Biological versus physical processes as drivers of large oscillations of the air–sea CO 2 flux in the Antarctic marginal ice zone during summer

Autor: Stoll, M.H.C, Thomas, H ^*, De Baar, H.J.W, Zondervan, I, De Jong, E, Bathmann, U.V, Fahrbach, E

Publikováno v: In Deep-Sea Research Part I 2002 49(9):1651-1667

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Significant long-term increase of fossil fuel CO2 uptake from reduced marine calcification

Autor: Ridgwell , A., Zondervan , I., Hargreaves , J. C., Bijma , J., Lenton , T. M.

Publikováno v: Biogeosciences Discussions
Biogeosciences Discussions, European Geosciences Union, 2006, 3 (6), pp.1763-1780

International audience; Analysis of available plankton manipulation experiments demonstrates a previously unrecognized wide range of sensitivities of biogenic calcification to simulated anthropogenic acidification of the ocean, with the "lab rat" of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0eabd9b872c2d87aa646ab5fe2a97a12
https://hal.science/hal-00297856

Response of primary production and calcification to changes of pCO2 during experimental blooms of the coccolithophorid Emiliania huxleyi

Autor: Delille, B., Harlay, J., Zondervan, I., Jacquet, S., Chou, L., Wollast, R., Bellerby, R.G.J., Frankignoulle, M., Borges, A.V., Riebesell, U., Gattuso, J.P.

Publikováno v: Global Biogeochemical Cycles, 19 . GB2023.
EPIC3Global biogeochemical cycles, 19, GB2023, 14 p.
Global Biogeochemical Cycles
Global Biogeochemical Cycles, American Geophysical Union, 2005, 19 (GB2023), pp.1-14. ⟨10.1029/2004GB002318⟩
Global Biogeochemical Cycles, 2005, 19 (GB2023), pp.1-14. ⟨10.1029/2004GB002318⟩

Primary production and calcification in response to different partial pressures of CO2 (PCO2) (“glacial,” “present,” and “year 2100” atmospheric CO2 concentrations) were investigated during a mesocosm bloom dominated by the coccolithophor

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::743c542bfa428f42b4949f4dafa5be5a
http://oceanrep.geomar.de/5109/

Chromophoric dissolved organic matter in experimental mesocosms maintained under different pCO2 levels

Autor: Rochelle-Newall, E., Delille, B., Frankignoulle, M., Gattuso, J.P., Jacquet, S., Riebesell, U., Terbruggen, A., Zondervan, I.

Chromophoric dissolved organic matter (CDOM) represents the optically active fraction of the bulk dissolved organic matter (DOM) pool. Recent evidence pointed towards a microbial source of CDOM in the aquatic environment and led to the proposal that

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______232::ae584e665c0a3e87380adbf7af85329a
http://www.vliz.be/nl/open-marien-archief?module=ref&refid=72775