Abstract

The phyllosphere microbiome is increasingly recognised as an influential component of plant physiology, yet it remains unclear whether stable host-microbe associations generally exist in the phyllosphere. Leptospermum scoparium (mānuka) is a tea tree indigenous to New Zealand, and honey derived from mānuka is widely known to possess unique antimicrobial properties. However, the host physiological traits associated with these antimicrobial properties vary widely, and the specific cause of such variation has eluded scientists despite decades of research. Notably, the mānuka phyllosphere microbiome remains uncharacterised, and its potential role in mediating host physiology has not been considered. Working within the prevailing core microbiome conceptual framework, we hypothesise that the phyllosphere microbiome of mānuka exhibits specific host association patterns congruent with those of a microbial community under host selective pressure (null hypothesis: the mānuka phyllosphere microbiome is recruited stochastically from the surrounding environment). To examine our hypothesis, we characterised the phyllosphere and associated soil microbiomes of five distinct and geographically distant mānuka populations across the North Island of New Zealand. We 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. Our results demonstrate the existence of a dominant and ubiquitous core microbiome in the phyllosphere of mānuka, supporting our hypothesis that phyllosphere microorganisms of mānuka exhibit specific host association and potentially mediate physiological traits of this nationally and culturally treasured indigenous plant. In addition, our results illustrate biogeographical patterns in mānuka phyllosphere microbiomes and offer insight into factors contributing to phyllosphere microbiome assembly.

Highlights

  • MethodsFive indigenous mānuka populations across the North Island of New Zealand were selected for study: Mohaka, Hawkes Bay (39 ̊01 S; 177 ̊08 E), Serpentine Lake, Waikato (37 ̊56 S, 175 ̊ 19 E), Mangatarere Valley, Wellington (40 ̊57 S; ̊26 E), Mamaku, Bay of Plenty (38 ̊02 S; ̊03 E), and North-eastern Kaimanawas, Taupo (39 ̊06 S; 176 ̊21 E) (S1 Fig)

  • Plants harbour distinct and dynamic microhabitats colonised by complex microbial communities known as plant microbiomes [1]

  • Inspired by the intriguing physiological characteristics of the mānuka tree and the increasingly recognised role of phyllosphere bacteria in plant physiology, we provide the first characterisation of the bacterial communities comprising the mānuka phyllosphere microbiome

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Summary

Methods

Five indigenous mānuka populations across the North Island of New Zealand were selected for study: Mohaka, Hawkes Bay (39 ̊01 S; 177 ̊08 E), Serpentine Lake, Waikato (37 ̊56 S, 175 ̊ 19 E), Mangatarere Valley, Wellington (40 ̊57 S; ̊26 E), Mamaku, Bay of Plenty (38 ̊02 S; ̊03 E), and North-eastern Kaimanawas, Taupo (39 ̊06 S; 176 ̊21 E) (S1 Fig). Steens Honey provided access to the sites in Mohaka and Mangatarere Valley. The East Taupō Lands Trust provided access to the north-eastern Kaimanawa site, Timberlands Ltd provided access to the Mamaku site. The Waipa District Council provided access to the site at Serpentine Lake. Straight-line distances between sites range from 65 km (Serpentine Lake and Mamaku) to 333 km (Serpentine Lake and Mangatarere Valley). Climate data for each site was retrieved from the National Climate Database (NIWA) (https://cliflo.niwa.co.nz/)

Results
Discussion
Conclusion

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