Matches in SemOpenAlex for { <https://semopenalex.org/work/W2085852792> ?p ?o ?g. }
Showing items 1 to 85 of
85
with 100 items per page.
- W2085852792 endingPage "277" @default.
- W2085852792 startingPage "259" @default.
- W2085852792 abstract "The tenth chapter is dealt with the history of research in older rocks and Cambro-Ordovician of eastern North America. In last century Pre-Cambrian stratigraphy was started in Canada, while the New York System was instituted around Albany, N. Y. and later it was correlated to the European sequence. Subsequently the Cambrian and Ordovician Systems were classified in detail. Starting with the ventral anatomy of trilobites Walcott made invaluable contributions on the Cambrian geology and palaeontology, i.e. the Olenellus fauna, unique fauna the Burgess shale and so forth. His “Cambrian Fauna of China” 1913 provided a firm basis for the Cambrian of Eastern Asia.The relation of the Cambro-Ordovician faunas of the continent to the European ones in the northern part of the Appalachian geosyncline and their distribution in the Appalachian mountains and further westerly beyond the lower Mississipy river and also in the interior lowland are briefly outlined.These systems in the Cordilleran geosyncline is described in the eleventh chapeter. Stratigraphy in the western sites is followed by notes on the Alaskan faunas in the north which were allied to the Siberian ones at the beginning, but later to the Eastern Asiatic ones also. In the south it is a remarkable fact that the Mexicoan faunas are more related to the Andean ones than those of the United States, particularly in the early Ordovician age.The Circum-Pacific Cambro-Ordovician belt is taken up in the final chapter. The history of this belt's history started in the Sinian period. In the early Cambrian age the eastern side belonged to the Olenellian province, but the other side constitued the Redlichia province. Subsequently, however, trilobites of the two sides became closer related to each other, although the early Upper Cambrian Kushan fauna was quite isolated. Trilobites were intimate between the two sides of the Northern Pacific and also on the southern Pacific side in the early Ordovician age. The aspect of the provinciality in the middle and late Ordovician ages is still obscure, sofar as trilobites are concerned." @default.
- W2085852792 created "2016-06-24" @default.
- W2085852792 creator A5024956751 @default.
- W2085852792 date "1987-01-01" @default.
- W2085852792 modified "2023-09-25" @default.
- W2085852792 title "The Cambrian and Ordovician Systems around the Pacific Basin, Part III" @default.
- W2085852792 cites W1711722542 @default.
- W2085852792 cites W1761292909 @default.
- W2085852792 cites W1828887908 @default.
- W2085852792 cites W1876563556 @default.
- W2085852792 cites W1888938260 @default.
- W2085852792 cites W1968538831 @default.
- W2085852792 cites W1986160716 @default.
- W2085852792 cites W2028906563 @default.
- W2085852792 cites W2065602538 @default.
- W2085852792 cites W2091882415 @default.
- W2085852792 cites W2094345991 @default.
- W2085852792 cites W2133155210 @default.
- W2085852792 cites W2137537192 @default.
- W2085852792 cites W2141861121 @default.
- W2085852792 cites W2164826218 @default.
- W2085852792 cites W2187253413 @default.
- W2085852792 cites W2282887450 @default.
- W2085852792 cites W2312411036 @default.
- W2085852792 cites W2312604932 @default.
- W2085852792 cites W2312677373 @default.
- W2085852792 cites W2319389736 @default.
- W2085852792 cites W2322132415 @default.
- W2085852792 cites W2322133520 @default.
- W2085852792 cites W2333760201 @default.
- W2085852792 cites W2334335441 @default.
- W2085852792 cites W2346699708 @default.
- W2085852792 cites W2413383410 @default.
- W2085852792 cites W2423083702 @default.
- W2085852792 cites W2497088758 @default.
- W2085852792 cites W2520788588 @default.
- W2085852792 cites W2530381467 @default.
- W2085852792 cites W2595981944 @default.
- W2085852792 cites W2604056337 @default.
- W2085852792 cites W2604201379 @default.
- W2085852792 cites W2611658870 @default.
- W2085852792 cites W2615625417 @default.
- W2085852792 cites W2615789430 @default.
- W2085852792 cites W2649128093 @default.
- W2085852792 cites W2909969484 @default.
- W2085852792 cites W3102036290 @default.
- W2085852792 cites W356932344 @default.
- W2085852792 cites W580577318 @default.
- W2085852792 doi "https://doi.org/10.5026/jgeography.96.5_259" @default.
- W2085852792 hasPublicationYear "1987" @default.
- W2085852792 type Work @default.
- W2085852792 sameAs 2085852792 @default.
- W2085852792 citedByCount "0" @default.
- W2085852792 crossrefType "journal-article" @default.
- W2085852792 hasAuthorship W2085852792A5024956751 @default.
- W2085852792 hasBestOaLocation W20858527921 @default.
- W2085852792 hasConcept C109007969 @default.
- W2085852792 hasConcept C127313418 @default.
- W2085852792 hasConcept C151730666 @default.
- W2085852792 hasConcept C91442348 @default.
- W2085852792 hasConceptScore W2085852792C109007969 @default.
- W2085852792 hasConceptScore W2085852792C127313418 @default.
- W2085852792 hasConceptScore W2085852792C151730666 @default.
- W2085852792 hasConceptScore W2085852792C91442348 @default.
- W2085852792 hasIssue "5" @default.
- W2085852792 hasLocation W20858527921 @default.
- W2085852792 hasOpenAccess W2085852792 @default.
- W2085852792 hasPrimaryLocation W20858527921 @default.
- W2085852792 hasRelatedWork W1964331141 @default.
- W2085852792 hasRelatedWork W1975774331 @default.
- W2085852792 hasRelatedWork W2003163387 @default.
- W2085852792 hasRelatedWork W2017333044 @default.
- W2085852792 hasRelatedWork W2104696163 @default.
- W2085852792 hasRelatedWork W2122110802 @default.
- W2085852792 hasRelatedWork W2149149528 @default.
- W2085852792 hasRelatedWork W2273013737 @default.
- W2085852792 hasRelatedWork W2337712059 @default.
- W2085852792 hasRelatedWork W4243318934 @default.
- W2085852792 hasVolume "96" @default.
- W2085852792 isParatext "false" @default.
- W2085852792 isRetracted "false" @default.
- W2085852792 magId "2085852792" @default.
- W2085852792 workType "article" @default.