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Maria Marino

Researcher at University of Bari

Publications -  83
Citations -  1685

Maria Marino is an academic researcher from University of Bari. The author has contributed to research in topics: Interglacial & Marine isotope stage. The author has an hindex of 26, co-authored 74 publications receiving 1496 citations.

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Calcareous plankton dissolution pattern and coccolithophore assemblages during the last 600 kyr at ODP Site 1089 (Cape Basin, South Atlantic): paleoceanographic implications

TL;DR: Coccolithophore assemblages at ODP Site 1089 in the southern Cape Basin were used to reconstruct surface-water conditions for the late Quaternary (Marine Isotope Stages (MIS) 1^15) in a region of strong hydrographic gradients in the southeast Atlantic.
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Calabrian and Ionian: A proposal for the definition of Mediterranean stages for the Lower and Middle Pleistocene

TL;DR: In this paper, a proposal is presented to formalize regional stages for the Lower Pleistocene (Calabrian) and for the Middle Plio and Ionian (Ionian) in Italy.
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Middle Eocene to early Oligocene calcareous nannofossil stratigraphy at Leg 177 Site 1090

TL;DR: In this paper, an interpretation of shipboard magnetic inclination data recognizes magnetic chrons from C12 to C19, according to the geomagnetic polarity time scale of Berggren et al.
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Rock magnetism and palaeomagnetism of the Montalbano Jonico section (Italy): evidence for late diagenetic growth of greigite and implications for magnetostratigraphy

TL;DR: The Montalbano Jonico (MJ) section, cropping out in Southern Italy, represents a potential candidate to define the Lower/Middle Pleistocene boundary and it has been proposed as a suitable Global Stratotype Section and Point (GSSP) of the Ionian Stage as mentioned in this paper.
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Proposal for Pliocene and Pleistocene land–sea correlation in the Italian area

TL;DR: In this article, a correlation between calcareous plankton (foraminifera and nannofossils) and terrestrial (pollen and mammal fauna) bioevents in Italy and Mediterranean Sea, through the last 3.3 million years, within a standard chronostratigraphical time scale was found.