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1.

001-es BibID:BIBFORM095932
035-os BibID:(cikkazonosító)100858
Első szerző:Palcsu László (fizikus)
Cím:Long-term time series of environmental tracers reveal recharge and discharge conditions in shallow karst aquifers in Hungary and Slovakia / László Palcsu, Alena Gessert, Marianna Túri, Attila Kovács, István Futó, Judit Orsovszki, Anita Puskás-Preszner, Marjan Temovski, Gabriella Koltai
Dátum:2021
ISSN:2214-5818
Tárgyszavak:Természettudományok Környezettudományok idegen nyelvű folyóiratközlemény külföldi lapban
folyóiratcikk
Megjelenés:Journal of Hydrology: Regional Studies. - 36 (2021), p. 1-12. -
További szerzők:Gessert, Alena Túri Marianna (1988-) (geográfus-geoinformatikus) Kovács Attila Futó István (fizikus) Orsovszki Judit Puskás-Preszner Anita (1984-) (vegyész) Temovski, Marjan Koltai Gabriella
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2.

001-es BibID:BIBFORM091780
Első szerző:Palcsu László (fizikus)
Cím:Preliminary Results of a Stalagmite Palaeoclimate Record Covering the Transition of the Last Interglacial/Glacial Period / László Palcsu, László Elemér, Gabriella Kiss, István Futó, Marianna Túri, Marjan Temovski, Hai Cheng
Dátum:2017
ISBN:978-973-0-24503-5
Tárgyszavak:Természettudományok Földtudományok előadáskivonat
Megjelenés:14th Workshop of the European Society for Isotope Research, ESIR 2017 : Book of Abstracts / Ed. Roxana Elena Ionete. - p. 103. -
További szerzők:László Elemér (1987-) (meteorológus előrejelző szakiránnyal) Kiss Gabriella Ilona (1992-) (vegyész) Futó István (fizikus) Túri Marianna (1988-) (geográfus-geoinformatikus) Temovski, Marjan Cheng, Hai
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3.

001-es BibID:BIBFORM083342
Első szerző:Palcsu László (fizikus)
Cím:Local temperature calibration of carbonate-water oxygen isotope fractionation and clumped isotopes (?47) in a karstic freshwater limestone environment / László Palcsu, Marianna Túri, István Futó, János Kovács, Péter Szabó, Judit Orsovszki, Marjan Temovski, László Rinyu
Dátum:2019
ISSN:1029-7006 1607-7962
Megjegyzések:Oxygen isotope ratios of carbonates are widely used as palaeoclimate indicators since isotope fractionation between the carbonate and the water phase is temperature dependent. The available empirical equationsare reliable for deposits which are precipitated under isotopic equilibrium. However, in many cases, precipitation of abiotic carbonate sediments (flowstones, freshwater limestones, travertines, tufas, etc.) can occur with fast CO2 degassing, which tends to result in a kinetic fractionation of isotope compositions. In karst environments, freshwater limestone is precipitated from cold spring waters as the creek is flowing and the dissolved CO2 is released from the water. This process creates tufa deposits. Our aim is to investigate the suitability of the tufa deposits as a palaeoclimate archive, even if kinetic fractionation plays a significant role during carbonate formation. In Mecsek Mts, Hungary, tufa deposits can be found in karst valleys. We have chosen a karst spring of constant annual temperature of 10.3 ?C. As the water is flowing away from the spring, it is heated up or cooled down by the ambient air, so the annual temperature variation is increasing with the distance from the spring. In 2015, glass plates, as well as temperature loggers, were placed in the water downstream from the spring along with a 200 m long section, so that carbonate could be precipitated onto the glass surface. In 3-4 weeks the glass plates are replaced. Daily average temperatures of the water vary between 0 and 25.6 ?C, while temperatures averaged to the sampling periods vary between 0.8 and 20.1 ?C. The first ? 18Ocarb and clumped isotope results show a significant temperature dependence, although the equations are shifted from those that are reliable to equilibrium circumstances. However, both ? 18Ocarb-T and ?47-T relationships seem to be significant and therefore applicable to the old tufa layers for reconstructing palaeotemperatures.
Tárgyszavak:Természettudományok Környezettudományok idézhető absztrakt
folyóiratcikk
Megjelenés:Geophysical Research Abstracts. - 21 (2019), p. 8493. -
További szerzők:Túri Marianna (1988-) (geográfus-geoinformatikus) Futó István (fizikus) Kovács János Szabó Péter Orsovszki Judit Temovski, Marjan Rinyu László (fizikus)
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4.

001-es BibID:BIBFORM074801
035-os BibID:(Cikkazonosító)12813 (WOS)000442608400001 (Scopus)85052329220
Első szerző:Palcsu László (fizikus)
Cím:Modulation of Cosmogenic Tritium in Meteoric Precipitation by the 11-year Cycle of Solar Magnetic Field Activity / László Palcsu, Uwe Morgenstern, Jürgen Sültenfuss, Gabriella Koltai, Elemér László, Marjan Temovski, Zoltán Major, Judit T. Nagy, László Papp, Carmen Varlam, Ionut Faurescu, Marianna Túri, László Rinyu, György Czuppon, Emese Bottyán, A. J. Timothy Jull
Dátum:2018
ISSN:2045-2322
Megjegyzések:The relationship between the atmospheric concentration of cosmogenic isotopes, the change of solar activity and hence secondary neutron flux has already been proven. The temporal atmospheric variation of the most studied cosmogenic isotopes shows a significant anti-correlation with solar cycles. However, since artificial tritium input to the atmosphere due to nuclear-weapon tests masked the expected variations of tritium production rate by three orders of magnitude, the natural variation of tritium in meteoric precipitation has not previously been detected. For the first time, we provide clear evidence of the positive correlation between the tritium concentration of meteoric precipitation andneutron flux modulated by solar magnetic activity. We found trends in tritium time series for numerouslocations worldwide which are similar to the variation of secondary neutron flux and sun spot numbers.This variability appears to have similar periodicities to that of solar cycle. Frequency analysis, crosscorrelation analysis, continuous and cross wavelet analysis provide mathematical evidence that thecorrelation between solar cycle and meteoric tritium does exist. Our results demonstrate that theresponse of tritium variation in precipitation to the solar cycle can be used to help us understand its rolein the water cycle.
Tárgyszavak:Természettudományok Földtudományok idegen nyelvű folyóiratközlemény külföldi lapban
folyóiratcikk
tritium, solar cycle
Megjelenés:Scientific Reports. - 8 : 1 (2018), p. 1-9. -
További szerzők:Morgenstern, Uwe Sültenfuss, Jürgen Koltai Gabriella László Elemér (1987-) (meteorológus előrejelző szakiránnyal) Temovski, Marjan Major Zoltán Nagy Judit, T. (1976-) (matematika tanár, közgazdász) Papp László Varlam, Carmen Faurescu, Ionut Túri Marianna (1988-) (geográfus-geoinformatikus) Rinyu László (fizikus) Czuppon György Bottyán Emese Jull, A. J. Timothy (1951-) (radiocarbon scientist)
Pályázati támogatás:GINOP-2.3.2.-15-2016-00009 'ICER'
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5.

001-es BibID:BIBFORM103310
035-os BibID:(WOS)000805561200044 (Scopus)85131125056 (cikkazonosító)9202
Első szerző:Temovski, Marjan
Cím:Combined use of conventional and clumped carbonate stable isotopes to identify hydrothermal isotopic alteration in cave walls / Marjan Temovski, László Rinyu, István Futó, Kata Molnár, Marianna Túri, Attila Demény, Bojan Otoničar, Yuri Dublyansky, Philippe Audra, Victor Polyak, Yemane Asmerom, László Palcsu
Dátum:2022
ISSN:2045-2322
Megjegyzések:Alteration of conventional carbonate stable isotopes (delta O-18, delta C-13) in cave walls has been shown to be a useful tool to identify cave formation driven by deep-seated processes, i.e., hypogene karstification. If combined with a prior information on the paleowater stable isotope composition, further insights can be obtained on the temperature and the source of the paleowater. Clumped isotope composition (Delta(47)) of carbonates is an independent measurement of temperature, and if combined with the conventional stable isotopes, can provide information on the paleowater stable isotope composition. On the example of Provalata Cave (N. Macedonia), we apply for the first time, both conventional and clumped stable isotope analysis, and identify two different isotope alteration trends, reflecting two distinct hydrothermal events: an older, hotter one, where isotope alteration was likely related to isotope diffusion, lowering the delta O-18 values of the carbonate; and a younger one, related to the cave formation by low-temperature CO2-rich thermal waters, with dissolution-reprecipitation as the alteration mechanism, causing decrease in delta O-18 values, and unexpected increase in delta C-13 values. The findings are further corroborated by additional insight from optical petrography and cathodoluminescence microscopy, as well as fluid inclusion analysis of secondary calcite crystals related to the cave forming phase.
Tárgyszavak:Természettudományok Fizikai tudományok idegen nyelvű folyóiratközlemény külföldi lapban
folyóiratcikk
Megjelenés:Scientific Reports. - 12 : 1 (2022), p. 1-17. -
További szerzők:Rinyu László (fizikus) Futó István (fizikus) Molnár Kata Túri Marianna (1988-) (geográfus-geoinformatikus) Demény Attila Otoničar, Bojan Dublyansky, Yuri Audra, Philippe Polyak, Victor Asmerom, Yemane Palcsu László (1975-) (fizikus)
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6.

001-es BibID:BIBFORM090692
Első szerző:Temovski, Marjan
Cím:Multi-method geochemical characterization of groundwater from a hypogene karst system / Temovski Marjan, Túri Marianna, Futó István, Braun Mihály, Molnár Mihály, Palcsu László
Dátum:2021
ISSN:1431-2174
Megjegyzések:An approach, combining several geochemical methods, was used to determine the groundwater properties and components of a hypogene karst system, where sampling is restricted only to the spring sites, and with a limited number of available sampling locations. Radiogenic isotopes (3H, 14C) were used to constrain the groundwater mean residence time and separate different groundwater components. Noble gases, stable isotopes of water (?18O, ?2H), dissolved inorganic carbon (?13C) and dissolved sulfate (?34S, ?18O), and major ion and trace element composition were used to identify the source of water, its chemical evolution and water?rock interactions, as well as to identify the contribution and composition of endogenic gases. This approach was applied to three low-temperature thermal springs located in Mariovo (North Macedonia) associated with fossil hypogene caves, previously identified by morphological and geochemical studies of caves and cave deposits. Based on the obtained results, the main studied springs represent an output part of a regional hypogene karst groundwater system with a deep-circulating (~1 km), old (~15 ka), thermal (?60 ?C) water, which mixes with young (<50 years), cold (<14 ?C) and shallow epigene karst groundwater. The output parts are structurally controlled, at the interception of low topography and deep faults, along which the groundwater interacts with deep-seated gases, dominantly CO2 of metamorphic origin (?13C of +4.5? VPDB), with some contribution of mantle helium. The thermal karst groundwater interacts at depth with volcanic rocks from the nearby Neogene-Quaternary volcanic complex, as well as with metamorphic basement rocks and granitoids.
Tárgyszavak:Természettudományok Földtudományok idegen nyelvű folyóiratközlemény külföldi lapban
folyóiratcikk
hipogén karszt
stabil izotóp
Észak-Macedónia
karsztvíz
Megjelenés:Hydrogeology Journal. - 29 (2021), p. 1129-1152. -
További szerzők:Túri Marianna (1988-) (geográfus-geoinformatikus) Futó István (fizikus) Braun Mihály (1966-) (vegyész, analitikus) Molnár Mihály (1974-) (fizikus) Palcsu László (1975-) (fizikus)
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7.

001-es BibID:BIBFORM073790
Első szerző:Temovski, Marjan
Cím:Sulfur and oxygen isotopes in the gypsum deposits of the Provalata sulfuric acid cave (Macedonia) / Temovski Marjan, Futó István, Túri Marianna, Palcsu László
Dátum:2018
ISSN:0169-555X
Megjegyzések:Sulfur stable isotopes from cave sulfates (mainly gypsum) have been used in a number of studies to trace the source of sulfur in caves formed by sulfuric acid, but only few studies apply combined use of sulfur and oxygen stable isotopes to further understand the processes operating in sulfuric acid speleogenesis (SAS). Here we present results of a detailed study of the distribution of sulfur and oxygen stable isotopes within the gypsum deposits formed during sulfuric acid speleogenesis of Provalata Cave (Macedonia). The ?18O (vs VSMOW) values range between ?3.9? and +8.2?, and the ?34S (vs CDT) values between ?7.5? and +0.7?. We found a strong positive correlation between the ?18O and ?34S values, with a 0.5? increase in the ?34S for every 1? increase in the ?18O, indicating that both oxygen and sulfur isotopes were concurrently affected during the oxidation process. We attribute these effects to be either due to environmental control (concentrations of H2S and O2) or due to isotope fractionation during multi-step microbial oxidation, also affected by the environmental conditions. Additionally a shift of +1.85? in the ?34S values prior to the H2S oxidation is found, indicating evolution of the H2S ?34S in the SAS system. The wide range of both ?18O and ?34S values in the gypsum deposits of the small Provalata Cave show that both the number of samples and their location can be an important factor for the understanding of sulfuric acid speleogenesis using stable isotopes.
Tárgyszavak:Természettudományok Földtudományok idegen nyelvű folyóiratközlemény külföldi lapban
oxigén stabil izotóp
kén stabil izotóp
hipogén karszt
gipsz kivállások
Megjelenés:Geomorphology. - 315 (2018), p. 80-90. -
További szerzők:Futó István (fizikus) Túri Marianna (1988-) (geográfus-geoinformatikus) Palcsu László (1975-) (fizikus)
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8.

001-es BibID:BIBFORM111676
035-os BibID:(cikkazonosító)13702
Első szerző:Túri Marianna (geográfus-geoinformatikus)
Cím:New estimation to the turnover time of Lake Ohrid: an environmental isotope and noble gas study / Marianna Túri, Marjan Temovski, Gabriella Ilona Kiss, István Csige, László Palcsu
Dátum:2023
Tárgyszavak:Természettudományok Földtudományok előadáskivonat
könyvrészlet
Megjelenés:EGU General Assembly Conference Abstracts / Egusphere. - p. 13702
További szerzők:Temovski, Marjan Kiss Gabriella Ilona (1992-) (vegyész) Csige István (1962-) (fizikus) Palcsu László (1975-) (fizikus)
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9.

001-es BibID:BIBFORM106949
Első szerző:Túri Marianna (geográfus-geoinformatikus)
Cím:ICER carbonate clumped isotope analysis of karst deposits / Marianna Túri, Andrea Czébely, Diána Kiss, Marjan Temovski, László Palcsu, László Rinyu
Dátum:2022
Megjegyzések:In April 2018, a 253 Plus 10 kV isotope ratio mass spectrometer equipped with a Kiel IV automatic carbonate device (Thermo Scientific) was installed at the Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Debrecen, Hungary. Beside the analysis of the conventional carbon and oxygen isotope composition of small carbonate samples, the main application of our system is the clumped isotope thermometry of different kind of carbonate samples. The clumped carbonate measurements are carried out following the methodology of Bernasconi et al. [1]. Carbonate replicate samples (100-110 ?g) are digested by three drops of 1.95 g/cm3 phosphoric acid in the Kiel IV carbonate device. The evolved CO2 is passed through a micro-volume inlet system, which contains two LN2 traps and a Porapak trap in order to eliminate the possible hydrocarbon contaminants. The Easotope software is used for data evaluation of the measurements using the Brand parameters [2] and the carbon dioxide equilibrium scales [3, 4]. To demonstrate the achievable accuracy, precision and long-term stability of the measurement system at ICER, we analyzed international carbonate reference materials and proposed standards (ETH4, IAEA-C1, IAEA-C2, NBS-18, NBS-19, Merck Carbonate) and naturally formed travertine samples (known formation temperatures are in the range of 5-95?C) and compared them to formerly published data of two reputable laboratories from the clumped community [1, 5]. We also applied clumped carbonate analysis to several karst related research topics. One aspect is the suitability of tufa deposits as a paleoclimate archive, even if kinetic fractionation might play a significant role during carbonate formation. Another aspect is the application of clumped isotope thermometry to mammillary speleothems and hydrothermal carbonates as part of paleoclimate and speleogenetic studies. In the poster we will present our current achievements in the field of carbonate clumped isotope measurement, as well as some results on clumped isotope analysis of various carbonate deposits (tufa, mammillary speleothems, hydrothermal carbonates, dolomites) from different karst environments.
Tárgyszavak:Természettudományok Földtudományok előadáskivonat
könyvrészlet
Megjelenés:Climate Change : The Karst Record IX (KR9) Programme & abstract / eds. Gina Moseley, Mojgan Soleimani, Linda Partl, et al. - p. 164. -
További szerzők:Czébely Andrea (1983-) (biológus) Kiss Diána Temovski, Marjan Palcsu László (1975-) (fizikus) Rinyu László (fizikus)
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10.

001-es BibID:BIBFORM083373
Első szerző:Túri Marianna (geográfus-geoinformatikus)
Cím:Paleotemperature reconstruction using environmental isotopes and noble gases in groundwater in Morocco / Marianna Túri, Radouan Saadi, Hamid Marah, Marjan Temovski, Mihály Molnár, László Palcsu
Dátum:2020
ISSN:1431-2174
Megjegyzések:A Turonian limestone-dolomite aquifer from the Tadla basin of Morocco was analysed using a multi-tracer approach (?18O, ?2H, ?13C, 3H, 14C and noble gases) to reconstruct the paleotemperature evolution from the late Pleistocene to the Holocene. The Turonian aquifer was found to be suitable for a groundwater-based paleoclimate reconstruction, representing the Holocene?late Pleistocene epochs. After correction for young water contribution, mean residence times (MRTs) of groundwater were calculated using the Pearson radiocarbon model. Additionally, terrigenic helium content was used as an age indicator. Noble gas temperature (NGT) results from wells with groundwater ages corresponding to glacial periods showed an average of 17.2???1.7?C. In contrast, samples of recent recharge water gave a mean NGT of 25.2???1.3?C. This reveals a temperature difference of 8.0???2.1 ?C between the Holocene and late Pleistocene. This significant Pleistocene?Holocene temperature difference observed in Africa has considerable significance and can be extended to address an important topic relating to the nature of the wet epochs during which the fossil aquifers of North Africa were recharged. It is evident that this aquifer was recharged during both interglacial (warm) and glacial (cool) wet periods.
Tárgyszavak:Természettudományok Földtudományok idegen nyelvű folyóiratközlemény külföldi lapban
folyóiratcikk
felszín alatti vizek
stabil izotópok
radiokarbon
nemes gázok
Megjelenés:Hydrogeology Journal. - 28 (2020), p. 973-986. -
További szerzők:Saadi, Radouan Marah, Hamid Temovski, Marjan Molnár Mihály Palcsu László (1975-) (fizikus)
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