Partial rupture of the quadriceps muscle in a child

<p>Abstract</p> <p>Background</p> <p>The quadriceps femoris muscle ruptures usually occur in the middle-aged population. We present a 4-year-old patient with partial rupture of the quadriceps femoris muscle. To our knowledge, this is the youngest patient reported with a quadriceps femoris muscle rupture.</p> <p>Case Presentation</p> <p>A 4-year-old girl admitted to our clinic with left knee pain and limitation in knee movements. Her father reported that she felt pain while jumping on sofa. There was no direct trauma to thigh or knee. We located a palpable soft tissue swelling at distal anterolateral side of thigh. The history revealed that 10 days ago the patient was treated for upper tract respiratory infection with intramuscular Clindamycin for 7 days. When we consulted the patient with her previous doctor and nurse, we learnt that multiple daily injections might be injected to same side of left thigh. MRI showed a partial tear of vastus lateralis muscle matching with the injection sites. The patient treated with long leg half-casting for three weeks. Clinical examination and knee flexion had good results with conservative treatment.</p> <p>Conclusions</p> <p>Multiple intramuscular injections may contribute to damage muscles and make prone to tears with muscle contractions. Doctors and nurses must be cautious to inject from different parts of both thighs.</p

Identification of Novel Single Nucleotide Polymorphisms (SNPs) in Deer (Odocoileus spp.) Using the BovineSNP50 BeadChip

Single nucleotide polymorphisms (SNPs) are growing in popularity as a genetic marker for investigating evolutionary processes. A panel of SNPs is often developed by comparing large quantities of DNA sequence data across multiple individuals to identify polymorphic sites. For non-model species, this is particularly difficult, as performing the necessary large-scale genomic sequencing often exceeds the resources available for the project. In this study, we trial the Bovine SNP50 BeadChip developed in cattle (Bos taurus) for identifying polymorphic SNPs in cervids Odocoileus hemionus (mule deer and black-tailed deer) and O. virginianus (white-tailed deer) in the Pacific Northwest. We found that 38.7% of loci could be genotyped, of which 5% (n = 1068) were polymorphic. Of these 1068 polymorphic SNPs, a mixture of putatively neutral loci (n = 878) and loci under selection (n = 190) were identified with the FST-outlier method. A range of population genetic analyses were implemented using these SNPs and a panel of 10 microsatellite loci. The three types of deer could readily be distinguished with both the SNP and microsatellite datasets. This study demonstrates that commercially developed SNP chips are a viable means of SNP discovery for non-model organisms, even when used between very distantly related species (the Bovidae and Cervidae families diverged some 25.1−30.1 million years before present)

Inference of Ancestral Recombination Graphs Using ARGweaver

This chapter describes the usage of the program ARGweaver, which estimates the ancestral recombination graph for as many as about 100 genome sequences. The ancestral recombination graph is a detailed description of the coalescence and recombination events that define the relationships among the sampled sequences. This rich description is useful for a wide variety of population genetic analyses. We describe the preparation of data and major considerations for running ARGweaver, as well as the interpretation of results. We then demonstrate an analysis using the DARC (Duffy) gene as an example, and show how ARGweaver can be used to detect signatures of natural selection and Neandertal introgression, as well as to estimate the dates of mutation events. This chapter provides sufficient detail to get a new user up and running with this complex but powerful analysis tool

Late Quaternary drainage dynamics in northern Brazil based on the study of a large paleochannel from southwestern Marajó Island

Marajó Island shows an abundance of paleochannels easily mapped in its eastern portion, where vegetation consists mostly of savannas. SRTM data make possible to recognize paleochannels also in western Marajó, even considering the dense forest cover. A well preserved paleodrainage network from the adjacency of the town of Breves (southwestern Marajó Island) was investigated in this work combining remote sensing and sedimentological studies. The palimpsest drainage system consists of a large meander connected to narrower tributaries. Sedimentological studies revealed mostly sharp-based, fining upward sands for the channelized features, and interbedded muds and sands for floodplain areas. The sedimentary structures and facies successions are in perfect agreement with deposition in channelized and floodplain environments, as suggested by remote sensing mapping. The present study shows that this paleodrainage was abandoned during Late Pleistocene, slightly earlier than the Holocene paleochannel systems from the east part of the island. Integration of previous studies with the data available herein supports a tectonic origin, related to the opening of the Pará River along fault lineaments. This would explain the disappearance of large, north to northeastward migrating channel systems in southwestern Marajó Island, which were replaced by the much narrower, south to southeastward flowing modern channels.<br>A Ilha do Marajó mostra uma abundância de paleocanais que são facilmente mapeáveis em sua porção leste, onde a vegetação consiste principalmente em savanas. Dados SRTM possibilitam reconhecer paleocanais também na porção oeste do Marajó, mesmo considerando a cobertura vegetal de floresta densa. Uma rede de paleodrenagem bem preservada nas adjacências da cidade de Breves (sudoeste da Ilha do Marajó) foi investigada neste trabalho combinando-se sensoriamento remoto e estudos sedimentológicos. O sistema de drenagem palimpséstico consiste em um amplo meandro conectado a uma malha de tributários estreitos. Estudos sedimentológicos revelaram, principalmente, sucessões granodecrescentes ascendentes de base abrupta nas feições canalizadas, e intercalações de argilas e areias nas planícies de inundação. As estruturassedimentares e sucessões de fácies estão em perfeita concordância com deposição em ambientes canalizados e de planícies de inundação, como sugerido pelo mapeamento com sensoriamento remoto. O presente estudo mostra que a paleodrenagem foi abandonada no final do Pleistoceno, um pouco antes dos sistemas de paleocanais holocênicos da porção leste da ilha. A integração de estudos prévios com os dados disponíveis no presente trabalho suporta causa tectônica, particularmenterelacionada com a abertura do Rio Pará ao longo de falhastectônicas. Isto explicaria o desaparecimento de canais largos que migravam para norte-nordeste no sudoeste da Ilha do Marajó. Estes foram substituídos por outros canais mais estreitos de direção sul-sudeste que dominam na paisagem atual