Eco-biostratigraphic advances on late Quaternary geochronology and palaeoclimate: the marginal Gulf of Mexico analogue

This study combines high-resolution planktonic foraminiferal eco-biostratigraphy and palaeoclimatic data from the high-sedimentation-rate core JPC-26 from the northwestern margin of the Gulf of Mexico (GoM). The eco-biozones recognized (GOMPFE1-12) being correlated with published Mg/Ca-based sea sur...

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Bibliographic Details
Published in:Geological Quarterly
Main Authors: Antonarakou, Assimina, Kontakiotis, George, Karageorgis, Aristomenis P., Besiou, Eva, Zarkogiannis, Stergios, Drinia, Hara, Mortyn, Graham P., Tripsanas, Eftymis
Other Authors: No funding for this work
Format: Article in Journal/Newspaper
Language:English
Published: Polish Geological Institute-National Research Institute 2019
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Online Access:https://gq.pgi.gov.pl/article/view/26094
https://doi.org/10.7306/gq.1457
Description
Summary:This study combines high-resolution planktonic foraminiferal eco-biostratigraphy and palaeoclimatic data from the high-sedimentation-rate core JPC-26 from the northwestern margin of the Gulf of Mexico (GoM). The eco-biozones recognized (GOMPFE1-12) being correlated with published Mg/Ca-based sea surface temperatures. This updated palaeoclimatic and stratigraphic reference record facilitates correlations with the Greenland ice core events and their climatic relationships, and also provides a solid stratigraphic framework for correlations with other palaeoclimatic and palaeoceanographic records in the circum-GOM/Caribbean region. This multidisciplinary approach underlines the utility of supporting conventional dating methodologies with different constraints, and further reveals a powerful tool for reliably correlating marine records between comparable deep-sea marginal settings and coeval sequences of this region