TY - JOUR AU - Kiss, Gabriella Ilona AU - Szabó, Péter AU - Túri, Marianna AU - Futó, István AU - Kovács, János AU - Palcsu, László TI - Comparison of different preparation methods for oxygen isotope determination of phosphate in mammal tooth enamel JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 65 PY - 2023 IS - 2 SP - 144 EP - 157 PG - 14 SN - 1788-2281 DO - 10.1556/24.2023.00132 UR - https://m2.mtmt.hu/api/publication/34180795 ID - 34180795 N1 - Isotope Climatology and Environmental Research Centre, HUN-REN Institute for Nuclear Research, Debrecen, Hungary Doctoral School of Physics, University of Debrecen, Debrecen, Hungary Institute of Geography and Earth Sciences, University of Pécs, Pécs, Hungary Export Date: 1 January 2024 Correspondence Address: Kiss, G.I.; Isotope Climatology and Environmental Research Centre, Bem tér 18/C, Hungary; email: kiss.gabriella@atomki.hu AB - We tested several sample pre-treatment protocols for the study of oxygen isotope ratios in the phosphate phase of mammalian enamel of ten different fossil samples. We investigated the effect of different pre-treatment methods and the duration of the hydrogen fluoride treatment on enamel samples from skeletal phosphate with known δ 18 O values. The samples had been measured previously, so we could compare the ratios measured in our laboratory with the previous values to choose the best chemical preparation procedure. Four pre-soaking methods and two different time intervals of 2 mol dm −3 hydrogen fluoride treatment were compared during our experiments. In our experimental conditions, the distilled water wash and the 6 h of soaking in hydrogen fluoride gave the closest results to the expected δ -values. The steps of the tested preparation processes were repeated at least three times on each sample, so the reproducibility of the process could be also investigated. LA - English DB - MTMT ER - TY - JOUR AU - Franca, LDM. AU - Dantas, MAT. AU - Araújo-Júnior, HID TI - Bibliometric analysis of isotopic studies on Quaternary megafauna available in the Scopus database JF - ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS J2 - AN ACAD BRAS CIENC VL - 94 PY - 2022 IS - 3 SN - 0001-3765 DO - 10.1590/0001-3765202220211404 UR - https://m2.mtmt.hu/api/publication/33298845 ID - 33298845 LA - English DB - MTMT ER - TY - JOUR AU - Szabó, Péter AU - Kovács, János AU - Kocsis, L AU - Vennemann, T AU - Domingo, L AU - Újvári, Gábor AU - Halmai, Ákos AU - Pirkhoffer, Ervin AU - Codrea, V TI - Pliocene - Early Pleistocene continental climate and vegetation in Europe based on stable isotope compositions of mammal tooth enamel JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 288 PY - 2022 PG - 19 SN - 0277-3791 DO - 10.1016/j.quascirev.2022.107572 UR - https://m2.mtmt.hu/api/publication/32861079 ID - 32861079 AB - There is an increasing need for paleoclimate records from continental settings to better understand the climatic changes during critical periods such as the Pliocene and Early Pleistocene. Present data indicates a transition from a warmer than present-day climate to a substantially different cooler climate. This study reviews the oxygen and carbon isotope compositions of mammalian tooth enamel for the Pliocene and Early Pleistocene of South and Central Europe to reconstruct the spatial distribution and temporal changes of the vegetation and oxygen isotope composition of precipitation (d18Oppt). In addition to a literature review, this study adds new stable isotope measurements for this period. All d13C values indicate C3 ecosystems and reflect major changes in the water use efficiency and/or in the prevailing humidity. The reconstructed major floral types range from woodland to woodland ‒ mesic grassland in all of the investigated regions. The carbon isotope compositions of fossil mammal teeth demonstrate that the spatial distribution of vegetation was broadly similar to those of the present-day for the Early/Late Pliocene e Early Pleistocene, with the most “closed” vegetation in Central and Northern Italy, while open mesic grassland vegetation covers can be reconstructed for the Iberian Peninsula, Massif Central region (Central France) and the Carpathian Basin. The calculated d18Oppt values give a negative temporal shift of about 1e1.5‰ from the Early Pliocene to Late Pliocene e Early Pleistocene in three regions (Iberian Peninsula, Central Italy, Carpathian Basin), potentially representing a 1.5e3.0 C decrease in mean annual temperatures (MAT) over time. In the Massif Central region and the Carpathian Basin, the d18Oppt values are almost the same for the Late Pliocene and Early Pleistocene, while in Northern Italy the values decreased over that period. The d18Oppt values are in the range of present-day d18Oppt values over the Early Pliocene and somewhat lower than present-day values for the Late Pliocene - Early Pleistocene in most of the regions. Because most other proxies indicate warmer than present-day climate for the Early Pliocene and similar to present-day climate for the Early Pleistocene, the d18Oppt values are generally lower than expected, which can be partially explained by local effects. LA - English DB - MTMT ER - TY - JOUR AU - Curran, S AU - Terhune, C AU - Croitor, R AU - Drăgușin, V AU - Fox, DL. AU - Garrett, N AU - Ironside, LB. AU - Petculescu, A AU - Pobiner, B AU - Robinson, C AU - Robu, M AU - Tanţău, I AU - Ungar, P TI - Multiproxy paleoenvironmental reconstruction of Early Pleistocene sites from the Olteţ River Valley of Romania JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 574 PY - 2021 SN - 0031-0182 DO - 10.1016/j.palaeo.2021.110445 UR - https://m2.mtmt.hu/api/publication/32032724 ID - 32032724 N1 - Export Date: 23 May 2021 CODEN: PPPYA LA - English DB - MTMT ER - TY - JOUR AU - Stefaniak, K AU - Stachowicz-Rybka, R AU - Borówka, RK. AU - Hrynowiecka, A AU - Sobczyk, A AU - Moskal-del Hoyo, M AU - Kotowski, A AU - Nowakowski, D AU - Krajcarz, MT. AU - Billia, EME. AU - Persico, D AU - Burkanova, EM. AU - Leshchinskiy, SV. AU - van Asperen, E AU - Ratajczak, U AU - Shpansky, AV. AU - Lempart, M AU - Wach, B AU - Niska, M AU - van der Made, J AU - Stachowicz, K AU - Lenarczyk, J AU - Piątek, J AU - Kovalchuk, O TI - Browsers, grazers or mix-feeders? Study of the diet of extinct Pleistocene Eurasian forest rhinoceros Stephanorhinus kirchbergensis (Jäger, 1839) and woolly rhinoceros Coelodonta antiquitatis (Blumenbach, 1799) JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 605-606 PY - 2021 SP - 192 EP - 212 PG - 21 SN - 1040-6182 DO - 10.1016/j.quaint.2020.08.039 UR - https://m2.mtmt.hu/api/publication/31811398 ID - 31811398 N1 - Funding Agency and Grant Number: National Science Centre, Poland [0201/2048/18]; Russian Science Foundation (RNF) [20-17-00033]; Russian Science Foundation [20-17-00033] Funding Source: Russian Science Foundation Funding text: This research was supported by the grant No. 0201/2048/18 "Life and death of extinct rhino (Stephanorhinus sp.) from Western Poland: a multiproxy paleoenvironmental approach" finaced by the National Science Centre, Poland. Research by Elena M. Burkanova and Sergey V. Leshchisnkiy was funded by a grant from the Russian Science Founda-tion (RNF) , Project No. 20-17-00033. We warmly thank Adele Bertini (University of Florence) and anonymous reviewer for very helpful re-view comments and suggestions. We are also thankful to Izabela Lorek and the Management of the Regional Museum in Konin for sharing the specimen of S. kirchergensis tooth from Konin, Gwidon Jakubowski and the Management of the Museum of the Earth of the Polish Academy of Sciences for providing the possibility of taking isotope samples from S. kirchbergensis teeth from Warsaw. Katarzyna Cywa from W. Szafer Botany Institute, Polish Academy of Science is acknowledged for the maceration of palynological samples. We also thank Zoltan Barkaszi for proofreading the text. LA - English DB - MTMT ER - TY - JOUR AU - Szabó, Bence AU - Pazonyi, Piroska AU - Tóth, Emőke AU - Magyari, Enikő Katalin AU - Kiss, Gabriella Ilona AU - Rinyu, László AU - Futó, István AU - Virág, Attila TI - Pleistocene and holocene palaeoenvironmental reconstruction of the carpathian basin based on multiproxy analysis of cervid teeth JF - HISTORICAL BIOLOGY J2 - HIST BIOL VL - 33 PY - 2021 IS - 12 SP - 3307 EP - 3325 PG - 19 SN - 0891-2963 DO - 10.1080/08912963.2020.1863960 UR - https://m2.mtmt.hu/api/publication/31797540 ID - 31797540 N1 - Eötvös Loránd University, Department of Palaeontology, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Debrecen, Hungary MTA-MTM-ELTE Research Group for Paleontology, Budapest, Hungary Eötvös Loránd University, Department of Environmental and Landscape Geography, Budapest, Hungary Export Date: 29 January 2021 Correspondence Address: Szabó, B.; Eötvös Loránd University, Hungary; email: szabobence.pal@gmail.com Eötvös Loránd University, Department of Palaeontology, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Debrecen, Hungary MTA-MTM-ELTE Research Group for Paleontology, Budapest, Hungary Eötvös Loránd University, Department of Environmental and Landscape Geography, Budapest, Hungary Export Date: 28 May 2021 Correspondence Address: Szabó, B.; Eötvös Loránd University, Hungary; email: szabobence.pal@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Cirilli, O AU - Pandolfi, L AU - Bernor, RL. TI - The Villafranchian perissodactyls of Italy: knowledge of the fossil record and future research perspectives JF - GEOBIOS J2 - GEOBIOS-LYON VL - 63 PY - 2020 SP - 1 EP - 21 PG - 21 SN - 0016-6995 DO - 10.1016/j.geobios.2020.09.001 UR - https://m2.mtmt.hu/api/publication/31811389 ID - 31811389 N1 - Dottorato di Ricerca in Scienze della Terra, Università degli Studi di Pisa, Via S. Maria 53, Pisa, I-56126, Italy Paleo[Fab]Lab, Dipartimento di Scienze della Terra, Università degli Studi di Firenze, Via G. La Pira 4, Firenze, I-50121, Italy College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, Washington D.C., 20059, United States Human Origins Program, Department of Anthropology, National Museum of Natural History, Smithsonian Institution, Washington D.C., 20013, United States Cited By :14 Export Date: 26 May 2023 Correspondence Address: Cirilli, O.; Dottorato di Ricerca in Scienze della Terra, Via S. Maria 53, Italy; email: omar.cirilli@phd.unipi.it LA - English DB - MTMT ER - TY - JOUR AU - Radović, P. AU - Radonjić, M. AU - Billia, EME. TI - Pleistocene rhinoceros from bogovina cave: The first report of stephanorhinus hundsheimensis toula, 1902 (mammalia, rhinocerotidae) from serbia JF - PALAEONTOLOGIA ELECTRONICA J2 - PALAEONTOL ELECTRON VL - 23 PY - 2020 IS - 2 PG - 20 SN - 1935-3952 DO - 10.26879/985 UR - https://m2.mtmt.hu/api/publication/31650468 ID - 31650468 N1 - Export Date: 4 November 2020 AB - Finds of Pleistocene rhinoceros are rare in Serbia, and only one species (the woolly rhinoceros Coelodonta antiquitatis Blumenbach, 1799) has been reported so far. The current paper presents the dental material of an extinct so-called Hundsheim rhinoceros, Stephanorhinus hundsheimensis Toula, 1902 from Bogovina Cave (Eastern Serbia). Both the morphological and metric characteristics of the teeth are consistent with the attribution to S. hundsheimensis. Unfortunately, the rhinoceros material originated from an uncertain geological context, so there is no firm basis for dating. However, a potential association with a caballoid horse tooth could hint at an age of 600 ka or less for the assemblage, which would indicate a relatively late date for the Hundsheim rhinoceros from Bogovina Cave. LA - English DB - MTMT ER - TY - JOUR AU - Ballatore, M AU - Breda, M TI - Revision of the rhinoceros remains (Rhinocerotidae, Mammalia) from the late Pliocene of Etouaires (Auvergne, France) and the morphological distinction between the postcranial bones of Stephanorhinus elatus and S. etruscus JF - COMPTES RENDUS PALEVOL J2 - CR PALEVOL VL - 18 PY - 2019 IS - 2 SP - 191 EP - 208 PG - 18 SN - 1631-0683 DO - 10.1016/j.crpv.2018.06.003 UR - https://m2.mtmt.hu/api/publication/27686285 ID - 27686285 LA - English DB - MTMT ER - TY - JOUR AU - Demény, Attila AU - Gugora, Ariana AU - Kesjár, D. AU - Lécuyer, C. AU - Fourel, F. TI - Stable isotope analyses of the carbonate component of bones and teeth: The need for method standardization JF - JOURNAL OF ARCHAEOLOGICAL SCIENCE J2 - J ARCHAEOL SCI VL - 109 PY - 2019 SN - 0305-4403 DO - 10.1016/j.jas.2019.104979 UR - https://m2.mtmt.hu/api/publication/30763353 ID - 30763353 N1 - Export Date: 12 August 2019 LA - English DB - MTMT ER - TY - THES AU - Esker, DA. TI - Thermoregulation and Dental Isotopes Reveal the Behavior and Environment of Pleistocene Megafauna at Waco Mammoth National Monument PB - Baylor University PY - 2019 SP - 120 SN - 9781392396599 UR - https://m2.mtmt.hu/api/publication/31176787 ID - 31176787 N1 - Import hibák 2020-02-14 11:14 A jelleget az importban szereplő adat alapján nem lehetett meghatározni a következő elemhez: THES, alapártelmezett érték került beállításra. A3: Forman, Steven L.; AB - Waco Mammoth National Monument (WMNM) in central Texas is a significant Pleistocene paleontological site, containing at least 16 Columbian mammoths and specimens of 12 other vertebrate taxa. Interpreting this site, however, is contingent on understanding the environment Pleistocene animals lived in and how they interacted with that environment behaviorally. Actualistic studies of modern analogs can be used to better understand the behavior and geographic range of a Pleistocene animal and thus increase their usefulness as paleoclimate and paleoenvironmental indicators. Mass and thermal modeling studies done on modern tortoises have been used to determine the temperature tolerance of the giant tortoise species of central Texas, constraining the climate present at WMNM during its formation. Understanding the long-term movements of a fossil organism can reflect the environment it lives in. Strontium isotope ratio analysis of megafaunal teeth from WMNM have shown that not all of the mammoths at the site shared a geographic origin. The behavior revealed–mammoths congregated at WMNM from a wide area–necessitated a reconsideration of the long-standing mechanism of death for the megafauna there. Serial analysis of carbon and oxygen isotopes from the same teeth revealed that while the animals at WMNM shared a diet, some may have had distinct sources of drinking water. They also reveal that the WMNM megafauna lived in a drier, more drought-prone world that previously thought. Taking a multi-proxy approach to better understand interactions between Pleistocene megafauna and the environmental changes they experienced should inform our attempts to conserve our remaining megafauna. LA - English DB - MTMT ER - TY - JOUR AU - Pandolfi, L AU - Codrea, VA. AU - Popescu, A TI - Stephanorhinus jeanvireti (Mammalia, Rhinocerotidae) from the early Pleistocene of Coltesti (southwestern Romania) JF - COMPTES RENDUS PALEVOL J2 - CR PALEVOL VL - 18 PY - 2019 IS - 8 SP - 1041 EP - 1056 PG - 16 SN - 1631-0683 DO - 10.1016/j.crpv.2019.01.004 UR - https://m2.mtmt.hu/api/publication/31082976 ID - 31082976 AB - The Rhinocerotidae material from the early Pleistocene Tetoiu Formation of Coltesti (south-western Romania) is here described for the first time. The rhinoceros is documented by calcaneus and second, third, and fourth metatarsals, probably belonging to the same individual. The morphology and the dimensions of these specimens enable us to record the presence of Stephanorhinus jeanvireti, a relatively rare rhinoceros usually reported from late Pliocene European localities and recently considered a junior synonym of S. elatus. Nevertheless, the taxon Rhinoceros elatus is here regarded as a nomen dubium and the name S. jeanvireti is retained in order to maintain nomenclatural stability, being it based on much more diagnostic material. In Romania, S. jeanvireti has been listed within a few late Pliocene faunal assemblages, but the rhinoceros remains are fragmentary and isolated bones. The Coltesti find is among the best documented records of S. jeanvireti in Romania. The biochronological distribution of S. jeanvireti is mainly confined within the MNQ16 (early and early middle Villafranchian), and its first occurrence is doubtfully reported in late MNQ15 faunas. The record of Coltesti (MNQ17/MNQ18) represents, instead, the last occurrence of this taxon in Europe. (C) 2019 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Xueye, W AU - Zihua, T TI - HIGH SPATIAL RESOLUTION ISOTOPE ANALYSIS OF ENAMEL BASED ON INCREMENTAL FEATURES JF - QUATERNARY SCIENCES J2 - QUATERN SCI VL - 39 PY - 2019 IS - 1 SP - 228 EP - 239 PG - 12 SN - 1001-7410 DO - 10.11928/j.issn.1001-7410.2019.01.21 UR - https://m2.mtmt.hu/api/publication/34040170 ID - 34040170 LA - Chinese DB - MTMT ER - TY - JOUR AU - Pandolfi, L AU - Spadi, M AU - Martinetto, E AU - Kotsakis, T AU - Esu, D TI - New data on the lower Pleistocene (Gelasian) lignite beds of Castel San Pietro (Rieti, Central Italy) JF - RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA J2 - RIV IT PALEON STRATIG VL - 123 PY - 2017 IS - 2 SP - 335 EP - 346 PG - 12 SN - 0035-6883 DO - 10.13130/2039-4942/8622 UR - https://m2.mtmt.hu/api/publication/26657648 ID - 26657648 LA - English DB - MTMT ER -