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Changes in Bioenergetics Associated with Ocean Acidification and Climate Changes | OMICS International
ISSN: 2167-7662
Bioenergetics: Open Access
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Changes in Bioenergetics Associated with Ocean Acidification and Climate Changes

Kunshan Gao*

State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, China

*Corresponding Author:
Gao K
State Key Laboratory of Marine Environmental Science
Xiamen University, Xiamen, 361005, China
Tel: +86 -2187982
Fax: +86-2187963
E-mail: [email protected]

Received date: January 10, 2017; Accepted date: February 18, 2017; Published date: February 22, 2017

Citation: Gao K (2017) Changes in Bioenergetics Associated with Ocean Acidification and Climate Changes. Bioenergetics 6:147. doi:10.4172/2167-7662.1000147

Copyright: © 2017 Gao K. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

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Ocean global changes, including CO2-triggered ocean acidification and warming as well as associated changes in physical and chemical environments affect metabolisms of marine organisms and increase their energetic demand to cope with the environmental stresses. Phytoplankton species grown under ocean acidification conditions alter their metabolic pathways, down-regulating their CO2 concentrating mechanisms, up-regulating photorespiration and heatdissipating processes and generating extra energy by degrading accumulated phenolic compounds, which are toxic and can be transferred to higher trophic levels, changing food quality. Calcifying algae, under influence of ocean acidification, need more energy to maintain their calcification and to synthesize UV screening compounds due to reduced thickness of the calcified "shell". Changes in the bioenergetics with exacerbating ocean global environmental issues will lead to ecological consequences and affect services of marine ecosystems.


Algae; Calcification; Climate change; Diatoms; Growth; Ocean acidification; Photosynthesis; Phytoplankton; Warming; UV radiation


Increasing atmospheric CO2 concentration due to combustion of fossil fuels result continuous dissolution of anthropogenic CO2 into the oceans, leading to ocean acidification (OA, declining pH in surface oceans). Increased availability of CO2 in seawater may save energy for photosynthetic CO2 fixers, but can increase energetic cost due to acidic stress caused by OA for all organisms that have adapted to the contemporary carbonate chemistry [1]. In view of the metabolic responses and associated energetics, changes in chemical and physical environments associated with OA and other ocean climate changes, such as warming and increasing exposures to solar UV radiation due to enhanced stratification (thinner upper mixing layer) for cells within this layer, may interactively (additive, synergistic or antagonistically) affect physiological processes and ecological functions of marine organisms.


Calcifying organisms are expected to need extra energy to sustain calcification processes with progressive OA, which are known to perform less efficiently under lowered pH. Corals, shellfishes and calcifying plankton as well as calcareous macroalgae usually produce thinner or less “skeleton” under OA conditions [2]. When calcifying macroalgae (such as coralline algae) and microalgae (such as coccolithorphores) are grown under OA, they calcify less and suffer more from solar UV radiation, then struggle to spend extra energy to synthesize UV-screening or absolving compounds [3,4]. The calcified coverage has been demonstrated to shield of UV irradiances by over 25% in Emiliania huxleyi [3]. Even for zooplankton and/or other noncalcifying organisms, in future oceans or some natural shallow environments today where pH is low, they need extra energy to cope with acidic stress and other stressors, such as UV and warming. Increasing temperature may help to gain the extra energy for some species at higher latitudes and may synergistically lift the costs as well.

Photosynthesis and Growth

Marine photosynthesis drives marine biological CO2 pump, that takes up over 1 million tons of CO2 on global average from the atmosphere. Since CO2 is the substrate of carboxylation, it is often thought that increased partial pressure of CO2 in seawater leads to increased CO2 availability, and therefore, enhances algal or cyanobacterial growth and stimulate primary productivity. In seaweeds (macroalgae) or seagrasses, excluding the calcifying species, this is usually true. In Nori (Porphyra yezoensis) and a green tide alga (Ulva sp.), elevated CO2 remarkably enhanced their growth [5,6], with their CO2 concentrating mechanisms (CCMs) being down-regulated. In diatoms, similar trend has been reported under laboratory conditions (low light and constant temperature), however, under high levels of sunlight, the diatoms grow much slower under the OA treatment compared to ambient CO2 condition [7]. Mechanistically, downregulation of CCMs under elevated pCO2 can save energy for active uptake of inorganic C, the saved energy could be employed to stimulate growth under light-limiting condition and to exacerbate light stress under over-saturating light levels, leading to up-regulated photorespiration. That is, the changed carbonate chemistry due to OA is supposed to increase light stress, as indicated in enhanced nonphotochemical quenching (NPQ) in surface phytoplankton assemblages in the South China Sea [7]. Nevertheless, increased NPQ under OA do not always couple with decreased growth or photosynthetic carbon fixation [6].


As global warming will cause upper mixed layer depths to decrease (enhanced surface ocean stratification) in the future ocean, plankton species within this layer will be exposed to higher daytime dose of solar radiation [8]. This in combination with OA can act synergistically to trigger additional light and/or UV stress and photo-damages, since less upward transport of nutrients would restrain the planktons to synthesize defensive proteins or components.

Performance and biochemical compositions of primary producers directly or indirectly influence secondary producers. Phytoplankton species (diatoms and coccolithorphores) grown under OA accumulate more phenolics within their cells, which lead to higher contents of phenolics in copepods who feed them [9]. This is caused by alterations in metabolic pathways (ß-oxidation and the Krebs cycle) that are considered to provide extra energy to cope with acidic stress under OA treatment (Figure 1). Since phenolics are toxic, OA impacts through food chain may affect food quality. Taste of shrimps grown under OA was shown to deteriorates [10], though there is no evidence that these shrimps had higher phenolic compounds compared to the control (ambient CO2 level). This aspect is certainly worth looking into from biochemical and molecular aspects, since degradation of extra phenolic compounds requires more related enzymes or higher activity of them, which then have imprints on expressions of genes.


Figure 1: Ocean acidification up-regulated (red) and downregulated (green) metabolic pathways in a calcifying microalga (Emiliania huxleyi) Jin et al. [9].


This work was supported by the national key research programs (2016YFA0601400) and National Natural Science Foundation (41430967; 41120164007).


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