Impact of seawater carbonate chemistry on the calcification of marine bivalves.

Thomsen, Jörn, Haynert, Kristin, Wegner, K. M. and Melzner, Frank (2015) Impact of seawater carbonate chemistry on the calcification of marine bivalves. Biogeosciences (BG), 12 (2). pp. 1543-1571. DOI 10.5194/bg-12-4209-2015.

[img]
Preview
Text
bg-12-4209-2015.pdf - Published Version
Available under License Creative Commons: Attribution 3.0.

Download (953Kb) | Preview
[img]
Preview
Text
bg-12-4209-2015-supplement.pdf - Supplemental Material
Available under License Creative Commons: Attribution 3.0.

Download (580Kb) | Preview

Supplementary data:

Abstract

Bivalve calcification, particularly of the early larval stages, is highly sensitive to the change in ocean carbonate chemistry resulting from atmospheric CO2 uptake. Earlier studies suggested that declining seawater [CO32−] and thereby lowered carbonate saturation affect shell production. However, disturbances of physiological processes such as acid-base regulation by adverse seawater pCO2 and pH can affect calcification in a secondary fashion. In order to determine the exact carbonate system component by which growth and calcification are affected it is necessary to utilize more complex carbonate chemistry manipulations. As single factors, pCO2 had no effects and [HCO3-] and pH had only limited effects on shell growth, while lowered [CO32−] strongly impacted calcification. Dissolved inorganic carbon (CT) limiting conditions led to strong reductions in calcification, despite high [CO32−], indicating that [HCO3-] rather than [CO32−] is the inorganic carbon source utilized for calcification by mytilid mussels. However, as the ratio [HCO3-] / [H+] is linearly correlated with [CO32−] it is not possible to differentiate between these under natural seawater conditions. An equivalent of about 80 μmol kg−1 [CO32−] is required to saturate inorganic carbon supply for calcification in bivalves. Below this threshold biomineralization rates rapidly decline. A comparison of literature data available for larvae and juvenile mussels and oysters originating from habitats differing substantially with respect to prevailing carbonate chemistry conditions revealed similar response curves. This suggests that the mechanisms which determine sensitivity of calcification in this group are highly conserved. The higher sensitivity of larval calcification seems to primarily result from the much higher relative calcification rates in early life stages. In order to reveal and understand the mechanisms that limit or facilitate adaptation to future ocean acidification, it is necessary to better understand the physiological processes and their underlying genetics that govern inorganic carbon assimilation for calcification.

Document Type: Article
Research affiliation: AWI
OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-P-OZ Paleo-Oceanography
OceanRep > GEOMAR > FB3 Marine Ecology > FB3-EOE-B Experimental Ecology - Benthic Ecology
Refereed: Yes
Open Access Journal?: Yes
DOI etc.: 10.5194/bg-12-4209-2015
ISSN: 1726-4170
Projects: BIOACID
Date Deposited: 03 Feb 2015 09:01
Last Modified: 12 Apr 2017 10:03
URI: http://oceanrep.geomar.de/id/eprint/27271

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...