Terrestrial organic matter in marine sediments of the Central Equatorial Atlantic

Terrestrial organic matter (OM) in pelagic sediments is discussed with regard to depositional processes and land-sea interactions in the modern and past glacial/interglacial Equatorial Atlantic. Special emphasis is placed on a critical evaluation of different analytical approaches (C/N, Rock-Eval Pyrolysis, stable carbon isotopes, palynology, organic petrology, and selected biomarkers) which are currently used for the qualitative and quantitative assessment of terrigenous organic carbon. If binary mixing equations are used to calculate terrestrial and marine proportions of organic carbon, we consider the definition of endmember values to be most critical since these values may be biased by a great number of independent controls. A combination of geochemical methods including optical studies (organic petrology and palynology) is therefore suggested to evaluate each individual proxy. Organic geochemical analyses performed on sediments from the modern and Late Quaternary Equatorial Atlantic evidence fluctuations in eolian supply of terrigenous OM related to changes in intensity of the trade winds. Quantification of this organic fraction leads to differing proportions depending on the approach applied, i.e. the organic carbon isotopic composition or maceral analyses. Modern distribution of terrigenous OM reveals a decrease in supply towards the basin contributing less than a fifth of the total OM in pelagic areas. Organic geochemical data indicate that sedimentation in the modern northeastern Brasil Basin is affected by lateral advection of reworked OM probably from southern source areas. Glacial/interglacial deposits from the pelagic Equatorial Atlantic (ODP Site 663), covering isotopic stages 12 and 11, reveal that deposition of terrigenous OM was higher under past glacial conditions, in correspondence to generally enhanced dust fluxes. Proportions of terrigenous OM, however, never exceed 50% of the total OM according to maceral analyses. Other estimates, recently proposed by Verardo and Ruddiman (1996), are considered to be too high probably for analytical reasons. Palynological records in the Equatorial Atlantic parallel dust records. Increased portions of grass pollen suggest the admixture of C4-plant material under modern and past glacial conditions. It is therefore assumed, as one possible interpetation, that C4-plant debris has an effect on sedimentary d13Corg and might explain differences between isotopic and microscopic quantitative estimates. Using the difference between these two records, we calculate that maximum supply of C4-material remains below 20% of the total OM for the deep modern and past glacial/interglacial Equatorial Atlantic.

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

Organic carbon accumulation in the South Atlantic Ocean

A compilation of 1118 surface sediment samples from the South Atlantic was used to map modern seafloor distribution of organic carbon content in this ocean basin. Using new data on Holocene sedimentation rates, we estimated the annual organic carbon accumulation in the pelagic realm (>3000 m water depth) to be approximately 1.8*10**12 g C/year. In the sediments underlying the divergence zone in the Eastern Equatorial Atlantic (EEA), only small amounts of organic carbon accumulate in spite of the high surface water productivity observed in that area. This implies that in the Eastern Equatorial Atlantic, organic carbon accumulation is strongly reduced by efficient degradation of organic matter prior to its burial. During the Last Glacial Maximum (LGM), accumulation of organic carbon was higher than during the mid-Holocene along the continental margins of Africa and South America (Brazil) as well as in the equatorial region. In the Eastern Equatorial Atlantic in particular, large relative differences between LGM and mid-Holocene accumulation rates are found. This is probably to a great extent due to better preservation of organic matter related to changes in bottom water circulation and not just a result of strongly enhanced export productivity during the glacial period. On average, a two- to three-fold increase in organic carbon accumulation during the LGM compared to mid-Holocene conditions can be deduced from our cores. However, for the deep-sea sediments this cannot be solely attributed to a glacial productivity increase, as changes in South Atlantic deep-water circulation seem to result in better organic carbon preservation during the LGM.

Diário da Constituinte [gravação de vídeo] : [programa n. 159]

Está pronto o calendário das sessões extraordinárias para o debate dos temas polêmicos da Assembleia Nacional Constituinte. O Deputado Bocayuva Cunha (PDT-RJ) espera a participação popular e que a sociedade possa acompanhar a posição dos partidos e dos constituintes em relação aos temas a serem debatidos. O PT quer discutir mais os temas sociais. O Deputado Vladimir Palmeiras (PT-RJ) declara que a bancada terá uma intervenção mais sistemática no Plenário, no sentido de afirmar que a redução da jornada de trabalho e a estabilidade no emprego são pontos essenciais para discussão do texto constitucional. Reunião do Grupo Interpartidário, com representantes do PMDB, PT, PDT, PCB e PFL, buscam o consenso. O Deputado Antonio Brito (PMDB-RS) afirma que a sabedoria de uma Constituinte é tentar estabelecer o que o país tem em comum, para criar uma Constituição duradoura. Na reunião interpartidária, os constituintes debateram os artigos do anteprojeto que tratam da censura, da criação de um conselho de comunicação social e da reforma agrária e definiram dezenove pontos em torno dos quais buscarão uma posição de consenso nas votações em Plenário. O Deputado Roberto Freire (PCB-PE) destaca a importância do diálogo entre os partidos. O Deputado Mário Covas (PMDB-SP) declara que há uma preocupação comum que é a de ter uma Constituição que reflita os anseios da sociedade brasileira. O Deputado Plínio Arruda Sampaio (PT-SP) afirma que há uma intenção dos grupos progressistas de comporem uma grande aliança para que esta Constituição represente um avanço. O Deputado Alceni Guerra (PFL-PR) defende que a Constituição deve representar o que pensa a sociedade brasileira e deve também ser flexível, para que tanto um governo de esquerda como um de direita possa governar o país. O Deputado Antonio Brito (PMDB-RS) ressalta que, pela primeira vez, os partidos estão negociando e que é isto o que deve ser uma Constituinte. Dom Luciano Mendes, Presidente da Confederação Nacional dos Bispos do Brasil (CNBB), entrega três emendas populares ao Presidente da Assembleia Nacional Constituinte (ANC) Ulysses Guimarães . Dom Luciano ressalta a importância das emendas populares.

The transport of aquatic animals by birds. [Translation from: Binnengewaesser 18, 156-159, 1950.]

A great deal has been written on the part which birds play in the dispersal of freshwater fauna. This article summarises literature on the dispersal of aquatic animals by birds and aquatic insects.

中能区~(40)Ar + ~(197)Au/~(159)Tb/~(nat)Ag反应中高激发热核性质研究

通过对中能区Ar+Au/Tb/Ag反应中高激发核的发射时标、发射次序、发射机制、核温度、集体运动等衰变特性的研究，提取了轻粒子和中等质量碎片（IMF）的发射时间，IMF发射时间随束流能的升高而变短，发射机制逐渐由相继衰变过渡至多重碎裂。研究了轻粒子和碎片间的发射次序，对高能粒子和碎片，轻粒子先于碎片发射，而低能时，则为碎片先于轻粒子发射。IMF发射成分与角度和碰撞参数有关，前角区来自于弹核碎裂，后角区来自于类靶热核的蒸发。在平面和出平面研究表明，中速粒子和碎片为在平面发射占主导，即存在类转动效应；对轻粒子，转动效应随粒子质量增加而增加；对中速产物均观测到该效应随碰撞参数饿增大而增大。采用几种不同的方法提取了热核的核温度，研究了不同方法之间的区别。

Resolución No. 159: por la cual se resuelve una revocatoria directa en el registro de las entidades sin ánimo de lucro

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Resolución N° 159 ¿La inscripción de cuotas cedidas que al momento de inscripción se encontraban embargadas, se puede revocar sin el consentimiento del beneficiario de las mismas en en virtud de la cesión?

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