TY  - JOUR
AU  - Hadi, Mehdi
AU  - Bahrami, Ali
AU  - Less, György
AU  - Consorti, Lorenzo
AU  - Parandavar, Mohammad
TI  - Biostratigraphy of the Eocene shallow-water succession of the south Sabzevar area (Central Iran) based on larger benthic foraminifera and calcareous nannofossils
JF  - MICROPALEONTOLOGY
J2  - MICROPALEONTOLOGY
VL  - 70
PY  - 2024
IS  - 2
SP  - 171
EP  - 196
PG  - 26
SN  - 0026-2803
DO  - 10.47894/mpal.70.2.05
UR  - https://m2.mtmt.hu/api/publication/34824866
ID  - 34824866
AB  - A rich larger foraminifera assemblage from the Eocene carbonates of the south Sabzevar region (Now-Deh section) in central Iran indicates a late Ypresian to early Lutetian age. Nine species of Alveolina d’Orbigny are studied for systematics and biostratigraphy. The assemblage includes A. minuta, A. decastroi, A. cremae, A. cremae elongata, A. decipiens ayrancensis, A. celali, A. rugosa, A. cuspidata, A. frumentiformis. We have also found nummulitids (genus Nummulites and Assilina) and orthophragmines identified as N. campesinus, N. praediscorbinus, A. placentula, A. praespira, A. reicheli, A. ex. intrec. laxispira-maior and Discocyclina archiaci bartholomei. The recovery of Alveolina cremae elongata, A. decipiens ayrancensis, A. celali, A. rugosa, A. cuspidata and Assilina praespira has permitted for the first time to extend their geographical distribution outside of the classical peri-Mediterranean area to the central Tethys regions. The obtained biostratigraphy points to the Shallow Benthic Zones SBZ11 to SBZ13, indicating the occurrence of a Lower–Middle Eocene carbonate system. Part of the age model is supported by the calcareous nannofossil biostratigraphy that belong to the NP14b and CNE8 biozones, recorded from the central portion of the studied section. Issues regarding the application of the SBZ into the Middle East domains are discussed in terms of relative stratigraphic position and biogeographic dispersal of some significant Alveolina species.
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Fodor, László
AU  - Oravecz, Éva
AU  - Less, György
AU  - Kövér, Szilvia
TI  - Structure and evolution of the Aggtelek and Rudabánya Hills, north-east Hungary. Guidebook for pre- and post-conference excursions related to the CETEG 2023 Meeting, Kazincbarcika, Hungary
TS  - Guidebook for pre- and post-conference excursions related to the CETEG 2023 Meeting, Kazincbarcika, Hungary
T2  - Guidebook for pre- and post-conference excursions related to the CETEG 2023 Meeting
T3  - Acta Mineralogica-Petrographica, Field Guide Series, ISSN 2061-9766 ; 34.
PY  - 2023
SP  - 66
UR  - https://m2.mtmt.hu/api/publication/34540745
ID  - 34540745
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Dimou, G.V.
AU  - Koukousioura, O.
AU  - Less, György
AU  - Triantaphyllou, M.
AU  - Dimiza, M.
AU  - Syrides, G.
TI  - Exceptionally abundant Larger Benthic Foraminiferal fauna from the uppermost Eocene of Fanari (Thrace Basin, Greece)
T2  - International Symposium on Foraminifera FORAMS 2023 – Abstracts with Program
SN  - 9788394195663
PY  - 2023
SP  - 93
EP  - 94
PG  - 2
UR  - https://m2.mtmt.hu/api/publication/34343340
ID  - 34343340
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Kövecsi, Sz.
AU  - Less, György
AU  - Ples, G.
AU  - Bindiu-Haitonic, R.
AU  - Silye, L.
TI  - The Albeşti nummulitic limestones: biostratigraphic, paleoenvironmental and paleogeographic remarks
T2  - International Symposium on Foraminifera FORAMS 2023 – Abstracts with Program
SN  - 9788394195663
PY  - 2023
SP  - 163
EP  - 164
PG  - 2
UR  - https://m2.mtmt.hu/api/publication/34343280
ID  - 34343280
LA  - English
DB  - MTMT
ER  - 

TY  - CONF
AU  - Less, György
AU  - Kövecsi, Sz.
AU  - Silye, L.
TI  - The distribution of some numerical parameters of Nummulites perforatus (Montfort) A-forms from the Bartonian of Transylvania (W Romania): evidence for trimorphic life cycle in fossil foraminifera?
T2  - International Symposium on Foraminifera FORAMS 2023 – Abstracts with Program
SN  - 9788394195663
PY  - 2023
SP  - 170
EP  - 171
PG  - 2
UR  - https://m2.mtmt.hu/api/publication/34343232
ID  - 34343232
LA  - English
DB  - MTMT
ER  - 

TY  - CHAP
AU  - Budai, Tamás
AU  - Konrád, Gyula
AU  - Less, György
AU  - Raucsik, Béla
AU  - Tóthné Makk, Ágnes
AU  - Koloszár, László
AU  - Haas, János
AU  - Vörös, Attila
AU  - Józsa, Sándor
AU  - Farics, Éva
AU  - Csillag, Gábor
AU  - Pálfy, József
AU  - Rálischné Felgenhauer, Erzsébet
AU  - Pelikán, Pál
AU  - Hips, Kinga
AU  - Németh, Norbert
AU  - Velledits, Felicitász
AU  - Gál, Péter
AU  - Szoldán, Zsolt
AU  - Róth, László
AU  - Piros, Olga
AU  - Péró, Csaba
AU  - Kovács, Sándor
AU  - Kövér, Szilvia
AU  - Grill, József
AU  - Török, Ákos
AU  - Szente, István
AU  - Bércziné, Makk Anikó
ED  - Babinszki, Edit
ED  - Piros, Olga
ED  - Budai, Tamás
ED  - Gyalog, László
ED  - Halász, Amadé
ED  - Király, Edit
ED  - Koroknai, B
ED  - Haranginé Lukács, Réka
ED  - M. Tóth, Tivadar
TI  - Mezozoikum. Triász
TS  - Triász
T2  - Magyarország litosztratigráfiai egységeinek leírása I.
PB  - Szabályozott Tevékenységek Felügyeleti Hatósága
CY  - Budapest
SN  - 9789636713263
PY  - 2023
SP  - 113
EP  - 186
PG  - 154
UR  - https://m2.mtmt.hu/api/publication/34342996
ID  - 34342996
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - CHAP
AU  - Halász, Amadé
AU  - Haranginé Lukács, Réka
AU  - Koroknai, B
AU  - Less, György
AU  - Raucsikné Varga, Andrea Beáta
AU  - Lelkesné Felvári, Gy
AU  - Józsa, Sándor
AU  - Kovács, Sándor
AU  - Király, Edit
AU  - Benkó, Zsolt
AU  - Majoros, Gy
AU  - Pentelényi, L
AU  - Szederkényi, T
AU  - Rálischné Felgenhauer, E
AU  - Pelikán, P
AU  - Szemerédi, Máté
AU  - Konrád, Gy
AU  - Barabásné Stuhl, Á
AU  - Pál-Molnár, E
ED  - Babinszki, Edit
ED  - Piros, Olga
ED  - Budai, Tamás
ED  - Gyalog, László
ED  - Halász, Amadé
ED  - Király, Edit
ED  - Koroknai, B
ED  - Haranginé Lukács, Réka
ED  - M. Tóth, Tivadar
TI  - Paleozoikum
T2  - Magyarország litosztratigráfiai egységeinek leírása I.
PB  - Szabályozott Tevékenységek Felügyeleti Hatósága
CY  - Budapest
SN  - 9789636713263
PY  - 2023
SP  - 43
EP  - 112
PG  - 70
UR  - https://m2.mtmt.hu/api/publication/34342977
ID  - 34342977
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - CHAP
AU  - Less, György
AU  - Sztanó, Orsolya
AU  - Kercsmár, Zs.
AU  - Fodor, László
AU  - Haranginé Lukács, Réka
AU  - Tóth, Kálmán
AU  - Knauer, József
AU  - Németh, András
AU  - Nyíri, Dániel
AU  - Zadravecz, Csilla
AU  - Daridáné, Tichy Mária
AU  - Benedek, Kálmán
AU  - Arató, Róbert
AU  - Zelenka, Tibor
AU  - Nagymarosy, András
AU  - Böröczky, Tamás
AU  - Mindszenty, Andrea
AU  - Selmeczi, Ildikó
AU  - Dávid, Árpád
AU  - Raucsikné Varga, Andrea Beáta
AU  - Benkó, Zsolt
ED  - Babinszki, Edit
ED  - Piros, Olga
ED  - Csillag, Gábor
ED  - Fodor, László
ED  - Gyalog, László
ED  - Kercsmár, Zsolt
ED  - Less, György
ED  - Haranginé Lukács, Réka
ED  - Sebe, Krisztina
ED  - Selmeczi, Ildikó
ED  - Szepesi, János
ED  - Sztanó, Orsolya
TI  - Paleogén. Mecsek DNy-i pereme (Szentlőrinc-Szigetvár)
TS  - Mecsek DNy-i pereme (Szentlőrinc-Szigetvár)
T2  - Magyarország litosztratigráfiai egységeinek leírása II.
PB  - Szabályozott Tevékenységek Felügyeleti Hatósága
CY  - Budapest
SN  - 9789636713294
PY  - 2023
SP  - 15
EP  - 49
PG  - 35
UR  - https://m2.mtmt.hu/api/publication/34342774
ID  - 34342774
LA  - Hungarian
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Fodor, László
AU  - Oravecz, Éva
AU  - Less, György
AU  - Kövér, Szilvia
TI  - Guidebook for pre- and post-conference excursions related to the CETEG 2023 Meeting, Kazincbarcika, Hungary.. Pre-conference excursion: From rifted margin to nappe stacking: Permo-Mesozoic structural evolution of the Aggtelek and Northern Rudabánya Hills. (spotlight on salt tectonics and nppe stacking). Post-conference excursion: From Triassic rifted margin sequences to Jurassic deep marine sediments: nappe stacking in the Southern Rudabánya Hills and Aggtelek margins
TS  - Pre-conference excursion: From rifted margin to nappe stacking: Permo-Mesozoic structural evolution of the Aggtelek and Northern Rudabánya Hills. (spotlight on salt tectonics and nppe stacking). Post-conference excursion: From Triassic rifted margin sequences to Jurassic deep marine sediments: nappe stacking in the Southern Rudabánya Hills and Aggtelek margins
JF  - ACTA MINERALOGICA PETROGRAPHICA-FIELD GUIDE SERIES
J2  - ACTA MINERAL PETROGR FIELD GUIDE
VL  - 34
PY  - 2023
SP  - 3
EP  - 65
PG  - 63
SN  - 2061-9766
UR  - https://m2.mtmt.hu/api/publication/34333252
ID  - 34333252
LA  - English
DB  - MTMT
ER  - 

TY  - JOUR
AU  - Dimou, Vasiliki-Grigoria
AU  - Koukousioura, Olga
AU  - Less, György
AU  - Triantaphyllou, Maria V.
AU  - Dimiza, Margarita D.
AU  - Syrides, George
TI  - Systematic paleontology and biostratigraphy of upper Eocene larger benthic foraminifera from Fanari (Thrace Basin, Greece)
JF  - MICROPALEONTOLOGY
J2  - MICROPALEONTOLOGY
VL  - 69
PY  - 2023
IS  - 4-5
SP  - 451
EP  - 480
PG  - 30
SN  - 0026-2803
DO  - 10.47894/mpal.69.4.04
UR  - https://m2.mtmt.hu/api/publication/34166654
ID  - 34166654
AB  - Paleogene sedimentary deposits are exposed in several localities along the extended Thrace Basin in the Greek territory. One of the best sites in terms of preservation, richness and type of sediment occurs along the coastline of Fanari village (SW ofKomotini city). Two outcrops, which consist of upper Eocene shallowmarine clastic sediments, were sampled to analyze the full spectrum of larger benthic foraminifera (LBF) that comprises a rich and diverse assemblage of orthophragmines (Discocyclina, Orbitoclypeus and Asterocyclina), nummulitids (Nummulites, Assilina, Operculina, Heterostegina and Spiroclypeus), and other benthic taxa (e.g., Silvestriella, Pellatispira, Fabiania, Sphaerogypsina, etc.).Adetailed systematic description of LBF from Fanari is presented,which refines the biostratigraphic age of SBZ (Shallow Benthic Zone) 20 corresponding to the late Priabonian for the whole sequence. Twenty-four taxa among which six at (chrono)subspecies level belonging to twelve genera were identified and morphometrically analyzed for the first time from Greece. The LBF assemblage is characterized by the constant presence of Nummulites fabianii almost throughout the whole sequence. The most abundant species are Pellatispira madaraszi and Spiroclypeus carpaticus, though they occur in the upper part of the sequence along with orthophragmines. The foraminiferal distribution in the sequence enables paleoenvironmental observations and the reconstruction of the evolution of the Fanari area. Three main depositional marine shelf facies are distinguished at the shallow upper foreslope of the carbonate platform, making the Fanari section a key area not only of latest Priabonian but also of outer shelf biofacies.
LA  - English
DB  - MTMT
ER  -