Zobrazeno 1 - 10
of 118
pro vyhledávání: '"Vlad, CODREA A."'
Autor:
Vlad, CODREA A.1,2,3,4, Florina, DIACONU5 florinadiaconu@yahoo.com
Publikováno v:
Oltenia, Studii si Comunicari Seria Stiintele Naturii. Nov2024, Vol. 40 Issue 1, p7-12. 6p.
Publikováno v:
Palaeoworld. 31:140-152
Isolated pharyngeal teeth, pectoral, dorsal and suborbital fish spines were unearthed in a new outcrop located on the right bank of the Prut River, at Falciu, Romania. They document Late Miocene aquatic ecosystems of the Dacian basin. Seven taxa were
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6fc96b17a476f16f11249fe28c60cb96
https://doi.org/10.1016/j.palwor.2021.01.004
https://doi.org/10.1016/j.palwor.2021.01.004
Autor:
Nicolae Trif, Vlad Codrea
Publikováno v:
Annales g?ologiques de la Peninsule balkanique. 83:1-12
Some discoveries from the continental deposits of the paleogeographic landmass named the ?Ha?eg Island? complete the fossil record of the Maastrichtian fish fauna of Europe. Teeth belonging to the Lonchidiidae and three morphotypes of Teleostei indet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::546b226f3ef25298e7d446ba8fb25c80
https://doi.org/10.2298/gabp220424001t
https://doi.org/10.2298/gabp220424001t
Autor:
Jérémy Tissier, Damien Becker, Vlad Codrea, Loïc Costeur, Cristina Fărcaş, Alexandru Solomon, Marton Venczel, Olivier Maridet
Publikováno v:
PLoS ONE, Vol 13, Iss 4, p e0193774 (2018)
Amynodontidae is a family of Rhinocerotoidea (Mammalia, Perissodactyla) known from the late Early Eocene to the latest Oligocene, in North America and Eurasia. European Amynodontidae are very rare, and all remains belong almost exclusively to a singl
Externí odkaz:
https://doaj.org/article/973fef18969440a5932e486e2b8a4da2
Autor:
László, VERESS1 laciveress@yahoo.com, Vlad, CODREA A.1 vlad.codrea@ubbcluj.ro
Publikováno v:
Oltenia, Studii si Comunicari Seria Stiintele Naturii. 2020, Vol. 36 Issue 1, p7-20. 14p.
Autor:
Ramona Bălc, Nicolae Trif, Vlad Codrea, Raluca Bindiu-Haitonic, Jason C. Seitz, Viorel Arghiuș
Publikováno v:
Historical Biology. 34:1788-1816
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6400c98431b07133428608f15c3950c5
https://doi.org/10.1080/08912963.2021.1980879
https://doi.org/10.1080/08912963.2021.1980879
Publikováno v:
Journal of Mammalian Evolution. 29:1-26
Among the Late Cretaceous fossil sites of Europe, only those from the so-called “Haţeg Island” in Transylvania, western Romania, are remarkable by their abundance in mammal remains. Curiously, all of them belong to a single family of multituberc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e06b40257b4647d6cfca4f1fa358398
https://doi.org/10.1007/s10914-021-09564-7
https://doi.org/10.1007/s10914-021-09564-7
Publikováno v:
Journal of Systematic Palaeontology. 19:1237-1270
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e22686b1458c985bec8e95e20ba458d6
https://doi.org/10.1080/14772019.2022.2028025
https://doi.org/10.1080/14772019.2022.2028025
Autor:
Péter Szabó, János Kovács, László Kocsis, Torsten Vennemann, Laura Domingo, Gábor Újvári, Ákos Halmai, Ervin Pirkhoffer, Vlad Codrea
Publikováno v:
E-Prints Complutense. Archivo Institucional de la UCM
instname
Quaternary Science Reviews, vol. 288, pp. 107572
instname
Quaternary Science Reviews, vol. 288, pp. 107572
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 presen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5304266848534eea5b9e115d92345225
https://eprints.ucm.es/id/eprint/73428/
https://eprints.ucm.es/id/eprint/73428/
Publikováno v:
Palaeontologia Electronica.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ece30e60e8f07eb911227394b43bcbe8
https://doi.org/10.26879/1156
https://doi.org/10.26879/1156