干旱区生态环境知识资源中心(Arid): The transition from a closed to an open lake in the Pannonian Basin System (Croatia) during the Miocene Climatic Optimum: Sedimentological evidence of Early Miocene regional aridity

Arid

DOI	10.1016/j.palaeo.2021.110786
	The transition from a closed to an open lake in the Pannonian Basin System (Croatia) during the Miocene Climatic Optimum: Sedimentological evidence of Early Miocene regional aridity
	Pavelic, Davor; Kovacic, Marijan; Tibljas, Darko; Galic, Ivo; Markovic, Frane; Pavicic, Ivica
通讯作者	Kovacic, M (corresponding author)，Univ Zagreb, Fac Sci, Horvatovac 95, HR-10000 Zagreb, Croatia.
来源期刊	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
ISSN	0031-0182
EISSN	1872-616X
出版年	2022
卷号	586
英文摘要	In the area of the North Croatian Basin, as the south-western part of the Pannonian Basin System, a lake that was characterized by mainly dolomite deposition evolved in the late Early Miocene. The dolomites precipitated directly from the water body, and are associated with tuffites and marls, together with minerals such as analcime, hydrous Ca-bearing magnesium carbonate, and natrolite. This indicates deposition in a shallow, hydrologically closed lake of highly alkaline waters controlled by an arid climate in the first stage of its evolution. The second evolutionary stage is represented by the intercalation of sandstones as a result of gravity flows, and dolomites that reflect changes of hydrologically open and closed lacustrine environments controlled by the frequent alternation of humid and arid climates. The third stage, that probably commenced in the Middle Miocene, indicates the formation of a long-lived, hydrologically mostly open lake, characterized by deposition of siliciclastics by gravity flows. The whole lacustrine depositional sequence coincides with the Miocene Climatic Optimum generally characterized by hot and warm, and humid climates. However, the evolution of the closed lake that is correlative with similar lakes in northern Bosnia and central Serbia, indicates the existence of an arid zone in the region that was confined by areas characterized by a more humid climate in the late Early Miocene.
英文关键词	Lacustrine deposition Climate controls Arid region South-Eastern Europe Early Miocene
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000737259500002
WOS关键词	EARLY-MIDDLE MIOCENE ; CENTRAL PARATETHYS ; PLAYA-LAKE ; LACUSTRINE SEDIMENTATION ; EVOLUTION ; NEOGENE ; STRATIGRAPHY ; PART ; PRECIPITATION ; ENVIRONMENTS
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS研究方向	Physical Geography ; Geology ; Paleontology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/376890
作者单位	[Pavelic, Davor; Galic, Ivo; Pavicic, Ivica] Univ Zagreb, Fac Min Geol & Petr Engn, Pierottijeva 6, HR-10000 Zagreb, Croatia; [Kovacic, Marijan; Tibljas, Darko; Markovic, Frane] Univ Zagreb, Fac Sci, Horvatovac 95, HR-10000 Zagreb, Croatia
推荐引用方式 GB/T 7714	Pavelic, Davor,Kovacic, Marijan,Tibljas, Darko,et al. The transition from a closed to an open lake in the Pannonian Basin System (Croatia) during the Miocene Climatic Optimum: Sedimentological evidence of Early Miocene regional aridity[J],2022,586.
APA	Pavelic, Davor,Kovacic, Marijan,Tibljas, Darko,Galic, Ivo,Markovic, Frane,&Pavicic, Ivica.(2022).The transition from a closed to an open lake in the Pannonian Basin System (Croatia) during the Miocene Climatic Optimum: Sedimentological evidence of Early Miocene regional aridity.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,586.
MLA	Pavelic, Davor,et al."The transition from a closed to an open lake in the Pannonian Basin System (Croatia) during the Miocene Climatic Optimum: Sedimentological evidence of Early Miocene regional aridity".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 586(2022).