Species
Richness and Adaptation of Marine Fungi from Deep-Subseafloor Sediments
Fungi have developed unique adaptation that have allowed
them to colonize a range of habitats from terrestrial to marine, as well as
occupy a variety of extreme and non-extreme environmental niches. One such
environmental niche is deep subseafloor sediment where fungi have been
identified at depths from a few centimetres to 1740m below the sea floor (mbsf).
At these kinds of depths physical and chemical properties including; low nutrient
availability, salinity, hydrostatic and lithostatic pressure, amongst others, set
limitations on habitability. Past studies have shown, using molecular methods
and cultured isolates, that although fungi are present at great depths below
the seafloor, not a lot is known about their role in these ecosystems. This
study by Redou et al (2015) set out to determine the distribution of culturable
communities along a deep sea sediment core, characterize their ecophysiological
profiles and ability to withstand extreme abiotic conditions, and finally to
test their potential in the synthesis of bioactive compounds, that could have
some potential in biotechnological applications.
A sediment core was drilled 1927.5 mbsf during the
Integrated Ocean Drilling Programme (IODP) in the Canterbury Basin near New
Zealand. 11 subsamples that ranged from 4 – 1884 mbsf were analysed. They were
grown on 5 different media at varying temperatures, pressures and nutrient
availability to mimic the in situ conditions.
DNA was extracted from the isolates and various methods of PCR amplification
carried out for genetic identification and fingerprinting before phylogenetic
analyses were carried out using BLAST. Growth rates were measured and the
presence of genes involved in the production of secondary metabolites was
investigated.
10 of the 11 samples (91%) yielded culturable fungi. As expected
the overall phylogenetic diversity was relatively low when compared to organic
rich terrestrial and marine environments. The greatest diversity was found in
the upper sediment down to 37 mbsf with 25 species accounting for 92% of the
whole diversity within the entire fungal culture. At greater depths (137 – 1844
mbsf) there was only 8 species. The phyla Ascomycota dominated filamentous
fungal collection and Basidiomycota dominated the yeast collection which is
generally consistent with work done on deep sea sediments from the Central
Indian Basin. Hydrostatic pressure increased the growth rate of a number of
fungal isolates showing that some sort of adaptive mechanism is present to be
able to thrive under such conditions. Under temperature and salinity tests the
filamentous fungal isolates shifted from non-halophilic to halotolerant when
temperatures were increased from 25-35˚C and a few isolates of Fusarium and Penicillium shifted to complete halophily with increased
temperature. 96% of the isolates had at least one gene involved in secondary
metabolite synthesis. As genes for secondary metabolite can evolve rapidly the
authors state this may confirm their hypothesis that there is some level of
ecophysiological adaptation present.
This paper was laid out well and easy to follow. It mentioned
in the introduction that there could be biotechnological potential in these deep
see fungal isolates but further studies would be required to assess any
validity in this claim as I do not believe this study provides evidence to
support it. Overall I feel this paper could have gone into better detail when
discussing the results but it is a good foundation for future marine fungal
studies.
Paper reviewed:
Redou, V., Navarri, M.,
Meslet-Cladiere, L., Barbier, G., Burgaud, G. (2015). Species Richness And
Adaptation Of Marine Fungi From Deep-Subseafloor Sediments. Applied and
Environmental Microbiology 81(10) 3571-3583
Hi Dominic,
ReplyDeleteGreat post! Do the authors suggest why the phylogenetic diversity of the fungi decreased with depth?
Thanks,
Johanna
Hi Johanna,
ReplyDeleteThanks for the comment. Firstly the most important limiting factor suggested by the authors was the amount of accessible organic matter which decreased with depth. Temperature was important in that with every 1km below the sea floor the temperature increased at a rate of 30-50 degrees C. Finally salinity decreased slightly with increasing depth. So it was the expected abiotic and biotic factors that set distribution limits in this study. The authors of this paper almost seemed scare to draw too many conclusions from the findings of their study however and I felt that their discussion lacked this.
Hope this helps
Thanks
Dominic
Hi Dom,
ReplyDeleteFascinating read, am I right to think they they only sampled from one location in Canterbury Basin near New Zealand. I am curious how varied the fungi diversity would be throughout different water masses around the globe, and how geological activity may effect the fungi assemblage as I have only brushed over an interesting paper mentioning how Deep-Sea Hydrothermal Fungi Ecosystems posses quite a lot of species diversity. I will link that paper if your interested.
Looking forward to your next read!
Le Calvez, T., Burgaud, G., Mahe, S., Barbier, G. and Vandenkoornhuyse, P. (2009). Fungal Diversity in Deep-Sea Hydrothermal Ecosystems. Applied and Environmental Microbiology, 75(20), pp.6415-6421.