Origin-specific molecular signatures of dissolved organic matter in the Lena Delta

Verfasser / Beitragende:
[I. Dubinenkov, R. Flerus, P. Schmitt-Kopplin, G. Kattner, B. Koch]
Ort, Verlag, Jahr:
2015
Enthalten in:
Biogeochemistry, 123/1-2(2015-03-01), 1-14
Format:
Artikel (online)
ID: 605517118
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024 7 0 |a 10.1007/s10533-014-0049-0  |2 doi 
035 |a (NATIONALLICENCE)springer-10.1007/s10533-014-0049-0 
245 0 0 |a Origin-specific molecular signatures of dissolved organic matter in the Lena Delta  |h [Elektronische Daten]  |c [I. Dubinenkov, R. Flerus, P. Schmitt-Kopplin, G. Kattner, B. Koch] 
520 3 |a Large Arctic rivers discharge significant amounts of dissolved organic matter (DOM) into the Arctic Ocean. We sampled natural waters of the Lena River, the Buor-Khaya Bay (Laptev Sea), permafrost melt water creeks, ice complex melt water creeks and a lake. The goal of this study was to characterize the molecular DOM composition with respect to different water bodies within the Lena Delta. We aimed at an identification of source-specific DOM molecular markers and their relative contribution to DOM of different origin. The molecular characterization was performed for solid-phase extracted DOM by Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS). Average dissolved organic carbon concentrations in the original samples were 490±75µmolCL−1 for riverine and bay samples and 399±115µmolCL−1 for permafrost melt water creeks. Average TDN concentrations were elevated in the permafrost melt waters (19.7±7.1µmolNL−1) in comparison to the river and the bay (both 13.2±2.6µmolNL−1). FT-ICR MS and statistical tools demonstrated that the origin of DOM in the Lena Delta was systematically reflected in its molecular composition. Magnitude weighted parameters calculated from MS data (O/Cwa, H/Cwa, C/Nwa) highlighted preliminary sample discrimination. The highest H/Cwa of 1.315 was found for DOM in melt water creeks in comparison to 1.281 for river and 1.230 for the bay samples. In the bay samples we observed a higher fraction of oxygen-rich components which was reflected in an O/Cwa ratio of 0.445 in comparison to 0.425 and 0.427 in the river and creeks, respectively. From the southernmost location to the bay a relative depletion of nitrogenous molecular markers and an enrichment of oxidized DOM components occurred. The highest contribution of nitrogenous components was indicative for creeks reflected in a C/Nwa of 104 in comparison to 143 and 176 in the river and bay, respectively. These observations were studied on a molecular formula level using principal component and indicator value analyses. The results showed systematic differences with respect to water origin and constitute an important basis for a better mechanistic understanding of DOM transformations in the changing Arctic rivers. 
540 |a Springer International Publishing Switzerland, 2014 
690 7 |a Arctic  |2 nationallicence 
690 7 |a Lena Delta  |2 nationallicence 
690 7 |a Permafrost  |2 nationallicence 
690 7 |a DOM  |2 nationallicence 
690 7 |a FT-ICR MS  |2 nationallicence 
690 7 |a Molecular markers  |2 nationallicence 
700 1 |a Dubinenkov  |D I.  |u Ecological Chemistry, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Am Handelshafen 12, 27570, Bremerhaven, Germany  |4 aut 
700 1 |a Flerus  |D R.  |u Ecological Chemistry, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Am Handelshafen 12, 27570, Bremerhaven, Germany  |4 aut 
700 1 |a Schmitt-Kopplin  |D P.  |u Research Unit Analytical BioGeoChemistry, Helmholtz Zentrum München, German Research Center for Environmental Health, Ingolstädter Landstraße 1, 85764, Neuherberg, Germany  |4 aut 
700 1 |a Kattner  |D G.  |u Ecological Chemistry, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Am Handelshafen 12, 27570, Bremerhaven, Germany  |4 aut 
700 1 |a Koch  |D B.  |u Ecological Chemistry, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Am Handelshafen 12, 27570, Bremerhaven, Germany  |4 aut 
773 0 |t Biogeochemistry  |d Springer International Publishing  |g 123/1-2(2015-03-01), 1-14  |x 0168-2563  |q 123:1-2<1  |1 2015  |2 123  |o 10533 
856 4 0 |u https://doi.org/10.1007/s10533-014-0049-0  |q text/html  |z Onlinezugriff via DOI 
898 |a BK010053  |b XK010053  |c XK010000 
900 7 |a Metadata rights reserved  |b Springer special CC-BY-NC licence  |2 nationallicence 
908 |D 1  |a research-article  |2 jats 
949 |B NATIONALLICENCE  |F NATIONALLICENCE  |b NL-springer 
950 |B NATIONALLICENCE  |P 856  |E 40  |u https://doi.org/10.1007/s10533-014-0049-0  |q text/html  |z Onlinezugriff via DOI 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Dubinenkov  |D I.  |u Ecological Chemistry, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Am Handelshafen 12, 27570, Bremerhaven, Germany  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Flerus  |D R.  |u Ecological Chemistry, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Am Handelshafen 12, 27570, Bremerhaven, Germany  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Schmitt-Kopplin  |D P.  |u Research Unit Analytical BioGeoChemistry, Helmholtz Zentrum München, German Research Center for Environmental Health, Ingolstädter Landstraße 1, 85764, Neuherberg, Germany  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Kattner  |D G.  |u Ecological Chemistry, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Am Handelshafen 12, 27570, Bremerhaven, Germany  |4 aut 
950 |B NATIONALLICENCE  |P 700  |E 1-  |a Koch  |D B.  |u Ecological Chemistry, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung, Am Handelshafen 12, 27570, Bremerhaven, Germany  |4 aut 
950 |B NATIONALLICENCE  |P 773  |E 0-  |t Biogeochemistry  |d Springer International Publishing  |g 123/1-2(2015-03-01), 1-14  |x 0168-2563  |q 123:1-2<1  |1 2015  |2 123  |o 10533