Hydrated silicate minerals on Mars observed by the Mars Reconnaissance Orbiter CRISM instrument.

Phyllosilicates, a class of hydrous mineral first definitively identified on Mars by the OMEGA (Observatoire pour la Mineralogie, L'Eau, les Glaces et l'Activitié) instrument, preserve a record of the interaction of water with rocks on Mars. Global mapping showed that phyllosilicates are widespread but are apparently restricted to ancient terrains and a relatively narrow range of mineralogy (Fe/Mg and Al smectite clays). This was interpreted to indicate that phyllosilicate formation occurred during the Noachian (the earliest geological era of Mars), and that the conditions necessary for phyllosilicate formation (moderate to high pH and high water activity) were specific to surface environments during the earliest era of Mars's history. Here we report results from the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) of phyllosilicate-rich regions. We expand the diversity of phyllosilicate mineralogy with the identification of kaolinite, chlorite and illite or muscovite, and a new class of hydrated silicate (hydrated silica). We observe diverse Fe/Mg-OH phyllosilicates and find that smectites such as nontronite and saponite are the most common, but chlorites are also present in some locations. Stratigraphic relationships in the Nili Fossae region show olivine-rich materials overlying phyllosilicate-bearing units, indicating the cessation of aqueous alteration before emplacement of the olivine-bearing unit. Hundreds of detections of Fe/Mg phyllosilicate in rims, ejecta and central peaks of craters in the southern highland Noachian cratered terrain indicate excavation of altered crust from depth. We also find phyllosilicate in sedimentary deposits clearly laid by water. These results point to a rich diversity of Noachian environments conducive to habitability.

Assessment of Mars Exploration Rover landing site predictions.

Comprehensive analyses of remote sensing data during the three-year effort to select the Mars Exploration Rover landing sites at Gusev crater and at Meridiani Planum correctly predicted the atmospheric density profile during entry and descent and the safe and trafficable surfaces explored by the two rovers. The Gusev crater site was correctly predicted to be a low-relief surface that was less rocky than the Viking landing sites but comparably dusty. A dark, low-albedo, flat plain composed of basaltic sand and haematite with very few rocks was expected and found at Meridiani Planum. These results argue that future efforts to select safe landing sites based on existing and acquired remote sensing data will be successful. In contrast, geological interpretations of the sites based on remote sensing data were less certain and less successful, which emphasizes the inherent ambiguities in understanding surface geology from remotely sensed data and the uncertainty in predicting exactly what materials will be available for study at a landing site.

Macrophage inflammatory protein-1 alpha activates basophils and mast cells.

Macrophage inflammatory protein-1 (MIP) is a recently cloned cytokine that causes neutrophilic infiltration and induces an inflammatory response. We studied the effect of MIP-1 alpha on histamine secretion from basophils and mast cells. Leukocytes from allergic and normal subjects were studied. MIP-1 alpha caused dose-dependent release of histamine from basophils of 14 of 20 allergic donors at concentrations of 10(-9)-10(-7) M, and the mean release was 13.50 +/- 2.9% at the highest concentration. In the same experiments, the mean histamine release by anti-immunoglobulin E and monocyte chemotactic and activating factor (MCAF) (10(-7) M) was 32 +/- 7% and 31 +/- 3%, respectively. The cells from only 2 of 10 normal subjects released histamine in response to MIP-1 alpha. Histamine release by MIP-1 alpha was rapid, and almost complete within the first 3 min. MIP-1 alpha-induced degranulation was a calcium-dependent noncytotoxic process. MIP-1 alpha showed chemotactic activity for purified basophils that was comparable to MCAF. Both MIP-1 alpha and MCAF at 10(-7) M concentration elicited a chemotactic response that was 40% of the maximal response to C5a (1 microgram/ml). Murine MIP-1 alpha induced histamine release from mouse peritoneal mast cells in a dose-dependent manner. Thus, we have established that MIP-1 alpha is a novel activator of basophils and mast cells.

Geology of the InSight landing site on Mars.

The Interior Exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) spacecraft landed successfully on Mars and imaged the surface to characterize the surficial geology. Here we report on the geology and subsurface structure of the landing site to aid in situ geophysical investigations. InSight landed in a degraded impact crater in Elysium Planitia on a smooth sandy, granule- and pebble-rich surface with few rocks. Superposed impact craters are common and eolian bedforms are sparse. During landing, pulsed retrorockets modified the surface to reveal a near surface stratigraphy of surficial dust, over thin unconsolidated sand, underlain by a variable thickness duricrust, with poorly sorted, unconsolidated sand with rocks beneath. Impact, eolian, and mass wasting processes have dominantly modified the surface. Surface observations are consistent with expectations made from remote sensing data prior to landing indicating a surface composed of an impact-fragmented regolith overlying basaltic lava flows.

Possible tornado-like tracks on Mars.

Distinct atmospheric conditions suggest that dark, ephemeral, filamentary lineations on the martian surface may be formed during the passage of intense atmospheric vortices.

Identification of a histamine release inhibitory factor produced by human mononuclear cells in vitro.

Human mononuclear cells (MNC) secrete histamine-releasing factor(s) (HRF) when cultured in vitro. HRF induces the release of histamine and other mediators from basophils and mast cells. We have shown that MNC also produced a histamine release inhibitory factor (HRIF), and that the synthesis is augmented by culture with physiologic concentrations of histamine (10(-10) to 10(-6) M) and by the mitogen concanavalin A (Con A). HRIF does not affect release initiated by other secretagogues such as allergen, anti-IgE, C5a, Con A, and phorbol myristate acetate. HRIF requires a preincubation with the cells for 5-10 min for maximal inhibition, and this effect is not abolished by washing the cells after the preincubation. The biological activity of HRIF is protease-sensitive, neuraminidase-resistant, and relatively heat-stable. HRIF can be distinguished from HRF by a lower apparent molecular mass (8,000-10,000 D).

Enhancement of basophil chemotaxis in vitro by virus-induced interferon.

It is well established that viral infections may precipitate or worsen attacks of bronchial asthma. Furthermore, in symptomatic atopic subjects, the local accumulation of basophils and the production of a basophil chemotactic factor have been reported. We have investigated the effect of cell-free supernates from viral stimulated cultures of human mononuclear cells on the in vitro migration of human basophils. Our results show the presence of a factor in these culture supernates that enhances the migration of basophils toward two separate chemoattractants, a peptide from C5 and a lymphokine. The enhancing activity, while affecting basophil migration, did not change the response of monocytes. The enhancing activity resembled viral-induced interferon when (a) pH 2 stability, (b) heat resistance, (c) trypsin sensitivity, and (d) species-specificity were compared. Finally, the enhancing activity for basophil chemotaxis and the interferon titer were highly correlated in preparations with a 10(4)-fold difference in interferon specific activity. Our studies show that viral-induced interferon can augment the in vitro chemotactic response of basophils. Because mediators present in basophils may be involved in the pathogenesis of immediate hypersensitivity, the modulation of basophil movement by interferon suggests a possible mechanism for the association between viral infections and atopic disorders.

Monocyte chemotactic and activating factor is a potent histamine-releasing factor for basophils.

Monocyte chemotactic and activating factor (MCAF) is a recently cloned cytokine that causes chemotaxis of basophils. In our pursuit of cytokines affecting basophil function, we studied the effect of MCAF on histamine secretion from basophils. Leukocytes from 20 donors, 10 allergic and 10 normal subjects, were studied. MCAF caused dose-dependent release of histamine at concentrations of 10(-8) and 10(-7) M, and the mean release was 31.25 +/- 2.9% at the highest concentration. In the same experiments the mean histamine release by anti-IgE and histamine releasing factor (HRF) was 27.05 +/- 4% and 32.70 +/- 2.7%, respectively. All 20 subjects responded to MCAF with significant histamine release. Allergic subjects released significantly more histamine than normals in response to anti-IgE (P less than 0.01) but not to MCAF (P = 0.2) and HRF (P = 0.1). The histamine release was significantly correlated between MCAF and HRF (P less than 0.01), but not between MCAF and anti-IgE (P greater than 0.05). The histamine release by MCAF was complete within the first 3 min. MCAF-induced degranulation was a calcium-dependent process. Leukocytes depleted of monocytes responded equally well to MCAF. Using an anti-MCAF affinity column we determined that greater than 50% of HRF activity of crude PBMC supernatant could be attributed to MCAF. Thus, we established that MCAF is a potent secretagogue for basophils.

Artificial composite bone as a model of human trabecular bone: the implant-bone interface.

The use of artificial bones in implant testing has become popular due to their low variability and ready availability. However, friction coefficients, which are critical to load transfer in uncemented implants, have rarely been compared between human and artificial bone, particularly for wet and dry conditions. In this study, the static and dynamic friction coefficients for four commercially used titanium surfaces (polished, Al(2)O(3) blasted, plasma sprayed, beaded) acting on the trabecular component of artificial bones (Sawbones) were compared to those for human trabecular bone. Artificial bones were tested in dry and wet conditions and normal interface stress was varied (0.25, 0.5, 1.0MPa). Friction coefficients were mostly lower for artificial bones than real bone. In particular, static friction coefficients for the dry polished surface were 20% of those for real bone and 42-61% for the dry beaded surface, with statistical significance (alpha<0.05). Less marked differences were observed for dynamic friction coefficients. Significant but non-systematic effects of normal stress or wet/dry condition on friction coefficients were observed within each surface type. These results indicate that the use of artificial bone models for pre-clinical implant testing that rely on interface load transfer with trabecular bone for mechanical integrity can be particularly sensitive to surface finish and lubrication conditions.

Redox stratification of an ancient lake in Gale crater, Mars.

In 2012, NASA's Curiosity rover landed on Mars to assess its potential as a habitat for past life and investigate the paleoclimate record preserved by sedimentary rocks inside the ~150-kilometer-diameter Gale impact crater. Geological reconstructions from Curiosity rover data have revealed an ancient, habitable lake environment fed by rivers draining into the crater. We synthesize geochemical and mineralogical data from lake-bed mudstones collected during the first 1300 martian solar days of rover operations in Gale. We present evidence for lake redox stratification, established by depth-dependent variations in atmospheric oxidant and dissolved-solute concentrations. Paleoclimate proxy data indicate that a transition from colder to warmer climate conditions is preserved in the stratigraphy. Finally, a late phase of geochemical modification by saline fluids is recognized.

Large wind ripples on Mars: A record of atmospheric evolution.

Wind blowing over sand on Earth produces decimeter-wavelength ripples and hundred-meter- to kilometer-wavelength dunes: bedforms of two distinct size modes. Observations from the Mars Science Laboratory Curiosity rover and the Mars Reconnaissance Orbiter reveal that Mars hosts a third stable wind-driven bedform, with meter-scale wavelengths. These bedforms are spatially uniform in size and typically have asymmetric profiles with angle-of-repose lee slopes and sinuous crest lines, making them unlike terrestrial wind ripples. Rather, these structures resemble fluid-drag ripples, which on Earth include water-worked current ripples, but on Mars instead form by wind because of the higher kinematic viscosity of the low-density atmosphere. A reevaluation of the wind-deposited strata in the Burns formation (about 3.7 billion years old or younger) identifies potential wind-drag ripple stratification formed under a thin atmosphere.

Deposition, exhumation, and paleoclimate of an ancient lake deposit, Gale crater, Mars.

The landforms of northern Gale crater on Mars expose thick sequences of sedimentary rocks. Based on images obtained by the Curiosity rover, we interpret these outcrops as evidence for past fluvial, deltaic, and lacustrine environments. Degradation of the crater wall and rim probably supplied these sediments, which advanced inward from the wall, infilling both the crater and an internal lake basin to a thickness of at least 75 meters. This intracrater lake system probably existed intermittently for thousands to millions of years, implying a relatively wet climate that supplied moisture to the crater rim and transported sediment via streams into the lake basin. The deposits in Gale crater were then exhumed, probably by wind-driven erosion, creating Aeolis Mons (Mount Sharp).

Development of a new technique for recovery of cytokines from inflammatory sites in situ.

We attempted to recover cytokines from nasal mucosal surface following allergen challenge. Repeated lavage of nasal mucosa of seven allergic patients was done, but we failed to detect IL-1 beta in the lavage samples even in ten-fold concentrated materials. Therefore, we developed a new technique to recover cytokines using filter strips. Small filter strips were placed on nasal turbinates for 10 min at different time points after allergen challenge. The strips were air-dried, and stored. For recovery of cytokines individual strips were washed with small volumes of Hepes buffer containing 0.3% human serum albumin. Eluates were assayed for the presence of IL-1 beta and GM-CSF using commercially available ELISA. We were able to detect IL-1 beta and GM-CSF in eluates. Both cytokines were consistently detectable in the late phase allergic reaction peaking at 5 h. Nasal challenge with saline failed to detect any cytokine during the 7 h observation period. In standardization experiments known quantities of IL-1 beta and GM-CSF were applied to filter strips and the recovery ranged from 67 to 89%. Thus, we developed a simple technique of recovery of cytokines from inflammatory mucosa in situ.

Purification of human basophils. Their response to anti-IgE.

Although usually the least prevalent blood leukocyte, the basophil can release potent soluble factors in response to multiple triggers. We purified basophils from normal volunteers by means of isopycnic centrifugation and affinity binding of mononuclear cells. The majority of the basophils from most subjects were recovered in a band formed between Percoll layers with densities of 1.070 and 1.080; at this stage basophils represented a mean of 22% of total leukocytes. These cells were reacted with monoclonal antibodies to T (OKT-11) and B (anti-HLA-DR) lymphocytes; B and T cells were removed by adsorption to insoluble antibodies against mouse immunoglobulin resulting in a mean purity of 75% basophils with a yield of 54%. These highly enriched basophils resembled unpurified basophils in terms of (1) intracellular histamine content, (2) spontaneous release of histamine in buffer, and (3) percentage of histamine released by anti-IgE. These findings suggest that the techniques used to purify the basophils do not affect the functional integrity of human basophils.

Hereditary angioedema: its diagnostic and management perspectives.

Although hereditary angioedema accounts for only a small fraction of all cases of angioedema, it is the most common genetically linked clinical disorder caused by the deficiency of a protein associated with complement activation. Attacks may be complicated by incapacitating cutaneous swelling, life-threatening upper airway impediment, and severe gastrointestinal colic. Recent physicochemical and genetic studies have contributed significantly to our understanding of the structure of the inhibitor protein. Measurement of serum C4 titer is an efficacious screening test. Normal levels during symptomatic periods rule out the diagnosis, whereas decreased levels warrant determination of C1 esterase inhibitor titer by immunoassay or functional assay. The functional assay is necessary to ascertain the genetic variant form. The importance of making the correct diagnosis cannot be overemphasized. It can avert potentially fatal consequences, such as upper airway obstruction and unnecessary abdominal surgery. The application of short-term preventive measures can avoid complications associated with trauma. Finally, abatement or elimination of symptoms in patients with incessant and disabling attacks can be attained by long-term therapy with currently available attenuated androgens.

Anaphylactic reactions following infusion of factor VIII in a patient with classic hemophilia.

A 28 year old white man with hemophilia A had, for several years, been successfully maintained on a home care program utilizing self-administration of factor VIII concentrates, but one such infusion resulted in severe anaphylaxis. An immunoglobulin E (IgE)-mediated hypersensitivity response was demonstrated by (1) the release of histamine from the patient's basophils in vitro upon challenge with several different lots of factor VIII concentrate; (2) immediate cutaneous response to commercial factor VIII, factor IX and cryoprecipitate; and (3) measurement of IgE antibodies against a commercial factor VIII preparation. A subsequent life-threatening hemorrhage required cautious infusion of another commercial lot of factor VIII concentrate. Despite pretreatment with antiallergic drugs and attempted desensitization, a moderately severe anaphylactic reaction was observed.

Interaction of selective alpha-adrenoceptor agonists and antagonists with human and rabbit blood platelets.

1 The selectivity of alpha-adrenoceptors mediating the pro-aggregatory response of human and rabbit platelets to adrenaline and the conditions required to permit expression of an aggregatory response to partial agonists at these alpha-adrenoceptors have been studied.2 Yohimbine causes effective blockade of the pro-aggregatory responses whereas indoramin and prazosin are ineffective.3 The clonidine analogue, UK-14304, is nearly as effective as adrenaline in inducing an aggregatory response in human platelets and a pro-aggregatory response in rabbit platelets. Cross-tachyphylaxis between adrenaline and UK-14304 has been demonstrated.4 Clonidine is a weak agonist for the pro-aggregatory response of rabbit platelets and in some donors for the aggregatory response of human platelets.5 Methoxamine induces a pro-aggregatory response in human platelets which is blocked by indoramin or prazosin but not by yohimbine. No such response to methoxamine is observed in rabbit platelets.6 The divalent cation ionophore, A-23187, induces an aggregatory response to clonidine (in platelets from a non-responsive donor), phenylephrine and methoxamine in human platelets and to adrenaline, UK-14304 and clonidine in rabbit platelets. A secretory response to clonidine is also induced by A-23187 in human platelets.7 The adenylate cyclase inhibitor, SQ-22536, is ineffective in either inducing a response to the alpha-agonists or potentiating the effect of A-23187.8 The aggregatory responses to adrenaline and UK-14304 in rabbit platelets and to clonidine in human and rabbit platelets, which can be induced by A-23187, are blocked by yohimbine but not by prazosin or indoramin.9 From these studies we conclude that the pro-aggregatory responses of human and rabbit platelets to adrenaline are mediated primarily by alpha(2)-adrenoceptors. The presence of alpha(1)-adrenoceptors on human platelets is confirmed but these receptors do not appear to be present on rabbit platelets. The conditions required for expression of an aggregatory response to partial agonists at the human and rabbit platelet alpha-adrenoceptors implicate an increase in cytosolic Ca(2+) concentration as a key event in stimulus-response coupling but do not indicate such a role for depression of cyclic adenosine-3',5'-monophosphate concentration.

Victor Darwin Lespinasse: a biographical sketch.

The first neuroendoscopic procedure was performed before 1913 by Victor Darwin Lespinasse, a Chicago urologist. He never reported it, thinking it to be "an intern's stunt." He achieved a measure of fame for his advocacy of testicular transplantation.

Monstrous, crablike hypertrophy of the cerebellar vermis and its relationship with Lhermitte-Duclos disease. Case report.

The case of an infant with a peculiar tumorous malformation of the cerebellum is described. The tumor apparently developed as an exophytic, hypertrophic sprout of the inferior vermis. It had a monstrous appearance resembling a crab, with a metameric body and multiple pairs of limbs attached to the folia of both cerebellar hemispheres. Histologically, the lesion was formed by poorly differentiated neuroepithelial cells without any evidence of organization into nuclei, cortex, or fascicles. Clinically, the tumor behaved in indolent manner and did not regrow after subtotal surgical resection. Because of its gross appearance and its biological behavior, this unusual hamartoblastomatous growth is readily distinguished from medulloblastoma. The morphology of the cerebellum in Lhermitte-Duclos disease is reviewed, and a new interpretation of its basic structure is proposed. This and other known types of cerebellar hypertrophy are different from the malformation in the present case.

Sjögren's syndrome presenting with hypereosinophilia, lymphopenia and circulating immune complexes.

Although mild peripheral eosinophilia is a common finding in Sjögren's syndrome (SS), severe eosinophilia with a clinical picture simulating hypereosinophilic syndrome is extremely rare. We report a 24 year old male with SS presenting with swelling of the parotid glands, redness and irritation of the eyes, polyarthralgias and polyarthritis, weight loss, exertional dyspnea, malaise, erythematous and urticarial skin lesions and enlarged lymph nodes. Laboratory tests showed hypereosinophilia (34%, total 3800/mm3), lymphopenia (2%, total 220/mm3), a positive RA factor (1:2560) and decreased C3 and C4. Biopsy of an enlarged submaxillary gland was consistent with SS. A Schirmer test showed decreased tear production. Salivary glands showed a marked decrease in uptake of radioactive (Tc99) dye. Circulating immune complexes (CIC) were markedly elevated by both C1q binding and Raji cell assays. T-cell subsets showed OKT3 = 63%, OKT4 = 32% and OKT8 = 16%. "Histamine trap" in vivo test for CIC revealed fluorescence in upper dermal blood vessels with IgM, C1q, C3 and fibrin. Biopsies of the liver, bone marrow and skin revealed eosinophilic infiltration. A notable response to therapy with high doses of corticosteroids was seen with recurrence of symptoms and laboratory abnormalities after the therapy was stopped. In conclusion, we present a case of SS which is remarkable for the age and sex of the patient, extreme hypereosinophilia, marked lymphopenia, and CIC.