<abstract xml:lang="en" xmlns="http://www.w3.org/1999/xhtml"><p>The Tanais Palaeobay was located in the northern periphery of the eastern Paratethys Sea during the Late Miocene. New data from the Safianovo section (Rostov Dome, South-West of Russia) confirm that skeletal limestones (coquinites) of the Merzhanovskaja Formation belong to the <italic>Congeria (Andrusoviconcha) amygdaloides navicula</italic> Zone of the upper Upper Maeotian (the Maeotian is a regional chronostratigraphic unit of the Upper Miocene). Correlation of reference sections of these Upper Maeotian deposits within the Rostov Dome results in pattern of the palaeobay transgression, which was punctuated. The relative importance of local and global controls on this trangsression is not yet clear.</p></abstract>

The Tanais Palaeobay was located in the northern periphery of the eastern Paratethys Sea during the Late Miocene. New data from the Safianovo section (Rostov Dome, South-West of Russia) confirm that skeletal limestones (coquinites) of the Merzhanovskaja Formation belong to the Congeria (Andrusoviconcha) amygdaloides navicula Zone of the upper Upper Maeotian (the Maeotian is a regional chronostratigraphic unit of the Upper Miocene). Correlation of reference sections of these Upper Maeotian deposits within the Rostov Dome results in pattern of the palaeobay transgression, which was punctuated. The relative importance of local and global controls on this trangsression is not yet clear.

Stratigraphic evidence of a Late Maeotian (Late Miocene) punctuated transgression in the Tanais Palaeobay (northern part of the Eastern Paratethys, South-West Russia)

Division of Mineralogy and Petrography, Geology and Geography Faculty, Southern Federal University, Zorge Street 40, Rostov-na-Donu, 344090, Russian Federation

P. O. Box (a/jashik) 7333, Rostov-na-Donu, 344056, Russian Federation

Geologos

The Tanais Palaeobay was located in the northern periphery of the eastern Paratethys Sea during the Late Miocene. New data from the Safianovo section (Rostov...

Stratigraphic evidence of a Late Maeotian (Late Miocene) punctuated transgression in the Tanais Palaeobay (northern part of the Eastern Paratethys, South-West Russia)

Pubblicato online: 22 ott 2010

Pagine: 169 - 181

DOI: https://doi.org/10.2478/v101118-009-0011-0

Parole chiave
Late Miocene, Late Maeotian, Eastern Paratethys, transgression, bivalves

This content is open access.

Stratigraphic evidence of a Late Maeotian (Late Miocene) punctuated transgression in the Tanais Palaeobay (northern part of the Eastern Paratethys, South-West Russia)

Pubblicato online: 22 ott 2010

Pagine: 169 - 181

DOI: https://doi.org/10.2478/v101118-009-0011-0

Parole chiaveLate Miocene, Late Maeotian, Eastern Paratethys, transgression, bivalves

This content is open access.

Parole chiave
Late Miocene, Late Maeotian, Eastern Paratethys, transgression, bivalves