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Arbuscular mycorrhiza

Symbiotic penetrative association between a fungus and the roots of a vascular plant

  • 30 min read
  • 7 chapters
Arbuscular mycorrhiza seen under microscope. Flax root cortical cells containing paired arbuscules.
Msturmel · Public domain

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Through Symbiosis, Root and Vascular plant

Arbuscular mycorrhizae are formed by fungi in the subphylum Glomeromycotina and some fungi from the Mucoromycotina. These subphyla, along with the Mortierellomycotina, form the phylum Mucoromycota, a sister clade of the more well-known and diverse dikaryan fungi.

AM fungi help plants to capture nutrients such as phosphorus, sulfur, nitrogen and micronutrients from the soil. It is believed that the development of the arbuscular mycorrhizal symbiosis played a crucial role in the initial colonisation of land by plants and in the evolution of the vascular plants. It has been said that it is quicker to list the plants that do not form endomycorrhizae than those that do. This symbiosis is a highly evolved mutualistic relationship found between fungi and plants, the most prevalent plant symbiosis known, and AMF is found in 80% of vascular plant families in existence today. There are an estimates 110-quadrillion kilometers of AM fungal hyphae in Earth's topsoils, with around 40% located in wild grasslands. Currently, 90% of biodiversity hotspots of AM fungi are unprotected.

Previously this type of mycorrhizal associations were called 'Vesicular arbuscular mycorrhiza (VAM)', but since some members of these fungi do not produce any vesicles, such as the members of Gigasporaceae; the term has been changed to 'Arbuscular Mycorrhizae' to include them.

Advances in research on mycorrhizal physiology and ecology since the 1970s have led to a greater understanding of the multiple roles of AMF in the ecosystem. An example is the important contribution of the glue-like protein glomalin to soil structure (see below). This knowledge is applicable to human endeavors of ecosystem management, ecosystem restoration, and agriculture.

Evolution of mycorrhizal symbiosis

Paleobiology

Both paleobiological and molecular evidence indicate that AM is an ancient symbiosis that originated at least 460 million years ago. AM symbiosis is ubiquitous among land plants, which suggests that mycorrhizas were present in the early ancestors of extant land plants. This positive association with plants may have facilitated the development of land plants.

The Rhynie chert of the lower Devonian has yielded fossils of the earliest land plants in which AM fungi have been observed. The fossilized plants containing mycorrhizal fungi were preserved in silica.

The Early Devonian saw the development of terrestrial flora. Plants of the Rhynie chert from the Lower Devonian (400 m.yrs ago) were found to contain structures resembling vesicles and spores of present Glomus species. Colonized fossil roots have been observed in Aglaophyton major and Rhynia, which are ancient plants possessing characteristics of vascular plants and bryophytes with primitive protostelic rhizomes.

Intraradical mycelium was observed in root intracellular spaces, and arbuscules were observed in the layer thin wall cells similar to palisade parenchyma. The fossil arbuscules appear very similar to those of existing AMF. The cells containing arbuscules have thickened walls, which are also observed in extant colonized cells.

Mycorrhizas from the Miocene exhibit a vesicular morphology closely resembling that of present Glomerales. This conserved morphology may reflect the ready availability of nutrients provided by the plant hosts in both modern and Miocene mutualisms. However, it can be argued that the efficacy of signaling processes is likely to have evolved since the Miocene, and this can not be detected in the fossil record. A finetuning of the signaling processes would improve coordination and nutrient exchange between symbionts while increasing the fitness of both the fungi and the plant symbionts.

The nature of the relationship between plants and the ancestors of arbuscular mycorrhizal fungi is contentious. Two hypotheses are:

  • Mycorrhizal symbiosis evolved from a parasitic interaction that developed into a mutually beneficial relationship.
  • Mycorrhizal fungi developed from saprobic fungi that became endosymbiotic.

Both saprotrophs and biotrophs were found in the Rhynie Chert, but there is little evidence to support either hypothesis.

There is some fossil evidence that suggests that the parasitic fungi did not kill the host cells immediately upon invasion, although a response to the invasion was observed in the host cells. This response may have evolved into the chemical signaling processes required for symbiosis.

In both cases, the symbiotic plant-fungi interaction is thought to have evolved from a relationship in which the fungi was taking nutrients from the plant into a symbiotic relationship where the plant and fungi exchange nutrients.

The ancient plants did not have true roots. Strullu-Derrien and Strullu proposed the term 'Paramycorrhizae' for the mycorrhizae that infected the rhizome or shoot or thalli, and 'Eumycorrhizae' that infects true roots. These structures were reported in both sporophytes and gametophytes of the early land plants.

Molecular evidence

Increased interest in mycorrhizal symbiosis and the development of sophisticated molecular techniques has led to the rapid development of genetic evidence. Wang et al. (2010) investigated plant genes involved in communication with order Glomales fungal partners (DMI1, DMI3, IPD3). These three genes could be sequenced from all major clades of modern land plants, including liverworts, the most basal group, and phylogeny of the three genes proved to agree with then current land plant phylogenies. This implies that mycorrhizal genes must have been present in the common ancestor of land plants, and that they must have been vertically inherited since plants colonized land.

AM fungi and cyanobacteria symbiosis

It was revealed that AM fungi have the bacterial type core enzyme (ribonuclease III) of the sRNA processing mechanism, probably by the process of horizontal gene transfer from a cyanobacterial ancestor, and possibly related to symbiosis. This finding of a genetic fossil inside AM fungi raises the possibility of an intimate relationship between AM fungi and cyanobacterial ancestors. A similar Geosiphon–Nostoc symbiosis was previously reported.

Circadian clock evolution in AM fungi

Surprisingly, despite their long evolution as an underground partner of plant roots, whose environment is far from light or temperature fluctuation, AMF still have a conserved circadian clock whose fungal circadian oscillator (frq) is activated by the blue light, similar to the model circadian fungus Neurospora crassa. The proven conservation of a circadian clock and output genes in R. irregulare opens the door to the study of circadian clocks in the fungal partner of AM symbiosis. The same research characterized the AMF frq gene, which is the first frq gene identified outgroup of Dikarya, and suggests the frq gene evolution in the fungal kingdom is much older than previously thought.

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