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Ocean acidification and global warming: Can we expect effects on microzooplankton communities?

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H.G. Horn1, M.G.J. Löder1,2, U. Riebesell3, U. Sommer3, M. Boersma1,4 and N. Aberle1

1 Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Biologische Anstalt Helgoland

2 University of Bayreuth

3 Representing the KOSMOS and the BIOACID Indoor Mesocosm Teams, GEOMAR Helmholtz-Zentrum für Ozeanforschung, Kiel

4 University of Bremen

Ocean acidification and global warming:

Can we expect effects on microzooplankton communities?

Conclusions

With exception for the Summer experiment, no effects of high CO2 on MZP biomass, diversity or taxonomic compo- sition were found. We observed increased MZP growth rates at high CO2. These results point at indirect effects of

Introduction

Microzooplankton (MZP) is an important competitor for food and a food source for larger mesozooplankton. With phyto- plankton growth being enhanced at high CO2 conditions, we expected an enhanced MZP growth as well.

Methods

MZP abundance, biomass, size classes and taxonomic composition were determined by microscopic counts in three mesocosm experiments. Additionally, grazing experiments were conducted.

Contact:

henriette.horn@awi.de

HELGOLAND

Kurpromenade 201 27498 Helgoland Telefon 04725 819-0 www.awi.de

GEOMAR Helmholtz Centre for Ocean Research Kiel www.geomar.de BIOACID Phase II Final Meeting Kiel 6 - 7 Oct. 2015

Consortium 1: Pelagic ecosystems under ocean acidification: Ecological, biogeochemical and evolutionary responses

WP 1.6: The role of microzooplankton under future ocean acidification and warming scenarios

CO2 caused by changes in phytoplankton being compen- sated on an ecosystem level. In contrast, warming can be expected to have a strong effect on MZP. It led to increased growth rates and a reduced time lag between phytoplankton bloom and MZP biomass maximum.

BIOACID 2012 Autumn Experiment

• 12 indoor mesocosms (Kiel)

• 9 and 15˚C

• 440 and 1040 ppm CO2

• Oct – Nov 2012 (24 days)

 Higher MZP diversity in the warm treatments but no differences between CO2 treatments

 Higher MZP growth rates and earlier timing of MZP in the warm treat- ments but no effect of CO2

KOSMOS 2013 Gullmar Fjord Experiment

• 10 outdoor mesocosms (Sweden)

• 400 and 900 ppm CO2

• 5 replicates

• Mar – June 2013 (107 days)

 No differences in MZP taxonomic composition or diversity between CO2 treatments

 No differences in MZP biomass or growth rates between CO2 treat- ments

BIOACID 2013 Summer Experiment

• 12 indoor mesocosms (Kiel)

• 16.5 and 22.5˚C

• 500 to 3000 ppm CO2 gradient

• Aug – Sept 2013 (28 days)

 Lower MZP biomass and diversity in the high CO2 treatments during phytoplankton bloom (day 0-12)

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