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Puerto Rico Bank

Coordinates:18°17′00″N65°36′00″W / 18.28333°N 65.60000°W /18.28333; -65.60000
From Wikipedia, the free encyclopedia
Insular shelf and carbonate platform comprising Puerto Rico and the Virgin Islands
Puerto Rico Bank
Puerto Rico Bank and major surrounding
geological features
Puerto Rico Bank is located in Caribbean
Puerto Rico Bank
Puerto Rico Bank
Location within the Caribbean
Geography
LocationCaribbean
Coordinates18°17′00″N65°36′00″W / 18.28333°N 65.60000°W /18.28333; -65.60000
ArchipelagoPuerto Rico
Virgin Islands
Area21.000 km2 (8.108 sq mi)
Administration
Islands and Cays140[a]
Islands and Cays52[b][1]
Islands and Cays36[1]

ThePuerto Rico Bank (PRB) (Spanish:Banco de Puerto Rico), also known as thePuerto Rican Bank (PRB), is acarbonate platform andinsular shelf comprising thearchipelagos ofPuerto Rico[a] and theVirgin Islands,[b] located between theGreater Antilles and theLesser Antilles in the northeasternCaribbean.[2][3][4][5][6][7][8][9] Lastsubaerially exposed from theLast Glacial Maximum in theLast Glacial Period of theLate PleistoceneAge to theNorthgrippianAge of theHoloceneEpoch, the bank connected Puerto Rico and the Virgin Islands into a singlelandmass untilsea level rise fragmented it into the present-day islands between 10,000 and 7,000 yearsBefore Present (8,050 and 5,050 yearsBefore Common Era).[10][11][12][13][14][15] It is within thePuerto Rico–Virgin Islands microplate between theNorth American plate andCaribbean plate.

Name

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Most commonly known as thePuerto Rico Bank andPuerto Rican Bank, the bank is named after the largest island within its limits, the eponymousmain island of the archipelago ofPuerto Rico. The part of the bank covering theVirgin Islands is occasionally referred to as theVirgin Bank.[16][17][18]

Location

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The demarcated banks of Puerto Rico, Anguilla,Saba, Saint Kitts, Barbuda, Monserrat, and Guadeloupe on nautical chart, 1857[19][20][14]

Separated from theGreater Antilles by theMona Passage and from theLesser Antilles by theAnegada passage in the northeasternCaribbean Sea of theAtlantic Ocean, the Puerto Rico Bank compromises themain island ofPuerto Rico, theSpanish Virgins Islands ofVieques andCulebra, theU.S. Virgin Islands ofSaint Thomas andSaint John, and theBritish Virgin Islands ofJost Van Dyke,Tortola,Virgin Gorda, andAnegada. It includes all surrounding minor islands and cays of each one of the aforementioned major islands. The westernmost islands ofDesecho,Mona, andMonito of Puerto Rico, and the southernmost island ofSaint Croix of the U.S. Virgin Islands do not form part of the bank, as they lie on their own platforms.[21][22]

Extent

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Including the island within the Puerto Rico Bank, it measures 350km (218mi) in length and 40 to 80 km (25 to 50 mi) in width.[4][3] Around themain island ofPuerto Rico, the bank is 2 to 15 km (1.2 to 9.3 mi) wide from the southeast to the southwest, over 15 to 2 km (9.3 to 1.2 mi) wide from the southwest to northwest, and less than 2 km (1.2 mi) wide from the northwest to the northeast.[23] Around thearchipelago of the Virgin Islands, the bank is 40 to 65 km (25 to 40 mi) wide.

The Puerto Rico Bank is less than 79m (260ft) in depth, with the portion connecting all the islands being less than 40 metres (130 feet) in depth.[24][25] All islands and cays in the archipelago of Puerto Rico, including Vieques and Culebra, are connected less than 25 metres (82 feet). Similarly, the main islands of the U.S. Virgin Islands and the British Virgin Islands are connected by less than 25 metres (82 feet).[26][11][27][28][29][30][31] The Spanish Virgin Islands of Vieques and Culebra and the American and British islands are separated by a narrowstrait, the Virgin Passage, which is 16 km (10 m) in length and 20 to 32 m (66 to 105 ft) in depth.[16]

With anarea of 21,000 km2 (8,100 sq mi),[4][32] it was last fully exposed during theLast Glacial Maximum when the sea level was 120 metres (390 feet) lower than the present-day.[15] The bank was inundated bysea level rise during theLate Pleistocene andEarly Holocene, losingsubaerial connection the main island of Puerto Rico and the Spanish Virgin Islands with the U.S. Virgin Islands and British Virgin Islands 10,000 to 8,000 yearsBefore Present ago (8,050 to 6,050 yearsBefore Christ ago). The main island of Puerto Rico with Vieques, and the U.S. Virgin Islands and the British Virgin Islands with each other lost their land connection 7,000 years BP ago (5,050 years BC ago), while the main island of Puerto Rico with some of its minorislands, cays, and islets 3,000 BP years ago (1,050 BC years ago).[10][11]

Notes

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  1. ^abExcluding the westernmost islands ofDesecheo,Mona, andMonito, which are politically part of thearchipelago of Puerto Rico but are not geologically part of the Puerto Rico Bank, as they lie on their own platforms.
  2. ^abExcluding the southernmost island ofSaint Croix, which is politically part of theVirgin Islands but is not geologically part of the Puerto Rico Bank, as it lies on its own platform.

References

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  1. ^ab"Where is the U.S. Virgin Islands: Geography".Virgin Islands. Retrieved2024-10-05.
  2. ^"Marine Regions · Puerto Rico Trench (Trench)".www.marineregions.org. Retrieved2024-09-26.
  3. ^ab"Geology and Hydrogeology of the Caribbean Islands Aquifer System of the Commonwealth of Puerto Rico and the U.S. Virgin Islands"(PDF).U.S. Geology Survey. Retrieved8 October 2024.
  4. ^abc"Archipelagic genetics in a widespread Caribbean anole"(PDF).Wiley Online Library. Retrieved8 October 2024.
  5. ^"The Bunce Fault and Strain Partitioning in the Northern Lesser Antilles".ResearchGate. Retrieved8 October 2024.
  6. ^"Sea level, topography and island diversity: Phylogeography of the Puerto Rican Red-eyed Coquí, Eleutherodactylus antillensis".ResearchGate. Retrieved8 October 2024.
  7. ^"The polyphased tectonic evolution of the Anegada Passage in the northern Lesser Antilles subduction zone".ResearchGate. Retrieved24 September 2024.
  8. ^"Exploring Puerto Rico's Seamounts, Trenches, and Troughs: Background: Mission Plan".NOAA Office of Ocean Exploration and Research. Retrieved2024-08-27.
  9. ^"Island lists of West Indian amphibians and reptiles"(PDF).Florida Museum of Natural History. pp. 137–147.
  10. ^ab"Biogeography of Puerto Rican Bank".ResearchGate. Retrieved8 October 2024.
  11. ^abc"Boraginaceae Varronia rupicola (Urb.) Brtton : biogeog- raphy, systematic placement and conservation genetics of a threatened species endemic to the Caribbean"(PDF).Birkbeck Institutional Research Online. pp. 86–87. Retrieved8 October 2024.
  12. ^"The beetles of the Lesser Antilles (Insecta, Coleoptera): diversity and distributions"(PDF).DigitalCommons. pp. 10 and 16. Retrieved8 October 2024.
  13. ^"Por el camino verde: Long-term tropical socioecosystem dynamics and the Anthropocene as seen from Puerto Rico".Research Gate. Retrieved24 August 2024.
  14. ^ab"Bats of St. Vincent, Lesser Antilles".ResearchGate. Retrieved8 October 2024.
  15. ^ab"The Late Pleistocene Human Settlement of Interior North America: The Role of Physiography and Sea Level Change".ResearchGate. Retrieved8 October 2024.
  16. ^ab"Virgin Islands"(PDF).National Oceanic and Atmospheric Administration (NOAA). Retrieved8 October 2024.
  17. ^"Archaeological reconnaissance of the Island of St. John, United States Virgin Islands".original-ufdc.uflib.ufl.edu. p. 2. Retrieved2024-10-10.
  18. ^"Bats of Guana, British Virgin Islands".AMNH Library Digital Repository. Retrieved8 October 2024.
  19. ^fig2 361960623 "Coexistence of Adjacent Siliciclastic, Carbonate, and Mixed Sedimentary Systems: An Example From Seafloor Morphology in the Northern Lesser Antilles Forearc".ResearchGate. Retrieved8 October 2024.{{cite web}}:Check|url= value (help)
  20. ^fig6 277893074 "Genetic Evidence of Hybridization between the Endangered Native Species Iguana delicatissima and the Invasive Iguana iguana (Reptilia, Iguanidae) in the Lesser Antilles: Management Implications".ResearchGate. Retrieved8 October 2024.{{cite web}}:Check|url= value (help)
  21. ^Schärer-Umpierre, Michelle T.; Mateos-Molina, Daniel; Appeldoorn, Richard; Bejarano, Ivonne; Hernández-Delgado, Edwin A.; Nemeth, Richard S.; Nemeth, Michael I.; Valdés-Pizzini, Manuel; Smith, Tyler B. (2014-01-01), Johnson, Magnus L.; Sandell, Jane (eds.),"Chapter Four - Marine Managed Areas and Associated Fisheries in the US Caribbean",Advances in Marine Biology, Marine Managed Areas and Fisheries, vol. 69, Academic Press, pp. 129–152,doi:10.1016/B978-0-12-800214-8.00004-9, retrieved2024-10-10
  22. ^"Island lists of West Indian amphibians and reptiles".ResearchGate. Retrieved8 October 2024.
  23. ^"A 50-year Reconstruction of Fisheries Catch in Puerto Rico"(PDF). Retrieved8 October 2024.
  24. ^"Baroclinic Coupling Improves Depth‐Integrated Modeling of Coastal Sea Level Variations Around Puerto Rico and the U.S. Virgin Islands".ResearchGate. March 2019. Retrieved4 October 2024.
  25. ^"PR/USVI Prioritization Mapping Inventory".noaa.hub.arcgis.com. Retrieved2024-10-09.
  26. ^"Baroclinic Coupling Improves Depth-Integrated Modeling of Coastal Sea Level Variations Around Puerto Rico and the U.S. Virgin Islands".ResearchGate. Retrieved8 October 2024.
  27. ^CARICOOS."CariCOOS".www.caricoos.org. Retrieved2024-10-09.
  28. ^"New species and new records of Cumacea (Crustacea: Peracarida: Cumacea) from mesophotic reefs of Puerto Rico and U.S. Virgin Islands, Caribbean Sea".Research Gate. Retrieved24 August 2024.
  29. ^"Potential Structuring Forces on a Shelf Edge Upper Mesophotic Coral Ecosystem in the US Virgin Islands".ResearchGate. Retrieved8 October 2024.
  30. ^"Physical drivers of community structure and growth among mesophotic coral ecosystems surrounding St. Thomas, U. S. Virgin Islands".ResearchGate. Retrieved8 October 2024.
  31. ^"Radiocarbon in otoliths of tropical marine fishes: Reference ΔC chronology for north Caribbean waters".ResearchGate. Retrieved8 October 2024.
  32. ^"Linking micro- and macroevolutionary perspectives to evaluate the role of Quaternary sea-level oscillations in island diversification"(PDF).University of Michigan Library. Retrieved8 October 2024.
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