Radiolarian assemblages of the late Neogene North Pacific

Radiolarian census and abundance data were collected from three deep-sea cores drilled by the Ocean Drilling Program Sites 884, 887 and 1151 to investigate patterns of ecologic changes in space and time during the last 16 million years for the mid-latitude to subarctic North Pacific. High concentrations of radiolarians occurred between 9.0 and 2.7 Ma. Radiolarian species richness was highest in the early middle Miocene at each site and gradually decreased up to about 7 Ma, coinciding with a well-established global cooling trend. A degree of overlap index calculated for radiolarian assemblages revealed 11 faunal change events, of which 8 corresponded to global cooling events and expansions of polar ice sheets. Three of the faunal change events were observed within the peak of radiolarian accumulation rate and were ascribed to changes in primary productivity in the North Pacific rather than global climatic changes. Our assemblage analyses revealed that north-south differentiation in radiolarian assemblages in the northwestern Pacific has existed since 16 Ma and became more distinct via major steps at 6.8 Ma and 2.7 Ma, coinciding with major glaciation events, and that east-west faunal contrasts in the subarctic region became obvious beginning at 11.7 Ma and changed to a different mode around 6.8 Ma. The observed east-west faunal differences possibly reflect east to west climate differences that were characterized by cooler temperatures in the east than the west during the late Miocene (11.7-6.8 Ma) and then by the opposite temperature trend (6.8 Ma-Recent). A severe glaciation at 2.7 Ma played a large role, particularly in temporal changes in radiolarian accumulation rate and assemblage composition.

Early Cenozoic Atlantic and Pacific benthic foraminiferal isotopes from 12 sites

Oxygen and carbon isotope records are important tools used to reconstruct past ocean and climate conditions, with those of benthic foraminifera providing information on the deep oceans. Reconstructions are complicated by interspecies isotopic offsets that result from microhabitat preferences (carbonate precipitation in isotopically distinct environments) and vital effects (species-specific metabolic variation in isotopic fractionation). We provide correction factors for early Cenozoic benthic foraminifera commonly used for isotopic measurements (Cibicidoides spp., Nuttallides truempyi, Oridorsalis spp., Stensioina beccariiformis, Hanzawaia ammophila, and Bulimina spp.), showing that most yield reliable isotopic proxies of environmental change. The statistical methods and larger data sets used in this study provide more robust correction factors than do previous studies. Interspecies isotopic offsets appear to have changed through the Cenozoic, either (1) as a result of evolutionary changes or (2) as an artifact of different statistical methods and data set sizes used to determine the offsets in different studies. Regardless of the reason, the assumption that isotopic offsets have remained constant through the Cenozoic has introduced an 1-2°C uncertainty into deep sea paleotemperature calculations. In addition, we compare multiple species isotopic data from a western North Atlantic section that includes the Paleocene-Eocene thermal maximum to determine the most reliable isotopic indicator for this event. We propose that Oridorsalis spp. was the most reliable deepwater isotopic recorder at this location because it was best able to withstand the harsh water conditions that existed at this time; it may be the best recorder at other locations and for other extreme events also.

Paleomagnetic of basalts from ODP Site 145-883 on Detroit Seamount

Paleomagnetic data were measured from basaltic flows cored by the Ocean Drilling Program (ODP) at Site 883 on the summit of Detroit Seamount, located in the northernmost Emperor seamounts. These data are important because they reflect the paleolatitude of Hawaiian volcanism for the Late Cretaceous and bear upon geodynamic models of hotspot drift. A total of 143 samples were measured, from cores acquired at two ~20-30 m apart. Most samples gave apparently reliable magnetic directions that were analyzed in a tiered fashion to compute a composite inclination vs. depth curve. One hole gave 13 distinct inclination groups, the other 10, and the two were combined into nine groups thought to represent independent measurements of paleofield direction. These data indicate normal magnetic polarity and give a mean inclination of 61.5+10.6°/-6.4° and paleolatitude of 42.8+13.2°/-7.6° (95% confidence limits). This paleolatitude is 6.2° higher than results from another ODP site (884) drilled on the lower flank of the same seamount. The difference is thought to result partly from an age difference (1-3 Myr) and partly from incomplete averaging of paleosecular variation at both drill sites. Together, the data from the two sites reinforce the conclusion that the northern Emperor seamounts were formed far north of the present-day hotspot latitude (~19.5°N) and suggest prior estimates of the amount and rate of southward drift may have been low. This analysis also illustrates uncertainties in determining paleolatitude from a small number of lava flow units from a single drill site.

Resolu????o simplificadora de formalidades e procedimentos relativos aos atos de que trata o art. 54 da Lei n?? 8.884 de 11 de junho 1994

O controle de ag??ncias de defesa da concorr??ncia sobre a estrutura dos mercados constitui pr??tica comum em pa??ses maduros e vem ganhando import??ncia crescente em economias emergentes. Tal atividade envolve exame de atos de concentra????o econ??mica tais como fus??es, aquisi????es, joint ventures ou incorpora????es. No Brasil este tipo de controle ?? recente, tendo sido institu??do pela Lei n?? 8.884, de junho de 1994. Desde ent??o, o Conselho Administrativo de Defesa da Concorr??ncia - CADE julgou 29 (vinte e nove) atos de concentra????o, em contraste com a experi??ncia secular de pa??ses como EUA, Canad?? e Austr??lia e de v??rias d??cadas nas na????es europ??ias depois da Segunda Guerra. A exemplo de v??rias outras ??reas de pol??tica p??blica, tornou-se imperativo agilizar os ??rg??os de defesa da concorr??ncia. Isto decorre, entre outros fatores, do intenso processo de reestrutura????o produtiva em curso no pa??s associados ?? desestatiza????o e abertura da economia. Diante das circunst??ncias descritas, ?? preciso assegurar agilidade, transpar??ncia, excel??ncia t??cnica no processo decis??rio e estabilidade de regras, todos ingredientes indispens??veis para gerar seguran??a jur??dica. Esta ??ltima, por seu turno, diminui o risco do investimento, estimulando invers??es, produ????o e emprego. Nesse sentido, o CADE promoveu mudan??as importantes no procedimento de an??lise de atos de concentra????o em colabora????o com a Secretaria de Direito Econ??mico do Minist??rio da Justi??a (SDE) e a Secretaria de Acompanhamento Econ??mico do Minist??rio da Fazenda (SEAE) mediante a edi????o da Resolu????o 5, de 28 de agosto de 1996

Presence of T 145 on cytolytic T cell lines and their lectin-resistant mutants.

Murine cytolytic T cell lines have been analyzed for the expression of two surface glycoproteins called T145 and T130. T145, known to be expressed by activated cytolytic T cells, is also expressed by such lines, but T130, which has been described by a universal T cell marker, is not. Our results suggest a structural relationship between T145 and T130. Vicia villosa lectin, which binds selectively to T145 of activated T cells and which is cytotoxic for cytolytic T cell lines, has been used to select lectin-resistant mutants from these lines. Five independent lectin-resistant mutants have been obtained. All of them are cytolytically active, bind up to 100-fold less lectin than the parental lines, but still express T145 or a closely related glycoprotein.