Articles | Volume 23, issue 3
https://doi.org/10.5194/bg-23-1103-2026
https://doi.org/10.5194/bg-23-1103-2026
Research article
 | 
06 Feb 2026
Research article |  | 06 Feb 2026

Reconstructing changes in nitrogen input to the Danube-influenced Black Sea Shelf during the Holocene

Andreas Neumann, Justus E. E. van Beusekom, Alexander Bratek, Jana Friedrich, Jürgen Möbius, Tina Sanders, Hendrik Wolschke, and Kirstin Dähnke

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Cited articles

Anderson, C. and Cabana, G.: Does delta15N in river food webs reflect the intensity and origin of N loads from the watershed?, Sci. Total Environ., 367, 968–978, https://doi.org/10.1016/j.scitotenv.2006.01.029, 2006. 
Appleby, P. G. and Oldfield, F.: The Calculation of Lead-210 Dates Assuming a Constant Rate of Supply of Unsupported 210Pb to the Sediment, Catena, 5, 1–8, https://doi.org/10.1016/S0341-8162(78)80002-2, 1978. 
Bratek, A., Emeis, K.-C., Sanders, T., Wankel, S. D., Struck, U., Möbius, J., and Dähnke, K.: Nitrate sources and the effect of land cover on the isotopic composition of nitrate in the catchment of the Rhône River, Isotopes in Environmental and Health Studies, 56, 14–35, https://doi.org/10.1080/10256016.2020.1723580, 2020. 
Bunzel, D., Milker, Y., Müller-Navarra, K., Arz, H. W., Friedrich, J., Lahajnar, N., and Schmiedl, G.: Integrated stratigraphy of foreland salt-marsh sediments of the south-eastern North Sea region, Newsletters Stratigr., 53, 415–442, https://doi.org/10.1127/nos/2020/0540, 2020. 
Constantinescu, A. M., Tyler, A. N., Stanica, A., Spyrakos, E., Hunter, P. D., Catianis, I., and Panin, N.: A century of human interventions on sediment flux variations in the Danube-Black Sea transition zone, Front. Mar. Sci., 10, 1068065, https://doi.org/10.3389/fmars.2023.1068065, 2023. 
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Short summary
The North-Western shelf of the Black Sea is substantially influenced by the discharge of nutrients from River Danube. We have sampled the sediment there and measured particulate carbon and nitrogen to reconstruct the variability of nitrogen sources to the NW shelf. Our results demonstrate that the balance of riverine nitrogen input and marine nitrogen fixation is sensitive to climate changes. Nitrogen from human activities is detectable in NW shelf sediment since the 12th century.
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