Anatomical traits and structural components of peduncle associated with lodging in Avena sativa L.

Received: May 14th, 2020 ; Accepted: June 19th, 2020 ; Published: January 5th, 2021 ; Correspondence: [email protected] dramatically reduces the yield of cereals and increases the difficulty of mechanical harvesting. Because it is a complex phenomenon, new cultivars with genetic resistance to lodging is a sustainable alternative in agricultural production systems. This resistance is associated with a combination of factors, such as stem thickness and stiffness, being closely linked to anatomical traits and structural carbohydrates present in the stem. In the present study we compared, under field conditions, eight contrasting oat cultivars in terms of lodging resistance. Our aim in this study was to investigate the association of anatomical traits and structural components of the peduncle with resistance to lodging, aiming to assist in the plant selection process. In addition, a second objective was to understand the genetic dissimilarity among oat cultivars according to the characters studied. Some characteristics for potential indirect selection were studied in this work and if correlated with lodging can be used to identify superior genotypes. From the anatomical point of view, the correlation obtained between the internal vascular bundle and the lodging resistance factor allowed us to confirm that this trait can be used in indirect selection to lodging resistance. The structural components of peduncle, in the two ways explored in the present study, comparison of mean and correlation, did not demonstrate the potential to be used exclusively as plant selection characters traits for lodging resistance. There is noticeable variability in oat cultivars for most stem traits

Seasonal drought limits tree species across the Neotropics

Within the tropics, the species richness of tree communities is strongly and positively associated with precipitation. Previous research has suggested that this macroecological pattern is driven by the negative effect of water-stress on the physiological processes of most tree species. This process implies that the range limits of taxa are defined by their ability to occur under dry conditions, and thus in terms of species distributions it predicts a nested pattern of taxa distribution from wet to dry areas. However, this ‘dry-tolerance’ hypothesis has yet to be adequately tested at large spatial and taxonomic scales. Here, using a dataset of 531 inventory plots of closed canopy forest distributed across the Western Neotropics we investigated how precipitation, evaluated both as mean annual precipitation and as the maximum climatological water deficit, influences the distribution of tropical tree species, genera and families. We find that the distributions of tree taxa are indeed nested along precipitation gradients in the western Neotropics. Taxa tolerant to seasonal drought are disproportionally widespread across the precipitation gradient, with most reaching even the wettest climates sampled; however, most taxa analysed are restricted to wet areas. Our results suggest that the ‘dry tolerance’ hypothesis has broad applicability in the world's most species-rich forests. In addition, the large number of species restricted to wetter conditions strongly indicates that an increased frequency of drought could severely threaten biodiversity in this region. Overall, this study establishes a baseline for exploring how tropical forest tree composition may change in response to current and future environmental changes in this region

Search for black holes and other new phenomena in high-multiplicity final states in proton-proton collisions at root s=13 TeV

Peer reviewe

Search for heavy resonances decaying into a vector boson and a Higgs boson in final states with charged leptons, neutrinos, and b quarks

Peer reviewe

Search for high-mass diphoton resonances in proton-proton collisions at 13 TeV and combination with 8 TeV search

Peer reviewe

Measurement of the mass difference between top quark and antiquark in pp collisions at root s=8 TeV

Peer reviewe

Search for leptophobic Z ' bosons decaying into four-lepton final states in proton-proton collisions at root s=8 TeV

Peer reviewe

Antropossolos em sítios arqueológicos de ambiente cárstico no norte de Minas Gerais

A ocupação e a dispersão territorial dos primeiros colonizadores da América do Sul, sobretudo do Brasil, são ainda pouco conhecidas e exigem esforço interdisciplinar contínuo, envolvendo a antropologia, arqueologia e pedologia. Sob abrigos naturais de rochas calcárias, populações pré-colombianas viveram por milhares de anos, aportando e removendo matérias de naturezas e procedências distintas, desenvolvendo solos antropogênicos muito peculiares, sobre os quais ainda não se têm estudos pedológicos. Para melhor conhecer os solos, procedeu-se à caracterização física, química e mineralógica de solos de dois abrigos calcários, Lapas do Boquete e do Malhador, situados no Parque Nacional Cavernas do Peruaçu, norte de Minas Gerais, tido como uma das mais importantes regiões arqueológicas do país. As amostras foram submetidas à caracterização física, química e mineralógica, ao ataque total, à determinação do carbono orgânico total, além de fracionamento das formas inorgânicas de fósforo. As características químicas dos solos estudados estão condizentes com a natureza calcária da rocha local, apresentando valores de pH elevados (> 7,7). O complexo de troca catiônica é praticamente todo preenchido pelas bases trocáveis, principalmente Ca e Mg, alcançando valores de V de 100 %. Os teores de P-extraível (Mehlich-1) encontrados foram elevados, de 131 a 749 mg dm-3. Nos solos analisados, predominou a fração areia, sendo todas as camadas enquadradas na classe textural franco. É marcante a presença de óxidos com atração magnética em todas as frações, especialmente na fração areia, associada principalmente a camadas carbonizadas. Os solos apresentaram predomínio, em sua matriz, de minerais silicatados do tipo 1:1 (caulinita), associados a minerais do tipo 2:1, basicamente illita. De acordo com os resultados encontrados, os solos estudados apresentaram gênese policíclica, marcada por pronunciada alternância climática associada a distintos períodos de ocupação antrópica, que resultaram na formação de camadas aparentemente sem relação pedogenética entre si