In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 22, No. 7 ( 2021-07)
Kurzfassung:
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
Materialart:
Online-Ressource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2020GC009369
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2021
ZDB Id:
2027201-7
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