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• W1980942085 endingPage "2005" @default.
• W1980942085 startingPage "1989" @default.
• W1980942085 abstract "Following the extreme low ice year of 2007, primary production and the sinking export of particulate and gel-like organic material, using short-term particle interceptor traps deployed at 100 m, were measured in the southeastern Beaufort Sea during summer 2008. The combined influence of early ice retreat and coastal upwelling contributed to exceptionally high primary production (500 ± 312 mg C m−2 day−1, n = 7), dominated by large cells (>5 μm, 73% ± 15%, n = 7). However, except for one station located north of Cape Bathurst, the sinking export of particulate organic carbon (POC) was relatively low (range: 38–104 mg C m−2 day−1, n = 12) compared to other productive Arctic shelves. Estimates indicate that 80% ± 20% of the primary production was cycled through large copepods or the microbial food web. Exopolymeric substances were abundant in the sinking material but did not appear to accelerate POC sinking export. The use of isotopic signatures (δ13C, δ15N) and carbon/nitrogen ratios to identify sources of the sinking material was successful only at two stations with a strong marine or terrestrial signature, indicating the limitations of this approach in hydrographically and biologically complex Arctic coastal waters such as in the Beaufort Sea. At these two stations influenced by either coastal upwelling or erosion, the composition and magnitude of particulate sinking fluxes were markedly different from other stations visited during the study. These observations underscore the fundamental role of mesoscale circulation patterns and hydrodynamic singularities on the export of particulate organic material on Arctic shelves." @default.
• W1980942085 created "2016-06-24" @default.
• W1980942085 creator A5018010301 @default.
• W1980942085 creator A5027045277 @default.
• W1980942085 creator A5072556059 @default.
• W1980942085 date "2011-08-02" @default.
• W1980942085 modified "2023-10-18" @default.
• W1980942085 title "Summertime primary production and carbon export in the southeastern Beaufort Sea during the low ice year of 2008" @default.
• W1980942085 cites W1502692695 @default.
• W1980942085 cites W1527801913 @default.
• W1980942085 cites W1600035625 @default.
• W1980942085 cites W1606968016 @default.
• W1980942085 cites W1646920304 @default.
• W1980942085 cites W1656843456 @default.
• W1980942085 cites W1836625471 @default.
• W1980942085 cites W1964819552 @default.
• W1980942085 cites W1965645800 @default.
• W1980942085 cites W1965801259 @default.
• W1980942085 cites W1965968996 @default.
• W1980942085 cites W1966529962 @default.
• W1980942085 cites W1968543674 @default.
• W1980942085 cites W1972398700 @default.
• W1980942085 cites W1972452490 @default.
• W1980942085 cites W1976636947 @default.
• W1980942085 cites W1977300523 @default.
• W1980942085 cites W1979503027 @default.
• W1980942085 cites W1980252858 @default.
• W1980942085 cites W1981355190 @default.
• W1980942085 cites W1982069483 @default.
• W1980942085 cites W1982959478 @default.
• W1980942085 cites W1985835475 @default.
• W1980942085 cites W1986098491 @default.
• W1980942085 cites W1988257696 @default.
• W1980942085 cites W1989527185 @default.
• W1980942085 cites W1990491823 @default.
• W1980942085 cites W1991535380 @default.
• W1980942085 cites W1992530079 @default.
• W1980942085 cites W1993190885 @default.
• W1980942085 cites W1993769665 @default.
• W1980942085 cites W1997120413 @default.
• W1980942085 cites W1999250331 @default.
• W1980942085 cites W2001052056 @default.
• W1980942085 cites W2003686021 @default.
• W1980942085 cites W2006631544 @default.
• W1980942085 cites W2013085580 @default.
• W1980942085 cites W2021998617 @default.
• W1980942085 cites W2024417959 @default.
• W1980942085 cites W2027125083 @default.
• W1980942085 cites W2028676286 @default.
• W1980942085 cites W2034871149 @default.
• W1980942085 cites W2040921034 @default.
• W1980942085 cites W2043416377 @default.
• W1980942085 cites W2043785409 @default.
• W1980942085 cites W2049051125 @default.
• W1980942085 cites W2050342188 @default.
• W1980942085 cites W2054373016 @default.
• W1980942085 cites W2054703399 @default.
• W1980942085 cites W2055194450 @default.
• W1980942085 cites W2058114772 @default.
• W1980942085 cites W2059707467 @default.
• W1980942085 cites W2060038313 @default.
• W1980942085 cites W2062242883 @default.
• W1980942085 cites W2067905703 @default.
• W1980942085 cites W2068677521 @default.
• W1980942085 cites W2076489367 @default.
• W1980942085 cites W2077630400 @default.
• W1980942085 cites W2083100551 @default.
• W1980942085 cites W2083483437 @default.
• W1980942085 cites W2084278313 @default.
• W1980942085 cites W2086477516 @default.
• W1980942085 cites W2087679370 @default.
• W1980942085 cites W2087883794 @default.
• W1980942085 cites W2094836065 @default.
• W1980942085 cites W2103030963 @default.
• W1980942085 cites W2103425624 @default.
• W1980942085 cites W2103607688 @default.
• W1980942085 cites W2107733948 @default.
• W1980942085 cites W2108889829 @default.
• W1980942085 cites W2110226083 @default.
• W1980942085 cites W2111573245 @default.
• W1980942085 cites W2114628556 @default.
• W1980942085 cites W2121719964 @default.
• W1980942085 cites W2123559861 @default.
• W1980942085 cites W2123619249 @default.
• W1980942085 cites W2129543789 @default.
• W1980942085 cites W2130133858 @default.
• W1980942085 cites W2131511954 @default.
• W1980942085 cites W2132590819 @default.
• W1980942085 cites W2141384827 @default.
• W1980942085 cites W2142037275 @default.
• W1980942085 cites W2143182887 @default.
• W1980942085 cites W2143723805 @default.
• W1980942085 cites W2144210118 @default.
• W1980942085 cites W2147345950 @default.
• W1980942085 cites W2151209927 @default.
• W1980942085 cites W2155655413 @default.
• W1980942085 cites W2156594912 @default.
• W1980942085 cites W2160575983 @default.

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