PeECE III - Pelagic Ecosystem CO2 Enrichment Study, Raunefjord, Bergen, Norway, 2005

The effects of CO2-induced seawater acidification on plankton communities were also addressed in a series of 3 mesocosm experiments, called the Pelagic Ecosystem CO2 Enrichment (PeECE I-III) studies, which were conducted in the Large-Scale Mesocosm Facilities of the University of Bergen, Norway in 2001, 2003 and 2005, respectively. Each experiment consisted of 9 mesocosms, in which CO2 was manipulated to initial concentrations of 190, 350 and 750 µatm in 2001 and 2003, and 350, 700 and 1050 µatm in 2005. The present dataset concerns PeECE III.

Mammalian karyopherin alpha 1 beta and alpha 2 beta heterodimers: alpha 1 or alpha 2 subunit binds nuclear localization signal and beta subunit interacts with peptide repeat-containing nucleoporins.

Although only 44% identical to human karyopherin alpha 1, human karyopherin alpha 2 (Rch1 protein) substituted for human karyopherin alpha 1 (hSRP-1/NPI-1) in recognizing a standard nuclear localization sequence and karyopherin beta-dependent targeting to the nuclear envelope of digitonin-permeabilized cells. By immunofluorescence microscopy of methanol-fixed cells, karyopherin beta was localized to the cytoplasm and the nuclear envelope and was absent from the nuclear interior. Digitonin permeabilization of buffalo rat liver cells depleted their endogenous karyopherin beta. Recombinant karyopherin beta can bind directly to the nuclear envelope of digitonin-permeabilized cells at 0 degree C (docking reaction). In contrast, recombinant karyopherin alpha 1 or alpha 2 did not bind unless karyopherin beta was present. Likewise, in an import reaction (at 20 degrees C) with all recombinant transport factors (karyopherin alpha 1 or alpha 2, karyopherin beta, Ran, and p10) import depended on karyopherin beta. Localization of the exogenously added transport factors after a 30-min import reaction showed karyopherin beta at the nuclear envelope and karyopherin alpha 1 or alpha 2, Ran, and p10 in the nuclear interior. In an overlay assay with SDS/PAGE-resolved and nitrocellulose-transferred proteins of the nuclear envelope, 35S-labeled karyopherin beta bound to at least four peptide repeat-containing nucleoporins--Nup358, Nup214, Nup153, and Nup98.

Utilização de metanol, etanol e metano como doadores de elétrons para a desnitrificação

Esta tese apresenta e discute os dados obtidos a partir de trabalho experimental projetado para avaliar comparativamente o desempenho de reatores desnitrificantes em batelada, tendo etanol, metanol e gás metano como doadores de elétrons. Os experimentos foram realizados em reatores em escala de bancada. Os ensaios com gás metano objetivaram verificar a efetividade deste sub-produto de reatores anaeróbios em substituir os doadores exógenos de elétrons comumente utilizados, tais como metanol e etanol. Para alcançar o objetivo principal deste trabalho, os parâmetros cinéticos de desnitrificação, para os doadores de elétrons ensaiados, foram determinados nas diferentes condições operacionais. Além disso, as alterações ocorridas na população microbiana, ao longo do período experimental, foram avaliadas em relação à diversidade microbiana, por meio de análises microscópicas (óptica, de fluorescência e eletrônica de varredura) e da técnica de Biologia Molecular de PCR/DGGE. A completa desnitrificação foi alcançada para todos os compostos testados, e o etanol foi o doador de elétrons mais eficiente para a desnitrificação. A melhor razão carbono-nitrogênio para a desnitrificação foi igual a 1,0. Contudo, este parâmetro foi encontrado ser inadequado para utilização no processo de desnitrificação, uma vez que não expressa a capacidade real do composto usado em doar elétrons. A desnitrificação com metano ocorreu tanto na presença como na ausência de oxigênio, embora a baixas velocidades quando comparado com os outros compostos. No entanto, a configuração do reator utilizado neste estudo não foi adequada para promover a efetiva dissolução do gás metano na fase líquida. Por essa razão, sugere-se o desenvolvimento de configurações de reatores apropriadas para minimizar as resistências à transferência de massa da fase gasosa para a líquida e também desta para a biomassa.

Table 1. Radiocarbon dates from TPC522 and box core surface samples from BC521 and BC523

Recent intensification of wind-driven upwelling of warm upper circumpolar deep water (UCDW) has been linked to accelerated melting of West Antarctic ice shelves and glaciers. To better assess the long term relationship between UCDWupwelling and the stability of theWest Antarctic Ice Sheet, we present a multi-proxy reconstruction of surface and bottom water conditions in Marguerite Bay, West Antarctic Peninsula (WAP), through the Holocene. A combination of sedimentological, diatom and foraminiferal records are, for the first time, presented together to infer a decline in UCDW influence within Marguerite Bay through the early to mid Holocene and the dominance of cyclic forcing in the late Holocene. Extensive glacial melt, limited sea ice and enhanced primary productivity between 9.7 and 7.0 ka BP is considered to be most consistent with persistent incursions of UCDW through Marguerite Trough. From 7.0 ka BP sea ice seasons increased and productivity decreased, suggesting that UCDW influence within Marguerite Bay waned, coincident with the equatorward migration of the Southern Hemisphere Westerly Winds (SWW). UCDW influence continued through the mid Holocene, and by 4.2 ka BP lengthy sea ice seasons persisted within Marguerite Bay. Intermittent melting and reforming of this sea ice within the late Holocene may be indicative of episodic incursions of UCDW into Marguerite Bay during this period. The cyclical changes in the oceanography within Marguerite Bay during the late Holocene is consistent with enhanced sensitively to ENSO forcing as opposed to the SWW-forcing that appears to have dominated the early to mid Holocene. Current measurements of the oceanography of the WAP continental shelf suggest that the system has now returned to the early Holocene-like oceanographic configuration reported here, which in both cases has been associated with rapid deglaciation.

Michigan Union tap room

Irving Kane and Allen B. Pond, architects. Plans for the Union were on a scale unknown at the time for "club houses" in American colleges and universities: 250 feet long and 200 feet wide. Construction began in 1916 and owing to war time difficulties was not ready to be used by students until 1919. Two new wings to the south were completed in 1936 and 1938. Another addition was begun 1954-55. Verso: 7636 MICHIGAN UNION BLDG., University of Mich., Ann Arbor Facing for stean table in tap room. Magnesium Oxycholride tiles, in buff red and blue laid in 1937. Substitute following caption for above: Michigan Union Bldg., University of Mich., Ann Arbor Facing for steam table of tap room of magnesium oxychloride in buff and brown with color inserts of red, green yelloe, blue , purple and gold. On image: 7636

Michigan Stadium Construction 1927

[Steam Shovels of R.C. Merriam Co. dig the first trench]