The extracellular surface of the GLP-1 receptor is a molecular trigger for biased agonism

Ligand-directed signal bias offers opportunities for sculpting molecular events, with the promise of better, safer therapeutics. Critical to the exploitation of signal bias is an understanding of the molecular events coupling ligand binding to intracellular signaling. Activation of class B G protein-coupled receptors is driven by interaction of the peptide N terminus with the receptor core. To understand how this drives signaling, we have used advanced analytical methods that enable separation of effects on pathway-specific signaling from those that modify agonist affinity and mapped the functional consequence of receptor modification onto three-dimensional models of a receptor-ligand complex. This yields molecular insights into the initiation of receptor activation and the mechanistic basis for biased agonism. Our data reveal that peptide agonists can engage different elements of the receptor extracellular face to achieve effector coupling and biased signaling providing a foundation for rational design of biased agonists.

The correlation of structure and electronic properties near the surface of transition metal oxides

The strong couplings between different degrees of freedom are believed to be responsible for novel and complex phenomena discovered in transition metal oxides (TMOs). The physical complexity is directly responsible for their tunability. Creating surfaces/interfaces add an additional ' man-made' twist, approaching the quantum phenomena of correlated materials. ^ The dissertation focused on the structural and electronic properties in proximity of surface of three prototype TMO compounds by using three complementary techniques: scanning tunneling microscopy, angle-resolved photoelectron spectroscopy and low energy electron diffraction, particularly emphasized the effects of broken symmetry and imperfections like defects on the coupling between charge and lattice degrees of freedom. ^ Ca1.5Sr0.5RuO4 is a layered ruthenate with square lattice and at the boundary of magnetic/orbital instability in Ca2-xSrxRuO4. That the substitution of Sr 2+ with Ca2+ causing RuO6 rotation narrows the dxy band width and changes the Fermi surface topology. Particularly, the γ(dxy) Fermi surface sheet exhibited hole-like in Ca1.5Sr0.5RuO4 in contrast to electron-like in Sr2RuO4, showing a strong charge-lattice coupling. ^ Na0.75CoO2 is a layered cobaltite with triangular lattice exhibiting extraordinary thermoelectric properties. The well-ordered CoO2-terminated surface with random Na distribution was observed. However, lattice constants of the surface are smaller than that in bulk. The surface density of states (DOS) showed strong temperature dependence. Especially, an unusual shift of the minimum DOS occurs below 230 K, clearly indicating a local charging effect on the surface. ^ Cd2Re2O7 is the first known pyrochlore oxide superconductor (Tc ∼ 1K). It exhibited an unusual second-order phase transition occurring at TS1 = 200 K and a controversial first-order transition at TS2 = 120 K. While bulk properties display large anomalies at TS1 but rather subtle and sample-dependent changes at TS2, the surface DOS near the EF show no change at T s1 but a substantial increase below TS2---a complete reversal as the signature for the transitions. We argued that crystal imperfections, mainly defects, which were considerably enhanced at the surface, resulted in the transition at TS2. ^

Endothelin 3 induces skin pigmentation in a keratin-driven inducible mouse model

Endothelin 3 (Edn3) is a ligand important to developing neural crest cells (NCC). Some NCC eventually migrate into the skin and give rise to the pigment-forming melanocytes found in hair follicles. Edn3's effects on NCC have been largely explored through spontaneous mutants and cell culture experiments. These studies have shown the Endothelin receptor B/Edn3 signaling pathway to be important in the proliferation/survival and differentiation of developing melanocytes. To supplement these investigations I have created doxycycline-responsive transgenic mice which conditionally over-express Edn3. These mice will help us clarify Edn3's role during the development of early embryonic melanoblasts, differentiating melanocyte precursors in the skin, and fully differentiated melanocytes in the hair follicle. The transgene mediated expression of Edn3 was predominantly confined to the roof plate of the neural tube and surface ectoderm in embryos and postnatally in the epidermal keratinocytes of the skin. Relative to littermate controls, transgenics develop increased pigmentation on most areas of the skin. My doxycycline-based temporal studies have shown that both embryonic and postnatal events are important for establishing and maintaining pigmented skin. The study of my Edn3 transgenic mice may offer some insight into the genetics behind benign dermal pigmentation and offer clues about the time periods important in establishing these conditions. This apparently abnormal development is echoed in a benign condition of human skin. Cases of dermal melanocytosis, such as common freckles, Mongolian spotting, and nevus of Ito demonstrate histological and etiological characteristics similar to those of the transgenic mice generated in this study.

Development of test-based wind-driven rain intrusion model for hurricane-induced building interior and contents damage

Major portion of hurricane-induced economic loss originates from damages to building structures. The damages on building structures are typically grouped into three main categories: exterior, interior, and contents damage. Although the latter two types of damages, in most cases, cause more than 50% of the total loss, little has been done to investigate the physical damage process and unveil the interdependence of interior damage parameters. Building interior and contents damages are mainly due to wind-driven rain (WDR) intrusion through building envelope defects, breaches, and other functional openings. The limitation of research works and subsequent knowledge gaps, are in most part due to the complexity of damage phenomena during hurricanes and lack of established measurement methodologies to quantify rainwater intrusion. This dissertation focuses on devising methodologies for large-scale experimental simulation of tropical cyclone WDR and measurements of rainwater intrusion to acquire benchmark test-based data for the development of hurricane-induced building interior and contents damage model. Target WDR parameters derived from tropical cyclone rainfall data were used to simulate the WDR characteristics at the Wall of Wind (WOW) facility. The proposed WDR simulation methodology presents detailed procedures for selection of type and number of nozzles formulated based on tropical cyclone WDR study. The simulated WDR was later used to experimentally investigate the mechanisms of rainwater deposition/intrusion in buildings. Test-based dataset of two rainwater intrusion parameters that quantify the distribution of direct impinging raindrops and surface runoff rainwater over building surface — rain admittance factor (RAF) and surface runoff coefficient (SRC), respectively —were developed using common shapes of low-rise buildings. The dataset was applied to a newly formulated WDR estimation model to predict the volume of rainwater ingress through envelope openings such as wall and roof deck breaches and window sill cracks. The validation of the new model using experimental data indicated reasonable estimation of rainwater ingress through envelope defects and breaches during tropical cyclones. The WDR estimation model and experimental dataset of WDR parameters developed in this dissertation work can be used to enhance the prediction capabilities of existing interior damage models such as the Florida Public Hurricane Loss Model (FPHLM).^

Water temperature reconstructions based on paired Uk'37 and Tex86 records, and paired surface and subsurface Mg/Ca records

This dataset contains the collection of available published paired Uk'37 and Tex86 records spanning multi-millennial to multi-million year time scales, as well as a collection of Mg/Ca-derived temperatures measured in parallel on surface and subsurface dwelling foraminifera, both used in the analyses of Ho and Laepple, Nature Geoscience 2016. As the signal-to-noise ratios of proxy-derived Holocene temperatures are relatively low, we selected records that contain at least the last deglaciation (oldest sample >18kyr BP).

Development of a high-frequency surface-wave radar cross section model for icebergs

In this thesis, the first-order radar cross section (RCS) of an iceberg is derived and simulated. This analysis takes place in the context of a monostatic high frequency surface wave radar with a vertical dipole source that is driven by a pulsed waveform. The starting point of this work is a general electric field equation derived previ- ously for an arbitrarily shaped iceberg region surrounded by an ocean surface. The condition of monostatic backscatter is applied to this general field equation and the resulting expression is inverse Fourier transformed. In the time domain the excitation current of the transmit antenna is specified to be a pulsed sinusoid signal. The result- ing electric field equation is simplified and its physical significance is assessed. The field equation is then further simplified by restricting the iceberg's size to fit within a single radar patch width. The power received by the radar is calculated using this electric field equation. Comparing the received power with the radar range equation gives a general expression for the iceberg RCS. The iceberg RCS equation is found to depend on several parameters including the geometry of the iceberg, the radar frequency, and the electrical parameters of both the iceberg and the ocean surface. The RCS is rewritten in a form suitable for simulations and simulations are carried out for rectangularly shaped icebergs. Simulation results are discussed and are found to be consistent with existing research.

Estimates of annual mean surface temperatures in the late Quaternary of the tropical Atlantic

At least two modes of glacial-interglacial climate change have existed within the tropical Atlantic Ocean during the last 20,000 years. The first mode (defined by cold glacial and warm interglacial conditions) occurred symmetrically north and south of the equator and dominated the eastern boundary currents and tropical upwelling areas. This pattern suggests that mode 1 is driven by a glacial modification of surface winds in both hemispheres. The second mode of oceanic climate change, defined by temperature extremes centered on the deglaciation, was hemispherically asymmetrical, with the northern tropical Atlantic relatively cold and the southern tropical Atlantic relatively warm during deglaciation. A likely cause for this pattern of variation is a reduction of the presently northward cross-equatorial heat flux during deglaciation. No single mechanism accounts for all the data. Potential contributors to oceanic climate changes are linkage to high-latitude climates, modification of monsoonal winds by ice sheet and/or insolation changes, atmospheric CO2 and greenhouse effects, indirect effects of glacial meltwater, and variations in thermohaline overturn of the oceans.

Novel surface-tethered estrogen polymeric platforms in cardiovascular regenerative medicine

L’estradiol (E2) est une hormone femelle qui joue un rôle essentiel, à la fois dans la régulation et dans la détermination de certaines conditions physiologiques in vivo, telle que la différenciation et la prolifération cellulaire. Lorsque l’E2 est donné en supplément, par exemple dans le cas de thérapie hormonale, deux effets sont observés, un effet génomique et un effet non-génomique, de par son interaction avec les récepteurs à œstrogène du noyau ou de la membrane cellulaire, respectivement. L’effet non-génomique est plus difficile à étudier biologiquement parce que l’effet se produit sur une échelle de temps extrêmement courte et à cause de la nature hydrophobe de l’E2 qui réduit sa biodisponibilité et donc son accessibilité aux cellules cibles. C’est pourquoi il est nécessaire de développer des systèmes d’administration de l’E2 qui permettent de n’étudier que l’effet non-génomique de l’œstrogène. Une des stratégies employée consiste à greffer l’E2 à des macromolécules hydrophiles, comme de l’albumine de sérum bovin (BSA) ou des dendrimères de type poly(amido)amine, permettant de maintenir l’interaction de l’E2 avec les récepteurs d’œstrogène de la membrane cellulaire et d’éviter la pénétration de l’E2 dans le noyau des cellules. Toutefois, ces systèmes macromolécules-E2 sont critiquables car ils sont peu stables et l’E2 peut se retrouver sous forme libre, ce qui affecte sa localisation cellulaire. L’objectif de cette thèse est donc de développer de nouvelles plateformes fonctionnalisées avec de l’E2 en utilisant les approches de synthèses ascendantes et descendantes. Le but de ces plateformes est de permettre d’étudier le mécanisme de l’effet non-génomique de l’E2, ainsi que d’explorer des applications potentielles dans le domaine biomédical. L’approche ascendante est basée sur un ligand d’E2 activé, l’acide 17,α-éthinylestradiol-benzoïque, attaché de façon covalente à un polymère de chitosan avec des substitutions de phosphorylcholine (CH-PC-E2). L’estradiol est sous forme de pro-drogue attachée au polymère qui s’auto-assembler pour former un film. L’effet biologique de la composition chimique du film de chitosan-phosphorylcholine a été étudié sur des cellules endothéliales. Les films de compositions chimiques différentes ont préalablement été caractérisés de façon physicochimique. La topographie de la surface, la charge de surface, ainsi que la rhéologie des différents films contenant 15, 25, ou 40% molaires de phosphorylcholine, ont été étudiés par microscopie à force atomique (AFM), potentiel zêta, résonance plasmonique de surface et par microbalance à cristal de quartz avec dissipation (QCM-D). Les résultats de QCM-D ont montré que plus la part molaire en phosphorylcholine est grande moins il y a de fibrinogène qui s’adsorbe sur le film de CH-PC. Des cellules humaines de veine ombilicale (HUVECs) cultivées sur des films de CH-PC25 et de CH-PC40 forment des amas cellulaire appelés sphéroïdes au bout de 4 jours, alors que ce n’est pas le cas lorsque ces cellules sont cultivées sur des films de CH-PC15. L’attachement de l’estradiol au polymère a été caractérisé par plusieurs techniques, telles que la résonance magnétique nucléaire de proton (1H NMR), la spectroscopie infrarouge avec transformée de Fourier à réfraction totale atténuée (FTIR-ATR) et la spectroscopie UV-visible. La nature hydrogel des films (sa capacité à retenir l’eau) ainsi que l’interaction des films avec des récepteurs à E2, ont été étudiés par la QCM-D. Des études d’imagerie cellulaires utilisant du diacétate de diaminofluoresceine-FM ont révélé que les films hydrogels de CH-PC-E2 stimulent la production d’oxyde nitrique par les cellules endothéliales, qui joue un rôle protecteur pour le système cardiovasculaire. L’ensemble de ces études met en valeur les rôles différents et les applications potentielles qu’ont les films de type CH-PC-E2 et CH-PC dans le cadre de la médecine cardiovasculaire régénérative. L’approche descendante est basée sur l’attachement de façon covalente d’E2 sur des ilots d’or de 2 μm disposés en rangées et espacés par 12 μm sur un substrat en verre. Les ilots ont été préparés par photolithographie. La surface du verre a quant à elle été modifiée à l’aide d’un tripeptide cyclique, le cRGD, favorisant l’adhésion cellulaire. L’attachement d’E2 sur les surfaces d’or a été suivi et confirmé par les techniques de SPR et de QCM-D. Des études d’ELISA ont montré une augmentation significative du niveau de phosphorylation de la kinase ERK (marqueur important de l’effet non-génomique) après 1 heure d’exposition des cellules endothéliales aux motifs alternant l’E2 et le cRGD. Par contre lorsque des cellules cancéreuses sont déposées sur les surfaces présentant des motifs d’E2, ces cellules ne croissent pas, ce qui suggère que l’E2 n’exerce pas d’effet génomique. Les résultats de l’approche descendante montrent le potentiel des surfaces présentant des motifs d’E2 pour l’étude des effets non-génomiques de l’E2 dans un modèle in vitro.

High-Resolution In Situ Oxygen-Argon Studies of Surface Biological and Physical Processes in the Polar Oceans

The Arctic Ocean and Western Antarctic Peninsula (WAP) are the fastest warming regions on the planet and are undergoing rapid climate and ecosystem changes. Until we can fully resolve the coupling between biological and physical processes we cannot predict how warming will influence carbon cycling and ecosystem function and structure in these sensitive and climactically important regions. My dissertation centers on the use of high-resolution measurements of surface dissolved gases, primarily O2 and Ar, as tracers or physical and biological functioning that we measure underway using an optode and Equilibrator Inlet Mass Spectrometry (EIMS). Total O2 measurements are common throughout the historical and autonomous record but are influenced by biological (net metabolic balance) and physical (temperature, salinity, pressure changes, ice melt/freeze, mixing, bubbles and diffusive gas exchange) processes. We use Ar, an inert gas with similar solubility properties to O2, to devolve distinct records of biological (O2/Ar) and physical (Ar) oxygen. These high-resolution measurements that expose intersystem coupling and submesoscale variability were central to studies in the Arctic Ocean, WAP and open Southern Ocean that make up this dissertation.

Key findings of this work include the documentation of under ice and ice-edge blooms and basin scale net sea ice freeze/melt processes in the Arctic Ocean. In the WAP O2 and pCO2 are both biologically driven and net community production (NCP) variability is controlled by Fe and light availability tied to glacial and sea ice meltwater input. Further, we present a feasibility study that shows the ability to use modeled Ar to derive NCP from total O2 records. This approach has the potential to unlock critical carbon flux estimates from historical and autonomous O2 measurements in the global oceans.

A New Method for Modeling Free Surface Flows and Fluid-structure Interaction with Ocean Applications

The computational modeling of ocean waves and ocean-faring devices poses numerous challenges. Among these are the need to stably and accurately represent both the fluid-fluid interface between water and air as well as the fluid-structure interfaces arising between solid devices and one or more fluids. As techniques are developed to stably and accurately balance the interactions between fluid and structural solvers at these boundaries, a similarly pressing challenge is the development of algorithms that are massively scalable and capable of performing large-scale three-dimensional simulations on reasonable time scales. This dissertation introduces two separate methods for approaching this problem, with the first focusing on the development of sophisticated fluid-fluid interface representations and the second focusing primarily on scalability and extensibility to higher-order methods.

We begin by introducing the narrow-band gradient-augmented level set method (GALSM) for incompressible multiphase Navier-Stokes flow. This is the first use of the high-order GALSM for a fluid flow application, and its reliability and accuracy in modeling ocean environments is tested extensively. The method demonstrates numerous advantages over the traditional level set method, among these a heightened conservation of fluid volume and the representation of subgrid structures.

Next, we present a finite-volume algorithm for solving the incompressible Euler equations in two and three dimensions in the presence of a flow-driven free surface and a dynamic rigid body. In this development, the chief concerns are efficiency, scalability, and extensibility (to higher-order and truly conservative methods). These priorities informed a number of important choices: The air phase is substituted by a pressure boundary condition in order to greatly reduce the size of the computational domain, a cut-cell finite-volume approach is chosen in order to minimize fluid volume loss and open the door to higher-order methods, and adaptive mesh refinement (AMR) is employed to focus computational effort and make large-scale 3D simulations possible. This algorithm is shown to produce robust and accurate results that are well-suited for the study of ocean waves and the development of wave energy conversion (WEC) devices.

Novel surface-tethered estrogen polymeric platforms in cardiovascular regenerative medicine

L’estradiol (E2) est une hormone femelle qui joue un rôle essentiel, à la fois dans la régulation et dans la détermination de certaines conditions physiologiques in vivo, telle que la différenciation et la prolifération cellulaire. Lorsque l’E2 est donné en supplément, par exemple dans le cas de thérapie hormonale, deux effets sont observés, un effet génomique et un effet non-génomique, de par son interaction avec les récepteurs à œstrogène du noyau ou de la membrane cellulaire, respectivement. L’effet non-génomique est plus difficile à étudier biologiquement parce que l’effet se produit sur une échelle de temps extrêmement courte et à cause de la nature hydrophobe de l’E2 qui réduit sa biodisponibilité et donc son accessibilité aux cellules cibles. C’est pourquoi il est nécessaire de développer des systèmes d’administration de l’E2 qui permettent de n’étudier que l’effet non-génomique de l’œstrogène. Une des stratégies employée consiste à greffer l’E2 à des macromolécules hydrophiles, comme de l’albumine de sérum bovin (BSA) ou des dendrimères de type poly(amido)amine, permettant de maintenir l’interaction de l’E2 avec les récepteurs d’œstrogène de la membrane cellulaire et d’éviter la pénétration de l’E2 dans le noyau des cellules. Toutefois, ces systèmes macromolécules-E2 sont critiquables car ils sont peu stables et l’E2 peut se retrouver sous forme libre, ce qui affecte sa localisation cellulaire. L’objectif de cette thèse est donc de développer de nouvelles plateformes fonctionnalisées avec de l’E2 en utilisant les approches de synthèses ascendantes et descendantes. Le but de ces plateformes est de permettre d’étudier le mécanisme de l’effet non-génomique de l’E2, ainsi que d’explorer des applications potentielles dans le domaine biomédical. L’approche ascendante est basée sur un ligand d’E2 activé, l’acide 17,α-éthinylestradiol-benzoïque, attaché de façon covalente à un polymère de chitosan avec des substitutions de phosphorylcholine (CH-PC-E2). L’estradiol est sous forme de pro-drogue attachée au polymère qui s’auto-assembler pour former un film. L’effet biologique de la composition chimique du film de chitosan-phosphorylcholine a été étudié sur des cellules endothéliales. Les films de compositions chimiques différentes ont préalablement été caractérisés de façon physicochimique. La topographie de la surface, la charge de surface, ainsi que la rhéologie des différents films contenant 15, 25, ou 40% molaires de phosphorylcholine, ont été étudiés par microscopie à force atomique (AFM), potentiel zêta, résonance plasmonique de surface et par microbalance à cristal de quartz avec dissipation (QCM-D). Les résultats de QCM-D ont montré que plus la part molaire en phosphorylcholine est grande moins il y a de fibrinogène qui s’adsorbe sur le film de CH-PC. Des cellules humaines de veine ombilicale (HUVECs) cultivées sur des films de CH-PC25 et de CH-PC40 forment des amas cellulaire appelés sphéroïdes au bout de 4 jours, alors que ce n’est pas le cas lorsque ces cellules sont cultivées sur des films de CH-PC15. L’attachement de l’estradiol au polymère a été caractérisé par plusieurs techniques, telles que la résonance magnétique nucléaire de proton (1H NMR), la spectroscopie infrarouge avec transformée de Fourier à réfraction totale atténuée (FTIR-ATR) et la spectroscopie UV-visible. La nature hydrogel des films (sa capacité à retenir l’eau) ainsi que l’interaction des films avec des récepteurs à E2, ont été étudiés par la QCM-D. Des études d’imagerie cellulaires utilisant du diacétate de diaminofluoresceine-FM ont révélé que les films hydrogels de CH-PC-E2 stimulent la production d’oxyde nitrique par les cellules endothéliales, qui joue un rôle protecteur pour le système cardiovasculaire. L’ensemble de ces études met en valeur les rôles différents et les applications potentielles qu’ont les films de type CH-PC-E2 et CH-PC dans le cadre de la médecine cardiovasculaire régénérative. L’approche descendante est basée sur l’attachement de façon covalente d’E2 sur des ilots d’or de 2 μm disposés en rangées et espacés par 12 μm sur un substrat en verre. Les ilots ont été préparés par photolithographie. La surface du verre a quant à elle été modifiée à l’aide d’un tripeptide cyclique, le cRGD, favorisant l’adhésion cellulaire. L’attachement d’E2 sur les surfaces d’or a été suivi et confirmé par les techniques de SPR et de QCM-D. Des études d’ELISA ont montré une augmentation significative du niveau de phosphorylation de la kinase ERK (marqueur important de l’effet non-génomique) après 1 heure d’exposition des cellules endothéliales aux motifs alternant l’E2 et le cRGD. Par contre lorsque des cellules cancéreuses sont déposées sur les surfaces présentant des motifs d’E2, ces cellules ne croissent pas, ce qui suggère que l’E2 n’exerce pas d’effet génomique. Les résultats de l’approche descendante montrent le potentiel des surfaces présentant des motifs d’E2 pour l’étude des effets non-génomiques de l’E2 dans un modèle in vitro.

(Table 1) TOC content, BIT, TEX86 and UK'37 indices, and sea surface temperature reconstruction for the middle Miocene to Pliocene of ODP Hole 175-1085A

The initiation of the Benguela upwelling has been dated to the late Miocene, but estimates of its sea surface temperature evolution are not available. This study presents data from Ocean Drilling Program (ODP) Site 1085 recovered from the southern Cape Basin. Samples of the middle Miocene to Pliocene were analyzed for alkenone-based (UK'37, SSTUK) and glycerol dialkyl glycerol tetraether (GDGT) based (TEX86, TempTEX) water temperature proxies. In concordance with global cooling during the Miocene, SSTUK and TempTEX exhibit a decline of about 8°C and 16°C, respectively. The temperature trends suggest an inflow of cold Antarctic waters triggered by Antarctic ice sheet expansion and intensification of Southern Hemisphere southeasterly winds. A temperature offset between both proxies developed with the onset of upwelling, which can be explained by differences in habitat: alkenone-producing phytoplankton live in the euphotic zone and record sea surface temperatures, while GDGT-producing Thaumarchaeota are displaced to colder subsurface waters in upwelling-influenced areas and record subsurface water temperatures. We suggest that variations in subsurface water temperatures were driven by advection of cold Antarctic waters and thermocline adjustments that were due to changes in North Atlantic deep water formation. A decline in surface temperatures, an increased offset between temperature proxies, and an increase in primary productivity suggest the establishment of the Benguela upwelling at 10 Ma. During the Messinian Salinity Crisis, between 7 and 5 Ma, surface and subsurface temperature estimates became similar, likely because of a strong reduction in Atlantic overturning circulation, while high total organic carbon contents suggest a "biogenic bloom." In the Pliocene the offset between the temperature estimates and the cooling trend was reestablished.

14C specific radiocarbon ages and bulk ages accompanied by geochemical proxys from surface sediment samples in the Black Sea

Transfer of organic carbon (OC) from the terrestrial to the oceanic carbon pool is largely driven by riverine and aeolian transport. Before transport, however, terrigenous organic matter can be retained in intermediate terrestrial reservoirs such as soils. Using compound-specific radiocarbon analysis of terrigenous biomarkers their average terrestrial residence time can be evaluated. Here we show compound-specific radiocarbon (14C) ages of terrigenous biomarkers and bulk 14C ages accompanied by geochemical proxy data from core top samples collected along transects in front of several river mouths in the Black Sea. 14C ages of long chain n-alkanes, long chain n-fatty acids and total organic carbon (TOC) are highest in front of the river mouths, correlating well with BIT (branched and isoprenoid tetraether) indices, which indicates contribution of pre-aged, soil-derived terrigenous organic matter. The radiocarbon ages decrease further offshore towards locations where organic matter is dominated by marine production and aeolian input potentially contributes terrigenous organic matter. Average terrestrial residence times of vascular plant biomarkers deduced from n-C29+31 alkanes and n-C28+30 fatty acids ages from stations directly in front of the river mouths range from 900 ± 70 years to 4400 ± 170 years. These average residence times correlate with size and topography in climatically similar catchments, whereas the climatic regime appears to control continental carbon turnover times in morphologically similar drainage areas of the Black Sea catchment. Along-transect data imply petrogenic contribution of n-C29+31 alkanes and input via different terrigenous biomarker transport modes, i.e., riverine and aeolian, resulting in aged biomarkers at offshore core locations. Because n-C29+31 alkanes show contributions from petrogenic sources, n-C28+30 fatty acids likely provide better estimates of average terrestrial residence times of vascular plant biomarkers. Moreover, sedimentary n-C28 and n-C30 fatty acids appear clearly much less influenced by autochthonous sources than n-C24 and n-C26 fatty acids as indicated by increasing radiocarbon ages with increasing chain-length and are, thus, more representative as vascular plant biomarkers.

Grain-size analysis of surface sediments, continental margin off NW Africa

The terrigenous fraction of seabed sediments recovered along the north-west African continental margin illustrates spatial variability in grain size attributed to different transport mechanisms. Three subpopulations are determined from the grain-size analyses (n = 78) of the carbonate-free silt fraction applying an end-member modelling algorithm (G. J. Weltje, 1997). The two coarsest end-members are interpreted as representing aeolian dust, and the fine-grained end-member is related to fluvial supply. The end-member model thus allows aeolian fallout to be distinguished from fluvial-sourced mud in this area. The relative contributions of the end-members show distinct regional variations that can be related to different transport processes and pathways. Understanding present-day sediment dispersal and mixing is important for a better understanding of older sedimentary records and palaeoclimate reconstructions in the region.

Carbon14 ages of surface sediment samples from ther Persian Gulf

A simplified classification of the Holocene sediments based on textures and grain type results in fourteen major units, twelve of which are essentially carbonate in composition. A brief description and photographic illustration of these units, together with the sedimentary and diagenetic processes which have contributed to their formation, is designed to give the reader a broad but valid impression of Persian Gulf sediments. The distribution of the fourteen sediment units throughout the Arabian parts of the basin, although complicated by numerous local bathymetric highs and depressions, is relatively simple. Because the Arabian sea floor slopes progressively from a windward shoreline to the basin center there is increasing protection from wave action towards the center of the basin. As a result sediments grade from skeletal, oolitic and pelletoidal sands (and muds in coastal lagoons) and fringing reefs, through an irregular zone of compound grain sands,into widespread skeletal muddy sands, and finally into basin center muds. These simple relationships vary laterally around the Arabian side of the gulf. Lateral variation is dependant upon orientation of the regional slope with respect to the prevailing NW wind-driven waves, angle of slope, and presence or absence of regional, structurally based barriers.