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      Elevated CO 2 increases energetic cost and ion movement in the marine fish intestine

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      a , 1 , 1
      Scientific Reports
      Nature Publishing Group

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          Abstract

          Energetic costs associated with ion and acid-base regulation in response to ocean acidification have been predicted to decrease the energy available to fish for basic life processes. However, the low cost of ion regulation (6–15% of standard metabolic rate) and inherent variation associated with whole-animal metabolic rate measurements have made it difficult to consistently demonstrate such a cost. Here we aimed to gain resolution in assessing the energetic demand associated with acid-base regulation by examining ion movement and O 2 consumption rates of isolated intestinal tissue from Gulf toadfish acclimated to control or 1900 μatm CO 2 (projected for year 2300). The active marine fish intestine absorbs ions from ingested seawater in exchange for HCO 3 to maintain water balance. We demonstrate that CO 2 exposure causes a 13% increase of intestinal HCO 3 secretion that the animal does not appear to regulate. Isolated tissue from CO 2-exposed toadfish also exhibited an 8% higher O 2 consumption rate than tissue from controls. These findings show that compensation for CO 2 leads to a seemingly maladaptive persistent base (HCO 3 ) loss that incurs an energetic expense at the tissue level. Sustained increases to baseline metabolic rate could lead to energetic reallocations away from other life processes at the whole-animal level.

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          Evidence for upwelling of corrosive "acidified" water onto the continental shelf.

          The absorption of atmospheric carbon dioxide (CO2) into the ocean lowers the pH of the waters. This so-called ocean acidification could have important consequences for marine ecosystems. To better understand the extent of this ocean acidification in coastal waters, we conducted hydrographic surveys along the continental shelf of western North America from central Canada to northern Mexico. We observed seawater that is undersaturated with respect to aragonite upwelling onto large portions of the continental shelf, reaching depths of approximately 40 to 120 meters along most transect lines and all the way to the surface on one transect off northern California. Although seasonal upwelling of the undersaturated waters onto the shelf is a natural phenomenon in this region, the ocean uptake of anthropogenic CO2 has increased the areal extent of the affected area.
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            Acidification of subsurface coastal waters enhanced by eutrophication

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              Ecophysiology. Climate change tightens a metabolic constraint on marine habitats.

              Warming of the oceans and consequent loss of dissolved oxygen (O2) will alter marine ecosystems, but a mechanistic framework to predict the impact of multiple stressors on viable habitat is lacking. Here, we integrate physiological, climatic, and biogeographic data to calibrate and then map a key metabolic index-the ratio of O2 supply to resting metabolic O2 demand-across geographic ranges of several marine ectotherms. These species differ in thermal and hypoxic tolerances, but their contemporary distributions are all bounded at the equatorward edge by a minimum metabolic index of ~2 to 5, indicative of a critical energetic requirement for organismal activity. The combined effects of warming and O2 loss this century are projected to reduce the upper ocean's metabolic index by ~20% globally and by ~50% in northern high-latitude regions, forcing poleward and vertical contraction of metabolically viable habitats and species ranges.
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                Author and article information

                Journal
                Sci Rep
                Sci Rep
                Scientific Reports
                Nature Publishing Group
                2045-2322
                29 September 2016
                2016
                : 6
                : 34480
                Affiliations
                [1 ]University of Miami- Rosenstiel School of Marine and Atmospheric Science , 4600 Rickenbacker Causeway, Miami, FL 33149, USA
                Author notes
                [*]

                Present address: University of North Texas, Department of Biological Sciences, 1511 West Sycamore, Denton, TX 76203, USA.

                Article
                srep34480
                10.1038/srep34480
                5041088
                27682149
                03b4575a-b7a3-410b-ac0f-09ae189cc882
                Copyright © 2016, The Author(s)

                This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History
                : 28 June 2016
                : 14 September 2016
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