Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Saccocoma"'
Publikováno v:
PalZ. 93:357-369
Lumbricaria Münster is described for the first time outside the Tethys domain from distal facies of the Tithonian Vaca Muerta Formation, Neuquén Basin, Argentina. The studied material consists of elongate, convolute, cylindrical coprolites, showing
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7c729923b0939a2c835764c4154438c1
https://doi.org/10.1007/s12542-019-00447-0
https://doi.org/10.1007/s12542-019-00447-0
Publikováno v:
Geobios. 60:61-77
Upper Jurassic (Kimmeridgian–Tithonian) and Cretaceous (Berriasian–Barremian) strata of the Ukrainian part of the Carpathian Foredeep basement are rich, at least locally, in crinoid remains. Crinoids belonging to cyrtocrinids (Cyrtocrinida) are r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee99a5b4d5ce23109baeecb1c3ea48cf
https://doi.org/10.1016/j.geobios.2020.04.005
https://doi.org/10.1016/j.geobios.2020.04.005
Publikováno v:
Facies. 66
In the Late Jurassic, the rifting process led to the disintegration of the southern margin of the North European Platform and to the opening of the Outer Carpathian flysch basin sedimentary system. The initial sediments accumulated in the northern pa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ea33072fefc5ef1f5301b1811fe3ccc
https://doi.org/10.1007/s10347-020-0595-y
https://doi.org/10.1007/s10347-020-0595-y
Publikováno v:
Cretaceous Research. 92:66-93
During Late Jurassic-Early Cretaceous the Pontides were the site of a wide carbonate platform facing the Tethys ocean in the south. In the western Pontides the Upper Jurassic-Lower Cretaceous shallow marine carbonates abut the Tethyan Izmir-Ankara su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::759958cc0ddee8a9b6bc202df0774aa0
https://doi.org/10.1016/j.cretres.2018.07.009
https://doi.org/10.1016/j.cretres.2018.07.009
Publikováno v:
Sedimentary Geology. 360:54-72
New biostratigraphical, chemical and stable isotope (C, O) data are presented from the Lokut section (Transdanubian Range, Hungary) representing a ca. 13 m thick continuous succession of Lower Tithonian–Lower Berriasian pelagic limestones. The stud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c6d5e6a154a303517f2efe4449b9ee4d
https://doi.org/10.1016/j.sedgeo.2017.08.004
https://doi.org/10.1016/j.sedgeo.2017.08.004
Autor:
Jozef Michalík, Daniela Reháková, Jacek Grabowski, Otília Lintnerová, Petr Schnabl, Šimon Kdýr
Publikováno v:
Cretaceous Research. 118:104659
An integrated study of micro- and nannoplankton distribution, O and C isotopes and palaeomagnetic record of nine Carpathian sections provided a key interpretation tool to characterize the Jurassic–Cretaceous (J/K) boundary transition. Biostratigrap
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::de70ca447021c6bcc97fa2425a91c8c7
https://doi.org/10.1016/j.cretres.2020.104659
https://doi.org/10.1016/j.cretres.2020.104659
Publikováno v:
The Earth After Us : What legacy will humans leave in the rocks?, 2008.
Externí odkaz:
https://doi.org/10.1093/oso/9780199214976.003.0014
Akademický článek
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Autor:
Hans Hess
Publikováno v:
Swiss Journal of Palaeontology. 134:77-107
New material of known roveacrinids from two Cretaceous sites in Texas is described. Upper Albian strata at Saginaw Quarry furnished rich material of Poecilocrinus latealatus and Roveacrinus pyramidalis; for these two forms cups can be combined with p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c173696fc96b2e3b3dea16c89ab163ca
https://doi.org/10.1007/s13358-015-0076-z
https://doi.org/10.1007/s13358-015-0076-z
Autor:
Hans Hess
Publikováno v:
Swiss Journal of Palaeontology. 133:121-140
The material for the present paper is based on 50 kg of processed sediment from the Early Kimmeridgian of Geisingen. The most frequent crinoids comprise cups and brachials of the roveacrinid Saccocoma quenstedti while Crassicoma feifeli is represente
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4120c123cf3a1314dc1e3fdb4e58f115
https://doi.org/10.1007/s13358-014-0064-8
https://doi.org/10.1007/s13358-014-0064-8