Sea ice working group (SIP)

The sea ice is a crucial component of the polar climate system, and has an impact on albedo, heat and gas ex- change, primary productivity and car- bon export, atmospheric and ocean circulation, freshwater budget, ocean stratification, and deep water mass for- mation. It is therefore critical that it is correctly specified as a forcing or pre- dicted as a feedback in modeling stud- ies

Variabilidad de la Respuesta de las Células Dendríticas Estimuladas in vitro con Porphyromonas gingivalis y Aggregatibacter actinomycetemcomitans

ResumenLas células dendríticas son células presentadoras de antígeno capaces de inducir la activación y maduración de linfocitos T CD4+ vírgenes hacia un fenotipo efector especifico Th1 o Th2, dependiendo del tipo de antigeno presentado, las senales co-estimuladoras que expresan y el ambiente de citoquinas en el cual se produce la interaccion celula-celula. El objetivo del presente trabajo es analizar la respuesta de las celulas dendriticas estimuladas in vitro con distintas concentraciones de las bacterias periodontopatógenas Pg y Aa. En celulas dendriticas derivadas de monocitos de sangre periferica estimuladas con 101 a 109 bacterias/mL de Pg y Aa se evaluo la expresion del marcador de maduracion CD80 mediante citometria de flujo y de las citoquinas IL1β, IL2, IL5, IL6, IL10, IL12, IL13, IFNγ, TNFα y TNFβ mediante RT-PCR cuantitativa. Aa y Pg indujeron maduracion de las celulas dendriticas, detectandose significativamente mayor expresion de CD80 con la estimulacion de Aa, e indujeron predominantemente la expresion de citoquinas propias de una respuesta Th1. Dependiendo de la carga bacteriana, fueron detectados distintos umbrales de induccion de expresion de citoquinas. Aa indujo la sintesis de IL1β, IL12, IFNγ, TNFα y TNFβ a menor carga bacteriana que Pg. Tomados en conjunto, estos datos nos permiten especular un mayor potencial antigenico y proyectar una mayor capacidad patogenica durante la infeccion periodontal de Aa en comparación a Pg.AbstractDendritic cells are potent antigen-presenting cells able to prime naive T cells and polarize them towards a Th1 or Th2 response, depending on the type of the antigen presented to the TCR, the type of costimulatory signals, and the cytokine pattern in the environment. The aim of this work was to analyze the response of dendritic cells to in vitro stimulation with Pg and Aa. In monocyte-derived dendritic cells stimulated with 101 to 109 bacteria/mL of Pg or Aa were evaluated both the expression of the maturation marker CD80 by flow cytometry and the expression of the cytokines IL1β, IL2, IL5, IL6, IL10, IL12, IL13, IFNγ, TNFα and TNFβ by quantitative RT-PCR. Both Pg and Aa led to dendritic cell maturation, detecting higher CD80 expression upon Aa-stimulation, and induced a Th1 pattern of cytokine expression. Aa-stimulated dendritic cells expressed IL1β, IL12, IFNγ, TNFα and TNFβ mRNAs with lower bacterial charge than with Pg. Furthermore, our data indicated the existence of distinct thresholds for the induction of the different cytokines analyzed. Taken together, these data allow us to speculate a higher antigenic potential and higher pathogenic capacity of Aa than Pg during periodontal infections

Western Arctic Ocean temperature variability during the last 8000 years

Author Posting. © American Geophysical Union, 2011. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 38 (2011): L24602, doi:10.1029/2011GL049714.We reconstructed subsurface (∼200–400 m) ocean temperature and sea-ice cover in the Canada Basin, western Arctic Ocean from foraminiferal δ18O, ostracode Mg/Ca ratios, and dinocyst assemblages from two sediment core records covering the last 8000 years. Results show mean temperature varied from −1 to 0.5°C and −0.5 to 1.5°C at 203 and 369 m water depths, respectively. Centennial-scale warm periods in subsurface temperature records correspond to reductions in summer sea-ice cover inferred from dinocyst assemblages around 6.5 ka, 3.5 ka, 1.8 ka and during the 15th century Common Era. These changes may reflect centennial changes in the temperature and/or strength of inflowing Atlantic Layer water originating in the eastern Arctic Ocean. By comparison, the 0.5 to 0.7°C warm temperature anomaly identified in oceanographic records from the Atlantic Layer of the Canada Basin exceeded reconstructed Atlantic Layer temperatures for the last 1200 years by about 0.5°C.J.R.F., T.M.C., and R.C.T. thank support by USGS Global Change Program, G.S.D. thanks support from the USGS Global Change Program and the NSF Office of Polar Programs, A.d.V. thanks support by Fond québécois de la recherché sur la nature et les technologies (FQRNT) and the Ministere du Développement économique, innovation et exportation (MDEIE) of Quebec.2012-06-1

Micro-tomographic characterization of the root and canal system morphology of mandibular first premolars in a Chilean population

Indexación ScopusThis study aimed to analyze the root anatomy and root canal system morphology of mandibular first premolars in a Chilean population. 186 teeth were scanned using micro-computed tomography and reconstructed three-dimensionally. The root canal system morphology was classified using both Vertucci’s and Ahmed’s criteria. The radicular grooves were categorized using the ASUDAS system, and the presence of Tomes’ anomalous root was associated with Ahmed’s score. A single root canal was identified in 65.05% of teeth, being configuration type I according to Vertucci’s criteria and code 1MP1 according to Ahmed’s criteria. Radicular grooves were observed in 39.25% of teeth. The ASUDAS scores for radicular grooves were 60.75%, 13.98%, 12.36%, 10.22%, 2.15%, and 0.54%, from grade 0 to grade 5, respectively. The presence of Tomes’ anomalous root was identified only in teeth with multiple root canals, and it was more frequently associated with code 1MP1–2 of Ahmed’s criteria. The root canal system morphology of mandibular first premolars showed a wide range of anatomical variations in the Chilean population. Teeth with multiple root canals had a higher incidence of radicular grooves, which were closely related to more complex internal anatomy. Only teeth with multiple root canals presented Tomes’ anomalous root. © 2021, The Author(s).https://www-nature-com.recursosbiblioteca.unab.cl/articles/s41598-020-80046-

The Atlantic Ocean at the last glacial maximum: 1. Objective mapping of the GLAMAP sea-surface conditions

Recent efforts of the German paleoceanographic community have resulted in a unique data set of reconstructed sea-surface temperature for the Atlantic Ocean during the Last Glacial Maximum, plus estimates for the extents of glacial sea ice. Unlike prior attempts, the contributing research groups based their data on a common definition of the Last Glacial Maximum chronozone and used the same modern reference data for calibrating the different transfer techniques. Furthermore, the number of processed sediment cores was vastly increased. Thus the new data is a significant advance not only with respect to quality, but also to quantity. We integrate these new data and provide monthly data sets of global sea-surface temperature and ice cover, objectively interpolated onto a regular 1°x1° grid, suitable for forcing or validating numerical ocean and atmosphere models. This set is compared to an existing subjective interpolation of the same base data, in part by employing an ocean circulation model. For the latter purpose, we reconstruct sea surface salinity from the new temperature data and the available oxygen isotope measurements

Using the past to constrain the future: how the palaeorecord can improve estimates of global warming

Climate sensitivity is defined as the change in global mean equilibrium temperature after a doubling of atmospheric CO2 concentration and provides a simple measure of global warming. An early estimate of climate sensitivity, 1.5-4.5{\deg}C, has changed little subsequently, including the latest assessment by the Intergovernmental Panel on Climate Change. The persistence of such large uncertainties in this simple measure casts doubt on our understanding of the mechanisms of climate change and our ability to predict the response of the climate system to future perturbations. This has motivated continued attempts to constrain the range with climate data, alone or in conjunction with models. The majority of studies use data from the instrumental period (post-1850) but recent work has made use of information about the large climate changes experienced in the geological past. In this review, we first outline approaches that estimate climate sensitivity using instrumental climate observations and then summarise attempts to use the record of climate change on geological timescales. We examine the limitations of these studies and suggest ways in which the power of the palaeoclimate record could be better used to reduce uncertainties in our predictions of climate sensitivity.Comment: The final, definitive version of this paper has been published in Progress in Physical Geography, 31(5), 2007 by SAGE Publications Ltd, All rights reserved. \c{opyright} 2007 Edwards, Crucifix and Harriso