{"title":"古生代棘皮动物和孤珊瑚不灵活的 \"根 \"的功能","authors":"Stephen K. Donovan","doi":"10.1111/gto.12456","DOIUrl":null,"url":null,"abstract":"<p>Although not a common feature of either group, solitary rugose corals and Palaeozoic crinoids may be anchored by unsegmented, rod-like root structures, referred to as ‘radiciform’ processes and ‘pseudoradices’, respectively. Crinoid pseudoradices likely penetrated the sediment radially from the column, like the roots of a tree. Radiciform processes may have fulfilled a similar function for a solitary rugose coral, but they were also encrusters.</p>","PeriodicalId":100581,"journal":{"name":"Geology Today","volume":"39 6","pages":"236-239"},"PeriodicalIF":0.0000,"publicationDate":"2023-12-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Function of inflexible ‘roots’ of Palaeozoic crinoids and solitary corals\",\"authors\":\"Stephen K. Donovan\",\"doi\":\"10.1111/gto.12456\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Although not a common feature of either group, solitary rugose corals and Palaeozoic crinoids may be anchored by unsegmented, rod-like root structures, referred to as ‘radiciform’ processes and ‘pseudoradices’, respectively. Crinoid pseudoradices likely penetrated the sediment radially from the column, like the roots of a tree. Radiciform processes may have fulfilled a similar function for a solitary rugose coral, but they were also encrusters.</p>\",\"PeriodicalId\":100581,\"journal\":{\"name\":\"Geology Today\",\"volume\":\"39 6\",\"pages\":\"236-239\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2023-12-25\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geology Today\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1111/gto.12456\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geology Today","FirstCategoryId":"1085","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/gto.12456","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Function of inflexible ‘roots’ of Palaeozoic crinoids and solitary corals
Although not a common feature of either group, solitary rugose corals and Palaeozoic crinoids may be anchored by unsegmented, rod-like root structures, referred to as ‘radiciform’ processes and ‘pseudoradices’, respectively. Crinoid pseudoradices likely penetrated the sediment radially from the column, like the roots of a tree. Radiciform processes may have fulfilled a similar function for a solitary rugose coral, but they were also encrusters.