urn:SDN:CSR:LOCAL:29SG20130514 utf8 Campaña/Survey Cruise Summary record Instituto Español de Oceanografía IEO/Spanish Oceanographic Institute +34 91 342 11 00 +34 91 597 47 70 Corazon de Maria, 8 MADRID 28002 Spain cedo@ieo.es http://www.ieo.es pointOfContact 2015-05-27 ISO 19115/SeaDataNet profile 1.0 Campaña: GALINCLIMARCH2 Survey: GALINCLIMARCH2 Referencia IEO: 29SG20130514 IEO ID: 29SG20130514 2013-05-17 creation urn:SDN:CSR:LOCAL:29SG20130514 urn:SDN:CSR:LOCAL:29SG20130514 Vigo university Marine geosciences and Spatial planing Department (UVIGO) Vigo university Marine geosciences and Spatial planing Department (UVIGO) +34 986 812614 +34 986 812556 Universidade de Vigo. Dpto. de Xeociencias Mariñas e Ordenación del Territorio. Campus As Lagoas- Marcosende Vigo 36310 Spain depc10@uvigo.es http://c10.webs.uvigo.es/webc10/ originator Vigo university Marine geosciences and Spatial planing Department (UVIGO) Vigo university Marine geosciences and Spatial planing Department (UVIGO) +34 932 309500 +34 932 309555 Paseo Maritimo de la Barceloneta, 37-49 Barcelona 08003 Spain info@utm.csic.es http://www.utm.csic.es/ originator The sediments of the Galician Interior Basin realm are capable of recording the peculiar conditions of the last glacial‐interglacial dynamics transition into the current interglacial and their evolution into present day, as they are influenced by the Thermohaline Circulation (THC) and because their proximity to the important continental land‐mass of western Iberia. The knowledge of the rates and magnitudes of change of this system is critical to understand its climate dynamics, processes and feedbacks, and hence its role on a local to sub‐regional scale. The inference of these climatic mechanisms encrypted in the deep‐sea sedimentary record needs to constrain the spatial and temporal scales of the sedimentary processes involved, in particular the identification of source areas, pathways and transport, storage times and hydrodynamic conditions. To adequately assess these encrypted sedimentary archives it is instrumental to identify the sedimentary expression of the main processes and forcements involved and accurately determine the spatial and temporal scales, rates and magnitudes of the processes and feedbacks that generate these records. This proposal aims to carry out a high‐resolution reconstruction of the transport time,provenance, sediment fluxes, wave climate, bottom‐current variability and post‐depositional alteration in a number of surficial samples and cores from the Galician Interior Basin. This project will provide a first insight into the relation between the last North Atlantic climate oscillation and the local regional components including abrupt climate changes (i.e. H events) and local events since the end of the last glacial period from a paleoclimatic proxies perspective. We will use a twofold approach by first constraining the current sedimentary conditions to their associated local wave climate and North Atlantic regional forcements to subsequently infer the paleoenvironmental conditions from the past 30‐50 ky sedimentary record. Firstly, analysing and modelling the present hydraulic conditions from newly acquired and historical wave climate and oceanographic records from the study area will study the current sedimentary conditions and forcements. These data will be linked to the present day sedimentation conditions by direct measurements of present day sedimentation and oceanographic conditions, supported by moored sediment traps, CTD, Doppler records and surficial samples. Epifauna, infauna, microfauna and sediment microestructure will also be studied. Subsequently we will udertake a multidisciplinary study combining high‐resolution geochemical, physical properties, environmental magnetic sediment derived records with high precision U‐series isotopes analyses in a well‐constrained geochronological framework. Further support will be provided by seismic‐acoustic data acquisition. The combination of these sedimentological, micropaleontological, geochemical and geophysical tools will help in better resolving the role of current strength, circulation and sediment provenance changes also considering across vs. along margin transport balances in the sedimentary record of the Galician Internal basin over the last 30‐50 ky The sediments of the Galician Interior Basin realm are capable of recording the peculiar conditions of the last glacial‐interglacial dynamics transition into the current interglacial and their evolution into present day, as they are influenced by the Thermohaline Circulation (THC) and because their proximity to the important continental land‐mass of western Iberia. The knowledge of the rates and magnitudes of change of this system is critical to understand its climate dynamics, processes and feedbacks, and hence its role on a local to sub‐regional scale. The inference of these climatic mechanisms encrypted in the deep‐sea sedimentary record needs to constrain the spatial and temporal scales of the sedimentary processes involved, in particular the identification of source areas, pathways and transport, storage times and hydrodynamic conditions. To adequately assess these encrypted sedimentary archives it is instrumental to identify the sedimentary expression of the main processes and forcements involved and accurately determine the spatial and temporal scales, rates and magnitudes of the processes and feedbacks that generate these records. This proposal aims to carry out a high‐resolution reconstruction of the transport time,provenance, sediment fluxes, wave climate, bottom‐current variability and post‐depositional alteration in a number of surficial samples and cores from the Galician Interior Basin. This project will provide a first insight into the relation between the last North Atlantic climate oscillation and the local regional components including abrupt climate changes (i.e. H events) and local events since the end of the last glacial period from a paleoclimatic proxies perspective. We will use a twofold approach by first constraining the current sedimentary conditions to their associated local wave climate and North Atlantic regional forcements to subsequently infer the paleoenvironmental conditions from the past 30‐50 ky sedimentary record. Firstly, analysing and modelling the present hydraulic conditions from newly acquired and historical wave climate and oceanographic records from the study area will study the current sedimentary conditions and forcements. These data will be linked to the present day sedimentation conditions by direct measurements of present day sedimentation and oceanographic conditions, supported by moored sediment traps, CTD, Doppler records and surficial samples. Epifauna, infauna, microfauna and sediment microestructure will also be studied. Subsequently we will udertake a multidisciplinary study combining high‐resolution geochemical, physical properties, environmental magnetic sediment derived records with high precision U‐series isotopes analyses in a well‐constrained geochronological framework. Further support will be provided by seismic‐acoustic data acquisition. The combination of these sedimentological, micropaleontological, geochemical and geophysical tools will help in better resolving the role of current strength, circulation and sediment provenance changes also considering across vs. along margin transport balances in the sedimentary record of the Galician Internal basin over the last 30‐50 ky Rey García, Daniel Vigo university Marine geosciences and Spatial planing Department (UVIGO) Vigo university Marine geosciences and Spatial planing Department (UVIGO) +34 986 812614 +34 986 812556 Universidade de Vigo. Dpto. de Xeociencias Mariñas e Ordenación del Territorio. Campus As Lagoas- Marcosende Vigo 36310 Spain depc10@uvigo.es http://c10.webs.uvigo.es/webc10/ pointOfContact http://www.seadatanet.ieo.es/csr_figures/29SG/29SG20130514_track_chart.jpg track chart JPEG Oceanographic geographical features theme GEMET - INSPIRE themes, version 1.0 2008-06-01 publication Vigo departure_place SeaDataNet Ports Gazetteer C38 2015-03-01 revision 45 http://www.seadatanet.org/urnurl/SDN:C38 Vigo arrival_place SeaDataNet Ports Gazetteer C38 2015-03-01 revision 45 http://www.seadatanet.org/urnurl/SDN:C38 Spain departure_country International Standards Organisation countries C32 2011-12-15 revision 6 http://www.seadatanet.org/urnurl/SDN:C32 Spain arrival_country International Standards Organisation countries C32 2011-12-15 revision 6 http://www.seadatanet.org/urnurl/SDN:C32 Sarmiento de Gamboa platform ICES Platform Codes C17 2015-03-19 revision 436 http://www.seadatanet.org/urnurl/SDN:C17 research vessel platform_class SeaVoX Platform Categories L06 2015-03-27 revision 11 http://www.seadatanet.org/urnurl/SDN:L06 Atlantic Ocean place SeaVoX salt and fresh water body gazetteer C19 2015-02-19 revision 16 http://www.seadatanet.org/urnurl/SDN:C19 145 146 marsden_square Ten-degree Marsden Squares C37 2009-01-09 revision 3 http://www.seadatanet.org/urnurl/SDN:C37 Salinity of the water column Temperature of the water column Vertical spatial coordinates Air temperature Wind speed and direction Atmospheric humidity Solar Radiation Air pressure Raw temperature and/or salinity instrument output Horizontal spatial co-ordinates Bathymetry and Elevation Concentration of inorganic sulphur species in sediment Dissolved concentration parameters for 'other' gases in sediment pore waters Magnetic susceptibility of sediment Mineral chemistry Palaeoclimatic indicators and parameters Redox potential in sediment Rock porosity and permeability Sediment density Sediment grain size parameters Sediment microfossil morphology parameters Sediment mineralogy parameters Sediment resistivity Sediment temperature Sediment thermal conductivity Sediment water content, porosity and surface area parameter SeaDataNet Parameter Discovery Vocabulary P02 2015-02-04 revision 87 http://www.seadatanet.org/urnurl/SDN:P02 meteorological packages thermosalinographs single-beam echosounders multi-beam echosounders >2000 Hz top-bandwidth sub-bottom penetrator and mud profiler systems systems Differential Global Positioning System receivers hydrophones wave recorders manual biota samplers sediment grabs sediment porewater samplers CTD redox potential sensors sediment traps unconsolidated sediment corers radiometers discrete water samplers gravimeters NAVSTAR Global Positioning System receivers instrument SeaDataNet device categories L05 2015-02-12 revision 49 http://www.seadatanet.org/urnurl/SDN:L05 Not applicable utf8 oceans -10.319286 -8.719273 41.8533147 42.7994847 2013-05-14T00:00:00 2013-05-17T00:00:00 XML 1 https://csr.seadatanet.org/ WWW:LINK-1.0-http--related Base de datos internacional con información de campañas desde 1873 hasta la actualidad. La presente campaña la podrás encontrar como GALINCLIMARCH2. International database with information of surveys from 1873 till today. Use the tag GALINCLIMARCH2 to locate the present survey. SeaDataNet - CRS inventory https://cdi.seadatanet.org/search WWW:LINK-1.0-http--related Descubre si hay datos de esta campaña disponibles, utilizando para ello la etiqueta GALINCLIMARCH2 en el buscador de datos de SeaDataNet. Discover if there are available data associated to this cruise by using the tag GALINCLIMARCH2 in the free search box of the SeaDataNet portal. SeaDataNet - CDI inventory Campaña/Survey Reglamento (UE) n o 1089/2010 de la Comisión de 23 de noviembre de 2010 por el que se aplica la Directiva 2007/2/CE del Parlamento Europeo y del Consejo en lo que se refiere a la interoperabilidad de los conjuntos y los servicios de datos espaciales Commission Regulation (EU) No 1312/2014 of 10 December 2014 amending Regulation (EU) No 1089/2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data services 2010-12-08 publication See the referenced specification true El Centro de datos aplica controles de calidad estandarizados a todos los datos de los que es responsable. Contacta con el Centro de datos para más información. The Data Center applies standard data quality control procedures on all data. Ask the Data Center for details.