Expression regulation of AP -2 gamma gene

AP-2γ is a member of the AP-2 transcription factor family, is highly enriched in the trophoblast cell lineage, and is essential for placenta development. In an effort to identify factors regulating AP-2γ gene expression we isolated and characterized the promoter and 5′ flanking region of the mouse and human AP-2γ genes. The transcription start site of the mouse AP-2γ gene was mapped by primer extension and 5′ RACE. Transient gene transfer studies showed that basal promoter activity resides within a highly conserved ∼200 by DNA sequence located immediately upstream of the transcription start site. The conserved region is highly GC-rich and lacks typical TATA or CCAAT boxes. Multiple potential Sp and AP-2 binding sites are clustered within this region. Electrophoretic mobility shift assays demonstrated that Sp1 and Sp3 bind to three sites in the promoter region of the mouse AP-2γ gene. Combined mutation of the three putative Sp sites reduced promoter activity by 80% in trophoblast and non-trophoblast cells, demonstrating the functional importance of these sites in AP-2γ gene expression. ^ Mutational analysis of the 5′-flanking region revealed a 117-bp positive regulatory region of the mouse AP-2γ gene located between −5700 and −5583 upstream of the transcription start site. This 117-bp positive regulatory element provided approximately 7-fold enhancement of reporter gene expression in cultured trophoblast cells. A C/EBP-Sp1 transcription factor-binding module is located in this DNA sequence. Electrophoretic mobility shift assays demonstrated that transcription factors Sp1, Sp3 and C/EBP bind to the enhancer element. Mutation of each protein-binding site reduced the enhanced expression significantly. Mutagenesis assays showed that two other protein-binding sites also contribute to the enhancer activity. In summary, we have shown that Sp1 and Sp3 bind to cis-regulatory elements located in the promoter region and contribute to basal promoter activity. We have identified a 117-bp positive regulatory element of AP-2γ gene, and we have shown that Sp and C/EBP proteins bind to the cis -regulatory elements and contribute to the enhanced gene expression. ^

Megabenthic communities in the waters around Svalbard during POLARSTERN cruise ARK-VIII/2 (EPOS II)

Composition and distribution of megabenthic communities around Svalbard were investigated in June/July 1991 with 20 Agassiz trawl and 5 bottom trawl hauls in depths between 100 and 2100 m. About 370 species, ranging from sponges to fish, were identified in the catches. Species numbers per station ranged from 21 to 86. Brittle stars, such as Ophiacantha bidentata, Ophiura sarsi and Ophiocten sericeum, were most important in terms of constancy and relative abundance in the catches. Other prominent faunal elements were eunephthyid alcyonarians, bivalves, shrimps, sea stars and fish (Gadidae, Zoarcidae, Cottidae). Multivariate analyses of the species and environmental data sets showed that the spatial distribution of the megabenthos was characterized by a pronounced depth zonation: abyssal, bathyal, off-shore shelf and fjordic communities were discriminated. However, a gradient in sediment properties, especially the organic carbon content, seemed to superimpose on the bathymetric pattern. Both main factors are interpreted as proxies of the average food availability, which is, hence, suggested to have the strongest influence in structuring megabenthic communities off Svalbard.

Establecimiento y desarrollo en el cultivo forzado de tomate : efecto de fitorreguladores

El proceso de fructificación y desarrollo en tomate puede ser inducido naturalmente por polinización o partenocarpia y artificialmente por aplicación de reguladores; esta respuesta es variable según tipo y dosis de hormona, momento de aplicación y cultivar involucrado. El objetivo de este trabajo fue evaluar la capacidad de auxinas y giberelinas para inducir el desarrollo partenocárpico en genotipos de crecimiento indeterminado. Como factores se consideraron tipo de regulador -AG3 y β-NOA- en dosis fija, momento de aplicación -0, 5, 12, 19, 26 dpa- y genotipo -Rutgers, Fortaleza F1 y Colt 45-. Las mejores respuestas a nivel de porcentaje de fructificación y peso fresco se obtuvieron con β-NOA en comparación con AG3. Considerando todos los factores analizados, solamente la aplicación de β-NOA a 5 dpa permitió alcanzar porcentajes de fructificación y tamaño final de frutos similares a los obtenidos por autopolinización. El período de sensibilidad y el tamaño final de los frutos presentaron interacción con las variables genotipo, momento de aplicación y tipo de regulador. Se observó además que AG3 provocó un escaso desarrollo placentario y ausencia de óvulos mientras que β-NOA indujo un desarrollo de placentas y óvulos similar al de los frutos obtenidos por autopolinización.

Practice advisory: interim guidance for care of obstetric patients during a zika virus outbreak

Zika during pregnancy has been associated with birth defects, specifically significant microcephaly. Transmission of Zika to the fetus has been documented in all trimesters; Zika virus RNA has been detected in fetal tissue from early missed abortions, amniotic fluid, term neonates and the placenta. However, much is not yet known about Zika virus in pregnancy. Uncertainties include the incidence of Zika virus infection among pregnant women in areas of Zika virus transmission, the rate of vertical transmission and the rate with which infected fetuses manifest complications such as microcephaly or demise. The absence of this important information makes management and decision making in the setting of potential Zika virus exposure (i.e. travel to endemic areas) or maternal infection, difficult. Currently, there is no vaccine or treatment for this infection.

Pollen and diatom analysis on varved sediments in Lake Jues (Harz Mountains, Germany)

Studies combining sedimentological and biological evidence to reconstruct Holocene climate beyond the major changes, and especially seasonality, are rare in Europe, and are nearly completely absent in Germany. The present study tries to reconstruct changes of seasonality from evidence of annual algal successions within the framework of well-established pollen zonation and 14C-AMS dates from terrestrial plants. Laminated Holocene sediments in Lake Jues (10°20.70' E, 51°39.30' N, 241 m a.s.l.), located at the SW margin of the Harz Mountains, central Germany, were studied for sediment characteristics, pollen, diatoms and coccal green algae. An age model is based on 21 calibrated AMS radiocarbon dates from terrestrial plants. The sedimentary record covers the entire Holocene period. Trophic status and circulation/stagnation patterns of the lake were inferred from algal assemblages, the subannual structure of varves and the physico-chemical properties of the sediment. During the Holocene, mixing conditions alternated between di-, oligo- and meromictic depending on length and variability of spring and fall periods, and the stability of winter and summer weather. The trophic state was controlled by nutrient input, circulation patterns and the temperature-dependent rates of organic production and mineralization. Climate shifts, mainly in phase with those recorded from other European regions, are inferred from changing limnological conditions and terrestrial vegetation. Significant changes occurred at 11,600 cal. yr. BP (Preboreal warming), between 10,600 and 10,100 cal. yr. BP (Boreal cooling), and between 8,400 and 4,550 cal. yr. BP (warm and dry interval of the Atlantic). Since 4,550 cal. yr. BP the climate became gradually cooler, wetter and more oceanic. This trend was interrupted by warmer and dryer phases between 3,440 and 2,850 cal. yr. BP and, likely, between 2,500 and 2,250 cal. yr. BP.

Miocene foraminiferal, bolboformid, dinoflagellate and diatom age calibrations for the northeastern North Atlantic

This study presents a new Miocene biostratigraphic synthesis for the high-latitude northeastern North Atlantic region. Via correlations to the bio-magnetostratigraphy and oxygen isotope records of Ocean Drilling Program and Deep Sea Drilling Project Sites, the ages of shallower North Sea deposits have been better constrained. The result has been an improved precision and documentation of the age designations of the existing North Sea foraminiferal zonal boundaries of King (1989) and Gradstein and Bäckström (1996). All calibrations have been updated to the Astronomically Tuned Neogene Time Scale (ATNTS) of Lourens et al. (2004). This improved Miocene biozonation has been achieved through: the updating of age calibrations for key microfossil bioevents, identification of new events, and integration of new biostratigraphic data from a foraminiferal analysis of commercial wells in the North Sea and Norwegian Sea. The new zonation has been successfully applied to two commercial wells and an onshore research borehole. At these high latitudes, where standard zonal markers are often absent, integration of microfossil groups significantly improves temporal resolution. The new zonation comprises 11 Nordic Miocene (NM) Zones with an average duration of 1 to 2 million years. This multi-group combination of a total of 92 bioevents (70 foraminifers and bolboformids; 16 dinoflagellate cysts and acritarchs; 6 marine diatoms) facilitates zonal identification throughout the Nordic Atlantic region. With the highest proportion of events being of calcareous walled microfossils, this zonation is primarily suited to micropaleontologists. A correlation of this Miocene biostratigraphy with a re-calibrated oxygen isotope record for DSDP Site 608 suggests a strong correlation between Miocene planktonic microfossil turnover rates and the inferred paleoclimatic trends. Benthic foraminifera zonal boundaries appear to often coincide with Miocene global sequence boundaries. The biostratigraphic record is punctuated by four main stratigraphic hiati which show variation in their geographic and temporal extent. These are related to the following regional unconformities: basal Neogene, Lower/Middle Miocene ("mid-Miocene unconformity"), basal Upper Miocene and basal Messinian unconformities. Further coring of Neogene sections in the North Sea and Norwegian Sea may better constrain their extent and their effect on the biostratigraphic record.