993 resultados para Bricker, John W. (John William), 1893-1986.


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The feasibility of establishment of continuously proliferating growth factor-dependent human B lymphocytes was investigated. Normal B lymphocytes prepared from peripheral venous blood were stimulated with a variety of known polyclonal B cell activators, in the continuous presence of various cytokine preparations. Continuously proliferating growth factor-dependent B cell populations were obtained from cultures activated with either insoluble anti-IgM ((mu)-chain specific), soluble anti-IgM, heat-killed Staphylococcus aureus Cowen I (SAC), or dextran sulphate (DxS), in the continuous presence of exogenously added growth factor preparations containing either IL-1, IL-2 and BCGF, or BCGF alone. Although growth factor-dependent B cell lines were obtained via all three methods of activation, the correlation of mode of activation and growth factor preparation proved to be critical. B cell lines could not be established with anti-(mu) activation in the presence of only BCGF; however, B cell lines were successfully obtained with SAC or DxS activation from those cultures continuously replenished with only BCGF. These cultured B lymphocyte populations were routinely maintained in logarithmic-phase growth in the presence of exogenously added growth factor, and exhibited a population doubling time of approximately 36 hours. They were shown to specifically absorb BCGF, suggesting the presence of membrane receptors for it. Also, these cultured B cells have been utilized for the development of a microassay for the assessment of a M(,r) 12,000-14,000 B cell growth factor activity that is accurate, sensitive, and precise. The pronounced sensitivity of this bioassay beyond that of the conventional peripheral blood B cell assay has aided in the purification to homogeneity of natural product extracellular BCGF (EC-BCGF), and in the determination of the nucleotide sequence for a gene coding for a protein exhibiting BCGF activity. Additionally, these B cell lines specifically absorb, and proliferate in the presence of, an affinity-purified M(,r) 60,000 trypsin-sensitive intracellular protein derived from freshly isolated human T lymphocytes, providing evidence for a putative intracellular precursor of EC-BCGF, or a novel high molecular weight BCGF species. ^

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Samples from the upper portion of a cyclic pelagic carbonate sediment sequence in Deep-Sea Drilling Project (DSDP) hole 503B (4.0°N, 95.6°W) are the first group to be analyzed for paleoceanographic and paleoclimatic proxy-indicators of ice volume, deep ocean and surface water circulation, and atmospheric circulation in order to resolve the complex origin of the cyclicity. Temporal resolution is taken from the delta18O time scale, most other parameters are calculated in terms of their mass flux to the seafloor. CaCO3 percent in the sediments fluctuates in the well-known Pacific pattern and is higher during glacial times. The fluxes of opal and organic carbon have patterns similar to each other and show a variability of a factor of 2.5 to 4. The longer organic carbon record shows flux maxima during both glacial and interglacial times. The accumulation patterns of both opal and organic carbon suggest that the variability in surface water productivity and/or seafloor preservation of those materials is not simply correlated to glacial or interglacial periods. Eolian dust fluxes are greater during interglacial periods by factors of 2 to 5, indicating that eolian source regions in central and northern South America were more arid during interglacial periods. The record of eolian grain size provides a semiquantitative estimation of the intensity of the transporting winds. The eolian data suggest more intense atmospheric circulation during interglacial periods, opposite to the anticipated results. We interpret this observation as recording the southerly shift of the intertropical convergence zone to the latitude of hole 503B during glaciations.

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From early in the AIDS epidemic, psychosocial stressors have been proposed as contributors to the variation in disease course. To test this hypothesis, rhesus macaques were assigned to stable or unstable social conditions and were inoculated with the simian immunodeficiency virus. Animals in the unstable condition displayed more agonism and less affiliation, shorter survival, and lower basal concentrations of plasma cortisol compared with stable animals. Early after inoculation, but before the emergence of group differences in cortisol levels, animals receiving social threats had higher concentrations of simian immunodeficiency virus RNA in plasma, and those engaging in affiliation had lower concentrations. The results indicate that social factors can have a significant impact on the course of immunodeficiency disease. Socially induced changes in pituitary–adrenal hormones may be one mechanism mediating this relationship.

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This small blue-covered paper notebook contains four leaves with the handwritten records of the Geographical Society, an undergraduate organization at Harvard in the late 1790s. The records consist of ten handwritten "Laws of the Geographical Society" and a short list of fines dispensed on October 7th. A list of six student surnames is written on a scrap of paper and attached with pins to the notebook's inside front cover. The surnames likely correspond to six members of the Harvard Class of 1798: John Abbot (1777-1854), Isaac Adams (d. 1807), Francis Brigham (d. November 14, 1796), Humphrey Devereux (1779-1867), Joseph Emerson (1777-1833), and Artemas Sawyer (d. 1826). The notebook is undated but was presumably kept in 1795 or 1796 around the time of Brigham's death on November 14, 1796. While Brigham's surname appears in the list of fines, it is crossed out on the inside front cover.

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We present a 5.3-Myr stack (the ''LR04'' stack) of benthic d18O records from 57 globally distributed sites aligned by an automated graphic correlation algorithm. This is the first benthic delta18O stack composed of more than three records to extend beyond 850 ka, and we use its improved signal quality to identify 24 new marine isotope stages in the early Pliocene. We also present a new LR04 age model for the Pliocene-Pleistocene derived from tuning the delta18O stack to a simple ice model based on 21 June insolation at 65 N. Stacked sedimentation rates provide additional age model constraints to prevent overtuning. Despite a conservative tuning strategy, the LR04 benthic stack exhibits significant coherency with insolation in the obliquity band throughout the entire 5.3 Myr and in the precession band for more than half of the record. The LR04 stack contains significantly more variance in benthic delta18O than previously published stacks of the late Pleistocene as the result of higher resolution records, a better alignment technique, and a greater percentage of records from the Atlantic. Finally, the relative phases of the stack's 41- and 23-kyr components suggest that the precession component of delta18O from 2.7-1.6 Ma is primarily a deep-water temperature signal and that the phase of d18O precession response changed suddenly at 1.6 Ma.

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Another ed. issued simultaneously, with flexible cloth binding (12mo), in series: English classics.

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Mode of access: Internet.