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The paper presents the new localities of 29 rare and interesting species of vascular plants from western part of the Pogórze Wielickie hills (Polish Carpathians).
EN
Mount Flora at Hope Bay, in northernmost part of Antarctic Peninsula, is a famous Jurassic flora locality. It has already been studied for a hundred years, but however, it is still possible to find there new taxa. Based on two species of liverworts found at Mount Flora (Schizolepidella gracilis and Schizolepidella birkenmajeri sp. nov.), the present study discusses affiliation of the genus Schizolepidella to liverworts. The new species Schizolepidella birkenmajeri is erected.
EN
The fossil flora from Hope Bay, West Antarctica, is ranking among the richest Jurassic floras of the world. So far, it was known mostly from loose blocks scattered at coastal plain below Mount Flora. The present collections from the Mount Flora Formation, include the fossil plants assembled mainly in situ (from the Flora Glacier Member), but also those obtained from loose blocks (derived from the Five Lakes Valley Member and the Flora Glacier Member). 41 plant taxons were identified: 2 from Hepatophyta, 2 from Sphenophyta, 9 from Pteridophyta, 5 from Pteridophylla, 6 from Pteridospermophyta, 9 from Cycadophyta and 8 from Coniferophyta. The taxons new for Antarctica include the species Coniopteris cf. simplex (Lindley & Hutton) Harris, Equisetum cf. columnare Brongniart emend. Harris, Otozamites gramin eus (Phillips) Harris, and the genera Conites Sternberg emend. Cleal et Rees and Stachyotaxus Na thorst. New taxa include: Crosso zamiamirabilis sp. nov. Ociepa and Pagiophyllum arctowskii sp. nov. Ociepa (Schizole pidella birkenmajeri sp. nov. Ociepa, 2007, has been described separately). A new combination Araucarites antarcticus (Gee) comb. nov. Ociepa is presented. The described flora confirms its Jurassic age. The paper presents also remarks on palaeoclimate and environment of the Antarctic Peninsula volcanic arc during the Jurassic.
EN
Studzianna well core (Triassic-Jurassic) from the Holy Cross Mts region were investigated. Fossil plants from the genus Neocalamites (Equisetales) were found mainly in the Triassic sediments. Fragments of Ginkgoales and Czekanowskiales and Coniferales were determined mainly from the Lower Jurassic. The Lower Jurassic microflora consists of sporomorphs from Bryophyta, Equisetales, Lycopodiales, Filicales from the family Cyatheaceae or Dicsoniaceae, Pteridospermophyta from Caytoniales, Ginkgoales or Cycadales or Bennettitales, Coniferales from the families Taxodiaceae, Pinaceae and Cheirolepidiaceae. Palynofacies have mainly terrestrial character and confirms earlier opinion (Karaszewski 1962, Pieńkowski 2004) of the prevailed terrestrial origin of the Lower Jurassic (Hettangian-Sinemurian) sediments from the Holy Cross Mts region.
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