Ocean acidification decreases plankton respiration: evidence from a mesocosm experiment.

Spilling, K., Paul, Allanah J., Virkkala, N., Hastings, T., Lischka, Silke , Stuhr, Annegret, Bermudez, Rafael, Czerny, Jan, Boxhammer, Tim , Schulz, Kai G., Ludwig, Andrea and Riebesell, Ulf (2016) Ocean acidification decreases plankton respiration: evidence from a mesocosm experiment. Open Access Biogeosciences (BG), 13 . pp. 4707-4719. DOI 10.5194/bg-13-4707-2016.

[thumbnail of bg-13-4707-2016.pdf]
bg-13-4707-2016.pdf - Published Version
Available under License Creative Commons: Attribution 3.0.

Download (190kB) | Preview
[thumbnail of bg-13-4707-2016-supplement.pdf]
bg-13-4707-2016-supplement.pdf - Supplemental Material
Available under License Creative Commons: Attribution 3.0.

Download (328kB) | Preview

Supplementary data:


Anthropogenic carbon dioxide (CO2) emissions are reducing the pH in the world's oceans. The plankton community is a key component driving biogeochemical fluxes, and the effect of increased CO2 on plankton is critical for understanding the ramifications of ocean acidification on global carbon fluxes. We determined the plankton community composition and measured primary production, respiration rates and carbon export (defined here as carbon sinking out of a shallow, coastal area) during an ocean acidification experiment. Mesocosms ( ∼  55 m3) were set up in the Baltic Sea with a gradient of CO2 levels initially ranging from ambient ( ∼  240 µatm), used as control, to high CO2 (up to  ∼  1330 µatm). The phytoplankton community was dominated by dinoflagellates, diatoms, cyanobacteria and chlorophytes, and the zooplankton community by protozoans, heterotrophic dinoflagellates and cladocerans. The plankton community composition was relatively homogenous between treatments. Community respiration rates were lower at high CO2 levels. The carbon-normalized respiration was approximately 40 % lower in the high-CO2 environment compared with the controls during the latter phase of the experiment. We did not, however, detect any effect of increased CO2 on primary production. This could be due to measurement uncertainty, as the measured total particular carbon (TPC) and combined results presented in this special issue suggest that the reduced respiration rate translated into higher net carbon fixation. The percent carbon derived from microscopy counts (both phyto- and zooplankton), of the measured total particular carbon (TPC), decreased from  ∼  26 % at t0 to  ∼  8 % at t31, probably driven by a shift towards smaller plankton (< 4 µm) not enumerated by microscopy. Our results suggest that reduced respiration leads to increased net carbon fixation at high CO2. However, the increased primary production did not translate into increased carbon export, and consequently did not work as a negative feedback mechanism for increasing atmospheric CO2 concentration.

Document Type: Article
Funder compliance: info:eu-repo/grantAgreement/EC/FP7/228224
Keywords: Carbon fluxes, carbon budget, gross primary production, respiration, bacterial production, sinking carbon flux, CO2 exchange with atmosphere
Research affiliation: OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-BI Biological Oceanography
Kiel University
Refereed: Yes
Open Access Journal?: Yes
Publisher: Copernicus Publications (EGU)
Date Deposited: 14 Dec 2015 13:21
Last Modified: 01 Feb 2019 15:15
URI: https://oceanrep.geomar.de/id/eprint/30540

Actions (login required)

View Item View Item