Romanian National Institute of Marine Geology and Geoecology GeoEcoMar

Bucharest, Romania

Romanian National Institute of Marine Geology and Geoecology GeoEcoMar

Bucharest, Romania
Time filter
Source Type

Roban R.D.,University of Bucharest | Krezsek C.,OMV Petrom | Melinte-Dobrinescu M.C.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar
Sedimentary Geology | Year: 2017

The mid Cretaceous is characterized by high eustatic sea-levels with widespread oxic conditions that made possible the occurrence of globally correlated Oceanic Red Beds. However, very often, these eustatic signals have been overprinted by local tectonics, which in turn resulted in Lower Cretaceous closed and anoxic basins, as in the Eastern Carpathians. There, the black shale to red bed transition occurs in the latest Albian up to the early Cenomanian. Although earlier studies discussed the large-scale basin configuration, no detailed petrography and sedimentology study has been performed in the Eastern Carpathians. This paper describes the Hauterivian to Turonian lithofacies and interprets the depositional settings based on their sedimentological features. The studied sections crop out only in tectonic half windows of the Eastern Carpathians, part of the Vrancea Nappe. The lithofacies comprises black shales interbedded with siderites and sandstones, calcarenites, marls, radiolarites and red shales. The siliciclastic muddy lithofacies in general reflects accumulation by suspension settling of pelagites and hemipelagites in anoxic (black shale) to dysoxic (dark gray and gray to green shales) and oxic (red shales) conditions. The radiolarites alternate with siliceous shales and are considered as evidence of climate changes. The sandstones represent mostly low and high-density turbidite currents in deep-marine lobes, as well as channel/levee systems. The source area is an eastern one, e.g., the Eastern Carpathians Foreland, given the abundance of low grade metamorphic clasts. The Hauterivian – lower Albian sediments are interpreted as deep-marine, linear and multiple sourced mud dominated systems deposited in a mainly anoxic to dysoxic basin. The anoxic conditions existed in the early to late Albian, but sedimentation changed to a higher energy mud/sand-dominated submarine channels and levees. This coarsening upwards tendency is interpreted as the effect of the Aptian to Albian compressional tectonics of the Carpathians. The deepening of the Moldavide Basin from the Cenomanian is most probably linked to a significant sea-level rise. © 2017 Elsevier B.V.

Stoica M.,University of Bucharest | Lazar I.,University of Bucharest | Krijgsman W.,University Utrecht | Vasiliev I.,University Utrecht | And 2 more authors.
Global and Planetary Change | Year: 2013

The thick and continuous Mio-Pliocene sedimentary successions of the Focşani Depression in the Dacian Basin of Romania provide an excellent opportunity to study the paleoecological changes in the Eastern Paratethys during the time when the Mediterranean and Black Sea experienced major sea level fluctuations related to the closure and re-opening of the marine connection to the Atlantic Ocean during the Messinian Salinity Crisis. These successions form the basis of high-resolution magneto-biostratigraphic studies that allow a detailed correlation to the standard Geological Time Scale. Here, we analyze the paleoenvironmental evolution of the East Carpathian foredeep by integrating micro- and macropaleontological data and sedimentological analyses. The ostracod and mollusc fossil associations fromthe Râmnicu Sǎrat river section indicate that the late Maeotian depositional environment was characterized by shallow waters and littoral to fluvio-deltaic sediments. The Maeotian-Pontian boundary (6.04 Ma) is marked by a marine ingression, comprising benthic (agglutinated and calcareous) and planktonic (Streptochilus spp.) foraminifera and nanofossils. Following this marine ingression, the Lower Pontian (Odessian; 6.04-5.8Ma) fauna shows an increased bathymetry of the basin. The presence of ostracod species with eye tubercles indicates depositional environments within the photic zone (b100 m). The Middle Pontian (Portaferrian; 5.8-5.5 Ma) is marked by a widespread sea level lowering resulting in dominant fluvio-deltaic conditions. This ecostratigraphy demonstrates that the main Messinian sea-level draw down (at 5.6-5.5 Ma) occurred in mid-Portaferrian times. Paleoenvironmental indicators show that the water level in the Foçsani Depression dropped less than 100 mduring Mediterranean desiccation. The Dacian Basin remained filled with water, suggesting a positive hydrological balance for the region. This is compatible with the presence of a shallow barrier at Dobrogea (the Galati passage), separating the Dacian Basin fromthe Black Sea Basin during the late Miocene. The Portaferrian-Bosphorian boundary (5.5 Ma) ismarked by a second transgressive event, but this time without marine foraminifera. We conclude that the Dacian Basin formed a semi-isolated entity during the Portaferrian and experienced connectivity to the Black Sea domain during the Odessian and Bosphorian. © 2012 Elsevier B.V.

Melinte-Dobrinescu M.C.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar | Roban R.-D.,University of Bucharest
Sedimentary Geology | Year: 2011

This study focused on the Cretaceous black shale successions, followed by red shales that crop out at the outer regions of the Romanian Carpathians, in the Moldavids. The oldest parts of the black shale units deposited in an abyssal plain during Late Valanginian-Late Barremian time; they are mainly characterized by hemipelagic and pelagic muddy siliciclastic rocks and carbonates, commonly intercalated with fine-grained turbidites. During the sedimentation of the middle part of the black shale units in the Late Barremian-Early Albian interval, the depth of the basin increased, as the carbonate hemipelagic sedimentation was replaced by a mainly siliceous one. Only a few thin turbidite intercalations are present. The youngest part (Albian pro parte) of the black shale units is characterized by a turbiditic sedimentation, with mainly sandy sequences of middle and lower deep-water fans. We may assume that the depth of the basin continuously decreased. The presence of authigenic glauconite in the Albian sandstones suggests a palaeoenvironmental change, linked to the occurrence of oxygenated turbidity current circulation. A significant shift in the sedimentation regime in the Eastern Carpathian Moldavids took place in the Late Albian, when Cretaceous Oceanic Red Beds (CORB) occurred. This type of sedimentation lasted up to the Coniacian. The lower part of the CORBs that contains radiolarites intercalated with variegated shales, pyroclastic tuffs and thin sandstones is interpreted as a hemipelagic and pelagic sedimentation in the abyssal plain environment, where rarely turbidites occurred. Upwards, there are mainly burrowed variegated red and green shales. The youngest parts of CORBs are characterized by increased thickness and frequency of the turbidites. While the main part of the CORB is carbonate free or has very low carbonate content, the upper part of these strata becomes rich in marl and mudstone strata, indicating a decrease of the basin-depth. The accumulation of black shales in the Eastern Carpathians during the Late Valanginian-Late Albian interval is linked to the existence of a small, silled basin of the Moldavian Trough, in which restricted circulation led to the density stratification of the water column, resulting in the deposition of anoxic Lower Cretaceous sediments (i.e., the black shales). Because of the tectonic deformation that took place within the Lower-Upper Cretaceous boundary interval, the restricted circulation had changed to an open circulation regime in the Moldavian Trough. Hence, the anoxic regime was progressively replaced by an oxic one, across the Albian-Cenomanian boundary interval. The beginning and the end of the CORBs in the Moldavid units depend thus on various palaeogeographic and palaeoenvironmental settings, and it was controlled by the regional tectonic activity. © 2010 Elsevier B.V.

Jipa D.C.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar | Olariu C.,University of Texas at Austin
Global and Planetary Change | Year: 2013

In the Late Neogene (Late Sarmatian s. l.-Dacian; 11 to 4 Ma) the Carpathian Mountains to Dacian Basin was an enclosed source-to-sink system. The volume of sediment eroded fromthe Carpathians (estimated fromprevious semi-quantitative studies) closely matches the volume of sediment deposited in the Dacian Basin (about 100,000 km3). The close values of the eroded and deposited sediment volume indicate the Carpathians as the main sediment source for Dacian Basin,with only limited input from adjacent areas. Based on depocenter thickness, grain size trend and paleocurrent data, two distinct areas in the Carpathian Mountains have been identified as themajor sediment sources during this time interval. Each source area most likely delivered sediments to different depocenters within the Dacian Basin creating distinct sediment routing and sinks. Because of the similar sediment volumes sourced in Carpathians and deposited in Dacian Basin connectivitywith adjacent basins did not significantly influence the sediment flux and routing of the Dacian Basin unless the sediment was bypassing the Dacian Basin. A probable sea-level drop of 50 to 100 m during Pontian (time of the Messinian Salinity Crisis in the Mediterranean Basin) did not inflict important morphological changes to the Carpathians - Dacian Basin source-to-sink system. The system of the semi-enclosed Dacian Basin appears to have been autonomous, efficiently trapping incoming clastic material and apparently preventing significant spillage to the larger and deeper Black Sea Basin until Romanian time when it was filled and depositional environments changed from marine/lacustrine to fluvial. © 2012 Elsevier B.V.

Balintoni I.,Babes - Bolyai University | Balica C.,Babes - Bolyai University | Seghedi A.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar | Ducea M.N.,University of Arizona
Precambrian Research | Year: 2010

The North Dobrogea orogen is a collage of dismembered terrane fragments between the Moesian platform and East European craton (Baltica). It records Alpine and Variscan deformation, magmatism and metamorphism. Its basement comprises three metamorphic complexes (Boclugea, Megina and Orliga) that are separated by tectonic boundaries. Detrital zircon U/Pb ages suggest the Boclugea and Orliga complexes represent two peri-Gondwanan terranes of Avalonian and Cadomian affinities, respectively. The new data clarify the original relationships between the North Dobrogea terranes, and Baltica and Moesia platform. © 2010 Elsevier B.V.

Dimitriu R.G.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar
Quaternary International | Year: 2012

An obvious discrepancy is noticed between the very few archaeological sites discovered until now on the Danube Delta plain area and the large number of such sites, whose ages range from the Middle Paleolithic to the Middle Ages and more recently, identified on its higher topography surroundings.The combined effects of the regional subsidence of the coast and delta area, with amplitudes of -2 to -4 mm/y and of the secular mean sea level rise (+0.5/1.0 mm/y) continuously change the " land-mean sea level" relative relationship, placing the prospective archaeo-cultural layer corresponding to the Late Prehistory - Antiquity period at a burial depth which now exceeds 4-5 m. This situation partly explains the limited success of the archaeological research carried out until now within the Danube Delta plain area and recommends a systematic use of the geophysical investigation methods in future. The integrated interpretation of the coastal zone bathymetry and sedimentology mappings and of the shoreline geomorphological evolution in time highlights the sedimentary processes that presently shape the littoral study zone allowing to divide it in sectors where either sediments accumulation or erosion processes prevail. The study draws attention to the împuţita - Câşla Vâdanei and Coşna - Vadu littoral sectors where the intense marine erosion of the shoreline and the adjacent seabed also imminently endangers their prospective archaeo-cultural load. © 2010 Elsevier Ltd and INQUA.

Seghedi A.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar
Turkish Journal of Earth Sciences | Year: 2012

An overview of lithological, palaeontological and geochronological evidence existing for the Palaeozoic formations from Dobrogea and Pre-Dobrogea has enabled a better understanding of the Palaeozoic history of these areas. The Lower Palaeozoic of Pre-Dobrogea, in places in continuity with the pelitic-silty facies of the underlying Vendian (Ediacaran) deposits, was one of the peri-Tornquist basins of Baltica, suggesting that the Scythian Platform in the Pre-Dobrogea basement represents the rift ed margin of the East European Craton. In North Dobrogea two types of Palaeozoic succession have formed in different tectonic settings. Deep marine Ordovician-Devonian deposits, including pelagic cherts and shales, associated with turbidites, and facing Devonian carbonate platform deposits of the East European Craton, form northward-younging tectonic units of an accretionary wedge, tectonically accreted above a south-dipping subduction zone. South of the accretionary prism, the basinal to shallow marine Silurian-Devonian deposits of North Dobrogea, showing a similar lithology to the East Moesian successions, accumulated on top of lowgrade Cambrian clastics with Avalonian affinity indicated by detrital zircons. Late Palaeozoic erosion was accompanied by deposition of continental alluvial, fluvial and volcano-sedimentary successions, overlying their basement above an imprecise Carboniferous gap. The low-grade metamorphic Boclugea terrane, showing Avalonian affinity, and the associated Lower Palaeozoic deposits represent East Moesian successions, docked to Baltica by the Lower Devonian and subsequently involved in the Hercynian orogeny, being affected by Late Carboniferous-Early Permian regional metamorphism and granite intrusion. The Late Carboniferous-Early Permian syn-tectonic sedimentation, regional metamorphism of Palaeozoic formations and development of a calc-alkaline volcano-plutonic arc indicate an active plate margin setting and an upper plate position of the Mǎcin-type successions during the Variscan collision, when the Orliga terrane, with Cadomian affinity, was accreted to Laurussia along a north-dipping subduction zone of the Rheic Ocean. The East Moesian Lower Palaeozoic succession, overstepping its Ediacaran basement, represents an Avalonian terrane, docked to the Baltica margin in the Early Palaeozoic. A narrow terrane detached from the Trans-European Suture Zone (TESZ) margin of the Baltica palaeocontinent forms a tectonic wedge within the East Moesian basement. The Palaeozoic sedimentary record of East Moesia shows a quartzitic facies in the Ordovician, graptolite shales in Upper Ordovician-Wenlock, black argillites in the Ludlow-Pridoli and fine-grained clastics in the Lower Devonian. Eifelian continental sandstones are followed by a carbonate platform from Givetian to Tournaisian times and coalbearing clastics in the Carboniferous, indicating a foredeep basin evolution. By the Eifelian both East Moesia and Pre-Dobrogea were part of Laurussia, sharing the same old red sandstone facies. The Permian is a time of rifting in Dobrogea and Pre-Dobrogea, although evidence for rifting in the East Moesian sedimentary record is very limited. In the eastern basins of Pre-Dobrogea, Permian rifting was accompanied by alkaline bimodal volcanism of the basalttrachyte association, that affected also the northern margin of North Dobrogea. Late Permian within-plate alkaline magmatic activity emplaced plutonic and hypabyssal complexes along the south-western margin of North Dobrogea. The model proposed for the Palaeozoic history based on existing data for the north-western margin of the Black Sea records early Palaeozoic docking to Baltica of the Avalonian terrane of East Moesia, including the Boclugea terrane of North Dobrogea. Late Carboniferous-Early Permian accretion of the Cadomian Orliga terrane from North Dobrogea, accompanied by Hercynian metamorphism and granite intrusion, correlates with the closure of the Rheic Ocean. Subsequently, Avalonian and Cadomian terranes, together with a narrow terrane detached from the TESZ margin of Baltica palaeocontinent, were displaced southward along the strike-slip fault system of the TESZ. © TÜBİTAK.

Jipa D.C.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar
Quaternary International | Year: 2014

New information on the entire Lower Danube Basin was obtained through the selection, reworking and integration of previously published data concerning the loess accumulations from the Romanian Danube Plain, Bulgarian Danube Plain, and Dobrogea Highland. A conceptual sedimentary model was outlined, based on the integrated textural and isopach maps of the Lower Danube loess and loess-like deposits. The loess in the Lower Danube Basin appears as an accumulation with the coarsest-grained and thickest loess deposits situated along the Lower Danube River channel. Both grain-size and thickness gradually decrease to the basin margin. During the initial genetic stage, the Lower Danube loess basin functioned as a large flood plain. The alluvial and eolian loess generation stages repeatedly alternated. Several sources supplied the Lower Danube loess clastics, determining the Danubian, Carpathian/Balkan and Black Sea littoral provenance of the detrital material. © 2013 Elsevier Ltd and INQUA.

Jipa D.C.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar
Geo-Eco-Marina | Year: 2014

The main goal of this study is the sedimentogenesis of the loess-like deposits in the Lower Danube Basin. A pros and cons genetic analysis of these deposits is carried out in the paper. Resulting from this analysis, the optimal logical solution to explain the distal loess-like sedimentation in the Lower Danube Basin is the joint action of the alluvial and eolian processes. The initial alluvial sedimentation (not solely by overbank flows) could have been continued and extended by the eolian action. The loess-like deposits of the Lower Danube Basin are sedimentary accumulations of primary genesis. © 2014, National Research and Development Institute for Marine Geology and Geoecology. All rights reserved.

Jipa D.C.,Romanian National Institute of Marine Geology and Geoecology GeoEcoMar
Geo-Eco-Marina | Year: 2015

Several large scale geological events controlled the Dacian Basin inception. The Dacian Basin can be defined as the southern Carpathian Foredeep area outlined after a long migration process, where the sediment accumulation was stimulated by the Carpathian orogenic climax and organized within a morphologically closed basin and in a Neogene Paratethys brackish-water ecosystem. © 2015, National Research and Development Institute for Marine Geology and Geoecology. All rights reserved.

Loading Romanian National Institute of Marine Geology and Geoecology GeoEcoMar collaborators
Loading Romanian National Institute of Marine Geology and Geoecology GeoEcoMar collaborators