Oligocene and Neogene radiolarians from the Labrador Sea

Two sites in the Labrador Sea and one site in Baffin Bay were drilled during Leg 105. Radiolarians were recovered at all three sites, although at Site 645 (Baffin Bay), radiolarians were present in useful numbers only in the mudline sample. Radiolarians of late Neogene age were recovered at Site 646 south of Greenland, while early Oligocene and early Miocene radiolarians were recovered from the Labrador Sea at Site 647. In Site 646, radiolarian and other coarse-fraction abundances vary dramatically from sample to sample and may reflect deep-water depositional processes as well as changes in surface-water conditions. Site 647 siliceous microfossils reach their peak abundance and preservation in Core 105-647A-25R and decline gradually upward into the lower Miocene (Cores 105-647A-13R and -14R). Siliceous microfossil abundances in counts of the > 38-µm Carbonate-free coarse fraction from the siliceous interval are correlated to each other, but not to the abundance of nonbiogenic coarse-fraction components. Radiolarian abundances in specimens per gram (but not diatom abundances) are correlated to bulk opal concentration and to the organic carbon content of the sediment. The abundance of radiolarians and other siliceous microfossils within the lower Oligocene to lower Miocene is interpreted as reflecting changes in surface-water productivity. With only a few exceptions, no stratigraphic indicator species were seen in samples from either Site 646 or Site 647. The absence of both tropical/subtropical and Norwegian-Greenland Sea stratigraphic forms is due to the dominance of subarctic North Atlantic taxa in Leg 105 assemblages. The early Oligocene and early Miocene assemblages recovered at Site 647 are of particular interest, as very little material of these ages has previously been recovered from the subarctic North Atlantic region, and virtually no descriptive work has been conducted on the more endemic components of the radiolarian assemblages from these time intervals. Thus, this report concentrates on providing, at least in part, the first comprehensive documentation of early Oligocene and early Miocene radiolarians from the subarctic North Atlantic, with emphasis on basic descriptions, measurements, and photographic documentation. However, synonymic work and formal designation of new species names has been deferred until additional material from other regions can be examined. The sole exception is the emendation of Theocalyptra tetracantha Bjorklund and Kellogg 1972 to Cycladophora tetracantha n. comb.

Revised Cenozoic hiatus database

The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of unconformities in the world's oceans. I identified temporal and depth patterns of hiatuses ("hiatus events") from a large and chronologically well constrained stratigraphic database of deep-sea sediments. The Paleogene is characterized by few, several million year long hiatuses. The most significant Cenozoic hiatus event spans most of the Paleocene. The Neogene is characterized by short, frequent hiatus events nearly synchronous in shallow and deep water sediments. Epoch boundaries are characterized by peaks in deep water hiatuses possibly caused by an increased circulation of corrosive bottom water and sediment dissolution. The Plio-Pleistocene is characterized by a gradual decrease in the frequency of hiatuses. Future studies will focus on the regional significance of the hiatus events and their possible causes.

Nd isotopes an geochemistry of bulk deep sea sediments of the Atlantic Ocean

Nd isotopes preserved in fossil fish teeth and ferromanganese crusts have become a common tool for tracking variations in water mass composition and circulation through time. Studies of Nd isotopes extracted from Pleistocene to Holocene bulk sediments using hydroxylamine hydrochloride (HH) solution yield high resolution records of Nd isotopes that can be interpreted in terms of deep water circulation, but concerns about diagenesis and potential contamination of the seawater signal limit application of this technique to geologically young samples. In this study we demonstrate that Nd extracted from the > 63 µm, decarbonated fraction of older Ocean Drilling Program (ODP) sediments using a 0.02 M HH solution produces Nd isotopic ratios that are within error of values from cleaned fossil fish teeth collected from the same samples, indicating that the HH-extractions are robust recorders of deep sea Nd isotopes. This excellent correlation was achieved for 94 paired fish teeth and HH-extraction samples ranging in age from the Miocene to Cretaceous, distributed throughout the north, tropical and south Atlantic, and composed of a range of lithologies including carbonate-rich oozes/chalks and black shales. The strong Nd signal recovered from Cretaceous anoxic black shale sequences is unlikely to be associated with ferromanganese oxide coatings, but may be derived from abundant phosphatic fish teeth and debris or organic matter in these samples. In contrast to the deep water Nd isotopic signal, Sr isotopes from HH-extractions are often offset from seawater values, suggesting that evaluation of Sr isotopes is a conservative test for the integrity of Nd isotopes in the HH fraction. However, rare earth elements (REE) from the HH-extractions and fish teeth produce distinctive middle REE bulge patterns that may prove useful for evaluating whether the Nd isotopic signal represents uncontaminated seawater. Alternatively, a few paired HH-extraction and cleaned fish teeth samples from each site of interest can be used to verify the seawater composition of the HH-extractions. The similarity between isotopic values for the HH-extraction and fish teeth illustrates that the extensive cleaning protocol applied to fish teeth samples is not necessary in typical, carbonate-rich, deep sea sediments.

Injury bulletin 105 : skateboard injury

Summary of findings: QISU estimates that approximately 1,000 skateboard-associated injuries are seen at emergency departments each year in Queensland. 10-14 year old males are the most likely group to present to a QISU ED with a skateboard related injury. The peak time for skateboard injuries to occur is on the weekend and in the late afternoon. Only 19% of skateboard injuries occur at skate park facilities, with the remainder oc-curring in non-skate parks, on roads and footpaths. Risk factors associated with more severe injuries are, age less than 10 years and involvement in a motor vehicle crash The most common types of injuries are fractures and sprains of the upper limbs. Isolated head injuries represent approximately 5% of skateboarding injuries, but 60% of serious injuries requiring resuscitation. These injuries may be minimized or pre-vented with helmet use.

Caracterización molecular de 105 accesiones de cacao(Theobroma Cacao L.) utilizando 10 marcadores moleculares tipo SSR en INTA-CNIAB, Nicaragua, 2011

Se realizó la caracterización molecular de 105 accesiones de Cacao que contemplan 79 colectas nacionales, 21 híbridos de referencia y 5 materiales criollo referencia , congregados en 8 grupos de acuerdo a su ubicación geográfica al momento de la colecta; utilizando 10 marcadores moleculares tipo SSR con el fin de conocer la divers idad genética de Cacao colectado en finca de productores nicaragüenses . Se utilizó el método de extracción de ADN C TAB - Buffer, Amplificación de fragmentos de ADN mediante la técnica PCR , visualización de fragmentos de ADN en cámara electroforesis. Se identificaron 183 alelos en las 105 ac cesiones con una media de 18.3, los rangos de Heterosigocidad observada y esperada resultaron mayores para MTcCIR12 con 0.437 y 0.81 respectivamente ; el CIP y el Índice de Shannon proporcionaron los mayores valores para MTcCIR12 con 0.96 y 1.94 respectivamente . La media general del CIP e Índice de Shannon para todos los locus es de 0.87 y 1.37 respectivamente; e l análisis molecular de varianza reveló que las diferencias genéticas dentro de los grupos (85%) es mayor que las diferencias entre grupos (15%) ; se realizó el dendograma basado en las distancia de Nei’s donde revela diferencias m ínimas entre los grupos , la mayor relación genética son entre los grupos RSJ y Carazo ; en cambio para el grupo Carazo e Hibrido referencia se encontraron las mayores diferencias. E n el PCA se encontró materiales colectados que resultaron genéticamente pare cidos a los criollo s referencias, es el caso de RSJ 0211, RSJ 0 311, RSJ 0511, Bomat0510, Ji0210 ; los materiales Ji - Cuá 0104 y RSJ0411 están estrechamente relacionado . Se demostró que existe una alta diversidad genética y que existen materiales promisorios para posteriores estudios de mejora genética

Código de processo civil : Lei nº 13.105, de 16 de março de 2015

Lei nº 13.105, de 16 de março de 2015, que institui o Código de Processo Civil Brasileiro.

Cytological aspects of gonadotropic cells and pre-opticoneurohypophysial neurosecretion during the ovarian cycle of Eudontomyzon danfordi. [Translation from: Studia Univ.Babes-Bolyai, Biologia 18 105-113, 1973.]

The connection between the activity of the gonadotropic cells of the hypophysis and the neurosecretion in the pre-optico neuro-hypophysial system in different groups of vertebrates has been examined by many authors. It has been established that in many species there exists some kind of synchronism between the sexual cycle and the cellular activity of neurosecretion, a fact that has led to the prevailing idea that gonadotropic activity in the hypophysis is regulated by the hypothalamus. This paper summarises the results of experiments made in this direction on Cyclostomata. The materials for research came from adult individuals of Eudontomyson danfordi Regan taken from the rivers Somes-Rece and Ivo (Harghita district) at different times of the year.

Z=105质量数为259的新同位素的合成和鉴别(英文)

利用 1 2 0MeV的2 2 Ne离子束轰击2 41　Am靶 ,通过2 41　Am(2 2 Ne ,4n) 2 5 9　Db反应合成了一个Z =1 0 5,质量数为 2 59的新同位素 .反应产物是用氦喷嘴技术和转动轮装置传输收集的 .借助一系列金硅面垒探测器探测到了反应产物及其子核的α衰变 .新同位素的原子序数Z和质量数A是借助该同位素和已知的2 5 5 　Lr核之间的遗传关系得到了确定的鉴别 .新同位素2 5 9　Db的测量半衰期为 (0 51± 0 1 6)s;它的α粒子能量为 9 4 7MeV .由本实验导出的2 5 9　Db的Qα 值同理论预言结果能够较好地符合