Neodymium isotopes of central Mediterranean phosphatic hardgrounds reveal Miocene paleoceanography

نویسندگان

چکیده

Abstract Understanding the causes of formation hardgrounds provides insights on oceanographic evolution a basin. Phosphate-rich hardground interrupted carbonate ramp deposition in Mediterranean during Miocene. We analyzed εNd record three central to identify origin phosphate-rich waters that formed them within frame Miocene paleoceanographic evolution. The Nd isotopes suggest eastern deep were controlled by runoff, contrast Atlantic and Indian Ocean waters. This isotope attests weakening circulation due closure Gateway. Limited exchange with shallow seawater led long residence times for indicates role upwelling phosphate shows influence global climate change local conditions.

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ژورنال

عنوان ژورنال: Geology

سال: 2022

ISSN: ['0091-7613', '1943-2682']

DOI: https://doi.org/10.1130/g50118.1