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  • 1
    Online Resource
    Online Resource
    Abiotic conditions in cephalopod (Sepia officinalis) eggs : embryonic development at low pH and high pCO2 (2009)
    Associated volumes
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    In: Marine biology, Berlin : Springer, 1967, 156(2009), 3, Seite 515-519, 1432-1793
    In: volume:156
    In: year:2009
    In: number:3
    In: pages:515-519
    Description / Table of Contents: Low pO2 values have been measured in the perivitelline fluids (PVF) of marine animal eggs on several occasions, especially towards the end of development, when embryonic oxygen consumption is at its peak and the egg case acts as a massive barrier to diffusion. Several authors have therefore suggested that oxygen availability is the key factor leading to hatching. However, there have been no measurements of PVF pCO2 so far. This is surprising, as elevated pCO2 could also constitute a major abiotic stressor for the developing embryo. As a first attempt to fill this gap in knowledge, we measured pO2, pCO2 and pH in the PVF of late cephalopod (Sepia officinalis) eggs. We found linear relationships between embryo wet mass and pO2, pCO2 and pH. pO2 declined from 〉12 kPa to less than 5 kPa, while pCO2 increased from 0.13 to 0.41 kPa. In the absence of active accumulation of bicarbonate in the PVF, pH decreased from 7.7 to 7.2. Our study supports the idea that oxygen becomes limiting in cephalopod eggs towards the end of development; however, pCO2 and pH shift to levels that have caused significant physiological disturbances in other marine ectothermic animals. Future research needs to address the physiological adaptations that enable the embryo to cope with the adverse abiotic conditions in their egg environment.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1432-1793
    DOI: 10.1007/s00227-008-1096-7
    Language: English
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  • 2
    Online Resource
    Online Resource
    Growth and calcification in the cephalopod Sepia officinalis under elevated seawater p CO2 (2008)
    Associated volumes
    Details Availability
    In: Marine ecology progress series, Oldendorf/Luhe : Inter-Research, 1979, 373(2008), Seite 303-309, 1616-1599
    In: volume:373
    In: year:2008
    In: pages:303-309
    Description / Table of Contents: Ocean acidification and associated changes in seawater carbonate chemistry negatively influence calcification processes and depress metabolism in many calcifying marine invertebrates. We present data on the cephalopod mollusc Sepia officinalis, an invertebrate that is capable of not only maintaining calcification, but also growth rates and metabolism when exposed to elevated partial pressures of carbon dioxide (pCO 2). During a 6 wk period, juvenile S. officinalis maintained calcification under ~4000 and ~6000 ppm CO 2, and grew at the same rate with the same gross growth efficiency as did control animals. They gained approximately 4% body mass daily and increased the mass of their calcified cuttlebone by over 500%. We conclude that active cephalopods possess a certain level of pre-adaptation to long-term increments in carbon dioxide levels. Our general understanding of the mechanistic processes that limit calcification must improve before we can begin to predict what effects future ocean acidification will have on calcifying marine invertebrates.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1616-1599
    URL: http://dx.doi.org/10.3354/meps07782
    DOI: 10.3354/meps07782
    Language: English
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  • 3
    Online Resource
    Online Resource
    Acidbase regulatory ability of the cephalopod (Sepia officinalis) in response to environmental hypercapnia (2010)
    Associated volumes
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    In: Journal of comparative physiology. B, Biochemical, systemic, and environmental physiology, Berlin : Springer, 1984, 180(2010), 3, Seite 323-335, 1432-136X
    In: volume:180
    In: year:2010
    In: number:3
    In: pages:323-335
    Description / Table of Contents: Acidification of ocean surface waters by anthropogenic carbon dioxide (CO2) emissions is a currently developing scenario that warrants a broadening of research foci in the study of acidbase physiology. Recent studies working with environmentally relevant CO2 levels, indicate that some echinoderms and molluscs reduce metabolic rates, soft tissue growth and calcification during hypercapnic exposure. In contrast to all prior invertebrate species studied so far, growth trials with the cuttlefish Sepia officinalis found no indication of reduced growth or calcification performance during long-term exposure to 0.6 kPa CO2. It is hypothesized that the differing sensitivities to elevated seawater pCO2 could be explained by taxa specific differences in acidbase regulatory capacity. In this study, we examined the acidbase regulatory ability of S. officinalis in vivo, using a specially modified cannulation technique as well as 31P NMR spectroscopy. During acute exposure to 0.6 kPa CO2, S. officinalis rapidly increased its blood [HCO3 -] to 10.4 mM through active ion-transport processes, and partially compensated the hypercapnia induced respiratory acidosis. A minor decrease in intracellular pH (pHi) and stable intracellular phosphagen levels indicated efficient pHi regulation. We conclude that S. officinalis is not only an efficient acidbase regulator, but is also able to do so without disturbing metabolic equilibria in characteristic tissues or compromising aerobic capacities. The cuttlefish did not exhibit acute intolerance to hypercapnia that has been hypothesized for more active cephalopod species (squid). Even though blood pH (pHe) remained 0.18 pH units below control values, arterial O2 saturation was not compromised in S. officinalis because of the comparatively lower pH sensitivity of oxygen binding to its blood pigment. This raises questions concerning the potentially broad range of sensitivity to changes in acidbase status amongst invertebrates, as well as to the underlying mechanistic origins. Further studies are needed to better characterize the connection between acidbase status and animal fitness in various marine species.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1432-136X
    URL: http://springerlink.metapress.com/content/6414w5170m873401/?p=512f5aa9d1644226a6ec4010843d2f79&pi=0
    DOI: 10.1007/s00360-009-0412-y
    Language: English
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  • 4
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    Acid-base regulatory capacity and associated proton extrusion mechanisms in marine invertebrates: An overview (2009)
    Elsevier
    Details
    Publication Date: 2023-01-31
    Description: Anthropogenic CO2 emissions will lead to an increased average ocean pCO2 of potentially 1900 ppm (ca. 0.2 kPa) by the year 2300 (Caldeira and Wickett 2003). Associated shifts in carbonate system speciation will cause ocean pH to fall by a maximum of 0.5–0.8 units. Most existing studies suggest that organisms/taxa with high standard metabolic rates, highly sophisticated convection systems and efficient gas exchange organs are coping best with elevated ocean pCO2. Typically, these taxa (decapod crustaceans, and cephalopods) are able to rapidly compensate extracellular pH by accumulating large amounts of bicarbonate. The underlying molecular machinery for this accumulatory response is still largely unknown for most marine invertebrate taxa. Thus, we will briefly review (a) acid-base regulatory responses in a range of marine invertebrates (bivalves, echinoderms, crustacea, and cephalopoda) and then (b) highlight and discuss their main ion-regulatory organs and potential acid-base regulatory proteins. In addition, we will present results from ongoing gene expression studies that specifically target transcripts relevant for ion- and acid-base regulation in the gill of the cephalopod Sepia officinalis, the crustacean Carcinus maenas and pluteus larvae of the sea urchin Strongylocentrotus purpuratus in response to environmental hypercapnia.
    Type: Article , PeerReviewed
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  • 5
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    Adaptation of a globally important coccolithophore to ocean warming and acidification (2014)
    Nature Publishing Group
    In:  Nature Climate Change, 4 (11). pp. 1024-1030.
    Details
    Publication Date: 2019-09-23
    Description: Although ocean warming and acidification are recognized as two major anthropogenic perturbations of today’s oceans we know very little about how marine phytoplankton may respond via evolutionary change. We tested for adaptation to ocean warming in combination with ocean acidification in the globally important phytoplankton species Emiliania huxleyi. Temperature adaptation occurred independently of ocean acidification levels. Growth rates were up to 16% higher in populations adapted for one year to warming when assayed at their upper thermal tolerance limit. Particulate inorganic (PIC) and organic (POC) carbon production was restored to values under present-day ocean conditions, owing to adaptive evolution, and were 101% and 55% higher under combined warming and acidification, respectively, than in non-adapted controls. Cells also evolved to a smaller size while they recovered their initial PIC:POC ratio even under elevated CO2. The observed changes in coccolithophore growth, calcite and biomass production, cell size and elemental composition demonstrate the importance of evolutionary processes for phytoplankton performance in a future ocean.
    Type: Article , PeerReviewed
    Format: text
    Format: text
    DOI: 10.1038/NCLIMATE2379
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  • 6
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    A unifying concept of coccolithophore sensitivity to changing carbonate chemistry embedded in an ecological framework (2015)
    Elsevier
    In:  Progress in Oceanography, 135 . pp. 125-138.
    Details
    Publication Date: 2017-04-12
    Description: Highlights • Calcification rates are stimulated by CO2 and HCO3− and inhibited by H+. • This novel substrate–inhibitor concept is tested with experimental data. • The concept enables us to reconcile conflicting results among laboratory studies. • We illustrate how this physiological concept can be included in ecological theory. • We apply the concept to discuss coccolithophore dispersal in the oceans. Abstract Coccolithophores are a group of unicellular phytoplankton species whose ability to calcify has a profound influence on biogeochemical element cycling. Calcification rates are controlled by a large variety of biotic and abiotic factors. Among these factors, carbonate chemistry has gained considerable attention during the last years as coccolithophores have been identified to be particularly sensitive to ocean acidification. Despite intense research in this area, a general concept harmonizing the numerous and sometimes (seemingly) contradictory responses of coccolithophores to changing carbonate chemistry is still lacking to date. Here, we present the “substrate–inhibitor concept” which describes the dependence of calcification rates on carbonate chemistry speciation. It is based on observations that calcification rate scales positively with bicarbonate (HCO3−), the primary substrate for calcification, and carbon dioxide (CO2), which can limit cell growth, whereas it is inhibited by protons (H+). This concept was implemented in a model equation, tested against experimental data, and then applied to understand and reconcile the diverging responses of coccolithophorid calcification rates to ocean acidification obtained in culture experiments. Furthermore, we (i) discuss how other important calcification-influencing factors (e.g. temperature and light) could be implemented in our concept and (ii) embed it in Hutchinson’s niche theory, thereby providing a framework for how carbonate chemistry-induced changes in calcification rates could be linked with changing coccolithophore abundance in the oceans. Our results suggest that the projected increase of H+ in the near future (next couple of thousand years), paralleled by only a minor increase of inorganic carbon substrate, could impede calcification rates if coccolithophores are unable to fully adapt. However, if calcium carbonate (CaCO3) sediment dissolution and terrestrial weathering begin to increase the oceans’ HCO3− and decrease its H+ concentrations in the far future (10–100 kyears), coccolithophores could find themselves in carbonate chemistry conditions which may be more favorable for calcification than they were before the Anthropocene.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1016/j.pocean.2015.04.012
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  • 7
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    Influence of Temperature, Hypercapnia, and Development on the Relative Expression of Different Hemocyanin Isoforms in the Common CuttlefishSepia officinalis (2012)
    Wiley
    In:  Journal of Experimental Zoology Part A: Ecological Genetics and Physiology, 317 (8). pp. 511-523.
    Details
    Publication Date: 2019-09-23
    Description: The cuttlefish Sepia officinalis expresses several hemocyanin isoforms with potentially different pH optima, indicating their reliance on efficient pH regulation in the blood. Ongoing ocean warming and acidification could influence the oxygen-binding properties of respiratory pigments in ectothermic marine invertebrates. This study examined whether S. officinalis differentially expresses individual hemocyanin isoforms to maintain optimal oxygen transport during development and acclimation to elevated seawater pCO2 and temperature. Using quantitative PCR, we measured relative mRNA expression levels of three different hemocyanin isoforms in several ontogenetic stages (embryos, hatchlings, juveniles, and adults), under different temperatures and elevated seawater pCO2. Our results indicate moderately altered hemocyanin expression in all embryonic stages acclimated to higher pCO2, while hemocyanin expression in hatchlings and juveniles remained unaffected. During the course of development, total hemocyanin expression increased independently of pCO2 or thermal acclimation status. Expression of isoform 3 is reported for the first time in a cephalopod in this study and was found to be generally low but highest in the embryonic stages (0.2% of total expression). Despite variable hemocyanin expression, hemolymph total protein concentrations remained constant in the experimental groups. Our data provide first evidence that ontogeny has a stronger influence on hemocyanin isoform expression than the environmental conditions chosen, and they suggest that hemocyanin protein abundance in response to thermal acclimation is regulated by post-transcriptional/translational rather than by transcriptional modifications
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1002/jez.1743
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  • 8
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    Genome and low-iron response of an oceanic diatom adapted to chronic iron limitation (2012)
    BioMed Central
    In:  Genome Biology, 13 (7). R66.
    Details
    Publication Date: 2019-09-23
    Description: ABSTRACT: BACKGROUND: Biogeochemical elemental cycling is driven by primary production of biomass via phototrophic phytoplankton growth, with 40% of marine productivity being assigned to diatoms. Phytoplankton growth is widely limited by the availability of iron, an essential component of the photosynthetic apparatus. The oceanic diatom Thalassiosira oceanica shows a remarkable tolerance to low-iron conditions and was chosen as a model for deciphering the cellular response upon shortage of this essential micronutrient. RESULTS: The combined efforts in genomics, transcriptomics and proteomics reveal an unexpected metabolic flexibility in response to iron availability for T. oceanica CCMP1005. The complex response comprises cellular retrenchment as well as remodeling of bioenergetic pathways, where the abundance of iron-rich photosynthetic proteins is lowered, whereas iron-rich mitochondrial proteins are preserved. As a consequence of iron deprivation, the photosynthetic machinery undergoes a remodeling to adjust the light energy utilization with the overall decrease in photosynthetic electron transfer complexes. CONCLUSIONS: Beneficial adaptations to low-iron environments include strategies to lower the cellular iron requirements and to enhance iron uptake. A novel contribution enhancing iron economy of phototrophic growth is observed with the iron-regulated substitution of three metal-containing fructose-bisphosphate aldolases involved in metabolic conversion of carbohydrates for enzymes that do not contain metals. Further, our data identify candidate components of a high-affinity iron-uptake system, with several of the involved genes and domains originating from duplication events. A high genomic plasticity, as seen from the fraction of genes acquired through horizontal gene transfer, provides the platform for these complex adaptations to a low-iron world.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    DOI: 10.1186/gb-2012-13-7-r66
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  • 9
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    Future ocean acidification will be amplified by hypoxia in coastal habitats (2013)
    Springer
    In:  Marine Biology, 160 . pp. 1875-1888.
    Details
    Publication Date: 2019-09-23
    Description: Ocean acidification is elicited by anthropogenic carbon dioxide emissions and resulting oceanic uptake of excess CO2 and might constitute an abiotic stressor powerful enough to alter marine ecosystem structures. For surface waters in gas-exchange equilibrium with the atmosphere, models suggest increases in CO2 partial pressure (pCO2) from current values of ca. 390 μatm to ca. 700–1,000 μatm by the end of the century. However, in typically unequilibrated coastal hypoxic regions, much higher pCO2 values can be expected, as heterotrophic degradation of organic material is necessarily related to the production of CO2 (i.e., dissolved inorganic carbon). Here, we provide data and estimates that, even under current conditions, maximum pCO2 values of 1,700–3,200 μatm can easily be reached when all oxygen is consumed at salinities between 35 and 20, respectively. Due to the nonlinear nature of the carbonate system, the approximate doubling of seawater pCO2 in surface waters due to ocean acidification will most strongly affect coastal hypoxic zones as pCO2 during hypoxia will increase proportionally: we calculate maximum pCO2 values of ca. 4,500 μatm at a salinity of 20 (T = 10 °C) and ca. 3,400 μatm at a salinity of 35 (T = 10 °C) when all oxygen is consumed. Upwelling processes can bring these CO2-enriched waters in contact with shallow water ecosystems and may then affect species performance there as well. We conclude that (1) combined stressor experiments (pCO2 and pO2) are largely missing at the moment and that (2) coastal ocean acidification experimental designs need to be closely adjusted to carbonate system variability within the specific habitat. In general, the worldwide spread of coastal hypoxic zones also simultaneously is a spread of CO2-enriched zones. The magnitude of expected changes in pCO2 in these regions indicates that coastal systems may be more endangered by future global climate change than previously thought.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1007/s00227-012-1954-1
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  • 10
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    Maintenance of coelomic fluid pH in sea urchins exposed to elevated CO2: the role of body cavity epithelia and stereom dissolution (2013)
    Springer
    In:  Marine Biology, 160 (10). pp. 2631-2645.
    Details
    Publication Date: 2019-09-23
    Description: Experimental ocean acidification leads to a shift in resource allocation and to an increased [HCO3 −] within the perivisceral coelomic fluid (PCF) in the Baltic green sea urchin Strongylocentrotus droebachiensis. We investigated putative mechanisms of this pH compensation reaction by evaluating epithelial barrier function and the magnitude of skeleton (stereom) dissolution. In addition, we measured ossicle growth and skeletal stability. Ussing chamber measurements revealed that the intestine formed a barrier for HCO3 − and was selective for cation diffusion. In contrast, the peritoneal epithelium was leaky and only formed a barrier for macromolecules. The ossicles of 6 week high CO2-acclimatised sea urchins revealed minor carbonate dissolution, reduced growth but unchanged stability. On the other hand, spines dissolved more severely and were more fragile following acclimatisation to high CO2. Our results indicate that epithelia lining the PCF space contribute to its acid–base regulation. The intestine prevents HCO3 − diffusion and thus buffer leakage. In contrast, the leaky peritoneal epithelium allows buffer generation via carbonate dissolution from the surrounding skeletal ossicles. Long-term extracellular acid–base balance must be mediated by active processes, as sea urchins can maintain relatively high extracellular [HCO3 −]. The intestinal epithelia are good candidate tissues for this active net import of HCO3 − into the PCF. Spines appear to be more vulnerable to ocean acidification which might significantly impact resistance to predation pressure and thus influence fitness of this keystone species
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1007/s00227-013-2257-x
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