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The missing piece – New insights to comprehend enigmatic Miocene palaeoceanography of the Mediterranean Sea using the Nd isotopic record

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F24%3A00588120" target="_blank" >RIV/67985831:_____/24:00588120 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11310/24:10493151

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S0012821X24003133?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0012821X24003133?via%3Dihub</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.epsl.2024.118880" target="_blank" >10.1016/j.epsl.2024.118880</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The missing piece – New insights to comprehend enigmatic Miocene palaeoceanography of the Mediterranean Sea using the Nd isotopic record

  • Original language description

    The evolution of the Mediterranean-Paratethys marine system during the Miocene represents one of the crucial milestones in the Earth's oceans history. It fundamentally affected the climate evolution not just in Europe and the adjacent continents, but also on a global scale. The progressive transition of the Mediterranean-Paratethys system from a latitudinal marine domain connecting two main Earth's oceans to a modern-day enclosed setting happened mainly from the Burdigalian (∼16–18 Ma) to Serravallian period (∼13.8–12.6 Ma). It triggered a complex interplay of palaeoceanographic events such as overturns in water circulation regimes that affected the large-scale palaeoclimatic settings. Here, we present 3D palaeoceanographic models from the late Burdigalian to the Serravallian that are based on a comprehensive 143Nd/144Nd dataset containing 59 individual measurements. Our results imply that the first indications of separation between the western and eastern parts of the Mediterranean occurred during the late Langhian (∼16–13.8 Ma) and were linked to the pronounced circulation overturn. The modern-day setting with the characteristic εNd signatures for the Western and Eastern Mediterranean developed during the Serravallian. Altogether, our set of models demonstrates the dynamics of the two-step closure of the Indian-Atlantic gateway and the palaeoceanographic evolution of this area during the middle Miocene.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10502 - Oceanography

Result continuities

  • Project

    <a href="/en/project/GA20-05872S" target="_blank" >GA20-05872S: The Langhian Mediterranean-Paratethys enigma: hydrography based on Nd isotopes proxy on foraminifera revealing changes in paleoceanography</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Earth and Planetary Science Letters

  • ISSN

    0012-821X

  • e-ISSN

    1385-013X

  • Volume of the periodical

    642

  • Issue of the periodical within the volume

    September

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    10

  • Pages from-to

    118880

  • UT code for WoS article

    001269545600001

  • EID of the result in the Scopus database

    2-s2.0-85198251799