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- W2062121393 abstract "Abstract Surface sediments from 4 contrasting environmental settings in the Southern Trough of Guaymas Basin were analysed to determine their texture, total organic matter (TOM), P (TP), and N (TN) content as well as the spatial variation in their C:N:P atomic ratios in hydrothermally altered sediments. Particle size analysis revealed a marked spatial heterogeneity among sites. Cores taken at Beggiatoa bacterial mats and at clam fields contained significant silt and clay content, while those obtained near venting sites had sand and gravel as the main components because no fine sedimentary materials are deposited at these sites. Fine grain sediments were common farther away from vents. High levels of organic C (3.4 to 12.4%) were recorded in the upper 8 cm but no clear trends of decreasing TOC with depth were noted. The presence of hydrothermally generated petroleum in some cores increased the organic C content between 8 and 12 cm. TN was generally high (456.3–4356 μg/g) and sustained a significant correlation with TOM ( r =0.834, P Beggiatoa or vesicomyd clams are predominant." @default.
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- W2062121393 date "1999-06-01" @default.
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- W2062121393 title "Sedimentary geochemistry of hydrothermal vents in Guaymas Basin, Gulf of California, Mexico" @default.
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- W2062121393 doi "https://doi.org/10.1016/s0883-2927(98)00064-x" @default.
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