[First Hit]

Hedberg: Geology of Middle America – the Gulf of Mexico, Yucatan, Caribbean, Grenada and Tobago Basins and Their Margins

Datapages, Inc.Print this page

Evidence for subaerial development of the Caribbean oceanic plateau in the Late Cretaceous and palaeo-environmental implications

Abstract

Accreted oceanic sequences exposed in the Western Cordillera of Colombia provide the first unequivocal evidence for an emergent volcanic phase of the Caribbean oceanic plateau in the Late Cretaceous (~90 Ma). This phase is documented by fallout tuffs with accretionary and armoured lapilli, which are interbedded with lahar deposits that host rounded clasts of basalt (Figures 1 and 2). These sequences record phreatomagmatic eruptions coeval to subaerial erosion on an oceanic island. Their origin is constrained by their whole-rock and clinopyroxene geochemical signatures that are similar to those of submarine lavas and intrusive igneous rocks that form most of the Caribbean plateau (Figure 1a). These results, which include the first known occurrence of lahar deposits on top of an oceanic plateau, complement previous in situ lithostratigraphic observations from the Ontong Java plateau and Shatsky rise. They suggest that syn-volcanic emergence of oceanic plateaus was a common process in the Pacific during the Mesozoic, which could have led to rapid releases of large volume of magmatic gases and aerosols in the atmosphere. In addition, we show that the emergence of the Caribbean plateau in the Late Cretaceous occurred in a complex tectonic setting associated with its migration from the Pacific to its present inter-American location. An arc-derived tuff bed within the studied subaerial plateau sequences (this study) and regional geological constraints (Wright and Wyld, 2011; RodrÌguez and Arango, 2013; Weber et al. 2015; Jaramillo et al., 2017) show that this migration involved interaction with subduction zones at least ~20 m.yr. before collision of the plateau with South America and arc initiation on the southwestern edge of the Caribbean Plate (Figure 3). This tectonic evolution and the formation of island(s) on top of the Caribbean plateau suggest that the inter-American seaway became largely obstructed ca. 90 Ma. We propose that this significantly reduced the flow of Pacific oxygenated bottom waters into the juvenile Atlantic, and so promoted anoxia in the Atlantic basin in the Turonian-Coniacian (OAE-3 event). This also suggests that strings of islands have existed across the inter-American seaway since the Late Cretaceous, and this likely facilitated inter-American migration of terrestrial organisms in the Cretaceous-Palaeogene.