Matches in SemOpenAlex for { <https://semopenalex.org/work/W2078147413> ?p ?o ?g. }
- W2078147413 endingPage "680" @default.
- W2078147413 startingPage "663" @default.
- W2078147413 abstract "Abstract. Cold-water coral ecosystems are considered hot-spots of biodiversity and biomass production and may be a regionally important contributor to carbonate production. The impact of these ecosystems on biogeochemical processes and carbonate preservation in associated sediments were studied at Røst Reef and Traenadjupet Reef, two modern (post-glacial) cold-water coral reefs on the Mid-Norwegian shelf. Sulfate and iron reduction as well as carbonate dissolution and precipitation were investigated by combining pore-water geochemical profiles, steady state modeling, as well as solid phase analyses and sulfate reduction rate measurements on gravity cores of up to 3.25 m length. Low extents of sulfate depletion and dissolved inorganic carbon (DIC) production, combined with sulfate reduction rates not exceeding 3 nmol S cm−3 d−1, suggested that overall anaerobic carbon mineralization in the sediments was low. These data showed that the coral fragment-bearing siliciclastic sediments were effectively decoupled from the productive pelagic ecosystem by the complex reef surface framework. Organic matter being mineralized by sulfate reduction was calculated to consist of 57% carbon bound in CH2O groups and 43% carbon in -CH2- groups. Methane concentrations were below 1 μM, and failed to support the hypothesis of a linkage between the distribution of cold-water coral reefs and the presence of hydrocarbon seepage. Reductive iron oxide dissolution linked to microbial sulfate reduction buffered the pore-water carbonate system and inhibited acid-driven coral skeleton dissolution. A large pool of reactive iron was available leading to the formation of iron sulfide minerals. Constant pore-water Ca2+, Mg2+ and Sr2+ concentrations in most cores and decreasing Ca2+ and Sr2+ concentrations with depth in core 23–18 GC indicated diagenetic carbonate precipitation. This was consistent with the excellent preservation of buried coral fragments." @default.
- W2078147413 created "2016-06-24" @default.
- W2078147413 creator A5000242763 @default.
- W2078147413 creator A5014454698 @default.
- W2078147413 creator A5044294804 @default.
- W2078147413 creator A5049765930 @default.
- W2078147413 creator A5077445912 @default.
- W2078147413 creator A5091569201 @default.
- W2078147413 date "2009-04-27" @default.
- W2078147413 modified "2023-10-12" @default.
- W2078147413 title "Carbon mineralization and carbonate preservation in modern cold-water coral reef sediments on the Norwegian shelf" @default.
- W2078147413 cites W114659497 @default.
- W2078147413 cites W151004304 @default.
- W2078147413 cites W1567877667 @default.
- W2078147413 cites W1579045893 @default.
- W2078147413 cites W1586239332 @default.
- W2078147413 cites W1598693886 @default.
- W2078147413 cites W1878137325 @default.
- W2078147413 cites W1964901884 @default.
- W2078147413 cites W1967408071 @default.
- W2078147413 cites W1969187290 @default.
- W2078147413 cites W1972929024 @default.
- W2078147413 cites W1972985749 @default.
- W2078147413 cites W1980834172 @default.
- W2078147413 cites W1986418862 @default.
- W2078147413 cites W1990250430 @default.
- W2078147413 cites W1990611318 @default.
- W2078147413 cites W1990830185 @default.
- W2078147413 cites W1992364148 @default.
- W2078147413 cites W1993115519 @default.
- W2078147413 cites W1994035604 @default.
- W2078147413 cites W1994270148 @default.
- W2078147413 cites W2002232631 @default.
- W2078147413 cites W2003167051 @default.
- W2078147413 cites W2003424328 @default.
- W2078147413 cites W2004373591 @default.
- W2078147413 cites W2008772238 @default.
- W2078147413 cites W2011195114 @default.
- W2078147413 cites W2011708564 @default.
- W2078147413 cites W2013278565 @default.
- W2078147413 cites W2014766704 @default.
- W2078147413 cites W2023242078 @default.
- W2078147413 cites W2028463498 @default.
- W2078147413 cites W2029048327 @default.
- W2078147413 cites W2030098873 @default.
- W2078147413 cites W2031357690 @default.
- W2078147413 cites W2032042205 @default.
- W2078147413 cites W2034633531 @default.
- W2078147413 cites W2036100486 @default.
- W2078147413 cites W2038360704 @default.
- W2078147413 cites W2039249654 @default.
- W2078147413 cites W2041291443 @default.
- W2078147413 cites W2045986399 @default.
- W2078147413 cites W2047346379 @default.
- W2078147413 cites W2047471599 @default.
- W2078147413 cites W2050544236 @default.
- W2078147413 cites W2051440740 @default.
- W2078147413 cites W2054448182 @default.
- W2078147413 cites W2054645658 @default.
- W2078147413 cites W2056392157 @default.
- W2078147413 cites W2058721748 @default.
- W2078147413 cites W2059991581 @default.
- W2078147413 cites W2062241188 @default.
- W2078147413 cites W2064642026 @default.
- W2078147413 cites W2067890461 @default.
- W2078147413 cites W2071003343 @default.
- W2078147413 cites W2071777728 @default.
- W2078147413 cites W2072172339 @default.
- W2078147413 cites W2072390800 @default.
- W2078147413 cites W2078076761 @default.
- W2078147413 cites W2079690318 @default.
- W2078147413 cites W2081756558 @default.
- W2078147413 cites W2082250875 @default.
- W2078147413 cites W2085166727 @default.
- W2078147413 cites W2085686866 @default.
- W2078147413 cites W2086816618 @default.
- W2078147413 cites W2094077212 @default.
- W2078147413 cites W2096827057 @default.
- W2078147413 cites W2104690806 @default.
- W2078147413 cites W2111826800 @default.
- W2078147413 cites W2112429339 @default.
- W2078147413 cites W2130490621 @default.
- W2078147413 cites W2131274593 @default.
- W2078147413 cites W2132408571 @default.
- W2078147413 cites W2137258492 @default.
- W2078147413 cites W2137854548 @default.
- W2078147413 cites W2139312273 @default.
- W2078147413 cites W2141131685 @default.
- W2078147413 cites W2142462683 @default.
- W2078147413 cites W2146189255 @default.
- W2078147413 cites W2150738554 @default.
- W2078147413 cites W2161582133 @default.
- W2078147413 cites W2166403415 @default.
- W2078147413 cites W2168610019 @default.
- W2078147413 cites W2252457570 @default.
- W2078147413 cites W2316193362 @default.
- W2078147413 cites W2499828714 @default.
- W2078147413 cites W324775466 @default.