@article{3069067,
    title = "Eco-biostratigraphic advances in late quaternary geochronology and palaeoclimate: The marginal Gulf of Mexico analogue",
    author = "Antonarakou, A. and Kontakiotis, G. and Karageorgis, A.P. and Besiou, E. and Zarkogiannis, S. and Drinia, H. and Mortyn, G.P. and Tripsanas, E.",
    journal = "QUARTERLY GEOLOGICAL NOTES",
    year = "2019",
    volume = "63",
    number = "1",
    pages = "178-191",
    publisher = "POLISH GEOLOGICAL INSTITUTE",
    issn = "0584-3219",
    doi = "10.7306/gq.1457",
    keywords = "biostratigraphy;  climate variation;  correlation;  deep-sea sediment;  geochronology;  Holocene;  late glacial;  paleoceanography;  paleoclimate;  planktonic foraminifera;  Quaternary, Atlantic Ocean;  Gulf of Mexico",
    abstract = "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. © 2019 Polish Geological Institute. All rights reserved."
}