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Tytuł:
A long-term influence of anthropogenic alkalization on molluscs biodiversity in an area affected by cement industry : Świętokrzyskie Mountains, South-Central Poland
Długotrwały wpływ antropogemicznej alkalizacji na bioróżnorodność mięczaków w obszarze oddziaływania przemysłu cementowo-wapienniczego : południowo-centralna Polska
Autorzy:
Barga-Więcławska, J. A.
Świercz, A.
Powiązania:
https://bibliotekanauki.pl/articles/204692.pdf
Data publikacji:
2015
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
malacofauna
cement industry
biodiversity
soil properties
Świętokrzyskie Mountains
South-Central Poland
przemysł cementowy
bioróżnorodność
właściwości gleby
Góry Świętokrzyskie
Opis:
The presented paper reports data from malacological and pedological studies carried out at sites representing diverse biotopes (beech wood, coniferous forest, and meadow) located 2 km away from the Dyckerhoff Cement Plant in Sitkówka-Nowiny in 1992 and in 2008–2009. The studies aimed to determine physicochemical properties of soils exposed to cement and limestone dust emission and to identify composition of snail communities inhabiting three different biotopes in relation to physicochemical properties of soils, and to grasp the dynamics of the alkalization-dependent changes in physicochemical properties of soils and their impact on the composition and ecological structure of malacofauna.
Prezentowana praca przedstawia wyniki wieloletnich badań malakologicznych i gleboznawczych, które zostały przeprowadzone w zróżnicowanych biotopach (las, bór, łąka) znajdujących się do 2 km od emitora pyłów, Cementowni Dyckerhoff Sitkówka-Nowiny w latach: 1992–1993 oraz 2008–2009. Celem pracy było przedstawienie zmian właściwości fizyczno-chemicznych gleb, przekształconych pod wpływem alkalizacji, które zadecydowały o składzie gatunkowym malakofauny bytującej w 3 różnych biotopach.
Źródło:
Archives of Environmental Protection; 2015, 41, 4; 49-61
2083-4772
2083-4810
Pojawia się w:
Archives of Environmental Protection
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Funkcjonowanie i zasięg oddziaływania przestrzennego klastra „Uzdrowiska świętokrzyskie”
The functioning and scope of spatial interaction of the „Świętokrzyskie Health-Resorts Cluster”
Autorzy:
Barcicki, M.
Gałuszka, G.
Kamińska, W.
Wilk-Grzywna, M.
Powiązania:
https://bibliotekanauki.pl/articles/2031826.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Health-resorts cluster
Polska
spatial extent
Świętokrzyskie voivodeship
Opis:
The aim of the article is to assess the functioning and scope of spatial interaction of the Świętokrzyskie Health-Resorts Cluster. It is one of the younger clusters of this type operating in the country. The study found that cluster functioning was not fully effective as the networks of cooperation and competition were mainly confined to members’ participation in conferences and working meetings. The biggest shortcoming of this cluster is the lack of formalized cooperation of members. Cluster functions as regional and supra-regional. The therapists come mainly from the Świętokrzyskie region and the neighboring regions.
Źródło:
Biuletyn Komitetu Przestrzennego Zagospodarowania Kraju PAN; 2017, 267; 133-162
0079-3493
Pojawia się w:
Biuletyn Komitetu Przestrzennego Zagospodarowania Kraju PAN
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Turystyka wiejska we Francji a agroturystyka i turystyka wiejska w regionie świętokrzyskim – analiza porównawcza
Rural Tourism in France vs. Agritourism and Rural Tourism in the Świętokrzyskie Region in Poland – Comparison Analise
Autorzy:
Plit, Florian
Powiązania:
https://bibliotekanauki.pl/articles/2028840.pdf
Data publikacji:
2015
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Differences
Massif Central (France)
rural tourism
similarities
Świętokrzyskie
(Poland).
Opis:
The purpose of the article is to compare tourist service in the countryside of Świętokrzyskie Region in Poland and in provincial France (Bourgogne, Auvergne, Midi-Pyrénées; which the author walked across in 2010-2014). These regions share a number of characteristics, such as differentiated natural environments, rich historical heritage, contemporary delays in the economic development. Even the common opinions on the inhabitants of these regions tend to be similar. The opportunities for development are sought in the domain of tourism. Both in Świętokrzyskie and in provincial French countryside rural tourism is quite well developed, and the hospitality infrastructure is highly diversified with respect to the quality of services and the levels of prices. The differences consist in, for instance, lower share of the grey economy in France, higher reliability of information in France, availability of information in France at the lodging places of the tourist attractions in the more broadly conceived neighbourhood than in Poland, provision of information on catering during excursions (e.g. recommended restaurants), as well as a wider spectrum of accompanying events, organised by the communes. On the other hand – it is easier in Poland to rent a bike.
Źródło:
Studia komitetu przestrzennego zagospodarowania kraju PAN; 2015, 162; 217-228
0079-3507
Pojawia się w:
Studia komitetu przestrzennego zagospodarowania kraju PAN
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Record of the Pleistocene at karst sites of the Świętokrzyskie (Holy Cross) Mountains region – a review
Autorzy:
Urban, Jan
Hercman, Helena
Ochman, Katarzyna
Kasza, Andrzej
Powiązania:
https://bibliotekanauki.pl/articles/2025126.pdf
Data publikacji:
2019
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
karst sites
caves
U-series dating
Pleistocene
Świętokrzyskie (Holy Cross) Mountains
Opis:
The objective of this paper is a review of data on reconstruction of the Pleistocene palaeogeography (environment) and stratigraphy based on studies of karst sites in the Świętokrzyskie (Holy Cross) Mountains. Although the number of known Pleistocene karst sites in this region is small, the investigations of them have played a crucial role in a research of the Pleistocene. The study of the Kozi Grzbiet site provided the first evidences for new climatostratigraphy and classification of glaciations in Poland. The explanation of genesis of cryogenic calcite crystals discovered in Chelosiowa Jama-Jaskinia Jaworznicka cave system started a new direction of palaeoenvironmental reconstructions of the last glacial period. Kadzielnia palaeontological site was one of the first Early Pleistocene fossil assemblages in karst studied in Poland, whereas Raj cave provided abundant palaeontological and archaeological material from the Last Glacial. Other sites are of less scientific importance, however some of them can be used in education and popularisation of geosciences. Small number of already studied sites does not exclude discoveries of next sites of high scientific importance.
Źródło:
Studia Quaternaria; 2019, 36; 87-108
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The oldest species of ?Yavorskia (Tabulata) from the Upper Famennian of the Holy Cross Mountains (Poland)
Autorzy:
Zapalski, M.
Berkowski, B.
Powiązania:
https://bibliotekanauki.pl/articles/138864.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
famen
Góry Świętokrzyskie
korale
migracje
Tabulata
corals
Famennian
Holy Cross Mountains
migrations
Opis:
A single perfectly preserved colony of a tabulate coral assigned tentatively to the genus Yavorskia Fomitchev, 1931, collected from Upper Famennian beds (Palmatolepis expansa conodont Zone) in a trench located north of the Kowala Quarry (Holy Cross Mts., central Poland) is here described as a new species, ?Y. paszkowskii sp. nov. It differs from other representatives of the genus in the lack of dissepimental structures and in smaller corallite diameters, and may therefore represent the ancestral taxon of this typically early Carboniferous genus. Yavorskia tabulates were apparently migrating eastwards along the southern margin of Laurussia and farther east and north towards Siberia, as they appear in the Famennian in Europe and in the early Carboniferous in the Altaides. Such a conclusion is consistent with previous observations on Early.Middle Devonian pleurodictyform tabulate distribution.
Źródło:
Acta Geologica Polonica; 2012, 62, 2; 197-204
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The uppermost Emsian and lower Eifelian in the Kielce Region of the Holy Cross Mts. Part I: Lithostratigraphy.
Autorzy:
Wójcik, K.
Powiązania:
https://bibliotekanauki.pl/articles/138993.pdf
Data publikacji:
2015
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
lithostratigraphy
Devonian
Eifelian
Holy Cross Mountains
Dolomites
litostratygrafia
dewon
Góry Świętokrzyskie
Dolomity
Opis:
The paper provides a description of primary geological logs, characteristics and formal lithostratigraphy of the uppermost Emsian and lower Eifelian of the Kielce Region of the Holy Cross Mts., central Poland. Nine sections of this interval, representing the whole area of the Kielce Region, and ranging between the Lower Devonian clastics of the Winna Formation and the Middle Devonian carbonates of the Kowala Formation were studied. The succession is divided into the Barania Góra Dolomite and Limestone Formation and the Wojciechowice Dolomite Formation. Six members are distinguished within the former. In the western part of the region these are (in stratigraphical order): Porzecze Claystone Member, Dębska Wola Dolomite Member, Dąbrowa Limestone Member, and Brzeziny Dolomite Member. In the eastern part, the formation is divided into the Janczyce Dolomite Member and the Jurkowice Dolomite Member. Additionally, the Wszachów Dolomite Member and Nowy Staw Dolomite Member are distinguished within the overlying Wojciechowice Formation. The thickness of the uppermost Emsian–Eifelian succession ranges from ca. 200 m in the eastern part to ca. 130 m in the western part of the Kielce Region.
Źródło:
Acta Geologica Polonica; 2015, 65, 2; 141-179
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Innowacyjność gospodarstw agroturystycznych w regionie świętokrzyskim
Innovation of Agritourist Enterprises in the Świętokrzyskie Region
Autorzy:
Baran, Ewa
Kiniorska, Iwona
Noga, Monika
Powiązania:
https://bibliotekanauki.pl/articles/2027647.pdf
Data publikacji:
2015
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Agritourist enterprises
innovation
Local Action Group „Ziemia Jędrzejowska –
Gryf”
Świętokrzyskie Region
„Ziemia Sandomierska”
Opis:
The aim of the work is to assess of the level an innovation of agritourist enterprises co-operating with Local Action Group „Ziemia Jędrzejowska – Gryf” and „Ziemia Sandomierska”. The grading procedure was used to measure the level of innovation of agrotturist farms. In total, 52 agritourist farms were analyzed. The analysis has presented a low level of innovation agritourist enterprises.
Źródło:
Studia komitetu przestrzennego zagospodarowania kraju PAN; 2015, 162; 247-262
0079-3507
Pojawia się w:
Studia komitetu przestrzennego zagospodarowania kraju PAN
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Evidence of Late Cretaceous/Cenozoic strike-slip faulting within the late Palaeozoic Holy Cross Mts. Fold Belt, Poland: Józefka releasing stepover
Autorzy:
Skompski, Stanisław
Konon, Andrzej
Wysocka, Anna
Czarniecka, Urszula
Powiązania:
https://bibliotekanauki.pl/articles/139410.pdf
Data publikacji:
2019
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
strike-slip faulting
releasing stepover
Holy Cross Mountains
Buntsandstein
uskok przesuwczy
Góry Świętokrzyskie
piaskowiec pstry
Opis:
The aim of this study was to reconstruct the location mechanism of a Triassic sandstone wedge within folded Palaeozoic rocks. A vertically oriented Buntsandstein succession (Lower Triassic) from Józefka Quarry (Holy Cross Mountains, central Poland), steeply wedged within folded Devonian carbonates, is recognised as an effect of normal faulting within a releasing stepover. The sandstone succession, corresponding to the Zagnańsk Formation in the local lithostratigraphic scheme, is represented by two complexes, interpreted as deposits of a sand-dominated alluvial plain (older complex), and coarse-grained sands and gravels of a braided river system (younger complex). The sandstone complex was primarily formed as the lowermost part of the several kilometres thick Mesozoic cover of the Holy Cross Mountains Fold Belt (HCFB), later eroded as a result of the Late Cretaceous/Paleogene uplift of the area. Tectonic analysis of the present-day position of the deformed sandstone succession shows that it is fault-bounded by a system of strike-slip and normal faults, which we interpret as a releasing stepover. Accordingly, the formation of the stepover in the central part of the late Palaeozoic HCFB is evidence of a significant role of strike-slip faulting within this tectonic unit during Late Cretaceous/Paleogene times. The faulting was probably triggered by reactivation of the terminal Palaeozoic strike-slip fault pattern along the western border of the Teisseyre–Tornquist Zone.
Źródło:
Acta Geologica Polonica; 2019, 69, 1; 89-105
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The oldest rocks of the Holy Cross Mountains, Poland – biostratigraphy of the Cambrian Czarna Shale Formation in the vicinity of Kotuszów
Autorzy:
Szczepanik, Z.
Żylińska, A.
Powiązania:
https://bibliotekanauki.pl/articles/138942.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Cambrian
Fortunian
Terreneuvian
Holy Cross Mountains
Kotuszów
acritarcha
biostratigraphy
kambr
fortun
terenew
Góry Świętokrzyskie
Acritarcha
biostratygrafia
Opis:
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 tornatum–Comasphaeridium velvetum Assemblage Zone to the Skiagia ornata–Fimbriaglomerella membranacea Assemblage Zone (most probably its lower part). According to current views (Moczydłowska and Yin 2012), this interval corresponds to the upper part of the Fortunian and to Stage 2 of the Terreneuvian Series. The strata yielding the oldest assemblage are thus the oldest precisely documented rocks in the Palaeozoic succession of the Holy Cross Mountains, and the oldest Cambrian rocks exposed on the surface in Poland. The current biostratigraphic scheme for the pre-trilobitic part of the Cambrian System in the Holy Cross Mountains should be modified so that it is based on local acritarch interval subzones.
Źródło:
Acta Geologica Polonica; 2016, 66, 3; 267-280
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Middle/Upper Devonian brachiopod shell concentrations from the intra-shelf basinal carbonates of the Holy Cross Mountains (central Poland)
Autorzy:
Skompski, S.
Baliński, A.
Szulczewski, M.
Zawadzka, I.
Powiązania:
https://bibliotekanauki.pl/articles/139310.pdf
Data publikacji:
2018
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Devonian
brachiopods
Holy Cross Mountains
allochthonous origin of coquina
dewon
ramienionogi
Góry Świętokrzyskie
skała osadowa
pochodzenie allochtoniczne
Opis:
A huge isolated accumulation, more than 3 m thick and 10 m wide, of densely packed, uncrushed brachiopods has been found in Józefka Quarry within the Middle/Upper Devonian Szydłówek Beds deposited in a relatively deep environment of an intrashelf basin (Kostomłoty facies zone, western Holy Cross Mountains, Poland). The low-diversity assemblage is strongly dominated by the atrypide Desquamatia globosa jozefkae Baliński subsp. nov. and, to a lesser degree, by the rhynchonellide Coeloterorhynchus dillanus (Schmidt, 1941), which constitute 72.8% and 22.1% of the fauna, respectively. Less frequent are specimens representing the genera Hypothyridina, Schizophoria and Phlogoiderynchus. According to the conodont fauna found within the coquina bed, the stratigraphic position of the shell accumulation is close to the Givetian/ Frasnian boundary. The brachiopods are associated with numerous crinoids and less frequent bryozoans, receptaculitids (Palaeozoic problematica), sponges and solitary corals. Although it is difficult to entirely exclude the autochthonous nature of the brachiopod coquina member, its allochthonous origin and redeposition of the brachiopod shells to the deep basin by gravity flows is much more probable. Such conclusion is supported by the following facts: (1) the position of the complex in a succession of deep-marine basinal facies impoverished in oxygen; (2) its lateral thinning-out and composite internal stratification; (3) the lensshaped geometry of the coquina bed in the section perpendicular to the bedding dip; (4) high variability of the sediments preserved within the shells; and (5) the preferred orientation of the shells. The brachiopods mixed with crinoidal debris were probably transported by low-velocity, high-density, gravity-induced debris flows. Lack of fossils typical of the Middle Devonian shallows, such as massive stromatoporoids, amphiporoids and tabulates, indicates that the source area of the bioclastic material was not located in the shallowest part of the shelf, but most probably on a submarine sea-mount to the north of present-day Józefka, as suggested by earlier investigators. The triggering mechanism of the allochthonous deposition was an earthquake rather than storm activity. The enormous thickness of the brachiopod complex is probably caused by the sinking of bioclastic material, transported in succeeding depositional multi-events, in a soft, muddy bottom, typical of the Szydłówek Beds deposition.
Źródło:
Acta Geologica Polonica; 2018, 68, 4; 607-633
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The oldest Cambrian trilobites from the Holy Cross Mountains, Poland : taxonomic, stratigraphic and biogeographic reappraisal
Autorzy:
Żylińska, A.
Powiązania:
https://bibliotekanauki.pl/articles/139416.pdf
Data publikacji:
2013
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
biogeografia
Ellipsocephalus
Góry Świętokrzyskie
kambr
stratygrafia
Trylobity
biogeography
Cambrian Series 2
Ellipsocephalidae
Holmiidae
Holy Cross Mountains
stratigraphy
Trilobita
Opis:
Authorship issues are clarified, new photographic documentation is provided and emended systematic descriptions are presented for the oldest Cambrian trilobite taxa from the Holy Cross Mountains (Poland). Biostratigraphic analysis of the fauna allows correlation with the traditional Holmia kjerulfi-group Zone of Scandinavia, the Callavia Zone of Britain and Newfoundland, the lower and middle part of the Sectigena Zone of Morocco and the Marianian Stage of Spain. The trilobites display a strong biogeographic signal linked with West Gondwana and Avalonia and a suggestion is made that the TESZ margin of Baltica with the Malopolska Massif was liable to currents from those areas that distributed planktonic trilobite larvae.
Źródło:
Acta Geologica Polonica; 2013, 63, 1; 57-87
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A new heterobranch gastropod, Chelidonura radwanskii sp. nov., from the middle Miocene of the Korytnica Basin (Holy Cross Mountains, Poland)
Autorzy:
Bałuk, W.
Powiązania:
https://bibliotekanauki.pl/articles/138602.pdf
Data publikacji:
2018
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
heterobranch gastropod
middle Miocene
littoral boulder
Korytnica Basin
Holy Cross Mountains
ślimaki
środkowy miocen
głaz przybrzeżny
basen Korytnica
Góry Świętokrzyskie
Opis:
A new species of heterobranch gastropods, the hammerhead Chelidonura radwanskii sp. nov., found in the socalled Pleurotoma-clays of middle Miocene (Langhian) age in the environs of Korytnica, southern Holy Cross Mountains, Poland, is described. It is the first fossil representative of Chelidonura A. Adams, 1850. This tiny gastropod is named in honour of the late Professor Andrzej Radwański.
Źródło:
Acta Geologica Polonica; 2018, 68, 4; 499-502
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Taxonomic revision of the Paradoxididae Hawle and Corda, 1847 from the Miaolingian (Cambrian) of the Holy Cross Mountains, Poland: a morphometric approach to simply deformed trilobites
Autorzy:
Nowicki, Jakub
Żylińska, Anna
Powiązania:
https://bibliotekanauki.pl/articles/2024019.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
paradoxididae
miaolingian
Cambrian
Holy Cross Mountains
geometric morphometrics
simple deformation
Słowiec Hill
trylobity
miaoling
kambr
góry Świętokrzyskie
morfometria geometryczna
Słowiec
Opis:
The taxonomy of simply deformed paradoxidids from the Miaolingian (Cambrian) of Słowiec Hill, Holy Cross Mountains, Poland, is revised based on morphometric analysis. The material represents two species: Acadoparadoxides slowiecensis (Czarnocki in Orłowski, 1965) and Hydrocephalus? polonicus (Czarnocki in Orłowski, 1965). A new assemblage zone based on the combined although not precisely known ranges of these two taxa is suggested replacing the previous Paradoxides polonicus Zone of Orłowski (1975, 1988, 1992a). The Acadoparadoxides slowiecensis–Hydrocephalus? polonicus Assemblage Zone corresponds to the middle and upper part of the Wuliuan Stage (lower Miaolingian).
Źródło:
Acta Geologica Polonica; 2021, 71, 4; 371--391
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mnin restraining stepover – evidence of significant Cretaceous–Cenozoic dextral strike-slip faulting along the Teisseyre-Tornquist Zone?
Autorzy:
Konon, A.
Ostrowski, S.
Rybak-Ostrowska, B.
Ludwiniak, M.
Śmigielski, M.
Wyglądała, M.
Uroda, J.
Kowalczyk, S.
Mieszkowski, R.
Kłopotowska, A.
Powiązania:
https://bibliotekanauki.pl/articles/138980.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
strike-slip fault pattern
restraining stepover
Permo-Mesozoic cover
Holy Cross Mountains Fold Belt
uskok przesuwczy
pokrywa
perm
mezozoik
Góry Świętokrzyskie
Opis:
A newly recognized Mnin restraining stepover is identified in the Permo-Mesozoic cover of the western part of the Late Palaeozoic Holy Cross Mountains Fold Belt (Poland), within a fault pattern consisting of dextral strikeslip faults. The formation of a large contractional structure at the Late Cretaceous – Cenozoic transition displays the significant role of strike-slip faulting along the western border of the Teisseyre-Tornquist Zone, in the foreland of the Polish part of the Carpathian Orogen. Theoretical relationships between the maximum fault offsets/ mean step length, as well as between the maximum fault offsets/mean step width allowed the estimation of the values of possible offsets along the Snochowice and Mieczyn faults forming the Mnin stepover. The estimated values suggest displacements of as much as several tens of kilometres. The observed offset along the Tokarnia Fault and theoretical calculations suggest that the strike-slip faults west of the Late Palaeozoic Holy Cross Mountains Fold Belt belong to a large strike-slip fault system. We postulate that the observed significant refraction of the faults forming the anastomosing fault pattern is related also to the interaction of the NW-SE-striking faults formed along the western border of the Teisseyre-Tornquist Zone and the reactivated WNW-ESE-striking faults belonging to the fault systems of the northern margin of the Tethys Ocean.
Źródło:
Acta Geologica Polonica; 2016, 66, 3; 429-449
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Brachiopods and stratigraphy of the Upper Devonian (Frasnian) succession of the Radlin Syncline (Holy Cross Mountains, Poland)
Autorzy:
Baliński, A.
Racki, G.
Halamski, A. T.
Powiązania:
https://bibliotekanauki.pl/articles/139163.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Devonian
Frasnian
stratigraphy
carbon isotope stratigraphy
punctata Event
brachiopods
Holy Cross Mountains
dewon
fran
stratygrafia
stratygrafia izotopowa węgla
zdarzenie punctata
ramienionogi
Góry Świętokrzyskie
Opis:
The lower part of the Frasnian succession in the Radlin Syncline (Kielce–Łagów Synclinorium, southern region of the Holy Cross Mountains), in the two studied successions: Józefka at Górno and (for the first time) Radlin, consists of the rhythmic marly Szydłówek Beds, the fossil-rich limestones of the Wietrznia Beds (locally) and the atypically developed, calcareous Kostomłoty Beds. The carbon isotope chemostratigraphic pattern overall corresponds well to the global Early–Middle Frasnian biogeochemical perturbation, even if the major punctata positive excursion is only fragmentarily recorded in the Kostomłoty intrashelf basin. Two brachiopod assemblages are abundantly represented in both sections: the Phlogoiderhynchus polonicus Assemblage, typical of the Szydłówek Beds, and the Biernatella lentiformis Assemblage, limited to the middle part of the Wietrznia Beds. Both are highly dominated by the index species. Twenty nine lower Frasnian brachiopod species (Craniida – 1 species, Strophomenida – 1, Productida – 2, Protorthida – 1, Orthida – 5, Pentamerida – 1, Rhynchonellida – 4, Atrypida – 4, Athyridida – 3, Spiriferida – 4, Spiriferinida – 3) are described from the Szydłówek and Wietrznia Beds. Seven new species are introduced: Skenidioides cretus Halamski sp. nov., Biernatium minus Baliński sp. nov., Monelasmina montisjosephi Baliński sp. nov., Atryparia (Costatrypa) agricolae Halamski and Baliński sp. nov., Davidsonia enmerkaris Halamski sp. nov., Leptathyris gornensis Baliński sp. nov., and Echinocoelia parva Baliński sp. nov. Davidsonia enmerkaris Halamski sp. nov. is intermediate between Davidsonia Bouchard-Chantereaux, 1849 and Rugodavidsonia Copper, 1996 and is the youngest known representative of the suborder Davidsonioidea Copper, 1996. Skenidioides cretus Halamski sp. nov. is the last representative of the genus. Statistical investigation of a large sample of Spinatrypina (Exatrypa) explanata did not confirm the existence of two dimorphic forms, coarse- and fine-ribbed. The high-diversity Biernatella lentiformis Assemblage is quite dissimilar to coeval brachiopod assemblages described heretofore from the Holy Cross Mountains region. It is interpreted as consisting of mostly parautochthonous dwellers of deep-slope muddy habitats and a local, occasionally storm-agitated, intra-basin brachiopod-crinoid-coral shoal. The fauna was adapted probably to cooler and nutrient-poor waters during an initial phase of the severe carbon cycle perturbation.
Źródło:
Acta Geologica Polonica; 2016, 66, 2; 125-174
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 16

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