Browse by Creators (Kiel)

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Number of items: 9.

Article in a Scientific Journal - peer-reviewed


Muglia, J., Somes, C. J., Nickelsen, L. and Schmittner, A. (2017) Combined Effects of Atmospheric and Seafloor Iron Fluxes to the Glacial Ocean Paleoceanography, 32 (11). pp. 1204-1218. DOI 10.1002/2016PA003077.

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Dale, A. W., Nickelsen, L., Scholz, F., Hensen, C., Oschlies, A. and Wallmann, K. (2015) A revised global estimate of dissolved iron fluxes from marine sediments Global Biogeochemical Cycles, 29 (5). pp. 691-707. DOI 10.1002/2014GB005017.

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Nickelsen, L. and Oschlies, A. (2015) Enhanced sensitivity of oceanic CO2 uptake to dust deposition by iron-light colimitation Geophysical Research Letters, 42 (2). pp. 492-499. DOI 10.1002/2014GL062969.

Conference presentation

Keller, D., Nickelsen, L., Floegel, S. and Sijp, W. (2015) UVic Model Marine Biogeochemistry Configurations at Kiel, Part II + a Cretaceous Configuration [Invited talk] In: University of Victoria Earth System Climate Model (UVIC ESCM) Developement Workshop, 04.-06.05.2015, University of Victoria.

Conference poster

Nickelsen, L. and Oschlies, A. (2013) Iron-light colimitation increases sensitivity of oceanic CO2 drawdown to dust deposition [Poster] In: ASP Summer Colloquium 2013, 29.07.-16.08.2013, Boulder, Colorado, USA.


Nickelsen, L. and Oschlies, A. (2012) Iron-light colimitation in a global ocean biogeochemical model and the sensitivity of oceanic CO2 uptake to dust deposition [Poster] In: AGU Fall Meeting 2012, 03.-07.12.2012, San Francisco, USA.

Thesis - not published by a publisher


Nickelsen, L. (2015) Modelling the marine biogeochemical implications of aeolian, sedimentary and riverine iron supply (Doctoral thesis/PhD), Christian-Albrechts-Universität Kiel, Kiel, Germany, 129 pp

Nickelsen, L. (2011) A model-based investigation of iron limitation of marine phytoplankton in High-Nutrient Low-Chlorophyll regions (Master thesis), Carl von Ossietzky-Universität, Oldenburg, Germany, 73 pp

This list was generated on Mon Jun 1 21:12:59 2020 CEST.