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• W1968757890 endingPage "2204" @default.
• W1968757890 startingPage "2178" @default.
• W1968757890 abstract "Abstract Continental-shelf lithofacies are described from a series of cores collected in the northern Gulf of Alaska, a high-energy paraglacial shelf experiencing rapid rates of sediment accumulation. Short-lived tracers (234Th and chlorophyll-a) indicate that during the annual peak in fluvial sediment input (summer), biologic sediment mixing coefficients in the surficial seabed are generally lower than other coastal environments ( 2 cm yr−1 and non-steady sediment deposition occurs. Depositional fabric is also observed in strata at 50–100 m water depths and is similar in appearance to beds that may form through deposition of wave-induced fluid-mud flows, which have been observed forming on other shelves with moderate to high wave energy. Five general lithofacies can be identified for the study area: inner-shelf sand facies, interbedded sandy mud facies, moderate-to-well-bioturbated mud facies, gravelly mud facies, and Tertiary bedrock facies. The moderate-to-well-bioturbated mud facies is areally dominant, representing over 50% of the shelf area, although roughly equal volumes (∼0.4 km3) of strata with some preservation of primary fabric are annually accumulating. Lithofacies on this paraglacial shelf generally resemble mid- and low-latitude allochthonous shelf strata to a much greater degree than Holocene glacimarine strata formed on shelves dominated by icebergs and floating ice shelves. Paraglacial strata may be differentiated from non-glacial shelf strata by lower organic carbon concentrations, a relatively lower degree of bioturbation, and increased preservation of primary depositional fabric." @default.
• W1968757890 created "2016-06-24" @default.
• W1968757890 creator A5038138915 @default.
• W1968757890 creator A5064025558 @default.
• W1968757890 date "2006-11-01" @default.
• W1968757890 modified "2023-09-24" @default.
• W1968757890 title "A quantitative examination of modern sedimentary lithofacies formation on the glacially influenced Gulf of Alaska continental shelf" @default.
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• W1968757890 doi "https://doi.org/10.1016/j.csr.2006.07.014" @default.
• W1968757890 hasPublicationYear "2006" @default.

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