14 results on '"Myhre, CL"'
Search Results
2. Measurements of δ$^{13}$C in CH$_{4}$ and using particle dispersion modeling to characterize sources of Arctic methane within an air mass
- Author
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France, JL, Cain, M, Fisher, RE, Lowry, D, Allen, G, O'Shea, SJ, Illingworth, S, Pyle, J, Warwick, N, Jones, BT, Gallagher, MW, Bower, K, Le Breton, M, Percival, C, Muller, J, Welpott, A, Bauguitte, S, George, C, Hayman, GD, Manning, AJ, Myhre, CL, Lanoisellé, M, and Nisbet, EG
- Subjects
Arctic ,13. Climate action ,methane ,d13C ,wetlands - Abstract
A stratified air mass enriched in methane (CH$_{4}$) was sampled at ~600 m to ~2000 m altitude, between the north coast of Norway and Svalbard as part of the Methane in the Arctic: Measurements and Modelling campaign on board the UK's BAe-146-301 Atmospheric Research Aircraft. The approach used here, which combines interpretation of multiple tracers with transport modeling, enables better understanding of the emission sources that contribute to the background mixing ratios of CH$_{4}$ in the Arctic. Importantly, it allows constraints to be placed on the location and isotopic bulk signature of the emission source(s). Measurements of δ$^{13}$C in CH$_{4}$ in whole air samples taken while traversing the air mass identified that the source(s) had a strongly depleted bulk δ$^{13}$C CH$_{4}$isotopic signature of −70 (±2.1)‰. Combined Numerical Atmospheric-dispersion Modeling Environment and inventory analysis indicates that the air mass was recently in the planetary boundary layer over northwest Russia and the Barents Sea, with the likely dominant source of methane being from wetlands in that region.
3. Constraints on oceanic methane emissions west of Svalbard from atmospheric in situ measurements and Lagrangian transport modeling
- Author
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Pisso, I, Myhre, CL, Platt, SM, Eckhardt, S, Hermansen, O, Schmidbauer, N, Mienert, J, Vadakkepuliyambatta, S, Bauguitte, S, Pitt, J, Allen, G, Bower, KN, O'Shea, S, Gallagher, MW, Percival, CJ, Pyle, J, Cain, M, and Stohl, A
- Subjects
13 Climate Action ,13. Climate action - Abstract
Methane stored in seabed reservoirs such as methane hydrates can reach the atmosphere in the form of bubbles or dissolved in water. Hydrates could destabilize with rising temperature further increasing greenhouse gas emissions in a warming climate. To assess the impact of oceanic emissions from the area west of Svalbard, where methane hydrates are abundant, we used measurements collected with a research aircraft (Facility for Airborne Atmospheric Measurements) and a ship (Helmer Hansen) during the Summer 2014 and for Zeppelin Observatory for the full year. We present a model-supported analysis of the atmospheric CH$_{4}$mixing ratios measured by the different platforms. To address uncertainty about where CH$_{4}$ emissions actually occur, we explored three scenarios: areas with known seeps, a hydrate stability model, and an ocean depth criterion. We then used a budget analysis and a Lagrangian particle dispersion model to compare measurements taken upwind and downwind of the potential CH$_{4}$ emission areas. We found small differences between the CH$_{4}$ mixing ratios measured upwind and downwind of the potential emission areas during the campaign. By taking into account measurement and sampling uncertainties and by determining the sensitivity of the measured mixing ratios to potential oceanic emissions, we provide upper limits for the CH$_{4}$ fluxes. The CH$_{4}$ flux during the campaign was small, with an upper limit of 2.5 nmol m$^{-2}$ s$^{-1}$ in the stability model scenario. The Zeppelin Observatory data for 2014 suggest CH$_{4}$ fluxes from the Svalbard continental platform below 0.2 Tg yr$^{-1}$. All estimates are in the lower range of values previously reported., MOCA—Methane Emissions from the Arctic OCean to the Atmosphere: Present and Future Climate Effects is funded by the Research Council of Norway, grant 225814. CAGE—Centre for Arctic Gas Hydrate, Environment and Climate research work was supported by the Research Council of Norway through its Centres of Excellence funding scheme grant 223259. eSTICC—eScience Tools for Investigating Climate Change in northern high latitudes is supported by Nordforsk as Nordic Center of Excellence grant 57001. NERC grants NE/I029293/1 (PI. H. Coe) and NE/I02916/1 (PI J. Pyle) and Methane & Other Greenhouse Gases in the Arctic—Measurements, Process Studies and Modelling (MAMM). The ERC through the ACCI project, project number 267760. The biogenic methane emission data from the LPX-Bern v1.2 model were provided by Renato Spahni. The methane emission data from the GAINS model were provided by IIASA. GFED data are available from http://www.globalfiredata.org/index.html. Airborne data were obtained using the BAe-146-301 Atmospheric Research Aircraft (ARA) flown by Directflight Ltd. and managed by the Facility for Airborne Atmospheric Measurements (FAAM), which is a joint entity of the Natural Environment Research Council (NERC) and the Met Office. Zeppelin and Helmer Hansen atmospheric measurement data are archived in EBAS (http://ebas.nilu.no/) for long-term preservation, access and use. All Zeppelin data for 2014: http://ebas.nilu.no/DataSets.aspx?stations=NO0042G&fromDate=2014-01-01&toDate=2014-12-31. All atmospheric data from RV Helmer Hanssen: http://ebas.nilu.no/DataSets.aspx?stations=NO1000R&fromDate=2014-01-01&toDate=2014-12-31 (password is required until the end of 2017).
4. The fingerprint of the summer 2018 drought in Europe on ground-based atmospheric CO 2 measurements.
- Author
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Ramonet M, Ciais P, Apadula F, Bartyzel J, Bastos A, Bergamaschi P, Blanc PE, Brunner D, Caracciolo di Torchiarolo L, Calzolari F, Chen H, Chmura L, Colomb A, Conil S, Cristofanelli P, Cuevas E, Curcoll R, Delmotte M, di Sarra A, Emmenegger L, Forster G, Frumau A, Gerbig C, Gheusi F, Hammer S, Haszpra L, Hatakka J, Hazan L, Heliasz M, Henne S, Hensen A, Hermansen O, Keronen P, Kivi R, Komínková K, Kubistin D, Laurent O, Laurila T, Lavric JV, Lehner I, Lehtinen KEJ, Leskinen A, Leuenberger M, Levin I, Lindauer M, Lopez M, Myhre CL, Mammarella I, Manca G, Manning A, Marek MV, Marklund P, Martin D, Meinhardt F, Mihalopoulos N, Mölder M, Morgui JA, Necki J, O'Doherty S, O'Dowd C, Ottosson M, Philippon C, Piacentino S, Pichon JM, Plass-Duelmer C, Resovsky A, Rivier L, Rodó X, Sha MK, Scheeren HA, Sferlazzo D, Spain TG, Stanley KM, Steinbacher M, Trisolino P, Vermeulen A, Vítková G, Weyrauch D, Xueref-Remy I, Yala K, and Yver Kwok C
- Subjects
- Europe, Atmosphere analysis, Carbon Cycle, Carbon Dioxide analysis, Droughts, Ecosystem
- Abstract
During the summer of 2018, a widespread drought developed over Northern and Central Europe. The increase in temperature and the reduction of soil moisture have influenced carbon dioxide (CO
2 ) exchange between the atmosphere and terrestrial ecosystems in various ways, such as a reduction of photosynthesis, changes in ecosystem respiration, or allowing more frequent fires. In this study, we characterize the resulting perturbation of the atmospheric CO2 seasonal cycles. 2018 has a good coverage of European regions affected by drought, allowing the investigation of how ecosystem flux anomalies impacted spatial CO2 gradients between stations. This density of stations is unprecedented compared to previous drought events in 2003 and 2015, particularly thanks to the deployment of the Integrated Carbon Observation System (ICOS) network of atmospheric greenhouse gas monitoring stations in recent years. Seasonal CO2 cycles from 48 European stations were available for 2017 and 2018. Earlier data were retrieved for comparison from international databases or national networks. Here, we show that the usual summer minimum in CO2 due to the surface carbon uptake was reduced by 1.4 ppm in 2018 for the 10 stations located in the area most affected by the temperature anomaly, mostly in Northern Europe. Notwithstanding, the CO2 transition phases before and after July were slower in 2018 compared to 2017, suggesting an extension of the growing season, with either continued CO2 uptake by photosynthesis and/or a reduction in respiration driven by the depletion of substrate for respiration inherited from the previous months due to the drought. For stations with sufficiently long time series, the CO2 anomaly observed in 2018 was compared to previous European droughts in 2003 and 2015. Considering the areas most affected by the temperature anomalies, we found a higher CO2 anomaly in 2003 (+3 ppm averaged over 4 sites), and a smaller anomaly in 2015 (+1 ppm averaged over 11 sites) compared to 2018. This article is part of the theme issue 'Impacts of the 2018 severe drought and heatwave in Europe: from site to continental scale'.- Published
- 2020
- Full Text
- View/download PDF
5. Author Correction: Global and regional trends of atmospheric sulfur.
- Author
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Aas W, Mortier A, Bowersox V, Cherian R, Faluvegi G, Fagerli H, Hand J, Klimont Z, Galy-Lacaux C, Lehmann CMB, Myhre CL, Myhre G, Olivié D, Sato K, Quaas J, Rao PSP, Schulz M, Shindell D, Skeie RB, Stein A, Takemura T, Tsyro S, Vet R, and Xu X
- Abstract
An amendment to this paper has been published and can be accessed via a link at the top of the paper.
- Published
- 2020
- Full Text
- View/download PDF
6. Microglia Express Insulin-Like Growth Factor-1 in the Hippocampus of Aged APP swe /PS1 ΔE9 Transgenic Mice.
- Author
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Myhre CL, Thygesen C, Villadsen B, Vollerup J, Ilkjær L, Krohn KT, Grebing M, Zhao S, Khan AM, Dissing-Olesen L, Jensen MS, Babcock AA, and Finsen B
- Abstract
Insulin-like growth factor-1 (IGF-1) is a pleiotropic molecule with neurotrophic and immunomodulatory functions. Knowing the capacity of chronically activated microglia to produce IGF-1 may therefore show essential to promote beneficial microglial functions in Alzheimer's disease (AD). Here, we investigated the expression of IGF-1 mRNA and IGF-1 along with the expression of tumor necrosis factor (TNF) mRNA, and the amyloid-β (Aβ) plaque load in the hippocampus of 3- to 24-month-old APP
swe /PS1ΔE9 transgenic (Tg) and wild-type (WT) mice. As IGF-1, in particular, is implicated in neurogenesis we also monitored the proliferation of cells in the subgranular zone (sgz) of the dentate gyrus. We found that the Aβ plaque load reached its maximum in aged 21- and 24-month-old APPswe /PS1ΔE9 Tg mice, and that microglial reactivity and hippocampal IGF-1 and TNF mRNA levels were significantly elevated in aged APPswe /PS1ΔE9 Tg mice. The sgz cell proliferation decreased with age, regardless of genotype and increased IGF-1/TNF mRNA levels. Interestingly, IGF-1 mRNA was expressed in subsets of sgz cells, likely neuroblasts, and neurons in both genotypes, regardless of age, as well as in glial-like cells. By double in situ hybridization these were shown to be IGF1 mRNA+ CD11b mRNA+ cells, i.e., IGF-1 mRNA-expressing microglia. Quantification showed a 2-fold increase in the number of microglia and IGF-1 mRNA-expressing microglia in the molecular layer of the dentate gyrus in aged APPswe /PS1ΔE9 Tg mice. Double-immunofluorescence showed that IGF-1 was expressed in a subset of Aβ plaque-associated CD11b+ microglia and in several subsets of neurons. Exposure of primary murine microglia and BV2 cells to Aβ42 did not affect IGF-1 mRNA expression. IGF-1 mRNA levels remained constant in WT mice with aging, unlike TNF mRNA levels which increased with aging. In conclusion, our results suggest that the increased IGF-1 mRNA levels can be ascribed to a larger number of IGF-1 mRNA-expressing microglia in the aged APPswe /PS1ΔE9 Tg mice. The finding that subsets of microglia retain the capacity to express IGF-1 mRNA and IGF-1 in the aged APPswe /PS1ΔE9 Tg mice is encouraging, considering the beneficial therapeutic potential of modulating microglial production of IGF-1 in AD.- Published
- 2019
- Full Text
- View/download PDF
7. Global and regional trends of atmospheric sulfur.
- Author
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Aas W, Mortier A, Bowersox V, Cherian R, Faluvegi G, Fagerli H, Hand J, Klimont Z, Galy-Lacaux C, Lehmann CMB, Myhre CL, Myhre G, Olivié D, Sato K, Quaas J, Rao PSP, Schulz M, Shindell D, Skeie RB, Stein A, Takemura T, Tsyro S, Vet R, and Xu X
- Abstract
The profound changes in global SO
2 emissions over the last decades have affected atmospheric composition on a regional and global scale with large impact on air quality, atmospheric deposition and the radiative forcing of sulfate aerosols. Reproduction of historical atmospheric pollution levels based on global aerosol models and emission changes is crucial to prove that such models are able to predict future scenarios. Here, we analyze consistency of trends in observations of sulfur components in air and precipitation from major regional networks and estimates from six different global aerosol models from 1990 until 2015. There are large interregional differences in the sulfur trends consistently captured by the models and observations, especially for North America and Europe. Europe had the largest reductions in sulfur emissions in the first part of the period while the highest reduction came later in North America and East Asia. The uncertainties in both the emissions and the representativity of the observations are larger in Asia. However, emissions from East Asia clearly increased from 2000 to 2005 followed by a decrease, while in India a steady increase over the whole period has been observed and modelled. The agreement between a bottom-up approach, which uses emissions and process-based chemical transport models, with independent observations gives an improved confidence in the understanding of the atmospheric sulfur budget.- Published
- 2019
- Full Text
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8. Corrigendum: Collocated observations of cloud condensation nuclei, particle size distributions, and chemical composition.
- Author
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Schmale J, Henning S, Henzing B, Keskinen H, Sellegri K, Ovadnevaite J, Bougiatioti A, Kalivitis N, Stavroulas I, Jefferson A, Park M, Schlag P, Kristensson A, Iwamoto Y, Pringle K, Reddington C, Aalto P, Äijälä M, Baltensperger U, Bialek J, Birmili W, Bukowiecki N, Ehn M, Fjæraa AM, Fiebig M, Frank G, Fröhlich R, Frumau A, Furuya M, Hammer E, Heikkinen L, Herrmann E, Holzinger R, Hyono H, Kanakidou M, Kiendler-Scharr A, Kinouchi K, Kos G, Kulmala M, Mihalopoulos N, Motos G, Nenes A, O'Dowd C, Paramonov M, Petäjä T, Picard D, Poulain L, Prévôt ASH, Slowik J, Sonntag A, Swietlicki E, Svenningsson B, Tsurumaru H, Wiedensohler A, Wittbom C, Ogren JA, Matsuki A, Yum SS, Myhre CL, Carslaw K, Stratmann F, and Gysel M
- Abstract
This corrects the article DOI: 10.1038/sdata.2017.3.
- Published
- 2018
- Full Text
- View/download PDF
9. TNFα affects CREB-mediated neuroprotective signaling pathways of synaptic plasticity in neurons as revealed by proteomics and phospho-proteomics.
- Author
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Jensen P, Myhre CL, Lassen PS, Metaxas A, Khan AM, Lambertsen KL, Babcock AA, Finsen B, Larsen MR, and Kempf SJ
- Abstract
Neuroinflammation is a hallmark of Alzheimer's disease and TNFα as the main inducer of neuroinflammation has neurodegenerative but also pro-regenerative properties, however, the dose-dependent molecular changes on signaling pathway level are not fully understood. We performed quantitative proteomics and phospho-proteomics to target this point. In HT22 cells, we found that TNFα reduced mitochondrial signaling and inhibited mTOR protein translation signaling but also led to induction of neuroprotective MAPK-CREB signaling. Stimulation of human neurons with TNFα revealed similar cellular mechanisms. Moreover, a number of synaptic plasticity-associated genes were altered in their expression profile including CREB . SiRNA-mediated knockdown of CREB in human neurons prior to TNFα stimulation led to a reduced number of protein/phospho-protein hits compared to siRNA-mediated knockdown of CREB or TNFα stimulation alone and countermeasured the reduced CREB signaling. In vivo data of TNFα knockout mice showed that learning ability did not depend on TNFα per se but that TNFα was essential for preserving the learning ability after episodes of lipopolysaccharide-induced neuroinflammation. This may be based on modulation of CREB/CREB signaling as revealed by the in vitro / in vivo data. Our data show that several molecular targets and signaling pathways induced by TNFα in neurons resemble those seen in Alzheimer's disease pathology., Competing Interests: CONFLICTS OF INTEREST The authors declare no competing interests.
- Published
- 2017
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10. Collocated observations of cloud condensation nuclei, particle size distributions, and chemical composition.
- Author
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Schmale J, Henning S, Henzing B, Keskinen H, Sellegri K, Ovadnevaite J, Bougiatioti A, Kalivitis N, Stavroulas I, Jefferson A, Park M, Schlag P, Kristensson A, Iwamoto Y, Pringle K, Reddington C, Aalto P, Äijälä M, Baltensperger U, Bialek J, Birmili W, Bukowiecki N, Ehn M, Fjæraa AM, Fiebig M, Frank G, Fröhlich R, Frumau A, Furuya M, Hammer E, Heikkinen L, Herrmann E, Holzinger R, Hyono H, Kanakidou M, Kiendler-Scharr A, Kinouchi K, Kos G, Kulmala M, Mihalopoulos N, Motos G, Nenes A, O'Dowd C, Paramonov M, Petäjä T, Picard D, Poulain L, Prévôt AS, Slowik J, Sonntag A, Swietlicki E, Svenningsson B, Tsurumaru H, Wiedensohler A, Wittbom C, Ogren JA, Matsuki A, Yum SS, Myhre CL, Carslaw K, Stratmann F, and Gysel M
- Abstract
Cloud condensation nuclei (CCN) number concentrations alongside with submicrometer particle number size distributions and particle chemical composition have been measured at atmospheric observatories of the Aerosols, Clouds, and Trace gases Research InfraStructure (ACTRIS) as well as other international sites over multiple years. Here, harmonized data records from 11 observatories are summarized, spanning 98,677 instrument hours for CCN data, 157,880 for particle number size distributions, and 70,817 for chemical composition data. The observatories represent nine different environments, e.g., Arctic, Atlantic, Pacific and Mediterranean maritime, boreal forest, or high alpine atmospheric conditions. This is a unique collection of aerosol particle properties most relevant for studying aerosol-cloud interactions which constitute the largest uncertainty in anthropogenic radiative forcing of the climate. The dataset is appropriate for comprehensive aerosol characterization (e.g., closure studies of CCN), model-measurement intercomparison and satellite retrieval method evaluation, among others. Data have been acquired and processed following international recommendations for quality assurance and have undergone multiple stages of quality assessment.
- Published
- 2017
- Full Text
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11. Measurements of δ 13 C in CH 4 and using particle dispersion modeling to characterize sources of Arctic methane within an air mass.
- Author
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France JL, Cain M, Fisher RE, Lowry D, Allen G, O'Shea SJ, Illingworth S, Pyle J, Warwick N, Jones BT, Gallagher MW, Bower K, Le Breton M, Percival C, Muller J, Welpott A, Bauguitte S, George C, Hayman GD, Manning AJ, Myhre CL, Lanoisellé M, and Nisbet EG
- Abstract
A stratified air mass enriched in methane (CH
4 ) was sampled at ~600 m to ~2000 m altitude, between the north coast of Norway and Svalbard as part of the Methane in the Arctic: Measurements and Modelling campaign on board the UK's BAe-146-301 Atmospheric Research Aircraft. The approach used here, which combines interpretation of multiple tracers with transport modeling, enables better understanding of the emission sources that contribute to the background mixing ratios of CH4 in the Arctic. Importantly, it allows constraints to be placed on the location and isotopic bulk signature of the emission source(s). Measurements of δ13 C in CH4 in whole air samples taken while traversing the air mass identified that the source(s) had a strongly depleted bulk δ13 C CH4 isotopic signature of -70 (±2.1)‰. Combined Numerical Atmospheric-dispersion Modeling Environment and inventory analysis indicates that the air mass was recently in the planetary boundary layer over northwest Russia and the Barents Sea, with the likely dominant source of methane being from wetlands in that region.- Published
- 2016
- Full Text
- View/download PDF
12. Constraints on oceanic methane emissions west of Svalbard from atmospheric in situ measurements and Lagrangian transport modeling.
- Author
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Pisso I, Myhre CL, Platt SM, Eckhardt S, Hermansen O, Schmidbauer N, Mienert J, Vadakkepuliyambatta S, Bauguitte S, Pitt J, Allen G, Bower KN, O'Shea S, Gallagher MW, Percival CJ, Pyle J, Cain M, and Stohl A
- Abstract
Methane stored in seabed reservoirs such as methane hydrates can reach the atmosphere in the form of bubbles or dissolved in water. Hydrates could destabilize with rising temperature further increasing greenhouse gas emissions in a warming climate. To assess the impact of oceanic emissions from the area west of Svalbard, where methane hydrates are abundant, we used measurements collected with a research aircraft (Facility for Airborne Atmospheric Measurements) and a ship (Helmer Hansen) during the Summer 2014 and for Zeppelin Observatory for the full year. We present a model-supported analysis of the atmospheric CH
4 mixing ratios measured by the different platforms. To address uncertainty about where CH4 emissions actually occur, we explored three scenarios: areas with known seeps, a hydrate stability model, and an ocean depth criterion. We then used a budget analysis and a Lagrangian particle dispersion model to compare measurements taken upwind and downwind of the potential CH4 emission areas. We found small differences between the CH4 mixing ratios measured upwind and downwind of the potential emission areas during the campaign. By taking into account measurement and sampling uncertainties and by determining the sensitivity of the measured mixing ratios to potential oceanic emissions, we provide upper limits for the CH4 fluxes. The CH4 flux during the campaign was small, with an upper limit of 2.5 nmol m-2 s-1 in the stability model scenario. The Zeppelin Observatory data for 2014 suggest CH4 fluxes from the Svalbard continental platform below 0.2 Tg yr-1 . All estimates are in the lower range of values previously reported.- Published
- 2016
- Full Text
- View/download PDF
13. Jury is still out on the radiative forcing by black carbon.
- Author
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Boucher O, Balkanski Y, Hodnebrog Ø, Myhre CL, Myhre G, Quaas J, Samset BH, Schutgens N, Stier P, and Wang R
- Subjects
- Carbon analysis, Air Pollution analysis, Soot
- Abstract
Competing Interests: The authors declare no conflict of interest.
- Published
- 2016
- Full Text
- View/download PDF
14. Telomere dysfunction reduces microglial numbers without fully inducing an aging phenotype.
- Author
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Khan AM, Babcock AA, Saeed H, Myhre CL, Kassem M, and Finsen B
- Subjects
- Animals, Antigens, CD, Antigens, Differentiation, Myelomonocytic, Apoptosis genetics, Dentate Gyrus cytology, Dentate Gyrus pathology, Ferritins, Leukocyte Common Antigens, Mice, Inbred C57BL, Mice, Knockout, Neurodegenerative Diseases, Spatial Learning, Telomere physiology, Aging genetics, Aging pathology, Cellular Senescence genetics, Cellular Senescence physiology, Microglia pathology, Phenotype, RNA genetics, Telomerase deficiency, Telomerase genetics, Telomere pathology
- Abstract
The susceptibility of the aging brain to neurodegenerative disease may in part be attributed to cellular aging of the microglial cells that survey it. We investigated the effect of cellular aging induced by telomere shortening on microglia by the use of mice lacking the telomerase RNA component (TERC) and design-based stereology. TERC knockout (KO) mice had a significantly reduced number of CD11b(+) microglia in the dentate gyrus. Because of an even greater reduction in dentate gyrus volume, microglial density was, however, increased. Microglia in TERC KO mice maintained a homogenous distribution and normal expression of CD45 and CD68 and the aging marker, ferritin, but were morphologically distinct from microglia in both adult and old wild-type mice. TERC KO mice also showed increased cellular apoptosis and impaired spatial learning. Our results suggest that individual microglia are relatively resistant to telomerase deficiency during steady state conditions, despite an overall reduction in microglial numbers. Furthermore, telomerase deficiency and aging may provide disparate cues leading to distinct changes in microglial morphology and phenotype., (Copyright © 2015 Elsevier Inc. All rights reserved.)
- Published
- 2015
- Full Text
- View/download PDF
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