BUSCADOR RECOLECTA

Supporting Information: Preparation Details and Physical and Spectroscopic Data of Compounds 13-36; 1H and 13C NMR Spectra of Compounds 13-36., Peer reviewed

[EN] Programa del Congreso Internacional “Western Europe in the First Millennium BC: Crossing the divide”, organizado por Tom Moore y Xosé-Lois Armada y celebrado en el Departamento de Arqueología de la Universidad de Durham, Reino Unido (23-25 de noviembre de 2007)., [ES] Programme of the International conference “Western Europe in the First Millennium BC: Crossing the divide”, organized by Tom Moore and Xosé-Lois Armada and held at the Department of Archaeology, Durham University, UK (November 23-25th, 2007).

The ALCUDIA transect is a 230 km long, vertical incidence deep seismic reflection profile acquired in 2007. The acquisition parameters, 35 m station spacing, 70 m Vibration Point spacing resulted in a 60-90 fold high resolution seismic reflection image. A 20 s long Vibroseis sweep with frequencies between 8-80 Hz was recorded by a 400 station recording cable and 14 km long split spread configuration., ALCUDIA Normal Incidence (ALCUDIA-NI) is a NE-SW oriented vertical incidence deep seismic reflection transect in the SW of Spain that aimed to image the Variscan Iberian Massif. This transect sampled the Central Iberian Zone and was designed to be the northward continuation of the IBERSEIS-NI seismic profile. The processed image shows a weakly reflective upper crust, a thick, highly reflective and laminated lower crust, and a flat Moho located at 10 s TWTT (30 km depth). The transect can be divided into three segments with different structural styles in the lower crust. In the central segment, the lower crust is imaged by regular, horizontal and parallel reflectors, whereas in the northern and southern segments it displays oblique reflectors interpreted as an important thrust (north) and tectonic wedging involving the mantle (south). The ALCUDIA-NI shows that in an intracontinental orogenic crust, far from the suture zones, the upper and lower crust may react differently to shortening in different sectors, which is taken as evidence for decoupling. The interpreted structures, as deduced from surface geology and the seismic image, show that deformation was distributed homogeneously in the upper crust, whereas it was concentrated in wedge/thrust structures at specific sectors in the lower crust., Spanish Ministry of Science and Innovation, CGL2004-04623/BTE, CSD2006-00041.-- Ministerio de economía y competitividad, CGL2007-63101/BTE.-- Ministerio de economía y competitividad; Fondos Europeos de desarrollo regional (FEDER), CGL2011-24101.-- Junta de Castilla-La Mancha.--, Peer reviewed

RODA-II Cruise (29HE20070201) carried out on the Research Vessel Hespérides in 2007, Oceanic eddies and atmospheric deposition: influence on particle flows and remineralization in the water column. Study of marine eddies and their relationship with cyclones and anticyclones. They have made diverse experiments, to analyze the lethal thresholds of complex mixtures of organic pollutants (PCBs, PAHs ) on natural communities of phytoplankton. Experiments related to ultraviolet radiation, PAHs and Net community production have also been carried out during the cruise

ATOS-1 Cruise (29HE20070627) carried out on the Research Vessel Hespérides in 2007, ATOS: Atmospheric inputs of organic carbon and pollutants to the polar ocean: rates, significance and outlook. The ATOS project aims at resolving the increasing role of air-sea exchanges of materials in the polar sea by (1) quantifying the atmospheric inputs of organic carbon and key organic pollutants both in aerosol and gaseous phases; (2) elucidating the role of sea ice cover in controlling these rates and the inputs associated to sea ice melting; (3) evaluating the fate of the materials, by assessing their use by biota and transference up the food webs, and (4) evaluating the effects on microplankton as the entry points of the materials in the food web, through evaluations of cell mortality in relation to pollutant inputs and parallel increases in ultraviolet raditation dosage, and the evaluation of the effect of the materials on planktonic primary production and community respiration. This project will advance current knowledge on the relevance of air-sea interactions for the metabolism, and flow of pollutants, of pelagic polar ecosystems, as well as provide a basis to forecast the effects of future reductions of sea icea in polar seas and oceans on the functioning of the pelagic ecosystems. Moreover, as the atmospheric materials that enter the sea in polar regions are likely to be introduced elsewhere, primarily on land, this research will provide novel insights onto the role of the atmosphere as a vector linking loading of organic carbon and pollutants in temperate and tropical latitudes and the inputs of these materials to polar seas and oceans. Moreover, the process-based examination of the response of microplankton to these inputs will allow formulation of models to forecast responses to future scenarios

SVAIS Cruise (29HE20070802) carried out on the Research Vessel Hespérides in 2007, The aim of the cruise is to reconstruct the changes that occurred on the seabed southwest of the Svalbard Islands (Norway) since the beginning of the glacial conditions, three million years ago, up to the present time. Thus, a better knowledge of the natural evolution of glaciers during past times, warmer than today, will help us a better understanding of current and future climate changes. 8,600 km2 of the seafloor surveyed for bathymetry and subbottom profiling , 516 km of single channel seismic reflection profiles 31 meters of sediment recovered (6 cores)

ZEE-2007 Cruise (29HE20070904) carried out on the Research Vessel Hespérides in 2007, Spanish Exclusive Economic Zone cruise 2007. Hydrography-oceanography research Plan of the Exclusive Spanish Economic Zone

EUROLEON Cruise (29HE20071006) carried out on the Research Vessel Hespérides in 2007, Study the relationships between the current morphology of the seabed, the sedimentary coating and the transport processes of active and past sediments. Integrated analysis of the sedimentary drainage systems of the continental margin, incorporating a "seascape" modeling component that includes the most determining control factors and the development rates of the morphosedimentary elements that make up the margin and the deep basin.The ROV transects were predefined from multibeam bathymetry in a seamount area in October 2007 during the ‘EUROLEON’ cruise on board R/V Hespérides, along the Iberian margin of the Valencia Trough. A video survey was performed with a ROV (Max Rover Mark II) equipped with two video cameras and with zoom (central and lateral view) and 6 light focus. The dive was conducted between 460 and 800 m depth. Videos were analyzed in real time onboard and observed animals were identified up to the possible minimum taxonomical level

TRYNITOP-1 Cruise (29HE20071116) carried out on the Research Vessel Hespérides in 2007, Trynitrop ('Trichodesmium and N2 fixation in the tropical Atlantic). The objective of the TRYNITROP project is to characterize the distribution and activity of Trichodesmium and other N2 fixatives, to determine the factors responsible for the control of N2 fixation as well as the contribution of these organisms to the fluxes of C and N mediated by the microbial plankton in the Phototic layer of the Tropical Atlantic. During the campaign, different experiments have been carried out

COPLA Cruise (29HE20080324) carried out on the Research Vessel Hespérides in 2007, Collaborative Cruise COPLA, National Commission of Outer Limits of the Continental Shelf Argentina (Comisión Nacional del Límite Exterior de la Plataforma Continental Argentina)