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1

Coiling direction in Middle Miocene globorotaliids (Foraminiferida) : a case study in the Paratethys (Upper Silesia Basin, Poland)

Gonera M.

Geological Quarterly

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2018

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Vol. 62, No. 1

155--171

EN

The paper deals with sub-evaporite Badenian deposits (Middle Miocene, Paratethys) that display a sudden appearance of globorotaliid taxa showing preferences in the taxonomic set and coiling direction. An interval of sinistrally coiled Jenkinsella mayeri with proportionally coiled Globoconella bykovae is at the bottom of the studied sequence. It is followed by an interval of proportionally coiled Jenkinsella transsylvanica. Proportionally coiled Globoconella bykovae with a small number of proportionally coiled Jenkinsella transsylvanica are at the top of the Moravian (CPN 7) substage (Orbulina suturalis alias Lagenidae Zone). The sub-evaporite part of the Wielician (CPN 8) substage (Uvigerina costai alias Spiroplectammina Zone) began with a globorotaliid-barren interval (IIC biozone). It is followed by biozone IID displaying three globorotallid peaks amongst globorotallid-barren deposits. Only globoconellas are present in all these three events. Proportionally coiled Globoconella bykovae appeared first. It is followed by proportionally coiled Globoconella minoritesta and sinistrally coiled Globoconella bykovae at the end of the biozone IID. Coiling preferences of globorotaliids have been compared to changes in the hydrographic regime unfolding during the CPN 7 and CPN 8 in the studied area of the Paratethys. The study discovers that the coiling of globorotaliids responded selectively to the hydrographic changes. Globoconella bykovae is highly opportunistic and can tolerate considerable temperature changes. Specimens of this taxon persist to coil proportionally during the sub-evaporite Badenian, except for the shift to sinistral coiling just prior to the Wielician evaporites. Sinistrally coiled Jenkinsella mayeri is the most sensitive to hydrographic changes. This taxon retreated at the onset of the temperature drop during the mid-Moravian cryptic cooling. This cooling is marked by the new jenkinsellid occurrence – proportionally coiled Jenkinsella transsylvanica. Proportionally coiled Globoconella minoritesta is present in the middle of the IID globorotaliid peaks. The globorotaliid coiling data, presented in this paper, has been calibrated to the global stratigraphy. The integrated data (foraminifera, nannofossils, oxygen and carbon stable isotopes, radiometric measurements) supports the view that the CPN 7/CPN 8 boundary is coeval to the Langhian/Serravalian one. In the Polish part of the Carpathian Foredeep, the boundary runs within the Skawina Formation.

2

Rewitalizacja stanowisk geologicznych na obszarach wiejskich – przykład Wyżyny Miechowskiej

Gonera M.

Inżynieria Ekologiczna

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2017

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Vol. 18, nr 4

168--175

PL

W badaniach chronologii oraz przebiegu całokształtu procesów, jakie utworzyły obecny stan litosfery, geologia bazuje na reperowych profilami geologicznych dla poszczególnych rejonów Ziemi – stratotypach. Są to szczególne, wyselekcjonowane, profile litostratygraficznymi w terenie. W sensie fizycznym są to obiekty przyrody nieożywionej spełniające określone warunki reprezentatywności przebiegu zjawisk w historii geologicznej danego obszaru oraz będące wzorcami i punktami odniesienia do wszelkich geologicznych porównań. Dzięki stratotypom możliwa staje się korelacja (komunikacja) badań dziejów geologicznych pomiędzy poszczególnymi częściami świata. Zbadano fizyczny stan stratotypów miocenu (jednej z najszerzej reprezentowanych epok geologicznych obszaru Polski) na Wyżynie Miechowskiej – obszarze o znaczącej tradycji badań geologicznych, posiadającej obecnie status regionu o wybitnie wiejskiej gospodarce. Z przeprowadzonych badań terenowych wynika, że żaden spośród stratotypów miocenu nie znalazł się pośród realizacji Ustawy o ochronie przyrody. Te formy dziedzictwa przyrody nieożywionej uległy fizycznej degradacji oraz wyparciu ze świadomości lokalnych społeczności. Wyjątkiem okazał się stratotyp zlokalizowany w miejscu pozyskiwania kopalin. Lokalny zakład wydobywczy okazał się najsprawniejszym rozwiązaniem dla funkcjonowania i dostępności stratotypów. Ten właśnie rodzaj przemysłu i powiązany z nim niewielki zakład przerabiający surowiec – okazały się najskuteczniejszym mechanizmem wiążącym naukę (podstawowe badania geologiczne) i rewitalizację obszarów wiejskich. Ten kierunek rewitalizacji odbywa się poprzez nieinwazyjne dla środowiska naturalnego i zgodne z zasadami społecznej odpowiedzialności biznesu (CSR) pozyskiwanie surowca mineralnego dla wytwarzania unikatowych, regionalnych, produktów.

EN

The Miechów Upland is one of the meaningful areas for the study of the Miocene geology. Middle Miocene (Karpatian to Early Sarmatian) sediments have been recognised there. The deposits are highly variegated in regard to lithology. Brackish and fresh-water Karpatian sediments are followed by different rocks of broad marine transgression during Moravian, and finally by the early Sarmatian ones. Depending on the prominent paleo relief of the Cretaceous basement, varieties of sediments have been deposited during this time. Marly claystones, silts, sands with mudstone intercalations and detrital limestones (Rhodolith bioherms) are the most common. Moreover, the Middle Badenian sulphate evaporates are found in the Miechów Upland. State of the Miocene stratotype outcrops has been checked in this area. The access to most of them is impossible because of the soil and vegetation coverage within the abandoned opencasts. The only exception is a small, still operational silt-pit of the local brick-yard. It turned out that the two interests can be combined, effectively animating the local economy and warranting the access to stratotype section. Due to fertile Pleistocene loess soils, the region is extensively used by agriculture, but marred by relevant economic and social problems. Small-scale opencast mining, accompanied with innovative manufacturing of the resources (silts, clays, sands and carbonates) is proposed. Modern mining strongly conforms to ecological engineering principles and Corporate Social Responsibility (CSR) standards. Therefore, it poses no threat to the state of soils and the agricultural character of the region. The development of unique, regional products on the basis of local resources (e.g. unique, regional decorative stones or pottery) is worth to be considered by the LEADER program activities. The initiation of innovative mining enterprises and handcraft seems to be a good strategy to improve the local economy and a promising solution to highlight the image of country. With this approach, the revitalization stratotype outcrops and the economic development of rural areas by mineral business it will be possible, parallel to the ongoing agricultural circumstances and benefits.

3

Wielician (Middle Badenian) foraminifers from the stratotype area : Wieliczka Salt Mine, Poland (Paratethys, Middle Miocene)

Gonera M., Wiewiórka J., d'Obyrn K., Bukowski K.

Geological Quarterly

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2014

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Vol. 58, No. 3

427--438

EN

The most abundant benthic foraminifers recorded in the Wielician salt-enclosed xenoliths are: Bulimina spp., Uvigerina spp., Valvulineria complanata, and Cibicides pseudoungerianus. The predominant taxon in the planktonic assemblage is Globigerina bulloides with a median 98.9% in biozone IIC and 89.1% in the later IID. The IIC assemblage differs from the IID one in both taxon composi tion and abundance. The most pronounced differences are those revealed by Valvulineria complanata counts, number of benfhic taxa and the plankfonic/benthic (P/B) rafio. Pseudotriplasia minuta (one of the Wielician index taxa) occurs only in the IID biozone, present in 16 among 28 samples. There is a noticeable difference in sur- face sculpture morphology pattern in the predominant Bulimina and Uvigerina taxa in the IIC versus the IID biozones. There are smooth (Bulimina elongata) and weakly striate (Uvigerina semiornata plexus) forms in the IIC biozone, foll owed by heavily costate (Bulimina striata) and spinose-pustu l ate (Uvigerina orbignyana plexus) forms in the IID. Globigerina druryi and G. decoraperta- the CPN 8 planktonic index taxa - had not been found in the material studied. Globigerinita uvula is un- usually common in the samples studied. The samples analysed display an abundance of Globigerina bulloides typical of the sub-evaporite Wielician. Hence the studied Wielician stratotype area supports the thesis of the Globigerina bulloides Acme as the valid name designation for the substage.

4

Globorotaliid intervals of the sub-evaporite Badenian (Middle Miocene) in the Upper Silesia Basin (Central Paratethys, Poland)

Gonera M.

Geological Quarterly

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2013

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Vol. 57, No. 4

757–-768

EN

Globorotaliids of the Skawina Formation (Badenian) come from deposits representing CPN 7 (Orbulina suturalis Zone) and CPN 8 sub-evaporite Wielician (Globigerina druryi–G. decoraperta Zone alias Uvigerina costai Zone) age. There are two taxonomic groups of globorotaliids in the studied material: globoconellids (Globoconella bykovae and G. minoritesta) and jenkinsellids (Jenkinsella mayeri and J. transsylvanica). There are five stratigraphically-rank intervals of these foraminifers prior to the Middle Badenian salinity crisis in Central Paratethys. The investigated Badenian begins with G. bykovae–J. mayeri association followed by the first occurence (FO) of J. transsylvanica. The closing member of the CPN 7 biozone is the G. bykovae–J. transsylvanica assemblage. The jenkinsellids disappear during CPN 7: J. mayeri first and J. transsylvanica after. Since the base of CPN 8 in situ jenkinsellids have not been noted in the Badenian deposits. The CPN 8 begins with a stratigraphic interval barren of globorotaliids (biozone IIC in the Polish Paratethys). It is followed by episodic appearances of globoconellids (G. bykovae and G. minoritesta) in the sub-evaporite Wielician (IID biozone in Poland). G. minoritesta has been found in only one case so far. The globorotaliid stratigraphic units are distinct and well-correlated with changes in climate and the circulation of water masses in Paratethys. This study provides additional data on Mi3 in Paratethys. It documents a cryptic cooling event in the late Orbulina suturalis Zone (mid CPN 7) located at the late IIA–B assemblage (alias upper lagenide zone) in regional biostratigraphic scale. The event is recorded by J. transsylvanica Acme, matching with circa 1‰VPDB δ18O positive excursion. The event must have resulted in a considerable sea level drop – a trigger of the Moravian ecosystem demolition in the Paratethys environment.

5

Palaeoecology of the Middle Miocene foraminifera of the Nowy Sącz Basin (Polish Outer Carpathians)

Gonera M.

Geological Quarterly

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2012

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Vol. 56, No 1

107-116

EN

Foraminifera from newly exposed outcrop sections located in a Middle Miocene piggyback basin of the Outer Carpathians Nowy Sącz Basin indicate an environment of normal saline waters on the inner shelf and a temperature not lower than 18oC. The area was ideal for the proliferation of: Miliolina spp., Elphidium crispum, Ammonia beccarii and Pararotalia. The habitat below the sediment surface was not colonised by foraminifera. Planktonic foraminifera are absent. The age of the population studied is referred based on the climate-related data, to the Orbulina suturalis Zone of the Miocene Climate Optimum.

6

Isotopic events in the Early/Middle Badenian (Miocene) of the Upper Silesia Basin (Central Paratethys)

Gonera M., Bukowski K.

Geological Quarterly

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2012

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Vol. 56, No 3

561--568

EN

Middle Miocene foraminifera from the Skawina Formation of the Upper Silesia Basin have been analysed. The stable oxygen and carbon isotope signatures in Globigerinoides quadrilobatus (shallow pelagic), Globigerina bulloides (deeperpelagic) and Uvigerina spp. (benthic) tests show a temporal pattern of changes in the sections studied. The foraminiferal assemblage biozones of the Badenian that were identified earlier, on the basis of taxonomic composition, correspond to changes in the foraminiferal ẟI8O and ẟI3C values. The CPN7/CPN8 transition - as the Moravian/Wielician border - is marked by distinct isotopic events: a ẟ18O increase (IIAB/IIC boundary) followed by a ẟ13C decrease (IIC/IID boundary).

7

Foraminifera in slump deposits of the Badenian (Middle Miocene) Green Stratified Salt in Wieliczka, Poland

Gonera M., Bukowski K., d'Obyrn K., Wiewiórka J.

Geological Quarterly

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2012

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Vol. 56, No. 4

869–-880

EN

Taxonomic, quantitative and isotopic study of foraminifera from mudstone and claystone xenoliths incorporated into slump facies of the Stratified Salt Member of the Wieliczka deposit shows that the majority of xenoliths represent the CPN 8 biozone (Wielician substage, Badenian, Middle Miocene). The share of the CPN 7 biozone is minor; it was recorded in two of 26 samples analysed. The source area of xenoliths was the basinal part of the Carpathian Foredeep, located far off the shoreline (shallow-water taxa are not present in the samples); it represents the upper bathyal zone, in oxygenated conditions. Inbenthic, eutrophic and opportunistic foraminifers dominate the benthic environment of the CPN 8 span of time. Increased d18O values of the Globigerina bulloides tests (from +1.7‰ in CPN 7 to +2.3‰ in CPN 8 sediments) was due to the change from the Middle Miocene Climate Optimum to the Middle Miocene Climate Transition at the CPN 7/CPN 8 boundary. This palaeoclimate event is the marker of the Moravian/Wielician chronostratigraphic boundary in the Central Paratethys. The Wielician shows the distinct taxonomic reduction of the Moravian planktonic foraminifera and includes the Globigerina bulloides Acme.

8

Middle Miocene (Early Badenian) Amphistegina (Foraminiferida) from Olimpów (Central Paratethys, Poland)

Gonera M.

Annales Societatis Geologorum Poloniae

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2012

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Vol. 82, No. 2

151–-159

EN

Specimens of Middle Miocene (Early Badenian) Amphistegina from the Polish Carpathians were examined. A section, sampled at the Olimpów quarry, displays chloralgal carbonates, rich in rhodolith nodules. Symbiont-bearing foraminifera (Amphistegina, Elphidium and Asterigerinata) constitute 15–57% of the total foraminifera assemblage. Amphistegina hauerina d’Orbigny, 1846 is the only species of the genus in the deposits studied. The sensitivity of larger foraminifera to water turbulence and light availability was applied in a reconstruction of the community habitat. The diameter and thickness of the Amphistegina tests indicate that the habitat was a zone of low light penetration and weak energy – a palaeoenvironment, similar to that of the modern A. radiata (Hottinger et al., 1993). Changes in the sphericity of the Amphistegina tests reflect a temporal drop of bathymetry in the middle part of the section. This is supported by other environmentally controlled features of the foraminiferal assemblage: the percentages of both planktonic and symbiont-bearing forms, as well as the proportions of robust and flat forms of Elphidium. It is possible that this variation in depth was due to eustatic changes in sea level, caused by Event Mi3 of the Middle Miocene climatic cooling. The spiral diameter of the test was at its lowest value then, indicating that maturity was reached at a faster rate. The period of shoaling offered the best life conditions for Amphistegina in this particular area.

9

Geoochrona konserwatorska profilu wzorcowego warstw chodenickich (miocen zapadliska przedkarpackiego)

Gonera M., Wiewiórka J., Charkot J., Bukowski K., Mikulski D., Dudek K.

Przegląd Geologiczny

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2011

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Vol. 59, nr 10

671-677

EN

Stratotypes are indispensable to the correct usage of litho- and chronostratigraphy units. Stratotypes sustainability is the crucial factor. As the sustainability of the Chodenice Beds stratotype became in risk the searching for the substitution site of this type section had been undertaken. Micropaleontological and petrological hallmarks of the unit have been considered and perfectly analogical deposits have been found near by – in the Bochnia Salt Mine. Two of the mine corridors where Chodenice Beds crop out have been selected. The sites are protected as elements of the geocoservation net of the Bochnia Salt Mine, nominated as geological site no. 4 and 21.

10

Znaczenie badań patentowych w procesie kreacji innowacji

Adamowicz B., Gonera M.

Elektronika : konstrukcje, technologie, zastosowania

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2011

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Vol. 52, nr 10

143-146

PL

Zdefiniowano pojęcie innowacji. Przedstawiono cykl kreacji innowacji w oparciu o model konwersji wiedzy. Omówiono znaczenie informacji patentowej w procesie innowacyjnym, w szczególności rolę badań patentowych dla inkubacji nowych pomysłów. Podano schemat ogólnej metodyki badań patentowych stanu techniki. Podkreślono znaczenie MKP dla efektywnego wyszukiwania informacji. Sformułowano postulaty upowszechnienia prowadzenia badań patentowych i ich obligatoryjności w celu zwiększenia potencjału wiedzy twórców oraz eliminacji dublowania prac badawczo-rozwojowych.

EN

Conception of innovation was defined. The cycle of innovation creation based on knowledge conversion model was presented. The role of patent information in innovation process, particularly the importance of patent research for incubation of new ideas was discussed. There was inserted the outline of patent research general methodology for technology state of art investigation. The significance of Intemational Patent Classification for effective information finding was underlined. The postulates of dissemination of patent research carrying on and its obligation for enlarging the knowledge potential of creators and elimination of research and development works doubling were formulated.

11

Stan geoochrony konserwatorskiej w parkach krajobrazowych Polski

Gonera M.

Przegląd Geologiczny

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2010

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Vol. 58, nr 12

1139-1146

EN

The idea of establishing protected landscape parks was put forward in Poland 50 years ago. The result was fairly quick expansion in the number of protected landscape areas, up to 120 by now. Figures 1 and 2 show the progress in creation of such areas and their geographical distribution. The major goals and approach in management of the landscape parks were changing in time. The following stages may be distinguished in the landscape parks policy: protection of environment followed by landscape protection, protection of nature diversity and currently - biodiversity conservation (in accordance with Natura 2000 prerogatives). Also "geodiversity" make it necessary to treat the existing landscape parks as the potential areas of geoparks. One of key requirements which should be met by geoparks is a network of geological sites subjected to legal protection. These sites are the "backbone" of geopark. The paper presents situation in the Polish landscape parks with regard of this requirement by the end of the year 2008. At that time the number of geoconservation objects selected and categorized in 75 of those parks reached 551 (Fig. 3). Table 1 shows the typology of geological sites in relation to their importance for the Earth sciences The objects of the category A are the most valuable for geology whereas the remaining ones are mainly of geomorphological (B) and hydrological (C) value. Tables 2, 3 and 4 show the current state of conservation of geological sites in Polish landscape parks. In that presentation the area of Poland was divided into two parts with the line of extent of the Warta Glaciation as the boundary (Fig. 2). The Pleistocene deposits predominate north of that boundary whereas rocks of older stratigraphic units crop out at the surface south of it.

12

Badenian tuffite levels within the Carpathian orogenic front (Gdów-Bochnia area, Southern Poland): radio-isotopic dating and stratigraphic position

Bukowski K., de Leeuw A., Gonera M., Kuiper K. F., Krzywiec P., Peryt D.

Geological Quarterly

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2010

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Vol. 54, No 4

449-464

EN

We present new results of investigation of Middle Miocene Badenian tuffite levels exposed in Southern Poland within the Gdów "embayment" area (tuffites from Wiatowice, upper part of the Skawina Beds, foraminiferal biozone IIg) and compare them with the well known and extensively described Bochnia Tuffite level at Chodenice near Bochnia (upper part of the Chodenice Beds, foraminiferal biozone IIIA). The 4039

13

Obszary górnicze i geoochrona konserwatorska - niedoszacowane partnerstwo

Gonera M.

Górnictwo Odkrywkowe

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2009

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R. 50, nr 2-3

37-41

PL

Roli odsłonięć i odkrywek w badaniach i popularyzacji geologii nie da się przecenić. Dlatego czynne kamieniołomy, cegielnie, kopalnie odkrywkowe i podziemne są ważnymi obiektami dla poznawania geologii. Jednak te obiekty zanikają. Intencją geoochrony konserwatorskiej jest temu przeciwdziałać opierając się na zapisach ustawy o ochronie przyrody. Geologia gospodarcza i górnictwo nie wykorzystały dotychczas swoich atutów i nie sięgnęły po korzyści dane im potencjalnie przez tę ustawę. Chodzi o aplikację stanowiska dokumentacyjnego. Chodzi o to, ażeby powołanie i utrzymywanie obiektów tej kategorii ochrony odbywało się w zamian za określone korzyści dla gospodarza terenu: na przykład ulgi finansowe w podatku i opłatach eksploatacyjnych. Nie dokona tego sama argumentacja geoochrony konserwatorskiej. Potrzebne jest lobby sektora wydobywczego.

EN

The role of outcrops in geology is really substantial. Therefore different kinds of quarries, mines and brick-fields are highly valuable in geological education, train and tourist. Unfortunately, these objects are disappearing. The geoconservation is against of this, trying to proceed by bring into play the decrees contained in Polish Nature Protection Act. As yet the mine and applying geology sectors have not used its trumps to gain the potential benefits brining them by this Act. They did not ask the economical circumstances on set the geological documentary site in mine areas. Foundation and management of these geoconservation objects should be reward and recompensed; for example by reduced tax and licenses. This can't be performed only by geoconservation itself. The mine lobby support is needed to strengthen mining and geology in land management policy.

14

Historic salt mines in Wieliczka and Bochnia

Wiewiórka J., Charkot J., Dudek K., Gonera M.

Geoturystyka

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2009

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nr 3

61-70

EN

Historic salt mines in Wieliczka and Bochnia are situated by the old trade road from Kraków to the east, in the region well known from salt-making from brines since the Neolith (ca. 3500 BC). In Bochnia the rock salt was discovered in 1248, whereas in Wieliczka production of the rock salt was confirmed in the town charter in 1290. At the end of the 13th century both mines were united into the Kraków Saltworks. In the 16th century it was the biggest production centre in Poland and one of the biggest in Europe. The rock-salt exploitation ended in Bochnia in 1990 and in Wieliczka in 1996. Both deposits are situated within the Miocene (Badenian - M4) folded strata of the salt-bearing complex, consisting of the Skawina Formation (at the bottom), the Wieliczka Formation (containing the evaporites), and the Chodenice beds (at the top). The Wieliczka deposit consists of the upper boulder deposit and the lower stratiform one. The boulder deposit was formed as a result of submarine flows in southern part of the evaporite basin. Both the boulder and the stratiform deposits were finally shaped by the overthrust movements of the Outer Carpathians. The Bochnia deposit is limited to the northern limb of the Bochnia anticline, at the northern edge of the Outer Carpathians. The Wieliczka Salt Mine is written into the first UNESCO List of the World Cultural and Natural Heritage (1978) and recognised as a National Monument of History (1994). Since 2000 the Bochnia Salt Mine is the National Monument of History as well. In 1997 the Małopolska voivode issued a decree comprising legal protection of 40 documentated sites, important for geology of the Wieliczka deposit, and in 2000 the Natural Reserve "Crystal Caves" in Wieliczka was established. In 2005, twenty seven documentated sites were established and provided with legal protection in the Bochnia Salt Mine.

PL

Zabytkowe kopalnie soli w Wieliczce i Bochni znajdują się przy starym trakcie handlowym z Krakowa na wschód, w rejonie znanym z warzenia soli jeszcze w neolicie (ok. 3500 lat p.n. e.). W Bochni sól kamienną odkryto w 1248 roku, podczas gdy w Wieliczce wydobycie soli kamiennej jest wzmiankowane w akcie lokacyjnym miasta z 1290 roku. Pod koniec XIII wieku obydwie kopalnie zostały połączone w jedno królewskie przedsiębiorstwo - Krakowskie Żupy Solne. W XVI wieku był to największy ośrodek produkcyjny w Polsce i jeden z największych w Europie. Wydobycie soli kamiennej zakończyło się w Bochni w 1990, a w Wieliczce w 1996 roku. Obydwa złoża znajdują się w utworach sfałdowanego miocenu (baden - M4) jednostki zgłobickiej Karpat zewnętrznych. Seria solonośna składa się z formacji skawińskiej, wielickiej (ewaporaty) i warstw chodenickich. Złoże solne Wieliczki zbudowane jest z górnego złoża bryłowego ż dolnego pokładowego. Złoże bryłowe zostało utworzone w wyniku podmorskich spływów w południowej części basenu ewaporacyjnego. Obydwie części złoża zostały ostatecznie uformowane w wyniku ruchów nasuwczych Karpat. Złoże soli Bochnia znajduje się w północnym skrzydle antykliny Bochni, na północ od brzegu Karpat. W 1978 roku Kopalnia Soli Wieliczka została wpisana na pierwszą listę Światowego Dziedzictwa Kulturowego i Przyrodniczego UNESCO, a w 1994 roku uznana za Narodowy Pomnik Historii. Od 2000 roku Kopalnia Soli Bochnia jest również Narodowym Pomnikiem Historii. W 1997 roku dekretem wojewody małopolskiego objęto ochroną prawną, w formie stanowisk dokumentacyjnych, 40obiektów geologicznych w Kopalni Soli Wieliczka, a w 2000 roku ustanowiono rezerwat przyrody "Groty Kryształowe" w Wieliczce. W 2005 roku ochroną prawną objęto również 27 stanowisk dokumentacyjnych w Kopalni Soli Bochnia.

15

Ekologia w elektronice.

Gonera M.

Recykling

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2006

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nr 7-8

34-34

16

Z kart historii Przemysłowego Instytutu Elektroniki

Gonera M.

Elektronika : konstrukcje, technologie, zastosowania

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2006

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Vol. 47, nr 7

5-9

PL

Przedstawiono okresy rozwojowe i tematykę badawczą Przemysłowego Instytutu Elektroniki w Warszawie latach 1956-2006. Szerzej omówiono osiągnięcia Instytutu w II połowie XX wieku, które są mniej znane współczesnemu czytelnikowi.

EN

Development periods and research subject matter of Industrial Institute of Electronics in the time from 1956 till 2006 were presented. The achievements of Institute in the second half of XX century that are less known to contemporary reader were discussed wider.

17

Zabytki przyrody nieożywionej, czyli dobro nie powszechnego użytku

Gonera M.

Przegląd Geologiczny

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2005

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Vol. 53, nr 3

199--204

18

Uwarunkowania pomiaru szumów podwodnych powodowanych przez "ciche" obiekty w środowisku podwodnym

Kiciński W., Gonera M., Opara T.

Prace Przemysłowego Instytutu Elektroniki

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2004

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nr 149

58--68

PL

W referacie podjęto zagadnienie analizy klasy sygnałów niestacjonarnych powodowanych przez aparat tlenowy płetwonurka. Zaproponowano metodę analizy sygnałów pomiarowych bazującą na transformacji falkowej oraz wielowymiarowej analizie danych.

EN

The problem of processing of the class of measuring signals, so called transient signals, caused by shocks of the oxygen tank of diver has been discussed. The method of transient signals processing based on wavelet transform and multivariate data analysis has been described.

19

Niejednoznaczności transformacji Wignera w analizie sygnałów niestacjonarnych

Gonera M., Opara T.

Prace Przemysłowego Instytutu Elektroniki

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2004

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nr 149

38--47

PL

Stosowanie transformacji Wignera w analizie sygnałów generuje nowe częstotliwości, które w analizowanym sygnale nie występują. Przedstawiono przykłady ilustrujące to niekorzystne zjawisko. Jest ono charakterystyczne dla większości powszechnie stosowanych transformacji i stanowi źródło niejednoznaczności w interpretacji wyników. Powstawanie pozornych częstotliwości nasila się dla sygnałów niestacjonarnych. Omówiono możliwości ich identyfikacji oraz ograniczenia ich wpływu.

EN

Using the Wigner transformation for the noise analysis cause new spurious frequencies, which are absent in the observed signal. Examples illustrating this disadvantage are presented. This disadvantage proves to be an ambiguity source in the interpretation of results and is typical for whole commonly used transformations. The spurious frequencies appearing escalate for the nonstationary signals. The abilities of their identification and reducing are discussed.

20

Metody i narzędzia proekologicznego projektowania wyrobów elektronicznych

Gonera M., Wach A. K.

Prace Przemysłowego Instytutu Elektroniki

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2004

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nr 150

51--65

PL

Omówiono zagadnienie wpływu elektroniki na środowisko naturalne człowieka. Wymieniono zagrożenia dla ekosystemu ze strony zużytego sprzętu elektronicznego. Przedstawiono procesowy model obiegu surowców i produktów elektronicznych. Scharakteryzowano metody proekologicznego projektowania wyrobów elektronicznych. Dokonano przeglądu stosownych metod proekologicznego projektowania takich, jak: metoda kompleksowa, weryfikacji listy, wskaźnika proekologicznego i intuicyjna. Omówiono również stan narzędzi wspomagających proces proekologicznego projektowania wyrobu elektronicznego.

EN

Present situation in used electronic equipment treatment is described. Main threats to environment and human being caused by hazardous substances arising from landfilling or incineration of electronic wastes are specified. Process-based model of row materials and electronic products circulation in environment is discussed. Methods of electronic systems design-for-environment are characterized. A survey of methods such as complex method, checklist verification method, ecological indicator and intuitive method is performed. The state of art. of computer aided design tools aiding the process of electronic systems design for environment is discussed.