Physical properties, mineral and chemical compositions, and accumulation rates of Holocene and Upper Pleistocene bottom sediments from the Sea of Okhotsk

Mineral and chemical compositions and physical properties of diatomaceous clayey-siliceous sediments from the Sea of Okhotsk are studied. Accumulation rates of silica are determined. Their compositional model based on silica content is similar to that of Late Jurassic and Olenekian-Middle Anisian cherts from the Sikhote Alin region. Thickness of Holocene siliceous unit and accumulation rates of siliceous deposits depended on bioproductivity in the upper water layer and seafloor topography. Accumulation rates of amorphous SiO2 (0.05-5.7 g/cm**2/ka) and free SiO2 (0.5-11.6 g/cm**2/ka) are minimal on seamounts and maximal in depressions near foothills. These values match accumulation rates of free SiO2 in Triassic and Late Jurassic basins of the Sikhote Alin region (0.33-3 g/cm**2/ka). Comparison of composition and accumulation rates of silica shows that Triassic and Late Jurassic siliceous sequences of Sikhote Alin could accumulate in a marginal marine basin near a continent.

Environmental characteristics, and growth traits and leaf chemistry of tundra plants in a warming experiment at Alexandra Fiord

Understanding plant trait responses to elevated temperatures in the Arctic is critical in light of recent and continuing climate change, especially because these traits act as key mechanisms in climate-vegetation feedbacks. Since 1992, we have artificially warmed three plant communities at Alexandra Fiord, Nunavut, Canada (79°N). In each of the communities, we used open-top chambers (OTCs) to passively warm vegetation by 1-2 °C. In the summer of 2008, we investigated the intraspecific trait responses of five key species to 16 years of continuous warming. We examined eight traits that quantify different aspects of plant performance: leaf size, specific leaf area (SLA), leaf dry matter content (LDMC), plant height, leaf carbon concentration, leaf nitrogen concentration, leaf carbon isotope discrimination (LCID), and leaf d15N. Long-term artificial warming affected five traits, including at least one trait in every species studied. The evergreen shrub Cassiope tetragona responded most frequently (increased leaf size and plant height/decreased SLA, leaf carbon concentration, and LCID), followed by the deciduous shrub Salix arctica (increased leaf size and plant height/decreased SLA) and the evergreen shrub Dryas integrifolia (increased leaf size and plant height/decreased LCID), the forb Oxyria digyna (increased leaf size and plant height), and the sedge Eriophorum angustifolium spp. triste (decreased leaf carbon concentration). Warming did not affect d15N, leaf nitrogen concentration, or LDMC. Overall, growth traits were more sensitive to warming than leaf chemistry traits. Notably, we found that responses to warming were sustained, even after many years of treatment. Our work suggests that tundra plants in the High Arctic will show a multifaceted response to warming, often including taller shoots with larger leaves.

Low-molecular-weight hydrocarbons in sediments of Broken Ridge and Ninetyeast Ridge

Core samples taken during Leg 121 drilling aboard the JOIDES Resolution in the central Indian Ocean were analyzed for their low-molecular-weight hydrocarbon contents. Forty-three samples from the Broken Ridge and 39 samples from the Ninetyeast Ridge drill sites, deep-frozen on board immediately after recovery, were studied by a dynamic headspace technique (hydrogen-stripping/thermovaporization). Light hydrocarbons (saturated and olefinic) with two to four carbon atoms, and toluene as a selected aromatic compound, were identified. Total C2-C4 saturated hydrocarbon yields vary considerably from virtually zero in a Paleogene calcareous ooze from Hole 757B to nearly 600 nanogram/gram of dry-weight sediment (parts per billion) in a Cretaceous claystone from Hole 758A. An increase of light-hydrocarbon yields with depth, and hence with sediment temperature, was observed from Hole 758A samples down to a depth of about 500 meters below seafloor. Despite extreme data scatter due to lithological changes over this depth interval, this increased yield indicates the onset of temperature-controlled hydrocarbon formation reactions. Toluene contents are also extremely variable (generally between 10 and 100 ppb) and reach more than 300 ppb in two samples of tuffaceous lithology (Sections 121-755A-17R-4 and 121-758A-48R-4). As for the saturated hydrocarbons, there was also an increase of toluene yields with increasing depth in Hole 758A.

Seawater carbonate chemistry and biological processes of Mytilus edulis during experiments, 2010

Marine organisms are exposed to increasingly acidic oceans, as a result of equilibration of surface ocean water with rising atmospheric CO2 concentrations. In this study, we examined the physiological response of Mytilus edulis from the Baltic Sea, grown for 2 months at 4 seawater pCO2 levels (39, 113, 243 and 405 Pa/385, 1,120, 2,400 and 4,000 µatm). Shell and somatic growth, calcification, oxygen consumption and excretion rates were measured in order to test the hypothesis whether exposure to elevated seawater pCO2 is causally related to metabolic depression. During the experimental period, mussel shell mass and shell-free dry mass (SFDM) increased at least by a factor of two and three, respectively. However, shell length and shell mass growth decreased linearly with increasing pCO2 by 6-20 and 10-34%, while SFDM growth was not significantly affected by hypercapnia. We observed a parabolic change in routine metabolic rates with increasing pCO2 and the highest rates (+60%) at 243 Pa. excretion rose linearly with increasing pCO2. Decreased O:N ratios at the highest seawater pCO2 indicate enhanced protein metabolism which may contribute to intracellular pH regulation. We suggest that reduced shell growth under severe acidification is not caused by (global) metabolic depression but is potentially due to synergistic effects of increased cellular energy demand and nitrogen loss.

Chemical composition of organic matter in ocean sediments

Group composition of organic matter in recent ocean sediments with high Corg content has been studied in detail. It has been shown that organic matter in sediments with Corg content greater than 4% is present in the very earliest stages of transformation. Group composition of amino acids is practically similar to that of their main producer, namely phytoplankton. Organic matter of sediments with Corg content below 4% is, from this standpoint, more transformed and is close to organic matter in usual type sediments with similar Corg content.

Respuesta fisiológica y agronómica del olivar en seto (cv. Arbequina) a la orientación de filas y al ancho de calle: relación entre la producción y calidad del aceite y la radiación interceptada

En las últimas dos décadas, los productores han plantado olivares en seto para lograr la mecanización de la poda y en especial de la cosecha, reducir los costes de mano de obra y permitir intervenciones de manejo rápidas y oportunas. Los olivares se desarrollaron en ausencia del conocimiento científico, sobre el diseño óptimo de la estructura de la copa, necesario para incrementar la producción y calidad del aceite. En contraste, con los árboles muy espaciados y distribuidos uniformemente de las plantaciones tradicionales, en el olivar en seto hay una marcada variabilidad espacial y temporal de la radiación disponible en función del diseño de la plantación. Así, conocer la respuesta fisiológica y productiva del olivo a la radiación resulta fundamental en el olivar en seto. La orientación de las filas y el ancho de calle son aspectos que se deciden en el diseño de las plantaciones en seto. Ambos aspectos modifican la radiación interceptada por la canopia y, por lo tanto, pueden incidir en la productividad y calidad del aceite. Una vez realizada la plantación no pueden ser modificados, y así las ventajas o desventajas permanecerán fijas durante toda la vida productiva del olivar. A pesar de esto, el impacto de la orientación de las filas y el ancho de calle han recibido poca atención en olivos y en la mayoría de los frutales conducidos en seto. Por todo ello, los objetivos principales de esta tesis fueron, (i) evaluar el efecto de la orientación del seto y del ancho de calle, sobre la productividad y calidad del aceite, (ii) evaluar un modelo que estime la radiación dentro de la canopia. Este modelo permitirá cuantificar las relaciones entre la radiación y los componentes del rendimiento y calidad del aceite de olivares en setos con un amplio rango de estructuras y (iii) conocer la variabilidad en las características de las hojas (morfológicas y fisiológicas) y de los tejidos del fruto (tamaño y composición) en diferentes posiciones de la copa de los setos. Para ello, se dispuso de 3 ensayos de olivar en seto (cv. Arbequina) implantados en 2008 en el municipio de La Puebla de Montalbán, Toledo. La primera cosecha fue en 2010 y a partir del 2012 los setos formaron una copa continua. A partir de ese año, los setos se mantuvieron mediante poda, con similar ancho (~1 m) y altura (~2,5 m), acordes a las dimensiones de la cosechadora vendimiadora. En los años 2012 y 2013 se estudió en profundidad la respuesta de las plantas de estos ensayos. En el ensayo 1, los setos fueron plantados con cuatro orientaciones de filas: N–S, NE–SO, NO–SE y E–O y el mismo ancho de calle (4 m). En los otros dos ensayos, los setos fueron plantados con tres anchos de calle (5,0, 4,0 y 2,5 m), y con filas orientadas N–S (ensayo 2) y E–O (ensayo 3). La respuesta de la orientación de las filas se evaluó a nivel de seto y de estratos del seto (alturas y caras), a través de mediciones del crecimiento de brotes, componentes reproductivos, características y temperatura del fruto, estado hídrico del suelo y de las plantas, fotosíntesis neta de las hojas y contenido de ácidos grasos. Los setos orientados NE–SO (2,7 t/ha) lograron la mayor producción de aceite, que fue significativamente más alta que la de los setos E–O (2,3 t/ha). La producción de aceite de los setos E–O no se diferenció estadísticamente de los setos N–S (2,5 t/ha). Las diferencias productivas entre orientaciones fueron explicadas por el número de frutos en cosecha, a su vez la variación en el número de frutos estuvo asociada al efecto de la orientación de las filas sobre el número de yemas desarrolladas y el porcentaje de inflorescencias fértiles. Las hojas en las caras iluminadas de los setos NE–SO y N–S presentaron mayor tasa fotosintética a la mañana (~10.0 h) que los setos E–O, en el año 2012, pero no en 2013. La orientación de las filas no tuvo un efecto significativo en el contenido de ácidos grasos de los aceites extraídos, esto ocurrió a pesar de variaciones en la temperatura interna de los frutos (3 °C) y de la radiación (40%) entre las distintas caras de los setos. La orientación del seto afectó significativamente al contenido relativo de agua del suelo, donde setos E–O presentaron valores más altos (12%) que setos N–S durante el verano y otoño. Sin embargo, el potencial hídrico de tallo fue similar entre orientaciones. En los ensayos 2 y 3, se evaluó el efecto que produce, a nivel de seto y de estratos (caras y alturas), reducir el ancho de calle de 5,0 a 4,0 y 2,5 m, en un seto orientado N–S y otro E–O, respectivamente. La relación entre altura/ancho de calle libre aumentó 0,6 a 0,8 y 1,6, al reducir 5,0, 4,0 y 2,5 m el ancho de calle, mientras la longitud de seto y el volumen de copa por hectárea incrementó 100% al reducir de 5,0 a 2,5 m, el ancho de calle. En los setos orientados N–S, la producción de aceite por ha acumulada en 4 campañas, incrementó significativamente un 52 %, al reducir de 5,0 a 2,5 m el ancho de calle. Los setos N–S con calle más estrecha (2,5 m) tuvieron un 19% menos frutos que los setos con calle más ancha (5,0 m) y a su vez el 60% de los mismos se localizaron los estratos altos de la canopia de los setos con calles estrecha en comparación al 40% en setos con calle de 5,0 m. En los estratos más bajos de los setos con calles de 2,5m hubo menor crecimiento de los brotes y los frutos tuvieron menor peso seco, contenido de aceite y madurez, que los frutos en los estratos bajos de los setos a 5,0 m. Los componentes del rendimiento y características de los frutos (agua y madurez) fueron similares entre la caras E y O, independientemente del ancho de calle. En los setos orientados E–O, la producción de aceite por ha acumulada en 4 campañas, no respondió significativamente al ancho de calle, debido a una disminución significativa en el número de frutos y producción de aceite por m de seto, al reducir de 5,0 a 2,5 m, el ancho de calle. En los setos orientados E–O, con calles de 5,0 m, los frutos presentaron similar peso seco, contenido de aceite y agua, en las caras S y N, sin embargo, cuando la calle fue reducida a 2,5, los frutos de la cara S fueron más pesado y maduros que en la cara N. Independientemente del ancho de calle y de la orientación del seto, el aceite presentó mayor contenido de ácidos palmitoleico, palmítico, esteárico y linoleico en los frutos del estrato más alto de la canopia disminuyendo hacia la base. En contraste, el contenido de ácido oleico aumentó desde el estrato más alto hacia la base de los setos. Las diferencias en el contenido de ácidos grasos entre la parte alta y baja de los setos, incrementó al reducir el ancho de calle en los setos N–S, pero no en los E-O. En conclusión, en olivares en seto, reducir el ancho de calle permite incrementar la producción de aceite, en setos orientados N–S, pero no en E–O. Un modelo que estima la cantidad y distribución de la radiación en toda la copa del seto, fue utilizado para estimar la radiación interceptada en distintos estratos del seto. El modelo requiere un valor del coeficiente de extinción (k) para estimar la transmisión de radiación a través de la copa, el cual fue obtenido experimentalmente (k=1,2). Utilizando los datos del ensayo 1, un único modelo lineal relacionó el peso seco y el rendimiento graso de setos con la radiación interceptada por los distintos estratos de setos con cuatro orientaciones de filas. La densidad de frutos fue también relacionada con la radiación, pero más débilmente. En los setos orientados N–S, plantados con tres anchos de calles, (ensayo 2) el contenido de ácidos palmitoleico y linoleico del aceite incrementó linealmente con el incremento de la radiación interceptada, mientras el contenido ácido oleico disminuyó linealmente con el incremento de la radiación. El contenido de ácidos grasos del aceite no estuvo relacionado con la radiación interceptada en setos orientados E–O (Ensayo 3). En los setos N–S y E–O, plantados con anchos de calle de 2,5 m, se estudiaron las interacciones entre la radiación y características de las hojas, número de fruto, tamaño y composición de los frutos a nivel de órgano, tejido y células. Independientemente de la orientación del seto, el área y el contenido de clorofila de las hojas incrementaron significativamente en los estratos más bajos de los setos. Mientras, las hojas de los estratos medios del seto presentaron mayor capacidad fotosintética que en los estratos bajos y alto de los setos. Los estratos del seto que interceptaron más radiación produjeron frutos con mayor tamaño y contenido de aceite en el mesocarpo, sin efectos sobre el tamaño y composición del endocarpo. A nivel celular, los frutos expuestos a mayor nivel de radiación desarrollaron en el mesocarpo células de mayor tamaño en comparación a frutos menos expuestos, mientras el número de células no fue afectado. Adicionalmente, el número y tamaño de las células estuvo relacionado con la composición del mesocarpo en términos de aceite, agua y peso seco menos aceite. Esta tesis, contribuye, desde una perspectiva integral del cultivo del olivo, a cuantificar el impacto de la orientación y ancho de calle sobre la producción y calidad del aceite en olivares conducidos en setos. El análisis y discusión de la relación entre la radiación y los componentes del rendimiento y calidad del aceite, puede ayudar a diseñar plantaciones en seto con dimensiones óptimas para la intercepción de la radiación. ABSTRACT In the last two decades, olive hedgerow system has been established by commercial growers to allow continuous mechanized pruning and especially harvest, reduce costs of manual labour and allow more rapid and timely management interventions. The adoption of hedgerow was done in the absence of adequate scientific knowledge of the impact of this orchard structure and associated mechanization on tree response, yield and quality, after centuries in low-density orchards and open-formed trees. The row orientation and width alley are fundamental aspects in the hedgerow design and have been scarcely studied in olive. Both aspects modify the radiation intercepted by the canopy, and consequently the productivity and oil quality, and once defined in orchard planting cannot be changed, so advantages and disadvantages remain fixed for the lifespan of the orchard. The main objectives of this thesis were to (i) evaluate the impact of the row orientation and width alley on productivity and oil quality by the measurements of profile of the determining processes of shoot growth, fruit temperature, yield components and fruit and oil characteristics on opposite sides of olive hedgerows. Additionally, the effect of row orientation on the plant water status was also evaluated; (ii) evaluate a mathematical model for estimating the radiation within the canopy and quantify the relationships between the radiation estimated and yield components and oil quality in olive hedgerows under wide range of structures and; (iii) determine the variability in the characteristics of the leaves (morphological and physiological) and fruit tissues (size and composition) in different positions of the hedgerows canopy. Three plots of olive hedgerows (cv. Arbequina) planted in 2008 in La Puebla de Montalbán, Toledo were evaluated during the 2012 and 2013 seasons. The hedgerows were maintained by lateral pruning and topping with the same width (1 m) and height (2.5 m) compatible with the intended harvester. In a plot (experiment 1), the hedgerows were planted with the same width alley (4 m) and four row orientations: N–S, NE–SW, NW–SE and E–W. Other two plots (Experiments 2 and 3) separated by approximately 100 m were planted with N–S and E–O oriented rows and three alley widths in each orientation: 5.0, 4.0 and 2.5 m. In the exp. 1, maximum fruit yield were achieved by NE–SW and NW–SW (15.7 t/ha). Of these, NE–SW achieved the highest oil yield (2.7 t/ha). There were no differences in fruit or oil yield between N–S (2.5 t oil/ha) and E–W (2.3 t oil/ha) orientations. Fruit number was the most important component to explain these differences, by previous influence on number of bud developed and percentage of fertile inflorescences. Fruit maturity and oil quality on both sides of the hedgerows were not affected by row orientation. This occurred despite significant variations in the internal fruit temperature, which was closely related to the irradiance received by the canopy and the time of day. Additionally, row orientation significantly affected the relative water content of the soil, where E–W oriented hedgerows showed consistently higher values than N–S during summer-autumn season. The stem water potential at midday, however, was similar between orientations, revealing possible lower water consumption of E–W than N–S oriented hedgerows. In the exp. 2, regardless of row orientation, reduction of row spacing from 5.0 to 4.0 and 2.5 m increases the ratio of canopy depth to free alley width (Al/An) from 0.6 to 0.8 and 1.6, respectively, and ads 25 and 100 % more hedgerow length per ha. In N–S oriented hedgerows, oil production per ha increased significantly by 14 and 52 % in 4.0 m and 2.5 m relative to 5.0 m row spacing, the effect being proportionally less than the increase in hedgerow length per ha. Hedgerows spaced 2.5 m with Al/An = 1.6 produced relatively fewer fruits per unit length than did wider spacings and were preferentially distributed in upper layers. Fruits located at the bottom of the canopy were smaller, with lower oil content and were less mature. In E–W oriented hedgerows, oil production per ha did not respond significantly to row spacing, despite the doubling of row length from the 5.0 to the 2.5 m row spacing. The explanation was found in fewer fruit per unit length of hedgerow and smaller oil content at 2.5 m than 5.0 m row spacing, averaged over the experimental period. In E–W hedgerows spaced at 5.0 m with Al/An = 0.6, the vertical profiles of fruit characteristics (mass, oil and water contents, and maturity) were similar between opposing sides, but at 4.0 m (Al/An= 0.8) and 2.5 m (Al/An=1.6) spacings, fruits on the S side were heavier and more mature than on N side. The oil extracted from fruits harvested at different heights of N–S and E–W oriented hedgerows showed higher palmitoleic, palmitic, stearic and linoleic contents at the canopy top decreasing toward base. The oleic content was reverse, increased from top to base. In N–S hedgerows, vertical gradients increased by reducing the alley width, but not in the E–W oriented hedgerows. The simulation of internal canopy irradiance was related in a single relationship (R2 = 0.63) to the vertical profiles of fruit weight and oil content of olive hedgerows with wide range of structures. The density of fruits was also associated with the irradiance but more weakly (R2 = 0.27), and revealed a more complex response involving changes in the vegetative structure by canopy management (topping) and the effect of radiation on the previous sequence that defines the number of fruits. The vertical profiles of oil quality traits were closely associated to canopy irradiance, but only when the N–S oriented hedgerows were considered. The contents of palmitoleic and linoleic acid in the oil increased linearly when intercepted irradiance increased from 9 to 19 mol PAR/m2. In contrast, oleic content decreased linearly in this irradiance range. Additionally, we advanced knowledge regarding the interactions among irradiance and leaf, fruit number, size and composition at organ-, tissue- and cellular- levels. The irradiance received at different positions in the canopy strongly affected the leaf area and chlorophyll content, and mesocarp size and composition (water and oil), without effects on endocarp size and composition. At the cellular level, light-exposed fruit developed larger mesocarp cells than shaded fruits, but cell number was not affected. Our results indicate that cell number and size are related to mesocarp composition in term of oil, water, and dry weight menus oil, although the specific manner in which they interact remains to be determined. This research contributes from an integral perspective of olive growing to quantify the impact of row orientation and width alley on productivity and oil quality in hedgerows systems. The analysis and discussion of the relationships between radiation and yield components and oil quality can help understand the impact of design olive hedgerows in general and in a wide range of environmental conditions.

(Table 2) Ice rafted debris abundance and accumulation rate, sedimentation rate and dry bulk density of bottom sediments from the Sea of Okhotsk

Oxygen isotope records, radiocarbon AMS data, carbonate and opal stratigraphy, sediment magnetic susceptibility, tephrachronology, and paleontological results were used to obtain detailed sediment stratigraphy and an age model for the studied cores. For studying sea-ice sedimentation an analysis of lithogenic grain number in >0.15 mm grain size fraction of bottom sediments was carried out. For quantitative estimation of intensity ice-rafting debris sedimentation number of IRD particles per sq cm per ka was calculated. Obtained results allowed to plot IRD AR distribution for the first oxygen isotope stage (0-12.5 14C ka, 14C) and for the second stage (12.5-24 14C ka). The first stage was subdivided into the latest deglaciation and the beginning of Holocene (6-12.5 14C ka) (transitive period), when the sea level was changing significantly, and the second part of Holocene (0-6 14C ka), when climate conditions and the sea level were similar to modern estimates. Data clearly show strong increase in ice formation in the glacial Sea of Okhotsk and its extent in the middle part of the sea. Average annual duration of ice coverage during glaciation was longer than that for interglaciation. However the sea ice cover was not continuous all the year round and disappeared in summer time except the far northwestern part of the sea.

Effect of the temperature on the composition of lignin pyrolysis products

The temperature dependence of the pyrolysis products of two types of lignin (Alcell lignin and Asian lignin) was investigated using pyrolysis-gas chromatography-mass spectrometry (PyGC-MS). About 50 compounds were identified and quantified for each type of lignin over a temperature range of 400-800C. The maximum yield of phenolic compounds was obtained at 600C for both lignins, which was 17.2% for Alcell lignin and 15.5% for Asian lignin. Most of the phenolic compounds had an individual yield of less than 1%; however, for Alcell lignin, 5-hydroxyvanillin was the highest yield at 4.29 wt%on dry ash-free lignin, and for Asian lignin, 2-methoxy-4-vinylphenol was the highest yield at 4.15 wt % on dry ash-free lignin.

Biogeochemical effects of iron availability on primary producers in a shallow marine carbonate environment

We completed a synoptic survey of iron, phosphorus, and sulfur concentrations in shallow marine carbonate sediments from south Florida. Total extracted iron concentrations typically were 50 μmol g-1 dry weight (DW) and tended to decrease away from the Florida mainland, whereas total extracted phosphorus concentrations mostly were 10 μmol g-1 DW and tended to decrease from west to east across Florida Bay. Concentrations of reduced sulfur compounds, up to 40 μmol g-1 DW, tended to covary with sediment iron concentrations, suggesting that sulfide mineral formation was iron-limited. An index of iron availability derived from sediment data was negatively correlated with chlorophyll a concentrations in surface waters, demonstrating the close coupling of sediment-water column processes. Eight months after applying a surface layer of iron oxide granules to experimental plots, sediment iron, phosphorus, and sulfur were elevated to a depth of 10 cm relative to control plots. Biomass of the seagrass Thalassia testudinum was not different between control and iron addition plots, but individual shoot growth rates were significantly higher in experimental plots after 8 months. Although the iron content of leaf tissues was significantly higher from iron addition plots, no difference in phosphorus content of T. testudinum leaves was observed. Iron addition altered plant exposure to free sulfide, documented by a significantly higher δ34S of leaf tissue from experimental plots relative to controls. Iron as a buffer to toxic sulfides may promote individual shoot growth, but phosphorus availability to plants still appears to limit production in carbonate sediments.

He isotope, U/Th isotope, Calcium carbonate, biogenic opal, rare earth element concentrations, and grain size distribution measured on core-top sediments during SONNE cruise SO202 (INOPEX)

Eolian dust is a significant source of iron and other nutrients that are essential for the health of marine ecosystems and potentially a controlling factor of the high nutrient-low chlorophyll status of the Subarctic North Pacific. We map the spatial distribution of dust input using three different geochemical tracers of eolian dust, 4He, 232Th and rare earth elements, in combination with grain size distribution data, from a set of core-top sediments covering the entire Subarctic North Pacific. Using the suite of geochemical proxies to fingerprint different lithogenic components, we deconvolve eolian dust input from other lithogenic inputs such as volcanic ash, ice-rafted debris, riverine and hemipelagic input. While the open ocean sites far away from the volcanic arcs are dominantly composed of pure eolian dust, lithogenic components other than eolian dust play a more crucial role along the arcs. In sites dominated by dust, eolian dust input appears to be characterized by a nearly uniform grain size mode at ~4 µm. Applying the 230Th-normalization technique, our proxies yield a consistent pattern of uniform dust fluxes of 1-2 g/m**2/yr across the Subarctic North Pacific. Elevated eolian dust fluxes of 2-4 g/m**2/yr characterize the westernmost region off Japan and the southern Kurile Islands south of 45° N and west of 165° E along the main pathway of the westerly winds. The core-top based dust flux reconstruction is consistent with recent estimates based on dissolved thorium isotope concentrations in seawater from the Subarctic North Pacific. The dust flux pattern compares well with state-of-the-art dust model predictions in the western and central Subarctic North Pacific, but we find that dust fluxes are higher than modeled fluxes by 0.5-1 g/m**2/yr in the northwest, northeast and eastern Subarctic North Pacific. Our results provide an important benchmark for biogeochemical models and a robust approach for downcore studies testing dust-induced iron fertilization of past changes in biological productivity in the Subarctic North Pacific.

(Table 1) Low molecular weight hydrocarbon concentrations and organic carbon contents at DSDP Hole 71-511

C2-C8 hydrocarbons (36 compounds identified) from 56 shipboard sealed, deep-frozen core samples of DSDP Leg 71, Site 511, Falkland Plateau, South Atlantic, were analyzed by a combined hydrogen stripping-thermovaporization method. Concentrations, which represent hydrocarbons dissolved in the pore water and adsorbed to the mineral surfaces of the sediment, vary from 24 ng/g of dry weight sediment in Lithologic Unit 4 to 17,400 ng/g in Lithologic Unit 6 ("black shale" unit). Likewise, the organic carbon normalized C2-C8 hydrocarbon concentrations range from 104 to 3.5 x 105 ng/g Corg. The latter value is more than one order of magnitude lower than expected for petroleum source beds in the main phase of oil generation. The low maturity at 600 meters depth is further supported by light hydrocarbon concentration ratios. The change of the kerogen type from Lithologic Unit 5 (Type III) to 6 (Type II) is evidenced by changes in the C6 and C7 hydrocarbon composition. Redistribution phenomena are observed close to the Tertiary-Cretaceous unconformity and at the contact between the "black shale" unit and the overlying Cretaceous chalks and claystones. Otherwise, the low molecular weight hydrocarbons in Hole 511 are formed in situ and remain at their place of formation. The core samples turned out to be contaminated by large quantities of acetone, which is routinely used as a solvent during sampling procedures onboard Glomar Challenger.