Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Scolecodont"'
Autor:
T. A. Kulashova
Publikováno v:
Paleontological Journal. 53:972-976
Five types of scolecodont microornamentation are recognized: striate, regular, granular, rhombic, and columnar. The connection between the type of ornamentation and the position of the scolecodont element in the jaw is analyzed. The ability of scolec
Publikováno v:
Stratigraphy and Geological Correlation. 27:207-233
Conodonts, scolecodonts, and foraminifers from the Frasnian Age (Upper Devonian) (Shchigry-16 borehole, Nizhnekrasnoe village, Voronezh anteclise) were studied. Six conodont assemblages were identified: I for the Timan regional stage, II and III for
Publikováno v:
Palynology. 43:321-332
The scolecodonts (polychaete jaws) are a significant group of dispersed palynomorphs in Palaeozoic rocks. The growing literature considering the taxonomy of fossil jaw-bearing polychaetes presents some debates on their systematics and has generally l
Autor:
Stanislava Vodrážková, Jiří Frýda, L. Ferrová, Olle Hints, Michal Kubajko, Petra Tonarová, G. Susana de la Puente
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 97:419-438
The Zlíchovian/Dalejan boundary interval (Emsian, Lower Devonian) of the Pekárek Mill section was studied employing biostratigraphy (dacryoconarid tentaculites, conodonts) and palynology (chitinozoans, prasinophytes, scolecodonts) and microfacies a
Publikováno v:
GFF; 138(4), pp 502-509 (2016)
The record of scolecodonts (polychaete jaws) from the Ordovician of Sweden is very poor. In this paper, we document a Darriwilian (Middle Ordovician) assemblage recovered from palynological samples from the “orthoceratite limestone” (Lanna and Ho
Autor:
Michał Zatoń, Michał Rakociński
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 394:1-11
Small, light-brown and beige cylindrical structures found in the lower Famennian (Upper Devonian) shales and marls of the Holy Cross Mountains area, central Poland, have been investigated for the first time. Their compact, pellet-shaped morphology an
Publikováno v:
PALAIOS. 28:433-437
Conodonts and scolecodonts are common Paleozoic microfossils that are often used to determine the geothermometry of Paleozoic sequences. The two fossils, which can be difficult morphologically to distinguish one from the other, undergo a different th
Publikováno v:
Geological Society, London, Memoirs. 38:265-272
Eunicidan polychaetes formed a significant part of Early Palaeozoic marine invertebrate communities, as shown by the abundance and diversity of scolecodonts (polychaete jaws) in the fossil record. In this study we summarize the early radiation and bi
Publikováno v:
Review of Palaeobotany and Palynology. 164:251-271
Surface samples from the Ghelli and Soltan Maidan Formations in the Khoshyeilagh area of the eastern Alborz Range, northern Iran, were analyzed to determine the age and the stratigraphic relationship of these two units. The samples contained rich pal
Autor:
Åsa M. Frisk, Mats Eriksson
Publikováno v:
Geological Magazine. 148:269-287
The post-impact Dalby Limestone (Kukruse; Upper Ordovician) of the Tvären crater, southeastern Sweden, has been analysed with regards to polychaetes, as represented by scolecodonts. A palaeoecological succession is observed in the Tvären-2 drill co