'' plant (left) and a leaf from a dysbiosis mutant plant (right) The aerial surface of a plant (stem, leaf, flower, fruit) is called the
phyllosphere and is considered comparatively nutrient poor when compared to the rhizosphere and endosphere. The environment in the phyllosphere is more dynamic than the rhizosphere and endosphere environments. Microbial colonizers are subjected to diurnal and seasonal fluctuations of heat, moisture, and radiation. In addition, these environmental elements affect plant physiology (such as photosynthesis, respiration, water uptake etc.) and indirectly influence microbiome composition. Interactions between plants and their associated microorganisms in many of these microbiomes can play pivotal roles in
host plant health, function, and evolution. The leaf surface, or
phyllosphere, harbours a microbiome comprising diverse communities of bacteria, fungi, algae, archaea, and viruses. Interactions between the host plant and phyllosphere bacteria have the potential to drive various aspects of host plant physiology. However, as of 2020 knowledge of these bacterial associations in the phyllosphere remains relatively modest, and there is a need to advance fundamental knowledge of phyllosphere microbiome dynamics. There can be up to 107 microbes per square centimetre present on the leaf surfaces of plants, and the bacterial population of the phyllosphere on a global scale is estimated to be 1026 cells. The population size of the fungal phyllosphere is likely to be smaller. Phyllosphere microbes from different plants appear to be somewhat similar at high levels of taxa, but at the lower levels taxa there remain significant differences. This indicates microorganisms may need finely tuned metabolic adjustment to survive in phyllosphere environment. Although there are similarities between the rhizosphere and soil microbial communities, very little similarity has been found between phyllosphere communities and microorganisms floating in open air (
aeroplankton). there is no consensus on the dominant driver of community assembly across phyllosphere microbiomes. For example, host-specific bacterial communities have been reported in the phyllosphere of co-occurring plant species, suggesting a dominant role of host selection. As a result, the processes that drive phyllosphere community assembly are not well understood but unlikely to be universal across plant species. However, the existing evidence does indicate that phyllosphere microbiomes exhibiting host-specific associations are more likely to interact with the host than those primarily recruited from the surrounding environment. The prevailing core microbiome concept is built on the notion that the persistence of a taxon across the spatiotemporal boundaries of an ecological niche is directly reflective of its functional importance within the niche it occupies; it therefore provides a framework for identifying functionally critical microorganisms that consistently associate with a host species. and even different species. defining core taxa
sensu stricto as those persistent across broad geographic distances within tissue- and species-specific host microbiomes, represents the most biologically and ecologically appropriate application of this conceptual framework.
Mānuka honey, produced from the
nectar of mānuka flowers, is known for its non-peroxide antibacterial properties. Microorganisms have been studied in the mānuka rhizosphere and endosphere. Earlier studies primarily focussed on fungi, and a 2016 study provided the first investigation of endophytic bacterial communities from three geographically and environmentally distinct mānuka populations using fingerprinting techniques and revealed tissue-specific core endomicrobiomes. on the left illustrates how the composition of OTUs in the mānuka phyllosphere and associated soil communities differed significantly. No core soil microbiome was detected.(B) The chart on the right shows how OTUs in phyllosphere and associated soil communities differed in relative abundances. A 2020 study identified a habitat-specific and relatively abundant core microbiome in the mānuka phyllosphere, which was persistent across all samples. In contrast, non-core phyllosphere microorganisms exhibited significant variation across individual host trees and populations that was strongly driven by environmental and spatial factors. The results demonstrated the existence of a dominant and ubiquitous core microbiome in the phyllosphere of mānuka. == Seed microbiome ==