphorus and far more abundant, but mycorrhizal interactions still provide a significant benefit in the allocation of nitrogen. Bioavailable nitrogen as nitrate and ammonium are absorbed from the soil media into the extraradical
mycelium of the mycorrhizal fungi and assimilated into amino acids. Amino acids contain a significant amount of carbon as well and the transport of carbon may be the primary driving cause of the observed upregulation of the amino acid transporter genes, nonetheless nitrogen can still be transported to the plant via this pathway. The transport of inorganic nitrogen in the form of ammonium and the transport of organic nitrogen as amino acids most likely will occur simultaneously in the same species and or organism, depending on the abundance of different nitrogenous species in the soil, These reactions are often instigated and progressed by the activity of the mycorrhizal fungus, being part of the basidiomycete phyla, orchid associated fungi have an extensive metabolic arsenal with which to pull from, and are readily able to digest cellulose and lignin to obtain the carbon. Further more the fungi which mycoheterotrophically interact with orchid plants are often also found in mycorrhizal association with beech trees, and translocation of photosynthate from tree to fungus and then to orchid has been proposed, but a thorough study is still lacking. Once acquired by the fungus the carbon is either converted into sugars, trehalose being extremely common for most mycorrhizal fungus, amino acids, or simply assimilated into the fungal organism. The transfer of carbon from fungi to plant happens in one of two forms either as carbohydrates primarily trehalose, but glucose and sucrose may also be involved, or as an amino acids primarily as arginine but glycine and glutamine can also be transferred. Once the fate of the peloton is decided, and degradation and digestion are to occur, a secondary membrane forms around the fungal peloton which is essentially a large vacuole which will allow the isolated degradation of the peloton.
Micro-nutrient transfer Micro-nutrient transfer is thought, for the most part, to occur by passive transport across cellular membranes, both during absorption, from soil by fungi, and transfer from fungi to host plants. The upregulation of cation transporters is observed in orchid
D. officinale symbioses, suggesting fungi may assisted in the transfer of nutrients from fungi to plant. Cations, especially iron, are often bound tightly to organic and clay substrates keeping them out of reach of plants, fungi and bacteria, but compounds such as siderophores are often secreted into the soil by fungi and bacteria to aid in the acquisition of these cations. These compounds are released into the soil surrounding the hyphal web and strip iron from mineral compounds in the soil, the siderophore can then be reabsorbed into the fungal hyphae where the iron can be dissociated from the spiderohore and used. Haselwandter investigated the presence of siderophores in orchid associated mycorrhizal fungi within the genus
Rhizoctonia which utilize the siderophore basidiochrome as the major iron-chelating compound. Other vital nutrients may be transferred between mycorrhizal fungi and orchid plants via specialized methods, such as chelating molecules, but more research on this subject is needed. == Symbiont specificity ==