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Primary production was measured from 1992-2010 in western Massachusetts Bay and Boston Harbor as part of the Massachusetts Water Resource Authority’s outfall monitoring program. In 2003, annual primary production rates decreased by 221-279 g C m-2 year-1 in both systems, with decreased rates continuing through 2010. Oceanographic and meteorological variables were analyzed with production rates to determine if concurrent changes in the environment were responsible for the reduced primary production rates in Massachusetts Bay. Zooplankton abundances and benthic flux rates were compared with production rates as well to determine if the decreased production rates had cascading effects on the ecosystem. Based on a constructed conceptual model, results indicated that larger influxes of low saline water derived from the western Maine Coastal Current (WMCC) from 2003-2010 may have been responsible for the reduced production rates. Increased river discharge (particularly the Merrimack River) and intrusion of Labrador Subarctic Slope Water into the Gulf of Maine appear to have freshened the WMCC in recent years. More northeasterly winds over the last several years were favorable in penetrating WMCC waters into Massachusetts Bay. The correlations between primary production and stratification and surface salinities suggested an impact of the WMCC on production rates. I hypothesized in a conceptual model that increased stratification resulted in decreased vertical mixing and nutrient concentrations in the surface waters for phytoplankton growth, but there were no significant correlations between nutrient availability and stratification in available data. While the Massachusetts Bay primary production rates were influenced by changes in oceanography, rates in Boston Harbor were a result of nutrient removal from the Boston Harbor outfall diffuser relocation. Significant relationships between surface salinity and wind stress and river runoff in the Harbor suggests the system is mor

Item does not contain fulltext, IL-37, a newly described member of the IL-1 family, functions as a fundamental inhibitor of innate inflammation and immunity. In the present study, we examined a role for IL-37 during experimental colitis. A transgenic mouse strain was generated to express human IL-37 (hIL-37tg), and these mice were subjected to dextran sulfate sodium (DSS)-induced colitis. Despite the presence of a CMV promoter to drive expression of IL-37, mRNA transcripts were not present in colons at the resting state. Expression was observed only upon disruption of the epithelial barrier, with a six- to sevenfold increase (P = 0.02) on days 3 and 5 after continuous exposure to DSS. During the development of colitis, clinical disease scores were reduced by 50% (P < 0.001), and histological indices of colitis were one-third less in hIL-37tg mice compared with WT counterparts (P < 0.001). Reduced inflammation was associated with decreased leukocyte recruitment into the colonic lamina propria. In addition, release of IL-1beta and TNFalpha from ex vivo colonic explant tissue was decreased 5- and 13-fold, respectively, compared with WT (P

This chapter reviews the incidence of coverage of Papua New Guinea affairs in the Australian press and in Australian broadcast media. It presents the findings of a formal monitoring of selected newspaper coverage and news broadcasts of the leading Australian television and radio outlets. The study also includes news stories published on ABC Online. The findings for print media suggest that coverage of PNG is inadequate and may be contributing towards negative images of that country in Australia. The broadcast monitoring found also that beyond the ABC's regular and balanced coverage, there was very little mention of PNG on Australian airwaves. The deployment of resources by the ABC was seen as a potential model for increased quantity and quality of coverage, with its maintenance of a correspondent and office in the country, and use of reports from PNG across a wide range of programs. The investigation noted some early indications of a shift in media attention, following the election of a new government in Australia in 2007, which gave some priority attention to PNG including a visit by the then Prime Minister.

Author Posting. © American Geophysical Union, 2009. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 114 (2009): C12013, doi:10.1029/2009JC005623., During the upwelling season in central California, northwesterly winds along the coast produce a strong upwelling jet that originates at Point Año Nuevo and flows southward across the mouth of Monterey Bay. A convergent front with a mean temperature change of 3.77 ± 0.29°C develops between the warm interior waters and the cold offshore upwelling jet. To examine the forcing mechanisms driving the location and movement of the upwelling shadow front and its effects on biological communities in northern Monterey Bay, oceanographic conditions were monitored using cross-shelf mooring arrays, drifters, and hydrographic surveys along a 20 km stretch of coast extending northwestward from Santa Cruz, California, during the upwelling season of 2007 (May–September). The alongshore location of the upwelling shadow front at the northern edge of the bay was driven by: regional wind forcing, through an alongshore pressure gradient; buoyancy forces due to the temperature change across the front; and local wind forcing (the diurnal sea breeze). The upwelling shadow front behaved as a surface-trapped buoyant current, which is superimposed on a poleward barotropic current, moving up and down the coast up to several kilometers each day. We surmise that the front is advected poleward by a preexisting northward barotropic current of 0.10 m s−1 that arises due to an alongshore pressure gradient caused by focused upwelling at Point Año Nuevo. The frontal circulation (onshore surface currents) breaks the typical two-dimensional wind-driven, cross-shelf circulation (offshore surface currents) and introduces another way for water, and the material it contains (e.g., pollutants, larvae), to go across the shelf toward shore., Funded primarily by the Gordon and Betty Moore Foundation and the David and Lucile Packard Foundation.

The biological and physical processes contributing to planktonic thin layer dynamics were examined in a multidisciplinary study conducted in East Sound, Washington, USA between June 10 and June 25, 1998. The temporal and spatial scales characteristic of thin layers were determined using a nested sampling strategy utilizing 4 major types of platforms: (1) an array of 3 moored acoustical instrument packages and 2 moored optical instrument packages that recorded distributions and intensities of thin layers; (2) additional stationary instrumentation deployed outside the array comprised of meteorological stations, wave-tide gauges, and thermistor chains; (3) a research vessel anchored 150 m outside the western edge of the array; (4) 2 mobile vessels performing basin-wide surveys to define the spatial extent of thin layers and the physical hydrography of the Sound. We observed numerous occurrences of thin layers that contained locally enhanced concentrations of material; many of the layers persisted for intervals of several hours to a few days. More than one persistent thin layer may be present at any one time, and these spatially distinct thin layers often contain distinct plankton assemblages. The results suggest that the species or populations comprising each distinct thin layer have responded to different sets of biological and/or physical processes. The existence and persistence of planktonic thin layers generates extensive biological heterogeneity in the water column and may be important in maintaining species diversity and overall community structure.