Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- 1 Major global change: framework for the modern world
- 2 Carboniferous-to-Triassic evolution of the Panthalassan margin in southern South America
- 3 Permian and Triassic geologic events in Sonora, northwestern Mexico
- 4 Advances in the correlation of the Permian
- 5 Examples of late Hercynian transtensional tectonics in the Southern Alps (Italy)
- 6 Succession of selected bioevents in the continental Permian of the Southern Alps (Italy): improvements in intrabasinal and interregional correlations
- 7 Permian chronostratigraphic subdivisions and events in China
- 8 Indosinian Tectogeny in the geological correlation of Vietnam and adjacent regions
- 9 Sitsa flora from the Permian of South Primorye
- 10 Late Permian bimodal volcanism in South Primorye
- 11 Syngenetic and epigenetic mineral deposits in Permian and Triassic sequences of the Primorye region
- 12 The mid-Permian: major changes in geology, environment, and faunas and some evolutionary implications
- 13 Variations in the disappearance patterns of rugosan corals in Tethys and their implications for environments at the end of the Permian
- 14 Fluctuations in pelagic environments near the Permian–Triassic boundary in the Mino-Tamba Terrane, southwest Japan
- 15 Late Changxingian ammonoids, bivalves, and brachiopods in South Primorye
- 16 Radiolaria from Permian–Triassic boundary beds in cherty deposits of Primorye (Sikhote-Alin)
- 17 Early Mesozoic magmatism in the Russian Far East
- 18 Transgressive conodont faunas of the early Triassic: an opportunity for correlation in the Tethys and the circum-Pacific
- 19 Triassic biostratigraphy and palaeobiogeography of East Asia
- 20 Classification and correlation of Triassic limestones in Sikhote-Alin on the basis of corals
- 21 Evolution of the platform elements of the conodont genus Metapolygnathus and their distribution in the Upper Triassic of Sikhote-Alin
- 22 Late Triassic North American halobiid bivalves: diversity trends and circum-Pacific correlations
- 23 Upper Triassic Chinle Group, Western United States: a nonmarine standard for late Triassic time
- 24 Otapirian Stage: its fauna and microflora
- 25 Upper Palaeozoic glaciation and Carboniferous and Permian faunal changes in Argentina
- Index
9 - Sitsa flora from the Permian of South Primorye
Published online by Cambridge University Press: 13 October 2009
- Frontmatter
- Contents
- List of contributors
- Preface
- 1 Major global change: framework for the modern world
- 2 Carboniferous-to-Triassic evolution of the Panthalassan margin in southern South America
- 3 Permian and Triassic geologic events in Sonora, northwestern Mexico
- 4 Advances in the correlation of the Permian
- 5 Examples of late Hercynian transtensional tectonics in the Southern Alps (Italy)
- 6 Succession of selected bioevents in the continental Permian of the Southern Alps (Italy): improvements in intrabasinal and interregional correlations
- 7 Permian chronostratigraphic subdivisions and events in China
- 8 Indosinian Tectogeny in the geological correlation of Vietnam and adjacent regions
- 9 Sitsa flora from the Permian of South Primorye
- 10 Late Permian bimodal volcanism in South Primorye
- 11 Syngenetic and epigenetic mineral deposits in Permian and Triassic sequences of the Primorye region
- 12 The mid-Permian: major changes in geology, environment, and faunas and some evolutionary implications
- 13 Variations in the disappearance patterns of rugosan corals in Tethys and their implications for environments at the end of the Permian
- 14 Fluctuations in pelagic environments near the Permian–Triassic boundary in the Mino-Tamba Terrane, southwest Japan
- 15 Late Changxingian ammonoids, bivalves, and brachiopods in South Primorye
- 16 Radiolaria from Permian–Triassic boundary beds in cherty deposits of Primorye (Sikhote-Alin)
- 17 Early Mesozoic magmatism in the Russian Far East
- 18 Transgressive conodont faunas of the early Triassic: an opportunity for correlation in the Tethys and the circum-Pacific
- 19 Triassic biostratigraphy and palaeobiogeography of East Asia
- 20 Classification and correlation of Triassic limestones in Sikhote-Alin on the basis of corals
- 21 Evolution of the platform elements of the conodont genus Metapolygnathus and their distribution in the Upper Triassic of Sikhote-Alin
- 22 Late Triassic North American halobiid bivalves: diversity trends and circum-Pacific correlations
- 23 Upper Triassic Chinle Group, Western United States: a nonmarine standard for late Triassic time
- 24 Otapirian Stage: its fauna and microflora
- 25 Upper Palaeozoic glaciation and Carboniferous and Permian faunal changes in Argentina
- Index
Summary
The Sitsa flora was first described by M. D. Zalessky in 1929. He investigated the collection sampled by M. A. Pavlov, I. A. Klock, and A. V. Martynov from the Malaya Sitsa River basin in the Partizansk region. Of the forms he described, only Pecopteris anthriscifolia Goeppert had been known earlier. The other species (Pecopteris maritime Zalessky, Callipteris sahnii Zalessky, C. orientalis Zalessky, C. congermana Zalessky, Thinnfeldia pavlovi Zalessky, Odontopteris ussuriensis Zalessky, Scapanophyllum sitzense Zalessky, Ctenis renaulti Zalessky) were described as being new species. There were also some species (Annularia schurowskii Schmalhausen, Phyllotheca cf. deliquescens Eichwald, and Noeggerathiopsis aegualis Goeppert) that were reported only in text. Those data suggested a late Permian age for the Sitsa flora. At the same time, Zalessky found some forms in his collection “that foretold the beginning of Mesozoic time” (Zalessky, 1929a, p. 124).
Later, Zalessky (1929b, 1930) described four other species (Synopteris demetriana Zalessky, Sitzia kloki Zalessky, Sitzopteris superba Zalessky, and Rhipidopsis elegans Zalessky). He concluded that the presence of Pecopteris anthriscifolia Goeppert in the Sitsa flora made it comparable with the late Permian floras of Pechora (Pechora Formation) and Kuznetsk (Kolchuginskian Formation).
When late Permian plant fossils were found in other localities of South Primorye, the question arose as to the position of the Sitsa Suite in the Upper Permian section of the region (the type of the suite is located in the type region of the Sitsa flora).
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- Late Palaeozoic and Early Mesozoic Circum-Pacific Events and their Global Correlation , pp. 97 - 105Publisher: Cambridge University PressPrint publication year: 1997