@article{MTMT:34757829,
	title = {Effects of root-derived organic acids on sorption of pharmaceutically active compounds in sandy topsoil},
	url = {https://m2.mtmt.hu/api/publication/34757829},
	author = {Szabó, Lili and Vancsik, Anna and Bauer, László and Jakab, Gergely Imre and Király, Csilla and Hatvani, István Gábor and Kondor, Attila Csaba and Szalai, Zoltán},
	doi = {10.1016/j.chemosphere.2024.141759},
	journal-iso = {CHEMOSPHERE},
	journal = {CHEMOSPHERE},
	volume = {355},
	unique-id = {34757829},
	issn = {0045-6535},
	year = {2024},
	eissn = {1879-1298},
	orcid-numbers = {Jakab, Gergely Imre/0000-0001-5424-1983; Hatvani, István Gábor/0000-0002-9262-7315; Szalai, Zoltán/0000-0001-5267-411X}
}

@article{MTMT:34753329,
	title = {At an important tephrostratigraphic crossroads: cryptotephra in Late Glacial to Early Holocene lake sediments from the Carpathian Mountains, Romania},
	url = {https://m2.mtmt.hu/api/publication/34753329},
	author = {Kearney, RJ. and Albert, PG. and Staff, RA. and Magyari, Enikő Katalin and Pál, I. and Veres, D. and Lane, CS. and McGuire, A. and Bronk Ramsey, C.},
	doi = {10.1016/j.quascirev.2024.108558},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {330},
	unique-id = {34753329},
	issn = {0277-3791},
	year = {2024},
	eissn = {1873-457X},
	orcid-numbers = {Kearney, RJ./0000-0001-8997-6808; Albert, PG./0000-0002-6757-1452; Staff, RA./0000-0002-8634-014X; Magyari, Enikő Katalin/0000-0002-2844-8937; Veres, D./0000-0003-3932-577X; Lane, CS./0000-0001-9206-3903; McGuire, A./0000-0001-6974-1171}
}

@article{MTMT:34753315,
	title = {Two chironomid-inferred mean July air temperature reconstructions in the South Carpathian Mountains over the last 2000 years},
	url = {https://m2.mtmt.hu/api/publication/34753315},
	author = {Szabó, Zoltán and Buczkó, Krisztina and Korponai, János and Luoto, T and Begy, RCs and Haliuc, A and Veres, D and Hamerlik, L and Csorba, R and Zsigmond, AR and Darabos, Gabriella and Méhes, Nikoletta and Kövér, Csilla and Magyari, Enikő Katalin},
	doi = {10.1177/09596836241236353},
	journal-iso = {HOLOCENE},
	journal = {HOLOCENE},
	volume = {In press},
	unique-id = {34753315},
	issn = {0959-6836},
	abstract = {We present chironomid-based reconstructions of mean July air temperature changes over the last 2000 years from Lake Latoriței (1530 m a.s.l.) in the Southern Carpathians. A multi-proxy analysis was performed along a 58 cm long sediment core and two training sets were used for quantitative July air temperature reconstructions: the Eastern-European (EE, 212 lakes) and the Finnish-Polish-Carpathian (FPC, 273 lakes). The transfer functions had a coefficient of determination (r2) 0.88 and 0.91 with a root mean squared error of prediction (RMSEP) 0.88°C and 1.02°C. Despite possible biases resulting from methodological problems and the ecological complexity of the chironomid response to both climatic and environmental changes, the agreement of the temperature reconstruction of Lake Latoriței with other alpine records suggests that the transfer function successfully reconstructed past summer temperatures between 750 and 1830 CE. Biases in the temperature reconstruction in the period before 750 and after 1830 CE were likely caused by increased abundance of rheophilic and semi-terrestrial chironomid species related to increased inflow activity before 750 CE and local land use changes after 1830 CE, which was also indicated by increasing deforestation and increasing lake productivity in the pollen and diatom records. Our results suggest that the region experienced a warm period between 750 and 1360 CE, and a cold period between 1360 and 1600 CE followed by fluctuating summer temperatures until 1830 CE. These events were associated with the so-called ‘Mediaeval Warm Period’ (MWP) and the ‘Little Ice Age’ (LIA), respectively. The inference models reconstructed a decrease in July air temperatures by 0.7°C–1.1°C during the LIA relative to the warmer MWP. We also demonstrated that the FPC training set gives better results, supporting that local/continental training sets are efficient to detect weak amplitude summer temperature changes in the Late-Holocene.},
	keywords = {Chironomids; late-Holocene; Finnish-Polish-Carpathian training set; mean July air temperature reconstruction; multi-proxy palaeoecology; RWP-LALIA-MWP-LIA},
	year = {2024},
	eissn = {1477-0911},
	orcid-numbers = {Korponai, János/0000-0003-0211-192X; Darabos, Gabriella/0000-0001-8070-5630; Magyari, Enikő Katalin/0000-0002-2844-8937}
}

@article{MTMT:34745482,
	title = {A global compilation of diatom silica oxygen isotope records from lake sediment - trends and implications for climate reconstruction},
	url = {https://m2.mtmt.hu/api/publication/34745482},
	author = {Meister, P. and Alexandre, A. and Bailey, H. and Barker, P. and Biskaborn, B.K. and Broadman, E. and Cartier, R. and Chapligin, B. and Couapel, M. and Dean, J.R. and Diekmann, B. and Harding, P. and Henderson, A.C.G. and Hernandez, A. and Herzschuh, U. and Kostrova, S.S. and Lacey, J. and Leng, M.J. and Lücke, A. and MacKay, A.W. and Magyari, Enikő Katalin and Narancic, B. and Porchier, C. and Rosqvist, G. and Shemesh, A. and Sonzogni, C. and Swann, G.E.A. and Sylvestre, F. and Meyer, H.},
	doi = {10.5194/cp-20-363-2024},
	journal-iso = {CLIM PAST},
	journal = {CLIMATE OF THE PAST},
	volume = {20},
	unique-id = {34745482},
	issn = {1814-9324},
	year = {2024},
	eissn = {1814-9332},
	pages = {363-392},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937}
}

@CONFERENCE{MTMT:34734757,
	title = {Effect of sample preparation on the FTIR DRIFT spectra in the case of soils with different organic material content},
	url = {https://m2.mtmt.hu/api/publication/34734757},
	author = {Szalai, Zoltán and Karlik, Máté and Jakab, Gergely Imre and Vancsik, Anna and Hatvani, István Gábor and Cseresznyés, Dóra and Király, Csilla},
	booktitle = {EGU General Assembly 2024 abstract kötet},
	doi = {10.5194/egusphere-egu24-10421},
	unique-id = {34734757},
	year = {2024},
	orcid-numbers = {Szalai, Zoltán/0000-0001-5267-411X; Jakab, Gergely Imre/0000-0001-5424-1983; Hatvani, István Gábor/0000-0002-9262-7315; Cseresznyés, Dóra/0000-0001-6676-7122}
}

@article{MTMT:34731774,
	title = {Confidence and consistency in discrimination: A new family of evaluation metrics for potential distribution models},
	url = {https://m2.mtmt.hu/api/publication/34731774},
	author = {Somodi, Imelda and Bede-Fazekas, Ákos and Botta-Dukát, Zoltán and Molnár, Zsolt},
	doi = {10.1016/j.ecolmodel.2024.110667},
	journal-iso = {ECOL MODEL},
	journal = {ECOLOGICAL MODELLING},
	volume = {491},
	unique-id = {34731774},
	issn = {0304-3800},
	year = {2024},
	eissn = {1872-7026},
	orcid-numbers = {Bede-Fazekas, Ákos/0000-0002-2905-338X; Botta-Dukát, Zoltán/0000-0002-9544-3474}
}

@misc{MTMT:34717979,
	title = {Neolithic, Copper and Bronze Ages forest composition and wood uses in the Great Hungarian Plain},
	url = {https://m2.mtmt.hu/api/publication/34717979},
	author = {Gabriella, Darabos and Máté, Róbert Merkl and Pál, Raczky and András, Füzesi and Attila, Gyucha and Danielle, Riebe and William, A. Parkinson and Magdalena, Moskal-de Hoyo and Szilvia, Fábián and Gabriella, Hajdrik and Hajdú, Tamás and Gémes, Anett and Csüllög, Gábor and Mester, Edit and Dani, János and Szeverényi, Vajk and Viktória, Kiss and Enikő, Katalin Magyari},
	unique-id = {34717979},
	year = {2024},
	orcid-numbers = {Csüllög, Gábor/0000-0001-8436-7931}
}

@article{MTMT:34679307,
	title = {Modelling of potential vegetation identifies diverging expectable outcomes of river floodplain widening},
	url = {https://m2.mtmt.hu/api/publication/34679307},
	author = {Somodi, Imelda and Konrád, Krisztina Dóra and Vizi, Dávid Béla and Tallósi, Béla and Samu, Andrea and Kajner, Péter and Bede-Fazekas, Ákos},
	doi = {10.1016/j.gecco.2024.e02859},
	journal-iso = {GLOB ECOL CONSERV},
	journal = {GLOBAL ECOLOGY AND CONSERVATION},
	volume = {50},
	unique-id = {34679307},
	issn = {2351-9894},
	abstract = {River re-naturalisations are at the forefront of conservation efforts. The hope is that these interventions will benefit both local ecosystems and facilitate flood mitigation. While hydrological modelling has been a standard procedure in assessing the outcomes of river re-naturalisations, vegetation modelling has not always been performed as part of these assessments. We hypothesised that the use of potential vegetation modelling, i.e. the modelling of self-sustainable vegetation that can survive after the intervention, can provide insight into vegetation outcome of river re-naturalisation and can thus support vegetation restoration and conservation planning. We investigated the utility of potential vegetation modelling under a specific, widespread element of river re-naturalisation: river floodplain widening at three study sites along the Tisza River in Hungary. We applied potential vegetation modelling, in addition to hydrological and groundwater modelling, to assess the expected vegetation outcome of the river floodplain widening. Flood frequency and duration were assessed by the HEC-RAS hydrological model. Based on the output this hydrological model provided, expected values of the water-related explanatory variables (including groundwater level) were calculated. Statistical relationships encompassed by the existing mulitple potential vegetation (MPV) models of Hungary were applied to the environmental variable sets corresponding to conditions before and after floodplain widening (pre- and post-treatment, respectively), including water-related and other explanatory variables. This resulted in predicted potential vegetation distribution for pre-treatment and post-treatment conditions, which were then compared via ordinations and PERMANOVA. At two of the study sites, post-treatment potential vegetation prediction typically showed vegetation types requiring wetter and less saline conditions when compared to the pre-treatment potential vegetation distribution. This pattern corresponds to general expectations given river floodplain widening. However, at one of the sites, the potentiality of saline and non-saline steppe vegetation was actually more pronounced under the expected post-treatment conditions than those before widening. The strengthening of the potentiality of dry vegetation types can be explained by the minor environmental differences related to the microrelief. As the studied sites were all located in the lowlands where geomorphological variation is small, the effect of these minor geomorphological differences on post-treatment potential vegetation would have remained hidden without applying MPV models. In conclusion, scenarios that employ MPV models help predict river restoration outcomes more accurately and can help identify factors that might otherwise be overlooked. Thus, when combined with physical modelling of river flow, their use can aid in the restoration and landscape planning decisions in river re-naturalisation projects.},
	keywords = {RIVER RESTORATION; vegetation modelling; Embankment removal; Potential vegetation; River re-naturalisation; Saline vegetation},
	year = {2024},
	eissn = {2351-9894},
	pages = {1-15},
	orcid-numbers = {Konrád, Krisztina Dóra/0000-0002-4414-8766; Bede-Fazekas, Ákos/0000-0002-2905-338X}
}

@article{MTMT:34568108,
	title = {Review on vegetation, landscape and climate changes in the Carpathian Basin during the Neolithic and Chalcolithic period},
	url = {https://m2.mtmt.hu/api/publication/34568108},
	author = {Magyari, Enikő Katalin and Raczky, Pál and Merkl, Máté and Pálfi, Ivett and Darabos, Gabriella and Hajnalova, M and Moskal-Hoyo, M},
	doi = {10.1007/s00334-024-00986-w},
	journal-iso = {VEG HIST ARCHAEOBOT},
	journal = {VEGETATION HISTORY AND ARCHAEOBOTANY},
	unique-id = {34568108},
	issn = {0939-6314},
	abstract = {The Neolithic and Copper Age (CA) of Hungary (6000–2800 cal bc ) represents a meticulous construction of settlement structure, material culture, arable farming and herding techniques with at least one, but likely several reappearing population movements that brought in innovations and possibly contributed to the societal changes in this period. The last couple of decades witnessed a considerable progress in the study of concurrent vegetation, climate and landscape management changes particularly via the increased number of high-resolution pollen records, archaeobotanical and archaeological investigations, coupled with stable isotope analyses of the charred cereal assemblages. In this review we synthetize the results of these research projects and demonstrate that the Neolithic and CA landscapes of Hungary were characterised by mixed oak forest communities, and in the territory of Hungary thermophilous steppe oak forests were present in the lowland landscape that were the principal choice of early farmers represented by the Körös-Starčevo-Criş cultures. Climate modelling and climate reconstruction from these regions indicate higher than preindustrial summer mean temperatures and higher than modern summer rainfall. We demonstrate that Linear Pottery Culture was the first culture that technologically advanced to clear larger plots of land for crop cultivation purposes. The first large scale and landscape level clearance is discernible in the Hungarian pollen records in the Late Neolithic period, when population size likely reached its Neolithic maximum, both in the lowlands and the surrounding mid-mountains.},
	year = {2024},
	eissn = {1617-6278},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Raczky, Pál/0000-0001-5556-723X; Pálfi, Ivett/0000-0001-9814-3410; Darabos, Gabriella/0000-0001-8070-5630}
}

@article{MTMT:34536076,
	title = {A Step from Vulnerability to Resilience: Restoring the Landscape Water-Storage Capacity of the Great Hungarian Plain—An Assessment and a Proposal},
	url = {https://m2.mtmt.hu/api/publication/34536076},
	author = {Timár, Gábor and Jakab, Gusztáv and Székely, Balázs},
	doi = {10.3390/land13020146},
	journal-iso = {LAND-BASEL},
	journal = {LAND (BASEL)},
	volume = {13},
	unique-id = {34536076},
	abstract = {The extreme drought in Europe in 2022 also hit hard the Great Hungarian Plain. In this short overview article, we summarize the natural environmental conditions of the region and the impact of river control works on the water-retention capacity of the landscape. In this respect, we also review the impact of intensive agricultural cultivation on soil structure and on soil moisture in light of the meteorological elements of the 2022 drought. The most important change is that the soil stores much less moisture than in the natural state; therefore, under the meteorological conditions of summer 2022, the evapotranspiration capacity was reduced. As a result, the low humidity in the air layers above the ground is not sufficient to trigger summer showers and thunderstorms associated with weather fronts and local heat convection anymore. Our proposed solution is to restore about one-fifth of the area to the original land types and usage before large-field agriculture. Low-lying areas should be transformed into a mosaic-like landscape with good water supply and evapotranspiration capacity to humidify the lower air layers. Furthermore, the unfavorable soil structure that has resulted from intensive agriculture should also be converted into more permeable soil to enhance infiltration.},
	year = {2024},
	eissn = {2073-445X},
	orcid-numbers = {Timár, Gábor/0000-0001-9675-6192; Jakab, Gusztáv/0000-0002-2569-5967; Székely, Balázs/0000-0002-6552-4329}
}