Dellagiustaite: A Novel Natural Spinel Containing V2+

Dellagiustaite, ideally Al2V2+O4, is a new spinel-group mineral from Sierra de Comechingones, San Luis, Argentina, where it is found associated with hibonite (containing tubular inclusions, 5–100 μm, of metallic vanadium), grossite, and two other unknown phases with ideal stoichiometry of Ca2Al3O6F and Ca2Al2SiO7. A very similar rock containing dellagiustaite has been found at Mt Carmel (northern Israel), where super-reduced mineral assemblages have crystallized from high-T melts trapped in corundum aggregates (micro-xenoliths) within picritic-tholeiitic lavas ejected from Cretaceous volcanoes. In the holotype, euhedral grains of dellagiustaite are found as inclusions in grossite. The empirical average chemical formula of dellagiustaite is (Al1.09 V 0.91 2 + V 0.87 3 + Mg0.08 Ti 0.04 3 + Mn0.01)Σ3O4, but it may show limited replacement of V2+ by Mg and of V3+ by Al. As Al is the dominant trivalent cation, the ideal formula is Al2V2+O4 according to the current IMA rules. Dellagiustaite shows the usual space group of spinel-group minerals (Fd 3 ¯ m, R1 = 1.46%) with a = 8.1950(1) Å. The observed mean bond lengths <T–O> = 1.782(2) Å and <M–O> = 2.0445(9) Å, the observed site scattering (T = 13.3 eps, M = 22.5 eps), and the chemical composition show that dellagiustaite is an inverse spinel: T tetrahedra are occupied by Al3+, whereas M octahedra are occupied by V2+ and V3+, leading to the site assignment as TAlM( V 0.91 2 + V 0.88 3 + Al 0.09 3 + Mg0.08 Ti 0.03 3 + Mn0.01)O4.

Platelet Pathology in GATA-1 Dyserythropoietic Macrothrombocytopenia.

Germline mutations in the X-linked hematopoietic transcription factor, GATA-1, have been associated with dyserythropoietic anemia (DEA), macrothrombocytopenia (MTP), and congenital erythropoietic porphyria. Recently, morphological features suggestive of the Gray Platelet Syndrome (GPS) were described in a pedigree with a germline R216Q GATA-1 mutation (Blood106:6a, 2005). The present study has evaluated platelets (Pl) in the electron microscope from members of a previously described pedigree (Blood98:2681–2688, 2001) with GATA-1 G208S, MTP, and dyserythropoiesis without anemia, for whom detailed platelet morphology studies have not been reported. The presence of a hemizygous GATA-1 mutation was confirmed by conventional fluorescent dye chemistry sequencing of DNA from patient peripheral blood mononuclear cells. Their Pl revealed wide variations in size, shape, internal and external structure. Some normal sized and giant Pl contained usual numbers of alpha granules and dense bodies, while most of the large cells were hypogranular. Some contained no membrane systems or organelles. Others were filled with masses of dense tubular system (DTS) channels, and others contained the tubular inclusions found in the Medich Giant Platelets Disorder (Platelets15:345–353, 2004). Many of the hypogranular cells contained small vacuoles that may have been enclosing membranes of alpha granules. Except for the tubular inclusions, all of these structural variations are observed in GPS Pl (Am. J. Pathol.95:445–462, 1979). However, additional striking abnormalities were seen in GATA-1 Pl that are not characteristic of GPS Pl. Many GATA-1 Pl contained unusual, closely associated dense double membranes differing from normal elements of rough endoplasmic reticulum, smooth endoplasmic reticulum, DTS or surface connected open canalicular system (OCS), but resembling channels of the OCS after exposure to EDTA. They were observed previously only in megakaryocytes (Mk) from one family with GATA-1 DEA-MTP (Nat. Genet, 24:266–270, 2000). The dense double membranes were often found in parallel association and, in some examples, isolating areas of cytoplasm. However, the isolated areas were not undergoing autophagic degradation as such areas enclosed by elements of the DTS do in White Platelet Syndrome Pl (Platelets 15:173,2004). Instead, they proved to be another unique feature of GATA-1 platelets, the presence of Pl within Pl. The sequestered cells were usually mature in appearance and often discoid in form with circumferential coils of microtubules. In some GATA-1 Pl there were two Pl within the same cell, and on rare occasions, a Pl within a Pl within a Pl. Pl within Pl have never been observed previously in any human platelet disorder. Another unique feature, related to Pl within Pl, was the frequent Pl to Pl surface attachment of non-activated cells forming large macrothrombocytes with no similarity to aggregates of stimulated normal platelets. Conclusion: The substructural abnormalities of Pl from patients with germline GATA-1 mutations share some overlap with those seen in GPS Pl, but are distinct and unique. The MTP, Pl within Pl and surface Pl to Pl attachments suggest a major defect in the formation and separation of GATA-1 Pl from pro-Pl of the parent Mk, resulting in the MTP characteristic of the disorder.

Age-related uterine and ovarian hypertrophy in FSH receptor knockout and FSHbeta subunit knockout mice

Female mice in which the gene encoding the follicle-stimulating hormone FSH receptor (FSHR) knockout (KO) or its ligand (FSHbetaKO) have been disrupted were infertile. Ovaries of these mice were significantly smaller than those of heterozygous littermates but significantly larger than those of hypogonadal mice of the same age. Uterine masses in all three mutants were <6 mg, significantly reduced compared with heterozygous mice. At 1 year of age uterine mass had increased to >12 mg in 63% of FSHRKO females and 88% of FSHbetaKO females. Despite the increase in uterine size there was no evidence of contractility: uteri were flaccid and unresponsive to electrical or pharmacological stimulation. In most females in which uterine growth had occurred there was evidence of ovarian growth with hypertrophy of the interstitial tissue, occurrence of ovarian cysts and epithelial and tubular inclusions. There was no evidence of uterine or ovarian hypertrophy in hypogonadal (hpg) mice at any age or in 1 year old females in which the FSH mutations were bred onto the hpg background. There was an inverse correlation of plasma LH concentrations and uterine mass in 1 year old mutant females with uterine hypertrophy. Ovariectomy of both FSHRKO and FSHbetaKO females with large uteri resulted in decreased uterine mass and increased plasma concentration of LH. The number of mice with ovarian pathology, reminiscent of the serous ovarian adenocarcinomas found in humans, was significantly greater in the FSHbetaKO mice, indicating that the presence of an intact FSH receptor on ovarian cells of FSHbetaKO females may allow constitutive basal stimulation of the ovary, which is absent in mice lacking FSH receptors.

Cytopathological characterization of Mal de Río Cuarto virus in corn, wheat and barley

The Mal de Río Cuarto disease is caused by Mal de Río Cuarto virus (MRCV) transmitted by Delphacodes kuscheli. Comparative studies were carried out on the cytopathological alterations produced by MRCV in corn (Zea mays), wheat (Triticum aestivum) and barley (Hordeum vulgare), as seen with a transmission electron microscope. Corn plants were infected with viruliferous D. kuscheli collected from the endemic disease area (i.e. Río Cuarto County, Córdoba, Argentina). For the viral transmission to small grain cereal plants, laboratory rared insects were used. In this case, the inoculum source was wheat and barley plants infected with MRCV isolate grown in a greenhouse. Leaf samples with conspicuous symptoms were collected: enations and size reduction in corn; crenatures, swelling veins and dark green color in small grain cereals. Viral infection was corroborated by DAS-ELISA. Viroplasms containing complete and incomplete virus particles and fibrillar material were found in the cytoplasm of infected cells in all species. Mature virions were between 60 and 70 nm diameter. In wheat and barley, viroplasms and dispersed particles were observed only in phloem, while in corn virions were also found in cells of the bundle sheath. Crystalline arrays of particles were detected in corn enation constitutive cells. Tubular inclusions were found only in wheat samples. The three species showed abnormalities in the chloroplasts of affected cells. The results showed that MRCV cytopathology has similarities with other viruses from the genus Fijivirus, family family Reoviridae, but slight differences depending upon the host plant.

Preservation of Articular Cartilage for Electron Microscopy

Water makes up 60-80% of the wet weight of articular cartilage. The remaining parts of this tissue are made up of a variety of cells, generally referred to as chondrocytes, and an extracellular matrix of, collagen fibrils (types II, IX and XI), proteoglycans. The collagens and proteoglycans, with associated water, are assembled into a structure that is capable of withstanding considerable loading.The micro-structure of adult rabbit articular cartilage has been described, based upon ultrastructural studies. The tissue is arranged into zones, mainly based on the general orientation of collagen fibrils (See Figure 1). The collagen framework in the radial zone forms a continuous area of radially oriented and tightly bound collagen fibrils, in which are embedded at regular interval, tubular inclusions of proteoglycans (Figure 2). in rabbit tibial plateau tissue these inclusions have diameter of 1-3 fim and can be continuous from the calcified to the tangential zone.

Les enclaves du volcanisme recent du rift syrien

In direct continuity with the Dead Sea fault, the Syrian rift, which links the rigid Arabian plate to the mobile ophiolite belt of Cyprus-southern Turkey, plays a very important role in the regional geodynamic structure. Its exact position, as well as the related fracture system, has been documented from the analysis of a complete aerial photo coverage of the whole Syrian territory. The rift corresponds to a transform fault, with lateral displacements decreasing from more than 100 km, to the south, to less than 30 km to the north. Several major episodes of volcanic activity have occurred since early Mesozoic times, with eruptive centers located in three major domains, southern (S), center (M) and northern (N), respectively. The recent (Neogene-Quaternary) volcanism is compared to the Cretaceous one (Bhannes-Tayasir episode). Erupted lavas are in general very basic (picrobasalts, basanites), with rather primitive magmas, except for one occurrence at El Kafr (southern Syria) which corresponds to a silica-undersaturated, strongly differentiated phonolite. Major and partial (Rb, Ba, Nb, Sr, Y, Lu) trace-element data show overall similarities between recent and Cretaceous volcanisms, with however a more distinct alkaline trend and stronger variations of LILE-elements for recent lavas. Few volcanoes contain a number of ultrabasic xenoliths, notably lherzolites, harzburgites and pyroxenites. Rare garnet-bearing varieties have also been observed in M and S-domains, including few grenatites. Xenolith texture is protogranular or granular, with a variable (mostly limited) degree of local melting by the enclosing basalt. Olivines are Mg-rich (mg (super *) = 0.93-0.83), as are ortho-and clinopyroxene. This last mineral, which may show spectacular Opx and spinel exsolution lamellae, is relatively abundant, as shown by the frequent occurrence of pyroxenite (Cpx-Opx) and Cpx-rich lherzolite (wehrlite). Because of the possible occurrence of Cretaceous rocks with kimberlitic affinities [Nabi Mata, Sharkov et al., 1993], garnet has been studied in detail. On the garnet triangle, most analyses plot well away from high-pressure mantle rocks, notably kimberlites, but close to infracrustal garnet-bearing rocks (granulites). Very few analytical points (3 out of a total of 20) could correspond to garnet peridotite. All other rocks are equilibrated in the field of spinel peridotite or infracrustal granulites. Pure CO 2 -bearing fluid inclusions have been found in olivine and pyroxenes from xenoliths and in phenocrysts from enclosing basalts. Highest density fluids (up to 1.15 g/cm 3 ), are observed in pyroxenites, especially from M-domain. They occur in primary, tubular inclusions adjacent to or even containing minute spinel grains, oriented along the exsolution lamellae of the clinopyroxene-host. P-T conditions of mineral equilibration in the xenoliths have been estimated from the pyroxene thermometer [Bertrand and Mercier, 1986; Brey and Kohler, 1990] and maximum density of fluid trapped in primary inclusions. They correspond to about 1 100-1 300 degrees C for the temperature, 10-13 kb for the pressure. These P-T conditions do not show any significant variation between different regional occurrences, but well between various petrographical types, the maximum conditions being recorded in pyroxenites. These results suggest that some clinopyroxene at least has been formed by mantle metasomatism caused by ephemeral carbonate magmas, in a mantle plume located under the Arabic plate.