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Gorringe Bank

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Gorringe Bank
NameGorringe Bank
LocationNorth Atlantic Ocean
Coordinates31°46′N 11°20′W
CountryPortugal (Exclusive Economic Zone)
TypeSubmarine mountain / seamount
Highest pointGettysburg Seamount (approximately 5–10 m below sea level)

Gorringe Bank is a prominent submarine ridge in the northeastern Atlantic Ocean located off the coast of Portugal and southwest of Lisbon. The feature lies near maritime boundaries involving Portugal, Spain, and international waters adjacent to the Azores and the Canary Islands. It is notable for abrupt bathymetric relief, complex seamount morphology, and significance for fisheries, marine biodiversity, and maritime navigation.

Geography and geology

The ridge occupies a position between the continental margin off Iberia and the mid-Atlantic domain near the Mid-Atlantic Ridge, rising from abyssal plains adjacent to the Setubal Canyon and the Gulf of Cadiz region. Bathymetric surveys conducted by vessels such as HMS Challenger (1872)-class research ships and modern platforms including NOAA Ship Okeanos Explorer and RV Pourquoi Pas? show pinnacles like Gettysburg Seamount and rocky outcrops that approach shallow depths comparable to submerged features near Porto Santo and Madeira. Rock samples recovered during dives using Alvin (DSV)-style submersibles and remotely operated vehicles from institutions including the Woods Hole Oceanographic Institution and the Portuguese Institute of the Sea and Atmosphere indicate lithologies similar to obducted ophiolite complexes found in areas such as Sierra de Grazalema and Betic Cordillera exposures.

Stratigraphic and petrological analyses associate the bank with magmatic and tectonic processes akin to those that formed structures like the Azores Triple Junction and Iberian Margin highs. The morphology presents terraces, scarps, and knolls that resemble features mapped on the Rockall Plateau and the Gorringe Bank vicinity by international collaborations including teams from Institut Français de Recherche pour l'Exploitation de la Mer and Instituto Hidrográfico (Portugal).

Tectonic setting and formation

Situated near the interaction of the Eurasian Plate and the African Plate, the feature is influenced by plate boundaries comparable to the Alboran Sea and the Gibraltar Arc. Geophysical data from seismic reflection profiles collected by research groups at ETH Zurich and GEOMAR Helmholtz Centre for Ocean Research Kiel reveal thrust faults, folded strata, and mantle-derived igneous rocks consistent with obduction processes seen in the Apennines and the Troodos Ophiolite of Cyprus. The tectonic history aligns with episodic convergence episodes that also shaped the Betic-Rif arc and the Atlas Mountains.

Hypotheses for genesis include uplift related to the reactivation of ancient fracture zones similar to the Gloria Fault and magmatic intrusions linked to mantle upwelling beneath the Azores hotspot. Paleogeographic reconstructions by teams from University of Lisbon and University of Southampton place formation events in the late Cretaceous to Cenozoic intervals with seismicity patterns comparable to events recorded near Madeira and the Canary Islands.

Oceanography and ecosystems

The bank modifies regional circulation by interacting with the North Atlantic Current and the Portugal Current, producing upwelling and retention zones analogous to processes observed at Farn Ridge and Rockall Trough. These hydrodynamic effects enhance primary productivity driven by phytoplankton assemblages documented in studies by researchers at Sorbonne University and Station Biologique de Roscoff and support rich zooplankton communities similar to those near Cape Verde seamounts.

Habitat complexity on rocky substrates supports sessile organisms such as gorgonians and sponges studied by expeditions from Natural History Museum, London and the Museu Nacional de História Natural e da Ciência. Mobile fauna include aggregation of demersal fishes comparable to European hake, blue shark migrations recorded by tagging programs from Plymouth Marine Laboratory, and cetacean presence akin to sightings of sperm whale and common dolphin recorded by observers from WWF and Oceana. Cold-water coral communities bear resemblance to those on the Porcupine Bank and the Northeast Atlantic mounds, while invasive species assessments reference taxa monitored by the International Council for the Exploration of the Sea.

Human history and exploration

Nineteenth-century hydrographic charts from institutions such as the Admiralty first noted the ridge following surveys reminiscent of voyages by HMS Challenger (1872) and USS Dolphin (1821). Naval incidents including groundings and sonar anomalies attracted attention from navies like the Royal Navy and research efforts by the Portuguese Navy Hydrographic Institute. Twentieth-century scientific expeditions involving universities including University of Lisbon, University of Oxford, and University of Hamburg advanced bathymetric mapping using tools like multibeam echo sounder systems developed by companies such as Kongsberg Maritime and institutions including NOAA.

Modern exploration employs submersibles and remotely operated vehicles from organizations such as Schmidt Ocean Institute and Monterey Bay Aquarium Research Institute, while international collaborations, including projects funded by the European Commission and the Horizon 2020 framework, have focused on biodiversity inventories, geological sampling, and hydroacoustic monitoring. Archaeological surveys reference shipping routes tied to historical ports like Lisbon and incidents during periods involving Age of Discovery voyages by fleets from Spain and Portugal.

Marine resources and conservation

The bank supports valuable demersal fisheries managed under regulations from bodies such as the European Union fisheries framework and monitored by agencies including the Food and Agriculture Organization regional offices and the International Council for the Exploration of the Sea. Exploitation of resources parallels concerns faced at other seamount fisheries like those off Azores and has prompted assessments by conservation organizations such as IUCN and BirdLife International.

Conservation measures considered include marine protected area proposals advanced by researchers at University of the Azores and policymakers in Lisbon with models informed by successful sites like the Vulnerable Marine Ecosystems designations overseen by United Nations bodies and regional Fisheries Management Organizations. Threats identified by studies from Greenpeace and WWF include overfishing, deep-sea trawling impacts similar to documented damage on Skomer-type reefs, and climate-driven changes affecting thermohaline circulation documented by IPCC assessments. Ongoing monitoring leverages partnerships among institutions including MARE (Marine and Environmental Sciences Centre) and Biodiversity Data Journal contributors to balance sustainable use and biodiversity protection.

Category:Seamounts of the Atlantic Ocean