Lee O Case's "Elements of the Phase Rule", Introduction and Explanation

This out of print 1939 manuscript, updated, is added to the literature with slight additions

A model for use by local public health departments to evaluate pandemic influenza plans

The events of the 1990's and early 2000's demonstrated the need for effective planning and response to natural and man-made disasters. One of those potential natural disasters is pandemic flu. Once defined, the CDC stated that program, or plan, effectiveness is improved through the process of program evaluation. (Centers for Disease Control and Prevention, 1999) Program evaluation should be accomplished not only periodically, but in the course of routine administration of the program. (Centers for Disease Control and Prevention, 1999) Accomplishing this task for a "rare, but significant event" is challenging. (Herbold, John R., PhD., 2008) To address this challenge, the RAND Corporation (under contract to the CDC) developed the "Facilitated Look-Backs" approach that was tested and validated at the state level. (Aledort et al., 2006).^ Nevertheless, no comprehensive and generally applicable pandemic influenza program evaluation tool or model is readily found for use at the local public health department level. This project developed such a model based on the "Facilitated Look-Backs" approach developed by RAND Corporation. (Aledort et al., 2006) Modifications to the RAND model included stakeholder additions, inclusion of all six CDC program evaluation steps, and suggestions for incorporating pandemic flu response plans in seasonal flu management implementation. Feedback on the model was then obtained from three LPHD's—one rural, one suburban, and one urban. These recommendations were incorporated into the final model. Feedback from the sites also supported the assumption that this model promotes the effective and efficient evaluation of both pandemic flu and seasonal flu response by reducing redundant evaluations of pandemic flu plans, seasonal flu plans, and funding requirement accountability. Site feedback also demonstrated that the model is comprehensive and flexible, so it can be adapted and applied to different LPHD needs and settings. It also stimulates evaluation of the major issues associated with pandemic flu planning. ^ The next phase in evaluating this model should be to apply it in a program evaluation of one or more LPHD's seasonal flu response that incorporates pandemic flu response plans.^

Influencia de cuatro alternativas de crianza en roble sobre el color, la composición polifenológica y las características organolépticas de vinos Malbec y Cabernet Sauvignon

Los costos de las barricas, por el tipo de cambio en la Argentina, son inaccesibles para muchas bodegas. Debido a esto, muchas de ellas utilizan sistemas alternativos de crianza, no conociendo claramente las consecuencias y los fenómenos que ocurren con el uso de estos sistemas. El objetivo del trabajo fue evaluar la composición polifenólica, el color y los caracteres sensoriales de vinos tratados con distintos sistemas de crianza en madera. Para ello se utilizaron métodos espectofotométricos rápidos y fácilmente realizables en bodega. Los tra tamientos a los cuales se sometió el vino fueron: barrica de roble americano de primer uso, barrica de más de cinco años de uso reacondicionada, vasija de acero inoxidable con “dominó" de roble en dosis comúnmente usadas en el medio, vasija de acero inoxidable con “dominó" de roble en dosis equivalentes a la superficie de contacto de la barrica y vino sin madera tomado como testigo. El ensayo se realizó con vinos cosecha 2007 de las variedades Malbec y Cabernet Sauvignon y el tiempo de crianza fue de 10 meses. Los resultados mostraron que en ninguna de las variedades los tratamientos con barricas obtuvieron mayor nivel de polimerización que el resto de los tratamientos ni tampoco los sistemas con agregado de fragmentos de roble superaron en polimerización al vino sin madera. Por otro lado, sólo en la variedad Cabernet Sauvignon la barrica nueva superó en intensidad de color al vino sin madera. En cambio, los tratamientos con roble favorecieron la copigmentación y los copigmentos inhibieron la polimerización, haciendo más lenta la formación de uniones tanino- antocianos pero también protegiendo el color y evitando oxidaciones, esta situación podría explicar los resultados contradictorios entre distintos autores. En el aspecto sensorial los vinos en barricas no obtuvieron mayor intensidad de color ni menor astringencia que los vinos con agregado de roble y tampoco estos últimos lograron diferencias con el vino testigo. Por otro lado en ambas variedades, la barrica nueva y el tratamiento con alta dosis de dominó de roble tuvieron la mayor intensidad aromática con descriptores como vainilla y chocolate aunque la alternativa de crianza con “dominó" estuvo muy ligada al descriptor “tabla". La barrica reacondicionada mostró el mayor nivel del descriptor betún y en el tratamiento testigo se detectaron aromas de reducción. El tratamiento con dominó de roble en dosis comerciales se encontró más ligado a los aromas frutados.

Textos y contextos en narraciones orales de migrantes provincianos

La tesis se centra en el estudio de las narraciones orales de migrantes provincianos, afincados en el conurbano platense, desde 1940. Las narraciones orales se denominan, en esta tesis, de retroalimentación ya que narradores y receptores recrean su origen, sus estrategias de reinserción en una nueva comunidad y de supervivencia de sus tradiciones. Estos textos han sido considerados de acuerdo con su problemática genérica (Bajtin; 1979) como narraciones de ficción (cuentos, chistes, fábulas) y de no-ficción (crónicas personales, anécdotas) y, asimismo, observar procesos de entextualización, cuando una misma narración presenta caracteres de ambas clasificaciones. De este modo, cada texto delimita su género en la situación de narración (Bauman y Briggs: 2003) Dichas narraciones deben ser analizadas por sus contextos de enunciación (Bausinger: 1988, 8-28). Los contextos de enunciación, según Hermann Bausinger, son textual, la conversación en sí misma, situacional, las circunstancias de emisores y receptores, social, del grupo de narración, de su grupo de pertenencia y de los grupos con los que interactúa, y societal, en cuanto a las relaciones con la sociedad mayoritaria son fundamentales al punto de que dos versiones de una misma narración se analizan de acuerdo con contextos de enunciación diferentes, con significaciones sociales disímiles. Dentro de los contextos de enunciación, la tesis propone el análisis del contexto ideológico (Coto: 2008), como signo de la intersubjetividad entre narradores y receptores. El contexto ideológico se analiza a partir de la selección de lexemas relevantes con sus definiciones contextuales, para constituir redes de enunciados, que revelan la ideología de narradores y receptores. La tesis propone establecer una matriz ideológica individual y grupal, observando los lexemas recurrentes en versiones de una misma narración, sus adiciones, supresiones y cambios de significación. Además, los textos puede compararse de acuerdo con sus relaciones intratextuales, intertextuales y extratextuales, en el marco de la genética textual (Palleiro: 2004). Finalmente, la tesis propone una metodología de análisis de las narrativas orales, en el marco de la cultura popular, tradicional y folklórica, con la observación de estrategias narrativas y macrorreglas (Van Dijk: 1983), estilo y (Kerbrat-Orecchioni: 1983) y representatividad sociolingüística. (Van Dijk: 1999 y Magariños: 1993). Estas consideraciones prueban la importancia de esta tesis para los intelectuales dedicados al análisis del discurso y a la interpretación de discursos sociales de grupos minoritarios, es decir, docentes, narradores orales, sociólogos y antropólogos. Asimismo, puede ser muy útil para animadores culturales y comunicadores sociales. La tesis postula continuar estos estudios, observando las relaciones entre narrativas de ficción y de no ficción, como el rumor, la leyenda urbana y la crónica periodística

Textos y contextos en narraciones orales de migrantes provincianos

La tesis se centra en el estudio de las narraciones orales de migrantes provincianos, afincados en el conurbano platense, desde 1940. Las narraciones orales se denominan, en esta tesis, de retroalimentación ya que narradores y receptores recrean su origen, sus estrategias de reinserción en una nueva comunidad y de supervivencia de sus tradiciones. Estos textos han sido considerados de acuerdo con su problemática genérica (Bajtin; 1979) como narraciones de ficción (cuentos, chistes, fábulas) y de no-ficción (crónicas personales, anécdotas) y, asimismo, observar procesos de entextualización, cuando una misma narración presenta caracteres de ambas clasificaciones. De este modo, cada texto delimita su género en la situación de narración (Bauman y Briggs: 2003) Dichas narraciones deben ser analizadas por sus contextos de enunciación (Bausinger: 1988, 8-28). Los contextos de enunciación, según Hermann Bausinger, son textual, la conversación en sí misma, situacional, las circunstancias de emisores y receptores, social, del grupo de narración, de su grupo de pertenencia y de los grupos con los que interactúa, y societal, en cuanto a las relaciones con la sociedad mayoritaria son fundamentales al punto de que dos versiones de una misma narración se analizan de acuerdo con contextos de enunciación diferentes, con significaciones sociales disímiles. Dentro de los contextos de enunciación, la tesis propone el análisis del contexto ideológico (Coto: 2008), como signo de la intersubjetividad entre narradores y receptores. El contexto ideológico se analiza a partir de la selección de lexemas relevantes con sus definiciones contextuales, para constituir redes de enunciados, que revelan la ideología de narradores y receptores. La tesis propone establecer una matriz ideológica individual y grupal, observando los lexemas recurrentes en versiones de una misma narración, sus adiciones, supresiones y cambios de significación. Además, los textos puede compararse de acuerdo con sus relaciones intratextuales, intertextuales y extratextuales, en el marco de la genética textual (Palleiro: 2004). Finalmente, la tesis propone una metodología de análisis de las narrativas orales, en el marco de la cultura popular, tradicional y folklórica, con la observación de estrategias narrativas y macrorreglas (Van Dijk: 1983), estilo y (Kerbrat-Orecchioni: 1983) y representatividad sociolingüística. (Van Dijk: 1999 y Magariños: 1993). Estas consideraciones prueban la importancia de esta tesis para los intelectuales dedicados al análisis del discurso y a la interpretación de discursos sociales de grupos minoritarios, es decir, docentes, narradores orales, sociólogos y antropólogos. Asimismo, puede ser muy útil para animadores culturales y comunicadores sociales. La tesis postula continuar estos estudios, observando las relaciones entre narrativas de ficción y de no ficción, como el rumor, la leyenda urbana y la crónica periodística

Major and trace element composition of sepentine muds and metabasic rocks of ODP Leg 195 and Leg 125 sites

New geochemical data on serpentinite muds and metamorphic clasts recovered during Ocean Drilling Program Legs 195 (Holes 1200A-1200E) and 125 (Holes 778A and 779A) provide insights into the proportions of rock types of various sources that compose the serpentinite mudflows and the fluid-rock interactions that predominate in these muds. We interpret the metamorphic rock fragments as derivatives of mostly metamorphosed mafic rocks from the descending Pacific oceanic crust. Based on their mid-ocean-ridge basalt (MORB)-like Al2O3, TiO2, CaO, Si/Mg, and rare earth element (REE) systematics, these metamorphic rocks are classified as metabasalts/metagabbros and, therefore, ~30-km depths represent an active subduction zone setting. The serpentinite muds from Holes 1200A and 1200E have slightly lower REE when compared to Hole 1200D, but overall the REE abundance levels range between 0.1-1 x chondrite (CI) levels. The chondrite-normalized patterns have [La/Sm]N ~ 2.3 and [Sm/Yb]N ~ 2. With the exception of one sample, the analyzed metamorphic clasts show flat to slightly depleted light REE patterns with 1.0-15 x CI levels, resembling MORBs. Visually, ~6 vol% of the serpentinized muds are composed of 'exotic' materials (metamorphic clasts [schists]). Our mixing calculations confirm this result and show that the serpentinite muds are produced by additions of ~5% metamafic materials (with flat and up to 10 x CI REE levels) to serpentinized peridotite clast material (with very low REE abundances and U-shaped chondrite-normalized patterns). The preferential incorporation of B, Cs, Rb, Li, As, Sb, and Ba into the structure of H2O-bearing sheet silicates (different than serpentine) in the Leg 125 and Leg 195 metamorphic clasts (chlorite, amphibole, and micas) have little effect on the overall fluid-mobile element (FME) enrichments in the serpentinite muds (average B = ~13 ppm; average Cs = ~0.05 ppm; average As = ~1.25 ppm). The extent of FME enrichment in the serpentinized muds is similar to that described for the serpentinized peridotites, both recording interaction with fluids very rich in B, Cs, and As originating from the subducting Pacific slab.

Textos y contextos en narraciones orales de migrantes provincianos

La tesis se centra en el estudio de las narraciones orales de migrantes provincianos, afincados en el conurbano platense, desde 1940. Las narraciones orales se denominan, en esta tesis, de retroalimentación ya que narradores y receptores recrean su origen, sus estrategias de reinserción en una nueva comunidad y de supervivencia de sus tradiciones. Estos textos han sido considerados de acuerdo con su problemática genérica (Bajtin; 1979) como narraciones de ficción (cuentos, chistes, fábulas) y de no-ficción (crónicas personales, anécdotas) y, asimismo, observar procesos de entextualización, cuando una misma narración presenta caracteres de ambas clasificaciones. De este modo, cada texto delimita su género en la situación de narración (Bauman y Briggs: 2003) Dichas narraciones deben ser analizadas por sus contextos de enunciación (Bausinger: 1988, 8-28). Los contextos de enunciación, según Hermann Bausinger, son textual, la conversación en sí misma, situacional, las circunstancias de emisores y receptores, social, del grupo de narración, de su grupo de pertenencia y de los grupos con los que interactúa, y societal, en cuanto a las relaciones con la sociedad mayoritaria son fundamentales al punto de que dos versiones de una misma narración se analizan de acuerdo con contextos de enunciación diferentes, con significaciones sociales disímiles. Dentro de los contextos de enunciación, la tesis propone el análisis del contexto ideológico (Coto: 2008), como signo de la intersubjetividad entre narradores y receptores. El contexto ideológico se analiza a partir de la selección de lexemas relevantes con sus definiciones contextuales, para constituir redes de enunciados, que revelan la ideología de narradores y receptores. La tesis propone establecer una matriz ideológica individual y grupal, observando los lexemas recurrentes en versiones de una misma narración, sus adiciones, supresiones y cambios de significación. Además, los textos puede compararse de acuerdo con sus relaciones intratextuales, intertextuales y extratextuales, en el marco de la genética textual (Palleiro: 2004). Finalmente, la tesis propone una metodología de análisis de las narrativas orales, en el marco de la cultura popular, tradicional y folklórica, con la observación de estrategias narrativas y macrorreglas (Van Dijk: 1983), estilo y (Kerbrat-Orecchioni: 1983) y representatividad sociolingüística. (Van Dijk: 1999 y Magariños: 1993). Estas consideraciones prueban la importancia de esta tesis para los intelectuales dedicados al análisis del discurso y a la interpretación de discursos sociales de grupos minoritarios, es decir, docentes, narradores orales, sociólogos y antropólogos. Asimismo, puede ser muy útil para animadores culturales y comunicadores sociales. La tesis postula continuar estos estudios, observando las relaciones entre narrativas de ficción y de no ficción, como el rumor, la leyenda urbana y la crónica periodística

Sulphur geochemistry of whole-rock samples from ODP Hole 176-735B

Sulfide petrography plus whole rock contents and isotope ratios of sulfur were measured in a 1.5 km section of oceanic gabbros in order to understand the geochemistry of sulfur cycling during low-temperature seawater alteration of the lower oceanic crust, and to test whether microbial effects may be present. Most samples have low SO4/Sum S values (<= 0.15), have retained igneous globules of pyrrhotite ± chalcopyrite ± pentlandite, and host secondary aggregates of pyrrhotite and pyrite laths in smectite ± iron-oxyhydroxide ± magnetite ± calcite pseudomorphs of olivine and clinopyroxene. Compared to fresh gabbro containing 100-1800 ppm sulfur our data indicate an overall addition of sulfide to the lower crust. Selection of samples altered only at temperatures <= 110 °C constrains microbial sulfate reduction as the only viable mechanism for the observed sulfide addition, which may have been enabled by the production of H2 from oxidation of associated olivine and pyroxene. The wide range in d34Ssulfide values (-1.5 to + 16.3 per mil) and variable additions of sulfide are explained by variable epsilon sulfate-sulfide under open system pathways, with a possible progression into closed system pathways. Some samples underwent oxidation related to seawater penetration along permeable fault horizons and have lost sulfur, have high SO4/Sum S (>= 0.46) and variable d34Ssulfide (0.7 to 16.9 per mil). Negative d34Ssulfate-d34Ssulfide values for the majority of samples indicate kinetic isotope fractionation during oxidation of sulfide minerals. Depth trends in sulfide-sulfur contents and sulfide mineral assemblages indicate a late-stage downward penetration of seawater into the lower 1 km of Hole 735B. Our results show that under appropriate temperature conditions, a subsurface biosphere can persist in the lower oceanic crust and alter its geochemistry.

Lithogeochemical and isotope (Rb-Sr, Sm-Nd, Pb-Pb whole rock and Lu-Hf zircon) composition of samples from the Shackleton Range, East Antarctica

Three distinct, spatially separated crustal terranes have been recognised in the Shackleton Range, East Antarctica: the Southern, Eastern and Northern Terranes. Mafic gneisses from the Southern Terrane provide geochemical evidence for a within-plate, probably back-arc origin of their protoliths. A plume-distal ridge origin in an incipient ocean basin is the favoured interpretation for the emplacement site of these rocks at c. 1850 Ma, which, together with a few ocean island basalts, were subsequently incorporated into an accretionary continental arc/supra-subduction zone tectonic setting. Magmatic underplating resulted in partial melting of the lower crust, which caused high-temperature granulite-facies metamorphism in the Southern Terrane at c. 1710-1680 Ma. Mafic and felsic gneisses there are characterised by isotopically depleted, positive Nd and Hf initials and model ages between 2100 and 2000 Ma. They may be explained as juvenile additions to the crust towards the end of the Palaeoproterozoic. These juvenile rocks occur in a narrow, c. 150 km long E-W trending belt, inferred to trace a suture that is associated with a large Palaeoproterozoic accretionary orogenic system. The Southern Terrane contains many features that are similar to the Australo-Antarctic Mawson Continent and may be its furthermost extension into East Antarctica. The Eastern Terrane is characterised by metagranitoids that formed in a continental volcanic arc setting during a late Mesoproterozoic orogeny at c. 1060 Ma. Subsequently, the rocks experienced high-temperature metamorphism during Pan-African collisional tectonics at 600 Ma. Isotopically depleted zircon grains yielded Hf model ages of 1600-1400 Ma, which are identical to Nd model ages obtained from juvenile metagranitoids. Most likely, these rocks trace the suture related to the amalgamation of the Indo-Antarctic and West Gondwana continental blocks at ~600 Ma. The Eastern Terrane is interpreted as the southernmost extension of the Pan-African Mozambique/Maud Belt in East Antarctica and, based on Hf isotope data, may also represent a link to the Ellsworth-Whitmore Mountains block in West Antarctica and the Namaqua-Natal Province of southern Africa. Geochemical evidence indicates that the majority of the protoliths of the mafic gneisses in the Northern Terrane formed as oceanic island basalts in a within-plate setting. Subsequently the rocks were incorporated into a subduction zone environment and, finally, accreted to a continental margin during Pan-African collisional tectonics. Felsic gneisses there provide evidence for a within-plate and volcanic arc/collisional origin. Emplacement of granitoids occurred at c. 530 Ma and high-temperature, high-pressure metamorphism took place at 510-500 Ma. Enriched Hf and Nd initials and Palaeoproterozoic model ages for most samples indicate that no juvenile material was added to the crust of the Northern Terrane during the Pan-African Orogeny but recycling of older crust or mixing of crustal components of different age must have occurred. Isotopically depleted mafic gneisses, which are spatially associated with eclogite-facies pyroxenites, yielded late Mesoproterozoic Nd model ages. These rocks occur in a narrow, at least 100 km long, E-W trending belt that separates alkaline ocean island metabasalts and within-plate metagranitoids from volcanic arc metabasalts and volcanic arc/syn-collisional metagranitoids in the Northern Terrane. This belt is interpreted to trace the late Neoproterozoic/early Cambrian Pan-African collisional suture between the Australo-Antarctic and the combined Indo-Antarctic/West Gondwana continental blocks that formed during the final amalgamation of Gondwana.

Chemical and mineral compositions of altered peridotites from ODP Leg 209

Abyssal peridotite from the 15°20'N area of the Mid-Atlantic Ridge show complex geochemical variations among the different sites drilled during ODP Leg 209. Major element compositions indicate variable degrees of melt depletion and refertilization as well as local hydrothermal metasomatism. Strongest evidence for melt-rock interactions are correlated Light Rare Earth Element (LREE) and High Field Strength Element (HFSE) additions at Sites 1270 and 1271. In contrast, hydrothermal alteration at Sites 1274, 1272, and 1268 causes LREE mobility associated with minor HFSE variability, reflecting the low solubility of HFSE in aqueous solutions. Site 1274 contains the least-altered, highly refractory, peridotite with strong depletion in LREE and shows a gradual increase in the intensity of isochemical serpentinization; except for the addition of H2O which causes a mass gain of up to 20 g/100 g. The formation of magnetite is reflected in decreasing Fe(2+)/Fe(3+) ratios. This style of alteration is referred to as rock-dominated serpentinization. In contrast, fluid-dominated serpentinization at Site 1268 is characterized by gains in sulfur and development of U-shaped REE pattern with strong positive Eu anomalies which are also characteristic for hot (350 to 400°C) vent-type fluids discharging from black smoker fields. Serpentinites at Site 1268 were overprinted by talc alteration under static conditions due to interaction with high a_SiO2 fluids causing the development of smooth, LREE enriched patterns with pronounced negative Eu anomalies. These results show that hydrothermal fluid-peridotite and fluid-serpentinite interaction processes are an important factor regarding the budget of exchange processes between the lithosphere and the hydrosphere in slow spreading environments.

Sulphur chemistry of the ODP Site 206-1256 volcanic section

Sulfide mineralogy and the contents and isotope compositions of sulfur were analyzed in a complete oceanic volcanic section from IODP Hole 1256D in the eastern Pacific, in order to investigate the role of microbes and their effect on the sulfur budget in altered upper oceanic crust. Basalts in the 800 m thick volcanic section are affected by a pervasive low-temperature background alteration and have mean sulfur contents of 530 ppm, reflecting loss of sulfur relative to fresh glass through degassing during eruption and alteration by seawater. Alteration halos along fractures average 155 ppm sulfur and are more oxidized, have high SO4/Sum S ratios (0.43), and lost sulfur through oxidation by seawater compared to host rocks. Although sulfur was lost locally, sulfur was subsequently gained through fixation of seawater-derived sulfur in secondary pyrite and marcasite in veins and in concentrations at the boundary between alteration halos and host rocks. Negative d34S[sulfide-S] values (down to -30 per mil) and low temperatures of alteration (down to ~40 °C) point to microbial reduction of seawater sulfate as the process resulting in local additions of sulfide-S. Mass balance calculations indicate that 15-20% of the sulfur in the volcanic section is microbially derived, with the bulk altered volcanic section containing 940 ppm S, and with d34S shifted to -6.0 per mil from the mantle value (0 per mil). The bulk volcanic section may have gained or lost sulfur overall. The annual flux of microbial sulfur into oceanic basement based on Hole 1256D is 3-4 * 10**10 mol S/yr, within an order of magnitude of the riverine sulfate source and the sedimentary pyrite sink. Results indicate a flux of bacterially derived sulfur that is fixed in upper ocean basement of 7-8 * 10**-8 mol/cm**-2/yr1 over 15 m.y. This is comparable to that in open ocean sediment sites, but is one to two orders of magnitude less than for ocean margin sediments. The global annual subduction of sulfur in altered oceanic basalt lavas based on Hole 1256D is 1.5-2.0 * 10**11 mol/yr, comparable to the subduction of sulfide in sediments, and could contribute to sediment-like sulfur isotope heterogeneities in the mantle.

(Table 1) Platinum group element abundanves in ODP Leg 135 samples

Ocean Drilling Program Leg 135 backarc basin lavas are characterized by anomalously high Au contents (1.0-11.4 ppb) and strongly fractionated relative platinum group element (PGE) abundances (Pd/Ir ratio, approximately 100). The Rh and Ir contents are very low, ranging from below detection (approximately 0.02 ppb) to 0.08 ppb. The Pd and Pt contents range from <0.3 to 4 ppb. Rh, Pd, and Pt values are consistently and significantly higher in Site 836 and 839 samples relative to those from Sites 834 and 835. Major, trace, and rare earth element (REE) data suggest Sites 836 and 839 have a more pronounced arc signature than Sites 834 and 835. No correlation exists between noble metal abundance and indices of alteration or fractionation (e.g., loss on ignition (LOI), Mg#, and Cr or Ni contents), suggesting that measured values and ratios are primary and reflect characteristics of the mantle source. The evaluation of Leg 135 noble metal data with respect to potential mantle-source components is hindered by the lack of data on magmas derived from such sources. However, analyses of the limited available data for the different magma types suggest that the characteristic enrichment of Leg 135 lavas in Au, relative to Pd and Cu, cannot be derived solely from simple MORB-type or ocean-island-type mantle, or mantle depleted by a previous melt extraction event. The Au-enriched signature of the Lau basin lavas could, however, be produced through the addition of a sedimentary component from the downgoing slab. Separation of Au from the PGE occurs within oceanic hydrothermal systems and gold values of the resultant precipitates are 2-3 orders of magnitude higher than other oceanic crustal components. Even small additions of this component from the downgoing oceanic crust to a supra-subduction zone mantle melt could account for the high mean Au/Pd ratios of the Leg 135 samples (Sites 834 and 835, Au/Pd = 5.04; Sites 836 and 839, Au/Pd = 2.26).

Seawater carbonate chemistry and calcification during experiments with a coral Madracis auretenra, 2010

Physiological data and models of coral calcification indicate that corals utilize a combination of seawater bicarbonate and (mainly) respiratory CO2 for calcification, not seawater carbonate. However, a number of investigators are attributing observed negative effects of experimental seawater acidification by CO2 or hydrochloric acid additions to a reduction in seawater carbonate ion concentration and thus aragonite saturation state. Thus, there is a discrepancy between the physiological and geochemical views of coral biomineralization. Furthermore, not all calcifying organisms respond negatively to decreased pH or saturation state. Together, these discrepancies suggest that other physiological mechanisms, such as a direct effect of reduced pH on calcium or bicarbonate ion transport and/or variable ability to regulate internal pH, are responsible for the variability in reported experimental effects of acidification on calcification. To distinguish the effects of pH, carbonate concentration and bicarbonate concentration on coral calcification, incubations were performed with the coral Madracis auretenra (= Madracis mirabilis sensu Wells, 1973) in modified seawater chemistries. Carbonate parameters were manipulated to isolate the effects of each parameter more effectively than in previous studies, with a total of six different chemistries. Among treatment differences were highly significant. The corals responded strongly to variation in bicarbonate concentration, but not consistently to carbonate concentration, aragonite saturation state or pH. Corals calcified at normal or elevated rates under low pH (7.6-7.8) when the seawater bicarbonate concentrations were above 1800 µm. Conversely, corals incubated at normal pH had low calcification rates if the bicarbonate concentration was lowered. These results demonstrate that coral responses to ocean acidification are more diverse than currently thought, and question the reliability of using carbonate concentration or aragonite saturation state as the sole predictor of the effects of ocean acidification on coral calcification.

Seawater carbonate chemistry and processes during an experiment with coral reef, 2000

The concentration of CO2 in the atmosphere is projected to reach twice the preindustrial level by the middle of the 21st century. This increase will reduce the concentration of [CO3]2- of the surface ocean by 30% relative to the preindustrial level and will reduce the calcium carbonate saturation state of the surface ocean by an equal percentage. Using the large 2650 m3 coral reef mesocosm at the BIOSPHERE-2 facility near Tucson, Arizona, we investigated the effect of the projected changes in seawater carbonate chemistry on the calcification of coral reef organisms at the community scale. Our experimental design was to obtain a long (3.8 years) time series of the net calcification of the complete system and all relevant physical and chemical variables (temperature, salinity, light, nutrients, Ca2+,pCO2, TCO2, and total alkalinity). Periodic additions of NaHCO3, Na2CO3, and/or CaCl2 were made to change the calcium carbonate saturation state of the water. We found that there were consistent and reproducible changes in the rate of calcification in response to our manipulations of the saturation state. We show that the net community calcification rate responds to manipulations in the concentrations of both Ca2+ and [CO3]2- and that the rate is well described as a linear function of the ion concentration product, [Ca2+]0.69[[CO3]2-]. This suggests that saturation state or a closely related quantity is a primary environmental factor that influences calcification on coral reefs at the ecosystem level. We compare the sensitivity of calcification to short-term (days) and long-term (months to years) changes in saturation state and found that the response was not significantly different. This indicates that coral reef organisms do not seem to be able to acclimate to changing saturation state. The predicted decrease in coral reef calcification between the years 1880 and 2065 A.D. based on our long-term results is 40%. Previous small-scale, short-term organismal studies predicted a calcification reduction of 14-30%. This much longer, community-scale study suggests that the impact on coral reefs may be greater than previously suspected. In the next century coral reefs will be less able to cope with rising sea level and other anthropogenic stresses.

Ocean acidification outweighs nutrient effects in structuring seagrass epiphyte communities

1. Developing a framework for assessing interactions between multiple anthropogenic stressors remains an important goal in environmental research. In coastal ecosystems, the relative effects of aspects of global climate change (e.g. CO2 concentrations) and localized stressors (e.g. eutrophication), in combination, have received limited attention. 2. Using a long-term (11 month) field experiment, we examine how epiphyte assemblages in a tropical seagrass meadow respond to factorial manipulations of dissolved carbon dioxide (CO2(aq)) and nutrient enrichment. In situ CO2(aq) manipulations were conducted using clear, open-top chambers, which replicated carbonate parameter forecasts for the year 2100. Nutrient enrichment consisted of monthly additions of slow-release fertilizer, nitrogen (N) and phosphorus (P), to the sediments at rates equivalent to theoretical maximum rates of anthropogenic loading within the region (1.54 g N/m**2/d and 0.24 g P m**2/d). 3. Epiphyte community structure was assessed on a seasonal basis and revealed declines in the abundance of coralline algae, along with increases in filamentous algae under elevated CO2(aq). Surprisingly, nutrient enrichment had no effect on epiphyte community structure or overall epiphyte loading. Interactions between CO2(aq) and nutrient enrichment were not detected. Furthermore, CO2(aq)-mediated responses in the epiphyte community displayed strong seasonality, suggesting that climate change studies in variable environments should be conducted over extended time-scales. 4. Synthesis. The observed responses indicate that for certain locations, global stressors such as ocean acidification may take precedence over local eutrophication in altering the community structure of seagrass epiphyte assemblages. Given that nutrient-driven algal overgrowth is commonly cited as a widespread cause of seagrass decline, our findings highlight that alternate climate change forces may exert proximate control over epiphyte community structure.