Late Neogene chronostratigraphy and integrated paleoecological trends in the southwestern Caribbean Sea

RODRÍGUEZ, GUILLERMO; GUERSTEIN, G. RAQUEL; DE LA PARRA, FELIPE; MARTÍNEZ, JHONATAN; PINZÓN, DIEGO; PRÁMPARO, MERCEDES B.; PÉREZ PANERA, JUAN P.; VENTO, BÁRBARA; RINCÓN-MARTÍNEZ, DANIEL; RESTREPO, SANDRA; VARGAS, MARIA CAROLINA

MARINE MICROPALEONTOLOGY

ELSEVIER SCIENCE BV

Año: 2022 vol. 172

0377-8398

Palynology of the Neogene marine stratigraphic sequences in tropical latitudes is poorly studied Most studies focus on lower to middle Miocene deposits in the Caribbean, emphasizing the biostratigraphic value of dinoflagellate cysts. The palynological and calcareous nannofossil analysis of 50 samples from DSDP Hole 502A and their integration with the paleomagnetic and planktonic foraminifera data reveal a detailed and reliable chronostratigraphic framework, and the interpretation of the paleobathymetric and paleoenvironmental evolution of the sequence. Fossil content in a continuous late Tortonian to late Gelasian (~7.56-1.80 Ma) sequence of deep marine sediments serves to calibrate ages of dinoflagellate cysts, and comparison with high latitude records reveals synchronous (Operculodinium janduchenei, Selenopemphix dionaeacysta, Barssidinium taxandrianum, and Lejeunecysta interrupta) and asynchronous events (Quadrina? condita) with biostratigraphic potential for the southwestern Caribbean Sea. Our results highlight the importance of analyzing continental palynomorphs in deep-marine deposits to increase the temporal resolution of future palynostratigraphic schemes. Micropaleontogical data indicate a lower bathyal?abyssal environment and four paleoceanographic settings defined by changes in surface water productivity. These intervals fluctuate from mesotrophic-oligotrophic (~7.56?6.31 Ma) to eutrophic (~6.18?4.98 Ma), oligotrophic (~4.74?3.41 Ma), and mesotrophic surface water conditions (~3.26?1.80 Ma). Changes in trophic conditions are strongly related to the paleoceanographic reorganization associated with the constriction and complete closure of the Central American Seaway, seasonal upwelling episodes, and the input of terrigenous organic matter probably transported from southern Central America and northern South America by turbidity currents.