Genomic evidence for the widespread presence of GH45 cellulases among soil invertebrates.

Lignocellulose is a major component of vascular plant biomass. Its decomposition is crucial for the terrestrial carbon cycle. Microorganisms are considered primary decomposers, but evidence increases that some invertebrates may also decompose lignocellulose. We investigated the taxonomic distribution and evolutionary origins of GH45 hydrolases, important enzymes for the decomposition of cellulose and hemicellulose, in a collection of soil invertebrate genomes. We found that these genes are common in springtails and oribatid mites. Phylogenetic analysis revealed that cellulase genes were acquired early in the evolutionary history of these groups. Domain architectures and predicted 3D enzyme structures indicate that these cellulases are functional. Patterns of presence and absence of these genes across different lineages prompt further investigation into their evolutionary and ecological benefits. The ubiquity of cellulase genes suggests that soil invertebrates may play a role in lignocellulose decomposition, independently or in synergy with microorganisms. Understanding the ecological and evolutionary implications might be crucial for understanding soil food webs and the carbon cycle.

The MetaInvert soil invertebrate genome resource provides insights into below-ground biodiversity and evolution.

Soil invertebrates are among the least understood metazoans on Earth. Thus far, the lack of taxonomically broad and dense genomic resources has made it hard to thoroughly investigate their evolution and ecology. With MetaInvert we provide draft genome assemblies for 232 soil invertebrate species, representing 14 common groups and 94 families. We show that this data substantially extends the taxonomic scope of DNA- or RNA-based taxonomic identification. Moreover, we confirm that theories of genome evolution cannot be generalised across evolutionarily distinct invertebrate groups. The soil invertebrate genomes presented here will support the management of soil biodiversity through molecular monitoring of community composition and function, and the discovery of evolutionary adaptations to the challenges of soil conditions.

Pitfalls of the site-concordance factor (sCF) as measure of phylogenetic branch support.

Confidence measures of branch reliability play an important role in phylogenetics as these measures allow to identify trees or parts of a tree that are well supported by the data and thus adequate to serve as basis for evolutionary inference of biological systems. Unreliable branch relationships in phylogenetic analyses are of concern because of their potential to represent incorrect relationships of interest among more reliable branch relationships. The site-concordance factor implemented in the IQ-TREE package is a recently introduced heuristic solution to the problem of identifying unreliable branch relationships on the basis of quartets. We test the performance of the site-concordance measure with simple examples based on simulated data and designed to study its behaviour in branch support estimates related to different degrees of branch length heterogeneities among a ten sequence tree. Our results show that in particular in cases of relationships with heterogeneous branch lengths site-concordance measures may be misleading. We therefore argue that the maximum parsimony optimality criterion currently used by the site-concordance measure may sometimes be poorly suited to evaluate branch support and that the scores reported by the site-concordance factor should not be considered as reliable.