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- W1644287766 abstract "Simple mass balance models are applied to a high resolution 234 Th profile from the northwest Pacific to examine the magnitude, rate, and depth distribution of particle remineralization processes below the euphotic zone (E z ). Here, excess 234 Th ( 234 Th > 238 U) below the E z is attributed to fragmentation processes that result in the conversion of sinking to non-sinking particles. By considering particulate organic carbon (POC) to 234 Th ratios on particles, we show that POC flux attenuation is larger than for 234 Th, which we attribute to bacterial and zooplankton consumption of sinking POC. Three case studies are used to demonstrate how different combinations of particle fragmentation and POC respiration impact flux attenuation below the E z . When sampled with high vertical resolution and precision, 234 Th and POC/ 234 Th ratios provide insights into both export from the E z and the extent to which sinking particle fluxes and associated minerals are attenuated with depth." @default.
- W1644287766 created "2016-06-24" @default.
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- W1644287766 date "2010-08-01" @default.
- W1644287766 modified "2023-10-04" @default.
- W1644287766 title "Insights into particle formation and remineralization using the short-lived radionuclide, Thoruim-234" @default.
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- W1644287766 doi "https://doi.org/10.1029/2010gl044063" @default.
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