Stable isotope composition of Holocene benthic foraminifers from the Eastern Mediterranean Sea

Temporal and regional changes in paleoproductivity and paleoceanography in the eastern Mediterranean Sea during the past 12 kyr were reconstructed on the basis of the stable oxygen and carbon isotope composition of the epibenthic Planulina ariminensis and the shallow endobenthic Uvigerina mediterranea from three sediment cores of the Aegean Sea and Levantine Basin. The Younger Dryas is characterized by high d18O values, indicating enhanced salinities and low temperatures of deep water masses at all investigated sites. With the onset of the Holocene, d18O records show a continuous decrease towards the onset of sapropel S1 formation, mainly caused by a freshening and warming of surface waters at deep water formation sites. In the middle and late Holocene, the similarity of d18O values from the southern Aegean Sea and Levantine Basin suggests the influence of isotopically identical deep water masses. By contrast, slightly higher d18O values are observed the northern Aegean Sea, which probably point to lower temperatures of North Aegean deep waters. The epifaunal d13C records reveal clear changes in sources and residence times of eastern Mediterranean deep waters associated with period of S1 formation. Available data for the early and late phase of sapropel S1 formation and for the interruption around 8.2 kyr display drops by 0.5 and 1.5 per mil, indicating the slow-down of deep water circulation and enhanced riverine input of isotopically light dissolved inorganic carbon from terrestrial sources into the eastern Mediterranean Sea. The decrease in epifaunal d13C signals is particularly expressed in the southern Aegean Sea and Levantine Basin, while it is less pronounced in the northern Aegean Sea. This points to a strong reduction in deep water exchange rates in the southern areas, but the persistence of local deep water formation in the northern Aegean Sea. The d13C values of U. mediterranea records reveal temporal and regional differences in paleoproductivity during the past 12 kyr, with rather eutrophic and mesotrophic conditions in the North Aegean Sea and southeast Levantine Basin, respectively, while the South Aegean Sea is characterized by rather oligotrophic conditions. After S1 formation, increasing d13C values reflect a progressive decrease in surface water productivity in the eastern Mediterranean Sea during the middle and late Holocene. In the northern Aegean Sea, this time interval is marked by repetitive changes in organic matter fluxes documented by significant fluctuations in the d13C signal of U. mediterranea on millennial- to multi-centennial time scales. These fluctuations can be linked to short-term changes in river runoff driven by northern hemisphere climatic variability.

Stable isotopic and carbonate cyclicity in deep sea sediments from different DSDP Holes

Oxygen and carbon isotopic variability of the dominant (<38 µm) carbonate fraction within bedded, organic-carbon rich Lower Cretaceous sediment intervals from various DSDP sites are closely correlated with preservational changes in the carbonates. Isotopic fluctuations are absent where carbonate contents vary little and where the carbonate fraction is dominated by biogenic phytoplankton remains. Within each of the studied intervals oxygen and carbon isotopic ratios become increasingly more negative in samples with carbonate contents higher than about 60% in which the proportion of diagenetic microcarbonate increases rapidly. Carbon isotopic ratios show a trend towards positive values in samples with carbonate contents of less than 40% and strong signs of dissolution. The taxonomic composition of nannofossil assemblages varies little within single intervals, despite significant differential diagenesis among individual beds; this points towards ecological stability of oceanic surface waters during the deposition of alternating beds. Bedding is, however, closely related to changing bioturbation intensity, indicating repeated fluctuations of the deep-water renewal rates and oxygen supply. Various microbial decomposition processes of organic matter leading to bed-specific differential carbonate diagenesis resulted in an amplification of primary bedding features and are considered responsible for most of the observed fluctuations in the stable isotopic ratios and carbonate contents.

Stable isotope analysis on planktic foraminifera in sediment cores from the eastern Mediterranean sapropel formation

During the late Pleistocene, sapropels (layers of organic-carbon rich sediment) formed throughout the entire Eastern Mediterranean Basin in close association with glacial/interglacial transitions. The current theory for the mechanism of sapropel formation involves a density stratification of the water column, due to the invasion of a large quantity of low-saline water, which resulted in oxygen depletion of the bottom waters. Most workers believe that this low-salinity water was glacial meltwater that entered the Mediterranean via the Black Sea and a series of interconnected glacial lakes, but the suggestion also has been made that the freshwater originated from the Nile River. In this study the oxygen isotope values of planktonic foraminifera,Globigerinoides ruber, have been examined in six gravity cores and one piston core from the southern Levantine Basin, and compared with the oxygen isotope records ofG. ruber from other areas of the Eastern Mediterranean. This study deals mainly with the latest sapropel which was deposited approximately 7000 to 9000 years ago. Results indicate that Nile discharge probably does reduce salinities somewhat in the immediate area surrounding the mouth of the Nile, but this water is rapidly mixed with the highly saline waters of the easternmost Mediterranean. Using a mixing equation and surface water salinity limitations, an approximate oxygen isotope balance of surface waters was calculated for the time of latest sapropel deposition. This calculation shows that neither Nile River discharge nor Black Sea input (nor both together) are large enough to account for the large-scale oxygen isotope depletion associated with latest sapropel deposition in the Eastern Mediterranean. This suggests that part of the isotopic change at Termination I is probably due to increased surface water salinities during the last glacial maximum. In addition, evidence from the timing of sapropel 1 deposition and the dissolved oxygen balance indicates that deposition of the latest sapropel is associated with increased surface water production of biogenic material, as much as three times higher than that of present day.

Nd isotope data for ODP Leg 208 holes

The flow of deep-water masses is a key component of heat transport in the modern climate system, yet the role of deep-ocean heat transport during periods of extreme warmth is poorly understood. The present mode of meridional overturning circulation is characterized by deep-water formation in both the North Atlantic and the Southern Ocean. However, a different mode of meridional overturning circulation operated during the extreme greenhouse warmth of the early Cenozoic, during which time the Southern Ocean was the dominant region of deep-water formation. The combination of general global cooling and tectonic evolution of the Atlantic basins over the past ~55 m.y. ultimately led to the development of a mode of overturning circulation characterized by both Southern Ocean and North Atlantic deep-water sources. The change in deep-water circulation mode may, in turn, have affected global climate; however, unraveling the causes and consequences of this transition requires a better understanding of the timing of the transition. New Nd isotope data from the southeastern Atlantic Ocean indicate that the initial transition to a bipolar mode of deep-water circulation occurred in the early Oligocene, ca. 33 Ma. The likely cause of significant deep-water production in the North Atlantic was tectonic deepening of the sill separating the Greenland-Norwegian Sea from the North Atlantic.

(Appendix table DR1) Foraminiferal distribution data for ODP Hole 178-1098B

Benthic foraminiferal data from Ocean Drilling Program Site 1098 indicate significant changes in deep-water conditions of the Palmer Deep, western Antarctic Peninsula margin, throughout the Holocene (13 ka to present). The earliest Holocene represents a period of transition from the Last Glacial Maximum (LGM). Cold bottom waters, similar to saline shelf water (SSW), dominated the middle Holocene. The late Holocene in the Palmer Deep has been characterized by alternating dominance of circumpolar deep water (CDW) and saline shelf water. These changes have global oceanographic and climatic implications. We suggest that the middle Holocene bottom-water record, in the absence of circumpolar deep water on the western Antarctic Peninsula shelf, indicates high saline shelf water production and/or weakened circumpolar deep water production during the middle Holocene climatic optimum. The late Holocene benthic foraminiferal record indicates rapidly fluctuating sea-ice conditions and may indicate a teleconnection between the South Pacific and Southern Ocean, thus having implications related to the Southern Oscillation Index.

Glacial-interglacial sediment record from the North Atlantic

Studies from the subtropical western and eastern Atlantic Ocean, using the 231Pa/230Th ratio as a kinematic proxy for deep water circulation, provided compelling evidence for a strong link between climate and the rate of meridional overturning circulation (MOC) over the last deglaciation. In this study, we present a compilation of existing and new sedimentary 231Pa/230Th records from North Atlantic cores between 1710 and 4550 m water depth. Comparing sedimentary 231Pa/230Th from different depths provides new insights into the evolution of the geometry and rate of deep water formation in the North Atlantic during the last 20,000 years. The 231Pa/230Th ratio measured in upper Holocene sediments indicates slow water renewal above ?2500 m and rapid flushing below, consistent with our understanding of modern circulation. In contrast, during the Last Glacial Maximum (LGM), Glacial North Atlantic Intermediate Water (GNAIW) drove a rapid overturning circulation to a depth of at least ?3000 m depth. Below ~4000 m, water renewal was much slower than today. At the onset of Heinrich event 1, transport by the overturning circulation declined at all depths. GNAIW shoaled above 3000 m and significantly weakened but did not totally shut down. During the Bølling-Allerød (BA) that followed, water renewal rates further decreased above 2000 m but increased below. Our results suggest for the first time that ocean circulation during that period was quite distinct from the modern circulation mode, with a comparatively higher renewal rate above 3000 m and a lower renewal rate below in a pattern similar to the LGM but less accentuated. MOC during the Younger Dryas appears very similar to BA down to 2000 m and slightly slower below.

Swift heavy ion damage to sodium chloride: synergy between excitation and thermal spikes

Systematic data on the effect of irradiation with swift ions (Zn at 735 MeV and Xe at 929 MeV) on NaCl single crystals have been analysed in terms of a synergetic two-spike approach (thermal and excitation spikes). The coupling of the two spikes, simultaneously generated by the irradiation, contributes to the operation of a non-radiative exciton decay model as proposed for purely ionization damage. Using this scheme, we have accounted for the π-emission yield of self-trapped excitons and its temperature dependence under ion-beam irradiation. Moreover, the initial production rates of F-centre growth have also been reasonably simulated for irradiation at low temperatures ( < 100 K), where colour centre annealing and aggregation can be neglected.

Efecto sobre el rendimiento productivo y calidad de la canal de la inclusión de guisantes (Pisum sativum) y alberjón (Vicia narbonensis) en el pienso de lechones y cerdos de cebo

Las leguminosas grano presentan un perfil nutricional de gran interés para alimentación de ganado porcino, debido principalmente a su elevado contenido proteico. Sin embargo, la presencia de factores antinutritivos (FAN), que según el género difieren en calidad y cantidad, condiciona la absorción de la proteína, el nutriente más valorado. El objetivo de esta Tesis Doctoral ha sido el estudio del efecto de los principales FAN de guisante y alberjón sobre el rendimiento productivo, de canal y de piezas nobles, cuando sustituyen a la soja, parcial o totalmente, durante la fase estárter y el periodo de engorde de cerdos grasos. Con este motivo se llevaron a cabo 4 ensayos con machos castrados y la misma línea genética: híbrido Duroc x (Landrace x Large white). En el ensayo 1, se estudió la influencia de distintos niveles de inhibidores de proteasas (IP) en el pienso sobre la productividad de lechones durante la fase estárter (40 a 61 días de edad). Para ello, se utilizaron tres variedades de guisantes de invierno que contenían diferentes cantidades de IP, tanto de tripsina (IT) como de quimotripsina (IQ) [unidades de tripsina inhibida/mg (UTI), unidades de quimotripsina inhibida/mg (UQI): 9,87- 10,16, 5,75-8,62 y 12,55-15,75, para guisantes Cartouche, Iceberg y Luna, respectivamente] más elevadas que en la harina de soja 47 (HnaS) y en la soja extrusionada (SE) (UTI/mg - UQI/mg: 0,61-3,56 y 2,36-4,65, para HnaS y SE, respectivamente). El diseño experimental fue al azar, con cuatro tratamientos dietéticos que diferían en las fuentes proteicas y en la cantidad de IP, enfrentando un pienso control de soja a otros tres piensos con guisantes de invierno de las variedades indicadas, que sustituían parcialmente a la soja. Cada tratamiento se replicó cuatro veces, siendo la celda con 6 lechones la unidad experimental. Los animales que consumieron el pienso con guisante Cartouche tuvieron más ganancia media diaria (GMD) que el resto (P < 0,001) con el mismo consumo medio diario (CMD) e índice de conversión (IC). No hubo diferencias significativas entre los animales del pienso control y los que consumieron piensos con guisantes Iceberg y Luna. En el ensayo 2 la leguminosa objeto de estudio fue el alberjón y su FAN el dipéptido _Glutamyl-S-Ethenyl-Cysteine (GEC). El diseño y el periodo experimental fueron los mismos que en el ensayo 1, con cuatro dietas que variaban en el porcentaje de alberjones: 0%, 5%, 15% y 25%, y de GEC (1,54% del grano). Los lechones que consumieron el pienso con 5% tuvieron un CMD y GMD más elevado (P < 0,001), con el mismo IC que los animales pertenecientes al tratamiento 0%. Los índices productivos empeoraron significativamente y de manera progresiva al aumentar el porcentaje de alberjones (15 y 25%). Se obtuvieron ecuaciones de regresión con estructura polinomial que fueron significativas tanto para el nivel de alberjón como para la cantidad de GEC presente en el pienso. El ensayo 3 se efectuó durante el periodo de engorde, sustituyendo por completo la soja a partir de los 84 días de edad con las tres variedades de guisantes de invierno, observando el efecto sobre el rendimiento productivo, de canal y piezas nobles. El diseño, en bloques completos al azar, tuvo cuatro tratamientos según el guisante presente en el pienso y, por lo tanto, los niveles de IP: Control-soja, Cartouche, Iceberg y Luna, con 12 réplicas de 4 cerdos por tratamiento. De 84 a 108 días de edad los animales que consumieron los piensos Control-soja e Iceberg, tuvieron el mismo CMD y GMD, empeorando en los cerdos alimentados con Luna y Cartouche (P < 0,05). El IC fue igual en los tratamientos Control-soja e Iceberg, ocupando una posición intermedia en Cartouche y peor en los cerdos del pienso Luna (P < 0,001). De 109 a 127 días de edad la GMD y el IC fueron iguales, con un CMD más elevado en Control-soja e Iceberg que en los cerdos que consumieron Cartouche y Luna (P < 0,05). No hubo diferencias significativas durante el acabado (128 a 167 días de edad). Globalmente el CMD y GMD fueron más elevados en los cerdos que comieron los piensos Iceberg y Control-soja, empeorando por igual en los que comieron Cartouche y Luna (P < 0,05); el IC fue el mismo en todos los tratamientos. No se observaron diferencias en los datos relacionados con peso y rendimiento de canal y piezas nobles (jamón, paleta y chuletero), ni del contenido de grasa intramuscular en el lomo y proporción de ácidos grasos principales (C16:0, C18:0, C18:1n-9) en la grasa subcutánea. En el ensayo 4, realizado durante el periodo de engorde (60 a 171 días de edad), se valoró el efecto de dietas con distintos niveles de alberjones, y en consecuencia de su factor antinutritivo el dipéptido GEC, sobre el rendimiento productivo y la calidad de la canal y piezas nobles. El diseño fue en cuatro bloques completos al azar, con cuatro tratamientos según el porcentaje de inclusión de alberjón en el pienso: 0%, 5%, 15% y 25%, con 12 réplicas por tratamiento y cuatro cerdos en cada una de ellas. El tratamiento con 5% mejoró la GMD al final de la fase de cebo (152 días de vida) y, junto con el 0%, presentaron los resultados más favorables de peso e IC al final del ensayo (171 días de vida). Del mismo modo, el peso y rendimiento de canal fueron más elevados en los cerdos alimentados con los tratamientos 0% y 5% (P < 0,001). Piensos con el 15 y 25% de alberjones empeoraron los resultados productivos, así como el rendimiento y peso de canal. Sucedió lo mismo con el peso de las piezas nobles (jamón, paleta y chuletero), significativamente superior en 0% y 5% frente a 15% y 25%, siendo los cerdos que consumieron este último pienso los peores. Por el contrario el rendimiento de jamón y chuletero fue más elevado en los cerdos de los tratamientos 25% y 15% que en los que consumieron los piensos con 5% y 0% (P < 0,001); en el rendimiento de paletas se invirtieron los resultados, siendo mayores en los animales de los tratamientos 0% y 5% (P < 0,001). Se obtuvieron ecuaciones de regresión polinomial, para estimar las cantidades de inclusión de alberjones y de GEC más favorables desde el punto de vista productivo, así como los contrastes ortogonales entre los distintos tratamientos. ABSTRACT The grain legumes have a nutritional profile of great interest to feed pigs, mainly due to high protein content. However, the presence of antinutritional factors (ANF), which differ in quality and quantity according to gender, hinder the absorption of the protein, the most valuable nutrient. The aim of this thesis was to study the effect of the main ANF of pea and narbon vetch (NV) on productive performance, of the carcass and main lean cuts, when replacing soybean, partially or totally, during the starter phase and the fattening period of heavy pigs. For this reason were carried four trials with barrows and the same genetic line: Duroc hybrid x (Landrace x Large white). In trial 1, was studied the influence of different levels of protease inhibitors (PI) in the diet over productivity of piglets during the starter phase (40-61 days of age). For this, were used three varieties of winter peas containing different amounts of PI, both trypsin (TI) and chymotrypsin (CI) [inhibited units/mg trypsin (TIU), inhibited units/mg chymotrypsin (CIU): 9.87 - 10.16, 5.75 - 8.62 and 12.55 - 15.75, for peas Cartouche, Iceberg and Luna, respectively] higher than in soybean meal 47 (SBM) and soybeans extruded (SBE) (TIU/mg - CIU/mg: 0.61 - 3.56 and 2.36 - 4.65 for SBM and SBE, respectively). The design was randomized with four dietary treatments differing in protein sources and the amount of PI, with a control diet of soybean and three with different varieties of winter peas: Cartouche, Iceberg and Luna, which partially replace soybean. Each treatment was replicated four times, being the pen with 6 piglets the experimental unit. Pigs that ate the feed with pea Cartouche had better growth (ADG) than the rest (P < 0.001), with the same average daily feed intake (ADFI) and feed conversion ratio (FCR). There were no significant differences between piglets fed with control diet and those fed Iceberg and Luna diets. In trial 2 the legume under study was the NV and your ANF the dipeptide _Glutamyl FAN-S-Ethenyl-Cysteine (GEC). The experimental period and the design were the same as in trial 1, with four diets with different percentage of NV: 0%, 5%, 15% and 25%, and from GEC (1.52% of the grain). The piglets that consumed the feed containing 5% had higher ADG and ADFI (P < 0.05), with the same FCR that pigs belonging to the 0% treatment. Production rates worsened progressively with increasing percentage of NV (15 and 25%). Were obtained regression equations with polynomial structure that were significant for NV percentage and amount of GEC present in the feed. The test 3 was carried out during the fattening period, completely replace soy from 84 days of age with three varieties of winter peas, observing the effect on the yield, carcass and main lean cuts. The design, randomized complete blocks, had four treatments with different levels of PI: Control-soy, Cartouche, Iceberg and Luna, with 12 replicates of 4 pigs per treatment. From 84 to 108 days of age the pigs fed with Control-soy and Iceberg feed, had the same ADFI and ADG, worsening in pigs fed with Luna and Cartouche (P < 0.05). The FCR was similar in diets Control-soy and Iceberg, occupying an intermediate position in Cartouche and worse in pigs fed with Luna (P < 0.001). From 109-127 days of age the ADG and FCR were equal, with higher ADFI in pigs fed with Control-soy and Iceberg, regarding pigs fed with Cartouche and Luna (P < 0.05). There was no difference in the finishing phase (128-167 days of age). In global period, the ADFI and ADG were higher in pigs that ate Control-soy and Iceberg, and worse in those who ate Cartouche and Luna. The FCR was the same in all treatments. No significant differences were observed in the data related to weight and carcass yield, main lean cuts (ham, shoulder and loin chop) and intramuscular fat loin content and major fatty acids proportion (C16:0, C18:0, C18:1n-9) of subcutaneous fat. In experiment 4, made during the fattening period (60-171 days of age), was assessed the effect of diets with different levels of NV, and consequently of GEC, in the performance and quality of carcass and main lean cuts. There was a completely randomized design with four dietary treatments differing in percentage of NV: 0%, 5%, 15% and 25%, with 12 replicates per treatment and four pigs each. Treatment with 5% improved the ADG at the end of the fattening phase (152 days of age) and, together with 0%, showed the most favorable body weight and FCR at the end of the trial (171 days of age). Similarly, the weight and performance of carcass were higher for pigs fed with diets 0% and 5% (P < 0.05). Diets with 15 and 25% worsened the productive and carcass results. The weight of the main lean cuts (ham, shoulder and loin chop) was significantly higher in 0% and 5% vs 15% and 25%.The diet 25% was the worst of all. By contrast the performance of ham and loin chop was higher in pigs fed with diets 25% and 15%, that those who ate diets with 5% and 0% (P < 0.001); the results of shoulder performance were reversed, being greater in pigs feed with diets 0% and 5% (P < 0.001). Polynomial regression equations were obtained to estimate the percentage of NV and GEC more favorable from the point of view of production, and orthogonal contrasts between treatments.

Investigación sobre la aplicación de energía solar a una depuradora convencional de fangos activos

El consumo de energía es responsable de una parte importante de las emisiones a la atmósfera de CO2, que es uno de los principales causantes del efecto invernadero en nuestro planeta. El aprovechamiento de la energía solar para la producción de agua caliente, permite economizar energía y disminuir el impacto del consumo energético sobre el medio ambiente y por tanto un menor impacto medioambiental. El objetivo de la presente investigación consiste en estudiar el aprovechamiento solar para el calentamiento de los fangos en los digestores anaerobios mediante agua caliente circulando en el interior de un serpentín que rodea la superficie de dicho digestor, como apoyo a los métodos convencionales del calentamiento de fangos como la resistencia eléctrica o el intercambiador de calor mediante la energía obtenida por el gas metano producido en la digestión anaerobia. Para el estudio se utilizaron 3 digestores, dos delos cuales se calentaron con agua caliente en el interior de un serpentín (uno aislado mediante una capa de fibra de vidrio y poliuretano y otro sin aislar).El tercer digestor no tenía calentamiento exterior con el objetivo de observar su comportamiento y comparar su evolución con el resto de los digestores .La comparación de los digestores 1 y 2 nos permitió estudiar la conveniencia de proveer de aislamiento al digestor. La transferencia de calor mediante serpentín de cobre dio valores comprendidos entre 83 y 92%. La aplicación de la instalación a una depuradora a escala real para mantenimiento en el interior del digestor a T=32ºC en diferentes climas: climas templados, cálidos y fríos, consistió en el cálculo de la superficie de colectores solares y superficie de serpentín necesario para cubrir las necesidades energéticas anuales de dicho digestor, así como el estudio de rentabilidad de la instalación, dando los mejores resultados para climas cálidos con períodos de retorno de 12 años y una tasa interna de rentabilidad (TIR) del 16% obteniendo una cobertura anual del 79% de las necesidades energéticas con energía solar térmica. Energy consumption accounts for a significant part of the emissions of CO2, which is one of the main causes of the greenhouse effect on our planet. The use of solar energy for hot water production. can save energy and reduce the impact of energy consumption on the environment and therefore a reduced environmental impact. The objective of this research is to study the solar utilization for heating the sludge in anaerobic digesters by hot water circulating inside a coil surrounding the surface of digester, to support conventional heating methods sludge as the electrical resistance or heat exchanger by energy generated by the methane gas produced in the anaerobic digestion. To study 3 digesters used two models which are heated with hot water within a coil (one insulated by a layer of fiberglass and polyurethane and other uninsulated) .The third digester had no external heating in order to observe their behavior and compare their evolution with the rest of the .The comparison digesters digesters 1 and 2 allowed us to study the advisability of providing insulation to the digester. Heat transfer through copper coil gave values between 83 and 92%. The installation application to a treatment for maintaining full scale within the digester at T = 32ºC in different climates: temperate, warm and cold climates, consisted of calculating the surface area of solar collectors and coil required to cover the annual energy needs of the digester, and the study of profitability of the installation, giving the best results for hot climates with return periods of 12 years and an internal rate of return (IRR) of 16% achieving an annual coverage of 79 % of energy needs with solar energy.

Paleoclimate and Amerindians: Evidence from stable isotopes and atmospheric circulation

Two Amerindian demographic shifts are attributed to climate change in the northwest plains of North America: at ≈11,000 calendar years before present (yr BP), Amerindian culture apparently split into foothills–mountains vs. plains biomes; and from 8,000–5,000 yr BP, scarce archaeological sites on the open plains suggest emigration during xeric “Altithermal” conditions. We reconstructed paleoclimates from stable isotopes in prehistoric bison bone and relations between weather and fractions of C4 plants in forage. Further, we developed a climate-change model that synthesized stable isotope, existing qualitative evidence (e.g., palynological, erosional), and global climate mechanisms affecting this midlatitude region. Our isotope data indicate significant warming from ≈12,400 to 11,900 yr BP, supporting climate-driven cultural separation. However, isotope evidence of apparently wet, warm conditions at 7,300 yr BP refutes emigration to avoid xeric conditions. Scarcity of archaeological sites is best explained by rapid climate fluctuations after catastrophic draining of the Laurentide Lakes, which disrupted North Atlantic Deep Water production and subsequently altered monsoonal inputs to the open plains.

Investigação de aquífero fraturado para entendimento de fluxo e transporte de contaminantes clorados: estudo de caso em Valinhos, SP

Casos de contaminação de aquíferos fraturados são bastante complexos, tendo em vista a heterogeneidade das redes de fraturas, e no geral, sua investigação demanda a utilização de técnicas pouco usuais, como por exemplo o imageamento acústico e a perfilagem de velocidade de fluxo de água. Na área de estudo, localizada em Valinhos/SP, o uso inadequado de solventes organoclorados no passado ocasionou a contaminação do aquífero raso em duas áreas, e o aparecimento de concentrações no aquifero profundo levaram a condução do atual trabalho, que teve como principal objetivo a elaboração de um modelo conceitual de fluxo de água e transporte de contaminantes no aquífero cristalino. Previamente à investigação do aquífero fraturado, foi realizada uma análise de trabalhos existentes, incluindo a interpretação de lineamentos, levantamentos geológicos além de perfilagens geofísicas de superfície. Em cada área investigada, foi realizada a perfuração de um poço profundo e aplicadas as técnicas de perfilagens de raios gama, cáliper, flowmeter, imageamento acústico, além da filmagem do poço e realização de ensaios hidráulicos nos dois pontos perfurados. Para caracterização química do aquífero fraturado, foram realizadas coletas de água subterrânea em intervalos selecionados com a utilização de obturadores pneumáticos. As cargas hidráulicas medidas durante a amostragem também auxiliaram no entendimento da direção do fluxo de água. O aquífero cristalino é formado por rochas gnáissicas e se encontra bastante fraturado e intemperizado, principalmente na porção superficial da rocha (até aproximadamente 65,0 m) onde as maiores velocidades de fluxo de água também foram observadas. A rocha sã possui uma menor densidade de fraturas e predominância de minerais mais claros. As fraturas de baixo a médio angulo de mergulho (Grupo 1) são as mais frequentes em ambas as perfurações e possuem direção principal N-S a NE-SW. São observadas, no geral, exercendo grande influência sobre o fluxo de água, principalmente na porção alterada do gnaisse. Fraturas com ângulo elevado de mergulho, classificadas como Grupo 2 (paralelas à foliação) e Grupo 3 (direção NW à W), são também observadas ao longo de toda a perfuração estabelecendo a conexão hidráulica entre as fraturas do Grupo 1. Em menor proporção, são ainda verificadas fraturas com ângulos de mergulho >40 ° pertencente aos Grupos 4 (NE-SW), 5 (E-W), 6 (NW-SE) e 7 (E-W). O fluxo de água subterrânea se mostrou descendente na porção superior da rocha alterada e ascendente na porção mais profunda, possivelmente direcionando a água subterrânea para a região de transição da rocha mais alterada para a rocha sã (entre 61 a 65 m de profundidade). Apesar do fluxo ascendente em profundidade, o bombeamento de poços tubulares existentes no entorno ao longo dos anos, favoreceu a migração dos contaminantes para porções mais profundas. Os contaminantes observados no poço tubular P6 possuem maior semelhança com os contaminantes observados na Área 2, e ambos estão localizados entre lineamentos NW-SE, indicando uma possível influência dos lineamentos no controle sobre o fluxo de água. No entanto, para entendimento do transporte dos contaminantes em área, é necessário um adensamento da rede de monitoramento, levando em consideração a heterogeneidade do meio e as incertezas relacionadas à extrapolação dos dados para áreas não investigadas.

Optimal Design of a Hybrid Membrane System Combining Reverse and Forward Osmosis for Seawater Desalination

In this work we study Forward Osmosis (FO) as an emerging desalination technology, and its capability to replace totally or partially Reverse Osmosis (RO) in order to reduce the great amount of energy required in the current desalination plants. For this purpose, we propose a superstructure that includes both membrane based desalination technologies, allowing the selection of only one of the technologies or a combination of both of them seeking for the optimal configuration of the network. The optimization problem is solved for a seawater desalination plant with a given fresh water production. The results obtained show that the optimal solution combines both desalination technologies to reduce not only the energy consumption but also the total cost of the desalination process in comparison with the same plant but operating only with RO.

Bulk sediment parameter of surface sediment samples (Table 3)

Comparison of rates of accumulation of organic carbon in surface marine sediments from the central North Pacific, the continental margins off northwest Africa, northwest and southwest America, the Argentine Basin, and the western Baltic Sea with primary production rates suggests that the fraction of primary produced organic carbon preserved in the sediments is universally related to the bulk sedimentation rate. Accordingly, less than 0.01% of the primary production becomes fossilized in slowly accumulating pelagic sediments [(2 to 6 mm (1000 y)**-1] of the Central Pacific, 0.1 to 2% in moderately rapidly accumulating [2 to 13 cm (1000 y)**-1] hemipelagic sediments off northwest Africa, northwest America (Oregon) and southeast America (Argentina), and 11 to 18% in rapidly accumulating [66 to 140 cm (1000 y)**-1] hemipelagic sediments off southwest America (Peru) and in the Baltic Sea. The emiprical expression: %Org-C = (0.0030*R*S**0.30)/(ps(1-Theta)) implies that the sedimentary organic carbon content (% Org-C) doubles with each 10-fold increase in sedimentation rate (S), assuming that other factors remain constant; i.e., primary production (R), porosity and sediment density (ps). This expression also predicts the sedimentary organic carbon content from the primary production rate, sedimentation rate, dry density of solids, and their porosity; it may be used to estimate paleoproductivity as well. Applying this relationship to a sediment core from the continental rise off northwest Africa (Spanish Sahara) suggests that productivity there during interglacial oxygen isotope stages 1 and 5 was about the same as today but was higher by a factor of 2 to 3 during glacial stages 2, 3, and 6.

Age determination and stable isotope record of sediment core MR06-04_PC23A

Millennial-scale variability in the behavior of North Pacific Intermediate Water during the last glacial and deglacial period, and its association with Dansgaard-Oeschger (D-O) cycles and Heinrich events, are examined based on benthic foraminiferal oxygen and carbon isotopes (d18Obf and d13Cbf) and %CaCO3 using a sediment core recovered from the northeastern slope of the Bering Sea. A suite of positive d18Obf excursions at intermediate depths of the Bering Sea, which seem at least in part associated with increases in the d18Obf gradients between the Bering and Okhotsk Seas, suggest the Bering Sea as a proximate source of intermediate water during several severe stadial episodes in the last glacial and deglacial period. Absence of such d18Obf gradients during periods of high surface productivity in the Bering and Okhotsk Seas, which we correlate to D-O interstadials, suggests a reduction in intermediate water production in the Bering Sea and subsequent introduction of nutrient-rich deep waters from the North Pacific into intermediate depths of the Bering Sea. We argue that a reorganization of atmospheric circulation in the high-latitude North Pacific during severe cold episodes in the last glacial and deglacial period created favorable conditions for brine rejection in the northeastern Bering Sea. The resulting salinity increase in the cold surface waters could have initiated intermediate (and deep) water formation that spread out to the North Pacific.