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1. A pangenome analysis reveals the center of origin and evolutionary history of Phytophthora infestans and 1c clade species

   https://doi.org/10.1371/journal.pone.0314509  

   Coomber, Allison L; Saville, Amanda C; Carbone, Ignazio; Martin, Michael; Bieker, Vanessa C; Ristaino, Jean Beagle (January 2025, PLOS ONE)

   Blair, Jaime E (Ed.)

   We examined the evolutionary history ofPhytophthora infestansand its close relatives in the 1c clade. We used whole genome sequence data from 69 isolates ofPhytophthoraspecies in the 1c clade and conducted a range of genomic analyses including nucleotide diversity evaluation, maximum likelihood trees, network assessment, time to most recent common ancestor and migration analysis. We consistently identified distinct and later divergence of the two MexicanPhytophthoraspecies,P.mirabilisandP.ipomoeae, fromP.infestansand other 1c clade species.Phytophthora infestansexhibited more recent divergence from other 1c clade species ofPhytophthorafrom South America,P.andinaandP.betacei. Speciation in the 1c clade and evolution ofP.infestansoccurred in the Andes.P.andina–P.betacei–P.infestansformed a species complex with indistinct species boundaries, hybridizations between the species, and short times to common ancestry. Furthermore, the distinction between modern Mexican and South AmericanP.infestansproved less discrete, suggesting gene flow between populations over time. Admixture analysis indicated a complex relationship among these populations, hinting at potential gene flow across these regions. HistoricP.infestans, collected from 1845–1889, were the first to diverge from all otherP.infestanspopulations. Modern South American populations diverged next followed by Mexican populations which showed later ancestry. Both populations were derived from historicP.infestans. Based on the time of divergence ofP.infestansfrom its closest relatives,P.andinaandP.betaceiin the Andean region, we consider the Andes to be the center of origin ofP.infestans, with modern globalization contributing to admixture betweenP.infestanspopulations today from Mexico, the Andes and Europe. 

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2. Bounding p-Brauer characters in finite groups with two conjugacy classes of p-elements

   https://doi.org/10.1007/s11856-024-2613-1  

   Hung, Nguyen Ngoc; Sambale, Benjamin; Tiep, Pham Huu (September 2024, Israel Journal of Mathematics)

   Abstract Letk(B₀) andl(B₀) respectively denote the number of ordinary andp-Brauer irreducible characters in the principal blockB₀of a finite groupG. We prove that, ifk(B₀)−l(B₀) = 1, thenl(B₀) ≥p− 1 or elsep= 11 andl(B₀) = 9. This follows from a more general result that for every finite groupGin which all non-trivialp-elements are conjugate,l(B₀) ≥p− 1 or elsep= 11 and$$G/{{\bf{O}}_{{p^\prime }}}(G) \cong C_{11}^2\, \rtimes\,{\rm{SL}}(2,5)$$ $G/O_{p^{\prime }}\left(G\right)\cong C_{11}^2⋊\text{SL}(2,5)$. These results are useful in the study of principal blocks with few characters. We propose that, in every finite groupGof order divisible byp, the number of irreducible Brauer characters in the principalp-block ofGis always at least$$2\sqrt {p - 1} + 1 - {k_p}(G)$$ $2\sqrt{p-1}+1-k_p\left(G\right)$, wherek_p(G) is the number of conjugacy classes ofp-elements ofG. This indeed is a consequence of the celebrated Alperin weight conjecture and known results on bounding the number ofp-regular classes in finite groups. 

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3. Paludicola gen. nov. and Revision of the Species Formerly in Batrachospermum Section  Turfosa (Batrachospermales, Rhodophyta)

   https://doi.org/10.1111/jpy.13001  

   Vis, Morgan L.; Lee, Janina; Eloranta, Pertti; Chapuis, Iara S.; Lam, Daryl W.; Necchi, Jr., Orlando; Oliveira, ed., M. C. (May 2020, Journal of Phycology)

   Since the first phylogenetic study of the order Batrachospermales,Batrachospermumwas shown to be paraphyletic. Subsequently, sections of the genus have been methodically investigated usingDNAsequences and morphology in order to propose new genera and delineate species.BatrachospermumsectionTurfosais the last section with multiple species yet to be examined. New sequence data of specimens from Europe and the United States were combined with the sparse sequence data already available. Phylogenetic analyses usingrbcL andCOI‐5P sequences showed this section to be a well‐supported clade, distinct fromBatrachospermumsectionBatrachospermumand its segregate genera. Section Turfosais raised to the generic rank asPaludicolagen. nov. Substantial genetic variation within the genus was discovered and 12 species are recognized based onDNAsequence data as well as morphological characters and geographic distribution. The following morphological characters were applied to distinguish species: branching pattern (pseudodichotomous or irregular), whorl size (reduced or well developed), primary fascicles (curved or straight), spermatangia origin (primary or secondary fascicles), and carposporophyte arrangement (loose or dense). Previously published species were transferred to the new genus:P. turfosa,P. keratophyta,P. orthosticha,P. phangiae,andP. periploca. Seven new species are proposed as follows:P. groenbladiifrom Europe;P. communis,P. johnhallii, andP. leafensisfrom North America; andP. aquanigra,P. diamantinensis, andP. turfosiformisfrom Brazil. In addition, three unsequenced species in the section,P. bakarensis,P. gombakensis, andP. tapirensis, were transferred to the new genus. 

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4. Relationship between local-scale topography and vegetation on the invasive C ₄ perennial bunchgrass buffelgrass ( Pennisetum ciliare ) size and reproduction

   https://doi.org/10.1017/inp.2023.9  

   Hovanes, Katherine A.; Lien, Aaron M.; Baldwin, Elizabeth; Li, Yue M.; Franklin, Kim; Gornish, Elise S. (March 2023, Invasive Plant Science and Management)

   Abstract Buffelgrass [Pennisetum ciliare(L.) Link] is an invasive C₄perennial bunchgrass that is a threat to biodiversity in aridlands in the Americas and Australia. Topography influencesP. ciliareoccurrence at large spatial scales, but further investigation into the relationship between local-scale topography andP. ciliaregrowth and reproduction would be beneficial. Further, density-dependent effects onP. ciliaregrowth and reproduction have been demonstrated in greenhouse experiments, but the extent to which density dependence influencesP. ciliarein natural populations warrants further investigation. Here we present a study on the relationships between local-scale topography (aspect and slope gradient) and vegetation characteristics (shrub cover,P. ciliarecover, andP. ciliaredensity) and their interactions on individualP. ciliareplant size and reproduction. We measured slope gradient, aspect, shrub cover,P. ciliarecover,P. ciliaredensity, and the total number of live culms and reproductive culms of 10P. ciliareplants in 33 4 by 4 m plots located in 11 transects at the Desert Laboratory at Tumamoc Hill, Tucson, AZ, USA. We modeled the relationships at the local scale of (1)P. ciliarecover and density with aspect and slope gradient and (2)P. ciliaresize and reproduction with abiotic (slope gradient and aspect) and biotic (P. ciliarecover and density and native shrub and cacti cover) characteristics. Aspect and slope gradient were poor predictors ofP. ciliarecover and density in already invaded sites at the scale of our plots. However, aspect had a significant relationship withP. ciliareplant size and reproduction.Pennisetum ciliareplants on south-facing aspects were larger and produced more reproductive culms than plants on other aspects. Further, we found no relationship betweenP. ciliaredensity andP. ciliareplant size and reproduction. Shrub cover was positively correlated withP. ciliarereproduction. South-facing aspects are likely most vulnerable to fast spread and infilling by newP. ciliareintroductions. 

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5. Enhancing Tsunami Warning Using P Wave Coda

   https://doi.org/10.1029/2019JB018221  

   Lay, Thorne; Liu, Chengli; Kanamori, Hiroo (October 2019, Journal of Geophysical Research: Solid Earth)

   Abstract Most large tsunamis are generated by earthquakes on offshore plate boundary megathrusts. The primary factors influencing tsunami excitation are the seismic moment, faulting geometry, and depth of the faulting. Efforts to provide rapid tsunami warning have emphasized seismic and geodetic methods for quickly determining the event size and faulting geometry. It remains difficult to evaluate the updip extent of rupture, which has significant impact on tsunami excitation. TeleseismicPwaves can constrain this issue; slip under deep water generates strongpwPwater reverberations that persist as ringingP_codaafter the directPphases from the faulting have arrived. Event‐averagedP_coda/Pamplitude measures at large epicentral distances (>80°), tuned to the dominant periods of deep waterpwP(~12–15 s), correlate well with independent models of whether slip extends to near the trench or not. Data at closer ranges (30° to 80°) reduce the time lag needed for inferring the updip extent of rupture to <15 min. Arrival ofPPandPPPphases contaminates closer distanceP_codameasures, but this can be suppressed by azimuthal or distance binning of the measures. Narrowband spectral ratio measures and differential magnitude measures ofP_codaand directP(m_B) perform comparably to broader band root‐mean‐square (RMS) measures.P_coda/Plevels for large nonmegathrust events are also documented. Rapid measurement ofP_coda/Pmetrics after a large earthquake can supplement quick moment tensor determinations to enhance tsunami warnings; observation of largeP_codalevels indicates that shallow submarine rupture occurred and larger than typical tsunami (for givenM_W) can be expected. 

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