993 resultados para Smith, Joseph Brown, 1823-1859.


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Las mujeres han debido atravesar un largo camino partiendo de la discriminación hasta empezar un proceso de equidad en la sociedad y en el deporte, de esta manera llegar a ser parte de un evento como los Juegos Olímpicos. Esta tesis toma el caso de tres atletas colombianas y describe su proceso de formación para lograr dos medallas de oro para el país.

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Despite increasing empirical data to the contrary, it continues to be claimed that morphosyntax and face processing skills of people with Williams syndrome are intact, This purported intactness, which coexists with mental retardation, is used to bolster claims about innately specified, independently functioning modules, as if the atypically developing brain were simply a normal brain with parts intact and parts impaired. Yet this is highly unlikely, given the dynamics of brain development and the fact that in a genetic microdeletion syndrome the brain is developing differently from the moment of conception, throughout embryogenesis, and during postnatal brain growth. In this article, we challenge the intactness assumptions, using evidence from a wide variety of studies of toddlers, children, and adults with Williams syndrome.

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welche der Landrichter Stecher im Jahre 1821 eingeführt hat, von ihm selbst hrsg.

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Malaria during the first pregnancy causes a high rate of fetal and neonatal death. The decreasing susceptibility during subsequent pregnancies correlates with acquisition of antibodies that block binding of infected red cells to chondroitin sulfate A (CSA), a receptor for parasites in the placenta. Here we identify a domain within a particular Plasmodium falciparum erythrocyte membrane protein 1 that binds CSA. We cloned a var gene expressed in CSA-binding parasitized red blood cells (PRBCs). The gene had eight receptor-like domains, each of which was expressed on the surface of Chinese hamster ovary cells and was tested for CSA binding. CSA linked to biotin used as a probe demonstrated that two Duffy-binding-like (DBL) domains (DBL3 and DBL7) bound CSA. DBL7, but not DBL3, also bound chondroitin sulfate C (CSC) linked to biotin, a negatively charged sugar that does not support PRBC adhesion. Furthermore, CSA, but not CSC, blocked the interaction with DBL3; both CSA and CSC blocked binding to DBL7. Thus, only the DBL3 domain displays the same binding specificity as PRBCs. Because protective antibodies present after pregnancy block binding to CSA of parasites from different parts of the world, DBL-3, although variant, may induce cross-reactive immunity that will protect pregnant women and their fetuses.

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The crystal structure of raite was solved and refined from data collected at Beamline Insertion Device 13 at the European Synchrotron Radiation Facility, using a 3 × 3 × 65 μm single crystal. The refined lattice constants of the monoclinic unit cell are a = 15.1(1) Å; b = 17.6(1) Å; c = 5.290(4) Å; β = 100.5(2)°; space group C2/m. The structure, including all reflections, refined to a final R = 0.07. Raite occurs in hyperalkaline rocks from the Kola peninsula, Russia. The structure consists of alternating layers of a hexagonal chicken-wire pattern of 6-membered SiO4 rings. Tetrahedral apices of a chain of Si six-rings, parallel to the c-axis, alternate in pointing up and down. Two six-ring Si layers are connected by edge-sharing octahedral bands of Na+ and Mn3+ also parallel to c. The band consists of the alternation of finite Mn–Mn and Na–Mn–Na chains. As a consequence of the misfit between octahedral and tetrahedral elements, regions of the Si–O layers are arched and form one-dimensional channels bounded by 12 Si tetrahedra and 2 Na octahedra. The channels along the short c-axis in raite are filled by isolated Na(OH,H2O)6 octahedra. The distorted octahedrally coordinated Ti4+ also resides in the channel and provides the weak linkage of these isolated Na octahedra and the mixed octahedral tetrahedral framework. Raite is structurally related to intersilite, palygorskite, sepiolite, and amphibole.

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Binding of infected erythrocytes to brain venules is a central pathogenic event in the lethal malaria disease complication, cerebral malaria. The only parasite adhesion trait linked to cerebral sequestration is binding to intercellular adhesion molecule-1 (ICAM-1). In this report, we show that Plasmodium falciparum erythrocyte membrane protein 1 (PfEMP1) binds ICAM-1. We have cloned and expressed PfEMP1 recombinant proteins from the A4tres parasite. Using heterologous expression in mammalian cells, the minimal ICAM-1 binding domain was a complex domain consisting of the second Duffy binding-like (DBL) domain and the C2 domain. Constructs that contained either domain alone did not bind ICAM-1. Based on phylogenetic criteria, there are five distinct PfEMP1 DBL types designated α, β, γ, δ, and ɛ. The DBL domain from the A4tres that binds ICAM-1 is DBLβ type. A PfEMP1 cloned from a distinct ICAM-1 binding variant, the A4 parasite, contains a DBLβ domain and a C2 domain in tandem arrangement similar to the A4tres PfEMP1. Anti-PfEMP1 antisera implicate the DBLβ domain from A4var PfEMP1 in ICAM-1 adhesion. The identification of a P. falciparum ICAM-1 binding domain may clarify mechanisms responsible for the pathogenesis of cerebral malaria and lead to interventions or vaccines that reduce malarial disease.

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Mineral surfaces were important during the emergence of life on Earth because the assembly of the necessary complex biomolecules by random collisions in dilute aqueous solutions is implausible. Most silicate mineral surfaces are hydrophilic and organophobic and unsuitable for catalytic reactions, but some silica-rich surfaces of partly dealuminated feldspars and zeolites are organophilic and potentially catalytic. Weathered alkali feldspar crystals from granitic rocks at Shap, north west England, contain abundant tubular etch pits, typically 0.4–0.6 μm wide, forming an orthogonal honeycomb network in a surface zone 50 μm thick, with 2–3 × 106 intersections per mm2 of crystal surface. Surviving metamorphic rocks demonstrate that granites and acidic surface water were present on the Earth’s surface by ∼3.8 Ga. By analogy with Shap granite, honeycombed feldspar has considerable potential as a natural catalytic surface for the start of biochemical evolution. Biomolecules should have become available by catalysis of amino acids, etc. The honeycomb would have provided access to various mineral inclusions in the feldspar, particularly apatite and oxides, which contain phosphorus and transition metals necessary for energetic life. The organized environment would have protected complex molecules from dispersion into dilute solutions, from hydrolysis, and from UV radiation. Sub-micrometer tubes in the honeycomb might have acted as rudimentary cell walls for proto-organisms, which ultimately evolved a lipid lid giving further shelter from the hostile outside environment. A lid would finally have become a complete cell wall permitting detachment and flotation in primordial “soup.” Etch features on weathered alkali feldspar from Shap match the shape of overlying soil bacteria.

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Catalysis at organophilic silica-rich surfaces of zeolites and feldspars might generate replicating biopolymers from simple chemicals supplied by meteorites, volcanic gases, and other geological sources. Crystal–chemical modeling yielded packings for amino acids neatly encapsulated in 10-ring channels of the molecular sieve silicalite-ZSM-5-(mutinaite). Calculation of binding and activation energies for catalytic assembly into polymers is progressing for a chemical composition with one catalytic Al–OH site per 25 neutral Si tetrahedral sites. Internal channel intersections and external terminations provide special stereochemical features suitable for complex organic species. Polymer migration along nano/micrometer channels of ancient weathered feldspars, plus exploitation of phosphorus and various transition metals in entrapped apatite and other microminerals, might have generated complexes of replicating catalytic biomolecules, leading to primitive cellular organisms. The first cell wall might have been an internal mineral surface, from which the cell developed a protective biological cap emerging into a nutrient-rich “soup.” Ultimately, the biological cap might have expanded into a complete cell wall, allowing mobility and colonization of energy-rich challenging environments. Electron microscopy of honeycomb channels inside weathered feldspars of the Shap granite (northwest England) has revealed modern bacteria, perhaps indicative of Archean ones. All known early rocks were metamorphosed too highly during geologic time to permit simple survival of large-pore zeolites, honeycombed feldspar, and encapsulated species. Possible microscopic clues to the proposed mineral adsorbents/catalysts are discussed for planning of systematic study of black cherts from weakly metamorphosed Archaean sediments.

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Contains a record of cases before magistrate William Pynchon from 1639 to 1650. Notes are continued by his son, John, from 1652 to 1701. Included also are a record of marriages (1665-1702), a list of freemen, and a record of freemen meetings (1660-1696).

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Deed of sale in fee simple absolute of land in Boston to Abigail Brightman.

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Back Row: Chris Grieves, Bob Franks, Gregg Willner, Dave Goldwaithe, Mark Slaughter, John Mandich, Pat Watts, James Blue, Nick Labun, Tony Woodford, C. Newhof, Jeff Lawley

9th Row: Steve Knickerbocker, Kyron Williams, Stacy Johnson, John Weisenburger, Bob Hollway, Chip Pederson, Dale Keitz, Tim Malinak, Leon Richardson, Rock Lindsay, Lewis Smith, Woody Brown

8th Row: Scott Smith, Mark Braman, Bob Patek, Jon Giesler, Mark Torzy, Curtis Greer, William Jackson, Jerry Meter, Rick Leach, Dave Stavale, Tom Melita

7th Row: Mike Smith, Tom Seabron, Mark DeSantis, Frank Bell, Harlan Huckleby, Gene Johnson, Mark Schmerge, Russell Davis, John Arbeznik, Andy Jackson, Dennis Richardson

6th Row: Joe Holland, Steve Nauta, Kevin King, Max Richardson, Dave Harding, Mike Kenn, Dominic Tedesco, Jim Pickens, Ray Johnson, Phil Brown, Ken Bush, Roger Bettis

5th Row: Roger Szafranski, Dwight Hicks, Scott Corbin, Mark Donahue, Bill Dufek, Rex Mackall, John Anderson, Derek Howard, Greg Bartnick, Walt Downing, Terry Stefan, Asst. Coach Bill McCartney

4th Row: Asst. Coach Paul Schudel, Curt Stephenson, Rob Carian, Phil Andrews, Eric Phelps, Steve Graves, Gerry Szara, Jim Hackett, Pete Traber, Steve Anderson, Bob Wood, Darrell Truitt, Phil Brumbaugh, Asst. Coach Jack Harbaugh

3rd Row: Asst. Coach Gary Moeller, Asst. Coach Tom Reed, Asst. Coach Jed Hughes, Jerry Zuver, Rick White, Jim Hall, Mike Strabley, Jerry Vogele, Jim Smith, Rob Lytle, John Hennessy, Bob Lang, Jim Bolden, John Ceddia, A. Miller, Asst. Coach Dennis Brown

2nd Row: Asst. Coach Tirrel Burton, Asst. Coach Jerry Hanlon, Greg Morton, Tom Jensen, George Przygodski, Mike Holmes, Co-Captain Kirk Lewis, Jeff Perlinger, Steve King, Dan Jilek, Jim Czirr, Bill Hoban, Calvin O'Neal, Chuck Randolph, Asst. Coach Chuck Stobart

Front Row: Mark Elzinga, Jerry Collins, Kurt Kampe, Rick Koschalk, Dave Devich, Co-captain Gordon Bell, Co-Captain Don Dufek, Tim Davis, Keith Johnson, Les Miles, Dave Whiteford, Greg Strinko, Head Coach Bo Schembechler