The Lithium, Boron and Beryllium content of serpentinized peridotites from ODP Leg 209 (Sites 1272A and 1274A): Implications for lithium and boron budgets of oceanic lithosphere

Despite the key importance of altered oceanic mantle as a repository and carrier of light elements (B, Li, and Be) to depth, its inventory of these elements has hardly been explored and quantified. In order to constrain the systematics and budget of these elements we have studied samples of highly serpentinized (>50%) spinel harzburgite drilled at the Mid-Atlantic Ridge (Fifteen-Twenty Fracture zone, ODP Leg 209, Sites 1272A and 1274A). In-situ analysis by secondary ion mass spectrometry reveals that the B, Li and Be contents of mantle minerals (olivine, orthopyroxene, and clinopyroxene) remain unchanged during serpentinization. B and Li abundances largely correspond to those of unaltered mantle minerals whereas Be is close to the detection limit. The Li contents of clinopyroxene are slightly higher (0.44-2.8 mu g g(-1)) compared to unaltered mantle clinopyroxene, and olivine and clinopyroxene show an inverse Li partitioning compared to literature data. These findings along with textural observations and major element composition obtained from microprobe analysis suggest reaction of the peridotites with a mafic silicate melt before serpentinization. Serpentine minerals are enriched in B (most values between 10 and 100 mu g g(-1)), depleted in Li (most values below I mu g g(-1)) compared to the primary phases, with considerable variation within and between samples. Be is at the detection limit. Analysis of whole rock samples by prompt gamma activation shows that serpentinization tends to increase B (10.4-65.0 mu g g(-1)), H2O and Cl contents and to lower Li contents (0.07-3.37 mu g g(-1)) of peridotites, implying that-contrary to alteration of oceanic crust-B is fractionated from Li and that the B and Li inventory should depend essentially on rock-water ratios. Based on our results and on literature data, we calculate the inventory of B and Li contained in the oceanic lithosphere, and its partitioning between crust and mantle as a function of plate characteristics. We model four cases, an ODP Leg 209-type lithosphere with almost no igneous crust, and a Semail-type lithosphere with a thick igneous crust, both at I and 75 Ma, respectively. The results show that the Li contents of the oceanic lithosphere are highly variable (17-307 kg in a column of I m x I m x thickness of the lithosphere (kg/col)). They are controlled by the primary mantle phases and by altered crust, whereas the B contents (25-904 kg/col) depend entirely on serpentinization. In all cases, large quantities of B reside in the uppermost part of the plate and could hence be easily liberated during slab dehydration. The most prominent input of Li into subduction zones is to be expected from Semail-type lithosphere because most of the Li is stored at shallow levels in the plate. Subducting an ODP Leg 209-type lithosphere would mean only very little Li contribution from the slab. Serpentinized mantle thus plays an important role in B recycling in subduction zones, but it is of lesser importance for Li. (C) 2008 Elsevier Ltd. All rights reserved.

Pavement Surface on Macadam Base: Adair County Final Report, Iowa Highway Reserach Board Project HR-209

The quality and availability of aggregate for pc concrete stone varies across Iowa. Southwest Iowa is one area of the state that is short of quality aggregates. The concrete stone generally available in the area is limestone from the Argentine or Winterset ledges with an overburden of up to 150 feet. This concrete stone is classified as Class 1 durability and is susceptible to 'ID"-cracking. In addition, the general engineering soil classification rates the soils of southwest Iowa as having the poorest subgrade bearing characteristics in the state. 1 The combination of poor soils and low quality aggregate has contributed to premature deterioration of many miles of portland cement concrete pavement. Research project HR-209 was initiated in 1979 to explore alternative construction methods that may produce better pavements for southwest Iowa.

gp100(209-2M) peptide immunization of human lymphocyte antigen-A2+ stage I-III melanoma patients induces significant increase in antigen-specific effector and long-term memory CD8+ T cells.

Thirty-five HLA-A2(+) patients with completely resected stage I-III melanoma were vaccinated multiple times over 6 months with a modified melanoma peptide, gp100(209-2M), emulsified in Montanide adjuvant. Direct ex vivo gp100(209-2M) tetramer analysis of pre- and postvaccine peripheral blood mononuclear cells (PBMCs) demonstrated significant increases in the frequency of tetramer(+) CD8(+) T cells after immunization for 33 of 35 evaluable patients (median, 0.36%; range, 0.05-8.9%). Ex vivo IFN-gamma cytokine flow cytometry analysis of postvaccine PBMCs after brief gp100(209-2M) in vitro activation showed that for all of the patients studied tetramer(+) CD8(+) T cells produced IFN-gamma; however, some patients had significant numbers of tetramer(+) IFN-gamma(-) CD8(+)T cells suggesting functional anergy. Additionally, 8 day gp100(209-2M) in vitro stimulation (IVS) of pre- and postvaccine PBMCs resulted in significant expansion of tetramer(+) CD8(+) T cells from postvaccine cells for 34 patients, and these IVS tetramer(+) CD8(+) T cells were functionally responsive by IFN-gamma cytokine flow cytometry analysis after restimulation with either native or modified gp100 peptide. However, correlated functional and phenotype analysis of IVS-expanded postvaccine CD8(+) T cells demonstrated the proliferation of functionally anergic gp100(209-2M)- tetramer(+) CD8(+) T cells in several patients and also indicated interpatient variability of gp100(209-2M) stimulated T-cell proliferation. Flow cytometry analysis of cryopreserved postvaccine PBMCs from representative patients showed that the majority of tetramer(+) CD8+ T cells (78.1 +/- 4.2%) had either an "effector" (CD45 RA(+)/CCR7(-)) or an "effector-memory" phenotype (CD45RA(-)/CCR7(-)). Notably, analysis of PBMCs collected 12-24 months after vaccine therapy demonstrated the durable presence of gp100(209-2M)-specific memory CD8(+) T cells with high proliferation potential. Overall, this report demonstrates that after vaccination with a MHC class I-restricted melanoma peptide, resected nonmetastatic melanoma patients can mount a significant antigen-specific CD8(+) T-cell immune response with a functionally intact memory component. The data further support the combined use of tetramer binding and functional assays in correlated ex vivo and IVS settings as a standard for immunomonitoring of cancer vaccine patients.

Proteasomal cleavage does not determine immunogenicity of gp100-derived peptides gp100 209-217 and gp100 209-217T210M.

Immune responses against tumor-associated antigens rely on efficient epitope presentation. The melanoma-associated antigen (Ag) gp100 contains HLA-A*0201 ligands that are characterized by low to medium binding affinity, among which gp100(209-217) is the most prominent (Kawakami et al., J Immunol 154:3961-3968, 1995). While this epitope is a natural T-cell target, it primes with low-efficiency T-cell responses during immunization. A modified gp100 epitope, gp100(209-217T210M), that contains a Thr to Met substitution at position 2 of the antigenic nonamer is characterized by high binding affinity for HLA-A*0201 and elicits strong and clinically effective T-cell responses. This higher affinity is believed to represent the sole reason for enhanced immunogenicity. Contrasting with this observation is the unpredictable relationship between affinity and immunogenicity observed in other antigen systems. In addition, we noted a striking difference between the capability of endogenously processed gp100(209-217) and gp100(209-217T210M) to induce T-cell responses in an in vitro model. Therefore, we questioned whether factors other than HLA-affinity might play a role in determining the immunogenicity of these epitopes. In the present study, we evaluated the in vitro proteasomal cleavages of 23meric precursor peptides encompassing the native sequence (gp100(201-223)) or the modified sequence (gp100(201-223T210M)). Here we show that the standard proteasome liberates the C-termini of both antigenic peptides but not the N-termini. Quantitative analysis of the digestion products revealed that more of the fragments displaying the final C-termini were produced from the wild-type precursor. However, a stronger TCR engagement was observed when fractions of digested gp100(201-223T210M) were used to activate an HLA-A*0201-expressing target T-cell clone. This difference was also found using separately produced, synthetic nonamers. In conclusion, the high binding affinity of gp100(209-217T210M) seems to compensate for possible differences in proteasomal cleavage at the biological level. Since the final antigenic nonamer is not directly produced by the proteasome, additional further factors may influence the antigenic peptide availability, such as post-proteasomal processing and intracellular peptide transport.

Pavement Surface on Macadam Base, Adair County, HR-209, Construction Report, 1980

The objectives were to determine the feasibility and performance of this type of construction and to determine if the macadam base is effective in reducin9or eliminating D-cracking deterioration.

Français 209

Contient : 1° « Gratianopolitanae urbis descriptio a LAURENTIO RABOTIO et PETRO GILIBERTO, senatoribus gratianopolitanis, 1572 » ; 2° « Inscriptiones duae quae Valentiae extant » ; 3° « Descriptio urbis Valentinae, versibus expressa ab eodem PETRO GILIBERTO » ; 4° « Ejusdem PETRI GILIBERTI de Gasparis Colignii acerba et improvisa morte carmen » ; 5° « Sommaire de ce que j'ay peu trouver de Valence sur le Rhodne ». (Extrait de Me MEDARD DU CLUSET) ; 6° « Extrait d'un livre fort ancien escript à la main en parchemin, de lettre fort caduque, estant en la possession de noble Clement Faure de Valence, avec autres extraits de STRABON, OROSE, PTOLEMEE, etc. » ; 7° « De la Cité de Valence sur le Rhone, selon Me FRANÇOIS ROALDES »

Resolución N° 209 ¿Cómo entiende la Cámara de comercio el evento de suspensión de deliberaciones en una asamblea de accionistas respecto del tiempo que estas se pueden suspender sin que la reunión pierda validez legal?

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Resolución N° 209 ¿Cómo estudia la cámara de comercio el elemento del quórum en las reuniones de asamblea en una sociedad en comandita por acciones?

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Precision laser spectroscopy of the ground state hyperfine splitting of hydrogenlike ^209 Bi^82+

The first direct observation of a hyperfine splitting in the optical regime is reported. The wavelength of the M1 transition between the F = 4 and F = 5 hyperfine levels of the ground state of hydrogenlike ^209 Bi^82+ was measured to be \lamda_0 = 243.87(4) nm by detection of laser induced fluorescence at the heavy-ion storage ring ESR at GSI. In addition, the lifetime of the laser excited F = 5 sublevel was determined to be \tau_0 = 0.351(16) ms. The method can be applied to a number of other nuclei and should allow a novel test of QED corrections in the previously unexplored combination of strong magnetic and electric fields in highly charged ions.

Acuerdo No. 209

Consagración de Colegiales de Número del COlegio Mayor de Nuestra Señora del Rosario. 3 de diciembre de 2009