Neogene molluscs, shallow marine paleoenvironments, and chronostratigraphy of the Guajira Peninsula, Colombia

Abstract

The Neogene sedimentary fill of the Cocinetas Basin in northern Colombia preserves a rich record of marine invertebrates and can be analyzed in the context of a high-resolution stratigraphy and excellent chronostratigraphy. Molluscan fossils are highly diverse and often well preserved, offering a window into the rapidly changing paleoenvironments and biogeography of northern South America during parts of the Early to Middle Miocene and latest Pliocene to Pleistocene. Before the evolutionary and biogeographic implications of these fossils can be understood, however, their associated depositional environments and geologic ages must be determined. Here, we present preliminary results from paleoenvironmental, biostratigraphic, and strontium isotope chronostratigraphic analyses of sediments and fossils from the Uitpa, Jimol, Castilletes, and Ware formations found in Cocinetas Basin. The basal unit in the Neogene succession, the Uitpa Formation, comprises mudstones redeposited sandstones and molluscs typical of bathyal to outer shelf environments at its base. It is a shallowing-up sequence and is conformable with the overlying Jimol Formation, which comprises coarsegrained lithic calcarenite, coquina, and mudstone that represent a regressive-transgressive-regressive sequence. This sequence includes foreshore and transition zone through lower inner shelf environments, but generally poorly preserved invertebrate assemblages. The conformably overlying Castilletes Formation contains a varied suite of depositional environments with better-developed shell beds and thicker successions of intervening siltstone. A significant unconformity exists between the Castilletes Formation and the overlying Ware Formation, which represents a deltaic to coastal shoreface deposition environment, rich in shallow marine molluscs from a variety of ecotopes. Biostratigraphic assessment and strontium isotopic results from the Jimol and Castilletes formations indicate that these units contain fossils of latest Early Miocene through Middle Miocene age, while those of the Ware are approximately Late Pliocene in age. These results help to place the shallow marine assemblages of Cocinetas Basin into a wider geologic context that aids our understanding of how these faunas relate to the broader evolutionary and biogeographic history of the southern Caribbean during the Neogene. Additionally, the isotope dating and paleoecology of this fauna help to place cooccurring terrestrial and aquatic vertebrate assemblages into a local paleoenvironmental and chronostratigraphic framework.

Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia

“…Rollins (1965), however, accepted that none of the macrofauna collected were diagnostic for age, although they seem to suggest a Pliocene age (following current biostratigraphic knowledge). As noted above, Rollins's (1965) identifications and interpretation are in doubt and are critically assessed by Hendy et al (2015) in this issue. Rollins (1965 p. 59) agreed with Renz (1960) that the base of the Castilletes was in the Miocene, but argued that the top of the unit was Pliocene on the basis of its stratigraphic position (Fig.…”

“…While these 'species' are largely supportive of a Late Miocene age (following current biostratigraphic knowledge), the identifications and interpretation of Rollins (1965) need to be revised. A review of macropalaeontological evidence for the age of the Neogene units of the Cocinetas Basin is provided by Hendy et al (2015) in this issue. The foraminiferal biotas that occur in the lower and upper parts of the Jimol Formation are associated with the Miogypsina günteri and the Miogypsina intermedia biozones (Renz 1960).…”

“…Scale bar is 10 km paleontological collections of variable quality. A review of macropalaeontological evidence for the age of the Neogene units of the Cocinetas Basin is provided by Hendy et al (2015) in this issue.…”

A New Early Miocene (Aquitanian) Elasmobranchii Assemblage from the la Guajira Peninsula, Colombia

“…Previous studies have suggested that the Uitpa Formation was deposited in an open water environment (Becker and Dusenbury, 1958;Rollins, 1965;Thomas, 1972;Hendy et al, 2015). Becker and Dusenbury (1958) The extant species corresponding to such sharks prefer environments with deep-water near the continental slope (Fig.…”

“…While an Oligocene to early Miocene age was proposed by Becker and Dusenbury (1958) based on benthic foraminifera, Lockwood (1965) and Rollins (1965) suggested an early Miocene age (Aquitanian) based on foraminifera and ostracods. More recently, an early Miocene to earliest middle Miocene age was proposed by Hendy et al (2015) based on mollusks and stratigraphic relations. The outcrop studied herein is located close to the Uitpa village ( Fig.…”