Ocean acidification and the loss of phenolic substances in marine plants

Rising atmospheric CO(2) often triggers the production of plant phenolics, including many that serve as herbivore deterrents, digestion reducers, antimicrobials, or ultraviolet sunscreens. Such responses are predicted by popular models of plant defense, especially resource availability models which link carbon availability to phenolic biosynthesis. CO(2) availability is also increasing in the oceans, where anthropogenic emissions cause ocean acidification, decreasing seawater pH and shifting the carbonate system towards further CO(2) enrichment. Such conditions tend to increase seagrass productivity but may also increase rates of grazing on these marine plants. Here we show that high CO(2) / low pH conditions of OA decrease, rather than increase, concentrations of phenolic protective substances in seagrasses and eurysaline marine plants. We observed a loss of simple and polymeric phenolics in the seagrass Cymodocea nodosa near a volcanic CO(2) vent on the Island of Vulcano, Italy, where pH values decreased from 8.1 to 7.3 and pCO(2) concentrations increased ten-fold. We observed similar responses in two estuarine species, Ruppia maritima and Potamogeton perfoliatus, in in situ Free-Ocean-Carbon-Enrichment experiments conducted in tributaries of the Chesapeake Bay, USA. These responses are strikingly different than those exhibited by terrestrial plants. The loss of phenolic substances may explain the higher-than-usual rates of grazing observed near undersea CO(2) vents and suggests that ocean acidification may alter coastal carbon fluxes by affecting rates of decomposition, grazing, and disease. Our observations temper recent predictions that seagrasses would necessarily be "winners" in a high CO(2) world.     

海洋酸化效应对海水鱼类的综合影响评述

人类活动引起的大气CO2浓度的升高,除了使全球温度升高外,导致的另一个严重生态问题——海洋酸化(Ocean acidification,OA),受到社会各界包括科研界的高度重视,该领域的大部分研究结果都是在近十年才发表出来的,目前还有很多需要解决的问题。海洋酸化的研究涉及到很多学科的交叉包括化学、古生物学、生态学、生物地球化学等等。在生物学领域,海洋酸化主要围绕敏感物种,例如由碳酸钙形成贝壳或外骨骼的贝类,珊瑚礁群体等。鱼类作为海洋脊椎动物的代表生物类群,自身具有一定的酸碱平衡调节能力,但相关海洋酸化方向的研究并不是很多。尽管人们对于海洋酸化对鱼类的影响了解甚少,这并不说明海洋酸化对鱼类没有作用或者效应小,在相关研究逐步展开的同时,发现鱼类同样受到海洋酸化的危害,几乎涉及到鱼类整个生活史和几乎大部分生理过程,尤其是早期生活史的高度敏感。因此就目前国内外对此领域研究结果做综述,以期待业界同行能够对海水鱼类这个大的类群引起重视。     

Hepatic urea synthesis and pH regulation. Role of CO2, HCO3-, pH and the activity of carbonic anhydrase

In isolated perfused rat liver, urea synthesis from ammonium ions was dependent on extracellular HCO3- and CO2 concentrations when the HCO3-/CO2 ratio in the influent perfusate was constant (pH 7.4). Urea synthesis was half-maximal at HCO3- = 4 mM, CO2 = 0.19 mM and was maximal at HCO3- and CO2 concentrations above 20 mM and 0.96 mM, respectively. At physiological HCO3- (25 mM) and CO2 (1.2 mM) concentrations in the influent perfusate, acetazolamide, the inhibitor of carbonic anhydrase, inhibited urea synthesis from ammonium ions (1 mM) by 50-60% and led to a 70% decrease in citrulline tissue levels. Acetazolamide concentrations required for maximal inhibition of urea synthesis were 0.01-0.1 mM. At subphysiological HCO3- and CO2 concentrations, inhibition of urea synthesis by acetazolamide was increased up to 90%. Inhibition of urea synthesis by acetazolamide was fully overcome in the presence of unphysiologically high HCO3- and CO2 concentrations, indicating that the inhibitory effect of acetazolamide is due to an inhibition of carbonic-anhydrase-catalyzed HCO3- supply for carbamoyl-phosphate synthetase, which can be bypassed when the uncatalyzed intramitochondrial HCO3- formation from portal CO2 is stimulated in the presence of high portal CO2 concentrations. With respect to HCO3- supply of mitochondrial carbamoyl-phosphate synthetase, urea synthesis can be separated into a carbonic-anhydrase-dependent (sensitive to acetazolamide at 0.5 mM) and a carbonic-anhydrase-independent (insensitive to acetazolamide) portion. Carbonic-anhydrase-independent urea synthesis linearly increased with the portal 'total CO2 addition' (which was experimentally determined to be CO2 addition plus 0.036 HCO3- addition) and was independent of the perfusate pH. At a constant 'total CO2 addition', carbonic-anhydrase-dependent urea synthesis was strongly affected by perfusate pH and increased about threefold when the perfusate pH was raised from 6.9 to 7.8. It is concluded that the pH dependent regulation of urea synthesis is predominantly due to mitochondrial carbonic anhydrase-catalyzed HCO3- supply for carbamoyl phosphate synthesis, whereas there is no control of urea synthesis by pH at the level of the five enzymes of the urea cycle. Because HCO3- provision for carbamoyl phosphate synthetase increases with increasing portal CO2 concentrations even in the absence of carbonic anhydrase activity, susceptibility of ureogenesis to pH decreases with increasing portal CO2 concentrations. This may explain the different response of urea synthesis to chronic metabolic and chronic respiratory acidosis in vivo.     

海洋酸化生态学研究进展

工业革命以来,人类排放的大量二氧化碳引起温室效应的同时,也被海洋吸收使得全球海洋出现了严重的酸化。海洋酸化及伴随的海水碳酸盐化学体系的变化对海洋生物产生深远的影响。以海洋酸化对钙化作用和光合作用的影响为重点,总结了近年来关于海洋酸化的研究,介绍了海洋中不同生态系统对海洋酸化的响应。一方面,海水中CO23-浓度和碳酸钙饱和度的降低对海洋钙化生物造成严重损害,生活在高纬的冷水珊瑚和翼足目等文石生产者是最早的受害者;贝类和棘皮动物在钙化早期对海洋酸化尤其敏感,其幼体存活率受到海洋酸化的严重制约。另一方面,CO2浓度的增加能促进海洋植物的光合作用和生长,增加初级生产力,改变浮游植物的群落组成。此外,海洋酸化可以促进固氮和脱氮作用同时削弱硝化作用,改变溶氧浓度分布和金属的生物可利用性,从而对海洋生物产生间接影响。海洋酸化对海洋生态系统的影响机制复杂,影响程度深远。为了能准确的评估海洋酸化的生态学效应,需要更全面深入的研究。     

The response of marine picoplankton to ocean acidification

Since industrialization global CO(2) emissions have increased, and as a consequence oceanic pH is predicted to drop by 0.3-0.4 units before the end of the century - a process coined 'ocean acidification'. Consequently, there is significant interest in how pH changes will affect the ocean's biota and integral processes. We investigated marine picoplankton (0.2-2?μm diameter) community response to predicted end of century CO(2) concentrations, via a 'high-CO(2) ' (～?750?ppm) large-volume (11?000?l) contained seawater mesocosm approach. We found little evidence of changes occurring in bacterial abundance or community composition due to elevated CO(2) under both phytoplankton pre-bloom/bloom and post-bloom conditions. In contrast, significant differences were observed between treatments for a number of key picoeukaryote community members. These data suggested a key outcome of ocean acidification is a more rapid exploitation of elevated CO(2) levels by photosynthetic picoeukaryotes. Thus, our study indicates the need for a more thorough understanding of picoeukaryote-mediated carbon flow within ocean acidification experiments, both in relation to picoplankton carbon sources, sinks and transfer to higher trophic levels.     

Effects of the peptide toxin from Microcystis aeruginosa on intracellular calcium,pH and membrane integrity in mammalian cells

Extracts of water blooms of the toxic cyanobacterium Microcystis aeruginosa showed a range of toxicities not related to their ability to lyse mammalian red cells. The HPLC-purified heptapeptide toxin (mol. wt. 1035) from Microcystis did not lyse red cells at up to 500-fold higher concentrations than that required to kill mice. This toxin (LD₅₀ 110 μg/kg for male mice) was used to investigate in vitro effects on isolated thymocytes, hepatocytes, mammary alveolar cells, and cultured Swiss 3T3 fibroblasts. Thymocytes were stimulated to progressive Ca²⁺ entry by toxin (0.1–10 μg/ml), reaching a peak after approx. 5 min. No deformation, intracellular pH change, Trypan Blue entry or cell lysis was seen within 60 min at 37°C. Hepatocytes were grossly deformed by the toxin, with a dose/response relationship between 0.1 and 1.0 μg/ml. No progressive Ca²⁺ entry was observed on toxin addition, instead a rapid rise in intracellular Ca²⁺, presumably from intracellular sources. No change in intracellular pH, Trypan Blue exclusion or cell lysis was observed over 60 min. Mammary alveolar cells and 3T3 fibroblasts were unresponsive to toxin at the concentrations tested. No change in protein synthesis or nucleic acid synthesis in thymocytes was observed after culture with 0.5 or 5.0 μg/ml toxin. It was concluded that cytoskeletal changes in deformed hepatocytes (the target cells in vivo) demonstrated the most probable cellular basis for toxicity, rather than changes in membrane permeability or cell metabolism.     

Effects of seawater acidification on cell cycle control mechanisms in Strongylocentrotus purpuratus embryos

Previous studies have shown fertilization and development of marine species can be significantly inhibited when the pH of sea water is artificially lowered. Little mechanistic understanding of these effects exists to date, but previous work has linked developmental inhibition to reduced cleavage rates in embryos. To explore this further, we tested whether common cell cycle checkpoints were involved using three cellular biomarkers of cell cycle progression: (1) the onset of DNA synthesis, (2) production of a mitotic regulator, cyclin B, and (3) formation of the mitotic spindle. We grew embryos of the purple sea urchin, Strongylocentrotus purpuratus, in seawater artifically buffered to a pH of ～7.0, 7.5, and 8.0 by CO(2) infusion. Our results suggest the reduced rates of mitotic cleavage are likely unrelated to common cell cycle checkpoints. We found no significant differences in the three biomarkers assessed between pH treatments, indicating the embryos progress through the G(1)/S, G(2)/M and metaphase/anaphase transitions at relatively similar rates. These data suggest low pH environments may not impact developmental programs directly, but may act through secondary mechanisms such as cellular energetics.     

High CO2 and silicate limitation synergistically increase the toxicity of Pseudo-nitzschia fraudulenta

Anthropogenic CO(2) is progressively acidifying the ocean, but the responses of harmful algal bloom species that produce toxins that can bioaccumulate remain virtually unknown. The neurotoxin domoic acid is produced by the globally-distributed diatom genus Pseudo-nitzschia. This toxin is responsible for amnesic shellfish poisoning, which can result in illness or death in humans and regularly causes mass mortalities of marine mammals and birds. Domoic acid production by Pseudo-nitzschia cells is known to be regulated by nutrient availability, but potential interactions with increasing seawater CO(2) concentrations are poorly understood. Here we present experiments measuring domoic acid production by acclimatized cultures of Pseudo-nitzschia fraudulenta that demonstrate a strong synergism between projected future CO(2) levels (765 ppm) and silicate-limited growth, which greatly increases cellular toxicity relative to growth under modern atmospheric (360 ppm) or pre-industrial (200 ppm) CO(2) conditions. Cellular Si:C ratios decrease with increasing CO(2), in a trend opposite to that seen for domoic acid production. The coastal California upwelling system where this species was isolated currently exhibits rapidly increasing levels of anthropogenic acidification, as well as widespread episodic silicate limitation of diatom growth. Our results suggest that the current ecosystem and human health impacts of toxic Pseudo-nitzschia blooms could be greatly exacerbated by future ocean acidification and 'carbon fertilization' of the coastal ocean.     

海洋酸化条件下Cd2+和Hg2+对斧文蛤幼贝急性毒性效应

为研究在海洋酸化条件下重金属污染物对滩涂贝类的影响,采用半静态急性毒性实验的研究方法,利用海洋酸化人工模拟系统,分析了不同酸化条件下(对照组pH 8.20、酸化组pH分别为7.80、7.60和7.40)Cd2+和Hg2+对斧文蛤(Meretrix lamarckii)幼贝急性毒性效应的影响。实验结果表明:在实验设定的海洋酸化范围内,单一的海洋酸化对斧文蛤幼贝的存活没有显著性影响,但海洋酸化显著增强了Cd2+和Hg2+的急性毒性。与对照组相比,酸化组Cd2+和Hg2+的毒性随着酸化程度的加剧而呈现出逐渐增强的趋势; Cd2+和Hg2+均在pH 7.40时对斧文蛤的毒性最强,其96h半致死(96h LC50)浓度分别为4.068 mg/L(Cd2+)和10.332 mg/L(Hg2+),明显低于pH 8.20、7.80和7.60时其对斧文蛤幼贝的96h LC50浓度(其值分别为Cd2+ 6.458、5.947、4.728 mg/L和Hg2+ 12.027、11.169、10.595 mg/L)。研究有助于丰富海洋酸化与重金属毒理作用在海洋贝类中的研究内容,为斧文蛤资源恢复和海洋环境保护提供科学依据。     

Effects of seawater acidification on Diopatra neapolitana (Polychaete,Onuphidae): Biochemical and regenerative capacity responses

Changes in atmospheric CO₂ concentrations and, consequently, ocean acidification, together with changes in seawater chemistry, are likely to have a large impact on marine ecosystems. Much of the current research concerning the consequences of ocean acidification has been limited to organisms dependent on the availability of carbonate ions in seawater, especially bivalves. Nevertheless, many marine organisms do not rely on calcium carbonate structures, such as most of the polychaete species that might also be affected by seawater acidification. However the effects of ocean acidification on these organisms are almost unknown. Thus, in the present study, the effects of pH decrease were studied in the polychaete Diopatra neapolitana, using tissue regenerative capacity and biochemical alterations as biomarkers. The results obtained revealed that individuals exposed for 28 days to low pH levels (7.5, 7.3, 7.1) exhibited lower capacity to regenerate their body, in comparison to control organisms (pH 7.8). This study also evidenced that seawater acidification induced oxidative stress in D. neapolitana, with individuals under lower pH levels showing higher LPO, lower GSH/GSSG values and higher enzymatic activity (CAT, SOD and GSTs). Additionally, organisms exposed to low pH presented significantly lower glycogen and protein content. Thus, the present work revealed the effects of pH on the polychaete species D. neapolitana, both at physiological and biochemical levels. Furthermore, our results validate the use of D. neapolitana as a test organism in laboratory-based bioassays, and also as an adequate bioindicator species to pH decrease in the environment. Finally, the regenerative capacity appears to be a promising endpoint to evaluate the effects of pH on D. neapolitana.     

Effect of low level zinc pretreatment on zinc-mediated toxicity in different lung cell lines

Reduced toxicity of high zinc exposure was observed after pretreatment of various lung cells with nonlethal zinc concentrations. This effect became significant when various parameters of cytotoxicity were assessed (e.g., inhibition of protein synthesis, depletion of reduced glutathione [GSH], increase of oxidized glutathione [GSSG], release of lactate dehydrogenase [LDH]). Similar protective effects by zinc have already been shown by several investigators for a variety of toxicity studies dealing with cadmium, in vitro and in vivo. Zinc-induced toxicity has been linked to glutathione metabolism and cellular GSH contents. Activity of glutathione reductase (GR) and rates of glutathione synthesis were identified as determinants of zinc (cyto)toxicity. However, these variables were virtually unaffected in our adapted cells. Consequently, another variable appears to be crucial for modulating cellular suscepticibility in zinc pretreated cells. Protection in our cells was achieved by pretreatment with 80–120 μmol/L zinc chloride for 24–72 h, roughly 10-fold more zinc in the medium than is normally found in human plasma. Protection was not observed when the cells were concomitantly exposed to cycloheximide, an inhibitor of protein synthesis, or actinomycin D, an inhibitor of RNA synthesis, but it was found in the presence of amanitin, an inhibitor of mRNA synthesis. It is therefore concluded that the altered zinc tolerance of pretreated cells is not attributable to the induction of metallothionein.     

H<Subscript>2</Subscript> enrichment from synthesis gas by <Emphasis Type="Italic">Desulfotomaculum</Emphasis><Emphasis Type="Italic">carboxydivorans</Emphasis> for potential applications in synthesis gas purification and biodesulfurization

Desulfotomaculum carboxydivorans, recently isolated from a full-scale anaerobic wastewater treatment facility, is a sulfate reducer capable of hydrogenogenic growth on carbon monoxide (CO). In the presence of sulfate, the hydrogen formed is used for sulfate reduction. The organism grows rapidly at 200 kPa CO, pH 7.0, and 55°C, with a generation time of 100 min, producing nearly equimolar amounts of H₂ and CO₂ from CO and H₂O. The high specific CO conversion rates, exceeding 0.8 mol CO (g protein)⁻¹ h⁻¹, makes this bacterium an interesting candidate for a biological alternative of the currently employed chemical catalytic water–gas shift reaction to purify synthesis gas (contains mainly H₂, CO, and CO₂). Furthermore, as D. carboxydivorans is capable of hydrogenotrophic sulfate reduction at partial CO pressures exceeding 100 kPa, it is also a good candidate for biodesulfurization processes using synthesis gas as electron donor at elevated temperatures, e.g., in biological flue gas desulfurization. Although high maximal specific sulfate reduction rates (32 mmol (g protein)⁻¹ h⁻¹) can be obtained, its sulfide tolerance is rather low and pH dependent, i.e., maximally 9 and 5 mM sulfide at pH 7.2 and pH 6.5, respectively.     

Acclimation of ion regulatory capacities in gills of marine fish under environmental hypercapnia

The preservation of ion balance and pH despite environmental fluctuations is essential for the maintenance of vital cellular functions. While several ion transporters contribute to acid-base regulation in fish, the involvement and expression of key transporters under hypercapnia remain to be established. Here, two members of the HCO(3)(-) transporter family (Na(+)/HCO(3)(-) cotransporter NBC1 and Cl(-)/HCO(3)(-) exchanger AE1) were described for the first time in gills of marine fish. Benthic eelpout Zoarces viviparus were acclimated to 10,000 ppm CO(2). Hypercapnia did not affect whole animal oxygen consumption over a period of 4 days. During a time series of 6 wk NBC1 mRNA levels first decreased by about 40% (8 to 24 h) but finally increased about threefold over control. mRNA expression of AE1 decreased transiently by 50% at day 4 but recovered to control levels only. Reduced mRNA levels were also found for two Na(+)/H(+) exchangers (NHE1A, NHE1B) during the first days (by 50-60% at days 1 and 2), followed by restoration of control levels. This pattern was mirrored in a slight decrease of NHE1 protein contents and its subsequent recovery. In contrast, Na(+)-K(+)-ATPase mRNA and protein contents, as well as maximum activity, rose steadily from the onset of hypercapnia, and reached up to twofold control levels at the end. These results indicate shifting acclimation patterns between short- and long-term CO(2) exposures. Overall, ion gradient-dependent transporter mRNA levels were transiently downregulated in the beginning of the disturbance. Upregulation of NBC1 on long timescales stresses the importance of this transporter in the hypercapnia response of marine teleosts. Long-term rearrangements include Na(+)-K(+)-ATPase at higher densities and capacities, indicating a shift to elevated rates of ion and acid-base regulation under environmental hypercapnia.     

Inorganic carbon acquisition in red tide dinoflagellates

Carbon acquisition was investigated in three marine bloom-forming dinollagellates-Prorocentrum minimum, Heterocapsa triquetra and Ceratium lineatum. In vivo activities of extracellular and intracellular carbonic anhydrase (CA), photosynthetic O2 evolution, CO2 and HCO3- uptake rates were measured by membrane inlet mass spectrometry (MIMS) in cells acclimated to low pH (8.0) and high pH (8.5 or 9.1). A second approach used short-term 14C-disequilibrium incubations to estimate the carbon source utilized by the cells. All three species showed negligible extracellular CA (eCA) activity in cells acclimated to low pH and only slightly higher activity when acclimated to high pH. Intracellular CA (iCA) activity was present in all three species, but it increased only in P. minimum with increasing pH. Half-saturation concentrations (K1/2) for photosynthetic O2 evolution were low compared to ribulose 1,5-bisphosphate carboxylase/oxygenase (Rubisco) kinetics. Moreover, apparent affinities for inorganic carbon (Ci) increased with increasing pH in the acclimation, indicating the operation of an efficient CO2 concentration mechanism (CCM) in these dinoflagellates. Rates of CO2 uptake were comparably low and could not support the observed rates of photosynthesis. Consequently, rates of HCO3- uptake were high in the investigated species, contributing more than 80% of the photosynthetic carbon fixation. The affinity for HCO3- and maximum uptake rates increased under higher pH. The strong preference for HCO3- was also confirmed by the 14C-disequilibrium technique. Modes of carbon acquisition were consistent with the 13C-fractionation pattern observed and indicated a strong species-specific difference in leakage. These results suggest that photosynthesis in marine dinoflagellates is not limited by Ci even at high pH, which may occur during red tides in coastal waters.     

The relation between intracellular pH and rate of protein synthesis in sea urchin eggs and the existence of a pH-independent event triggered by ammonia

The relation between rate of protein synthesis and intracellular pH (pHi) was investigated in the eggs of the sea urchin Strongylocentrotus purpuratus. Increasing external pH (pHo) resulted in raising pHi of eggs and also in increased rate of protein synthesis. Similarly, at constant pHo, adding various concentrations of NH4Cl to eggs caused graded increases of both pHi and protein synthesis. Using various concentrations of NH4Cl at a low pHo and incubating eggs at high pHo, we compared protein synthesis under similar pHi conditions and this revealed that at least half the increased protein synthesis stimulated by NH4Cl is independent of induced rise of pHi, as also seems to be chromosome condensation which was never observed in eggs incubated at high pHoS. The additional pH-independent event triggered by NH4Cl does not appear related to elevated free Ca2+, since protein synthesis and chromosome condensation do not require external Ca2+ and no increases of free Ca2+ sufficient to activate the Ca2+-calmodulin-mediated enzyme NAD kinase occurred. Monensin disrupts intravesicular pH gradients but does not stimulate protein synthesis, indicating that this local effect, also promoted by NH4Cl, is not involved in ammonia-induced increase of protein synthesis. Using two other amines which have low pKa values, benzocaine and tricaine, we observed 2-fold increases in protein synthesis rates, even though pHi was lowered. While the exact nature of the pH-independent event(s) triggered by NH4Cl, and possibly by other amines, remains unidentified, its possible involvement in normal mitosis is stressed.     

Influence of CO2 and pH on the attachment response of the cercaria of Diplostomum spathaceum (trematoda) (author's transl)]

1. The attachment of the cercaria to artificial substrates (offered via dialyzing membranes) in definite media was investigated under conditions of variable pH and [CO2]. 2. A decrease of the pH of the substrate releases only attachments in CO2 containing media and consequently acts via CO2 systems of the medium. 3. As effective components of CO2 systems, dissolved CO2 + H2CO3 are confirmed. 4. The sensitivity of the reaction on gradients of the CO2 partial pressure (in solution) could be established by offering substrates with lowered pH in CO2 containing media. Thus, by raising the CO2 partial pressure from ca. 0,04% to 0,15% maximal fixation rates were obtained (Fig. 3). 5. The carboanhydrase inhibitor acetazolamide, when added to the medium, had no direct influence on the CO2 receptors.     

Impacts of increased atmospheric CO_2 concentration on photosynthesis and growth of micro-and macro-algae

Marine photosynthesis drives the oceanic biological CO2 pump to absorb CO2 from the atmosphere, which sinks more than one third of the industry-originated CO2 into the ocean. The increasing atmos-pheric CO2 and subsequent rise of pCO2 in seawater, which alters the carbonate system and related chemical reactions and results in lower pH and higher HCO3- concentration, affect photosynthetic CO2 fixation processes of phytoplanktonic and macroalgal species in direct and/or indirect ways. Although many unicellular and multicellular species can operate CO2-concentrating mechanisms (CCMs) to util-ize the large HCO3- pool in seawater, enriched CO2 up to several times the present atmospheric level has been shown to enhance photosynthesis and growth of both phytoplanktonic and macro-species that have less capacity of CCMs. Even for species that operate active CCMs and those whose photo-synthesis is not limited by CO2 in seawater, increased CO2 levels can down-regulate their CCMs and therefore enhance their growth under light-limiting conditions (at higher CO2 levels, less light energy is required to drive CCM). Altered physiological performances under high-CO2 conditions may cause genetic alteration in view of adaptation over long time scale. Marine algae may adapt to a high CO2 oceanic environment so that the evolved communities in future are likely to be genetically different from the contemporary communities. However, most of the previous studies have been carried out under indoor conditions without considering the acidifying effects on seawater by increased CO2 and other interacting environmental factors, and little has been documented so far to explain how physi-ology of marine primary producers performs in a high-CO2 and low-pH ocean.     

高浓度CO2引起的海水酸化对小珊瑚藻光合作用和钙化作用的影响

为了探讨CO2海底封存潜在的渗漏危险对于海洋生物的可能影响,以大型钙化藻类小珊瑚藻(Corallina pilulifera)为研究对象,在室内控光控温条件下,通过向培养海水充入CO2气体得到3种不同酸化程度的培养条件(pH 8.1、6.8和5.5),24h后比较藻体光合作用和钙化作用情况。结果显示:相对于自然海水培养条件(pH 8.1),在pH 6.8条件下培养的小珊瑚藻光合固碳速率得到了增强,而在pH 5.5条件下光合固碳速率则降低;随着酸化程度的增强,藻体的钙化固碳速率越来越低,在pH 5.5条件下甚至表现为负值[(-2.53±0.57)mg C g-1干重h-1];藻体颗粒无机碳(PIC)和颗粒有机碳(POC)含量的比值随着酸化程度的加强而降低,这反映了酸化对光合和钙化作用的综合效应。快速光反应曲线的测定结果显示:随着酸化程度的增强,强光引起的光抑制程度越来越强;在酸化条件下,藻体的光饱和点显著降低,但pH 6.8和5.5之间没有显著差异;低光下的电子传递速率在pH 8.1和6.8之间没有显著差异,pH 5.5培养条件下显著降低;最大电子传递速率在pH 6.8时最大,在pH 5.5时最低。以上结果说明,高浓度CO2引起的海水酸化显著地影响着小珊瑚藻的光合和钙化过程,不同的酸化程度下,藻体的光合、钙化反应不同,在较强的酸化程度下(pH 5.5),藻体的光合和钙化过程都将受到强烈的抑制,这些结果为认识CO2海底封存渗漏危险对海洋钙化藻类的可能影响提供了理论参考。     

Calcification rates and the effect of ocean acidification on Mediterranean cold-water corals

Global environmental changes, including ocean acidification, have been identified as a major threat to scleractinian corals. General predictions are that ocean acidification will be detrimental to reef growth and that 40 to more than 80 per cent of present-day reefs will decline during the next 50 years. Cold-water corals (CWCs) are thought to be strongly affected by changes in ocean acidification owing to their distribution in deep and/or cold waters, which naturally exhibit a CaCO(3) saturation state lower than in shallow/warm waters. Calcification was measured in three species of Mediterranean cold-water scleractinian corals (Lophelia pertusa, Madrepora oculata and Desmophyllum dianthus) on-board research vessels and soon after collection. Incubations were performed in ambient sea water. The species M. oculata was additionally incubated in sea water reduced or enriched in CO(2). At ambient conditions, calcification rates ranged between -0.01 and 0.23% d(-1). Calcification rates of M. oculata under variable partial pressure of CO(2) (pCO(2)) were the same for ambient and elevated pCO(2) (404 and 867 μatm) with 0.06 ± 0.06% d(-1), while calcification was 0.12 ± 0.06% d(-1) when pCO(2) was reduced to its pre-industrial level (285 μatm). This suggests that present-day CWC calcification in the Mediterranean Sea has already drastically declined (by 50%) as a consequence of anthropogenic-induced ocean acidification.     

Physiological responses to hyper-saline waters in sailfin mollies (Poecilia latipinna)

We examined the ionoregulatory physiology and biochemistry of the teleost sailfin molly (Poecilia latipinna), an inhabitant of salt marshes along the gulf coast, during exposure to hyper-saline waters (salinity range 35-95 ppt). Mollies were able to tightly control plasma Na(+) and Cl(-) concentrations and tissue water levels up to 65 ppt, but at higher salinities plasma ion levels began to rise and muscle water content dropped. Still, even at the highest salinity (90 ppt) plasma Na(+) and Cl(-) levels were only 32% and 39%, respectively, above levels at 35 ppt. Drinking rates at 60 ppt climbed 35%, while gut Na(+)/K(+)-ATPase (NAK) activity rose 70% and branchial NAK activity jumped 200%. The relatively small rise in drinking rate, in the face of a more than doubling of the osmotic gradient, suggests that a reduction in branchial water permeability significantly limited water loss and associated salt load. At 80 ppt, a salinity where plasma ion levels just begin to rise, drinking rate rose more rapidly, but gut and gill NAK activity did not, suggesting that mollies employed other pathways (perhaps renal) of salt excretion. At higher salinities, plasma ion levels continued to rise and muscle water content fell slightly indicating the beginnings of internal osmotic disturbances. To evaluate the energetic costs of hyper-salinity on mollies we measured the rate of O(2) consumption and found it rose with salinity, in sharp contrast to virtually all species previously examined. Interestingly, despite higher metabolism, growth was unaffected by hyper-salinity.