Abstract

AME Aquatic Microbial Ecology Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials AME 64:221-232 (2011) - DOI: https://doi.org/10.3354/ame01520 Effects of elevated CO2 partial pressure and temperature on the coccolithophore Syracosphaera pulchra Sarah Fiorini1,2,3,*, Jack J. Middelburg3,4, Jean-Pierre Gattuso1,2 1INSU-CNRS, Laboratoire d’Océanographie de Villefranche, BP 28, 06234 Villefranche-sur-Mer Cedex, France 2UPMC University of Paris 06, Observatoire Océanologique de Villefranche-sur-Mer, 06230 Villefranche-sur-Mer, France 3Netherlands Institute of Ecology (NIOO-KNAW), PO Box 140, 4400 AC Yerseke, The Netherlands 4Faculty of Geosciences, Utrecht University, PO Box 80.021, 3508 TA Utrecht, The Netherlands *Email: fiorini.sarah@gmail.com ABSTRACT: The effects of elevated partial pressure of CO2 (pCO2) and temperature on the cocco­lithophore Syracosphaera pulchra were investigated in isolation and in combination. Both the diploid and the haploid life stages were studied. Batch cultures were grown under 4 conditions: 400 µatm and 19°C; 400 µatm and 22°C; 740 µatm and 19°C; and 740 µatm and 22°C. The growth rate (μ) ­significantly increased under elevated pCO2 only in the haploid stage and showed a different pattern with respect to temperature: it was higher at an elevated temperature in the haploid stage at 400 µatm whereas it decreased in the diploid stage at 740 µatm. Increasing both parameters together increased the growth rate by 11% in the haploid stage only. Elevated pCO2 had a negative impact on the content of particulate organic carbon (POC), production and cell size in both life stages at 19°C, while no significant effect was observed at 22°C. Increasing temperature significantly increased the content of POC and production in the diploid stage at 740 µatm, while at 400 µatm it significantly decreased both the content of POC and production in the haploid stage. A simultaneous increase in pCO2 and temperature had a negative effect on the content of POC and production in the haploid stage only. Neither the rate of calcification (production of particulate inorganic carbon, PIC) nor the PIC:POC ratio were significantly affected by elevated pCO2, temperature or their interaction. These results showed a strong interactive effect between pCO2 and temperature in affecting the physiology of S. pulchra, an effect that was often more pronounced in the haploid life stage. Elevated pCO2 had a stronger effect than temperature. KEY WORDS: Coccolithophores · Ocean acidification · Global warming · Carbon dioxide · Temperature · Calcification · Primary production · PIC:POC ratio Full text in pdf format PreviousNextCite this article as: Fiorini S, Middelburg JJ, Gattuso JP (2011) Effects of elevated CO2 partial pressure and temperature on the coccolithophore Syracosphaera pulchra. Aquat Microb Ecol 64:221-232. https://doi.org/10.3354/ame01520 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in AME Vol. 64, No. 3. Online publication date: September 20, 2011 Print ISSN: 0948-3055; Online ISSN: 1616-1564 Copyright © 2011 Inter-Research.

Highlights

  • The concentration of atmospheric carbon dioxide (CO2) has risen from 280 parts per million before the industrial era to a current value of 387 ppm

  • The growth rate (μ) significantly increased under elevated pressure of CO2 (pCO2) only in the haploid stage and showed a different pattern with respect to temperature: it was higher at an elevated temperature in the haploid stage at 400 μatm whereas it decreased in the diploid stage at 740 μatm

  • Elevated pCO2 had a negative impact on the content of particulate organic carbon (POC), production and cell size in both life stages at 19°C, while no significant effect was observed at 22°C

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Summary

Introduction

The concentration of atmospheric carbon dioxide (CO2) has risen from 280 parts per million (ppm) before the industrial era to a current value of 387 ppm. It is currently rising at a rate of ~3.3% yr−1 and will reach more than 700 ppm by the end of this century (Solomon et al 2007). Doubling atmospheric CO2, and the concomitant increase in other atmospheric greenhouse gases, will have important consequences for the Earth’s climate, leading to an average warming of 1.5 to > 5°C of global air temperature at the Earth’s surface by 2100 (Solomon et al 2007). Over the course of the present century, the concentration of CO2 in seawater is projected to increase by about 25 μmol kg–1 with a corresponding decrease in the pH of seawater to ~7.8, roughly 0.3 units lower than today’s value (Gattuso & Lavigne 2009).

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