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1
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Candle wax shells, morphodynamics, and the Cambrian explosion

100%
Seilacher A.
Acta Palaeontologica Polonica
|
1993
|
tom 38
|
nr 3-4
2

The Pomeranian Phase marginal scarp of the outwash plain near Insko (West Pomerania)

86%
Karczewski A.
Quaestiones Geographicae
|
2003
|
tom 22
3

Ecological aspects of sedimentology. 7th National Meeting of Sedimentologists, Wojcieszow, July 2-4, 1998

86%
Raczynski P.
Geologia Sudetica
|
1999
|
tom 32
|
nr 1
4

Depositional processes within the frontal ice-cored moraine system, Ragnar glacier, Svalbard

72%
Ewertowski M., Kasprzak L., Szuman I., Tomczyk A. M.
Quaestiones Geographicae
|
2010
|
tom 29
|
nr 1
5

Albian to Early Turonian flysch-flyschoid deposits in the Branisko Succession at Kietowy Stream, Pieniny Klippen Belt, Carpathians

72%
Bak K.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1993
|
tom 41
|
nr 1
6

Polish geological research on King George Island, West Antarctica [1977-1996]

72%
Birkenmajer K.
Polish Polar Research
|
1996
|
tom 17
|
nr 3-4
7

The Kapp Lyell diamictite [Late Proterozoic], Bellsund, Spitsbergen: sedimentological evidence for its non-glacial origin

72%
Birkenmajer K.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
2003
|
tom 51
|
nr 1
8

Shell thanatocenoses as an object of malacological studies

58%
Alexandrowicz S. W.
Folia Malacologica
|
1998
|
tom 06
|
nr 1-4
9
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Ostracods and facies of the Early and Middle Frasnian at Devils Gate in Nevada: Relationship to the Alamo Event

58%
Casier J. G., Berra I., Olempska E., Sandberg C., Preat A.
Acta Palaeontologica Polonica
|
2006
|
tom 51
|
nr 4
813-828
In order to document the Alamo Event and to investigate its influence on shallow−marine environments, we undertook a study of ostracods, conodonts, and analysis of the sedimentology of the lower member of the type Devils Gate Limestone. Six major carbonate microfacies (MF1–MF6) ranging from open−marine environments below storm wave base to pre−evaporitic supratidal lagoons were recognized. The sedimentological study detected no important sedimentological changes during the Alamo Event; only an influx of detrital material and lithoclasts indicate that an unusual event had occurred. Ostracods are generally rare or absent in the lower member of the Devils Gate Limestone, and only 2,000 carapaces, valves and fragments were extracted; from these some 26 taxa were identified. Two new species, Voronina? eureka and Serenida dorsoplicata are proposed. The ostracods belong to the Eifelian Mega−Assemblage and their distribution was influenced by strong salinity variations. Because of the rarity and low diversity of ostracods and conodonts in samples collected from the lower part of the lower member of the Devils Gate Limestone it is not adequate to demonstrate conclusively an extinction event close to the Alamo Event Bed. Nevertheless the greater abundance and diversity of ostracods above this bed seems to indicate that the Alamo Event did not result in significant extinction of ostracod taxa in this shallow water setting. The ostracod fauna present in the lower member of the Devils Gate Limestone suggests faunal exchanges between Nevada and the Russian Platform via the Western Canadian platform.
10

Geological research of the Polish Geodynamic Expeditions to West Antarctica, 1984-1991: Antarctic Peninsula and adjacent islands

58%
Birkenmajer K.
Polish Polar Research
|
1998
|
tom 19
|
nr 1-2
11
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Ostracods and fore-reef sedimentology of the Frasnian-Famennian boundary beds in Kielce [Holy Cross Mountains, Poland]

58%
Casier J. G., Devleeschouwer X., Lethiers F., Preat A., Racki G.
Acta Palaeontologica Polonica
|
2002
|
tom 47
|
nr 2
Four major microfacies have been recognized in the Psie Górki section and the bioclastic content indicates an open marine environment in the photic zone close to an algal shole. Sedimentological studies point to a regressive episode starting close to the Frasnian–Famennian boundary. The regressive microfacies pattern is revealed by the presence of semirestricted algal microbreccias that compose all of the lower part of the Famennian. The regression was accompanied by meteoric water invasion as the sea level fell. Seventy−six ostracod species are recorded. The ostracod assemblage, dominated by podocopids, belongs to the Eifelian ecotype and is indicative of a well−oxygenated marine environment below fair−weather wave base in the Frasnian part of the section, and of shallower environments in the base of the Famennian. No ostracod assemblage characteristic of hypoxic or semi−restricted water conditions has been recorded. The rate of extinction of ostracod species (>70%) close to the Frasnian–Famennian boundary is comparable with that known on the same level in several other sections investigated in the world. Five new ostracod species are proposed by J.−G. Casier and F. Lethiers: Selebratina vellicata, Samarella? minuta, Bairdiocypris ventrorecta, Acratia pentagona, and “Bairdia” psiegorkiensis.
12

The earliest fossil record of a medium-sized penguin

51%
Jadwiszczak P., Chapman S. D.
Polish Polar Research
|
2011
|
tom 32
|
nr 3
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