2009
DOI: 10.1144/sp328.1
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Tectonic evolution of the Gulf of Mexico, Caribbean and northern South America in the mantle reference frame: an update

Abstract: We present an updated synthesis of the widely accepted 'single-arc Pacific-origin' and 'Yucatán-rotation' models for Caribbean and Gulf of Mexico evolution, respectively. Fourteen palaeogeographic maps through time integrate new concepts and alterations to earlier models. Pre-Aptian maps are presented in a North American reference frame. Aptian and younger maps are presented in an Indo-Atlantic hot spot reference frame which demonstrates the surprising simplicity of Caribbean-American interaction. We use the M… Show more

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Cited by 577 publications
(724 citation statements)
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References 145 publications
(219 reference statements)
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“…The Gibraltar Arc occupies the location of the Mesozoic Atlantic-Tethys connection during the Mesozoic and early Cenozoic and of Atlantic-Mediterranean oceanographic interactions during the late Cenozoic (Maldonado and Nelson, 1999;Vergés and Fernández, 2012.). The Caribbean Arc, in the central western Atlantic Ocean represents the subduction of the western central Atlantic oceanic crust beneath the Caribbean Plate and has been active since the Eocene (DeMets et al, 1990;Pindell and Kennan, 2009;Evain et al, 2013). The development of the Isthmus of Panama closed the oceanographic connection between the Pacific and the Atlantic oceans during the Pliocene and subsequently all oceanographic connections between these two oceans became restricted to the Drake Passage in the Scotia Arc (Lawver and Gahagan, 2003;Coates et al, 2013).…”
mentioning
confidence: 99%
“…The Gibraltar Arc occupies the location of the Mesozoic Atlantic-Tethys connection during the Mesozoic and early Cenozoic and of Atlantic-Mediterranean oceanographic interactions during the late Cenozoic (Maldonado and Nelson, 1999;Vergés and Fernández, 2012.). The Caribbean Arc, in the central western Atlantic Ocean represents the subduction of the western central Atlantic oceanic crust beneath the Caribbean Plate and has been active since the Eocene (DeMets et al, 1990;Pindell and Kennan, 2009;Evain et al, 2013). The development of the Isthmus of Panama closed the oceanographic connection between the Pacific and the Atlantic oceans during the Pliocene and subsequently all oceanographic connections between these two oceans became restricted to the Drake Passage in the Scotia Arc (Lawver and Gahagan, 2003;Coates et al, 2013).…”
mentioning
confidence: 99%
“…The latter occurrences establish that the Atlantic forests had a greater species richness in the recent past, Base map is a composite of maps of Amazonia by Wesselingh et al (2010), the Early Miocene Paranense Sea by Dávila et al (2010Dávila et al ( , 2013 the Early Miocene Patagonian region by Malumián (1999) and Cuitiño and Scasso (2013). For the Caribbean and Central America, see (Pindell et al, 1988;Wadge and Burke, 1993;Iturralde-Vinent and MacPhee, 1999;Kirby et al, 2008;Pindell and Kennan, 2009). Light outlines represent the modern position of land masses.…”
Section: Crown Platyrrhinesmentioning
confidence: 92%
“…maximum subduction, is younger than 114-106 Ma (intrusive age of overprinted trondhjemite) and older than 85 Ma (age of post-HP/LT granitic intrusives), most probably c. 100-90 Ma, a time span during which the northern South American margin was clearly a passive margin (Pindell & Drake, 1998). The assembly of Margaritan protoliths and their HP/LT overprint occurred far to the west, off western northern South America, a scenario completely in accord with the details of the Pacific-origin model as outlined and updated by Pindell & Kennan (2009): Late Jurassic rifting in NW South America led to an Andean intraarc basin, which opened during the Neocomian to form a back-arc basin floored by oceanic sequences (protoliths of La Rinconada tholeiites and associated ultramafic rocks, either underlying the tholeiites or as rifted continental margin), and providing a catchment for sediments (Juan Griego unit) both on the continental margin and the back-arc floor. By 120 Ma, intra-arc extension had ceased and the Caribbean Arc was converging with the western flank of the Antioquia Terrane, closing the back-arc basin by arc-continent collision.…”
Section: Gzg Abt Geochemie Universität Göttingen Germany Mmiriamentioning
confidence: 65%