Morphological description and phylogenetic estimation of Favolus roseus (Polyporaceae): first documented records for the Indian mycobiota

During the course of macrofungal forays, we collected several wood-rotting fungi from three states in India: Bihar, Jharkhand, and Maharashtra. We identified some of these macrofungal collections as Favolus roseus Lloyd. A critical literature survey and taxonomic investigation established that this is the first report of F. roseus from India. We give a detailed morphological description, illustration, and molecular phylogeny of the species, along with taxonomic note and extended biogeographical distributional map.

Indo-European phylogenetics with R

The last twenty or so years have witnessed a dramatic increase in the use of computational methods for inferring linguistic phylogenies. Although the results of this research have been controversial, the methods themselves are an undeniable boon for historical and Indo-European linguistics, if for no other reason than that they allow the field to pursue questions that were previously intractable. After a review of the advantages and disadvantages of computational phylogenetic methods, I introduce the following methods of phylogenetic inference in R: maximum parsimony; distance-based methods (UPGMA and neighbor joining); and maximum likelihood estimation. I discuss the strengths and weaknesses of each of these methods and in addition explicate various measures associated with phylogenetic estimation, including homoplasy indices and bootstrapping. Phylogenetic inference is carried out on the Indo-European dataset compiled by Don Ringe and Ann Taylor, which includes phonological, morphological, and lexical characters.

Morphological evolution and molecular phylogenetics of the Merostachys clade (Poaceae: Bambusoideae: Bambuseae: Arthrostylidiinae) based on multi-locus plastid sequences

Merostachys is a Neotropical woody bamboo genus that occurs in the understory and along forest borders. Our taxonomic studies of its species and morphological analyses have allowed us to recognize morphological groups in the genus. Previous molecular analyses, which included relatively few species, supported Merostachys as monophyletic and sister to Actinocladum or Athroostachys. We here provide a phylogenetic estimation for Merostachys based on a broader taxon sampling and seven plastid markers (one coding: ndhF 3′ end; four intergenic spacers: rps16-trnQ, trnC-rpoB, trnD-trnT and trnT-trnL; and two introns: rpl16 and rps16). We aimed to test the monophyly of the genus, to verify its relationship with other genera of Arthrostylidiinae, mainly Athroostachys and Actinocladum, and to test whether the previously identified morphological groups were congruent with the molecular data. The monophyly of the genus was confirmed, as was its sister relationship with Athroostachys, although alternate hypothesis testing could not reject a sister relationship with Actinocladum. Two well-supported clades in Merostachys were recovered, one of which encompasses a polytomy. These clades did not exhibit consistent morphological synapomorphies and were not congruent with the morphological groups; however, floret surface (shiny vs. dull) was correlated with the two clades. The lack of resolution in Merostachys, as exemplified by the polytomy, can be attributed mainly to incomplete lineage sorting, suggesting a recent radiation in this group.

Joint Phylogenetic Estimation of Geographic Movements and Biome Shifts during the Global Diversification of Viburnum

Phylogeny, molecular sequences, fossils, biogeography, and biome occupancy are all lines of evidence that reflect the singular evolutionary history of a clade, but they are most often studied separately, by first inferring a fossil-dated molecular phylogeny, then mapping on ancestral ranges and biomes inferred from extant species. Here we jointly model the evolution of biogeographic ranges, biome affinities, and molecular sequences, while incorporating fossils to estimate a dated phylogeny for all of the 163 extant species of the woody plant clade Viburnum (Adoxaceae) that we currently recognize in our ongoing worldwide monographic treatment of the group. Our analyses indicate that while the major Viburnum lineages evolved in the Eocene, the majority of extant species originated since the Miocene. Viburnum radiated first in Asia, in warm, broad-leaved evergreen (lucidophyllous) forests. Within Asia, we infer several early shifts into more tropical forests, and multiple shifts into forests that experience prolonged freezing. From Asia, we infer two early movements into the New World. These two lineages probably first occupied warm temperate forests and adapted later to spreading cold climates. One of these lineages (Porphyrotinus) occupied cloud forests and moved south through the mountains of the Neotropics. Several other movements into North America took place more recently, facilitated by prior adaptations to freezing in the Old World. We also infer four disjunctions between Asia and Europe: the Tinus lineage is the oldest and probably occupied warm forests when it spread, whereas the other three were more recent and in cold-adapted lineages. These results variously contradict published accounts, especially the view that Viburnum radiated initially in cold forests and, accordingly, maintained vessel elements with scalariform perforations. We explored how the location and biome assignments of fossils affected our inference of ancestral areas and biome states. Our results are sensitive to, but not entirely dependent upon, the inclusion of fossil biome data. It will be critical to take advantage of all available lines of evidence to decipher events in the distant past. The joint estimation approach developed here provides cautious hope even when fossil evidence is limited. [Biogeography; biome; combined evidence; fossil pollen; phylogeny; Viburnum.]

Identifying model violations under the multispecies coalescent model using P2C2M.SNAPP

Phylogenetic estimation under the multispecies coalescent model (MSCM) assumes all incongruence among loci is caused by incomplete lineage sorting. Therefore, applying the MSCM to datasets that contain incongruence that is caused by other processes, such as gene flow, can lead to biased phylogeny estimates. To identify possible bias when using the MSCM, we present P2C2M.SNAPP. P2C2M.SNAPP is an R package that identifies model violations using posterior predictive simulation. P2C2M.SNAPP uses the posterior distribution of species trees output by the software package SNAPP to simulate posterior predictive datasets under the MSCM, and then uses summary statistics to compare either the empirical data or the posterior distribution to the posterior predictive distribution to identify model violations. In simulation testing, P2C2M.SNAPP correctly classified up to 83% of datasets (depending on the summary statistic used) as to whether or not they violated the MSCM model. P2C2M.SNAPP represents a user-friendly way for researchers to perform posterior predictive model checks when using the popular SNAPP phylogenetic estimation program. It is freely available as an R package, along with additional program details and tutorials.

Joint phylogenetic estimation of geographic movements and biome shifts during the global diversification of Viburnum

Phylogeny, fossils, biogeography, and biome occupancy provide evidence that reflects the singular evolutionary history of a clade. Despite the connections that bind them together, these lines of evidence are most often studied separately, by first inferring a fossil-dated molecular phylogeny, then mapping on ancestral ranges and biomes inferred from extant species. Here we jointly model the evolution of biogeographic ranges, biome affinities, and molecular sequences, incorporating fossils to estimate a dated phylogeny for all of the 163 extant species of the woody plant clade Viburnum (Adoxaceae) that we currently recognize. Our analyses indicate that while the major Viburnum lineages evolved in the Eocene, the majority of extant species originated since the Miocene. Viburnum radiated first in Asia, in warm, broad-leaved evergreen (lucidophyllous) forests. Within Asia we infer several early shifts into more tropical forests, and multiple shifts into forests that experience prolonged freezing. From Asia we infer two early movements into the New World. These two lineages probably first occupied warm temperate forests and adapted later to spreading cold climates. One of these lineages (Porphyrotinus) occupied cloud forests and moved south through the mountains of the Neotropics. Several other movements into North America took place more recently, facilitated by prior adaptations to freezing in the Old World. We also infer four disjunctions between Asia and Europe: the Tinus lineage is the oldest and probably occupied warm forests when it spread, while the other three were more recent and in cold-adapted lineages. These results variously contradict published accounts, especially the view that Viburnum radiated initially in cold forests and, accordingly, maintained vessel elements with scalariform perforations. We explored how the location and biome assignments of fossils affected our inference of ancestral areas and biome states. Our results are sensitive to, but not entirely dependent upon, the inclusion of fossil biome data. We argue that it will be critical to take advantage of all available lines of evidence to decipher events in the distant past, and the joint estimation approach developed here provides cautious hope even when fossil evidence is limited.

A novel species in Lactarius sect. Atroviridi from Indian Himalaya

Lactarius viridinigrellus, a milkcap with green-black matted-fibrillose azonate pileus is proposed here as a novel species under L. subg. Lactarius sect. Atroviridi from subalpine forests of Eastern Himalaya in India. Detailed morphological description, supporting illustrations and nrITS-based phylogenetic estimation are presented. Comparison with allied species is also given.