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  • 1
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (111 Seiten = 4 MB) , Illustrationen, Graphen, Karten
    Edition: 2021
    Language: English
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  • 2
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    PANGAEA
    In:  Supplement to: McCulloch, Malcolm T; Trotter, Julie; Montagna, Paolo; Falter, James L; Dunbar, Robert G; Freiwald, André; Försterra, Günter; López Correa, Matthias; Maier, Cornelia; Rüggeberg, Andres; Taviani, Marco (2012): Resilience of cold-water scleractinian corals to ocean acidification: Boron isotopic systematics of pH and saturation state up-regulation. Geochimica et Cosmochimica Acta, 87, 21-34, https://doi.org/10.1016/j.gca.2012.03.027
    Publication Date: 2023-12-13
    Description: The boron isotope systematics has been determined for azooxanthellate scleractinian corals from a wide range of both deep-sea and shallow-water environments. The aragonitic coral species, Caryophyllia smithii, Desmophyllum dianthus, Enallopsammia rostrata, Lophelia pertusa, and Madrepora oculata, are all found to have relatively high d11B compositions ranging from 23.2 per mil to 28.7 per mil. These values lie substantially above the pH-dependent inorganic seawater borate equilibrium curve, indicative of strong up-regulation of pH of the internal calcifying fluid (pH(cf)), being elevated by ~0.6-0.8 units (Delta pH) relative to ambient seawater. In contrast, the deep-sea calcitic coral Corallium sp. has a significantly lower d11B composition of 15.5 per mil, with a corresponding lower Delta pH value of ~0.3 units, reflecting the importance of mineralogical control on biological pH up-regulation. The solitary coral D. dianthus was sampled over a wide range of seawater pH(T) and shows an approximate linear correlation with Delta pH(Desmo) = 6.43 - 0.71 pH(T) (r**2 = 0.79). An improved correlation is however found with the closely related parameter of seawater aragonite saturation state, where Delta pH(Desmo) = 1.09 - 0.14 Omega(arag) (r**2 = 0.95), indicating the important control that carbonate saturation state has on calcification. The ability to up-regulate internal pH(cf), and consequently Omega(cf), of the calcifying fluid is therefore a process present in both azooxanthellate and zooxanthellate aragonitic corals, and is attributed to the action of Ca2+ -ATPase in modulating the proton gradient between seawater and the site of calcification. These findings also show that the boron isotopic compositions (d11Bcarb) of aragonitic corals are highly systematic and consistent with direct uptake of the borate species within the biologically controlled extracellular calcifying medium.
    Keywords: HERMIONE; Hotspot Ecosystem Research and Mans Impact On European Seas; International Polar Year (2007-2008); IPY
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 3
    Publication Date: 2024-02-02
    Keywords: Area/locality; Caryophyllia smithii, δ11B; Comau Fjord, Patagonia, Chile; Corallium sp., δ11B; D248; D248_13831#1; Darwin Mounds; DD_MS; Desmophyllum dianthus, δ11B; Discovery (1962); Dredge; DRG; Elevation of event; Elevation of event 2; Enallopsammia rostrata, δ11B; Event label; GeoB6739-1; GeoB8021-1; GS: M70/1-752 (D 111); Hawaiian Islands, North Central Pacific; Hill_B1; Latitude of event; Longitude of event; Lophelia pertusa, δ11B; M70/1; M70/1_752; Madrepora oculata, δ11B; MAL; Marmara Sea; MedCor_MAL; MedCor-25-D; MedCor-25-L; MedCor-41-CA; MedCor-57-CA; MedCor-59-CA; MedCor-74-D; MedCor-74-L; Mediterranean Sea; Meteor (1986); Monitoring station; MONS; Northeast Atlantic; Parameter; pH; pH change; PO228-216; Porcupine Seabight; POS265; POS292; POS499-1; POS544-1; Poseidon; Punto_Llonco; PV703_Cor_5; PV703_Enal_2; PV703_Enal_7; Remote operated vehicle; ROV; Sample ID; Species; SR: POS-228-216; Tasman Sea; TRAWL; Trawl net; VH97-351
    Type: Dataset
    Format: text/tab-separated-values, 168 data points
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  • 4
    Publication Date: 2024-02-02
    Keywords: Alkalinity, total; Aragonite saturation state; Aragonite saturation state, standard deviation; Area/locality; Calcite saturation state; Calcite saturation state, standard deviation; Comau Fjord, Patagonia, Chile; D248; D248_13831#1; Darwin Mounds; Date/Time of event; DD_MS; Discovery (1962); Dredge; DRG; ELEVATION; Elevation, maximum; Elevation, minimum; Event label; GeoB6739-1; GeoB8021-1; GS: M70/1-752 (D 111); Hawaiian Islands, North Central Pacific; Hill_B1; Latitude of event; Longitude of event; M70/1; M70/1_752; MAL; Marmara Sea; MedCor_MAL; MedCor-25-D; MedCor-25-L; MedCor-41-CA; MedCor-57-CA; MedCor-59-CA; MedCor-74-D; MedCor-74-L; Mediterranean Sea; Meteor (1986); Monitoring station; MONS; Northeast Atlantic; pH; PO228-216; Porcupine Seabight; POS265; POS292; POS499-1; POS544-1; Poseidon; Punto_Llonco; PV703_Cor_5; PV703_Enal_2; PV703_Enal_7; Reference/source; Remote operated vehicle; ROV; Salinity; Sample ID; Species; SR: POS-228-216; Tasman Sea; Temperature, water; TRAWL; Trawl net; VH97-351
    Type: Dataset
    Format: text/tab-separated-values, 220 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Maier, Cornelia; Hegeman, Jan; Weinbauer, Markus G; Gattuso, Jean-Pierre (2009): Calcification of the cold-water coral Lophelia pertusa under ambient and reduced pH. Biogeosciences, 6(8), 1671-1680, https://doi.org/10.5194/bg-6-1671-2009
    Publication Date: 2024-03-15
    Description: The cold-water coral Lophelia pertusa is one of the few species able to build reef-like structures and a 3-dimensional coral framework in the deep oceans. Furthermore, deep cold-water coral bioherms may be among the first marine ecosystems to be affected by ocean acidification. Colonies of L. pertusa were collected during a cruise in 2006 to cold-water coral bioherms of the Mingulay reef complex (Hebrides, North Atlantic). Shortly after sample collection onboard these corals were labelled with calcium-45. The same experimental approach was used to assess calcification rates and how those changed due to reduced pH during a cruise to the Skagerrak (North Sea) in 2007. The highest calcification rates were found in youngest polyps with up to 1% d-1 new skeletal growth and average rates of 0.11±0.02% d-1±S.E.). Lowering pH by 0.15 and 0.3 units relative to the ambient level resulted in calcification being reduced by 30 and 56%. Lower pH reduced calcification more in fast growing, young polyps (59% reduction) than in older polyps (40% reduction). Thus skeletal growth of young and fast calcifying corallites suffered more from ocean acidification. Nevertheless, L. pertusa exhibited positive net calcification (as measured by 45Ca incorporation) even at an aragonite saturation state below 1.
    Keywords: Alkalinity, total; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcification rate; Calcite saturation state; Calcium; Calculated using seacarb; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Coast and continental shelf; Date; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laboratory experiment; Lophelia pertusa; Lophelia pertusa, skeleton, dry weight; Lophelia pertusa, tissue, dry weight; Measured; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Salinity; Sample ID; see reference(s); Single species; Species; Temperate; Temperature, water; Time in days
    Type: Dataset
    Format: text/tab-separated-values, 7748 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Maier, Cornelia; Popp, Pauline; Sollfrank, Nicole; Weinbauer, Markus G; Wild, Christian; Gattuso, Jean-Pierre (2016): Effects of elevated pCO2 and feeding on net calcification and energy budget of the Mediterranean cold-water coral Madrepora oculata. Journal of Experimental Biology, 219(20), 3208-3217, https://doi.org/10.1242/jeb.127159
    Publication Date: 2024-03-15
    Description: Ocean acidification is a major threat to calcifying marine organisms such as deep-sea cold-water corals (CWC), but related knowledge is scarce. The aragonite saturation threshold (Omega a) for calcification, respiration, and organic matter fluxes was investigated experimentally in the Mediterranean Madrepora oculata (Linnaeus 1758). Over 10 weeks, colonies were maintained under two feeding regimes (uptake of 36.75 and 7.46 µmol C/polyp/week) and exposed in 2 week intervals to a consecutively changing air-CO2 mix (pCO2) of 400, 1600, 800, 2000 and 400 ppm. There was a significant effect of feeding on calcification at initial ambient pCO2, while at consecutive pCO2 treatments feeding had no effect on calcification. Respiration was not significantly affected by feeding or pCO2 levels. Coral skeletons started to dissolve at an average Omega a threshold of 0.92, but recovered and started to calcify again at Omega a〉 or =1. The surplus energy required to counteract dissolution at elevated pCO2 (〉 or =1600µatm) was twice that at ambient pCO2. Yet, feeding had no mitigating effect at increasing pCO2 levels. This could be due to the fact that the energy required for calcification is a small fraction (1 to 3%) of the total metabolic energy demand and corals even under low food conditions might therefore still be able to allocate this small portion of energy to calcification. The response and resistance to ocean acidification is consequently not controlled by feeding in this species, but more likely by chemical reaction at the site of calcification and exchange processes between the calicoblastic layer and ambient seawater.
    Keywords: Alkalinity, total; Animalia; Aragonite saturation state; Area; Bari_Canyon_OA; Benthic animals; Benthos; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcification rate; Calcification rate of calcium carbonate; Calcite saturation state; Calculated using seacarb; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, organic, total, change rate; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Coral; Deep-sea; Dry mass; EXP; Experiment; Feeding mode; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gas, flux; Growth/Morphology; Incubation duration; Laboratory experiment; Madrepora oculata; Mediterranean Sea; OA-ICC; Ocean Acidification International Coordination Centre; Other; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate organic carbon uptake rate; Percentage; pH; Polyp number; Pressure; Registration number of species; Respiration; Respiration rate, oxygen; Respiratory quotient; Salinity; Sample code/label; Sample type; Sampling date; Single species; Species; Temperate; Temperature, water; Treatment; Type; Uniform resource locator/link to reference; Volume
    Type: Dataset
    Format: text/tab-separated-values, 11229 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Maier, Cornelia; Watremez, P; Taviani, Marco; Weinbauer, Markus G; Gattuso, Jean-Pierre (2012): Calcification rates and the effect of ocean acidification on Mediterranean cold-water corals. Proceedings of the Royal Society B-Biological Sciences, 279(1734), 1716-1723, https://doi.org/10.1098/rspb.2011.1763
    Publication Date: 2024-05-22
    Description: 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 CaCO3 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 CO2. At ambient conditions, calcification rates ranged between -0.01 and 0.23% d-1. Calcification rates of M. oculata under variable partial pressure of CO2 (pCO2) were the same for ambient and elevated pCO2 (404 and 867 µatm) with 0.06 ± 0.06% d-1, while calcification was 0.12 ± 0.06% d-1 when pCO2 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.
    Keywords: AIRICA analyzer (Miranda); Alkalinity, total; Alkalinity, total, standard deviation; Alkalinity anomaly technique (Smith and Key, 1975); Ammonium; Ammonium, standard deviation; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcification rate; Calcification rate, standard deviation; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Coral polyp; Coral polyp, standard deviation; Deep-sea; Desmophyllum sp.; Desmophyllum sp., dry weight; Desmophyllum sp., dry weight, standard deviation; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experiment day; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Identification; Laboratory experiment; Lophelia pertusa; Lophelia pertusa, tissue, dry weight; Lophelia pertusa, tissue, dry weight, standard error; Madrepora oculata; Madrepora oculata, dry weight; Madrepora oculata, dry weight, standard deviation; Measured; Mediterranean Sea; Metrohm Titrando titrator; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Phosphate; Phosphate, standard deviation; Replicates; Salinity; Single species; Site; Species; Temperate; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 608 data points
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  • 8
    Publication Date: 2024-05-22
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Ammonium; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Buoyant mass; Calcification/Dissolution; Calcification rate; Calcification rate of calcium carbonate; Calcification rate of calcium carbonate per polyp; Calcite saturation state; Calculated using seacarb; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Deep-sea; Desmophyllum sp.; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Identification; Incubation duration; Laboratory experiment; Lacaze_Duthiers; Lophelia pertusa; Madrepora oculata; Mass; Mediterranean Sea; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Phosphate; Polyp number; Respiration; Respiration rate, oxygen; Salinity; Single species; Species; Temperate; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 14120 data points
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  • 9
    Publication Date: 2017-06-29
    Description: The boron isotope systematics has been determined for azooxanthellate scleractinian corals from a wide range of both deep-sea and shallow-water environments. The aragonitic coral species, Caryophyllia smithii, Desmophyllum dianthus, Enallopsammia rostrata, Lophelia pertusa, and Madrepora oculata, are all found to have relatively high δ11B compositions ranging from 23.2‰ to 28.7‰. These values lie substantially above the pH-dependent inorganic seawater borate equilibrium curve, indicative of strong up-regulation of pH of the internal calcifying fluid (pHcf), being elevated by ∼0.6–0.8 units (ΔpH) relative to ambient seawater. In contrast, the deep-sea calcitic coral Corallium sp. has a significantly lower δ11B composition of 15.5‰, with a corresponding lower ΔpH value of ∼0.3 units, reflecting the importance of mineralogical control on biological pH up-regulation. The solitary coral D. dianthus was sampled over a wide range of seawater pHT and shows an approximate linear correlation with ΔpHDesmo = 6.43 − 0.71pHT (r2 = 0.79). An improved correlation is however found with the closely related parameter of seawater aragonite saturation state, where ΔpHDesmo = 1.09 − 0.14Ωarag (r2 = 0.95), indicating the important control that carbonate saturation state has on calcification. The ability to up-regulate internal pHcf, and consequently Ωcf, of the calcifying fluid is therefore a process present in both azooxanthellate and zooxanthellate aragonitic corals, and is attributed to the action of Ca2+-ATPase in modulating the proton gradient between seawater and the site of calcification. These findings also show that the boron isotopic compositions (δ11Bcarb) of aragonitic corals are highly systematic and consistent with direct uptake of the borate species within the biologically controlled extracellular calcifying medium. We also show that the relatively strong up-regulation of pH and consequent elevation of the internal carbonate saturation state (Ωcf ∼8.5 to ∼13) at the site of calcification by cold-water corals, facilitates calcification at or in some cases below the aragonite saturation horizon, providing a greater ability to adapt to the already low and now decreasing carbonate ion concentrations. Although providing greater resilience to the effects of ocean acidification and enhancing rates of calcification with increasing temperature, the process of internal pHcf up-regulation has an associated energetic cost, and therefore growth-rate cost, of ∼10% per 0.1 pH unit decrease in seawater pHT. Furthermore, as the aragonite saturation horizon shoals with rapidly increasing pCO2 and Ωarag 〈 1, increased dissolution of the exposed skeleton will ultimately limit their survival in the deep oceans.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 10
    Publication Date: 2019-10-23
    Description: Knowledge on basic biological functions of organisms is essential to understand not only the role they play in the ecosystems but also to manage and protect their populations. The study of biological processes, such as growth, reproduction and physiology, which can be approached in situ or by collecting specimens and rearing them in aquaria, is particularly challenging for deep-sea organisms like cold-water corals. Field experimental work and monitoring of deep-sea populations is still a chimera. Only a handful of research institutes or companies has been able to install in situ marine observatories in the Mediterranean Sea or elsewhere, which facilitate a continuous monitoring of deep-sea ecosystems. Hence, today’s best way to obtain basic biological information on these organisms is (1) working with collected samples and analysing them post-mortem and / or (2) cultivating corals in aquaria in order to monitor biological processes and investigate coral behaviour and physiological responses under different experimental treatments. The first challenging aspect is the collection process, which implies the use of oceanographic research vessels in most occasions since these organisms inhabit areas between ca. 150 m to more than 1000 m depth, and specific sampling gears. The next challenge is the maintenance of the animals on board (in situations where cruises may take weeks) and their transport to home laboratories. Maintenance in the home laboratories is also extremely challenging since special conditions and set-ups are needed to conduct experimental studies to obtain information on the biological processes of these animals. The complexity of the natural environment from which the corals were collected cannot be exactly replicated within the laboratory setting; a fact which has led some researchers to question the validity of work and conclusions drawn from such undertakings. It is evident that aquaria experiments cannot perfectly reflect the real environmental and trophic conditions where these organisms occur, but: (1) in most cases we do not have the possibility to obtain equivalent in situ information and (2) even with limitations, they produce relevant information about the biological limits of the species, which is especially valuable when considering potential future climate change scenarios. This chapter includes many contributions from different authors and is envisioned as both to be a practical “handbook” for conducting cold-water coral aquaria work, whilst at the same time offering an overview on the cold-water coral research conducted in Mediterranean laboratories equipped with aquaria infrastructure. Experiences from Atlantic and Pacific laboratories with extensive experience with cold-water coral work have also contributed to this chapter, as their procedures are valuable to any researcher interested in conducting experimental work with cold-water corals in aquaria. It was impossible to include contributions from all laboratories in the world currently working experimentally with cold-water corals in the laboratory, but at the conclusion of the chapter we attempt, to our best of our knowledge, to supply a list of several laboratories with operational cold-water coral aquaria facilities.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
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