English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/108894
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

DC FieldValueLanguage
dc.contributor.authorLatasa, Mikel-
dc.contributor.authorHenjes, Joachim-
dc.contributor.authorScharek, Renate-
dc.contributor.authorAssmy, Philipp-
dc.contributor.authorRöttgers, Rüdiger-
dc.contributor.authorSmetacek, V.-
dc.identifierdoi: 10.3354/meps10937-
dc.identifierissn: 0171-8630-
dc.identifiere-issn: 1616-1599-
dc.identifier.citationMarine Ecology Progress Series 513: 39-50 (2014)-
dc.description12 pages, 5 figures, 3 tables-
dc.description.abstractDilution experiments were performed to quantify growth and mortality rates of phytoplankton groups (as defined by pigment markers) for 5 wk in an iron-induced phytoplankton bloom during the European Iron Fertilization Experiment (EIFEX) conducted in the Southern Ocean. Rates could be reliably measured for the 2 main groups, diatoms and prymnesiophytes. Mean phytoplankton intrinsic growth rates were around 0.23 d-1, without a significant temporal trend. Mortality rates, however, decreased with time (from ∼0.3 to ∼0.06 d-1), leading to an increase in decoupling between phytoplankton growth and microzooplankton grazing. The decrease in grazing was correlated with the decrease in concentrations of small microprotozooplankton (<60 μm). As a consequence, net growth in the dilution experiments increased from around 0 d-1 up to 0.13 d-1 in the last days of the experiment, 35 d after the initial iron fertilization. This pattern did not reflect the dynamics of net phytoplankton accumulation in the fertilized patch, which increased until Days 24 to 27 and decreased thereafter. The difference between experimental and natural phytoplankton net growth is the biomass that escapes microzooplankton grazing and does not accumulate in the surface mixed layer, i.e. the biomass that went to higher trophic levels plus that exported out of the mixed layer. It increased throughout EIFEX and suggests a shift from a predominantly recycling system towards a more exporting one. © Inter-Research 2014-
dc.description.sponsorshipThis work was partly supported by Spanish Ministry of Education (MEC) research grant REN2002-12076-E/ANT and by the Alfred Wegener Institute Helmholtz Center for Polar and Marine Research-
dc.publisherInter Research-
dc.subjectHPLC pigments-
dc.subjectC export-
dc.subjectMicrozooplankton grazing-
dc.subjectFlow cytometry-
dc.subjectDilution experiments-
dc.subjectTop-down control-
dc.subjectIron fertilization-
dc.titleProgressive decoupling between phytoplankton growth and microzooplankton grazing during an iron-induced phytoplankton bloom in the Southern Ocean (EIFEX)-
dc.description.versionPeer Reviewed-
Appears in Collections:(ICM) Artículos
Files in This Item:
File Description SizeFormat 
Latasa_et_al_2014.pdf352,92 kBAdobe PDFThumbnail
Show simple item record

WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.