2010
DOI: 10.1590/s0103-50532010001200019
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Geochemical markers as a tool to assess sedimentary organic matter sources of the Laguna Estuarine System, south Brazil: aliphatic and polycyclic aromatic hydrocarbons

Abstract: Amostras de sedimentos superficiais do Sistema Estuarino de Laguna foram analisadas objetivando a identificação das fontes de matéria orgânica. Razões entre n-alcanos selecionados, elevados teores de hidrocarbonetos alifáticos (HA) (média de 9.168 µg g -1 de carbono orgânico, CO) e policíclicos aromáticos (HPA) (média total de 426.593 ng g -1 CO), e a distribuição de hopanos com estereoquímica αβ detectados nas amostras da Lagoa de Santo Antônio foram evidências de que o aporte de hidrocarbonetos petrogênicos … Show more

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Cited by 28 publications
(12 citation statements)
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References 41 publications
(63 reference statements)
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“…The total concentrations of n-alkanes in sediments of Colony Z3 (Pelotas, RS, Brazil) were found to be 337.6 to 5,868.9 mg/kg (Sanches Filho et al, 2013). The concentrations of aliphatic hydrocarbons found in the Forcados River sediment were comparable to levels reported for Red Sea sediments but they were very much lower than those previously reported for some river sediments in the Niger Delta Fubara et al, 2012Fubara et al, , 2014Eguvbe et al, 2015) and in sediment systems of some other regions with high anthropogenic activities (Jeng and Huh, 2006;Gao et al, 2007;Jeng, 2007;Sakari et al, 2008aSakari et al, , 2008bCompanioni Damas et al, 2009;Tarozo et al, 2010;Bouzid et al, 2012;Sakari et al, 2012;Yusoff et al, 2012;Zrafi et al, 2013). n-C 11 had the highest concentration in the study area, as shown in Figure 2.…”
Section: Alkane Distribution and Characterizationsupporting
confidence: 70%
See 1 more Smart Citation
“…The total concentrations of n-alkanes in sediments of Colony Z3 (Pelotas, RS, Brazil) were found to be 337.6 to 5,868.9 mg/kg (Sanches Filho et al, 2013). The concentrations of aliphatic hydrocarbons found in the Forcados River sediment were comparable to levels reported for Red Sea sediments but they were very much lower than those previously reported for some river sediments in the Niger Delta Fubara et al, 2012Fubara et al, , 2014Eguvbe et al, 2015) and in sediment systems of some other regions with high anthropogenic activities (Jeng and Huh, 2006;Gao et al, 2007;Jeng, 2007;Sakari et al, 2008aSakari et al, , 2008bCompanioni Damas et al, 2009;Tarozo et al, 2010;Bouzid et al, 2012;Sakari et al, 2012;Yusoff et al, 2012;Zrafi et al, 2013). n-C 11 had the highest concentration in the study area, as shown in Figure 2.…”
Section: Alkane Distribution and Characterizationsupporting
confidence: 70%
“…In this study, the ratio of n-C 17 /pristane and n-C 18 /phytane ranged from 0.62 to 2.11 and 0.13 to 2.74 respectively. Since microorganisms generally utilize n-alkanes before isoprenoids as an energy source during biodegradation, low values for these ratios (less than 1) indicate biodegraded oils, while recent input may yield values greater than 1 (Tarozo et al, 2010). The n-C 17 /pristane and n-C 18 / phytane ratios of our sediment samples correspond to non-heavily degraded petroleum, i.e., recent inputs (Companioni Damas et al, 2009).…”
Section: Ratio Of C 31 /C 19mentioning
confidence: 96%
“…Variations within the weathered coal samples were evident, such as a hopene series present only in sample 6, and esters of palmitic (C16:0) and stearic (C18:0) acids in five of the samples (1, 4, 5, 7, and 9). The presence in sample 6 of 17α(H),21β(H)-homohopanes might indicate a high degree of geochemical maturity of this weathered coal [37,38]. However, since these indicator compounds typically originate from bacterial membrane lipids and were predominantly in the R,S-or α,βstereochemical configuration, any bacterial activity most likely occurred prior to transformation of hard coal to weathered coal.…”
Section: Pyrolysis Gc-msmentioning
confidence: 99%
“…6,7 Eles podem ser utilizados na caracterização da fonte e distribuição de MO, além fornecer informações a respeito de mudanças em paleoambientes marinho e continental. [8][9][10][11] A determinação de biomarcadores em amostras de perfis sedimentares envolve uma série de etapas, entre elas a extração com solvente, cleanup, fracionamento dos compostos, derivatização e concentração dos analitos para posterior analise cromatográfica. Em função do grande número de etapas envolvidas, é preciso garantir que as concentrações determinadas sejam representativas do sedimento, de forma a não comprometer os dados das análises.…”
Section: Introductionunclassified