THE ROLE OF B CELLS IN THE T CELL DEPENDENT RELEASE OF HUMAN B CELL GROWTH FACTOR

Quiescent human B cells are postulated to go through activation and proliferation phases before undergoing differentiative phase for immunoglobulin secretion. The present studies address some of the aspects of activation and proliferation phase of normal human B cells. The definitions of signals responsible for B cell activation and proliferation resulted in the development of a highly specific, reproducible B cell growth factor (BCGF) assay. This BCGF bioassay utilizes activation by rabbit anti-human IgM-antibody. The functional specificity of this assay for measuring BCGF activity was demonstrated by the finding that target B cells proliferated but did not differentiate. The factor specificity was determined by specific absorption of BCGF by anti-IgM activated B cells. This assay was utilized for the studies of T-B cell collaboration and the essential function of monocytes in the production and/or release of B cell growth factor in a syngeneic in vitro system. It is apparent that highly purified T cells are poor producers of BCGF by themselves and require monocytes to secrete significant quantities of BCGF upon PHA stimulation. Macrophage soluble factor, Interleukin 1, is capable of replacing monocyte function for the release of BCGF by activated T cells. In our studies, B cells are incapable to function as accessory cells to replace monocyte function. Normal B cells are also not capable of producing BCGF under our experimental observations. However, the addition of these B cells at an optimum cell density (T:B ratio 1:1) doubles the monocyte dependent release of BCGF by syngeneic T cells. The augmentative role of B cells is expanded to understand the mechanism of BCGF release by T cells. It is observed from our studies that DR antigen of B cell surface is involved in the release of BCGF. The functional difference between DR of B cells and monocytes is observed as IL-1 could replace DR-treated monocytes whereas failed to replace DR-treated B cells for the release of BCGF by T cells. This functional difference may be attributed to the reported microheterogeneity in DR of B cells and monocytes. The addition of irradiated B cells increased the monocyte dependent T cell proliferation, suggesting the increase of T cell pool for BCGF release. In summary, the development of a biological assay specific for B cell growth factor led to the delineation of an interesting role of B cells in the release of its own growth factor by T cells. . . . (Author's abstract exceeds stipulated maximum length. Discontinued here with permission of author.) UMI ^

Chemical composition of pumices from the Great Meteor Seamount

Two samples of pumice, obtained by trawling from depths of 3100 and 4300 m on the eastern slope of the Great Meteor Seamount in the Atlantic Ocean, have been examined. Their petrochemical composition has been studied. The pumice is probably a product of youthful explosive volcanism on the Azores, displaced southward by surface currents.

Sedimentation across the Great Barrier Reef

The continental margin off northeast Australia, comprising the Great Barrier Reef (GBR) platform and Queensland Trough, is the largest tropical mixed siliciclastic/carbonate depositional system in existence. We describe a suite of 35 piston cores and two Ocean Drilling Program (ODP) sites from a 130*240 km rectangular area of the Queensland Trough, the slope and basin setting east of the central GBR platform. Oxygen isotope records, physical property (magnetic susceptibility and greyscale) logs, analyses of bulk carbonate content and radiocarbon ages at these locations are used to construct a high resolution stratigraphy. This information is used to quantify mass accumulation rates (MARs) for siliciclastic and carbonate sediments accumulating in the Queensland Trough over the last 31,000 years. For the slope, highest MARs of siliciclastic sediment occur during transgression (1.0 Million Tonnes per year; MT/yr), and lowest MARs of siliciclastic (<0.1 MT/yr) and carbonate (0.2 MT/yr) sediment occur during sea level lowstand. Carbonate MARs are similar to siliciclastic MARs for transgression and highstand (1.1-1.4 MT/yr). In contrast, for the basin, MARs of siliciclastic (0-0.1 MT/yr) and carbonate sediment (0.2-0.4 MT/yr) are continuously low, and within a factor of two, for lowstand, transgression, and highstand. Generic models for carbonate margins predict that maximum and minimum carbonate MARs on the slope will occur during highstand and lowstand, respectively. Conversely, most models for siliciclastic margins suggest maximum and minimum siliciclastic MARs will occur during lowstand and transgression, respectively. Although carbonate MARs in the Queensland Trough are similar to those predicted for carbonate depositional systems, siliciclastic MARs are the opposite. Given uniform siliciclastic MARs in the basin through time, we conclude that terrigenous material is stored on the shelf during sea level lowstand, and released to the slope during transgression as wave driven currents transport shelf sediment offshore.

Cosmos : a sketch of a physical description of the universe / By Alexander von Humboldt ; Translated from the German by E.C. Otté.

3

Cosmos : a sketch of a physical description of the universe / By Alexander von Humboldt ; Translated from the German by E.C. Otté.

4

Cosmos : a sketch of a physical description of the universe / By Alexander von Humboldt ; Translated from the German by E.C. Otté.

2

Cosmos : a sketch of a physical description of the universe / By Alexander von Humboldt ; Translated from the German by E.C. Otté.

1

Cosmos : a sketch of a physical description of the universe / By Alexander von Humboldt ; Translated from the German by E.C. Otté.

5

Visualizing the dynamics of T cell activation: Intracellular adhesion molecule 1 migrates rapidly to the T cell/B cell interface and acts to sustain calcium levels

T cell recognition typically involves both the engagement of a specific T cell receptor with a peptide/major histocompatibility complex (MHC) and a number of accessory interactions. One of the most important interactions is between the integrin lymphocyte function-associated antigen 1 (LFA-1) on the T cell and intracellular adhesion molecule 1 (ICAM-1) on an antigen-presenting cell. By using fluorescence video microscopy and an ICAM-1 fused to a green fluorescent protein, we find that the elevation of intracellular calcium in the T cell that is characteristic of activation is followed almost immediately by the rapid accumulation of ICAM-1 on a B cell at a tight interface between the two cells. This increased density of ICAM-1 correlates with the sustained elevation of intracellular calcium in the T cell, known to be critical for activation. The use of peptide/MHC complexes and ICAM-1 on a supported lipid bilayer to stimulate T cells also indicates a major role for ICAM-1/LFA-1 in T cell activation but, surprisingly, not for adhesion, as even in the absence of ICAM-1 the morphological changes and adhesive characteristics of an activated T cell are seen in this system. We suggest that T cell antigen receptor-mediated recognition of a very small number of MHC/peptide complexes could trigger LFA-1/ICAM-1 clustering and avidity regulation, thus amplifying and stabilizing the production of second messengers.