Revision of the endemic dinoflagellate cyst genus Pontiadinium Stover & Evitt, 1978 from Lake Pannon and the Paratethys realm (Late Miocene–Early Pliocene, Central Europe)

Palynology ◽  
2021 ◽  
Author(s):  
Viktória Baranyi ◽  
Peta J. Mudie ◽  
Imre Magyar ◽  
Ádám Kovács ◽  
Mária Sütő-Szentai ◽  
...  
Keyword(s):  
Central Europe ◽  
Late Miocene ◽  
Lake Pannon ◽  
Early Pliocene ◽  
Dinoflagellate Cyst

Mendicodinium mataschenensis: a new endemic dinoflagellate cyst from the Late Miocene (Tortonian) of Lake Pannon (Austria)

Palynology ◽  
2013 ◽  
Vol 37 (1) ◽  
pp. 35-47 ◽  
Author(s):  
Ali Soliman ◽  
Susanne Feist-Burkhardt ◽  
Mathias Harzhauser ◽  
Andrea K. Kern ◽  
Werner E. Piller
Keyword(s):  
Late Miocene ◽  
Lake Pannon ◽  
Dinoflagellate Cyst

Paleogeographic evolution of the Late Miocene Lake Pannon in Central Europe

1999 ◽  
Vol 147 (3-4) ◽  
pp. 151-167 ◽  
Author(s):  
Imre Magyar ◽  
Dana H Geary ◽  
Pál Müller
Keyword(s):  
Central Europe ◽  
Late Miocene ◽  
Lake Pannon

scholarly journals Dinoflagellate cysts from the Pannonian (late Miocene) "white marls" in Pécs-Danitzpuszta, southern Hungary

2021 ◽  
Vol 151 (3) ◽  
pp. 267-274
Author(s):  
Krešimir Krizmanić ◽  
Krisztina Sebe ◽  
Imre Magyar
Keyword(s):  
Late Miocene ◽  
Depositional Environment ◽  
Middle Miocene ◽  
Dinoflagellate Cysts ◽  
Middle Segment ◽  
Lake Pannon ◽  
Dinoflagellate Cyst ◽  
Upper Miocene ◽  
Reference Section

Dinoflagellate-cyst based biostratigraphy is an important tool in the stratigraphical subdivision and correlation of the Neogene Lake Pannon deposits. A total of 66 palynological samples were investigated from the Pannonian (upper Miocene) marl succession exposed in the Pécs-Danitzpuszta sand pit in order to evaluate the biostratigraphical assignment and constrain the age of the strata. Earlier attempts to recover dinoflagellate cysts from this important reference section had failed. In our material, six samples contained well-preserved palynomorphs. One sample from the lower part of the succession (D25) contained a probably reworked middle Miocene assemblage. Samples from the middle segment of the succession (D3, D2, D1) indicate the Pontiadinium pecsvaradensis Zone (ca. 10.8 to 10.6 Ma). Samples from the top of the marl (D219, D221) did not give additional stratigraphic information (P. pecsvaradensis Zone or younger). The palynofacies of samples D3 to D221 indicates a relatively distal, calm, occasionally oxygen-deficient, probably deep depositional environment.

scholarly journals Upper Miocene Pannonian sediments from Belgrade (Serbia): new evidence and paleoenvironmental considerations

2011 ◽  
Vol 62 (3) ◽  
pp. 267-278 ◽  
Author(s):  
Ljupko Rundić ◽  
Meri Ganić ◽  
Slobodan Knežević ◽  
Ali Soliman
Keyword(s):  
Late Miocene ◽  
Pannonian Basin ◽  
Point Of View ◽  
Lake Pannon ◽  
Dinoflagellate Cyst ◽  
Upper Miocene ◽  
The North ◽  
New Evidence ◽  
Stratigraphic Range ◽  
Ostracod Species

Upper Miocene Pannonian sediments from Belgrade (Serbia): new evidence and paleoenvironmental considerationsThe Late Miocene sublittoral marls of the Pannonian Stage (the long-lived Lake Pannon) were studied. From neotectonic point of view, the investigated area represents a natural border between two different morphostructural domains: the Pannonian Basin to the north and the Peri-Pannonian Realm to the south. More than 20 mollusc and 34 ostracod species were identified which indicate the upper part of the Lower Pannonian and the lower part of the Middle Pannonian ("Serbian") predominantly. The identified dinoflagellate cyst assemblage (21 taxa) hinders assignment of the studied samples to a Pannonian substage but supports the high endemism of the Pannonian flora. The lithostratigraphical, paleontological, and paleoecological analyses indicate a mesohaline (8-16 ‰), sublittoral (<90 m deep) environment of the early Lake Pannon. The estimated stratigraphic range for the investigated deposits is 9.8-11.4 Ma.

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