7 research outputs found
Miocene otoliths of the southern edge of the Pannonian Basin
Π£ Π΄ΠΎΠΊΡΠΎΡΡΠΊΠΎΡ Π΄ΠΈΡΠ΅ΡΡΠ°ΡΠΈΡΠΈ ΡΠ΅ ΠΎΠΏΠΈΡΠ°Π½Π° ΠΈ ΠΎΠ±ΡΠ°ΡΠ΅Π½Π° Π°ΡΠΎΡΠΈΡΠ°ΡΠΈΡΠ° ΡΠΈΠ±Π° ΡΠ° ΠΎΡΠΎΠ»ΠΈΡΠΈΠΌΠ° in situ
ΠΈ ΠΈΠ·ΠΎΠ»ΠΎΠ²Π°Π½ΠΈΡ
Π½Π°Π»Π°Π·Π° ΠΎΡΠΎΠ»ΠΈΡΠ° ΡΠ° ΠΏΡΠΎΡΡΠΎΡΠ° ΡΡΠΆΠ½ΠΎΠ³ ΠΎΠ±ΠΎΠ΄Π° ΠΠ°Π½ΠΎΠ½ΡΠΊΠΎΠ³ Π±Π°ΡΠ΅Π½Π°. ΠΠ΅ΡΠ΅ΡΠΌΠΈΠ½ΠΈΡΠ°Π½Π°
ΡΠ°ΡΠ½Π° ΠΎΠ±ΡΡ
Π²Π°ΡΠ° ΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΡΠΊΠΈ ΠΎΠΏΡΠ΅Π³ ΠΎΠ΄ ΠΌΠ»Π°ΡΠ΅Π³ Π΄ΠΎΡΠ΅Π³ ΠΌΠΈΠΎΡΠ΅Π½Π° Π΄ΠΎ Π³ΠΎΡΡΠ΅Π³ ΠΌΠΈΠΎΡΠ΅Π½Π°. ΠΠ΅ΠΎ
Π°Π½Π°Π»ΠΈΠ·ΠΈΡΠ°Π½ΠΎΠ³ ΠΌΠ°ΡΠ΅ΡΠΈΡΠ°Π»Π° ΡΠ΅ Π°ΡΡΠΎΡ ΡΠ°ΠΌ ΠΏΡΠΈΠΊΡΠΏΠΈΠΎ, Π° Π΄Π΅ΠΎ ΠΏΡΠ΅ΡΠ·Π΅ΠΎ ΠΈΠ· Π·Π±ΠΈΡΠΊΠΈ ΠΡΠΈΡΠΎΠ΄ΡΠ°ΡΠΊΠΎΠ³
ΠΌΡΠ·Π΅ΡΠ° Ρ ΠΠ΅ΠΎΠ³ΡΠ°Π΄Ρ, ΠΌΡΠ·Π΅ΡΠ° ΠΠ΅ΠΏΠ°ΡΡΠΌΠ°Π½Π° Π·Π° ΠΏΠ°Π»Π΅ΠΎΠ½ΡΠΎΠ»ΠΎΠ³ΠΈΡΡ ΠΈ ΠΠ°ΡΠ΅Π΄ΡΠ΅ Π·Π° ΠΈΡΡΠΎΡΠΈΡΡΠΊΡ Π³Π΅ΠΎΠ»ΠΎΠ³ΠΈΡΡ
Π ΡΠ΄Π°ΡΡΠΊΠΎβΠ³Π΅ΠΎΠ»ΠΎΡΠΊΠΎΠ³ ΡΠ°ΠΊΡΠ»ΡΠ΅ΡΠ°, Π£Π½ΠΈΠ²Π΅ΡΠ·ΠΈΡΠ΅ΡΠ° Ρ ΠΠ΅ΠΎΠ³ΡΠ°Π΄Ρ. Π£ ΠΎΠΊΠ²ΠΈΡΡ Π΄ΠΈΡΠ΅ΡΡΠ°ΡΠΈΡΠ΅ Π΄Π°Ρ ΡΠ΅
ΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΡΠΊΠΈ ΠΏΡΠΈΠΊΠ°Π· 15 Π»ΠΎΠΊΠ°Π»ΠΈΡΠ΅ΡΠ° ΡΠ° ΠΏΡΠ°ΡΠ΅ΡΠΈΠΌ ΠΈ ΡΠΈΠ½ΡΠ΅ΡΡΠΊΠΈΠΌ Π»ΠΈΡΠΎΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΡΠΊΠΈΠΌ
ΡΡΡΠ±ΠΎΠ²ΠΈΠΌΠ°, ΠΏΡΠ΅Π³Π»Π΅Π΄ΠΎΠΌ ΡΠ°Π½ΠΈΡΠΈΡ
ΠΈΡΡΡΠ°ΠΆΠΈΠ²Π°ΡΠ°, ΠΊΠ°ΠΎ ΠΈ ΡΠ°Π±Π΅Π»Π°ΡΠ½ΠΈΠΌ ΠΏΡΠΈΠΊΠ°Π·ΠΎΠΌ ΠΏΡΠΈΠΊΡΠΏΡΠ΅Π½Π΅ ΡΠ»ΠΎΡΠ΅
ΠΈ ΡΠ°ΡΠ½Π΅. ΠΠ±ΡΡ
Π²Π°ΡΠ΅Π½ΠΈ Π»ΠΎΠΊΠ°Π»ΠΈΡΠ΅ΡΠΈ ΡΡ: ΠΠ»ΠΈΠ½ΡΠΈ, ΠΡΠ°ΡΠ΅Π²ΠΈΡ, ΠΡΠ°ΡΠΊΠΎΠ²Π°Ρ, ΠΠΎΡΠ΅ΡΠ΅Π²Π°, Π Π°ΠΊΠΎΠ²ΠΈΡΠΊΠΈ
ΠΏΠΎΡΠΎΠΊ, ΠΠ°ΠΌΠ΅Π½ΠΎΠ²ΠΎ, Π‘ΡΠ°Π΄ΠΈΠΎΠ½ Π¦ΡΠ²Π΅Π½Π° Π·Π²Π΅Π·Π΄Π°, Π²ΠΎΠ΄ΠΎΠ²ΠΎΠ΄Π½ΠΈ ΡΡΠ½Π΅Π» ΠΡΠ°ΡΠ°Ρ, ΠΠ΅ΡΡΠΎΠ²Π°Ρ, ΠΠ°Π»ΠΎ ΠΠ°ΠΎΠ»Π΅,
ΠΠ΅ΡΠΊΠΎΠ²Π°Ρ, ΠΠΎΠ»ΡΠ±Π°ΡΡΠΊΠΈ ΡΠ³ΡΠ΅Π½ΠΈ Π±Π°ΡΠ΅Π½, Π£ΠΌΡΠ°Π½ΡΠΊΠΈ ΡΡΠ½Π΅Π», ΠΡΠ΅ΡΠ°Ρ ΠΈ ΠΡΠΌΠ½ΠΎ. Π£ΠΊΡΠΏΠ½ΠΎ ΡΠ΅
ΠΏΡΠΈΠΊΠ°Π·Π°Π½ΠΎ, Π΄Π΅ΡΠ΅ΡΠΌΠΈΠ½ΠΈΡΠ°Π½ΠΎ ΠΈ ΠΎΠΏΠΈΡΠ°Π½ΠΎ 24 ΡΠΎΠ΄Π° ΠΈ 40 Π²ΡΡΡΠ° ΠΎΡΠΎΠ»ΠΈΡΠ°. ΠΠ° ΠΎΡΠ½ΠΎΠ²Ρ Π΄Π°ΡΠΈΡ
ΡΠΈΡΡΠ΅ΠΌΠ°ΡΡΠΊΠΈΡ
ΠΈ ΡΠ°ΠΊΡΠΎΠ½ΠΎΠΌΡΠΊΠΈΡ
ΠΎΠ΄ΡΠ΅Π΄Π½ΠΈΡΠ° ΠΈ ΠΏΠΎΠ΄Π°ΡΠ°ΠΊΠ° ΠΈΠ· Π»ΠΈΡΠ΅ΡΠ°ΡΡΡΠ΅ ΠΈΠ·Π²ΡΡΠ΅Π½Π° ΡΠ΅
Π±ΠΈΠΎΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΡΠΊΠ°, ΠΏΠ°Π»Π΅ΠΎΠ΅ΠΊΠΎΠ»ΠΎΡΠΊΠ° ΠΈ ΠΏΠ°Π»Π΅ΠΎΠ³Π΅ΠΎΠ³ΡΠ°ΡΡΠΊΠ° Π°Π½Π°Π»ΠΈΠ·Π° ΠΏΡΠΈΠΊΡΠΏΡΠ΅Π½Π΅ ΡΠ°ΡΠ½Π΅ ΠΎΡΠΎΠ»ΠΈΡΠ°.
ΠΡΠΎΡΡΠ°Π²Π°ΡΠ΅ΠΌ Π±ΠΈΠΎΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΡΠΊΠΈΡ
ΠΊΠ°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ° ΠΎΡΠΎΠ»ΠΈΡΠ° ΠΈ ΠΊΠΎΡΠ΅Π»Π°ΡΠΈΡΠΎΠΌ ΡΠ° Π΄ΡΡΠ³ΠΎΠΌ
ΡΠΎΡΠΈΠ»Π½ΠΎΠΌ ΡΠ°ΡΠ½ΠΎΠΌ ΠΈΡΡΠΈΡ
Π»ΠΎΠΊΠ°Π»ΠΈΡΠ΅ΡΠ°, ΠΎΠ΄ΡΠ΅ΡΠ΅Π½Π° ΡΠ΅ ΡΡΠ°ΡΠΎΡΡ ΠΈΡΡΡΠ°ΠΆΠΈΠ²Π°Π½ΠΈΡ
ΡΠ΅Π΄ΠΈΠΌΠ΅Π½Π°ΡΠ°.
ΠΠ΅ΠΎΠ»ΠΎΡΠΊΠ΅ ΠΊΠ°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ΅ ΠΏΠΎΡΠ΅Π΄ΠΈΠ½ΠΈΡ
Π»ΠΎΠΊΠ°Π»ΠΈΡΠ΅ΡΠ° ΠΈ ΡΠΈΡ
ΠΎΠ² ΠΏΠ°Π»Π΅ΠΎΠ½ΡΠΎΠ»ΠΎΡΠΊΠΈ ΡΠ°Π΄ΡΠΆΠ°Ρ, ΠΏΡΠΈΠΊΠ°Π·Π°Π½ΠΈ
ΡΡ Ρ
ΡΠΎΠ½ΠΎΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΡΠΊΠΈ. Π£ΡΠ²ΡΡΠ΅Π½ΠΎ ΡΠ΅ Π΄Π° Π½Π°ΡΡΡΠ°ΡΠΈΡΠΈ Π»ΠΎΠΊΠ°Π»ΠΈΡΠ΅Ρ ΠΠ»ΠΈΠ½ΡΠΈ (ΠΠ°ΡΠ΅Π²ΡΠΊΠΎ-ΠΠΈΠΎΠ½ΠΈΡΠΊΠΈ
Π±Π°ΡΠ΅Π½) ΠΏΡΠΈΠΏΠ°Π΄Π° ΡΠ»Π°ΡΠΊΠΎΠ²ΠΎΠ΄Π½ΠΎΠΌ ΠΌΠ»Π°ΡΠ΅ΠΌ Π΄ΠΎΡΠ΅ΠΌ ΠΌΠΈΠΎΡΠ΅Π½Ρ (ΠΎΡΠ½Π°Π½Π³?-ΠΊΠ°ΡΠΏΠ°Ρ), Π° Π»ΠΎΠΊΠ°Π»ΠΈΡΠ΅ΡΠΈ
ΠΡΠ°ΡΠ΅Π²ΠΈΡ ΠΈ ΠΡΠ°ΡΠΊΠΎΠ²Π°Ρ ΡΠ»Π°ΡΠΊΠΎΠ²ΠΎΠ΄Π½ΠΈΠΌ Π΅ΠΊΠ²ΠΈΠ²Π°Π»Π΅Π½ΡΠΈΠΌΠ° ΡΡΠ°ΡΠΈΡΠ΅Π³ ΡΡΠ΅Π΄ΡΠ΅Π³ ΠΌΠΈΠΎΡΠ΅Π½Π° (Π±Π°Π΄Π΅Π½).
ΠΠΎΡΠ΅ΡΠ΅Π²Π°, Π Π°ΠΊΠΎΠ²ΠΈΡΠΊΠΈ ΠΏΠΎΡΠΎΠΊ ΠΈ ΠΠ°ΠΌΠ΅Π½ΠΎΠ²ΠΎ ΠΎΠ΄Π³ΠΎΠ²Π°ΡΠ°ΡΡ ΡΠΈΠΏΠΈΡΠ½ΠΎΠΌ ΠΌΠΎΡΡΠΊΠΎΠΌ ΡΠ°Π·Π²ΠΈΡΡ Π¦Π΅Π½ΡΡΠ°Π»Π½ΠΎΠ³
ΠΠ°ΡΠ°ΡΠ΅ΡΠΈΡΠ° Π·Π° Π²ΡΠ΅ΠΌΠ΅ ΡΡΠ°ΡΠΈΡΠ΅Π³ ΡΡΠ΅Π΄ΡΠ΅Π³ ΠΌΠΈΠΎΡΠ΅Π½Π° (Π±Π°Π΄Π΅Π½ΡΠΊΠΈ ΠΊΠ°Ρ), Π΄ΠΎΠΊ ΠΌΠ»Π°ΡΠ΅ΠΌ ΡΡΠ΅Π΄ΡΠ΅ΠΌ ΠΌΠΈΠΎΡΠ΅Π½Ρ
β ΡΠ°ΡΠΌΠ°ΡΡ ΠΎΠ΄Π³ΠΎΠ²Π°ΡΠ°ΡΡ ΡΠ΅Π΄ΠΈΠΌΠ΅Π½ΡΠΈ Π½Π°ΡΠ΅Π½ΠΈ Π½Π° Π‘ΡΠ°Π΄ΠΈΠΎΠ½Ρ Π¦ΡΠ²Π΅Π½Π° Π·Π²Π΅Π·Π΄Π°, Ρ Π²ΠΎΠ΄ΠΎΠ²ΠΎΠ΄Π½ΠΎΠΌ ΡΡΠ½Π΅Π»Ρ
ΠΡΠ°ΡΠ°Ρ, ΠΠ΅ΡΡΠΎΠ²ΡΡ, ΠΠ°Π»ΠΎΠΌ ΠΠ°ΠΎΠ»Ρ ΠΈ ΠΠ΅ΡΠΊΠΎΠ²ΡΡ. ΠΠ΅ΡΠ΅ΡΠΌΠΈΠ½ΠΈΡΠ°Π½ΠΈ ΠΎΡΠΎΠ»ΠΈΡΠΈ ΠΈΠ· ΠΠΎΠ»ΡΠ±Π°ΡΡΠΊΠΎΠ³
ΡΠ³ΡΠ΅Π½ΠΎΠ³ Π±Π°ΡΠ΅Π½Π° ΠΈ Π£ΠΌΡΠ°Π½ΡΠΊΠΎΠ³ ΡΡΠ½Π΅Π»Π° ΡΠΊΠ°Π·ΡΡΡ Π½Π° ΡΠ°Π·Π²ΠΎΡ ΡΠ»Π°Π½ΠΊΠ°ΡΡΠΎΠ³ ΡΠ΅Π·Π΅ΡΠ° (ΠΊΠ°ΡΠΏΠΈΠ±ΡΠ°ΠΊΠΈΡΠ½ΠΎ
ΡΠ΅Π·Π΅ΡΠΎ ΠΠ°Π½ΠΎΠ½) Π·Π° Π²ΡΠ΅ΠΌΠ΅ ΡΡΠ°ΡΠΈΡΠ΅Π³ Π³ΠΎΡΡΠ΅Π³ ΠΌΠΈΠΎΡΠ΅Π½Π° β ΠΏΠ°Π½ΠΎΠ½Π°, Π΄ΠΎΠΊ Π΄Π²Π° Π»ΠΎΠΊΠ°Π»ΠΈΡΠ΅ΡΠ° ΠΡΠ΅ΡΠ°Ρ ΠΈ
ΠΡΠΌΠ½ΠΎ ΠΏΡΠΈΠΏΠ°Π΄Π°ΡΡ Π½Π°ΡΠΌΠ»Π°ΡΠ΅ΠΌ Π³ΠΎΡΡΠ΅ΠΌ ΠΌΠΈΠΎΡΠ΅Π½Ρ (ΠΏΠΎΠ½Ρ s. str. - ΠΏΡΠ΅ΠΌΠ° Π. Π‘ΡΠ΅Π²Π°Π½ΠΎΠ²ΠΈΡΡ).
ΠΠ° ΠΎΡΠ½ΠΎΠ²Ρ ΡΠ°ΡΠ½Π΅ ΠΈΠ·Π΄Π²ΠΎΡΠ΅Π½Π΅ ΠΈΠ· ΡΠ΅Π΄ΠΈΠΌΠ΅Π½Π°ΡΠ° ΡΠ·Π². Π‘ΡΠΏΡΠΊΠΎΠ³ ΡΠ΅Π·Π΅ΡΡΠΊΠΎΠ³ ΡΠΈΡΡΠ΅ΠΌΠ° ΠΊΠΎΠΌΠ΅
ΠΏΡΠΈΠΏΠ°Π΄Π°ΡΡ: ΠΠ»ΠΈΠ½ΡΠΈ, ΠΡΠ°ΡΠ΅Π²ΠΈΡ ΠΈ ΠΡΠ°ΡΠΊΠΎΠ²Π°Ρ, Π·Π°ΠΊΡΡΡΠ΅Π½ΠΎ ΡΠ΅ Π΄Π° ΡΠ΅ Π½Π° ΠΈΡΠΏΠΈΡΠΈΠ²Π°Π½ΠΎΠΌ ΠΏΡΠΎΡΡΠΎΡΡ
ΡΠΎΠΊΠΎΠΌ ΠΌΠ»Π°ΡΠ΅Π³ Π΄ΠΎΡΠ΅Π³ ΠΌΠΈΠΎΡΠ΅Π½Π° ΠΈ ΡΡΠ°ΡΠΈΡΠ΅Π³ ΡΡΠ΅Π΄ΡΠ΅Π³ ΠΌΠΈΠΎΡΠ΅Π½Π° (ΡΠ»Π°ΡΠΊΠΎΠ²ΠΎΠ΄Π½ΠΈ Π΅ΠΊΠ²ΠΈΠ²Π°Π»Π΅Π½ΡΠΈ ΠΎΡΠ½Π°Π½Π³?-
ΠΊΠ°ΡΠΏΠ°ΡΠ°-Π±Π°Π΄Π΅Π½Π°) ΠΏΠΎΡΡΠΎΡΠ°Π»Π° ΠΏΠ»ΠΈΡΠΊΠΎΠ²ΠΎΠ΄Π½Π° ΡΠ΅Π·Π΅ΡΡΠΊΠ° ΡΡΠ΅Π΄ΠΈΠ½Π°. ΠΡΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½ΠΎ, Ρ Π΄ΠΎΡΠ΅ΠΌ Π±Π°Π΄Π΅Π½Ρ Ρ
ΡΠΈΠΏΠΈΡΠ½ΠΎ ΠΌΠΎΡΡΠΊΠΎΡ ΡΡΠ΅Π΄ΠΈΠ½ΠΈ ΡΠΎΠΏΠ»ΠΎΠ³ ΠΏΠ°Π»Π΅ΠΎΠΊΠ»ΠΈΠΌΠ°ΡΠ°, Π΅Π³Π·ΠΈΡΡΠΎΠ²Π°Π»Π΅ ΡΡ ΡΠΎΡΠΌΠ΅ ΠΊΠ°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΡΠ½Π΅ Π·Π°
Π΄ΡΠ±ΡΠ΅ Π΄Π΅Π»ΠΎΠ²Π΅ Π²ΠΎΠ΄Π΅Π½ΠΎΠ³ ΡΡΡΠ±Π° (ΡΠΈΠ±Π΅ ΠΈΠ· ΡΠ°ΠΌΠΈΠ»ΠΈΡΠ΅ Bregmacerotidae ΠΈ ΠΏΠ»Π°Π½ΠΊΡΠΎΠ½ΡΠΊΠ΅
ΡΠΎΡΠ°ΠΌΠΈΠ½ΠΈΡΠ΅ΡΠ΅). Π£ ΠΏΠ΅ΡΠΈΠΎΠ΄Ρ ΠΌΠ»Π°ΡΠΈ Π±Π°Π΄Π΅Π½ - ΡΠ°ΡΠΌΠ°Ρ, ΠΌΠ΅ΡΡ ΡΠΈΠ±Π°ΠΌΠ° ΠΏΡΠΈΠΌΠ°Ρ ΠΏΡΠ΅ΡΠ·ΠΈΠΌΠ°ΡΡ Π±Π΅Π½ΡΠΎΡΠΊΠ΅
ΡΠΎΡΠΌΠ΅, ΠΏΠΎΠ·Π½Π°ΡΠΈΡΠ΅ ΠΈ ΠΊΠ°ΠΎ ΠΠΎΠ½ΡΠΎ-ΠΊΠ°ΡΠΏΠΈΡΡΠΊΠ΅ Π³ΠΎΠ±ΠΈΠ΄Π΅ (ΡΠ°ΠΌΠΈΠ»ΠΈΡΠ΅ Gobiidae), ΠΊΠΎΡΠ΅ ΡΠΊΠ°Π·ΡΡΡ Π½Π° ΡΠΎΠΏΠ»Ρ,
ΠΌΠΎΡΡΠΊΡ ΠΈ ΠΌΠΎΡΡΠΊΠΎ-Π±ΡΠ°ΠΊΠΈΡΠ½Ρ ΡΡΠ΅Π΄ΠΈΠ½Ρ Π»ΠΈΡΠΎΡΠ°Π»Π° ΠΈ ΡΡΠ±Π»ΠΈΡΠΎΡΠ°Π»Π°. ΠΠ° Π²ΡΠ΅ΠΌΠ΅ ΠΊΠ°ΡΠ½ΠΎΠ³ ΠΌΠΈΠΎΡΠ΅Π½Π° (ΠΏΠ°Π½ΠΎΠ½
ΠΈ ΠΏΠΎΠ½Ρ s.str.), Ρ ΡΠ΅Π΄ΠΈΠΌΠ΅Π½ΡΠΈΠΌΠ° Π΄Π΅ΠΏΠΎΠ½ΠΎΠ²Π°Π½ΠΈΠΌ Ρ ΡΠ»Π°Π½ΠΊΠ°ΡΡΠΎΠΌ ΠΠ°Π½ΠΎΠ½ΡΠΊΠΎΠΌ ΡΠ΅Π·Π΅ΡΡ Π·Π½Π°ΡΠ½ΠΎ ΡΠΌΠ°ΡΠ΅Π½ΠΎΠ³
ΡΠ°Π»ΠΈΠ½ΠΈΡΠ΅ΡΠ°, Π΄ΠΎΠΌΠΈΠ½Π°Π½ΡΠ½Π΅ ΡΡ ΡΠΎΡΠΌΠ΅ ΡΠΈΠ±Π° (ΡΠ°ΠΌΠΈΠ»ΠΈΡΠ΅ Sciaenidae) ΡΠΈΠΏΠΈΡΠ½Π΅ Π·Π° ΠΏΠ»ΠΈΡΠΊΠΎ ΠΈ ΡΠΎΠΏΠ»ΠΎ
ΠΏΡΠΈΠΎΠ±Π°ΡΠ΅.
ΠΠΎΡΠ΅Π±Π½ΠΎ ΡΡΠ΅Π±Π° ΠΈΡΡΠ°ΡΠΈ Π·Π½Π°ΡΠ°Ρ ΡΡΠ°Π³Π»Π°ΡΠ°Π²Π°ΡΠ° ΡΠΈΡΡΠ΅ΠΌΠ°ΡΠΈΠΊΠ΅, ΠΎΠ΄Π½ΠΎΡΠ½ΠΎ ΠΊΠΎΡΠ΅Π»Π°ΡΠΈΡΠ΅ Π½Π°Π»Π°Π·Π°
ΠΎΡΠΎΠ»ΠΈΡΠ° in situ ΡΠ° ΠΈΠ·ΠΎΠ»ΠΎΠ²Π°Π½ΠΈΠΌ ΠΎΡΠΎΠ»ΠΈΡΠΈΠΌΠ° ΠΈ ΡΠ΅Π²ΠΈΠ·ΠΈΡΠ΅ Π°ΡΡΠΈΠΊΡΠ»ΠΈΡΠ°Π½ΠΈΡ
ΡΠΊΠ΅Π»Π΅ΡΠ° Π½Π° ΠΎΡΠ½ΠΎΠ²Ρ
Π΄ΠΎΠ±ΠΈΡΠ΅Π½ΠΈΡ
ΠΏΠΎΠ΄Π°ΡΠ°ΠΊΠ°. ΠΡΠ΅ΡΡ
ΠΎΠ΄Π½ΠΎ ΠΏΡΠ±Π»ΠΈΠΊΠΎΠ²Π°Π½ΠΈ ΡΠ΅Π·ΡΠ»ΡΠ°ΡΠΈ ΠΈ ΡΠ΅Π·ΡΠ»ΡΠ°ΡΠΈ ΠΏΡΠΈΠΊΠ°Π·Π°Π½ΠΈ Ρ ΠΎΠ²ΠΎΡ ΡΠ΅Π·ΠΈ
ΠΏΠΎΡΠ²ΡΡΡΡΡ Π²Π°ΠΆΠ½ΠΎΡΡ Π½Π°Π»Π°Π·Π° ΡΠΊΠ΅Π»Π΅ΡΠ° ΡΠ° ΠΎΡΠΎΠ»ΠΈΡΠΈΠΌΠ° in situ, Π½Π΅ ΡΠ°ΠΌΠΎ Ρ Π²ΠΈΠ΄Ρ Π΄Π΅ΡΠΈΠ½ΠΈΡΠ°ΡΠ°ΡΠΈΡΡΠ΅ΠΌΠ°ΡΡΠΊΠ΅ ΠΏΡΠΈΠΏΠ°Π΄Π½ΠΎΡΡΠΈ, Π²Π΅Ρ ΠΈ Ρ ΡΠΌΠΈΡΠ»Ρ ΡΠ°Π·ΡΠΌΠ΅Π²Π°ΡΠ° Π΄ΠΈΡΡΡΠΈΠ±ΡΡΠΈΡΠ΅ Π²ΡΡΡΠ° Ρ ΠΏΡΠΎΡΡΠΎΡΡ ΠΈ
Π²ΡΠ΅ΠΌΠ΅Π½Ρ. ΠΠ° ΠΎΡΠ½ΠΎΠ²Ρ ΠΎΠ²ΠΈΡ
Π½Π°Π»Π°Π·Π° ΡΠ°ΡΠ½ΠΎ ΡΠ΅ ΠΌΠΎΠΆΠ΅ ΡΠ°Π³Π»Π΅Π΄Π°ΡΠΈ ΠΏΡΠ΅Π»Π°Π· ΠΎΠ΄ ΠΏΡΠΈΠΌΠΈΡΠΈΠ²Π½ΠΈΡ
Π³ΠΎΠ±ΠΈΠ΄Π°
(ΠΌΠ»Π°ΡΠΈ Π΄ΠΎΡΠΈ ΠΌΠΈΠΎΡΠ΅Π½ ΠΠ»ΠΈΠ½Π°ΡΠ° ΠΈ ΡΡΠ°ΡΠΈΡΠΈ ΡΡΠ΅Π΄ΡΠΈ ΠΌΠΈΠΎΡΠ΅Π½ ΠΡΠ°ΡΠ΅Π²ΠΈΡΠ°) Π΄ΠΎ ΠΠΎΠ½ΡΠΎ-ΠΊΠ°ΡΠΏΠΈΡΡΠΊΠΈΡ
Π³ΠΎΠ±ΠΈΠ΄Π° (Π³ΠΎΡΡΠΈ Π±Π°Π΄Π΅Π½/ΡΠ°ΡΠΌΠ°Ρ: Π Π°ΠΊΠΎΠ²ΠΈΡΠΊΠΈ ΠΏΠΎΡΠΎΠΊ, ΠΠ°ΠΌΠ΅Π½ΠΎΠ²ΠΎ, ΠΠ΅ΡΡΠΎΠ²Π°Ρ ΠΈ ΠΠ°Π»ΠΎ ΠΠ°ΠΎΠ»Π΅).The doctoral dissertation describes and analyzes the fish association with otoliths in situ and
isolated findings of otoliths from the southern rim of the Pannonian Basin. In terms of stratigraphic
distribution, the studied fauna extends from the late Lower to the Upper Miocene. Part of the
analyzed material was collected by the author himself, while other parts come from the collections
of the Natural History Museum in Belgrade, the Department of Paleontology and the Chair of
Historical Geology (Faculty of Mining and Geology, University of Belgrade). The dissertation
provides a stratigraphic overview of 15 fossiliferous localities, with the accompanying and local
lithostratigraphic columns, an overview of previous research, as well as a tabular overview of the
collected flora and fauna. The studied localities include Klinci, VraΔeviΔ, Brajkovac, Koceljeva,
Rakovica stream, Kamenovo, Crvena Zvezda Stadium, VraΔar water supply tunnel, Petrovac, Malo
Laole, Leskovac, Kolubara coal basin, Umka Tunnel, OreΕ‘ac, and Drmno. A total of 24 otolithbased genera and 40 otolith-based species are presented, determined and described. The resulting
systematic/taxonomic data, combined with the data obtained from the available published literature,
served as a basis for a detailed biostratigraphic, paleoecological and paleogeographic analysis.
The age of sediments was assessed via the otolith-based biostratigraphic data, which was
correlated with other fossil faunas recorded at the same localities. The geological characteristics of
individual localities and their paleontological content are presented chronostratigraphically. The
oldest among the studied localities was Klinci (the Valjevo-Mionica Basin in Western Serbia)
belonging to the Lower Miocene (Ottnangian? β Karpatian) freshwater environment, while
VraΔeviΔ and Brajkovac were found to represent freshwater equivalents of the Badenian stage (i.e.
earlier part of the Middle Miocene). The sediments from Koceljeva, Rakovica stream and
Kamenovo correspond to the typical marine environments of the Central Paratethys during the early
Middle Miocene (i.e. Badenian), while the sediments from the Crvena Zvezda Stadium, the VraΔar
water supply tunnel, Petrovac, Malo Laole and Leskovac correspond to the later part of the Middle
Miocene (i.e. Sarmatian).
Determined otoliths from the coal basin of Kolubara and the Umka Tunnel indicate the
development of a saline lake (i.e. the caspibrackish Lake Pannon) during the earlier Upper Miocene
(Pannonian), while the localities of OreΕ‘ac and Drmno belong to the latest Upper Miocene (i.e.
Pontian s. str., according to P. StevanoviΔ).
The fauna isolated from the sediments of the so-called Serbian Lake system (Klinci,
VraΔeviΔ, and Brajkovac) indicated the presence of shallow-water lake environments in the studied
area during the late Lower Miocene and the early Middle Miocene (i.e. freshwater equivalents of
the Ottnangian? β Karpatian β Badenian). On the other hand, warm marine environments of the
lower Badenian were inhabited by the forms characteristic of the deeper parts of the water column,
such as planktonic foraminifera and fish of the family Bregmacerotidae. The late Badenian to
Sarmatian interval is dominated by benthic fish known as the Ponto-Caspian gobies (family
Gobiidae), indicative of the warm marine and brackish environments within littoral and sublittoral
zones. During the Late Miocene (i.e. Pannonian and Pontian s. str.), the sediments deposited in the
Lake Pannon (in the environments with significantly reduced salinity) are dominated by the forms
typical for shallow and warm coastal areas (family Sciaenidae).
Particularly significant are the results in the domain of systematics: the correlation of
otoliths in situ with those found as isolated specimens, and the revision of the attributed skeletal
remains. The results presented in this dissertation, as well as the previously published results,
confirm the importance of articulated skeletons with otoliths in situ, not only as a means fortaxonomic attribution, but also for the understanding of distributions of taxa in space and time.
Importantly, the obtained data provides an insight into the transition from primitive gobies (late
Lower Miocene of Klinci and early Middle Miocene of VraΔeviΔ) to the Ponto-Caspian gobies
(upper Badenian β Sarmatian of the Rakovica stream, Kamenovo, Petrovac, and Malo Laole)
A new elephantoid dental specimen from the Miocene of KruΕ‘evac basin in Central Serbia
Elephantoid cheek teeth from the late Early and Middle Miocene of Europe frequently display mixtures of bunodont and zygodont features, making their taxonomical attributions difficult and subjective. Today, these teeth with βintermediateβ morphologies are attributed either to the mammutid species Zygolophodon turicensis, or to the gomphothere genus Gomphotherium - as a variation of G. angustidens or as a separate species G. subtapiroideum. This paper presents one such specimen, a fragmented lower third molar which originated from Miocene sandstones within the KruΕ‘evac Basin (possibly from the village of Bela Voda) in Central Serbia. We described the fossil and examined its metric properties in comparative context. Furthermore, we applied the semiquantitative method of WANG et al. (2016) in order to reduce subjectivity in our assessment of the degree of specimenβs zygodonty. Our results suggested that the specimen resembles Z. turicensis more closely than either G. angustidens and G. subtapiroideum, both in terms of the metrics and the degree of zygodonty. However, we were not able to make a firm taxonomical attribution, due to the fact that the specimen represents an isolated and incomplete fossil.ΠΡΠ±ΠΈ Π΅Π»Π΅ΡΠ°Π½ΡΠΎΠΈΠ΄Π° ΠΈΠ· ΠΊΠ°ΡΠ½ΠΎΠ³-ΡΠ°Π½ΠΎΠ³ ΠΈ ΡΡΠ΅Π΄ΡΠ΅Π³ ΠΌΠΈΠΎΡΠ΅Π½Π° ΠΠ²ΡΠΎΠΏΠ΅ ΡΠ΅ΡΡΠΎ ΠΏΠΎΠΊΠ°Π·ΡΡΡ ΠΌΠ΅ΡΠ°Π²ΠΈΠ½Π΅
Π±ΡΠ½ΠΎΠ΄ΠΎΠ½ΡΠ½ΠΈΡ
ΠΈ Π·ΠΈΠ³ΠΎΠ΄ΠΎΠ½ΡΠ½ΠΈΡ
ΠΊΠ°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ°, ΡΡΠΎ ΠΎΡΠ΅ΠΆΠ°Π²Π° ΠΈ ΡΡΠ±ΡΠ΅ΠΊΡΠΈΠ²ΠΈΠ·ΡΡΠ΅ ΡΠΈΡ
ΠΎΠ²Ρ ΡΠ°ΠΊΡΠΎΠ½ΠΎΠΌΡΠΊΡ Π°ΡΡΠΈΠ±ΡΡΠΈΡΡ. ΠΠ²Π°ΠΊΠ²ΠΈ Π·ΡΠ±ΠΈ ΡΠ° βΠΈΠ½ΡΠ΅ΡΠΌΠ΅Π΄ΠΈΡΠ°ΡΠ½ΠΈΠΌβ ΠΌΠΎΡΡΠΎΠ»ΠΎΡΠΊΠΈΠΌ ΠΊΠ°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ°ΠΌΠ° Π΄Π°Π½Π°Ρ ΡΠ΅ ΡΠ²ΡΡΡΠ°Π²Π°ΡΡ ΠΈΠ»ΠΈ Ρ
ΠΎΠΊΠ²ΠΈΡΠ΅ ΠΌΠ°ΠΌΡΡΠΈΠ΄ΡΠΊΠ΅ Π²ΡΡΡΠ΅ Zygolophodon turicensis, ΠΈΠ»ΠΈ ΠΌΠ΅ΡΡ ΠΏΡΠΈΠΏΠ°Π΄Π½ΠΈΠΊΠ΅ Π³ΠΎΠΌΡΠΎΡΠ΅ΡΠΈΠ΄ΡΠΊΠΎΠ³ ΡΠΎΠ΄Π° Gomphotherium - ΠΊΠ°ΠΎ Π²Π°ΡΠΈΡΠ°ΡΠΈΡΠ° Π²ΡΡΡΠ΅ G. angustidens ΠΈΠ»ΠΈ ΠΊΠ°ΠΎ Π·Π°ΡΠ΅Π±Π½Π° Π²ΡΡΡΠ° G. subtapiroideum. Π£ ΠΎΠ²ΠΎΠΌ ΡΠ°Π΄Ρ
ΡΠ΅ ΠΏΡΠ΅Π΄ΡΡΠ°Π²ΡΠ΅Π½ ΡΠ΅Π΄Π°Π½ ΡΠ°ΠΊΠ°Π² ΠΏΡΠΈΠΌΠ΅ΡΠ°ΠΊ ΡΡΠ°Π³ΠΌΠ΅Π½ΡΠΈΡΠ°Π½ΠΎΠ³ Π΄ΠΎΡΠ΅Π³ ΡΡΠ΅ΡΠ΅Π³ ΠΊΡΡΡΠ°ΠΊΠ°, ΠΊΠΎΡΠΈ ΠΏΠΎΡΠΈΡΠ΅ ΠΈΠ· ΠΌΠΈΠΎΡΠ΅Π½ΡΠΊΠΈΡ
ΠΏΠ΅ΡΡΠ°ΡΠ° Ρ ΠΎΠΊΠ²ΠΈΡΡ ΠΊΡΡΡΠ΅Π²Π°ΡΠΊΠΎΠ³ Π±Π°ΡΠ΅Π½Π° (ΠΌΠΎΠ³ΡΡΠ΅ ΠΈΠ· ΡΠ΅Π»Π° ΠΠ΅Π»Π° ΠΠΎΠ΄Π°) Ρ ΡΠ΅Π½ΡΡΠ°Π»Π½ΠΎΡ Π‘ΡΠ±ΠΈΡΠΈ. ΠΠΏΠΈΡΠ°Π»ΠΈ
ΡΠΌΠΎ ΡΠΎΡΠΈΠ»Π½ΠΈ ΠΏΡΠΈΠΌΠ΅ΡΠ°ΠΊ ΠΈ ΠΈΡΠΏΠΈΡΠ°Π»ΠΈ ΡΠ΅Π³ΠΎΠ²Π΅ ΠΌΠ΅ΡΡΠΈΡΠΊΠ΅ ΠΎΡΠΎΠ±ΠΈΠ½Π΅ Ρ ΠΊΠΎΠΌΠΏΠ°ΡΠ°ΡΠΈΠ²Π½ΠΎΠΌ ΠΊΠΎΠ½ΡΠ΅ΠΊΡΡΡ. Π’Π°ΠΊΠΎΡΠ΅, ΠΏΡΠΈΠΌΠ΅Π½ΠΈΠ»ΠΈ ΡΠΌΠΎ ΠΏΠΎΠ»ΡΠΊΠ²Π°Π½ΡΠΈΡΠ°ΡΠΈΠ²Π½ΠΈ ΠΌΠ΅ΡΠΎΠ΄ WANG et al. (2016) ΠΊΠ°ΠΊΠΎ Π±ΠΈ ΡΠΌΠ°ΡΠΈΠ»ΠΈ ΡΡΠ±ΡΠ΅ΠΊΡΠΈΠ²Π½ΠΎΡΡ ΠΏΡΠΈΠ»ΠΈΠΊΠΎΠΌ
ΠΏΡΠΎΡΠ΅Π½Π΅ ΡΡΠ΅ΠΏΠ΅Π½Π° Π·ΠΈΠ³ΠΎΠ΄ΠΎΠ½ΡΠΈΡΠ΅. ΠΠ°ΡΠΈ ΡΠ΅Π·ΡΠ»ΡΠ°ΡΠΈ ΡΡΠ³Π΅ΡΠΈΡΡ Π΄Π° ΠΏΡΠΈΠΌΠ΅ΡΠ°ΠΊ Π²ΠΈΡΠ΅ ΠΏΠΎΠ΄ΡΠ΅ΡΠ° Π½Π° Π²ΡΡΡΡ Z. turicensis Π½Π΅Π³ΠΎ Π½Π° Π²ΡΡΡΠ΅ G. angustidens ΠΈ G. subtapiroideum, ΠΊΠ°ΠΊΠΎ Ρ ΠΏΠΎΠ³Π»Π΅Π΄Ρ ΠΌΠ΅ΡΡΠΈΡΠΊΠΈΡ
ΠΊΠ°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ°, ΡΠ°ΠΊΠΎ
ΠΈ Ρ ΠΏΠΎΠ³Π»Π΅Π΄Ρ ΡΡΠ΅ΠΏΠ΅Π½Π° Π·ΠΈΠ³ΠΎΠ΄ΠΎΠ½ΡΠΈΡΠ΅. ΠΠ΅ΡΡΡΠΈΠΌ, Π½ΠΈΡΠΌΠΎ ΡΡΠΏΠ΅Π»ΠΈ Π΄Π° ΡΡΠΏΠΎΡΡΠ°Π²ΠΈΠΌΠΎ ΡΠΈΠ³ΡΡΠ½ΠΈΡΡ ΡΠ°ΠΊΡΠΎΠ½ΠΎΠΌΡΠΊΡ Π°ΡΡΠΈΠ±ΡΡΠΈΡΡ, Π·Π±ΠΎΠ³ ΡΠΈΡΠ΅Π½ΠΈΡΠ΅ Π΄Π° ΠΏΡΠΈΠΌΠ΅ΡΠ°ΠΊ ΠΏΡΠ΅Π΄ΡΡΠ°Π²ΡΠ° ΠΈΠ·ΠΎΠ»ΠΎΠ²Π°Π½ΠΈ ΠΈ Π½Π΅ΠΊΠΎΠΌΠΏΠ»Π΅ΡΠ°Π½ ΡΠΎΡΠΈΠ»
The lost freshwater goby fish fauna (Teleostei, Gobiidae) from the early Miocene of Klinci (Serbia)
First Record of Fossil Fish (Enchodontoidei, Actinopterygii) in the Struganik Quarry in Western Serbia
This paper presents the first Upper Cretaceous remains of fish in Serbia, discovered near the village of Struganik. This is also the first described find of Mesozoic fish in Serbia. A stone slab with visible contours of an almost complete fish, with a total body length of about 20 cm, was excavated from the Struganik quarry. Most bones are preserved as imprints. The number of vertebrae, the shape and position of the cranial bones, the type of teeth, and the position of the first dorsal fin all indicate that the studied specimen belongs to the genus Enchodus known from several Upper Cretaceous localities in the Tethys domain Β© 2022, Geoloski Anali Balkanskoga Poluostrva.All Rights Reserved