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• W1908159055 startingPage "7663" @default.
• W1908159055 abstract "Abstract Current estimates suggest that more than 60% of the global seafloor are covered by millions of abyssal hills and mountains. These features introduce spatial fluid‐dynamic “granularity” whose influence on deep‐ocean sediment biogeochemistry is unknown. Here we compare biogeochemical surface‐sediment properties from a fluid‐dynamically well‐characterized abyssal hill and upstream plain: (1) In hill sediments, organic‐carbon and ‐nitrogen contents are only about half as high as on the plain while proteinaceous material displays less degradation; (2) on the hill, more coarse‐grained sediments (reducing particle surface area) and very variable calcite contents (influencing particle surface charge) are proposed to reduce the extent, and influence compound‐specificity, of sorptive organic‐matter preservation. Further studies are needed to estimate the representativeness of the results in a global context. Given millions of abyssal hills and mountains, their integrative influence on formation and composition of deep‐sea sediments warrants more attention." @default.
• W1908159055 created "2016-06-24" @default.
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• W1908159055 date "2015-09-25" @default.
• W1908159055 modified "2023-10-11" @default.
• W1908159055 title "An abyssal hill fractionates organic and inorganic matter in deep‐sea surface sediments" @default.
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• W1908159055 doi "https://doi.org/10.1002/2015gl065658" @default.
• W1908159055 hasPublicationYear "2015" @default.
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