List of Contributors

Akbulut, Aydın; Akbulut, Nuray; Aleksandrov, Jurij V.; Alexevnina, Margarita S.; Amoros, Claude; Andersen, Hans Erik; Arnaut, N.A.; Arndt, Hartmut; Baklanov, Mikhail A.; Bäthe, Jürgen; Baumgartner, Christian; Bayarl, Serdar; Behrendt, Horst; Bekh, V.V.; Bloesch, Jürg; Boz, B.; Bravard, Jean‐Paul; Brittain, John E.; Bogen, Jim; Briede, Agrita; Brørs, Sturla; Carrel, Georges; Descy, Jean‐Pierre; Dole‐Olivier, Marie‐José; Druvietis, Ivars; Двинских, Светлана Александровна; Economou, Alcibiades N.; Eie, Jon Arne; Eremkina, Tatjana V.; Faugli, Per Einar; Feio, Maria João; Fischer, Helmut; Friberg, Nikolai; Gancarczyk, Aleksandra; Ritma, Gaumiga; Gavrilova, Ģsertrude; Gerasimov, Yuri V.; Gibbins, Chris; Gíslason, Gísli Már; Graça, Manuel A. S.; Gritzalis, Konstantinos; Gumiero, B.; Hachoł, Justyna; Haugland, Svein; Hein, Thomas; Hildrew, Alan G.; Hoffmann, Carl. C.; Hvidsten, Nils Arne; Jensen, Arne J.; Katolikov, V.M.; Khokhlova, Ludmila G.; Kitaev, Alexander B.; Kochanov, Sergej K.; Kokovkin, Alexander V.; Korneva, L. G.; Kronvang, Brian; Kudersky, L.A.; L’Abée-Lund, Jan Henning; Lamouroux, Nicolas; Łapińska, Małgorzata; Лазарева, В. И.; Leuven, Rob. S. E. W; Litvinov, A. S.; Loboda, N.S.; Maiolini, B.; Malard, Florian; Malcolm, I. A.; Malmqvist, B.; Mel'nik, Marina M.; Melvold, Kjetil; Минеева, Н. М.; Moroni, F.; Muñoz, Isabel; Muotka, T.; Nilsson, C.; Noskov, Victor; Nowacki, Franciszek; Охапкин, А. Г.; Ólafsson, Jón S.; Olivier, Jean‐Michel; Olšauskytè, Vaida; Ostojić, Ana; Папченков, В. Г.; Parele, Elga; Paunović, Momír; Pedersen, Morten Lauge; Peter, Fabian D.; Pettersen, Vegard; Petterson, Lars-Evan; Пономарев, В. И.; Преснова, Е В; Pusch, Martin; Rinaldi, M.; Robinson, Christopher T.; Romaní, Anna M.; Sabater, Sergi; Şahin, Yalçln; Saltveit, Svein Jakob; Sandin, Leonard; Schneider-Jacoby, Martin; Schöll, Franz; Scholten, Matthias; Seletkova, Elena B.; Shcherbina, Grigory Kh.; Шурганова, Г. В.; Siber, Rosi; Skakalsky, B.G.; Skorupskas, Ričardas; Skoulikidis, Nikolaos Th.; Sommerwerk, Nike; Soulsby, Chris; Sprińǵe, Gunta; Statzner, Bernhard; Stendera, Sonja; Stenina, A. S.; Sukhodolov, A.N.; Surian, N.; Svendsen, Lars M.; Tetzlaff, Doerthe; Timm, H.; Tockner, Klement; Tonolla, Diego; Uehlinger, Urs; Usatii, M.A.; Wantzen, Karl M.; Wnuk-Gławdel, Ewa; Wolter, Christian; Yarushina, M. I.; Zalewski, Maciej; Zinov'ev, Euvgeny A.; Zogaris, Stamatis; Olšauskyté, Vaida; Skorupskas, Riĉardas

doi:10.1016/b978-0-12-369449-2.00022-9

Cited by 1 publication

(1 citation statement)

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“…Taking into consideration that the Tulcea branch accounts for 45% of the total Danube discharge, all fluxes were upscaled to 100% to derive fluxes for the entire river as it enters the delta. This results in a water discharge of 10,100/7,800 m 3 /s (2013/2014, respectively), significantly above the average yearly discharge of 6,486 m 3 /s in both years (Sommerwerk et al, 2009). In 2013, the discharge was close to the average annual flood discharge of 10,889 m 3 /s.…”

Section: Implications For Oc Export To the Black Seamentioning

confidence: 90%

Constraining Instantaneous Fluxes and Integrated Compositions of Fluvially Discharged Organic Matter

Freymond

Lupker

Peterse

et al. 2018

Geochem Geophys Geosyst

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Fluvial export of organic carbon (OC) and burial in ocean sediments comprises an important carbon sink, but fluxes remain poorly constrained, particularly for specific organic components. Here OC and lipid biomarker contents and isotopic characteristics of suspended matter determined in depth profiles across an active channel close to the terminus of the Danube River are used to constrain instantaneous OC and biomarker fluxes and integrated compositions during high to moderate discharges. During high (moderate) discharge, the total Danube exports 8 (7) kg/s OC, 7 (3) g/s higher plant‐derived long‐chain fatty acids (LCFA), 34 (21) g/s short‐chain fatty acids (SCFA), and 0.5 (0.2) g/s soil bacterial membrane lipids (brGDGTs). Integrated stable carbon isotopic compositions were TOC: −28.0 (−27.6)‰, LCFA: −33.5 (−32.8)‰ and Δ14C TOC: −129 (−38)‰, LCFA: −134 (−143)‰, respectively. Such estimates will aid in establishing quantitative links between production, export, and burial of OC from the terrestrial biosphere.

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Section: Implications For Oc Export To the Black Seamentioning

confidence: 90%