Project Name | PES - Pockmarks and fluid seepage in the Estremadura Spur: implications for regional geology, biology, and petroleum systems | |
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Funding entity | FCT - Fundação para a Ciência e a Tecnologia (PTDC/GEO-FIQ/5162/2014) | |
Project leader | IPMA | |
Project manager | Vitor Hugo da Silva Magalhães | |
Description | PES is a process-oriented multidisciplinary project focused on the pockmarks, fluid migration and seepage recently discovered in the Estremadura Spur continental shelf (Portugal), and on their implications to the regional geology, to the evolution of this section of the margin and to their petroleum system, and their significance to the ecosystems. A field with more than 40 individual pockmarks, covering an area of at least 27 km2, was
recently discovered and partially surveyed (Kim and shipboard scientific party, 2011; PACEMAKER
project funded by the European Research Council). This data set was made available for this
project. This field of pockmarks is located at the outer shelf of the Estremadura Spur, between 200
and 350 m water depth, with individual pockmarks up to 120 m in diameter and 10 m depth. A
preliminary processing of the backscatter data indicate that some pockmarks have a high acoustic
seafloor reflectivity in their central part, most probably indicating the presence of
methane-derived authigenic carbonate hard-grounds. While fluid flow is a widespread process in
continental margins and sedimentary basins, this is the first record of fluid escape processes were
not previously identified on the W Iberian margin. Gas seepage evidence in the Iberia margin has
only been reported in estuarine environments such as the Ria de Vigo (Iglesias and Garcia-Gil,
2007), the Aveiro Estuary/lagoon (Duarte et al., 2007), and in the Gulf of Cadiz (Magalhães, 2007;
Magalhães et al., 2012; Pinheiro et al., 2003). This pockmark field and underlying fluid generation
and escape processes, which are the focus of this project, are thus the first fluid seepage system
identified and reported from the W Portuguese margin, not yet investigated.
The PES research team has a large experience with regards to fluid seepage systems, embracing geology, geophysics, geochemistry, ecosystem characterization and habitat mapping, and includes also key members of the European PEACEMAKER project. The proposed research objectives will be achieved, in a first stage, through the processing of the existing geophysical data where 4 pockmarks will be selected for detailed investigation during one research cruise. Detailed geophysical surveys will be acquired with swath-bathymetry, backscatter, seismics, sidescan sonar and water column acoustics. This will guide the direct seafloor observation with an ROV, capable of seawater analysis and sampling. The geophysical data and ROV observations will allow the characterization of the seepage system, at the seafloor and in depth, at a detailed (at structure) scale. Systematic sampling of sediments, authigenic carbonates, pore-waters fluid and gas, and macrofauna will follow using gravity, box and multi-corer. Sediments and authigenic carbonates will be characterized for their grain-size, mineralogy, geochemistry, C and O isotopes, pore water inorganic and organic geochemistry and seepage gas composition, so that the seepage activity will be characterized, allowing to infer the significance of the system to the regional geology and ecology. Team: Vitor Hugo Magalhaes, IPMA, Vitor.magalhaes@ipma.pt
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Start date | 2016-05-01 | |
End date | 2019-04-30 |