Literature DB >> 24501056

Productivity gains do not compensate for reduced calcification under near-future ocean acidification in the photosynthetic benthic foraminifer species Marginopora vertebralis.

Sven Uthicke1, Katharina E Fabricius.   

Abstract

Changes in the seawater carbonate chemistry (ocean acidification) from increasing atmospheric carbon dioxide (CO2 ) concentrations negatively affect many marine calcifying organisms, but may benefit primary producers under dissolved inorganic carbon (DIC) limitation. To improve predictions of the ecological effects of ocean acidification, the net gains and losses between the processes of photosynthesis and calcification need to be studied jointly on physiological and population levels. We studied productivity, respiration, and abundances of the symbiont-bearing foraminifer species Marginopora vertebralis on natural CO2 seeps in Papua New Guinea and conducted additional studies on production and calcification on the Great Barrier Reef (GBR) using artificially enhanced pCO2 . Net oxygen production increased up to 90% with increasing pCO2 ; temperature, light, and pH together explaining 61% of the variance in production. Production increased with increasing light and increasing pCO2 and declined at higher temperatures. Respiration was also significantly elevated (~25%), whereas calcification was reduced (16-39%) at low pH/high pCO2 compared to present-day conditions. In the field, M. vertebralis was absent at three CO2 seep sites at pHTotal levels below ~7.9 (pCO2 ~700 μatm), but it was found in densities of over 1000 m(-2) at all three control sites. The study showed that endosymbiotic algae in foraminifera benefit from increased DIC availability and may be naturally carbon limited. The observed reduction in calcification may have been caused either by increased energy demands for proton pumping (measured as elevated rates of respiration) or by stronger competition for DIC from the more productive symbionts. The net outcome of these two competing processes is that M. vertebralis cannot maintain populations under pCO2 exceeding 700 μatm, thus are likely to be extinct in the next century.
© 2012 Blackwell Publishing Ltd.

Entities:  

Keywords:  calcification; extinctions; ocean acidification; physiology; population consequences; production; shallow CO2 seeps

Year:  2012        PMID: 24501056     DOI: 10.1111/j.1365-2486.2012.02715.x

Source DB:  PubMed          Journal:  Glob Chang Biol        ISSN: 1354-1013            Impact factor:   10.863


  12 in total

1.  In situ developmental responses of tropical sea urchin larvae to ocean acidification conditions at naturally elevated pCO2 vent sites.

Authors:  Miles D Lamare; Michelle Liddy; Sven Uthicke
Journal:  Proc Biol Sci       Date:  2016-11-30       Impact factor: 5.349

2.  Ocean acidification induces biochemical and morphological changes in the calcification process of large benthic foraminifera.

Authors:  Martina Prazeres; Sven Uthicke; John M Pandolfi
Journal:  Proc Biol Sci       Date:  2015-03-22       Impact factor: 5.349

3.  Probabilistic risk assessment of the effect of acidified seawater on development stages of sea urchin (Strongylocentrotus droebachiensis).

Authors:  Wei-Yu Chen; Hsing-Chieh Lin
Journal:  Environ Sci Pollut Res Int       Date:  2018-02-24       Impact factor: 4.223

4.  The O2, pH and Ca2+ microenvironment of benthic foraminifera in a high CO2 world.

Authors:  Martin S Glas; Katharina E Fabricius; Dirk de Beer; Sven Uthicke
Journal:  PLoS One       Date:  2012-11-15       Impact factor: 3.240

5.  The coral reef-dwelling Peneroplis spp. shows calcification recovery to ocean acidification conditions.

Authors:  Laurie M Charrieau; Yukiko Nagai; Katsunori Kimoto; Delphine Dissard; Beatrice Below; Kazuhiko Fujita; Takashi Toyofuku
Journal:  Sci Rep       Date:  2022-04-16       Impact factor: 4.379

6.  Impacts of ocean acidification on early life-history stages and settlement of the coral-eating sea star Acanthaster planci.

Authors:  Sven Uthicke; Danilo Pecorino; Rebecca Albright; Andrew Peter Negri; Neal Cantin; Michelle Liddy; Symon Dworjanyn; Pamela Kamya; Maria Byrne; Miles Lamare
Journal:  PLoS One       Date:  2013-12-16       Impact factor: 3.240

7.  Symbiodinium community composition in scleractinian corals is not affected by life-long exposure to elevated carbon dioxide.

Authors:  Sam H C Noonan; Katharina E Fabricius; Craig Humphrey
Journal:  PLoS One       Date:  2013-05-22       Impact factor: 3.240

8.  The physiological response of two green calcifying algae from the Great Barrier Reef towards high dissolved inorganic and organic carbon (DIC and DOC) availability.

Authors:  Friedrich Wilhelm Meyer; Nikolas Vogel; Mirta Teichberg; Sven Uthicke; Christian Wild
Journal:  PLoS One       Date:  2015-08-12       Impact factor: 3.240

9.  Oxygen metabolic responses of three species of large benthic foraminifers with algal symbionts to temperature stress.

Authors:  Kazuhiko Fujita; Takaaki Okai; Takashi Hosono
Journal:  PLoS One       Date:  2014-03-03       Impact factor: 3.240

10.  Effects of High Dissolved Inorganic and Organic Carbon Availability on the Physiology of the Hard Coral Acropora millepora from the Great Barrier Reef.

Authors:  Friedrich W Meyer; Nikolas Vogel; Karen Diele; Andreas Kunzmann; Sven Uthicke; Christian Wild
Journal:  PLoS One       Date:  2016-03-09       Impact factor: 3.240

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