Results 91 to 100 of about 1,410 (213)

New localities of Protostropharia alcis (Basidiomycota, Agaricales) in Poland

open access: yesActa Mycologica, 2014
The present paper provides new records of Protostropharia alcis in Poland. So far this species was known in the country only from several latest localities in the Biebrza National Park (Biebrza Basin) and the Kampinos National Park (Warsaw Basin).
Marek Halama, Barbara Kudławiec
doaj   +1 more source

Lower Cambrian trace fossils from the Holy Cross Mountains, Poland

open access: yes, 2002
Additional data on the Lower Cambrian ichnotaxa from the Holy Cross Mountains are presented. Nine ichnotaxa are described for the first time from the area, additional descriptions of three known ichnotaxa are supplied, and two ichnotaxa are shown to have
Żylińska, A., Orłowski, S.
core  

The oldest rocks of the Holy Cross Mountains, Poland – biostratigraphy of the Cambrian Czarna Shale Formation in the vicinity of Kotuszów

open access: yes, 2016
Three lower Cambrian acritarch assemblages recognized in four outcrops in the vicinity of Kotuszów in the southernmost part of the Palaeozoic inlier of the Holy Cross Mountains span a stratigraphic interval from the uppermost part of the Asteridium ...
Żylińska, A., Szczepanik, Z.
core   +1 more source

Geochemistry and mineralogy of technogenic soils developed on old mine heaps of abandoned iron ore mines in the Ławęczna area (Holy Cross Mountains, south-central Poland)

open access: yesSoil Science Annual, 2018
The article presents the results of preliminary geochemical and mineralogical studies of technogenic soils (Technosols) of abandoned iron ore mines on the Ławęczna Hill near Miedziana Góra in the Holy Cross (Świętokrzyskie) Mountains, southcentral Poland.
Swęd Maciej, Niedzielski Przemysław
doaj   +1 more source

Tectonic subdivision of Poland: Holy Cross Mountains and adjacent areas

open access: yes, 2008
The Holy Cross Mountains Fold Belt, the Odrzywół–Ćmielów Graben, the Radom-Kraoenik Horst and the Mazovia-Lublin Graben are located in the contact zone between the Paleozoic Platform and the East European Craton, eastwards of the Variscan foreland basin.
Konon, A.
core  

Seismic Imaging of the Mesozoic Bedrock Relief and Geological Structure under Quaternary Sediment Cover: The Bolmin Syncline (SW Holy Cross Mountains, Poland)

open access: yesGeosciences, 2019
The clear and detailed images of geological structures that can be obtained by seismic methods are one of the main drivers of their popularity in geological research.
Bartosz Owoc   +4 more
doaj   +1 more source

Fossils of Antiarcha (Vertebrata, Placodermi) in the Devonian of the Holy Cross Mountains (central Poland)

open access: yes, 2006
The paper indicates a similarity between remains of various Palaeozoic fishes thus hindering identification of fossil of Antiarcha—rare placoderms in the Holy Cross Mountains.
Szrek, P.
core  

The first occurrence of the earliest species of Acadoparadoxides outside West Gondwana (Cambrian; Holy Cross Mountains, Poland)

open access: yes, 2018
Two hundred and eighty specimens of paradoxidids from two localities in the Holy Cross Mountains (Poland) have been reanalysed using morphometric techniques. Revision of the dataset provided evidence for the presence of two endemic taxa: Acadoparadoxides
JAKUB NOWICKI, ANNA ŻYLIŃSKA
core   +1 more source

Small-scale cyclic deposition in the Frasnian (Upper Devonian) of the Holy Cross Mountains, Poland [PDF]

open access: yes, 2014
In sections exposing Frasnian limestones at five outcrops in the Holy Cross Mountains, five lithofacies (L1 to L5) that represent upper slope to basinal environments are identified.
Vierek, A., Vierek, Aleksandra
core   +1 more source

Palaeoenvironments of the Eifelian dolomites with earliest tetrapod trackways (Holy Cross Mountains, Poland)

open access: yesPalaeogeography, Palaeoclimatology, Palaeoecology, 2015
Abstract The Eifelian dolomites in the Zachelmie Quarry (Holy Cross Mountains, Poland) contain trackways and tracks of tetrapods 390–391 Ma old, and thus the oldest known so far. The environments of the trackway-bearing beds have been investigated using sedimentological, palaeontological, geochemical and palaeomagnetic methods.
Marek, Narkiewicz   +6 more
openaire   +2 more sources

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