id	sid	eid	entity	type
gc-1013	1	1	2020	DATE
gc-1013	2	1	73/3 | 177–195	TIME
gc-1013	2	2	13 figs	QUANTITY
gc-1013	3	1	1 tab	QUANTITY
gc-1013	4	1	1 suppl	QUANTITY
gc-1013	5	1	croatian	NORP
gc-1013	5	2	croatian	NORP
gc-1013	6	1	2012	DATE
gc-1013	6	2	systems.­they­can­reach­a­thickness­of­over­6­km­and­represent­ the­time­interval­between­~11.6-2.6­ma.­in­spite­of­their­substantial­volume,­their­stratigraphic­subdivision­has­been­problematic­	GPE
gc-1013	7	1	2004;­magyar­&­	CARDINAL
gc-1013	7	2	independently­	GPE
gc-1013	7	3	neighbouring­	DATE
gc-1013	7	4	within­the­pannonian­basin­system,­although­the­lithostratigraphic­units­are­continuous­across­political­boundaries.­significant	PERSON
gc-1013	7	5	croatia	GPE
gc-1013	7	6	hungary	GPE
gc-1013	8	1	sebe1	GPE
gc-1013	8	2	marijan kovačić2	PERSON
gc-1013	8	3	imre magyar3,4	ORG
gc-1013	8	4	krešimir krizmanić5	PERSON
gc-1013	8	5	špelić6	ORG
gc-1013	8	6	bigunac7	ORG
gc-1013	8	7	kovács9	GPE
gc-1013	8	8	andrea szuromi-korecz10	PERSON
gc-1013	8	9	valentina hajek-tadesse6	PERSON
gc-1013	8	10	tamara troskot-čorbić5	PERSON
gc-1013	8	11	sztanó9 1 university of pécs	ORG
gc-1013	8	12	7624	CARDINAL
gc-1013	8	13	ifjúság ú	ORG
gc-1013	8	14	6	CARDINAL
gc-1013	8	15	hungary	GPE
gc-1013	8	16	2	CARDINAL
gc-1013	8	17	10000	CARDINAL
gc-1013	8	18	zagreb	GPE
gc-1013	8	19	95	CARDINAL
gc-1013	8	20	croatia	GPE
gc-1013	8	21	mkovacic@geol.pmf.unizg.hr	PERSON
gc-1013	9	1	3	CARDINAL
gc-1013	9	2	hungarian	NORP
gc-1013	9	3	1117	CARDINAL
gc-1013	9	4	október huszonharmadika utca 18	PERSON
gc-1013	9	5	hungary	GPE
gc-1013	9	6	4	CARDINAL
gc-1013	9	7	mta	ORG
gc-1013	9	8	budapest	GPE
gc-1013	9	9	hungary	GPE
gc-1013	9	10	5	CARDINAL
gc-1013	9	11	plc	ORG
gc-1013	9	12	exploration & production	ORG
gc-1013	9	13	lovinčićeva 4	ORG
gc-1013	9	14	10 000	CARDINAL
gc-1013	9	15	croatia	GPE
gc-1013	9	16	kresimir.krizmanic@ina.hr	PERSON
gc-1013	9	17	6	CARDINAL
gc-1013	9	18	croatian	NORP
gc-1013	9	19	10000	CARDINAL
gc-1013	9	20	zagreb	GPE
gc-1013	9	21	2	CARDINAL
gc-1013	9	22	croatia	GPE
gc-1013	9	23	7	CARDINAL
gc-1013	9	24	plc	ORG
gc-1013	9	25	10	CARDINAL
gc-1013	9	26	zagreb	GPE
gc-1013	9	27	croatia	GPE
gc-1013	9	28	8 7300	CARDINAL
gc-1013	9	29	1 utca 7	DATE
gc-1013	9	30	hungary	GPE
gc-1013	9	31	9	CARDINAL
gc-1013	9	32	1117	CARDINAL
gc-1013	9	33	konformista@caesar.elte.hu	PERSON
gc-1013	10	1	10	CARDINAL
gc-1013	10	2	1039	CARDINAL
gc-1013	10	3	14	CARDINAL
gc-1013	10	4	hungary	GPE
gc-1013	10	5	10.4154/gc.2020.12	QUANTITY
gc-1013	10	6	11.6-2.6 ma	QUANTITY
gc-1013	12	1	hungary	GPE
gc-1013	12	2	croatia	GPE
gc-1013	13	1	croatica	PERSON
gc-1013	13	2	medvedski breg	GPE
gc-1013	13	3	croatia	GPE
gc-1013	13	4	hungary	GPE
gc-1013	14	1	croatia	GPE
gc-1013	14	2	fms	ORG
gc-1013	15	1	hungary	GPE
gc-1013	16	1	the nova gradiška fm.	ORG
gc-1013	16	2	croatia	GPE
gc-1013	16	3	hungary	GPE
gc-1013	17	1	croatia	GPE
gc-1013	17	2	hungary	GPE
gc-1013	17	3	lignites	PERSON
gc-1013	18	1	fms	ORG
gc-1013	19	1	sveti matej	PERSON
gc-1013	19	2	the croatica fm	ORG
gc-1013	19	3	hungary	GPE
gc-1013	19	4	the medvedski breg fm	ORG
gc-1013	19	5	croatia	GPE
gc-1013	20	1	w	GPE
gc-1013	21	1	mura	ORG
gc-1013	21	2	more than 8 ma old	CARDINAL
gc-1013	21	3	5.3 ma	QUANTITY
gc-1013	22	1	180 km	QUANTITY
gc-1013	22	2	at least 700	CARDINAL
gc-1013	22	3	the last 3.5 million years	DATE
gc-1013	25	1	croatia	GPE
gc-1013	25	2	hungary	GPE
gc-1013	27	1	cvetković,­2013).­the­need­for­this­is­well­demonstrated­by­ malvić­&­cvetković­(2013),­who­called­attention­to­the­fact­ that­the­otherwise­lithologically­similar­upper­miocene­formations­appear­in­the­stratigraphic­charts­as­time	PERSON
gc-1013	27	2	pliocene sediments­along­the­croatian-hungarian­border”,­we­aimed­to­	PERSON
gc-1013	27	3	lake pannon deposits between­hungary­and­croatia­in­the­drava­basin,­a­deep­subarticle	ORG
gc-1013	27	4	april 27, 2020	DATE
gc-1013	27	5	august 24, 2020	DATE
gc-1013	27	6	october 26	DATE
gc-1013	27	7	2020	DATE
gc-1013	27	8	drava basin	PERSON
gc-1013	28	1	73/3178	FAC
gc-1013	29	1	that­the­drava­basin­covers­a­significant­proportion­of­the­distribution­area­of­lake­pannon­deposits­in­croatia­and­that­several­	ORG
gc-1013	29	2	area.­here­we­	GPE
gc-1013	31	1	2	CARDINAL
gc-1013	34	1	2003;­	CARDINAL
gc-1013	34	2	2012;­ malvić­&­cvetković,­2013;­pavelić­&­kovačić,­2018).­	NORP
gc-1013	35	1	lake pannon	PERSON
gc-1013	35	2	to­modern­fluvial­system­following­the­lake	GPE
gc-1013	36	1	north croatia	LOC
gc-1013	38	1	kovačić­&­grizelj,­2006;­kovačić­et­al	PERSON
gc-1013	38	2	al.	PERSON
gc-1013	40	1	in­the­marginal­areas­surrounding­the­drava­basin,­sedimentation­across­the­sarmatian	NORP
gc-1013	40	2	in­the­deepest­part­of­small­sub	NORP
gc-1013	40	3	horváth­et­al	DATE
gc-1013	40	4	within­the­drava­basin­itself,­the­existence­of­sarmatian­sediments­has­not­been­proven­with­fauna­yet,­only­in­the­nw­in­the­ mura	PERSON
gc-1013	40	5	post-rift­phase­of­basin­evolution­(pavelić,­2001;­horváth­	EVENT
gc-1013	42	1	3	CARDINAL
gc-1013	42	2	1	CARDINAL
gc-1013	44	1	2012	DATE
gc-1013	46	1	moslavačka gora	PERSON
gc-1013	46	2	požeška gora	PERSON
gc-1013	46	3	republic of serbia	ORG
gc-1013	48	1	croatia	GPE
gc-1013	48	2	hungary	GPE
gc-1013	48	3	179	CARDINAL
gc-1013	48	4	fel)-i,­zaláta­(zal)-1,­dravica­(dra)-1,­krunoslavlje­(kru)-2­and­	NORP
gc-1013	48	5	49,­41­and­31­km,­respectively,­were­also­compiled­(figs.­1,­8).­ key­wells­iharosberény­(ih)-i,­vízvár	GPE
gc-1013	49	1	4	CARDINAL
gc-1013	49	2	croatia	GPE
gc-1013	49	3	hungary	GPE
gc-1013	49	4	croatia	GPE
gc-1013	49	5	three	CARDINAL
gc-1013	49	6	today	DATE
gc-1013	50	1	dependent­on­changes­of­the­depositional­environment­(magyar­ &­geary,­2012).­furthermore,­it­has­since­been­shown­that­the­ pontian­stage,­originally­defined­in­the­euxinian­(black­sea)­basin,­was­erroneously­correlated­into­the­pannonian­basin­system­	ORG
gc-1013	52	1	2	CARDINAL
gc-1013	52	2	croatia	GPE
gc-1013	54	1	1996	DATE
gc-1013	54	2	magyar et al	PERSON
gc-1013	54	3	1999	DATE
gc-1013	55	1	j en ko	PERSON
gc-1013	55	2	1 94 4	DATE
gc-1013	55	3	ć	PERSON
gc-1013	55	4	20 01	DATE
gc-1013	56	1	1980	DATE
gc-1013	57	1	2003	DATE
gc-1013	57	2	malvić & cvetković	ORG
gc-1013	57	3	2013	DATE
gc-1013	58	1	g eo lo	PERSON
gc-1013	58	2	the national committee for stratigraphy	ORG
gc-1013	58	3	the­republic­of­croatia­(map­sheets­for­the­slavonia­area:­filjak­et­al	CARDINAL
gc-1013	59	1	croatia	GPE
gc-1013	62	1	surface,­the­scheme­contains­six­lithostratigraphic­units­of­formation­rank,­described­in­detail­below­(kovačić,­2004;­filjak­	NORP
gc-1013	63	1	2016a,­	CARDINAL
gc-1013	63	2	2016b;­	CARDINAL
gc-1013	63	3	kovačić­ &­	ORG
gc-1013	63	4	2017;­	CARDINAL
gc-1013	65	1	krndija,­papuk­and­bilogora­mts.­however,­as­a­result­of­terrain­	GPE
gc-1013	66	1	hungary	GPE
gc-1013	67	1	juhász,­1998;­korpásné­hódi,­1998).­the­past­two­decades­have­brought­progress­in­recognizing­that­except­for­the­oldest­formations­(békés,­	GPE
gc-1013	67	2	indicating­	GPE
gc-1013	67	3	in­filling­process.­therefore­a­basin-wide­correlation­of­deep,­	DATE
gc-1013	67	4	sztanó­et­al	CARDINAL
gc-1013	68	1	2015a	DATE
gc-1013	68	2	by­the­long-term­normal­regression­interrupted­by­minor­flooding­events­or­local­variations­in­sediment­input.­official­formation	PERSON
gc-1013	69	1	4.1	CARDINAL
gc-1013	70	1	their­fossil­content­showed­that­formation­boundaries­are­timetransgressive­over­the­entire­drava­basin­and­its­surroundings,­	FAC
gc-1013	71	1	pliocene lacustrine­to­fluvial­succession­should­be­based­on­the­lithological­	PERSON
gc-1013	72	1	4.1.1	CARDINAL
gc-1013	73	1	1973;­sztanó­et­al	CARDINAL
gc-1013	74	1	3	CARDINAL
gc-1013	75	1	croatia	GPE
gc-1013	75	2	hungary	GPE
gc-1013	81	1	croatia	GPE
gc-1013	81	2	hungary	GPE
gc-1013	81	3	181	CARDINAL
gc-1013	83	1	2015).­in­most­places­it­is­a­transgressive­deposit­at­the­base­of­	CARDINAL
gc-1013	84	1	lake­was­high,­it­overlies­offshore­calcareous­marls­and­prinches­	GPE
gc-1013	84	2	at­a­later­stage­it­interfingers­with,­or­it­is­overlain­by­the­újfalu­ formation­(e.g.­budai­et­al.	PERSON
gc-1013	84	3	c. ungulacaprae	PERSON
gc-1013	84	4	l. dumi­	PERSON
gc-1013	84	5	cici	ORG
gc-1013	84	6	l. cf.	PERSON
gc-1013	85	1	l. schmidti	PERSON
gc-1013	85	2	l. szaboi	PERSON
gc-1013	86	1	4.1.2	CARDINAL
gc-1013	86	2	sveti matej	PERSON
gc-1013	86	3	croatica formation coarse clastics	ORG
gc-1013	86	4	while­sorting­and­rounding­is­variable,­depending­on­the­transport­	PERSON
gc-1013	87	1	hungary­are­classified­into­the­ősi­variegated­clay­fm.	GPE
gc-1013	89	1	the­békés­conglomerate­(fig.­5b)­comprises­gravels­reworked­by­lacustrine­wave­action­and­is­conformably­overlain­by­ the­calcareous­marls­of­the­endrőd­fm.­typical­grain­size­is­below­10­cm,­but­the­largest­clasts­can­exceed­1­m.­matrix­material­	PERSON
gc-1013	89	2	is­either­missing­or­is­identical­to­the­overlying­marls.­the­unit­	PRODUCT
gc-1013	89	3	1-2	QUANTITY
gc-1013	89	4	~20­m.­the­wave-reworked­gravels­indicate­the­flooding­of­drylands,­therefore­the­unit­occurs­at­locations­where­open­lacustrine­ sediments­overlie­older­rocks­unconformably:­along­the­margins­	ORG
gc-1013	90	1	the monyoród	DATE
gc-1013	91	1	4	CARDINAL
gc-1013	92	1	cserdi	ORG
gc-1013	92	2	w mecsek mts	PERSON
gc-1013	93	1	5	CARDINAL
gc-1013	95	1	sveti matej	ORG
gc-1013	95	2	sveti matej	PERSON
gc-1013	95	3	medvednica mts	ORG
gc-1013	97	1	monyoród quarry	PERSON
gc-1013	98	1	g eo lo	PERSON
gc-1013	98	2	73/3182 4.1.3	DATE
gc-1013	99	1	croatica	PERSON
gc-1013	99	2	medvedski breg	GPE
gc-1013	99	3	lake	LOC
gc-1013	100	1	gravel)­occur­in­the­lower­part­of­the­calcareous­marls.­its­thickness­ranges­from­a­few­tens­of­metres­in­marginal­areas­to­50-200­	PERSON
gc-1013	100	2	hungarian	NORP
gc-1013	101	1	the­west­of­the­danube.­it­can­be­white­near­basement­highs­or­	GPE
gc-1013	102	1	vető,­2012).­the­upper­part­comprising­clay­marls­is­distinguished­as­the­nagykörű­mb.­in­the­great­hungarian­plain­and­ as­the­nagylengyel­mb.­in­the­west­(juhász,­1998),­and­it­occurs­mostly­in­deep­basins.­the­endrőd­fm.­corresponds­to­the­ croatica­and­medvedski­breg­fms.­in­croatia,­which,­based­on­	PERSON
gc-1013	103	1	medvedski breg fms	PERSON
gc-1013	104	1	2	CARDINAL
gc-1013	104	2	the croatica fm	ORG
gc-1013	105	1	našice quarry	PERSON
gc-1013	105	2	krndija mts.	PERSON
gc-1013	105	3	medvedski breg fm	ORG
gc-1013	106	1	našice quarry	PERSON
gc-1013	107	1	fms	ORG
gc-1013	108	1	tp-1	ORG
gc-1013	108	2	2564	CARDINAL
gc-1013	109	1	croatia	GPE
gc-1013	109	2	hungary	GPE
gc-1013	109	3	183	CARDINAL
gc-1013	110	1	geria banatica	PERSON
gc-1013	110	2	digitifera	PERSON
gc-1013	111	1	2015).­littoral­fossils­occur­in­redeposited­interbeds.­a­diverse­	CARDINAL
gc-1013	111	2	the­uppermost­part­of­the­formation­(hably­&­sebe,­2016).­	ORG
gc-1013	112	1	9­ma;­bakrač­et­al	CARDINAL
gc-1013	113	1	sections­(croatica­fm.)­and­the­medvedski­breg­section­(m.­b.­ fm.)­in­the­nw­part­of­the­sava­basin,­on­the­slopes­of­the­medvednica­mts.­	PERSON
gc-1013	113	2	2016,­ 2017a;­	CARDINAL
gc-1013	113	3	kovačić­&­ pavelić,­2017).­at­present­the­most­representative­surface­occurrences­are­the­našice­quarry­on­the­northern­slopes­of­the­ krndija­mts.­(kovačić­et­al	PERSON
gc-1013	114	1	croatica	PERSON
gc-1013	114	2	the croatica fm	ORG
gc-1013	114	3	croatia	GPE
gc-1013	117	1	laterally­and­upwards­it­gradually­passes­into­the­marls­of­the­ medvedski­breg­fm.­it­is­widely­distributed­in­the­marginal­parts­	PERSON
gc-1013	118	1	radix croatica	PERSON
gc-1013	120	1	i. pavelici	PERSON
gc-1013	120	2	kovačić­et­al.	GPE
gc-1013	121	1	sigmopollis spp.­have­also­been­identified­ in­this­formation­(kovačić­et­al	ORG
gc-1013	126	1	thousand years	DATE
gc-1013	127	1	ultima­zone­(sütőszentai,­1982),­and­the­mecsekia	GPE
gc-1013	128	1	been­	GPE
gc-1013	130	1	juhász­&­magyar,­1992;­geary­et­al	PERSON
gc-1013	130	2	va­ lenciennius­occur­in­core­samples­from­the­bottom­of­several­	PERSON
gc-1013	132	1	dorozsma marl	PERSON
gc-1013	132	2	the medvedski breg	ORG
gc-1013	133	1	g eo lo	PERSON
gc-1013	136	1	c om po si te se	PERSON
gc-1013	136	2	fle ct io	PERSON
gc-1013	144	1	1	CARDINAL
gc-1013	146	1	ar ke rs u se	PERSON
gc-1013	146	2	st ry se e vr ba	PERSON
gc-1013	147	1	2	CARDINAL
gc-1013	149	1	cu rr en ce s s er ve s	ORG
gc-1013	150	1	8 .	CARDINAL
gc-1013	150	2	ec	ORG
gc-1013	150	3	ns 2	ORG
gc-1013	153	1	croatia	GPE
gc-1013	153	2	hungary	GPE
gc-1013	153	3	185	CARDINAL
gc-1013	155	1	szolnok	ORG
gc-1013	156	1	same­deposits­are­assigned­to­the­szolnok­and­algyő­fms.­in­ hungary	GPE
gc-1013	157	1	2013b).­these­deep-water­formations­conformably­overlie­the­ endrőd	QUANTITY
gc-1013	157	2	parts­of­vinkovci­fm.­in­the­edb.­	GPE
gc-1013	157	3	the­szolnok­fm.­and­the­lower­part­of­the­algyő­fm.­consist­	CARDINAL
gc-1013	158	1	cmto dm-thick	PERSON
gc-1013	158	2	beds­commonly­show­sedimentary­structures­including­plane­to­	CARDINAL
gc-1013	159	1	8	CARDINAL
gc-1013	160	1	2	CARDINAL
gc-1013	160	2	4	CARDINAL
gc-1013	162	1	1	CARDINAL
gc-1013	163	1	g eo lo	PERSON
gc-1013	163	2	100	CARDINAL
gc-1013	164	1	on­the­1-2­reflections­thick­endrőd­fm.­the­lower­part­of­the­	TIME
gc-1013	167	1	1300­m­in­the­centre­of­the­	DATE
gc-1013	170	1	profundal­mollusc­fauna­with­congeria banatica	PERSON
gc-1013	170	2	digitifera	PERSON
gc-1013	170	3	paradacna abichi	PERSON
gc-1013	170	4	otiophora	PERSON
gc-1013	170	5	valenciennius reussi	PERSON
gc-1013	170	6	c. czjzeki	GPE
gc-1013	170	7	c. zagrabiensis	PERSON
gc-1013	170	8	c. croatica	PERSON
gc-1013	171	1	candona (caspiolla	ORG
gc-1013	171	2	minata	PERSON
gc-1013	171	3	deis dominate,­while­the­dinocyst­assemblage­consists­of­mainly­	PERSON
gc-1013	171	4	s. virgulaefor­ mis	ORG
gc-1013	171	5	s. paradoxus	PERSON
gc-1013	171	6	s. balcanicus	PERSON
gc-1013	171	7	s. validus­etc.­the­vertical­arrangement­of­the­facies­within­the­andraševec­fm.­and­the­accompanying­fossil­communities­indicate­the­shallowing­of­the­ depositional­environment	PERSON
gc-1013	172	1	where­	GPE
gc-1013	173	1	4.1.5	CARDINAL
gc-1013	174	1	nova gradiška	FAC
gc-1013	175	1	9).­the­sediments­display­a­coarsening­upward­trend­on­the­scale­	CARDINAL
gc-1013	177	1	mineralogically­very­similar­to­the­sands­of­the­andraševec­fm	GPE
gc-1013	180	1	and­ lignite­ are­	ORG
gc-1013	182	1	300­m­thick­in­the­se­(fig.­7).­the­unit­conformably­overlies­the­	CARDINAL
gc-1013	183	1	with­congeria rhomboidea	FAC
gc-1013	183	2	c. balatonica	PERSON
gc-1013	183	3	c. triangularis	PERSON
gc-1013	183	4	lymnocardium majeri	PERSON
gc-1013	183	5	l. diprosopum	PERSON
gc-1013	183	6	l. arpadense	PERSON
gc-1013	183	7	l. hungaricum	PERSON
gc-1013	183	8	l. rogenhoferi	PERSON
gc-1013	183	9	paradacna okrugici	PERSON
gc-1013	183	10	kovačić,­2004).­the­dinocyst assemblage	ORG
gc-1013	183	11	impagidinium globosum	PERSON
gc-1013	183	12	ga­ leacysta	PERSON
gc-1013	183	13	and­in­the­eastern­part­of­the­drava­basin­(fig.­7)­during­the­	PERSON
gc-1013	184	1	croatia	GPE
gc-1013	184	2	hungary	GPE
gc-1013	184	3	187	CARDINAL
gc-1013	184	4	­earliest­pliocene,­based­on­the­well­to­seismic­correlation­of­the­ miocene	PERSON
gc-1013	186	1	deposited­on­the­prodelta­to­the­lower­delta­front.­most­of­the­sand­ was­deposited­on­mouth­bars­in­the­upper­delta­front­environment.­sand­deposition­on­the­mouth­bars­was­related­to­prolonged,­frequent­floods­under­humid­climate­conditions.­proximal	PERSON
gc-1013	186	2	brackish­interdistributary­bays,­in­brackish­wetlands­or­in­freshwater­marshes­and­ponds­in­a­delta­plain­environment­(juhász­ &­magyar­1992;­juhász,­1994;­kovačić­et­al	ORG
gc-1013	187	1	the­nova­gradiška­formation­is­named­after­sections­located­near­the­town­of­nova­gradiška­in­western­slavonia.­apart­	PERSON
gc-1013	187	2	1961).­some­small­occurrences­are­also­detected­in­the­northern­	CARDINAL
gc-1013	187	3	1999)­also­belongs­to­this­formation	CARDINAL
gc-1013	188	1	4.1.6	CARDINAL
gc-1013	188	2	clay­(fig.­10).­close­to­basement­highs,­gravels­may­also­occur.­	ORG
gc-1013	188	3	the­formation­is­composed­of­fine	ORG
gc-1013	189	1	1000	CARDINAL
gc-1013	190	1	9	CARDINAL
gc-1013	191	1	gradiška fm	PERSON
gc-1013	192	1	mučna reka	PERSON
gc-1013	192	2	bilogora hills	GPE
gc-1013	192	3	croatia	GPE
gc-1013	194	1	10	CARDINAL
gc-1013	195	1	pluska fm	ORG
gc-1013	195	2	the nova gradiška fm	ORG
gc-1013	195	3	pluska	ORG
gc-1013	196	1	dubravica	PERSON
gc-1013	197	1	g eo lo	PERSON
gc-1013	197	2	73/3188	CARDINAL
gc-1013	198	1	2011).­the­latter­attain­a­thickness­of­nearly­300­m­in­the­northern­marginal­part­of­the­drava­basin­(e.g.­borehole­görgeteg	CARDINAL
gc-1013	199	1	2.1­ma,­	CARDINAL
gc-1013	199	2	2001;­krolopp,­2002	CARDINAL
gc-1013	200	1	5	CARDINAL
gc-1013	200	2	5.1	CARDINAL
gc-1013	200	3	2001;­bakrač,­2007;­bakrač­et­al	DATE
gc-1013	201	1	11	CARDINAL
gc-1013	202	1	3d	CARDINAL
gc-1013	202	2	approximately 650	CARDINAL
gc-1013	204	1	croatia	GPE
gc-1013	204	2	hungary	GPE
gc-1013	204	3	189	CARDINAL
gc-1013	205	1	boundaries.­the­following­significant­change­in­the­dinocyst­record­is­benchmarked­with­the­more­or­less­coeval­first­appearance­	ORG
gc-1013	205	2	coniunctus	ORG
gc-1013	205	3	s. val­ idus	PERSON
gc-1013	205	4	s. balcanicus	PERSON
gc-1013	205	5	s. paradoxus.­in­this­interval,­either­one­	PERSON
gc-1013	205	6	s.	PERSON
gc-1013	206	1	paradoxus	NORP
gc-1013	206	2	s. co­ niunctus	PERSON
gc-1013	206	3	s. validus;­sütő-szentai,­1991;­krizmanić	PERSON
gc-1013	207	1	paradoxus	NORP
gc-1013	207	2	s. validus	PERSON
gc-1013	207	3	s. tih­	PERSON
gc-1013	207	4	anyensis;­sütő-szentai,­2000)­biozones­are­distinguished.­	PERSON
gc-1013	207	5	marker­in­the­sedimentary­succession­of­lake­pannon­(bakrač­ et­al	GPE
gc-1013	208	1	galeacysta	NORP
gc-1013	209	1	this­occurrence­approaches­the­best­the­real­fad­of­g	CARDINAL
gc-1013	211	1	5.2	CARDINAL
gc-1013	212	1	1992;­magyar­et­al	DATE
gc-1013	215	1	the­profundal­deposits­of­lake­pannon­were­divided­into­	DATE
gc-1013	216	1	congeria banatica	ORG
gc-1013	216	2	c. banatica	PERSON
gc-1013	216	3	provalenciennesia	GPE
gc-1013	216	4	digitifera zone	PERSON
gc-1013	216	5	d.	NORP
gc-1013	216	6	digitifera	PERSON
gc-1013	216	7	,­1999;­magyar­&­geary,­2012;­fig.­3).­in­the­	PERSON
gc-1013	218	1	carbonifera­was­recovered­from­a­sedimentary­inclusion­embedded­into­volcanic­ material­in­the­tihany­peninsula,­lake­balaton­(sztanó­et­al	PRODUCT
gc-1013	218	2	2013a).­the­tihany­maar­volcano­is­known­to­have­started­its­activity­7.92±0.22­to­7.96±0.03­ma­ago­(as­assessed­by­k	CARDINAL
gc-1013	218	3	2018;­magyar­et­al	CARDINAL
gc-1013	218	4	magyar­&­geary,­2012),­although­the­two­fossils­	PRODUCT
gc-1013	219	1	the­biostratigraphic­boundary­between­the­congeria bana­ tica	ORG
gc-1013	219	2	1	CARDINAL
gc-1013	220	1	first	ORDINAL
gc-1013	221	1	galeacysta	PERSON
gc-1013	222	1	two	CARDINAL
gc-1013	222	2	1680 2005	DATE
gc-1013	222	3	f-1d	WORK_OF_ART
gc-1013	222	4	1565 1942	DATE
gc-1013	222	5	2780	CARDINAL
gc-1013	222	6	1330 1550	CARDINAL
gc-1013	222	7	1570 2174	CARDINAL
gc-1013	222	8	two	CARDINAL
gc-1013	222	9	1232 1310	DATE
gc-1013	222	10	1714	CARDINAL
gc-1013	222	11	2065	CARDINAL
gc-1013	222	12	1210 1370	DATE
gc-1013	223	1	g eo lo	PERSON
gc-1013	223	2	73/3190	CARDINAL
gc-1013	223	3	12	CARDINAL
gc-1013	225	1	1	CARDINAL
gc-1013	225	2	2880–2885	CARDINAL
gc-1013	225	3	2	CARDINAL
gc-1013	225	4	2840–2845	CARDINAL
gc-1013	225	5	3	CARDINAL
gc-1013	225	6	2820–2825	CARDINAL
gc-1013	225	7	4	CARDINAL
gc-1013	225	8	2800–2805	CARDINAL
gc-1013	225	9	5	CARDINAL
gc-1013	225	10	2695–2700	CARDINAL
gc-1013	225	11	6	CARDINAL
gc-1013	225	12	2190–2195	CARDINAL
gc-1013	225	13	7	CARDINAL
gc-1013	225	14	galeacysta	PERSON
gc-1013	225	15	1300–1310	CARDINAL
gc-1013	225	16	8	CARDINAL
gc-1013	225	17	1300–1310	CARDINAL
gc-1013	225	18	9	CARDINAL
gc-1013	225	19	2076–2081	CARDINAL
gc-1013	225	20	10	CARDINAL
gc-1013	225	21	1659–1665	CARDINAL
gc-1013	225	22	11	CARDINAL
gc-1013	225	23	1659–1665	CARDINAL
gc-1013	225	24	12	CARDINAL
gc-1013	225	25	1659–1665	CARDINAL
gc-1013	225	26	13	CARDINAL
gc-1013	225	27	3260	CARDINAL
gc-1013	225	28	14	CARDINAL
gc-1013	225	29	3204	CARDINAL
gc-1013	225	30	15	CARDINAL
gc-1013	225	31	3174	CARDINAL
gc-1013	225	32	16	CARDINAL
gc-1013	225	33	3040	CARDINAL
gc-1013	225	34	17	CARDINAL
gc-1013	225	35	galeacysta	PERSON
gc-1013	225	36	2780	CARDINAL
gc-1013	225	37	18	CARDINAL
gc-1013	225	38	2750–2760	CARDINAL
gc-1013	225	39	19	CARDINAL
gc-1013	225	40	galeacysta	PERSON
gc-1013	225	41	480–490	CARDINAL
gc-1013	225	42	20	CARDINAL
gc-1013	225	43	920–930	CARDINAL
gc-1013	225	44	21	CARDINAL
gc-1013	225	45	2540	CARDINAL
gc-1013	225	46	22	CARDINAL
gc-1013	225	47	zalata-k-1	PERSON
gc-1013	225	48	2500	CARDINAL
gc-1013	225	49	23	CARDINAL
gc-1013	225	50	2460	CARDINAL
gc-1013	225	51	24	CARDINAL
gc-1013	225	52	zalata-k-1	PERSON
gc-1013	225	53	1980	DATE
gc-1013	225	54	25	CARDINAL
gc-1013	225	55	galeacysta	PERSON
gc-1013	225	56	zalata-k-1	PERSON
gc-1013	225	57	1640	CARDINAL
gc-1013	225	58	m. g	PERSON
gc-1013	226	1	croatia	GPE
gc-1013	226	2	hungary	GPE
gc-1013	226	3	191	CARDINAL
gc-1013	226	4	succession­of­the­drava­basin­in­its­northern­margin­(ujszászi­ &­vakarcs,­1993;­sacchi­et­al.	ORG
gc-1013	226	5	hungarian	NORP
gc-1013	226	6	and­ 6.8­ma­	PERSON
gc-1013	226	7	magyar­&­	ORG
gc-1013	226	8	2008­	CARDINAL
gc-1013	226	9	therein).­as­the­vertebrate­fauna­was­miocene­below­and­pliocene­above­the­unconformity­in­several­boreholes,­its­basinward­	GPE
gc-1013	228	1	7.	CARDINAL
gc-1013	228	2	hungarian	NORP
gc-1013	228	3	croatian	NORP
gc-1013	228	4	deposited­in­delta­plain­and­alluvial­environments.­these­units­can­be­ well­correlated­across­the­basin	GPE
gc-1013	231	1	interpreted­ seismic­network,­	GPE
gc-1013	231	2	northernmost­part­of­the­drava­basin,­between­the­wells­leg-1j­and­ sev-1­in­croatia­and­between­wells­­ib-i­and­víz-é-4­in­hungary.­	PERSON
gc-1013	231	3	of­the­drava­basin­are­younger­than­the­–­supposedly­–­miocene	CARDINAL
gc-1013	232	1	croatian	NORP
gc-1013	233	1	04	CARDINAL
gc-1013	234	1	hungarian	NORP
gc-1013	235	1	and­ina-industrija­nafte­d.d.­are­acknowledged­for­their­permission­to­use­seismic­and­borehole­data­for­our­study.­this­is­mtamtm-elte­paleo­contribution­no­328.­we­are­grateful­to­oleg­	ORG
gc-1013	235	2	part­of­the­pannonian­basin:­the­potential­for­shale­gas­and­shale­oil­plays.–­marine­and­petroleum­geology,­31,­53–69.­doi:­10.1016/j.marpetgeo.2011.08.015	PERSON
gc-1013	235	3	pontian	NORP
gc-1013	235	4	m7	GPE
gc-1013	235	5	1:300000­–­in­croatian].­croatian­geological­survey,­	CARDINAL
gc-1013	235	6	13	CARDINAL
gc-1013	236	1	digitifera	PERSON
gc-1013	236	2	valenciennius reussi	PERSON
gc-1013	236	3	2060	CARDINAL
gc-1013	236	4	md	GPE
gc-1013	238	1	galeacysta	NORP
gc-1013	239	1	500	CARDINAL
gc-1013	239	2	lake pannon	LOC
gc-1013	239	3	700	CARDINAL
gc-1013	239	4	balázs et al.	PERSON
gc-1013	239	5	2018	DATE
gc-1013	240	1	g eo lo	PERSON
gc-1013	240	2	basin­–­in­croatian­with­	PERSON
gc-1013	245	1	,­horváth,­f.­&­cloetingh,­s.­(2016):­ the­link­between­tectonics­and­sedimentation­in­back-arc­basins:­new­genetic­constraints­from­the­analysis­of­the­pannonian­basin.–­tectonics,­35,­1526–1559.­­doi:­	PERSON
gc-1013	249	1	transdanubia	GPE
gc-1013	250	1	bérczi,­i.­(1988):­preliminary­sedimentological­investigation­of­a­neogene­depression­ in­the­great­hungarian­plain.–­in:­royden,­l.h.­&­horváth,­f.­(eds.):­the­ pannonian­basin.­aapg­memoir,­45,­107–116	PERSON
gc-1013	251	1	neogene deltaic-lacustrine	PERSON
gc-1013	251	2	southeast hungary	LOC
gc-1013	256	1	grossen­ungarischen­tiefebene.–­in:­jámbor,­á.­(ed.):­geologische­charakterisierung­der­ablagerungen­der­kunság-stufe­in­ungarn.–­annals­of­the­hungarian­ geological­institute,­69,­179–198	ORG
gc-1013	257	1	budai,­s	PERSON
gc-1013	259	1	hungary	GPE
gc-1013	267	1	geophysical institute	ORG
gc-1013	267	2	hungary	GPE
gc-1013	267	3	budapest	GPE
gc-1013	267	4	50–51	CARDINAL
gc-1013	270	1	1:300000	CARDINAL
gc-1013	270	2	croatian].–­croatian­geological­survey,­department­of­geology,­zagreb	PRODUCT
gc-1013	271	1	dezső,­j	PERSON
gc-1013	273	1	hungary	GPE
gc-1013	278	1	3	CARDINAL
gc-1013	278	2	croatian	NORP
gc-1013	279	1	croatian	NORP
gc-1013	281	1	4	CARDINAL
gc-1013	285	1	279/3,­261–271.­doi:­10.1127	CARDINAL
gc-1013	285	2	halamić,­j	PERSON
gc-1013	291	1	požeška gora	PERSON
gc-1013	291	2	croatian].–­croatian­geological­survey,­department­of­geology,­zagreb	CARDINAL
gc-1013	297	1	4th­croatian­geological­congress,­sibenik,­14-15.­10.­2010.­abstract­book.­croatian­geological­survey,­zagreb,­369–370	DATE
gc-1013	297	2	hilgen,­f­j	PERSON
gc-1013	302	1	r.a.	PERSON
gc-1013	304	1	neogene­period.–­in:­gradstein,­f.­m	MONEY
gc-1013	305	1	0-44459425	CARDINAL
gc-1013	314	1	10.1190	CARDINAL
gc-1013	314	2	0100.1	CARDINAL
gc-1013	316	1	juhász,­	ORG
gc-1013	316	2	gy.­	PRODUCT
gc-1013	316	3	hungary	GPE
gc-1013	316	4	budapest	GPE
gc-1013	316	5	469–484	CARDINAL
gc-1013	317	1	juhász,­gy.­&­magyar,­i.­(1992):­review­and­correlation­of­the­late­neogene­(pannonian s.l.	ORG
gc-1013	317	2	hungary	GPE
gc-1013	319	1	kelder,­n.a.	PERSON
gc-1013	323	1	pannon:­problems,­pitfalls,­and­progress­in­using­iron­sulfides­for­magnetostratigraphy.–­ geochemistry,­ geophysics,­	ORG
gc-1013	323	2	19,­ 3405–3429.­	DATE
gc-1013	325	1	2a­fúrások­fúrások­negyedidőszaki­képződményeinek­párhuzamosítása­[correla­	NORP
gc-1013	325	2	holes­-­in­hungarian].–­földtani­közlöny,­131/3–4,­443–460	PERSON
gc-1013	326	1	konrád,­gy.­&­sebe,­k.­(2010):­new­records­of­young­tectonic­phenomena­in­the­ western­mecsek­mts.­and­their­surroundings.–­földtani­közlöny,­140/2,­445–468	GPE
gc-1013	329	1	korpás-hódi,­m.­(1987):­korrelationsmöglichkeit­der­jungen­neogenbildungen­ungarns.–­annals­of­the­geological­institute­of­hungary,­69,­435–452	PERSON
gc-1013	330	1	hungary	GPE
gc-1013	334	1	croatia	GPE
gc-1013	334	2	hungary	GPE
gc-1013	334	3	193	CARDINAL
gc-1013	334	4	495–510	CARDINAL
gc-1013	336	1	workshop­neogene­of­central­and­south-eastern­europe,­28–31­5.­2017.­field­trip­	ORG
gc-1013	340	1	,­bakrač,­ k.	PERSON
gc-1013	342	1	gc.2011.10 kovačić,­m	WORK_OF_ART
gc-1013	349	1	pannonian)­boundary­in­central­paratethys­(vranović­locality,­slavonija).–­in:­horvat,­m.­&­wacha,­l.­(eds.):­abstract­book.­5th­croatian­geological­congress­with­international­participation,­osijek­23.–25.09.2015.­croatian­geological­survey,­136-137	ORG
gc-1013	351	1	m.,­sant,­k.	PERSON
gc-1013	357	1	k.,­hajek-tadesse,­v	PERSON
gc-1013	360	1	croatian	NORP
gc-1013	363	1	south-eastern europe	LOC
gc-1013	369	1	krolopp,­e.­(2002):­alsó	PERSON
gc-1013	369	2	fauna­a­görgeteg	CARDINAL
gc-1013	369	3	hungary	GPE
gc-1013	375	1	10.1016	CARDINAL
gc-1013	375	2	8172(00)00038	CARDINAL
gc-1013	376	1	magyar,­i.­&­sztanó,­o.­(2008):­is­there­a­messinian­unconformity­in­the­central­ paratethys?­–­stratigraphy,­5,­247–257	PERSON
gc-1013	385	1	hungarian	NORP
gc-1013	389	1	,­synak,­r	PERSON
gc-1013	397	1	tóth,­e	PERSON
gc-1013	401	1	149,­ 351–370.­	PERCENT
gc-1013	401	2	10.23928	CARDINAL
gc-1013	405	1	müller,­p.­&­magyar,­i.­(1992):­continuous­record­of­the­evolution­of­lacustrine­	PRODUCT
gc-1013	407	1	392.­doi:­10.2110	DATE
gc-1013	407	2	doi:­10.1007/978	ORG
gc-1013	410	1	,­bakrač,­ k.,­tišljar,­j.­galović,­i.­&­bortek,­ž.­(2003):­the­evolution­of­the­miocene­environments­in­the­slavonian­mts.­area­(northern­croatia).–­in:­vlahović,­ i.­&­tišljar,­j.­(eds.):­evolution­of­depositional­environments­from­the­paleozoic­to­the­quaternary­in­the­karst­dinarides­and­the­pannonian­basin.­field­trip­ guidebook,­22,­ias,­173–181	PERSON
gc-1013	411	1	pigott,­j.d.­&­radivojević,­d.­(2010):­seismic­stratigraphy­based­chronostratigraphy­(ssbc)­of­the­serbian­banat­region­of­the­pannonian­basin.–­central­european­journal­of­geosciences,­2/4,­481–500.­doi:­10.2478	PERSON
gc-1013	411	2	pikija,­m.­(2009):­vapnenačko-klastične­naslage­(sarmat,­panon­–­m5,6)­[limestone	NORP
gc-1013	411	3	1:300000	CARDINAL
gc-1013	411	4	pogácsás,­gy.­&­révész,­i.­(1987):­seismic­stratigraphic­and­sedimentological­ analysis­of­neogene­delta­features­in­the­pannonian­basin.–­annals­of­the­geological­institute­of­hungary,­70,­267–273	PERSON
gc-1013	412	1	prelogović,­e.	GPE
gc-1013	415	1	1998):­tectonic­activity­in­the­croatian­part­of­the­pannonian­basin.–­tectonophysics,­297,­283–293.­doi:­10.1016	CARDINAL
gc-1013	415	2	5	CARDINAL
gc-1013	415	3	hills­­-­in­hungarian].–­annals­of­the­geological­institute­of­hungary,­41/2,­ 27­p	ORG
gc-1013	416	1	rögl,­f.­(1996):­stratigraphic­correlation­of­the­paratethys­oligocene­and­miocene.–­ mitt.­gesell.­geol.­bergbaustud.­österr	PERSON
gc-1013	422	1	,­velić,­j	PERSON
gc-1013	424	1	hungary	GPE
gc-1013	425	1	geologia croatica,­56,­101–122.­ sebe,­k.	ORG
gc-1013	426	1	hungary	GPE
gc-1013	426	2	hungarian	NORP
gc-1013	434	1	sebe,­k.­(eds.):­neogene­of­the­paratethyan­region.­6th­workshop­on­the­neogene­ g eo lo	PERSON
gc-1013	444	1	petersi­bei­kadar­an­der­ save­(nordbosnien).–­annales­géologiques­de­la­péninsule­balkanique,­28,­177	GPE
gc-1013	444	2	216	CARDINAL
gc-1013	445	1	sütő-szentai,­m.­(1982):­organic­microplanktonic­biozones­in­the­pannonian­complex­of­central­transdanubia.–­annual­report­of­the­hungarian­geological­institute­ of­1980,­309–344	ORG
gc-1013	452	1	sütő-szentai,­m.­(1991):­szervesvázú­mikroplankton­zónák­magyarország­pannóniai­rétegösszletében.­újabb­adatok­a­zónációról­és­a­dinoflagellaták­evolúciójáról­	PERSON
gc-1013	455	1	bosta	PERSON
gc-1013	456	1	1	CARDINAL
gc-1013	456	2	hungary	GPE
gc-1013	456	3	hungarian	NORP
gc-1013	457	1	transylvanian­basin.–­földtani­közlöny,­138,­279–296	GPE
gc-1013	458	1	soliman,­a.­&­riding,­j.b.­(2017):­late­miocene­(tortonian)­gonyaulacacean­dinoflagellate­cysts­from­the­vienna­basin,­austria.–­review­of­palaeobotany­and­palynology,­244,­325–346.­doi:­10.1016/j.revpalbo.2017.02.003	ORG
gc-1013	458	2	szónoky,­m	ORG
gc-1013	460	1	müller,­p.	GPE
gc-1013	467	1	167–182	CARDINAL
gc-1013	473	1	,­lenkey,­ l.	PERSON
gc-1013	473	2	2013a):­a­tihanyi­	CARDINAL
gc-1013	473	3	lake balaton:	FAC
gc-1013	481	1	hungary	GPE
gc-1013	487	1	of­the­danube­/­kisalföld­basin:­interregional­correlation­of­depositional­systems,­	GPE
gc-1013	487	2	10.1515	CARDINAL
gc-1013	487	3	šikić,­k.	GPE
gc-1013	488	1	1979):­osnovna­	CARDINAL
gc-1013	488	2	karta­	GPE
gc-1013	488	3	1:100000,­tumač­za­list­zagreb­[basic	DATE
gc-1013	488	4	zagreb	ORG
gc-1013	490	1	in­croatian].–­fond­	GPE
gc-1013	496	1	j. sedgeo.2019.105566 tomljenović,­b.­&­csontos,­­l.­(2001):­neogene–quaternary­structures­in­the­ border­zone­between­alps,­dinarides­and­pannonian­basin­(hrvatsko­zagorje­and­ karlovac­basins,­croatia).–­int.­j.­earth­sciences­(geol.­rundschau),­90,­560–578.­	PERSON
gc-1013	498	1	croatia	GPE
gc-1013	498	2	geologia croatica	PERSON
gc-1013	498	3	62/2,­123–133.­doi:­10.4154/ gc.2009.11 uhrin,­a.	PERSON
gc-1013	509	1	2007):­palaeomagnetic­results­from­the­sarmatian	CARDINAL
gc-1013	509	2	vranović­section,­našice­quarry).–­geologia­croatica,­60/2,­	ORG
gc-1013	509	3	velić,­j.­(2007):­geologija­ležišta­nafte­i­plina.	GPE
gc-1013	511	1	miocene­sediments­of­the­ivanić­grad­formation­in­the­sava­depression­(nw­	PRODUCT
gc-1013	514	1	wijbrans,­j	PERSON
gc-1013	515	1	croatia	GPE
gc-1013	515	2	hungary	GPE
gc-1013	515	3	195	CARDINAL
gc-1013	515	4	1	CARDINAL