In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 22, No. 7 ( 2021-07)
Abstract:
The early Maeotian transgression (7.6–7.4 Ma) started with an incursion of Eastern Paratethys (i.e., Black Sea) waters into the Dacian Basin The Maeotian‐Pontian transition (6.3–5.9 Ma) records a second incursion of Eastern Paratethys followed by a short influx of marine (Mediterranean) waters The Bosphorian transgression at ca. 5.5 Ma was probably related to the increased influence of Pannonian and local river water in the Dacian Basin
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2020GC009369
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
2027201-7
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