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Autor:
C. Eich, M. van Manen, J. S. P. McCain, L. J. Jabre, W. H. van de Poll, J. Jung, S. B. E. H. Pont, H.-A. Tian, I. Ardiningsih, G.-J. Reichart, E. M. Bertrand, C. P. D. Brussaard, R. Middag
Publikováno v:
Biogeosciences, Vol 21, Pp 4637-4663 (2024)
Iron (Fe) is a key limiting nutrient for Southern Ocean phytoplankton. Input of Fe into the Southern Ocean is projected to change due to global warming, yet the combined effects of a concurrent increase in temperature with dissolved Fe (dFe) addition
Externí odkaz:
https://doaj.org/article/a53ea26d63e34433a8098a2d8dbba0a6