Geochemistry of tetrapyrrole, tetraterpenoid, and perylene pigments in sediments from the Gulf of California

Results and discussion cover pigment analyses of 36 sediment samples recovered by Deep Sea Drilling Project Leg 64, and six samples from the Leg 64 site-survey cruise in the Guaymas Basin (Scripps Institution of Oceanography, Leg 3). Pigments investigated were tetrapyrroles, tetraterpenoids, and the PAH compound perylene. Traces of mixed nickel and copper ETIO-porphyrins were ubiquitous in all sediment samples, except for the very surface (i.e., <2 m sub-bottom), and their presence is taken as an indication of minor influxes of previously oxidized allochthonous (terrestrial) organic matter. Phorbides and chlorins isolated from Site 479 sediment samples (i.e., the oxygen-minimum locale, northeast of the Guaymas Basin) well represent the reductive diagenesis ("Treibs Scheme"; see Baker and Palmer, 1978; Treibs, 1936) of chlorophyll derivatives. Three forms of pheophytin-a, plus a variety of phorbides, were found to give rise to freebase porphyrins, nickel phylloerythrin, and nickel porphyrins, with increasing depth of burial (increasing temperature). Sediments from Sites 481, 10G, and 18G yielded chlorophyll derivatives characteristic of early oxidative alterations. Included among these pigments are allomerized pheophytin-a, purpurin-18, and chlorin-p6. The high thermal gradient imposed upon the late Quaternary sediments of Site 477 greatly accelerated chlorophyll diagenesis in the adjacent overlying sediments, that is, the production of large quantities of free-base desoxophylloerythroetioporphyrin (DPEP) occurred in a section (477-7-5) presently only 49.8 meters sub-bottom. Present depth and age of these sediments are such that only chlorins and phorbides would be expected. Carotenoid (i.e., tetraterpenoids) concentrations were found to decrease rapidly with increasing sub-bottom depth. Less deeply buried sediments (e.g., 0-30 m) yielded mixtures of carotenes and oxygen-substituted carotenoids. Oxygencontaining (oxy-, oxo-, epoxy-) carotenoids were found to be lost preferentially with increased depth of burial. Early carotenoid diagenesis is suggested as involving interacting reductions and dehydrations whereby dehydro-, didehydro-, and retro-carotenes are generated. Destruction of carotenoids as pigments may involve oxidative cleavage of the isoprenoid chain through epoxy intermediates, akin to changes in the senescent cells of plants. Perylene was found to be a common component of the extractable organic matter from all sediments investigated. The generation of alkyl perylenes was found to parallel increases in the existing thermal regime at all sites. Igneous sills and sill complexes within the sediment profile of Site 481 altered (i.e., scrambled) the otherwise straightforward thermally induced alkylation of perylene. The degree of perylene alkylation is proposed as an indicator of geothermal stress for non-contemporaneous marine sediments.

Hydrochemical Atlas of the Arctic Ocean

Introduction: Chemical composition of water determines its physical properties and character of processes proceeding in it: freezing temperature, volume of evaporation, density, color, transparency, filtration capacity, etc. Presence of chemical elements in water solution confers waters special physical properties exerting significant influence on their circulation, creates necessary conditions for development and inhabitance of flora and fauna, and imparts to the ocean waters some chemical features that radically differ them from the land waters (Alekin & Liakhin, 1984). Hydrochemical information helps to determine elements of water circulation, convection depth, makes it easier to distinguish water masses and gives additional knowledge of climatic variability of ocean conditions. Hydrochemical information is a necessary part of biological research. Water chemical composition can be the governing characteristics determining possibility and limits of use of marine objects, both stationary and moving in sea water. Subject of investigation of hydrochemistry is study of dynamics of chemical composition, i.e. processes of its formation and hydrochemical conditions of water bodies (Alekin & Liakhin 1984). The hydrochemical processes in the Arctic Ocean are the least known. Some information on these processes can be obtained in odd publications. A generalizing study of hydrochemical conditions in the Arctic Ocean based on expeditions conducted in the years 1948-1975 has been carried out by Rusanov et al. (1979). The "Atlas of the World Ocean: the Arctic Ocean" contains a special section "Hydrochemistry" (Gorshkov, 1980). Typical vertical profiles, transects and maps for different depths - 0, 100, 300, 500, 1000, 2000, 3000 m are given in this section for the following parameters: dissolved oxygen, phosphate, silicate, pH and alkaline-chlorine coefficient. The maps were constructed using the data of expeditions conducted in the years 1948-1975. The illustrations reflect main features of distribution of the hydrochemical elements for multi-year period and represent a static image of hydrochemical conditions. Distribution of the hydrochemical elements on the ocean surface is given for two seasons - winter and summer, for the other depths are given mean annual fields. Aim of the present Atlas is description of hydrochemical conditions in the Arctic Ocean on the basis of a greater body of hydrochemical information for the years 1948-2000 and using the up-to-date methods of analysis and electronic forms of presentation of hydrochemical information. The most wide-spread characteristics determined in water samples were used as hydrochemical indices. They are: dissolved oxygen, phosphate, silicate, pH, total alkalinity, nitrite and nitrate. An important characteristics of water salt composition - "salinity" has been considered in the Oceanographic Atlas of the Arctic Ocean (1997, 1998). Presentation of the hydrochemical characteristics in this Hydrochemical Atlas is wider if compared with that of the former Atlas (Gorshkov, 1980). Maps of climatic distribution of the hydrochemical elements were constructed for all the standard depths, and seasonal variability of the hydrochemical parameters is given not only for the surface, but also for the underlying standard depths up to 400 m and including. Statistical characteristics of the hydrochemical elements are given for the first time. Detailed accuracy estimates of initial data and map construction are also given in the Atlas. Calculated values of mean-root deviations, maximum and minimum values of the parameters demonstrate limits of their variability for the analyzed period of observations. Therefore, not only investigations of chemical statics are summarized in the Atlas, but also some elements of chemical dynamics are demonstrated. Digital arrays of the hydrochemical elements obtained in nodes of a regular grid are the new form of characteristics presentation in the Atlas. It should be mentioned that the same grid and the same boxes were used in the Atlas, as those that had been used by creation of the US-Russian climatic Oceanographic Atlas. It allows to combine hydrochemical and oceanographic information of these Atlases. The first block of the digital arrays contains climatic characteristics calculated using direct observational data. These climatic characteristics were not calculated in the regions without observations, and the information arrays for these regions have gaps. The other block of climatic information in a gridded form was obtained with the help of objective analysis of observational data. Procedure of the objective analysis allowed us to obtain climatic estimates of the hydrochemical characteristics for the whole water area of the Arctic Ocean including the regions not covered by observations. Data of the objective analysis can be widely used, in particular, in hydrobiological investigations and in modeling of hydrochemical conditions of the Arctic Ocean. Array of initial measurements is a separate block. It includes all the available materials of hydrochemical observations in the form, as they were presented in different sources. While keeping in mind that this array contains some amount of perverted information, the authors of the Atlas assumed it necessary to store this information in its primary form. Methods of data quality control can be developed in future in the process of hydrochemical information accumulation. It can be supposed that attitude can vary in future to the data that were rejected according to the procedure accepted in the Atlas. The hydrochemical Atlas of the Arctic Ocean is the first specialized and electronic generalization of hydrochemical observations in the Arctic Ocean and finishes the program of joint efforts of Russian and US specialists in preparation of a number of atlases for the Arctic. The published Oceanographic Atlas (1997, 1998), Atlas of Arctic Meteorology and Climate (2000), Ice Atlas of the Arctic Ocean prepared for publication and Hydrochemical Atlas of the Arctic Ocean represent a united series of fundamental generalizations of empirical knowledge of Arctic Ocean nature at climatic level. The Hydrochemical Atlas of the Arctic Ocean was elaborated in the result of joint efforts of the SRC of the RF AARI and IARC. Dr. Ye. Nikiforov was scientific supervisor of the Atlas, Dr. R. Colony was manager on behalf of the USA and Dr. L. Timokhov - on behalf of Russia.

Contribuição da consulta de enfermagem na adesão ao tratamento do diabetes mellitus na estratégia saúde da família do município de Ribeirão Preto, SP

Trata-se de estudo de intervenção tipo antes e depois, no qual o sujeito é seu próprio controle, fator que permite identificar os efeitos na adesão ao tratamento e controle dos níveis glicêmicos. Teve como objetivo avaliar a contribuição da consulta de enfermagem na adesão ao tratamento do diabetes mellitus tipo 2, em uma Unidade Saúde da Família, de acordo com o \"Protocolo de atendimento as pessoas com diabetes mellitus,\" em Ribeirão Preto, SP. A coleta de dados foi realizada no período de setembro de 2014 a janeiro de 2015. O trabalho foi aprovado pelo Comitê de Ética em Pesquisa da Escola de Enfermagem de Ribeirão Preto, SP, sob Parecer nº 648.970. Participaram 31 pessoas com diabetes mellitus, por meio de três consultas de enfermagem, na unidade de saúde e no domicílio, com intervalo de um mês entre as três consultas de todos os participantes. Foi utilizado um roteiro contendo variáveis sociodemográficos e clínicas e o teste de Medida de Adesão ao Tratamento. Para a análise da adesão, durante e após a intervenção, utilizou-se a estatística descritiva e o teste de Mann- Whitney; para a comparação do antes e após a intervenção, utilizou-se o teste de Wilcoxon; para análise de correlação com as variáveis numéricas, o coeficiente de correlação de Spearman e o teste Q de Cochran, para a comparação dos exames nos momentos anterior, durante e posterior à intervenção. Os resultados mostraram que os participantes tinham entre 33 e 79 anos, sendo 58,1% do sexo feminino; 71% tinham companheiro; renda familiar de 1 a 3 salários-mínimos (83,9%); 80,6% referiram ser profissionalmente inativos (aposentados, pensionistas ou do lar); média de 5,68 anos de estudo e predomínio de menos de 8 anos de estudo (67,7%). Em relação aos valores da pressão arterial sistêmica constatou hipertensão arterial sistêmica grau I em 25,8% das pessoas com diabetes mellitus, 90,3% com índice de massa corporal apresentando excesso de peso, quanto à circunferência abdominal, 32,2% dos homens estavam com valores maiores que 102 cm e 45,2% das mulheres com valores acima de 88 cm. A avaliação dos pés, com uso do monofilamento Semmes-Weinstein de 10g, apresentou 9,7% das pessoas com diabetes mellitus com pé em risco para ulceração e diminuição ou ausência de sensibilidade tátil pressórica protetora dos pés. O tempo de diagnóstico do diabetes mellitus tipo 2 variou entre 1 a 39 anos, predominando as comorbidades hipertensão arterial (83,9%), dislipidemia (58,1%) e obesidade (41,8%). Quanto aos exames laboratoriais, observa-se que, em 64,5% da população estudada, os níveis da glicemia de jejum estavam acima de 100 mg/dL , ocorrendo pequena redução para 61,3% nos casos de pessoas com diabetes mellitus durante a intervenção e se manteve após. No que se refere à glicemia pós-prandial, os casos das pessoas com diabetes mellitus com valores iguais ou acima de 160 mg/dL, antes da intervenção era de 45,2% e durante e após a intervenção caiu para 38,7%. Em contrapartida, aumentou o número de pessoas com diabetes mellitus durante e após a intervenção, com valores da glicemia pós-prandial abaixo de 160 mg/dL, de 54,8% para 61,3%. E, em relação à hemoglobina glicada, foi observado que em 61,3% das pessoas com diabetes mellitus os valores antes da intervenção eram iguais ou acima de 7%. Durante a intervenção, caiu para 19,3% e após a intervenção o número de pessoas com diabetes mellitus, com a hemoglobina glicada igual ou superior a 7%, chegou a 38,7%. Quanto aos valores abaixo de 7%, observou-se aumento de 38,7% antes da intervenção para 80,6 e 61,3% respectivamente, durante e após a intervenção, com diferença estatisticamente significante (p< 0,001). As pessoas com diabetes mellitus desse estudo, apresentaram 83,87% de adesão ao tratamento antes da intervenção, e esses escores subiram para 96,78% após a intervenção, fato corroborado pelo teste de Wilcoxon que mostrou escores estatisticamente significantes (p<0,001), entre antes e após a intervenção. Esse estudo contribui para ressaltar a importância do enfermeiro, enquanto integrante da equipe multiprofissional, seguindo as orientações do \"Protocolo de atendimento ao indivíduo com diabetes\", tanto no atendimento individual quanto em grupo, reorganizando o processo de trabalho, contribuindo para maior adesão ao tratamento e controle dos níveis glicêmicos, ao minimizar a fragmentação e assegurar a continuidade na assistência, por meio de abordagem integral ao diabético