FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2318062509> ?p ?o ?g. }

• W2318062509 endingPage "521" @default.
• W2318062509 startingPage "492" @default.
• W2318062509 abstract "Using two complimentary approaches (pore water advection/diffusion/ reaction modeling and stable isotope mass balance calculations) we show that carbonate dissolution/reprecipitation occurs on early diagenetic time scales across a broad range of sediments on the Great Bahamas Bank. The input of oxygen into the sediments, which strongly controls sediment carbonate dissolution, has two major sources---belowground input by seagrasses (that is, seagrass O~2~ pumping), and permeability-driven advective pore water exchange. The relative importance of these O~2~ delivery mechanisms depends on both seagrass density, and on how bottom water flow interacts with the seagrass canopy and leads to this advective exchange. Dissolution appears to involve the preferential dissolution of high-Mg calcite, and the rates of dissolution increase linearly with increasing seagrass density. Isotopic evidence of dissolution/reprecipitation is consistent with the occurrence of Ostwald ripening as the mechanism of reprecipitation, in which smaller crystals dissolve and then reprecipitate as larger crystals, with little or no change in mineralogy. Estimates of the aerially-integrated dissolution flux on the Bahamas Bank suggest that carbonate dissolution is an important loss term in the budget of shallow water carbonate sediments, and that on-bank carbonate dissolution, rather than offshore transport, may represent an important sink for gross shallow water carbonate production. Dissolution in carbonate bank and bay sediments may also be a significant alkalinity source to the surface ocean, and should be considered in global alkalinity/carbonate budget. Finally, coupled dissolution/reprecipitation may have a major impact on the stable isotope composition of carbonate sediments that are ultimately preserved in the rock record. These processes may therefore need to be considered, for example, when using carbon isotope records to obtain information on the operation of the global carbon cycle during the Phanerozoic." @default.
• W2318062509 created "2016-06-24" @default.
• W2318062509 creator A5032402620 @default.
• W2318062509 creator A5042032867 @default.
• W2318062509 creator A5071520289 @default.
• W2318062509 date "2010-06-01" @default.
• W2318062509 modified "2023-09-26" @default.
• W2318062509 title "The widespread occurrence of coupled carbonate dissolution/reprecipitation in surface sediments on the Bahamas Bank" @default.
• W2318062509 cites W1582006139 @default.
• W2318062509 cites W1595502742 @default.
• W2318062509 cites W1968172155 @default.
• W2318062509 cites W1976805835 @default.
• W2318062509 cites W1982119230 @default.
• W2318062509 cites W1985320004 @default.
• W2318062509 cites W1986916739 @default.
• W2318062509 cites W1987524149 @default.
• W2318062509 cites W1988527311 @default.
• W2318062509 cites W1990783861 @default.
• W2318062509 cites W1991608935 @default.
• W2318062509 cites W1992375285 @default.
• W2318062509 cites W2003805168 @default.
• W2318062509 cites W2011556233 @default.
• W2318062509 cites W2017386151 @default.
• W2318062509 cites W2019764231 @default.
• W2318062509 cites W2020097986 @default.
• W2318062509 cites W2030502376 @default.
• W2318062509 cites W2032314413 @default.
• W2318062509 cites W2035598111 @default.
• W2318062509 cites W2048615333 @default.
• W2318062509 cites W2054645658 @default.
• W2318062509 cites W2057660325 @default.
• W2318062509 cites W2058721748 @default.
• W2318062509 cites W2061848701 @default.
• W2318062509 cites W2063500510 @default.
• W2318062509 cites W2065716465 @default.
• W2318062509 cites W2065756726 @default.
• W2318062509 cites W2067910389 @default.
• W2318062509 cites W2070850624 @default.
• W2318062509 cites W2071003343 @default.
• W2318062509 cites W2076323160 @default.
• W2318062509 cites W2081484203 @default.
• W2318062509 cites W2083547279 @default.
• W2318062509 cites W2085103365 @default.
• W2318062509 cites W2086484327 @default.
• W2318062509 cites W2088385926 @default.
• W2318062509 cites W2089660798 @default.
• W2318062509 cites W2100734663 @default.
• W2318062509 cites W2100999514 @default.
• W2318062509 cites W2101495560 @default.
• W2318062509 cites W2102181771 @default.
• W2318062509 cites W2107757701 @default.
• W2318062509 cites W2122651062 @default.
• W2318062509 cites W2123816680 @default.
• W2318062509 cites W2130340844 @default.
• W2318062509 cites W2130490621 @default.
• W2318062509 cites W2133178772 @default.
• W2318062509 cites W2134971691 @default.
• W2318062509 cites W2135750227 @default.
• W2318062509 cites W2144516661 @default.
• W2318062509 cites W2145449126 @default.
• W2318062509 cites W2149287950 @default.
• W2318062509 cites W2149340013 @default.
• W2318062509 cites W2150209683 @default.
• W2318062509 cites W2154997609 @default.
• W2318062509 cites W2164336439 @default.
• W2318062509 cites W2171233235 @default.
• W2318062509 cites W2178971318 @default.
• W2318062509 cites W2182016570 @default.
• W2318062509 cites W2330059339 @default.
• W2318062509 cites W2331592735 @default.
• W2318062509 cites W2583406289 @default.
• W2318062509 cites W2764433274 @default.
• W2318062509 cites W2943535113 @default.
• W2318062509 cites W3100816615 @default.
• W2318062509 cites W578243753 @default.
• W2318062509 cites W631848896 @default.
• W2318062509 cites W87496107 @default.
• W2318062509 cites W2465310271 @default.
• W2318062509 cites W2884723486 @default.
• W2318062509 doi "https://doi.org/10.2475/06.2010.03" @default.
• W2318062509 hasPublicationYear "2010" @default.
• W2318062509 type Work @default.
• W2318062509 sameAs 2318062509 @default.
• W2318062509 citedByCount "72" @default.
• W2318062509 countsByYear W23180625092012 @default.
• W2318062509 countsByYear W23180625092013 @default.
• W2318062509 countsByYear W23180625092014 @default.
• W2318062509 countsByYear W23180625092015 @default.
• W2318062509 countsByYear W23180625092016 @default.
• W2318062509 countsByYear W23180625092017 @default.
• W2318062509 countsByYear W23180625092018 @default.
• W2318062509 countsByYear W23180625092019 @default.
• W2318062509 countsByYear W23180625092020 @default.
• W2318062509 countsByYear W23180625092021 @default.
• W2318062509 countsByYear W23180625092022 @default.
• W2318062509 countsByYear W23180625092023 @default.
• W2318062509 crossrefType "journal-article" @default.
• W2318062509 hasAuthorship W2318062509A5032402620 @default.

• next