2012
DOI: 10.4319/lom.2012.10.353
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Evaluation of electrophoretic protein extraction and database‐driven protein identification from marine sediments

Abstract: Intact proteins comprise a major component of organic carbon and nitrogen produced globally and are likely an important fraction of organic matter in sediments and soils. Extracting the protein component from sediments and soils for mass spectral characterization and identification represents a substantial challenge given the range of products and functionalities present in the complex matrix. Multiple forms of gel electrophoresis were evaluated as a means of enhancing recovery of sedimentary protein before pr… Show more

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Cited by 10 publications
(17 citation statements)
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“…The identification of algal peptides and proteins in the deep marine sediment core section demonstrates that gel electrophoresis can be an effective method for isolating proteins present in complex matrices, but further improvements can be made in the total recovery of material. The results obtained by loading sediment buffer mixture directly to the gel interface supports previous findings by Moore et al [16] that an electric field applied directly to sediment particles enhances protein extraction. The number of proteins identified was increased by running the gel for a longer period of time, allowing the ion front to move further down the gel (7 cm vs. 2 cm) and the electric field to mobilize proteins out of the sediment.…”
Section: Resultssupporting
confidence: 81%
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“…The identification of algal peptides and proteins in the deep marine sediment core section demonstrates that gel electrophoresis can be an effective method for isolating proteins present in complex matrices, but further improvements can be made in the total recovery of material. The results obtained by loading sediment buffer mixture directly to the gel interface supports previous findings by Moore et al [16] that an electric field applied directly to sediment particles enhances protein extraction. The number of proteins identified was increased by running the gel for a longer period of time, allowing the ion front to move further down the gel (7 cm vs. 2 cm) and the electric field to mobilize proteins out of the sediment.…”
Section: Resultssupporting
confidence: 81%
“…These identified proteins represent material that may have been preserved after burial [12,[54][55][56][57] or mixed from the surface into deeper sediments by bioturbators [58][59][60]. Thus, it is expected that fewer proteins, with potentially lower sequence coverage, would be identified in the Bering Sea 8-to 10-cm core section than in surface sediments observed by Moore et al [16,29]. Age estimation of these sediments can be uncertain, because the surface sedimentary mixed layer can extend from 0 to 16.5 cm on the outer Bering Sea shelf [61].…”
Section: Resultsmentioning
confidence: 84%
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