Publications

4547

Significance Symbiotic dinitrogen (N 2 )-fixing trees fulfill a critical function in tropical forests by bringing in new nitrogen, yet it remains unclear how they overcome constraints by highly weathered, nutrient-poor tropical soils. We advance forest biogeochemistry and microbial ecology with the discovery from field trials in Panama that fast-growing N 2 -fixing trees in tropical forests exhibit accelerated mineral weathering and distinctive soil metagenomes that improve their access to inorganic nutrients in nutrient-poor soils. Furthermore, we show that N 2 -fixing trees exert similar effects on non-N 2 –fixing trees nearby thus having previously overlooked community-wide effects on tropical forest nutrient cycling. These results offer insights into the role of N 2 -fixing trees and their associated microbiomes in safeguarding the function of tropical forests within the global biosphere.

Peptidoglycan (PG) is essential for bacterial survival and maintaining cell shape. The rod-shaped model bacterium Escherichia coli has a set of seven endopeptidases that remodel the PG during cell growth. The gamma proteobacterium Candidatus Thiosymbion oneisti is also rod-shaped and attaches to the cuticle of its nematode host by one pole. It widens and divides by longitudinal fission using the canonical proteins MreB and FtsZ. The PG layer of Ca. T. oneisti has an unusually high peptide cross-linkage of 67% but relatively short glycan chains with an average length of 12 disaccharides. Curiously, it has only two predicted endopeptidases, MepA and PBP4. Cellular localization of symbiont PBP4 by fluorescently labeled antibodies reveals its polar localization and its accumulation at the constriction sites, suggesting that PBP4 is involved in PG biosynthesis during septum formation. Isolated symbiont PBP4 protein shows a different selectivity for β-lactams compared to its homologue from E. coli. Bocillin-FL binding by PBP4 is activated by some β-lactams, suggesting the presence of an allosteric binding site. Overall, our data point to a role of PBP4 in PG cleavage during the longitudinal cell division and to a PG that might have been adapted to the symbiotic lifestyle.

Abstract BackgroundArchaea were originally discovered in extreme environments, and thrive in many extreme habitats including soda lakes with high pH and salinity. Characteristic and diverse archaeal community played a significant role in biogeochemical cycles; however, the archaeal community and their functions are still less-studied in the intricate sediment of soda lakes. ResultsIn this article, the archaeal community of the deep sediment (40-50 cm depth) of five artificially-separated ponds with a salinity range from 7.0% to 33.0% in a soda saline lake was systematically surveyed using culture-independent metagenomics combined with the next-generation sequencing of the archaeal 16S rRNA amplicons. Nine archaeal phyla were detected, which accounted for 2.2% to 35.73% of microbial community in the five deep sediments. Besides the well-known class Halobacteria, one novel archaeal order (Candidatus Natranaeroarchaeales) of the class Thermoplasmata was even more abundant than Halobacteria in some deep sediment samples. Of 69 dereplicated archaeal metagenome-assembled genomes (MAGs), 30 MAGs belonged to Ca. Natranaeroarchaeales. Different genera of the Ca. Natranaeroarchaeales preferred to inhabit in the different salinities, and the divergent halophilic adaptation strategies (salt-out or salt-in) suggested the fast evolution adaptation within this lineage. Most high-quality MAGs had the genes of Wood-Ljungdahl pathway, organic acid fermentation and sulfur respiration, suggesting the putative functions in carbon fixation and sulfur reduction. Interestingly, heterodisulfide reductase and F420-non-reducing hydrogenase complex HdrABC-MvhADG were widely distributed in Ca. Natranaeroarchaeales and may play the core roles in energy metabolism from hydrogen. The regeneration of CoM-S-S-CoB was coupled to succinate or 2-oxoglutarate production in Ca. Natranaeroarchaeales instead of methanogenesis in the close related Methanomassiliicoccales. It suggested that methyl-coenzyme M reductase in Methanomassiliicoccales may be laterally transferred from other methanogens. ConclusionA novel archaeal order Ca. Natranaeroarchaeales of Thermoplasmata was found by culture-independent approaches. This order was the most abundant archaeal lineage in the deep sediment of soda lakes, with the characteristic environmental adaptation and biogeochemical potentials in carbon fixation and sulfur reduction. The difference in fermentation products coupled to energy metabolism between methanogens and Ca. Natranaeroarchaeales provided additional insights into the origination of methanogenesis in Thermoplasmata from the energy metabolism perspective.