FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2326856085> ?p ?o ?g. }

• W2326856085 abstract "I. Outline of historical reviewsThe Paleozoic bryozoan researches in Asia were introduced after the 20th century except for the reported from the Salt Range bryozoan fauna which was described by WAAGEN and PICHL (1885), and WAAGEN and WENTZEL (1886). In East Asia, although there are some pioneered works on the Paleozoic bryozoans by MANSUY (1912, 1913), YABE and HAYASAKA (1920), NEWTON (1926), REED (1927), YOH (1932), OZAKI (1933), YABE and SUGIYAMA (1942) and so on, they were not systematic studies of Bryozoa.The Paleozoic bryozoan studies in East Asia were earnestly made since 1950, namely, in China by YANG, Loo, Hu, HSIA, LIU, LI ; in Altai and Siberia of USSR. by NEKHOROSHEV, TRIZNA, ASTROVA, MODZALEVSKAYA, ROMANTCHUK and MOROZOVA ; in Japan and Southeast Asia by SAKAGAMI and SUGIMURA.II. Study of Paleozoic bryozoans in JapanGenerally the Silurian-Devonian bryozoans in Japan are ill-preserved and rare, and only one species of the Silurian bryozoan : Monotrypella? yabei has been hitherto described by SUGIYAMA (1944) from the middle Silurian of Japan. Recently, some materials, however, were collected from the Kitakami and Hida massifs. They are Stereotoechus Kitakamiensis (n. sp., MS) and some fenestellids from the middle Devonian of the Kitakami massif, and Eridotrypella? sp. (probably n. sp., MS), Fenestella sp. indet. and Sulcoretepora sp. indet. from the Devonian of the Hida massif. They will be described paleontologically in the near future. The Carboniferous-Permian bryozoans in Japan have been summarized by SAKAGAMI (1967b, 1970a). Later, SUGIMURA and OTA (1971), SUGIMURA (1972, 1974), and SAKAGAMI and SUGIMURA (1978) studied some Upper Paleozoic bryozoans from the Akiyoshi limestone.III. Study of Paleozoic bryozoans in ChinaRecently, its Paleozoic bryozoan studies have been greatly progressed by the efforts of YANG, K. C. and his collaborators. At present, 440 species of the Paleozoic bryozoans have been described and illustrated as shown in Table 1.IV. Study of Paleozoic bryozoans in Southeast AsiaThe Silurian and Devonian bryozoans from Indo-China are very poor and insufficient for comparison with those of other areas, however, the “Anthracolithic” bryozoan fauna, in spite of small one, contains the European and/or Salt Range elements. The further studies should be expected.On the other hand, our knowledge of the Paleozoic bryozoan fauna from the Thai-Malayan district has much progressed in this decade by SAKAGAMI (1963-). At present, about 30 species of the Carboniferous and more than 90 species of the Permian bryozoans have been described from 16 localities in the Thai-Malayan district. Generally these bryozoan faunas constitute a unique assemblage but contain both European and Asian elements among its genera.V. Comparison of Paleozoic bryozoan facies between Japan, China and Southeast AsiaTable 2 shows the distributions of the bryozoan genera in East Asia. As shown in Table 3, total numbers of bryozoan genera in each Period are gradually increased to the younger, but it is different from the world-wide tendency.The most world-wide genera in the Paleozoic Group, i. e., Fistulipora, Fenestella and Polypora are known abundantly also in East Asia. They are known from the Ordovician to Permian, but are extremely rare in the Ordovician and Silurian. Thus, there seems to be a large change of the Paleozoic bryozoan facies between the Silurian and Devonian. On the other hand, in East Asia, the common genera between the Devonian and Carboniferous bryozoan faunas are only 8 and a considerable change between them is recognized. There are 20 common genera between the Carboniferous and Permian faunas, and their relationship between two faunas seems to be successive." @default.
• W2326856085 created "2016-06-24" @default.
• W2326856085 creator A5080359350 @default.
• W2326856085 date "1978-01-01" @default.
• W2326856085 modified "2023-10-01" @default.
• W2326856085 title "Study of the Paleozoic Bryozoa in East Asia" @default.
• W2326856085 cites W1512471203 @default.
• W2326856085 cites W1884215913 @default.
• W2326856085 cites W1982626895 @default.
• W2326856085 cites W2012881077 @default.
• W2326856085 cites W2051422508 @default.
• W2326856085 cites W2069058071 @default.
• W2326856085 cites W2351981806 @default.
• W2326856085 cites W2359643950 @default.
• W2326856085 cites W2373567103 @default.
• W2326856085 cites W2381660598 @default.
• W2326856085 cites W2489840949 @default.
• W2326856085 cites W2509023973 @default.
• W2326856085 cites W2509218961 @default.
• W2326856085 cites W2509724320 @default.
• W2326856085 cites W2510087066 @default.
• W2326856085 cites W2517982634 @default.
• W2326856085 cites W2522940702 @default.
• W2326856085 cites W2524962642 @default.
• W2326856085 cites W2525234885 @default.
• W2326856085 cites W2600391287 @default.
• W2326856085 cites W2611939300 @default.
• W2326856085 cites W2618144435 @default.
• W2326856085 cites W2948253255 @default.
• W2326856085 cites W3141575729 @default.
• W2326856085 cites W435312981 @default.
• W2326856085 cites W585549333 @default.
• W2326856085 cites W639675371 @default.
• W2326856085 cites W651186937 @default.
• W2326856085 cites W659012152 @default.
• W2326856085 cites W76968898 @default.
• W2326856085 cites W986144346 @default.
• W2326856085 cites W1926330691 @default.
• W2326856085 cites W2785576551 @default.
• W2326856085 cites W92834464 @default.
• W2326856085 doi "https://doi.org/10.5026/jgeography.87.6_313" @default.
• W2326856085 hasPublicationYear "1978" @default.
• W2326856085 type Work @default.
• W2326856085 sameAs 2326856085 @default.
• W2326856085 citedByCount "0" @default.
• W2326856085 crossrefType "journal-article" @default.
• W2326856085 hasAuthorship W2326856085A5080359350 @default.
• W2326856085 hasBestOaLocation W23268560851 @default.
• W2326856085 hasConcept C107832698 @default.
• W2326856085 hasConcept C109007969 @default.
• W2326856085 hasConcept C125471540 @default.
• W2326856085 hasConcept C127313418 @default.
• W2326856085 hasConcept C13106087 @default.
• W2326856085 hasConcept C149918038 @default.
• W2326856085 hasConcept C151730666 @default.
• W2326856085 hasConcept C160776313 @default.
• W2326856085 hasConcept C181727316 @default.
• W2326856085 hasConcept C18903297 @default.
• W2326856085 hasConcept C2778540584 @default.
• W2326856085 hasConcept C58642233 @default.
• W2326856085 hasConcept C83365034 @default.
• W2326856085 hasConcept C86803240 @default.
• W2326856085 hasConceptScore W2326856085C107832698 @default.
• W2326856085 hasConceptScore W2326856085C109007969 @default.
• W2326856085 hasConceptScore W2326856085C125471540 @default.
• W2326856085 hasConceptScore W2326856085C127313418 @default.
• W2326856085 hasConceptScore W2326856085C13106087 @default.
• W2326856085 hasConceptScore W2326856085C149918038 @default.
• W2326856085 hasConceptScore W2326856085C151730666 @default.
• W2326856085 hasConceptScore W2326856085C160776313 @default.
• W2326856085 hasConceptScore W2326856085C181727316 @default.
• W2326856085 hasConceptScore W2326856085C18903297 @default.
• W2326856085 hasConceptScore W2326856085C2778540584 @default.
• W2326856085 hasConceptScore W2326856085C58642233 @default.
• W2326856085 hasConceptScore W2326856085C83365034 @default.
• W2326856085 hasConceptScore W2326856085C86803240 @default.
• W2326856085 hasLocation W23268560851 @default.
• W2326856085 hasOpenAccess W2326856085 @default.
• W2326856085 hasPrimaryLocation W23268560851 @default.
• W2326856085 hasRelatedWork W118613385 @default.
• W2326856085 hasRelatedWork W1434323696 @default.
• W2326856085 hasRelatedWork W1978408499 @default.
• W2326856085 hasRelatedWork W1993222399 @default.
• W2326856085 hasRelatedWork W2026817432 @default.
• W2326856085 hasRelatedWork W2086816441 @default.
• W2326856085 hasRelatedWork W2086884538 @default.
• W2326856085 hasRelatedWork W2144938997 @default.
• W2326856085 hasRelatedWork W2156029653 @default.
• W2326856085 hasRelatedWork W2173295268 @default.
• W2326856085 hasRelatedWork W2189598482 @default.
• W2326856085 hasRelatedWork W2336654711 @default.
• W2326856085 hasRelatedWork W2362653508 @default.
• W2326856085 hasRelatedWork W2563294239 @default.
• W2326856085 hasRelatedWork W2790263253 @default.
• W2326856085 hasRelatedWork W2909728686 @default.
• W2326856085 hasRelatedWork W2995064429 @default.
• W2326856085 hasRelatedWork W3055295061 @default.
• W2326856085 hasRelatedWork W2110061306 @default.
• W2326856085 hasRelatedWork W2212883427 @default.
• W2326856085 isParatext "false" @default.

• next