TY - JOUR
AU - Cseresznyés, Dóra
AU - Király, Csilla
AU - Gál, Á
AU - Papucs, A
AU - Kónya, P
AU - Lakos, I
AU - Kovács, Ivett
AU - Rinyu, László
AU - Szamosfalvi, Á
AU - Szabó, Csaba
AU - Falus, György
AU - Czuppon, György
TI - Surface occurrence of dawsonite and natural CO2 emanation in Covasna, in the Eastern Carpathians: A stable isotope study
JF - CHEMICAL GEOLOGY
J2 - CHEM GEOL
VL - 645
PY - 2024
SN - 0009-2541
DO - 10.1016/j.chemgeo.2023.121883
UR - https://m2.mtmt.hu/api/publication/34445854
ID - 34445854
N1 - Lithosphere Fluid Research Lab (LRG), Eötvös Loránd University (ELTE), Pázmány Péter sétány 1/C, Budapest, 1117, Hungary
Doctoral School of Environmental Science, Eötvös Loránd University (ELTE), Pázmány Péter sétány 1/C, Budapest, 1117, Hungary
Geographical Institute (GI), Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network, Budaörsi út 45, Budapest, 1112, Hungary
Department of Geology, Babeș-Bolyai University, Kogălniceanu str. 1., Cluj, RO-400084, Romania
County Nature Conservation and Mountain Rescue Center, Gábor Áron str. 1., Sfântu Gheorghe, RO-520003, Romania
Directorate of Geology, Supervisory Authority for Regulatory Affairs (SARA), Sas utca 20-22., Budapest, 1051, Hungary
Institute for Geological and Geochemical Research, HUN-REN Research Centre for Astronomy and Earth Sciences, Budaörsi út 45, Budapest, 1112, Hungary
CSFK, MTA Centre of Excellence, Konkoly Thege Miklós út 15–17, Budapest, 1121, Hungary
Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research (ATOMKI), HUN-REN, Bem tér 18/c., Debrecen, 4026, Hungary
Institute of Earth Physics and Space Science, HUN-REN, Csatkai Endre utca 6-8., Sopron, 9400, Hungary
Export Date: 15 January 2024
Correspondence Address: Czuppon, G.; Institute for Geological and Geochemical Research, Budaörsi út 45, Hungary; email: czuppon@geochem.hu
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Demény, Attila
AU - Czuppon, György
AU - Kern, Zoltán
AU - Hatvani, István Gábor
AU - Topál, Dániel
AU - Karlik, Máté
AU - Surányi, Gergely
AU - Molnár, Mihály
AU - Kiss, Gabriella Ilona
AU - Szabó, Máté Zoltán
AU - Shen, CC
AU - Hu, HM
AU - May, Zoltán
TI - A speleothem record of seasonality and moisture transport around the 8.2 ka event in Central Europe (Vacska Cave, Hungary)
JF - QUATERNARY RESEARCH
J2 - QUATERNARY RES
VL - 118
PY - 2024
SP - 195
EP - 210
PG - 16
SN - 0033-5894
DO - 10.1017/qua.2023.33
UR - https://m2.mtmt.hu/api/publication/34082661
ID - 34082661
N1 - Published online: 28 July 2023
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Demény, Attila
AU - Berentés, A
AU - Rinyu, László
AU - Kovács, Ivett
AU - Surányi, Gergely
AU - Virág, Magdolna
TI - Subaqueous carbonate speleothems as paleotemperature archives – clumped isotope thermometry and stable isotope compositions of inclusion-hosted wate
JF - INTERNATIONAL JOURNAL OF SPELEOLOGY
J2 - INT J SPELEOL
VL - 53
PY - 2024
IS - 1
SP - 25
EP - 37
PG - 13
SN - 0392-6672
DO - 10.5038/1827-806X.53.1.2480
UR - https://m2.mtmt.hu/api/publication/34659670
ID - 34659670
N1 - Funding Agency and Grant Number: Balaton Uplands National Park [102-2/2022]; Eotvos Lorand Research Network; European Union [GINOP-2.3.2-15-2016-00009 'ICER']; Hungarian State; European Regional Development Fund; [SA-41/2021]
Funding text: The sampling conducted for this study in Berger Karoly Cave was permitted by the directorate of the Balaton Uplands National Park (No. 102-2/2022) . Rezso Szilaj and Denes Szieberth provided essential help during sampling in Berger Karoly and Molnar Janos caves, respectively. The authors are indebted to Ariana Gugora for polishing the English of the manuscript. Constructive reviews and helpful comments of three anonymous reviewers, and the editorial handling by Bogdan P. Onac are gratefully thanked. The study was financed by the Eotvos Lorand Research Network (projects SA-41/2021; ELKH KEP-1/2020) . The clumped isotope facility of the Institute for Nuclear Research was supported by the European Union and the Hungarian State, co -financed by the European Regional Development Fund in the project of GINOP-2.3.2-15-2016-00009 'ICER'.
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Fernandez, A.
AU - Løland, M. H.
AU - Maccali, J.
AU - Krüger, Y.
AU - Vonhof, H. B.
AU - Sodemann, H.
AU - Meckler, A. N.
TI - Characterization and Correction of Evaporative Artifacts in Speleothem Fluid Inclusion Isotope Analyses as Applied to a Stalagmite From Borneo
JF - GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
J2 - GEOCHEM GEOPHY GEOSY
VL - 24
PY - 2023
IS - 6
SN - 1525-2027
DO - 10.1029/2023GC010857
UR - https://m2.mtmt.hu/api/publication/34040121
ID - 34040121
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Honiat, C
AU - Koltai, G
AU - Dublyansky, Y
AU - Edwards, RL
AU - Zhang, H
AU - Cheng, H
AU - Spötl, C
TI - A paleoprecipitation and paleotemperature reconstruction of the Last Interglacial in the southeastern Alps
JF - CLIMATE OF THE PAST
J2 - CLIM PAST
VL - 19
PY - 2023
IS - 6
SP - 1177
EP - 1199
PG - 23
SN - 1814-9324
DO - 10.5194/cp-19-1177-2023
UR - https://m2.mtmt.hu/api/publication/34020329
ID - 34020329
N1 - Funding Agency and Grant Number: Austrian Science Fund [P300040]; National Natural Science Foundation of China [41888101]
Funding text: This research has been supported by the Austrian Science Fund (grant no. P300040) and the National Natural Science Foundation of China (grant no. 41888101).
AB - Abstract. The Last Interglacial (LIG, ∼130–116 ka) was one of the warmest interglacials of the past 800 000 years and an important test bed for future climate conditions warmer than today. LIG temperature reconstructions from marine records and paleoclimate models show that middle and high northern latitudes were considerably warmer (by about 2 to5 ∘C) compared to today. In central Europe, the LIG has been widely studied using pollen and more recently chironomids preserved in lakesediments. While these bio-archives document temperature changes across the LIG, they are commonly poorly constrained chronologically. Speleothems and fluid inclusions contained therein offer superior age control and provide information on past climate, including qualitative and partly alsoquantitative records of temperature and precipitation. Here, we present aprecisely dated fluid-inclusion record based on seven speleothems from twocaves in the southeastern Alps (Obir and Katerloch) and use a δ2H/T transfer function to reconstruct regional LIG temperatures. We report a temperature change across the glacial–interglacial transition of 5.2±3.1 ∘C and peak temperatures at ∼127 ka of 2.4±2.8 ∘C above today's mean (1973–2002). The fluid-inclusion δ2H record of these speleothems exhibits millennial-scale events during the LIG that are not well expressed in the δ18Ocalcite. The early LIG in the southeastern Alps was marked by an important climate instability followed by progressively more stable conditions. Our record suggests that the southeastern Alps predominantly received Atlantic-derived moisture during the early and middle LIG, while more Mediterranean moisture reached the study site at the end of the LIG, buffering the speleothem δ18Ocalcite signal. The return towards colder conditions is marked by an increase in δ13Cstarting at ∼118 ka, indicating a decline in the vegetation and soil activity.
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Baloghné Kiss, Gabriella
AU - Molnár, Kata
AU - Benkó, Zsolt
AU - Skoda, P
AU - Kapui, Zsuzsanna
AU - Garuti, G
AU - Zaccarini, F
AU - Palcsu, László
AU - Czuppon, György
TI - Tracing the Source of Hydrothermal Fluid in Ophiolite-Related Volcanogenic Massive Sulfide Deposits: A Case Study from the Italian Northern Apennines
JF - MINERALS
J2 - MINERALS-BASEL
VL - 13
PY - 2023
IS - 1
PG - 18
SN - 2075-163X
DO - 10.3390/min13010008
UR - https://m2.mtmt.hu/api/publication/33527205
ID - 33527205
N1 - Department of Mineralogy, Institute of Geography and Earth Sciences, ELTE Eötvös Loránd University, Budapest, 1117, Hungary
Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Debrecen, 4026, Hungary
Department of Mineralogy and Geology, University of Debrecen, Debrecen, 4032, Hungary
Geosciences Programme, Faculty of Science, University Brunei Darussalam, Bandar Seri Begawan, BE1410, Brunei Darussalam
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network, Budaőrsi út 45, Budapest, 1112, Hungary
Export Date: 9 February 2023
Correspondence Address: Kiss, G.B.; Department of Mineralogy, Hungary; email: gabriella.b.kiss@ttk.elte.hu
AB - The Italian Northern Apennines contain several Fe-Cu-Zn-bearing, Cyprus-type volcanogenic massive sulfide (VMS) deposits, which significantly contribute to the Cu resources of Italy. The massive sulfide lenses and related stockwork mineralizations are hosted by several levels (from basalt to serpentinite) of the unmetamorphosed ophiolitic series; therefore, this region offers perfect locations to study the ore-forming hydrothermal system in detail. A combination of fluid inclusion microthermometry, Raman spectroscopy, electron probe analyses (chlorite thermometry) and stable and noble gas isotope geochemistry was used to determine the fluid source of the VMS system at Bargone, Boccassuolo, Campegli, Casali–Monte Loreto, Corchia, Reppia and Vigonzano. This question of the fluid source is the focus of modern VMS research worldwide, as it has a direct influence on the metal content of the deposit. The obtained temperature and compositional data are both in the typical range of VMS systems and basically suggest evolved seawater origin for the mineralizing fluid. Modification of seawater was most commonly due to fluid–rock interaction processes, which happened during long-lasting circulation in the crust. The role of a small amount of magmatic fluid input was traced only at the lower block of Boccassuolo, which may be responsible for its higher ore grade. This fluid origin model is evidenced by O, H and C stable isotopic as well as He, Ne and Ar noble gas isotopic values.
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Lange-Enyedi, Nóra
AU - Kériné Borsodi, Andrea
AU - Németh, Péter
AU - Czuppon, György
AU - Kovács, Ivett
AU - Leél-Őssy, Szabolcs
AU - Dobosy, Péter
AU - Felföldi, Tamás
AU - Demény, Attila
AU - Makk, Judit
TI - Habitat-related variability in the morphological and taxonomic diversity of microbial communities in two Hungarian epigenic karst caves
JF - FEMS MICROBIOLOGY ECOLOGY
J2 - FEMS MICROBIOL ECOL
VL - 99
PY - 2023
IS - 12
PG - 17
SN - 0168-6496
DO - 10.1093/femsec/fiad161
UR - https://m2.mtmt.hu/api/publication/34431117
ID - 34431117
N1 - Institute for Geological and Geochemical Research, HUN-REN Research Centre for Astronomy and Earth Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Department of Microbiology, Institute of Biology, Faculty of Science, Eötvös Loránd University, Pázmány P. sétány 1/C, Budapest, H-1117, Hungary
Institute of Aquatic Ecology, HUN-REN Centre for Ecological Research, Karolina út 29, Budapest, H-1113, Hungary
Research Institute of Biomolecular and Chemical Engineering, Nanolab, University of Pannonia, Egyetem út 10, Veszprém, H-8200, Hungary
Department of Physical and Applied Geology, Faculty of Science, Eötvös Loránd University, Pázmány P. sétány 1/C, Budapest, H-1117, Hungary
Export Date: 8 February 2024
CODEN: FMECE
Correspondence Address: Makk, J.; Department of Microbiology, Pázmány P. sétány 1/C, Hungary; email: makk.judit@ttk.elte.hu
AB - The physical and chemical characteristics of the bedrock, along with the geological and hydrological conditions of karst caves may influence the taxonomic and functional diversity of prokaryotes. Most studies so far have focused on microbial communities of caves including only a few samples and have ignored the chemical heterogeneity of different habitat types such as sampling sites, dripping water, carbonate precipitates, cave walls, cave sediment and surface soils connected to the caves. The aim of the present study was to compare the morphology, the composition and physiology of the microbiota in caves with similar environmental parameters (temperature, host rock, elemental and mineral composition of speleothems) but located in different epigenic karst systems. Csodabogyós Cave and Baradla Cave (Hungary) were selected for the analysis of bacterial and archaeal communities using electron microscopy, amplicon sequencing, X-ray diffraction and mass spectroscopic techniques. The microbial communities belonged to the phyla Pseudomonadota, Acidobacteriota, Nitrospirota and Nitrososphaerota, and they showed site-specific variation in composition and diversity. The results indicate that morphological and physiological adaptations provide survival for microorganisms according to the environment. In epigenic karst caves, prokaryotes are prone to increase their adsorption surface, cooperate in biofilms, and implement chemolithoautotrophic growth with different electron-donors and acceptors available in the microhabitats.
LA - English
DB - MTMT
ER -
TY - CONF
AU - Lázár, Anett
AU - Karlik, Máté
AU - Molnár, Zsombor
AU - Demény, Attila
AU - Németh, Péter
TI - Ikaite (CaCO3*6H2O) -> ACC (amorphous calcium carbonate) -> calcite transformation and its paleoclimatological implication
T2 - EGU General Assembly 2023: Abstracts
PB - European Geosciences Union (EGU)
C1 - München
PY - 2023
DO - 10.5194/egusphere-egu23-1133
UR - https://m2.mtmt.hu/api/publication/33828942
ID - 33828942
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Lázár, Anett
AU - Molnár, Zsombor
AU - Demény, Attila
AU - Kótai, László
AU - Trif, László
AU - Béres, Kende Attila
AU - Bódis, Eszter
AU - Bortel, Gábor
AU - Aradi, László Előd
AU - Karlik, Máté
AU - Szabó, Máté Zoltán
AU - Pekker, Áron
AU - Németh, Gergely
AU - Kamarás, Katalin
AU - Garvie, L.A.J.
AU - Németh, Péter
TI - Insights into the amorphous calcium carbonate (ACC) → ikaite → calcite transformations
JF - CRYSTENGCOMM
J2 - CRYSTENGCOMM
VL - 25
PY - 2023
IS - 3
SP - 738
EP - 750
PG - 13
SN - 1466-8033
DO - 10.1039/d2ce01444k
UR - https://m2.mtmt.hu/api/publication/33606758
ID - 33606758
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Levy, EJ.
AU - Vonhof, HB.
AU - Bar-Matthews, M
AU - Martínez-García, A
AU - Ayalon, A
AU - Matthews, A
AU - Silverman, V
AU - Raveh-Rubin, S
AU - Zilberman, T
AU - Yasur, G
AU - Schmitt, M
AU - Haug, GH.
TI - Weakened AMOC related to cooling and atmospheric circulation shifts in the last interglacial Eastern Mediterranean
JF - NATURE COMMUNICATIONS
J2 - NAT COMMUN
VL - 14
PY - 2023
IS - 1
SN - 2041-1723
DO - 10.1038/s41467-023-40880-z
UR - https://m2.mtmt.hu/api/publication/34118086
ID - 34118086
N1 - Funding Agency and Grant Number: We thank P. Hoppe (MPIC) and A. Sorowke (MPIC) for SEM-EDX, Yvan Rome for fruitful discussions, ECMWF for providing access to ERA-5, and NASA OceanColor for the AQUA-MODIS-terra L3SMI SST data. This research was supported by the Minerva foundation and the; NASA OceanColor; Minerva foundation; Max Planck Society (MPG)
Funding text: We thank P. Hoppe (MPIC) and A. Sorowke (MPIC) for SEM-EDX, Yvan Rome for fruitful discussions, ECMWF for providing access to ERA-5, and NASA OceanColor for the AQUA-MODIS-terra L3SMI SST data. This research was supported by the Minerva foundation and the Max Planck Society (MPG).
AB - There is limited understanding of temperature and atmospheric circulation changes that accompany an Atlantic Meridional Overturning Circulation (AMOC) slowdown beyond the North Atlantic realm. A Peqi’in Cave (Israel) speleothem dated to the last interglacial period (LIG), 129–116 thousand years ago (ka), together with a large modern rainfall monitoring dataset, serve as the base for investigating past AMOC slowdown effects on the Eastern Mediterranean. Here, we reconstruct LIG temperatures and rainfall source using organic proxies (TEX 86 ) and fluid inclusion water d-excess . The TEX 86 data show a stepwise cooling from 19.8 ± 0.2° ( ca . 128–126 ka) to 16.5 ± 0.6 °C ( ca . 124–123 ka), while d-excess values decrease abruptly ( ca . 126 ka). The d-excess shift suggests that rainfall was derived from more zonal Mediterranean air flow during the weakened AMOC interval. Decreasing rainfall d-excess trends over the last 25 years raise the question whether similar atmospheric circulation changes are also occurring today.
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Weissbach, T
AU - Kluge, T
AU - Affolter, S
AU - Leuenberger, MC.
AU - Vonhof, H
AU - Riechelmann, DFC.
AU - Fohlmeister, J
AU - Juhl, MC
AU - Hemmer, B
AU - Wu, Y
AU - Warken, SF.
AU - Schmidt, M
AU - Frank, N
AU - Aeschbach, W
TI - Constraints for precise and accurate fluid inclusion stable isotope analysis using water-vapour saturated CRDS techniques
JF - CHEMICAL GEOLOGY
J2 - CHEM GEOL
VL - 617
PY - 2023
SN - 0009-2541
DO - 10.1016/j.chemgeo.2022.121268
UR - https://m2.mtmt.hu/api/publication/33334510
ID - 33334510
N1 - Heidelberg Graduate School of Fundamental Physics, Heidelberg University, Im Neuenheimer Feld 226, Heidelberg, 69120, Germany
Institute of Environmental Physics, Heidelberg University, Im Neuenheimer Feld 229, Heidelberg, 69120, Germany
Heidelberg Center for the Environment, Heidelberg University, Im Neuenheimer Feld 229, Heidelberg, 69120, Germany
Institute of Applied Geosciences, Karlsruhe Institute of Technology, Adenauerring 20b, Karlsruhe, 76131, Germany
Department of Environmental Sciences, University of Basel, Bernoullistrassse 30/32, Basel, 4056, Switzerland
Climate and Environmental Physics Division, Physics Institute and Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, Bern, 3012, Switzerland
Climate Geochemistry Department, Max Planck Institute for Chemistry, Hahn-Meitner-Weg 1, Mainz, 55128, Germany
Institute for Geosciences, Johannes Gutenberg University Mainz, Johann-Joachim-Becher-Weg 21, Mainz, 55128, Germany
Federal Office for Radiation Protection, Köpenicker Allee 120-130, Berlin, 10318, Germany
GFZ German Research Centre for Geosciences, Section ‘Climate Dynamics and Landscape Development’, Telegrafenberg, Potsdam, 14473, Germany
Institute of Earth Sciences, Heidelberg University, Im Neuenheimer Feld 234, Heidelberg, 69120, Germany
Export Date: 3 January 2023
Correspondence Address: Kluge, T.; Heidelberg Graduate School of Fundamental Physics, Im Neuenheimer Feld 226, Germany; email: tobias.kluge@kit.edu
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Frisia, S
AU - Borsato, A
AU - Hartland, A
AU - Faraji, M
AU - Demény, Attila
AU - Drysdale, RN.
AU - Marjo, CE.
TI - Crystallization pathways, fabrics and the capture of climate proxies in speleothems: Examples from the tropics
JF - QUATERNARY SCIENCE REVIEWS
J2 - QUATERN SCI REV
VL - 297
PY - 2022
SN - 0277-3791
DO - 10.1016/j.quascirev.2022.107833
UR - https://m2.mtmt.hu/api/publication/33199458
ID - 33199458
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Lange-Enyedi, Nóra
AU - Németh, Péter
AU - Kériné Borsodi, Andrea
AU - Halmy, R
AU - Czuppon, György
AU - Kovács, Ivett
AU - Leél-Őssy, Szabolcs
AU - Demény, Attila
AU - Makk, Judit
TI - Calcium Carbonate Precipitating Cultivable Bacteria from Different Speleothems of Karst Caves
JF - GEOMICROBIOLOGY JOURNAL
J2 - GEOMICROBIOL J
VL - 39
PY - 2022
IS - 2
SP - 107
EP - 122
PG - 16
SN - 0149-0451
DO - 10.1080/01490451.2021.2019857
UR - https://m2.mtmt.hu/api/publication/32560409
ID - 32560409
N1 - Faculty of Science, Doctoral School of Biology, Institute of Biology, Eötvös Loránd University, Budapest, Hungary
Department of Microbiology, Faculty of Science, Institute of Biology, Eötvös Loránd University, Budapest, Hungary
Research Centre for Astronomy and Earth Sciences, Institute for Geological and Geochemical Research, Eötvös Loránd Research Network, Budapest, Hungary
Research Institute of Biomolecular and Chemical Engineering, Nanolab, University of Pannonia, Veszprém, Hungary
Centre for Ecological Research, Institute of Aquatic Ecology, Eötvös Loránd Research Network, Budapest, Hungary
Department of Physical and Applied Geology, Faculty of Science, Eötvös Loránd University, Budapest, Hungary
Export Date: 19 May 2022
Correspondence Address: Lange-Enyedi, N.T.; Faculty of Science, Hungary; email: nora.tunde.lange-enyedi@ttk.elte.hu
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Németh, Péter
AU - Töchterle, P
AU - Dublyansky, Y
AU - Stalder, R
AU - Molnár, Zsombor
AU - Klébert, Szilvia
AU - Spötl, C
TI - Tracing structural relicts of the ikaite-to-calcite transformation in cryogenic cave glendonite
JF - AMERICAN MINERALOGIST
J2 - AM MINERAL
VL - 107
PY - 2022
SP - 1960
EP - 1967
PG - 8
SN - 0003-004X
DO - 10.2138/am-2022-8162
UR - https://m2.mtmt.hu/api/publication/32484920
ID - 32484920
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Temovski, Marjan
AU - Rinyu, László
AU - Futó, István
AU - Molnár, Kata
AU - Túri, Marianna
AU - Demény, Attila
AU - Otoničar, B
AU - Dublyansky, Y
AU - Audra, P
AU - Polyak, V
AU - Asmerom, Y
AU - Palcsu, László
TI - Combined use of conventional and clumped carbonate stable isotopes to identify hydrothermal isotopic alteration in cave walls
JF - SCIENTIFIC REPORTS
J2 - SCI REP
VL - 12
PY - 2022
IS - 1
SN - 2045-2322
DO - 10.1038/s41598-022-12929-4
UR - https://m2.mtmt.hu/api/publication/32867940
ID - 32867940
N1 - Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Eötvös Loránd Research Network, Bem tér 18/c, Debrecen, 4026, Hungary
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, MTA Centre of Excellence, Eötvös Loránd Research Network, Budaörsi út 45, Budapest, 1112, Hungary
Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts, Titov trg 2, Postojna, 6230, Slovenia
Institute of Geology, University of Innsbruck, Innrain 52, Innsbruck, 6020, Austria
Polytech’Lab, University Nice Côte d’Azur, 930 Route des Colles, Sophia-Antipolis, Nice, 06903, France
Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131, United States
Export Date: 4 January 2023
Correspondence Address: Temovski, M.; Isotope Climatology and Environmental Research Centre, Bem tér 18/c, Hungary; email: temovski.marjan@atomki.hu
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Warken, SF.
AU - Weißbach, T
AU - Kluge, T
AU - Vonhof, H
AU - Scholz, D
AU - Vieten, R
AU - Schmidt, M
AU - Winter, A
AU - Frank, N
TI - Last glacial millennial-scale hydro-climate and temperature changes in Puerto Rico constrained by speleothem fluid inclusion δ18O and δ2H values
JF - CLIMATE OF THE PAST
J2 - CLIM PAST
VL - 18
PY - 2022
IS - 1
SP - 167
EP - 181
PG - 15
SN - 1814-9324
DO - 10.5194/cp-18-167-2022
UR - https://m2.mtmt.hu/api/publication/32647449
ID - 32647449
N1 - Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany
Institute of Earth Sciences, University of Heidelberg, Heidelberg, Germany
Heidelberg Graduate School of Fundamental Physics, Heidelberg University, Heidelberg, Germany
Institute of Applied Geosciences, Karlsruhe Institute of Technology, Karlsruhe, Germany
Max Planck Institute for Chemistry, Climate Geochemistry Department, Mainz, Germany
Institute for Geosciences, University of Mainz, Mainz, Germany
Department of Marine Sciences, University of Puerto Rico, Mayaguez, Puerto Rico
Earth and Environmental Systems Department, Indiana State University, Terre Haute, IN, United States
Export Date: 4 January 2023
Correspondence Address: Warken, S.F.; Institute of Environmental Physics, Germany; email: swarken@iup.uni-heidelberg.de
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Wortham, BE.
AU - Montañez, IP.
AU - Swart, PK.
AU - Vonhof, H
AU - Tabor, C
TI - Variability in effective moisture inferred from inclusion fluid δ18O and δ2H values in a central Sierra Nevada stalagmite (CA)
JF - QUATERNARY SCIENCE REVIEWS
J2 - QUATERN SCI REV
VL - 279
PY - 2022
SN - 0277-3791
DO - 10.1016/j.quascirev.2022.107399
UR - https://m2.mtmt.hu/api/publication/32665359
ID - 32665359
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Zhang, Y
AU - Pan, W
AU - Zhu, B
AU - Li, W
AU - Yang, LW
AU - Chen, Y
AU - Yang, T
TI - Recrystallization of dolostones in the Cambrian Xiaoerbrak Formation, Tarim Basin and possible link to reservoir development
JF - MARINE AND PETROLEUM GEOLOGY
J2 - MAR PETROL GEOL
VL - 136
PY - 2022
SN - 0264-8172
DO - 10.1016/j.marpetgeo.2021.105452
UR - https://m2.mtmt.hu/api/publication/32525758
ID - 32525758
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Affolter, S
AU - Leuenberger, MC.
TI - Challenges in the Direct Determination of 17Oexcess in Microliter Amount of Water Extracted From Speleothem Fluid Inclusions
JF - FRONTIERS IN EARTH SCIENCE
J2 - FRONT EARTH SC-SWITZ
VL - 9
PY - 2021
SN - 2296-6463
DO - 10.3389/feart.2021.612436
UR - https://m2.mtmt.hu/api/publication/31992674
ID - 31992674
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Barale, L.
AU - Bertok, C.
AU - D’atri, A.
AU - Piana, F.
AU - Bernasconi, S.M.
AU - Czuppon, György
AU - Palcsu, László
AU - Gerdes, A.
AU - Birgel, D.
AU - Martire, L.
TI - U-pb dating and geochemical constraints to early cretaceous hydrothermal dolomitization in the provenÇal domain (Maritime alps, nw italy-se france)
JF - OFIOLITI
J2 - OFIOLITI
VL - 46
PY - 2021
IS - 2
SP - 131
EP - 149
PG - 19
SN - 0391-2612
DO - 10.4454/ofioliti.v46i2.543
UR - https://m2.mtmt.hu/api/publication/32089112
ID - 32089112
N1 - National Research Council of Italy, Institute of Geosciences and Earth Resources, Torino, Italy
University of Torino, Department of Earth Sciences, Torino, Italy
ETH Zurich, Department of Earth Sciences, Zurich, Switzerland
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network, Budapest, Hungary
Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Debrecen, Hungary
Goethe University Frankfurt, Department of Geosciences, Frankfurt am Main, Germany
University of Hamburg, Department of Earth Sciences, Institute for Geology, Hamburg, Germany
Export Date: 2 July 2021
Correspondence Address: Bertok, C.; University of Torino, Italy; email: carlo.bertok@unito.it
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Cseresznyés, Dóra
AU - Czuppon, György
AU - Király, Csilla
AU - Demény, Attila
AU - Györe, D
AU - Forray, V
AU - Kovács, Ivett
AU - Szabó, Csaba
AU - Falus, György
TI - Origin of dawsonite-forming fluids in the Mihályi-Répcelak field (Pannonian Basin) using stable H, C and O isotope compositions: Implication for mineral storage of carbon-dioxide
JF - CHEMICAL GEOLOGY
J2 - CHEM GEOL
VL - 584
PY - 2021
SN - 0009-2541
DO - 10.1016/j.chemgeo.2021.120536
UR - https://m2.mtmt.hu/api/publication/32240638
ID - 32240638
N1 - Lithosphere Fluid Research Lab (LRG), Department of Petrology and Geochemistry, Institute of Geography and Earth Sciences, Eötvös Loránd University (ELTE), Pázmány Péter sétány 1/C, Budapest, 1117, Hungary
Mining and Geological Survey of Hungary (MBFSZ), Colombus utca 17-23, Budapest, 1145, Hungary
Institute for Geological and Geochemical Research (IGGR), Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network, Budaörsi út 45, Budapest, 1112, Hungary
Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Bem tér 18/c, Debrecen, 4026, Hungary
Geographical Institute (GI), Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network, Budaörsi út 45, Budapest, 1112, Hungary
Isotope Geosciences Unit, Scottish Universities Environmental Research Centre (SUERC), East Kilbride, Scotland G75 0QF, United Kingdom
Export Date: 6 January 2022
Correspondence Address: Czuppon, G.; Institute for Geological and Geochemical Research (IGGR), Budaörsi út 45, Hungary; email: czuppon@geochem.hu
AB - Natural CO2 reservoirs provide an opportunity to study long-term fluid-rock interactions, which are essential to reassure the safety of mineral storage of carbon-dioxide. The Mihályi-Répcelak field (Pannonian Basin, Central Europe) is one of the largest natural CO2-bearing reservoirs in Europe (25 Mt). The CO2 was trapped in Neogene sandstones, which contain various carbonate minerals (dolomite, ankerite, siderite, dawsonite). To reveal the origin of the parent fluid, from which these minerals precipitated, dawsonite and siderite were separated by a new physical method to minimise the uncertainties in the analysis of their stable isotope composition. The δ13CDaw values range from +1.3 to +1.6‰ and the calculated δ13CCO2 values in equilibrium with dawsonite (−4.8‰ - –2.0‰) overlap with the carbon isotope compositions of the local CO2 and the European Subcontinental Lithospheric Mantle (−3.9‰ - –2.1‰). This indicates that the dawsonite-forming CO2 had a magmatic origin. The siderite data indicates that some formed from the magmatic CO2, possibly simultaneously with dawsonite (−6.0‰ - –3.9‰), whereas the rest (−8.4 - –6.1‰) formed either from a fractionated CO2 with magmatic origin or before the CO2 invasion. The hydrogen isotope composition of structural OH− of dawsonite (−57‰ to −74‰) was determined and was used to estimate the origin of the interacting porewater. The calculated porewater data (δD: −69‰ - –103‰ and δ18O: −1.4‰ - +4.7‰) indicate that the parent fluid was meteoric water modified by water-rock interaction. Our data allows estimation of the total amount of CO2 stored in the dawsonite-bearing sandstone reservoir to be 25 kg/m3, well in line with previous modelling works, which gives a total of 2.01 × 106 t of CO2, higher than previous estimates. We suggest that individual mineral analysis complemented by hydrogen isotope analysis is to be employed to effectively trace in-reservoir fluid-rock interactions in CO2 reservoirs and provide valuable input data for geochemical modelling for better predicting conditions for mineral storage of CO2.
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Demény, Attila
AU - Rinyu, László
AU - Kern, Zoltán
AU - Hatvani, István Gábor
AU - Czuppon, György
AU - Surányi, Gergely
AU - Leél-Őssy, Szabolcs
AU - Shen, CC
AU - Koltai, Gabriella
TI - Paleotemperature reconstructions using speleothem fluid inclusion analyses from Hungary
JF - CHEMICAL GEOLOGY
J2 - CHEM GEOL
VL - 563
PY - 2021
PG - 11
SN - 0009-2541
DO - 10.1016/j.chemgeo.2020.120051
UR - https://m2.mtmt.hu/api/publication/31813634
ID - 31813634
N1 - Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Bem tér 18/c, Debrecen, H-4026, Hungary
MTA-ELTE Geological, Geophysical and Space Sciences Research Group, Pázmány Péter s. 1/c, Budapest, 1117, Hungary
Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány Péter sétány. 1/C, Budapest, H-1117, Hungary
High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei, 10617, Taiwan
Research Center for Future Earth, National Taiwan University, Taipei, 10617, Taiwan
Institut für Geologie, Leopold-Franzens-Universität Innsbruck, Austria
Export Date: 25 January 2021
Correspondence Address: Demény, A.; Institute for Geological and Geochemical Research, Budaörsi út 45, Hungary; email: demeny@geochem.hu
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Bem tér 18/c, Debrecen, H-4026, Hungary
MTA-ELTE Geological, Geophysical and Space Sciences Research Group, Pázmány Péter s. 1/c, Budapest, 1117, Hungary
Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány Péter sétány. 1/C, Budapest, H-1117, Hungary
High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei, 10617, Taiwan
Research Center for Future Earth, National Taiwan University, Taipei, 10617, Taiwan
Institut für Geologie, Leopold-Franzens-Universität Innsbruck, Austria
Export Date: 28 May 2021
Correspondence Address: Demény, A.; Institute for Geological and Geochemical Research, Budaörsi út 45, Hungary; email: demeny@geochem.hu
LA - English
DB - MTMT
ER -
TY - JOUR
AU - He, M
AU - Cai, Y
AU - Zhang, H
AU - Xue, G
AU - Cheng, X
AU - Lu, Y
AU - Wang, G
AU - Qin, X
AU - Ma, L
AU - Wei, Y
AU - Huang, S
AU - Chang, H
AU - Yan, H
TI - The impact and implications of aragonite-to-calcite transformation on speleothem trace element composition
JF - SEDIMENTARY GEOLOGY
J2 - SEDIMENT GEOL
VL - 425
PY - 2021
SN - 0037-0738
DO - 10.1016/j.sedgeo.2021.106010
UR - https://m2.mtmt.hu/api/publication/32470867
ID - 32470867
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Johnston, VE.
AU - Borsato, A
AU - Frisia, S
AU - Spötl, C
AU - Hellstrom, JC.
AU - Cheng, H
AU - Edwards, RL
TI - Last interglacial hydroclimate in the Italian Prealps reconstructed from speleothem multi-proxy records (Bigonda Cave, NE Italy)
JF - QUATERNARY SCIENCE REVIEWS
J2 - QUATERN SCI REV
VL - 272
PY - 2021
SN - 0277-3791
DO - 10.1016/j.quascirev.2021.107243
UR - https://m2.mtmt.hu/api/publication/32464629
ID - 32464629
N1 - Museo delle Scienze, Corso del Lavoro e della Scienza, 3, Trento, 38122, Italy
Karst Research Institute ZRC SAZU, Titov trg 2, Postojna, 6230, Slovenia
School of Environmental and Life Sciences, University of Newcastle, Callaghan, NSW 2308, Australia
Institute of Geology, University of Innsbruck, Innrain 52, Innsbruck, 6020, Austria
School of Geography, Earth and Atmospheric Sciences, University of Melbourne, Melbourne, VIC 3010, Australia
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an, 710054, China
Key Laboratory of Karst Dynamics, MLR, Institute of Karst Geology, CAGS, Guilin, 541004, China
Earth and Environmental Sciences, University of Minnesota, Minneapolis, United States
Export Date: 3 January 2023
CODEN: QSRED
Correspondence Address: Johnston, V.E.; Karst Research Institute ZRC SAZU, Titov trg 2, Slovenia; email: vanessa.johnston@zrc-sazu.si
LA - English
DB - MTMT
ER -
TY - CHAP
AU - Lammers, LN.
AU - Koishi, A.
ED - Zhang, X
TI - Isotopic tracers of nonclassical crystallization
T2 - ACS Symposium Series Vol 1383
VL - 1383
PB - American Chemical Society
CY - Washington DC
SN - 9780841298262
T3 - Symposium on Novel Solutions to Water Pollution, ISSN 0097-6156 ; 1398.
PY - 2021
SP - 167
EP - 198
PG - 32
DO - 10.1021/bk-2021-1383.ch007
UR - https://m2.mtmt.hu/api/publication/34570870
ID - 34570870
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Lopez-Elorza, M
AU - Muñoz-García, MB
AU - González-Acebrón, L
AU - Martín-Chivelet, J
TI - Fluid-inclusion petrography in calcite stalagmites: Implications for entrapment processes
JF - JOURNAL OF SEDIMENTARY RESEARCH
J2 - J SEDIMENT RES
VL - 91
PY - 2021
IS - 11
SP - 1206
EP - 1226
PG - 21
SN - 1527-1404
DO - 10.2110/jsr.2021.016
UR - https://m2.mtmt.hu/api/publication/32539441
ID - 32539441
N1 - Departamento de Geodinámica Estratigrafia y Paleontologia, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, c/ José Antonio Novais 12, Madrid, 28040, Spain
Instituto de Geociencias, CSIC-UCM, c/ Severo Ochoa 7, Madrid, 28040, Spain
Export Date: 19 May 2022
LA - English
DB - MTMT
ER -
TY - THES
AU - Wortham, BE
TI - Investigating Climate Dynamics in CA: A Multi-Proxy Approach to Stalagmite Paleoclimate Reconstruction
PB - University of California, Davis
PY - 2021
SN - 9798492754389
UR - https://m2.mtmt.hu/api/publication/34448808
ID - 34448808
LA - English
DB - MTMT
ER -
TY - JOUR
AU - de Graaf, S
AU - Vonhof, HB.
AU - Weissbach, T
AU - Wassenburg, JA.
AU - Levy, EJ.
AU - Kluge, T
AU - Haug, GH.
TI - A comparison of isotope ratio mass spectrometry and cavity ring-down spectroscopy techniques for isotope analysis of fluid inclusion water
JF - RAPID COMMUNICATIONS IN MASS SPECTROMETRY
J2 - RAPID COMMUN MASS SPECTR
VL - 34
PY - 2020
IS - 16
SN - 0951-4198
DO - 10.1002/rcm.8837
UR - https://m2.mtmt.hu/api/publication/31329820
ID - 31329820
N1 - Climate Geochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
Ruprecht-Karls University Heidelberg, Institute of Environmental Physics, Heidelberg, Germany
Export Date: 3 January 2023
CODEN: RCMSE
Correspondence Address: de Graaf, S.; Climate Geochemistry Department, Germany; email: stefan.graaf@mpic.de
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Ghadiri, E
AU - Affolter, S
AU - Brennwald, MS.
AU - Fleitmann, D
AU - Häuselmann, AD.
AU - Cheng, H
AU - Maden, C
AU - Leuenberger, M
AU - Kipfer, R
TI - Estimation of temperature – altitude gradients during the Pleistocene–Holocene transition from Swiss stalagmites
JF - EARTH AND PLANETARY SCIENCE LETTERS
J2 - EARTH PLANET SC LETT
VL - 544
PY - 2020
SN - 0012-821X
DO - 10.1016/j.epsl.2020.116387
UR - https://m2.mtmt.hu/api/publication/31355952
ID - 31355952
LA - English
DB - MTMT
ER -
TY - THES
AU - Ghadiri, E.
TI - Noble Gas Temperature Reconstructions in New Paleoclimate Archives
PB - ETH Zürich
PY - 2020
DO - 10.3929/ethz-b-000431784
UR - https://m2.mtmt.hu/api/publication/31606792
ID - 31606792
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Uemura, R
AU - Kina, Y
AU - Shen, CC
AU - Omine, K
TI - Experimental evaluation of oxygen isotopic exchange between inclusion water and host calcite in speleothems
JF - CLIMATE OF THE PAST
J2 - CLIM PAST
VL - 16
PY - 2020
IS - 1
SP - 17
EP - 27
PG - 11
SN - 1814-9324
DO - 10.5194/cp-16-17-2020
UR - https://m2.mtmt.hu/api/publication/31146940
ID - 31146940
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Affolter, S
AU - Häuselmann, A
AU - Fleitmann, D
AU - Edwards, RL
AU - Cheng, H
AU - Leuenberger, M
TI - Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years
JF - SCIENCE ADVANCES
J2 - SCI ADV
VL - 5
PY - 2019
IS - 6
SN - 2375-2548
DO - 10.1126/sciadv.aav3809
UR - https://m2.mtmt.hu/api/publication/30731182
ID - 30731182
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Demény, Attila
AU - Kern, Zoltán
AU - Németh, Alexandra
AU - Frisia, S
AU - Hatvani, István Gábor
AU - Czuppon, György
AU - Leél-Őssy, Szabolcs
AU - Molnár, Mihály
AU - Óvári, Mihály
AU - Surányi, Gergely
AU - Gilli, A
AU - Wu, CC
AU - Shen, CC
TI - North Atlantic influences on climate conditions in East-Central Europe in the late Holocene reflected by flowstone compositions
JF - QUATERNARY INTERNATIONAL
J2 - QUATERN INT
VL - 512
PY - 2019
SP - 99
EP - 112
PG - 14
SN - 1040-6182
DO - 10.1016/j.quaint.2019.02.014
UR - https://m2.mtmt.hu/api/publication/30688739
ID - 30688739
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Kern, Zoltán
AU - Demény, Attila
AU - Persoiu, A
AU - Hatvani, István Gábor
TI - Speleothem Records from the Eastern Part of Europe and Turkey—Discussion on Stable Oxygen and Carbon Isotopes
JF - QUATERNARY
J2 - Quaternary
VL - 2
PY - 2019
IS - 3
PG - 26
SN - 2571-550X
DO - 10.3390/quat2030031
UR - https://m2.mtmt.hu/api/publication/30806565
ID - 30806565
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Li, W
AU - Bialik, OM
AU - Wang, X
AU - Yang, T
AU - Hu, Z
AU - Huang, Q
AU - Zhao, S
AU - Waldmann, ND
TI - Effects of early diagenesis on Mg isotopes in dolomite: The roles of Mn(IV)-reduction and recrystallization
JF - GEOCHIMICA ET COSMOCHIMICA ACTA
J2 - GEOCHIM COSMOCHIM AC
VL - 250
PY - 2019
SP - 1
EP - 17
PG - 17
SN - 0016-7037
DO - 10.1016/j.gca.2019.01.029
UR - https://m2.mtmt.hu/api/publication/30587693
ID - 30587693
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Allan, M
AU - Fagel, N
AU - van der Lubbe, HJL
AU - Vonhof, HB
AU - Cheng, H
AU - Edwards, RL
AU - Verheyden, S
TI - High-resolution reconstruction of 8.2-ka BP event documented in Père Noël cave, southern Belgium
JF - JOURNAL OF QUATERNARY SCIENCE
J2 - J QUATERNARY SCI
VL - 33
PY - 2018
IS - 7
SP - 840
EP - 852
PG - 13
SN - 0267-8179
DO - 10.1002/jqs.3064
UR - https://m2.mtmt.hu/api/publication/27670578
ID - 27670578
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Carlson, P
AU - Miller, NR
AU - Banner, JL
AU - Breecker, DO
AU - Casteel, RC
TI - The potential of near-entrance stalagmites as high-resolution terrestrial paleoclimate proxies: Application of isotope and trace-element geochemistry to seasonally-resolved chronology
JF - GEOCHIMICA ET COSMOCHIMICA ACTA
J2 - GEOCHIM COSMOCHIM AC
VL - 235
PY - 2018
SP - 55
EP - 75
PG - 21
SN - 0016-7037
DO - 10.1016/j.gca.2018.04.036
UR - https://m2.mtmt.hu/api/publication/27445446
ID - 27445446
LA - English
DB - MTMT
ER -
TY - THES
AU - Carlson, P.E.
TI - Recent climate records from a near-entrance stalagmite
PB - University of Texas at Austin
PY - 2018
SN - 9798678116581
UR - https://m2.mtmt.hu/api/publication/30317241
ID - 30317241
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Frisia, S
AU - Borsato, A
AU - Hellstrom, J
TI - High spatial resolution investigation of nucleation, growth and early diagenesis in speleothems as exemplar for sedimentary carbonates
JF - EARTH-SCIENCE REVIEWS
J2 - EARTH-SCI REV
VL - 178
PY - 2018
SP - 68
EP - 91
PG - 24
SN - 0012-8252
DO - 10.1016/j.earscirev.2018.01.014
UR - https://m2.mtmt.hu/api/publication/27377234
ID - 27377234
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Garaguly, István
AU - Raucsikné Varga, Andrea Beáta
AU - Raucsik, Béla
AU - Schubert, Félix
AU - Czuppon, György
AU - Frei, R
TI - Pervasive early diagenetic dolomitization, subsequent hydrothermal alteration, and late stage hydrocarbon accumulation in a Middle Triassic carbonate sequence (Szeged Basin, SE Hungary)
JF - MARINE AND PETROLEUM GEOLOGY
J2 - MAR PETROL GEOL
VL - 98
PY - 2018
SP - 270
EP - 290
PG - 21
SN - 0264-8172
DO - 10.1016/j.marpetgeo.2018.07.024
UR - https://m2.mtmt.hu/api/publication/3399845
ID - 3399845
N1 - Funding Agency and Grant Number: National Research, Development and Innovation Fund of Hungary [K 108375]
Funding text: This research was supported by the National Research, Development and Innovation Fund of Hungary (project no. K 108375). The authors would like to thank MOL Plc for providing the core material that were essential for this research. We would like to thank Dr. Fadi H. Nader and the anonymous referee for their suggestions and comments that improve our manuscript, as well as Associated Editor Dr. Ihsan Al-Aasm for the editorial work.
Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem utca 2-6, Szeged, 6702, Hungary
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Department of Geosciences and Natural Resource Management, University of Copenhagen, ØsterVoldgade10, Copenhagen, 1350, Denmark
Nordic Center for Earth Evolution (NordCEE), Copenhagen, Denmark
Cited By :15
Export Date: 12 September 2021
Correspondence Address: Garaguly, I.; Department of Mineralogy, Egyetem utca 2-6, Hungary; email: garagulyistvan@gmail.com
Funding text 1: This research was supported by the National Research, Development and Innovation Fund of Hungary (project no. K 108375 ). The authors would like to thank MOL Plc for providing the core material that were essential for this research. We would like to thank Dr. Fadi H. Nader and the anonymous referee for their suggestions and comments that improve our manuscript, as well as Associated Editor Dr. Ihsan Al-Aasm for the editorial work.
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Johnston, V
AU - Borsato, A
AU - Frisia, S
AU - Spötl, C
AU - Dublyansky, Y
AU - Töchterle, P
AU - Hellstrom, JC
AU - Bajo, P
AU - Edwards, RL
AU - Cheng, H
TI - Evidence of thermophilisation and elevation-dependent warming during the Last Interglacial in the Italian Alps
JF - SCIENTIFIC REPORTS
J2 - SCI REP
VL - 8
PY - 2018
IS - 1
SN - 2045-2322
DO - 10.1038/s41598-018-21027-3
UR - https://m2.mtmt.hu/api/publication/27178184
ID - 27178184
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Cseresznyés, Dóra
AU - Czuppon, György
AU - Szabó-Krausz, Zsuzsanna
AU - Király, Csilla
AU - Szabó, Csaba
AU - Falus, György
TI - Stable Isotope Compositions of Different Mineral Phases Found in a Natural CO2-reservoir (NW-Hungary): Implication for their Origin
JF - ENERGY PROCEDIA
J2 - ENERGY PROCEDIA
VL - 114
PY - 2017
SP - 2812
EP - 2818
PG - 7
SN - 1876-6102
DO - 10.1016/j.egypro.2017.03.1399
UR - https://m2.mtmt.hu/api/publication/3262057
ID - 3262057
N1 - Lithosphere Fluid Research Lab, Eötvös University, Pazmany Peter setany 1/C, Budapest, H-1117, Hungary
Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, HAS, Budaörsi 45, Budapest, H-1112, Hungary
Geological and Geophysical Institute of Hungary, Stefánia 14, Budapest, 1143, Hungary
Export Date: 14 December 2020
Correspondence Address: Falus, G.; Geological and Geophysical Institute of Hungary, Stefánia 14, Hungary; email: falus.gyorgy@mfgi.hu
AB - Stable isotope systems provide exceptional insight into fluid-solid interactions occurring in the sub-surface. We provide detailed
insight into the stable isotope distribution of carbonate minerals in a natural CO2 reservoir system from Mihályi-Répcelak area,
NW-Hungary. Several types of measurements and calculations have been applied for the estimation of CO2 and H2O isotopic
composition in equilibrium with dawsonite. The estimated G13C of CO2 exhibit values around -4.5 to -2.6 ‰ overlapping with
assumed magmatic values and the presently measured gas data confirming magmatic origin, whereas we may assume that the
water present during carbonate formation likely had meteoric origin.
© 2017 The Authors. Published by Elsevier Ltd.
Peer-review under responsibility of the organizing committee of GHGT-13.
Keywords: stable isotopes; natural CO2 reservoir; carbonate minerals
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Demény, Attila
TI - Cseppkövek és klímakutatás: nanométerektől a kontinentális léptékig
JF - MAGYAR TUDOMÁNY
J2 - MAGYAR TUDOMÁNY
VL - 178
PY - 2017
IS - 10
SP - 1247
EP - 1261
PG - 15
SN - 0025-0325
DO - 10.1556/2065.178.2017.10.8
UR - https://m2.mtmt.hu/api/publication/3275170
ID - 3275170
LA - Hungarian
DB - MTMT
ER -
TY - JOUR
AU - Demény, Attila
AU - Németh, Alexandra
AU - Kern, Zoltán
AU - Czuppon, György
AU - Molnár, Mihály
AU - Leél-Ossy, S
AU - Óvári, M
AU - Stieber, J
TI - Recently forming stalagmites from the Baradla Cave and their suitability assessment for climate-proxy relationships
JF - CENTRAL EUROPEAN GEOLOGY
J2 - CENT EUR GEOL
VL - 60
PY - 2017
IS - 1
SP - 1
EP - 34
PG - 34
SN - 1788-2281
DO - 10.1556/24.60.2017.001
UR - https://m2.mtmt.hu/api/publication/3212802
ID - 3212802
N1 - Institute for Geological and Geochemical Research, RCAES, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary
Department of Physical and Applied Geology, Eötvös Loránd University, Budapest, Hungary
Institute of Chemistry, Eötvös Loránd University, Budapest, Hungary
Stieber Environmental Ltd., Budapest, Hungary
Export Date: 15 October 2019
Correspondence Address: Demény, A.; Institute for Geological and Geochemical Research, RCAES, Hungarian Academy of Sciences, Budaörsi út 45, Hungary; email: demeny@geochem.hu
Institute for Geological and Geochemical Research, RCAES, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary
Department of Physical and Applied Geology, Eötvös Loránd University, Budapest, Hungary
Institute of Chemistry, Eötvös Loránd University, Budapest, Hungary
Stieber Environmental Ltd., Budapest, Hungary
Export Date: 14 December 2020
Correspondence Address: Demény, A.; Institute for Geological and Geochemical Research, RCAES, Hungarian Academy of Sciences, Budaörsi út 45, Hungary; email: demeny@geochem.hu
Institute for Geological and Geochemical Research, RCAES, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary
Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary
Department of Physical and Applied Geology, Eötvös Loránd University, Budapest, Hungary
Institute of Chemistry, Eötvös Loránd University, Budapest, Hungary
Stieber Environmental Ltd., Budapest, Hungary
Export Date: 22 February 2021
Correspondence Address: Demény, A.; Institute for Geological and Geochemical Research, Budaörsi út 45, Hungary; email: demeny@geochem.hu
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Demény, Attila
AU - Kern, Zoltán
AU - Czuppon, György
AU - Németh, Alexandra
AU - Leél-Őssy, Szabolcs
AU - Siklósy, Z
AU - Lin, K
AU - Hsun-Ming, H
AU - Shen, Ch-Ch
AU - Vennemann, T W
AU - Haszpra, László
TI - Stable isotope compositions of speleothems from the last interglacial e Spatial patterns of climate fluctuations in Europe
JF - QUATERNARY SCIENCE REVIEWS
J2 - QUATERN SCI REV
VL - 161
PY - 2017
SP - 68
EP - 80
PG - 13
SN - 0277-3791
DO - 10.1016/j.quascirev.2017.02.012
UR - https://m2.mtmt.hu/api/publication/3191622
ID - 3191622
N1 - Megjegyzés-26494825
N1 Funding details: LP2012-27/2012, MTA, Magyar Tudományos Akadémia
N1 Funding details: OTKA CK 80661, OTKA, Országos Tudományos Kutatási Alapprogramok
N1 Funding details: OTKA NK 101664, OTKA, Országos Tudományos Kutatási Alapprogramok
N1 Funding text: We would like to express our gratitude to three anonymous reviewers whose suggestions helped clarify our ideas. This research was supported by the National Office for Research and Technology of Hungary (GVOP-3.2.1-2004-04-0235/3.0), the Hungarian Scientific Research Fund (OTKA CK 80661 and OTKA NK 101664) and the “Momentum-Lendület” program of the Hungarian Academy of Sciences (LP2012-27/2012). The Bolyai János research scholarship received by György Czuppon greatly helped his work. U-Th dating was supported by Taiwan ROC MOST and NTU grants (103-2119-M-002-022, 104-2119-M-002-003 and 101R7625). This is contribution No. 41 of the 2ka Palaeoclimatology Research Group.
Megjegyzés-26505658
N1 Funding details: LP2012-27/2012, MTA, Magyar Tudományos Akadémia
N1 Funding details: OTKA CK 80661, OTKA, Országos Tudományos Kutatási Alapprogramok
N1 Funding details: OTKA NK 101664, OTKA, Országos Tudományos Kutatási Alapprogramok
N1 Funding text: We would like to express our gratitude to three anonymous reviewers whose
suggestions helped clarify our ideas. This research was supported by the National Office
for Research and Technology of Hungary (GVOP-3.2.1-2004-04-0235/3.0), the Hungarian
Scientific Research Fund (OTKA CK 80661 and OTKA NK 101664) and the “Momentum-Lendület”
program of the Hungarian Academy of Sciences (LP2012-27/2012). The Bolyai János research
scholarship received by György Czuppon greatly helped his work. U-Th dating was supported
by Taiwan ROC MOST and NTU grants (103-2119-M-002-022, 104-2119-M-002-003 and 101R7625).
This is contribution No. 41 of the 2ka Palaeoclimatology Research Group.
Megjegyzés-26494805
N1 Funding details: LP2012-27/2012, MTA, Magyar Tudományos Akadémia
N1 Funding details: OTKA CK 80661, OTKA, Országos Tudományos Kutatási Alapprogramok
N1 Funding details: OTKA NK 101664, OTKA, Országos Tudományos Kutatási Alapprogramok
N1 Funding text: We would like to express our gratitude to three anonymous reviewers whose suggestions helped clarify our ideas. This research was supported by the National Office for Research and Technology of Hungary (GVOP-3.2.1-2004-04-0235/3.0), the Hungarian Scientific Research Fund (OTKA CK 80661 and OTKA NK 101664) and the “Momentum-Lendület” program of the Hungarian Academy of Sciences (LP2012-27/2012). The Bolyai János research scholarship received by György Czuppon greatly helped his work. U-Th dating was supported by Taiwan ROC MOST and NTU grants (103-2119-M-002-022, 104-2119-M-002-003 and 101R7625). This is contribution No. 41 of the 2ka Palaeoclimatology Research Group.
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Millo, C
AU - Strikis, NM
AU - Vonhof, HB
AU - Deininger, M
AU - da Cruz, FW Jr
AU - Wang, X
AU - Cheng, H
AU - Edwards, RL
TI - Last glacial and Holocene stable isotope record of fossil dripwater from subtropical Brazil based on analysis of fluid inclusions in stalagmites
JF - CHEMICAL GEOLOGY
J2 - CHEM GEOL
VL - 468
PY - 2017
SP - 84
EP - 96
PG - 13
SN - 0009-2541
DO - 10.1016/j.chemgeo.2017.08.018
UR - https://m2.mtmt.hu/api/publication/26887562
ID - 26887562
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Purgstaller, B
AU - Konrad, F
AU - Dietzel, M
AU - Immenhauser, A
AU - Mavromatis, V
TI - Control of Mg2+/Ca2+ Activity Ratio on the Formation of Crystalline Carbonate Minerals via an Amorphous Precursor
JF - CRYSTAL GROWTH & DESIGN
J2 - CRYST GROWTH DES
VL - 17
PY - 2017
IS - 3
SP - 1069
EP - 1078
PG - 10
SN - 1528-7483
DO - 10.1021/acs.cgd.6b01416
UR - https://m2.mtmt.hu/api/publication/26470655
ID - 26470655
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Demény, Attila
AU - Németh, Péter
AU - Czuppon, György
AU - Leél-Őssy, Szabolcs
AU - Szabó, Máté Zoltán
AU - Judik, Katalin
AU - Németh, Tibor
AU - Stieber, J
TI - Formation of amorphous calcium carbonate in caves and its implications for speleothem research
JF - SCIENTIFIC REPORTS
J2 - SCI REP
VL - 6
PY - 2016
SN - 2045-2322
DO - 10.1038/srep39602
UR - https://m2.mtmt.hu/api/publication/3158886
ID - 3158886
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Mindrescu, M
AU - Veres, D
TI - Recent contributions and prospects for climatic variability studies in Central and Eastern Europe
JF - QUATERNARY INTERNATIONAL
J2 - QUATERN INT
VL - 415
PY - 2016
SP - 1
EP - 5
PG - 5
SN - 1040-6182
DO - 10.1016/j.quaint.2016.04.046
UR - https://m2.mtmt.hu/api/publication/26242217
ID - 26242217
N1 - Cited By :2
Export Date: 27 February 2023
LA - English
DB - MTMT
ER -
TY - JOUR
AU - Németh, Alexandra
AU - Demény, Attila
AU - Czuppon, György
AU - Kern, Zoltán
AU - Leél-Őssy, Szabolcs
AU - Molnár, Mihály
TI - Petrographic comparison of four recent stalagmites from Baradla Cave Hungary-implications for the paleoclimate interpretation
JF - GEOREVIEW: ANALELE UNIVERSITATII STEFAN CEL MARE DIN SUCEAVA SERIA GEOGRAFIE
J2 - GEOREVIEW: AN UNIV STEFAN CEL MARE D SUC SER GEOGRAF
VL - 26
PY - 2016
IS - 2
SP - 64
EP - 66
PG - 3
SN - 1583-1469
UR - https://m2.mtmt.hu/api/publication/3187834
ID - 3187834
LA - English
DB - MTMT
ER -