mineral and energy resources from the portuguese ... · need to assess the real potential of deep...
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Luis Menezes Pinheiro Dep. Geociências and CESAM, Univ. Aveiro, Portugal
Mineral and Energy Resources
from the Portuguese Continental
Shelf
Câmara do Comércio e Indústria, Lisboa, 14 de Dezembro de 2011
The oceans and the sub-seafloor: the next frontier
occupy 2/3 Earth’s surface, but still largely unknown
Oil, gas, gas hydrates, polymetalic crusts and nodules,
massive sulphides, phosphorites, placers (tin, tungsten,
gold, diamonds), glauconites, carbonates, sand and gravel
Need to assess the real potential of deep sea mineral,
energy and biotechnological resources – Need for
observations - (Ships, ROV’s, AUV’s, Submersibles, Deep
Sea Drilling, Observatories). International Cooperation.
Deep biosphere: geosphere/biosphere coupling processes
Geomicrobiology, Biotechnology
Portuguese Proposal of Extension of the Continental Shelf to the UN
Courtesy Nuno Lourenço, EMAM
Sand and Gravel Exploitation from the continental shelf
Legislation
Normally depths greater than 20m
Distance from the coast usually greater than 2-3 km
Dias, 2003
Sand and Gravel from the Continental shelf
Environmental legislation more rigorous in face of the negative impacts
associated with exploration in rivers and beaches
Marine aggregates extraction (sand and gravel) are becoming more and more an
important mineral resource as land based recourses are being depleted, polluted
or subjected to more severe laws for environmental protection (International
Council for the Exploration of the Sea, 2000).
Areas of the globe where there is more intense exploration:
North Sea, USA costs and the Far East
Sand/gravel extraction in the UK
1959 - 3.9 Mton: 5.7% internal consumption needs
1970 - 13 Mton: 12% “ “ “
1980 – 16.5 Mton: 16.5% “ “ “
Japan – early 80’s was already exploiting 57 Mton submarine sand & gravel
It is becoming a current practice to use such exploitation for beach nourishment.
Açores – exploitation under way for several years.
Potencial in sand and gravel in the Portuguese Margin Artificial Beach Nourishment
Edisto Beach, S. Carolina, USA
Vale do Lobo, Portugal
c Hydrothermal Systems: Açores
Massive sulphides
Biotechnological resources
AÇORES
TTR Cruise, Lucky Strike, 2004
Polimetalic crusts and nodules
Koelle, personal photo
Manganese nodules at around 4100m water
depth in the Peru Basin (Sonne cruise SO-79)
Nodules known since the HMS
Challenger voyage (1872-76).
Manganese nodules and crusts consist of
about 20-30% Manganese, 10-20% iron
oxides, 1.5% Nickel and less than 1% of
cobalt, copper, zinc and lead.
Polymetalic nodules & crusts Seawater lithosphere Fe-Mn crusts
Contents in Manganese, Iron, Cobalt, Nickel, platinum,
cerium, copper and Telurium (wt %) in Fe-Mn crusts, in
comparison with their contents in the seawater and the
lithosphere (adapted from Hein, 2000).
Madeira EEZ, TTR11 Research Cruise - 2001
Cobalt is a strategic metal used in making jet engines, magnetic, wear-resistant,
and high-strength alloys, paints, as a commercially important radioisotope, used as
a tracer and in the production of gamma rays for industrial use.
The U.S. cannot produce sufficient cobalt to meet its needs
Cobalt-rich polymetalic nodules and crusts – Madeira EEZ
S. Muiños (2005)
Fe/Mn polymetalic crusts rich in Cobalt
Madeira EEZ TTR11 Research Cruise - 2001
Fe/Mn polymetalic crusts rich in Cobalt
Madeira EEZ TTR11 Research Cruise - 2001
J. H.Monteiro
Fe/Mn polymetalic crusts rich in Cobalt
Madeira EEZ TTR11 Research Cruise - 2001
Portuguese Margin: Polimetalic nodules and crusts rich in cobalt
Area South Pacific North Pacific Indian Atlantic
Elements (%)
Mn 16.61 12.29 13.56 16.10
Fe 13.92 12.00 15.77 21.82
Ni+Cu+Co (%) 1.213 0.860 0.782 0.715
Area Lion Nameless Josephine Lion Sul
Ni+Cu+Co (%) 1.096 0.960 0.865 0.801
Muinos, 2005
Polymetalic Nodules and Crusts rich in Cobalt – Underwater Video
Madeira EEZ TTR11 Research Cruise - 2005
Phosphorous is necessary for the growth of organisms.
Phosphorites
Phosphate deposits are formed in
submarine terraces in areas where
upwelling generates a high
productivity
Organic wastes and remains
accumulate in the sediment and as
they decay, they release
phosphorus compounds which
precipitate as phosphate nodules.
Normally occur in areas of the
oceans with water depths between
100 and 1000 m. Nodules grow at
the rate of about 1-10mm/1000
years
Onshore reserves are still sufficient. The world consumption, particularly in the
agriculture and the chemical industry is of about 150 million tons per year and
the known reserves should last probably until 2050. Estimated reserves in the
oceans are probably > 50 billion Tons.
Deep Portuguese Basins – Oil Potential (TGN-NOPEC Speculative Survey 2000/01)
20
Deep offshore Basins
Amplitude anomalies
Cortesy J. Pacheco
Deep offshore Portuguese Basins – Direct Hydrocarbon indicators
Cortesy J. Pacheco
Discovered in 1999 (NRL / IGM / UA).
44 mud volcanoes confirmed by coring.
Gas hydrates (4 MVs; evidence in several others
(Bonjardim, Ginsburg, Ct. Arutjunov, Porto MVs).
Gas Hydrates / Mud volcanoes, S. Portuguese Margin and Gulf of Cadiz
Vulcão
de lama Hidratos
de gás
INGMAR (2000-2003); ESF Euromargins MVSEIS (2003-2007), FCT.
MvSeis
Mud volcanoes: Gulf of Cadiz
CAPTAIN ARUTYUNOV MV: Discovered in 2002 (TTR-12)
Thermogenic Gas hydrates recovered (TTR-12, TTR-15 and GAP)
Chemosynthetic fauna (pogonophora)
• Mud breccia; strong H2S smell Clear structural control
Captain Arutyunov MV
TTR-17 June 2008: NEW MUD VOLCANO – SAGRES MUD VOLCANO MvSeis
Chemosynthetic Frenulata
667 GR
Mud breccia clasts
Bonjardim Mud Volcano – TTR-16
June/2006
Gas Hydrates from the S. Portuguese Margin MvSeis
Crystalline solids. 1 cm3 HG 160 cm3 gas.
Mud volcanoes Bonjardim, Ct. Arutjunov & Ginsburg.
Thermogenic gas 81%-88% metano; 12-19% C2-C5.
Oil reservoirs at depth? Huge(?) reserves in the ocean
1 km
75 m
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Porto Mud Volcano – TTR-17 July/2008
Gas Hydrates from the S. Portuguese Margin
MvSeis
Anastasya 2000 Cruise
5 m
Climate change
Carbon sequestration
Anaerobic Methane Oxidation
Geomicrobiology
MDAC occurrences discovered in the Gulf of Cadiz since 1999. Structural control
Methane-derived authigenic carbonates
Anastasya 2000 Cruise
Somoza et al.
Ibérico Diapiric Ridge
SEM Observations of microbial involvement in the precipitation of the dolomite chimneys
Chimney 3463-B2: bacterial filaments Crust 3458-A3: calcified bacterial
filaments over dolomite crystals
Magalhães et al., 2005; Magalhães, 2006 Framboidal pyrite sugesting the presence
of sulfate reduction bacteria
Dumbbell like structures?
MvSeis
V. Magalhães
Solemyidae
Natsushima sp.
Siboglinum sp.
Brachyura und.
Apseudes grossimanus
Alpheidae und. Gnathiidae und.
(new species?)
MvSeis Faunal Communities in the Gulf of Cadiz
Courtesy M. Cunha
Family Siboglinidae, previously 2 different phyla:
Vestimentifera Pogonophora
Both groups occur in reducing environments and tipically
are found at depths below several hundred meters
They lack a functional gut as adults and rely on
endosymbiotic bacteria for nutrition.
The endosymbiotic bacteria are chemoautotrophic sulphide
oxidizers that generate organic material from inorganic
compounds delivered to the trophosome by the host
vascular and celomic systems.
Riftia pachyptila (East Pacific Rise)
Spirobrachia n. sp. (Gulf of Cadiz)
Unexpected diversity of
pogonophoran tubeworms
Morphological and molecular analysis
show 7 different species belonging to 5
different genera (Hilário et al., in prep)
IODP – Deep Ocean Drilling – Deep Biosphere
IODP – Deep Ocean Drilling – Deep Biosphere
Opportunities for Portugal
• Excellent Natural Laboratories in the area under natural
jurisdiction (Hydrothermal Systems and Cold Seeps)
• Mineral and Energy Resources
(massive sulphides, Cobalt-rich crusts, gas, gas hydrates,
oil(?), sand and gravel, phosphorites
Extreme Ecosystems: Hydrothermal systems and Cold Seeps
Deep Biosphere and biotechnology
Açores South Portuguese Margin Madeira-Tore Rise
and Gulf of Cadiz
Deep Margin
Obrigado!
Thank you !
Tusen takk!