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Relevant bibliographies by topics / Ocean acidification

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Academic literature on the topic 'Ocean acidification'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 June 2024

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Journal articles on the topic "Ocean acidification"

1

Schnoor, Jerald L. "Ocean Acidification." Environmental Science & Technology 47, no. 21 (November 5, 2013): 11919. http://dx.doi.org/10.1021/es404263h.

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Fenchel, Tom. "Ocean Acidification." Marine Biology Research 7, no. 4 (May 2011): 418–19. http://dx.doi.org/10.1080/17451000.2010.550051.

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Huo, Chuan Lin, Cheng Huo, and Dao Ming Guan. "Advances in Studies of Ocean Acidification." Applied Mechanics and Materials 295-298 (February 2013): 2191–94. http://dx.doi.org/10.4028/www.scientific.net/amm.295-298.2191.

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During the past 200 years, approximately one-half of the carbon dioxide from human activities is being taken up by the oceans. The uptake of carbon dioxide has led to a reduction of the pH value of surface seawater of 0.1 units, equivalent to a 30% increase in the concentration of hydrogen ions. If global emission of carbon dioxide from human activities continues to rise at the current rates, the average pH value of the oceans could fall by 0.5 units by the year 2100. This was equivalent to a three fold increase in the concentration of hydrogen ions. Global ocean acidification has become one of the most threatening disasters to the ocean ecosystem and has been attached great importance by the countries adjacent to oceans and the related international organizations in the world. In this paper the current situation and development of ocean acidification and the impacts of ocean acidification are described. It also summarizes the latest research achievements of ocean acidification and the ocean acidification studies in such countries as US, Europe, Japan, Australia, the Republic of Korea, and China, etc.

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Falkenberg, Laura J., Richard G. J. Bellerby, Sean D. Connell, Lora E. Fleming, Bruce Maycock, Bayden D. Russell, Francis J. Sullivan, and Sam Dupont. "Ocean Acidification and Human Health." International Journal of Environmental Research and Public Health 17, no. 12 (June 24, 2020): 4563. http://dx.doi.org/10.3390/ijerph17124563.

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The ocean provides resources key to human health and well-being, including food, oxygen, livelihoods, blue spaces, and medicines. The global threat to these resources posed by accelerating ocean acidification is becoming increasingly evident as the world’s oceans absorb carbon dioxide emissions. While ocean acidification was initially perceived as a threat only to the marine realm, here we argue that it is also an emerging human health issue. Specifically, we explore how ocean acidification affects the quantity and quality of resources key to human health and well-being in the context of: (1) malnutrition and poisoning, (2) respiratory issues, (3) mental health impacts, and (4) development of medical resources. We explore mitigation and adaptation management strategies that can be implemented to strengthen the capacity of acidifying oceans to continue providing human health benefits. Importantly, we emphasize that the cost of such actions will be dependent upon the socioeconomic context; specifically, costs will likely be greater for socioeconomically disadvantaged populations, exacerbating the current inequitable distribution of environmental and human health challenges. Given the scale of ocean acidification impacts on human health and well-being, recognizing and researching these complexities may allow the adaptation of management such that not only are the harms to human health reduced but the benefits enhanced.

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Boyd, Philip W. "Beyond ocean acidification." Nature Geoscience 4, no. 5 (April 29, 2011): 273–74. http://dx.doi.org/10.1038/ngeo1150.

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Contestabile, Monica. "Ocean acidification costs." Nature Climate Change 2, no. 3 (February 24, 2012): 146–47. http://dx.doi.org/10.1038/nclimate1439.

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Pope, Aaron, and Elizabeth Selna. "Communicating Ocean Acidification." Journal of Museum Education 38, no. 3 (October 2013): 279–85. http://dx.doi.org/10.1080/10598650.2013.11510780.

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Ridgwell, Andrew, and D. Schmidt. "Dangerous ocean acidification." IOP Conference Series: Earth and Environmental Science 6, no. 7 (February 1, 2009): 072005. http://dx.doi.org/10.1088/1755-1307/6/7/072005.

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Lan, Yilin. "The review of how ocean acidification affect organisms and ecological environment." Applied and Computational Engineering 58, no. 1 (April 30, 2024): 43–47. http://dx.doi.org/10.54254/2755-2721/58/20240689.

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The pH of our sea water is decreasing nowadays. Therefore, ocean acidification has gradually become a problem that people have to face. Human activities since Industrial Revolution are making sea water more and more acidic. Human activity has done some damage to the environment that will directly or indirectly increases the amount of hydrogen ions in seawater, which will finally make the seawater more acidic. One of the result of this changes is ocean acidification. People should start playing attention on this problem. If people do not intervene in advance to acidify the oceans, this issue can cause some consequences that will hurt our environment. The following is the main content of this paper. The reason why carbon dioxide can cause ocean acidification, effects of ocean acidification on Marine ecological environment, the shape of Balanophyllias bones changes in different PH environment and Changes in metabolic pathways of phytoplankton under ocean acidification.

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Ollier, Clifford. "The hoax of ocean acidification." Quaestiones Geographicae 38, no. 3 (September 10, 2019): 59–66. http://dx.doi.org/10.2478/quageo-2019-0029.

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Abstract A widespread alarm is sweeping the world at present about the ill effects of man-made increases in carbon dioxide (CO2) production. One aspect is that it may cause the ocean to become acid, and dissolve the carbonate skeletons of many living things including shellfish and corals. However, the oceans are not acid, never have been in geological history, and cannot become acid in the future. Changes in atmospheric CO2 cannot produce an acid ocean. Marine life depends on CO2, and some plants and animals fix it as limestone. Over geological time enormous amounts of CO2 have been sequestered by living things, and today there is far more CO2 in limestones than in the atmosphere or ocean. Carbon dioxide in seawater does not dissolve coral reefs, but is essential to their survival.

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Dissertations / Theses on the topic "Ocean acidification"

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Bednarsek, Nina. "Vulnerability of Southern ocean pteropods to anthropogenic ocean acidification." Thesis, University of East Anglia, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.533722.

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Spence, Elspeth Mairi. "Public risk perceptions of ocean acidification." Thesis, Cardiff University, 2017. http://orca.cf.ac.uk/104099/.

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Ocean acidification has been called the ‘evil twin’ of climate change and has become acknowledged as a serious risk to the marine environment. This thesis aims to explore public perceptions of ocean acidification as there is limited work on how people understand this emerging risk. It is important to engage the public because ocean acidification will contribute to how carbon emissions are addressed. The mental models approach was used to compare and examine public and expert perceptions of ocean acidification to help inform future risk communications. Many of the findings were similar to those of climate change; for example, it was not seen as a personal risk but something which would impact on the environment. Results showed that ocean acidification was unfamiliar to the public with low levels of knowledge and awareness found. People could identify possible impacts of ocean acidification but they were unsure about the main cause, stating that pollution from chemicals and industrial waste was one of the main causes. Risk perceptions of ocean acidification were influenced by factors other than knowledge about the risk such as affect, place attachment and environmental identity. A key finding of this thesis was that people were concerned about ocean acidification despite this being an unfamiliar risk issue, perceiving it as a highly negative risk. This exploratory thesis will help develop more effective risk communications around ocean acidification with these findings in mind. Future work should test ocean acidification frames; whether or not it should be framed as part of climate change. The mental models approach allowed initial understandings of this unfamiliar risk to be explored using mixed methods and helped examine how ocean acidification was conceptualised through social representations theory. Public response to ocean acidification may mean that there would be greater support for policies aimed at reducing carbon emissions.

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Williams, Maria C. "The pelagic record of ocean acidification." Thesis, University of Bristol, 2015. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.686814.

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Ocean acidification (OA) as a result of anthropogenic CO2 accumulation has major implications for the calcification of marine organisms. Assessing the calcification response of coccolithophores and planktic foraminifera to OA in particular is paramount as together they produce the majority of pelagic carbonate burial and thus impact biogeochemical cycling and oceanic CO2 uptake. In this thesis, two sediment cores from Eirik Drift and the Norwegian Sea are used to reconstruct the natural calcification response of marine plankton since the Last Glacial Maximum and compare these changes to recent anthropogenic influences over the last 200 years. Reconstructions of the bottom water dynamics and thus sedimentation at Eirik Drift infers the suitability of the core for palaeo-analysis of plankton calcification. The calcification response of three foraminiferal species and two morphotypes of the dominant polar species Neogloboquadrina pachyderma are significantly correlated throughout the Holocene suggesting similar calcification mechanisms between and within species. Although the drivers of calcification appear to vary temporally and geographically, down-core planktic foraminiferal Mg/Ca and faunal assemblage counts point towards the importance of sea surface temperature and optimal growth conditions on the calcification of N pachyderma. Unlike Globigerina bulloides, N pachyderma shows little sensitivity to CO2 changes across the last deglaciation Since the beginning of industrialisation, foraminiferal calcification fluctuates within the natural long-term trends observed over the last 22 kyrs inferring minimal anthropogenic impacts on foraminiferal calcification. Interspecies-specific responses are evident, as the test weight of G. bulloides increases since the early 1900s in response to a warming North Altantic Current, whilst Neogloboquadrina incompta shows little change over the last 200 years. Furthermore, an increase in the degree of calcification of the abundant coccolithophore Emiliania huxleyi occurs in response to accelerated 20th century climate change pointing towards increased carbonate burial in the sub-polar North Atlantic under future global change.

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Vance, Thomas. "The response of marine assemblages to ocean acidification." Thesis, University of Newcastle Upon Tyne, 2011. http://hdl.handle.net/10443/1451.

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Global industrialisation has led to the anthropogenic raising of global CO2 concentration from 280 pp to over 380 ppm in the last 200 years causing oceanic pH to drop by 0.1 unit as a result of a processes called ocean acidification. It is expected to further drop by between 0.3 and 0.4 units over the next 100 years. Quantifying the impact of such a pH shift has, to date, largely relied on laboratory studies of model organisms or simple assemblages in mesocosms. Conversely, this work undertook a series of field experiments to examine the effect of predicted pH environmental conditions on a robust marina fouling assemblage and microorganisms through the manipulation of local CO2 concentration. CO2 was delivered and controlled above replicated settlement panels that were freely accessible to normal propagule supply. Over 5 months, recruitment and development of macroorganisms and diversity of microorganisms in biofilms was shown to be largely unaffected by low pH. Results of this investigation were contrasted against microbial diversity in biofilms from a low pH volcanic vent site. Molecular analysis of biofilms failed to detect an influence of pH on diversity. The development of an alternative method of CO2 delivery using silicone membranes is described, which proved to have both antifouling and ocean acidification experimental applications. In conclusion, the marine organisms examined in this study showed little response to pH change of the order that is expected with the progression of ocean acidification. Significant methodological advances to in situ pH experimentation have been made, however, which should assist further investigations.

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Hopkins, Frances Elizabeth. "Ocean acidification and marine biogenic trace gas production." Thesis, University of East Anglia, 2010. https://ueaeprints.uea.ac.uk/10582/.

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The oceanic uptake of anthropogenic CO2 emissions is leading to an alteration of seawater carbonate chemistry, manifested as increasing [H+], falling [CO32-] and a drop in seawater pH. Over the coming centuries this process, termed “ocean acidification”, is expected to negatively impact marine biota, with implications for marine biological and biogeochemical processes. In this thesis, the impact that such changes may have on the net production of a range of climatically- and atmospherically-important marine biogenic trace gases, including halocarbons and dimethyl sulphide (DMS), is assessed through a mesocosm phytoplankton bloom CO2 perturbation experiment, two laboratory CO2 incubation experiments on natural seawater samples, and at a volcanically-acidified shallow marine fieldsite in Italy. Large and significant reductions in DMS and DMSP concentrations under future high CO2 conditions were observed during the mesocosm experiment (mean decreases of 57 percent and 24 percent, respectively), a finding in strong support of a previous study (Avgoustidi 2007). Furthermore, concentrations of iodocarbons showed large decreases, with mean decreases under high CO2 ranging from 59 to 93 percent. Results for the laboratory incubation experiments also showed a reduction in iodocarbon concentrations (when normalised to chlorophyll a) under high CO2. These changes may be the result of shifts in plankton community composition in response to the high CO2 conditions, and/or impacts on dissolved organic matter and the bacterial communities involved in the formation of these compounds. The response of bromocarbons was less clear cut during the experimental studies. Following investigations at a naturally-acidified fieldsite in Italy, it was concluded that this site was a poor natural analogue to the impact of future ocean acidification on marine trace gas production. Taking the results of the mesocosm and laboratory incubations into consideration, a combined decrease in both DMS and iodocarbons in response to ocean acidification may have considerable impacts on future atmospheric chemistry and global climate.

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Cripps, Gemma Louise. "Ocean acidification : impacts on copepod growth and reproduction." Thesis, Swansea University, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.678388.

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Williamson, Christopher James. "The impacts of ocean acidification on calcifying macroalgae." Thesis, Cardiff University, 2015. http://orca.cf.ac.uk/73409/.

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The ecophysiology of calcified macroalgal species of the genera Corallina (C. officinalis and C. caespitosa) and Ellisolandia (E. elongata) (Corallinales, Rhodophyta) was examined in intertidal rock pools of the NE Atlantic, to facilitate predictions of ocean-acidification and warming impacts on these ecosystem engineers. An initial phylogenetic study highlighted significant cryptic diversity within the genus Corallina, and demonstrated that C. officinalis is restricted predominantly to the North Atlantic, while the recently established C. caespitosa shows a cosmopolitan distribution. Three subsequent studies were performed across the NE Atlantic (Iceland to northern Spain) to examine (i) the production, respiration, calcification and growth of Corallina in relation to irradiance, water temperature, and carbonate chemistry; (ii) the photoacclimation and photoregulation strategies of Corallina and Ellisolandia; and (iii) the recent-past (1850 – 2010) and present-day skeletal mineralogy (Mg/Ca ratios) of Corallina and Ellisolandia and its relationship to sea surface temperature. Data demonstrated that species currently experience significant seasonal and tidal fluctuations in abiotic conditions that may be important when considering future responses to ocean-acidification and climate-change. Seasonality in production, calcification and growth were demonstrated, with decreasing growth observed with increasing latitude. Photoacclimation to allow maximal light utilisation during winter periods, and photoregulation via nonphotochemical quenching were highlighted as important in allowing Corallina and Ellisolandia to maintain maximal productivity while controlling for photo-stress. Seasonal cycles in skeletal Mg incorporation were demonstrated with strong relation to sea surface temperature, though no significant change in skeletal mineralogy was evident since pre-industrial times. Taken together, data indicated that Corallina and Ellisolandia have the potential to survive under future ocean-acidification and warming conditions, though loss of species at high latitudes and shifts in the relative abundances of species across the region is likely to be evident, with overall range contraction predicted for C. officinalis due to both warming and ocean-acidification impacts.

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Suckling, Coleen Claire. "Calcified marine invertebrates : the effects of ocean acidification." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.608228.

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Khanna, Nikki. "The biological response of foraminifera to ocean acidification." Thesis, University of St Andrews, 2014. http://hdl.handle.net/10023/8089.

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Elevated atmospheric concentrations of carbon dioxide (CO₂), partly driven by anthropogenic activity, are decreasing the pH of the oceans. This thesis aimed to assess the biological response of foraminifera to ocean acidification. Foraminifera are single-celled organisms that form the dominant component of many marine communities. A series of laboratory experiments were carried out on benthic intertidal foraminifera from the Eden and Ythan estuaries, NE Scotland, to assess the impacts of ocean acidification. The responses of two dominant intertidal species of foraminifera (Haynesina germanica and Elphidium williamsoni) to ocean acidification were initially investigated in a short-term (6 week) experiment. Multiple species and multiple stressors (seasonal temperature regime and elevated CO₂) were then incorporated in a long-term (18 month) mesocosm study to investigate the physiological consequences (e.g. survival, growth) of ocean acidification. Survival of both Haynesina germanica and Elphidium williamsoni was significantly reduced under low pH conditions. Live specimens of both these calcareous species were however recorded at low pH, in reduced numbers. Following long-term exposure to ocean acidification, foraminiferal populations were still dominated by calcareous forms. Agglutinated foraminifera were recorded throughout the long-term incubations but their numbers were not high enough in the initial sediment collections to allow them to contribute significantly to the populations. Overall, survival of all foraminifera was greatly reduced in elevated CO₂ treatments. Temperature effects were observed on foraminiferal survival and diversity with the largest CO₂ effects recorded under the seasonally varying temperature regime. Foraminiferal test damage for all live species was also highest under elevated CO₂ conditions. Test dissolution was particularly evident in Haynesina germanica with important morphological features, such as functional ornamentation, becoming reduced or completely absent under elevated CO₂ conditions. A reduction in functionally important ornamentation could lead to a reduction in feeding efficiency with consequent impacts on this organism's survival and fitness. In addition, changes in the relative abundance and activities of these important species could affect biological interactions (e.g. food web function) and habitat quality.

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Ingrosso, Gianmarco. "Ocean acidification processes in coastal and offshore ecosystems." Doctoral thesis, Università degli studi di Trieste, 2015. http://hdl.handle.net/10077/10916.

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2013/2014
Since the beginning of Industrial Revolution a massive amount of atmospheric carbon dioxide, produced by human activity, has been absorbed by the World’s Oceans. This process has led to an acidification of marine waters on a global scale and is one of the most serious threats facing marine ecosystems in this century. The negative impacts of ocean acidification could be much more relevant in coastal ecosystems, where marine life is concentrated and biogeochemical processes are more active. However, future projections of pH reduction in these areas are difficult to estimate because result from multiple physical and biological drivers, including watershed weathering, river-born nutrient inputs, and changes in ecosystem structure and metabolism. In order to assess the sensibility of the Gulf of Trieste to the ocean acidification, high quality determination of the marine carbonate system (pHT, total alkalinity, dissolved inorganic carbon-DIC, buffer capacity) and other related biogeochemical parameters were carried out along a transect from the Isonzo River mouth to the centre of the gulf and at the coastal Long Term Ecological Research station C1. At the same time the biological influence of organic matter production and decomposition on the marine CO2 system was estimated using 14C primary production and heterotrophic prokaryote production (by 3H-leucine incorporation). The two years long measurements revealed a complex dynamic of the marine carbonate system, due to the combined effects of local freshwater inputs, biological processes, and air-sea CO2 exchange. However, it was possible to estimate the influence of the different drivers on a seasonal time scale. In winter the very low seawater temperature (minima = 2.88 °C) and strong Bora events determined a marked dissolution of atmospheric CO2 and elevated DIC concentration. During warm seasons the DIC concentration gradually decreased in the surface layer, due to biological drawdown (primary production) and thermodynamic equilibria (CO2 degassing), whereas under the pycnocline the respiration and remineralisation of organic matter prevailed, causing a temporary acidification of bottom waters. The winter seawater invasion of atmospheric CO2 was balanced by high riverine AT input (maxima ∼ 2933 µmol kg-1), derived mainly from chemical weathering of carbonate rocks of the surrounding karstic area, which increased the buffer capacity of this system and probably could mitigate the effect of ocean acidification. The marine carbonate system was also analysed in the Middle and Southern Adriatic Sea, in order to estimate the concentration of anthropogenic carbon dioxide currently present in this area. The results suggested that the entire water column was contaminated by a large amount of anthropogenic CO2 and very high concentration was detected near the bottom, in correspondence of the North Adriatic Dense Waters. This finding supported the hypothesis that during dense water formation events the very low seawater temperature can favour the physical dissolution of atmospheric carbon dioxide, and also revealed the active role of the North Adriatic Sea in sequestering and storing anthropogenic CO2 into the deep layers of Mediterranean Sea.
Dall’inizio della Rivoluzione Industriale ad oggi, una grande quantità di anidride carbonica antropogenica presente in atmosfera è stata assorbita dagli Oceani di tutto il mondo. Questo processo ha portato all’acidificazione del mare su scala globale e rappresenta una delle più gravi minacce per gli ecosistemi marini in questo secolo. L’impatto negativo di tale fenomeno, noto come ocean acidification, potrebbe essere maggiore soprattutto negli ecosistemi costieri, poiché è qui che si concentrano gli organismi marini ed è qui che i cicli biogeochimici risultano più attivi. Tuttavia è difficile stimare il futuro abbassamento del pH in queste aree a causa della loro complessità e della moltitudine dei processi fisici, chimici e biologici coinvolti (cambiamenti dello stato trofico e del metabolismo dell’ecosistema, input fluviale di nutrienti, materia organica e prodotti di dissoluzione delle rocce, ecc.). Allo scopo di valutare la vulnerabilità del Golfo di Trieste rispetto al processo di ocean acidification, per due anni sono state eseguite misure di elevata precisione del sistema carbonatico marino (pHT, alcalinità totale, carbonio inorganico disciolto-DIC, capacità tamponante) e di altri parametri biogeochimici correlati lungo un transetto che congiunge la foce del fiume Isonzo al centro del Golfo e nella stazione C1 sito LTER (Long Time Ecological Research C1). Inoltre, per valutare in maniera più approfondita l’influenza dei processi biologici sulla variabilità del sistema carbonatico, è stata stimata la produzione primaria, attraverso il metodo dell’incorporazione di 14C, e la produzione procariotica eterotrofa, attraverso l’incorporazione di 3H-leucina. I risultati hanno evidenziato una complessa dinamica del sistema carbonatico dovuta all’effetto e all’interazione degli apporti fluviali, dei processi biologici e dello scambio di CO2 tra atmosfera e mare. Su scala stagionale, tuttavia, è stata stimata l’influenza e il contributo dei diversi processi. In inverno, la bassa temperatura dell’acqua, che in un caso estremo ha raggiunto i 2.88 °C, e i forti venti di Bora hanno favorito la dissoluzione della CO2 atmosferica, determinando un incremento della concentrazione di DIC. Durante la primavera e l’estate i livelli di DIC sono diminuiti gradualmente negli strati superficiali, grazie all’effetto combinato della produzione primaria e alla perdita di CO2 verso l’atmosfera per degassamento. Nel periodo tardo estivo-autunnale, invece, al di sotto del picnoclino i processi di respirazione e remineralizzazione della materia organica sono risultati predominanti determinando, a causa dell’elevata concentrazione di CO2 prodotta, una temporanea acidificazione delle acque di fondo. Il forte assorbimento di CO2 atmosferica stimato durante l’inverno era, però, controbilanciato dall’apporto fluviale di alcalinità totale, derivante dal processo di dissoluzione delle rocce calcaree presenti nell’area carsica. Tale fenomeno ha determinato un aumento della capacità tamponante del sistema, mitigando probabilmente il processo di ocean acidification in quest’area. Parallelamente alle analisi nel Golfo di Trieste, il sistema carbonatico marino è stato analizzato anche nel Medio e Sud Adriatico, con lo scopo di stimare la concentrazione di anidride carbonica antropogenica attualmente presente in questi sottobacini. I risultati hanno dimostrato come tutta la colonna d’acqua avesse assorbito una grande quantità di CO2 antropica. In particolare elevate concentrazioni sono state individuate sul fondo, in corrispondenza delle acque dense di origine nord adriatica. Tali risultati hanno confermato l’ipotesi secondo la quale in inverno, durante il processo di formazione di acque dense nel Nord Adriatico, le basse temperature raggiunte dalle acque possono favorire la dissoluzione fisica della CO2 atmosferica. Hanno dimostrato, inoltre, l’importante ruolo svolto da tutto il bacino nord adriatico nel sequestrare e trasportare la CO2 antropica nelle profondità del mare, estendendo il processo di ocean acidification anche ad aree meno contaminate.
XXVII Ciclo
1982

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Books on the topic "Ocean acidification"

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Ocean acidification. Oxford: Oxford University Press, 2011.

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Carballo, José Luis, and James J. Bell, eds. Climate Change, Ocean Acidification and Sponges. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-59008-0.

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Feely, Richard A., Rik Wanninkhof, John E. Stein, Michael Frederick Sigler, Elizabeth Bromley Jewett, Luis Felipe Arzayus, Dwight Kuehl Gledhill, and Adrienne J. Sutton. NOAA ocean and Great Lakes acidification research plan. [Silver Spring, Md.]: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, 2010.

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Secretariat of the Convention on Biological Diversity. Scientific synthesis of the impacts of ocean acidification on marine biodiversity. Montreal, Quebec, Canada: Secretariat of the Convention on Biological Diversity, 2009.

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Ocean acidification: A national strategy to meet the challenges of a changing ocean. Washington, D.C: National Academies Press, 2010.

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Oceanic acidification: A comprehensive overview. Boca Raton, FL: CRC Press, 2012.

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1948-, Mason Geoffrey, ed. Poisoning and acidification of the Earth's oceans. Hauppauge, N.Y: Nova Science Publishers, 2009.

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Bausch, Alexandra Renee. Interactive effects of ocean acidification with other environmental drivers on marine plankton. [New York, N.Y.?]: [publisher not identified], 2018.

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The environmental and economic impacts of ocean acidification: Hearing before the Subcommittee on Oceans, Atmosphere, Fisheries, and Coast Guard of the Committee on Commerce, Science, and Transportation, United States Senate, One Hundred Eleventh Congress, second session, April 22, 2010. Washington: U.S. G.P.O., 2011.

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Latif, Mojib. Das Ende der Ozeane: Warum wir ohne die Meere nicht überleben werden. Freiburg im Breisgau: Herder, 2014.

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Book chapters on the topic "Ocean acidification"

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Iglesias-Rodriguez, Maria Debora. "Ocean ocean/oceanic Acidification ocean/oceanic acidification." In Encyclopedia of Sustainability Science and Technology, 7229–42. New York, NY: Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4419-0851-3_494.

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Iglesias-Rodriguez, Maria Debora. "Ocean Acidification." In Earth System Monitoring, 269–89. New York, NY: Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4614-5684-1_12.

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Mukherjee, Swapna, Kaushik Kiran Ghosh, and Abhra Chanda. "Ocean Acidification." In Environmental Oceanography and Coastal Dynamics, 205–12. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-34422-0_12.

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Thor, Peter, and Sam Dupont. "Ocean Acidification." In Handbook on Marine Environment Protection, 375–94. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-60156-4_19.

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Spellman, Frank R. "Ocean Acidification." In The Science of Ocean Pollution, 187–92. Boca Raton: CRC Press, 2023. http://dx.doi.org/10.1201/9781003407638-16.

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Faria, Ana M. "CO2-Induced Ocean Acidification." In Encyclopedia of the UN Sustainable Development Goals, 1–10. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-319-71064-8_44-1.

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Faria, Ana M. "CO2-Induced Ocean Acidification." In Encyclopedia of the UN Sustainable Development Goals, 121–29. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-319-98536-7_44.

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Galdies, Charles, Rachel Tiller, and Beatriz Martinez Romera. "Global Ocean Governance and Ocean Acidification." In Encyclopedia of the UN Sustainable Development Goals, 421–33. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-319-98536-7_109.

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Galdies, Charles, Rachel Tiller, and Beatriz Martinez Romera. "Global Ocean Governance and Ocean Acidification." In Encyclopedia of the UN Sustainable Development Goals, 1–12. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-319-71064-8_109-1.

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Roleda, Michael Y., and Catriona L. Hurd. "Seaweed Responses to Ocean Acidification." In Ecological Studies, 407–31. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-28451-9_19.

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Conference papers on the topic "Ocean acidification"

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Potty, Gopu R. "Ocean acidification: Implications to underwater acoustics." In 2009 International Symposium on Ocean Electronics (SYMPOL 2009). IEEE, 2009. http://dx.doi.org/10.1109/sympol.2009.5664163.

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Barry, J. P., C. Lovera, C. Okuda, E. Nelson, and E. Pane. "A Gas-Controlled Aquarium System for Ocean Acidification Studies." In OCEANS 2008 - MTS/IEEE Kobe Techno-Ocean. IEEE, 2008. http://dx.doi.org/10.1109/oceanskobe.2008.4531029.

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Kirkwood, W., E. Peltzer, P. Walz, and P. Brewer. "Cabled observatory technology for ocean acidification research." In OCEANS 2009-EUROPE (OCEANS). IEEE, 2009. http://dx.doi.org/10.1109/oceanse.2009.5278337.

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Thompson, Cara K., Astrid Schnetzer, and Michelle Kinzel. "STUDENT-CENTERED TEACHING DEMONSTRATION FOR OCEAN ACIDIFICATION." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-324085.

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Feely, R. A., R. A. Feely, R. A. Feely, R. A. Feely, R. A. Feely, R. A. Feely, R. A. Feely, et al. "An International Observational Network for Ocean Acidification." In OceanObs'09: Sustained Ocean Observations and Information for Society. European Space Agency, 2010. http://dx.doi.org/10.5270/oceanobs09.cwp.29.

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Iglesias-Rodriguez, M. Debora, Kenneth R. N. Anthony, Jella Bijma, Andrew G. Dickson, Scott C. Doney, Victoria J. Fabry, Richard A. Feely, et al. "Developing a Global Ocean Acidification Observation Network." In OceanObs'09: Sustained Ocean Observations and Information for Society. European Space Agency, 2010. http://dx.doi.org/10.5270/oceanobs09.pp.24.

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Reggiani, Emanuele R., Richard G. J. Bellerby, and Kai Sorensen. "Underwater spectrophotometric detection: Scaling down ocean acidification monitoring." In 2014 IEEE Sensor Systems for a Changing Ocean (SSCO). IEEE, 2014. http://dx.doi.org/10.1109/ssco.2014.7000376.

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Wang, Jiuyuan, Gabriella Kitch, Benjamin J. Linzmeier, Andrew D. Jacobson, Bradley B. Sageman, and Matthew T. Hurtgen. "CALCIUM ISOTOPE VARIABILITY ACROSS ANCIENT CANDIDATE OCEAN ACIDIFICATION EVENTS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355894.

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Ramdas, Rithvik, Balivada Srinivas Patnaik, Ansh Parmar, Satya Kiranmai Tadepalli, and K. Vasanth. "Beyond pH Levels: A Comprehensive Survey on Ocean Acidification." In 2024 Second International Conference on Emerging Trends in Information Technology and Engineering (ICETITE). IEEE, 2024. http://dx.doi.org/10.1109/ic-etite58242.2024.10493656.

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Kirkwood, W. J., E. T. Peltzer, P. Walz, K. Headley, B. Herlien, C. Kecy, T. Maughan, et al. "Cabled instrument technologies for ocean acidification research — FOCE (free ocean CO2 enrichment)." In 2011 IEEE Symposium on Underwater Technology (UT) and Workshop on Scientific Use of Submarine Cables and Related Technologies (SSC). IEEE, 2011. http://dx.doi.org/10.1109/ut.2011.5774089.

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Reports on the topic "Ocean acidification"

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Baird, Kaitlin, Anne Cohen, and Samantha de Putron. Ocean Acidification: Building a Skeleton in a Changing Ocean. American Museum of Natural History, 2015. http://dx.doi.org/10.5531/cbc.ncep.0168.

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Coral reefs are particularly vulnerable to ocean acidification due to their calcium carbonate “skeletons,” yet little is known about how ocean acidification will affect coral recruitment. In this exercise, students will examine a species of stony or hard coral belonging to the Order Scleractinia, Favia fragum, and examine how ocean acidification and changes in seawater saturation state (carbonate ion concentration) can affect the calcification process of new recruits of this coral species in Bermuda. After a brief introduction to coral reproduction and recruitment, as well as the chemistry behind calcification and acidification, students will go on to understand the experimental design, obtain and manipulate real data, and analyze the dataset.

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Baker, T. Ocean Acidification and Fisheries: Alaska's Challenge and Response. Alaska Sea Grant, University of Alaska Fairbanks, 2012. http://dx.doi.org/10.4027/oafacr.2012.

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Peter Girguis, Peter Girguis. Do seawater microbes help oysters cope with ocean acidification? Experiment, April 2023. http://dx.doi.org/10.18258/50593.

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Ward, Nicholas. Electrochemical Acid Sequestration to Ease Ocean Acidification (EASE-OA) - CRADA 600 (Abstract). Office of Scientific and Technical Information (OSTI), June 2023. http://dx.doi.org/10.2172/1995374.

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Jewett, L., and A. Romanou. Ch. 13: Ocean Acidification and Other Ocean Changes. Climate Science Special Report: Fourth National Climate Assessment, Volume I. Edited by D. J. Wuebbles, D. W. Fahey, K. A. Hibbard, D. J. Dokken, B. C. Stewart, and T. K. Maycock. U.S. Global Change Research Program, 2017. http://dx.doi.org/10.7930/j0qv3jqb.

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Keller, David P. Quantification of “constrained” potential of ocean NETs. OceanNets, 2022. http://dx.doi.org/10.3289/oceannets_d4.1.

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This study uses an existing perturbed parameter ensemble (PPE) of simulated ocean CO2 removal (CDR) to better determine sustainable pathways of ocean-based NET deployment and to provide information to constrain the design of subsequent modelling experiments. The results show that ocean alkalinity enhancement (OAE) can only help meet SDG13 (Climate Action) when other ambitious mitigation efforts are taken. This reinforces that OAE is not a substitute for emissions reduction, but could contribute to meeting our climate goals (if other factors suggest OAE is worth doing). For SDG14 (Life Below Water), the results suggest OEA can contribute to limiting or even reversing ocean acidification. Meeting many other SDG14 objectives is closely linked to also meeting SDG13. A key recommendation is therefore, that subsequent simulations in OceanNETs should only use SDG13 compatible baseline scenarios, unless there is some specific need for process understanding at higher levels of climate change. The analysis has also determined that the idealized CDR in the PPE is not suitable for determining many socio-economic constraints and the implications that these have for meeting the SDGs. Another key recommendation is therefore, that subsequent simulations within OceanNETs should use more realistic scenarios of CDR deployment.

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Kessler, John, and Carolyn Ruppel. Final Scientific/Technical Report: Characterizing Ocean Acidification and Atmospheric Emission caused by Methane Released from Gas Hydrate Systems along the US Atlantic Margin. Office of Scientific and Technical Information (OSTI), June 2020. http://dx.doi.org/10.2172/1634089.

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King, E. L., A. Normandeau, T. Carson, P. Fraser, C. Staniforth, A. Limoges, B. MacDonald, F. J. Murrillo-Perez, and N. Van Nieuwenhove. Pockmarks, a paleo fluid efflux event, glacial meltwater channels, sponge colonies, and trawling impacts in Emerald Basin, Scotian Shelf: autonomous underwater vehicle surveys, William Kennedy 2022011 cruise report. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/331174.

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A short but productive cruise aboard RV William Kennedy tested various new field equipment near Halifax (port of departure and return) but also in areas that could also benefit science understanding. The GSC-A Gavia Autonomous Underwater Vehicle equipped with bathymetric, sidescan and sub-bottom profiler was successfully deployed for the first time on Scotian Shelf science targets. It surveyed three small areas: two across known benthic sponge, Vazella (Russian Hat) within a DFO-directed trawling closure area on the SE flank of Sambro Bank, bordering Emerald Basin, and one across known pockmarks, eroded cone-shaped depression in soft mud due to fluid efflux. The sponge study sites (~ 150 170 m water depth) were known to lie in an area of till (subglacial diamict) exposure at the seabed. The AUV data identified gravel and cobble-rich seabed, registering individual clasts at 35 cm gridded resolution. A subtle variation in seabed texture is recognized in sidescan images, from cobble-rich on ridge crests and flanks, to limited mud-rich sediment in intervening troughs. Correlation between seabed topography and texture with the (previously collected) Vazella distribution along two transects is not straightforward. However there may be a preference for the sponge in the depressions, some of which have a thin but possibly ephemeral sediment cover. Both sponge study sites depict a hereto unknown morphology, carved in glacial deposits, consisting of a series of discontinuous ridges interpreted to be generated by erosion in multiple, continuous, meandering and cross-cutting channels. The morphology is identical to glacial Nye, or mp;lt;"N-mp;lt;"channels, cut by sub-glacial meltwater. However their scale (10 to 100 times mp;lt;"typicalmp;gt;" N-channels) and the unique eroded medium, (till rather than bedrock), presents a rare or unknown size and medium and suggests a continuum in sub-glacial meltwater channels between much larger tunnel valleys, common to the eastward, and the bedrock forms. A comparison is made with coastal Nova Scotia forms in bedrock. The Emerald Basin AUV site, targeting pockmarks was in ~260 to 270 m water depth and imaged eight large and one small pockmark. The main aim was to investigate possible recent or continuous fluid flux activity in light of ocean acidification or greenhouse gas contribution; most accounts to date suggested inactivity. While a lack of common attributes marking activity is confirmed, creep or rotational flank failure is recognized, as is a depletion of buried diffuse methane immediately below the seabed features. Discovery of a second, buried, pockmark horizon, with smaller but more numerous erosive cones and no spatial correlation to the buried diffuse gas or the seabed pockmarks, indicates a paleo-event of fluid or gas efflux; general timing and possible mechanisms are suggested. The basinal survey also registered numerous otter board trawl marks cutting the surficial mud from past fishing activity. The AUV data present a unique dataset for follow-up quantification of the disturbance. Recent realization that this may play a significant role in ocean acidification on a global scale can benefit from such disturbance quantification. The new pole-mounted sub-bottom profiler collected high quality data, enabling correlation of recently recognized till ridges exposed at the seabed as they become buried across the flank and base of the basin. These, along with the Nye channels, will help reconstruct glacial behavior and flow patterns which to date are only vaguely documented. Several cores provide the potential for stratigraphic dating of key horizons and will augment Holocene environmental history investigations by a Dalhousie University student. In summary, several unique features have been identified, providing sufficient field data for further compilation, analysis and follow-up publications.

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Ocean Acidification: What It Means to Alaskans and How We Can Adapt. Alaska Sea Grant, University of Alaska Fairbanks, July 2011. http://dx.doi.org/10.4027/oawimahwca.2011.

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