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Państwowej Szkoły Wyższej w Białej Podlaskiej

Baza tworzona przez Bibliotekę Akademii Bialskiej im. Jana Pawła II.



Zapytanie: PALINOLOGIA
Liczba odnalezionych rekordów: 2



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Nr opisu: rtress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.^aZbucki, Łukasz^cy^atwierdza krzyżacka^aTeutonic fortress^amalakologia^amalacology^apalinologia^apalynology
Autorzy: .
Tytuł pracy w innym języku: 0001-5709003Changes for sedimentation in the Drużno Lake based on geoarchaeological data from the Teutonic fortress in Elbląg, North PolandActa Geologica Polonica20160001-57092015/201610.1515/agp-2016-0004Nitychoruk, Jerzyosady jeziorneLacustrine sedimentsIF za rok Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.FINAL_PUBLISHEDThe wooden structures unearthed in 2012 during archaeological excavation in the courtyard of the Museum of Archaeology and History in Elbląg have been dated using the dendrochronological method to the period between 1245 and 1302, which allows them to be considered to be parts of a Teutonic fortress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.Zbucki, Łukasztwierdza krzyżackaTeutonic fortressmalakologiamalacologypalinologiapalynology : A : 001 : Vol. 66 : OTHER
Szczegóły:
Tytuł monografii w innym języku: 0001-5709003Changes for sedimentation in the Drużno Lake based on geoarchaeological data from the Teutonic fortress in Elbląg, North PolandActa Geologica Polonica20160001-57092015/201610.1515/agp-2016-0004Nitychoruk, Jerzyosady jeziorneLacustrine sedimentsIF za rok Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.FINAL_PUBLISHEDThe wooden structures unearthed in 2012 during archaeological excavation in the courtyard of the Museum of Archaeology and History in Elbląg have been dated using the dendrochronological method to the period between 1245 and 1302, which allows them to be considered to be parts of a Teutonic fortress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.Zbucki, Łukasztwierdza krzyżackaTeutonic fortressmalakologiamalacologypalinologiapalynology : A : 001 : Vol. 66 : OTHER
Charakterystyka formalna:
Punktacja ministerstwa: ew/25291/17234PRACA RECENZOWANA100^a0001-5709^bA^fA^gABC^hABC^iX^jXY^a003^b001^c2016-02-02, 12:57^d2017-06-19, 09:30^e3829028982^f3724859309^aChanges for sedimentation in the Drużno Lake based on geoarchaeological data from the Teutonic fortress in Elbląg, North Poland^aActa Geologica Polonica^a2016^bVol. 66^cno. 1^dp. 85--98^a0001-5709^a2015/2016^a10.1515/agp-2016-0004^aNitychoruk, Jerzy^cy^aosady jeziorne^aLacustrine sediments^aIF za rok Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.^aFINAL_PUBLISHED^bOTHER^cAT_PUBLICATION^eOPEN_JOURNAL^aThe wooden structures unearthed in 2012 during archaeological excavation in the courtyard of the Museum of Archaeology and History in Elbląg have been dated using the dendrochronological method to the period between 1245 and 1302, which allows them to be considered to be parts of a Teutonic fortress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.^aZbucki, Łukasz^cy^atwierdza krzyżacka^aTeutonic fortress^amalakologia^amalacology^apalinologia^apalynology
Praca recenzowana
Słowa kluczowe ang.: DANAENGhttps://geojournals.pgi.gov.pl/agp/article/view/25291/17234PRACA RECENZOWANA100^a0001-5709^bA^fA^gABC^hABC^iX^jXY^a003^b001^c2016-02-02, 12:57^d2017-06-19, 09:30^e3829028982^f3724859309^aChanges for sedimentation in the Drużno Lake based on geoarchaeological data from the Teutonic fortress in Elbląg, North Poland^aActa Geologica Polonica^a2016^bVol. 66^cno. 1^dp. 85--98^a0001-5709^a2015/2016^a10.1515/agp-2016-0004^aNitychoruk, Jerzy^cy^aosady jeziorne^aLacustrine sediments^aIF za rok Kopia dostępna w Dziale Gromadzenia, Opracowania i Kontroli Zbiorów Biblioteki PSW.^aFINAL_PUBLISHED^bOTHER^cAT_PUBLICATION^eOPEN_JOURNAL^aThe wooden structures unearthed in 2012 during archaeological excavation in the courtyard of the Museum of Archaeology and History in Elbląg have been dated using the dendrochronological method to the period between 1245 and 1302, which allows them to be considered to be parts of a Teutonic fortress. The remains of the wooden building located directly on the prehistoric lacustrine sediments created a unique opportunity to reconstruct the near-shore sedimentation of the Drużno Lake. Geological, malacological and palynological methods were applied during the investigation. The results, compared with the ranges of both the Drużno Lake and the Vistula Lagoon, known from previous studies of the region, allowed the correlation of a phase of a deep lake with the "Roman Period". Rapid shallowing of the lake occured in the "Migration Period". The final disappearance of the lake in the area of modern Elbląg occured in the early Middle Ages.^aZbucki, Łukasz^cy^atwierdza krzyżacka^aTeutonic fortress^amalakologia^amalacology^apalinologia^apalynology
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Słowa kluczowe ang.: ;
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Nr opisu: n total, over 70 sporomorph taxa and over 25 dinoflagellate cyst taxa have been identified in four samples collected from the filling of the palaeokarstic forms in the cave. The results of the analysis of sporomorphs and dinoflagellate cysts point to the formation of the palaeokarst during the sedimentation break that took place at the end of the late Badenian evaporitic cycle in the Western Ukraine region. The subsequent marine transgression led to the filling of the karst forms in gypsum with chemogenic carbonate material, precipitated from marine water (draperies) and with fine-grained, clastic material (pockets and fissures).^apalinologia^apalynology^asporomorfy^asporomorphs^abruzdnice^adinoflagellate cysts^ajaskinia^acaves^aZachodnia Ukraina^aWestern Ukraine^aPlatforma Wschodnioeuropejska^aEastern European Platform^abaden^aBadenian
Autorzy: , .
Tytuł czasopisma:
Tytuł wynalazku: The Zoloushka Cave belongs to a group of the largest gypsum caves in Western Ukraine (Bukovina region), developed in the middle Miocene (upper Badenian) evaporite series (Tyras Formation) on the SW periphery of the East European Platform. It is developed in the lower part of the evaporite series composed of gypsum, which is covered by a carbonate layer (Ratyn Limestone). The uneven upper surface of the gypsum at the contact with the limestone, the frequent occurrence of palaeokarst forms, and the presence of karstified fissures filled with allochthonous material indicate a sedimentation break between the gypsum and the overlying limestone. To support this thesis and to add new data on the age and palaeoenvironmental conditions of palaeokarst formation in the Bukovina region, palynological studies were carried out on material from the Zoloushka Cave. Palynofacies, sporomorphs and dinoflagellate cysts were studied. In total, over 70 sporomorph taxa and over 25 dinoflagellate cyst taxa have been identified in four samples collected from the filling of the palaeokarstic forms in the cave. The resu, OTHER
Charakterystyka wg MNiSW:
Słowa kluczowe ang.: e largest gypsum caves in Western Ukraine (Bukovina region), developed in the middle Miocene (upper Badenian) evaporite series (Tyras Formation) on the SW periphery of the East European Platform. It is developed in the lower part of the evaporite series composed of gypsum, which is covered by a carbonate layer (Ratyn Limestone). The uneven upper surface of the gypsum at the contact with the limestone, the frequent occurrence of palaeokarst forms, and the presence of karstified fissures filled with allochthonous material indicate a sedimentation break between the gypsum and the overlying limestone. To support this thesis and to add new data on the age and palaeoenvironmental conditions of palaeokarst formation in the Bukovina region, palynological studies were carried out on material from the Zoloushka Cave. Palynofacies, sporomorphs and dinoflagellate cysts were studied. In total, over 70 sporomorph taxa and over 25 dinoflagellate cyst taxa have been identified in four samples collected from the filling of the palaeokarstic forms in the cave. The results of the analysis of sporomorphs and dinoflagellate cysts point to the formation of the palaeokarst during the sedimentation break that took place at the end of the late Badenian evaporitic cycle in the Western Ukraine region. The subsequent marine transgression led to the filling of the karst forms in gypsum with chemogenic carbonate material, precipitated from marine water (draperies) and with fine-grained, clastic material (pockets and fissures).^apalinologia^apalynology^asporomorfy^asporomorphs^abruzdnice^adinoflagellate cysts^ajaskinia^acaves^aZachodnia Ukraina^aWestern Ukraine^aPlatforma Wschodnioeuropejska^aEastern European Platform^abaden^aBadenian
Słowa kluczowe: ;
Słowa kluczowe ang.: ; ;
Inne bazy podające opis:
  • n total, over 70 sporomorph taxa and over 25 dinoflagellate cyst taxa have been identified in four samples collected from the filling of the palaeokarstic forms in the cave. The results of the analysis of sporomorphs and dinoflagellate cysts point to the formation of the palaeokarst during the sedimentation break that took place at the end of the late Badenian evaporitic cycle in the Western Ukraine region. The subsequent marine transgression led to the filling of the karst forms in gypsum with chemogenic carbonate material, precipitated from marine water (draperies) and with fine-grained, clastic material (pockets and fissures).^apalinologia^apalynology^asporomorfy^asporomorphs^abruzdnice^adinoflagellate cysts^ajaskinia^acaves^aZachodnia Ukraina^aWestern Ukraine^aPlatforma Wschodnioeuropejska^aEastern European Platform^abaden^aBadenian


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