FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2118615531> ?p ?o ?g. }

• W2118615531 endingPage "843" @default.
• W2118615531 startingPage "843" @default.
• W2118615531 abstract "Research Article| April 01, 1971 Endolithic Algae and Micrite Envelope Formation in Bahamian Oölites as Revealed by Scanning Electron Microscopy STANLEY MARGOLIS; STANLEY MARGOLIS Department of Geological Sciences, University of California, Riverside, California 92502 PRESENT ADDRESS: (MARGOLIS) DEPARTMENT OF GEOLOGICAL SCIENCES, UNIVERSITY OF CALIFORNIA, SANTA BARBARA, CALIFORNIA 93106 Search for other works by this author on: GSW Google Scholar ROBERT W REX ROBERT W REX Department of Geological Sciences, University of California, Riverside, California 92502 Search for other works by this author on: GSW Google Scholar GSA Bulletin (1971) 82 (4): 843–852. https://doi.org/10.1130/0016-7606(1971)82[843:EAAMEF]2.0.CO;2 Article history received: 02 Jul 1970 rev-recd: 17 Dec 1970 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation STANLEY MARGOLIS, ROBERT W REX; Endolithic Algae and Micrite Envelope Formation in Bahamian Oölites as Revealed by Scanning Electron Microscopy. GSA Bulletin 1971;; 82 (4): 843–852. doi: https://doi.org/10.1130/0016-7606(1971)82[843:EAAMEF]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Examination of Holocene Bahamian oölites by scanning electron and light microscopy has revealed the morphology and orientation of aragonite crystals in the lamellar oölitic envelope, and their modification by the boring activities of endolithic algae. The voids produced by these algae are found in progressive stages of being lined and filled with precipitated microcrystalline aragonite, which is similar to the process of micrite envelope formation in molluscan and other skeletal carbonate grains, as described by Illing (1954) and Bathurst (1966).Areas in the outer portion of the oöliths that contain algal borings filled in with micrite are shown to represent the crypto-crystalline unoriented lamellae described by Newell and others (1960). The oriented prismatic layers in Bahamian oölites, on the other hand, contain minute aragonite crystals with their c-axes oriented roughly parallel to the layers, as suggested by Newell and others (1960) and Cloud (1962).Similar scanning electron microscope techniques when applied to the study of Holocene and ancient carbonate sediments will clarify our understanding of the micritization process. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2118615531 created "2016-06-24" @default.
• W2118615531 creator A5083155989 @default.
• W2118615531 creator A5090299969 @default.
• W2118615531 date "1971-01-01" @default.
• W2118615531 modified "2023-09-27" @default.
• W2118615531 title "Endolithic Algae and Micrite Envelope Formation in Bahamian Oölites as Revealed by Scanning Electron Microscopy" @default.
• W2118615531 doi "https://doi.org/10.1130/0016-7606(1971)82[843:eaamef]2.0.co;2" @default.
• W2118615531 hasPublicationYear "1971" @default.
• W2118615531 type Work @default.
• W2118615531 sameAs 2118615531 @default.
• W2118615531 citedByCount "51" @default.
• W2118615531 countsByYear W21186155312016 @default.
• W2118615531 countsByYear W21186155312017 @default.
• W2118615531 countsByYear W21186155312018 @default.
• W2118615531 countsByYear W21186155312019 @default.
• W2118615531 countsByYear W21186155312020 @default.
• W2118615531 countsByYear W21186155312021 @default.
• W2118615531 countsByYear W21186155312022 @default.
• W2118615531 crossrefType "journal-article" @default.
• W2118615531 hasAuthorship W2118615531A5083155989 @default.
• W2118615531 hasAuthorship W2118615531A5090299969 @default.
• W2118615531 hasConcept C109007969 @default.
• W2118615531 hasConcept C127313418 @default.
• W2118615531 hasConcept C146588470 @default.
• W2118615531 hasConcept C151730666 @default.
• W2118615531 hasConcept C161191863 @default.
• W2118615531 hasConcept C2778805511 @default.
• W2118615531 hasConcept C2780897241 @default.
• W2118615531 hasConcept C41008148 @default.
• W2118615531 hasConceptScore W2118615531C109007969 @default.
• W2118615531 hasConceptScore W2118615531C127313418 @default.
• W2118615531 hasConceptScore W2118615531C146588470 @default.
• W2118615531 hasConceptScore W2118615531C151730666 @default.
• W2118615531 hasConceptScore W2118615531C161191863 @default.
• W2118615531 hasConceptScore W2118615531C2778805511 @default.
• W2118615531 hasConceptScore W2118615531C2780897241 @default.
• W2118615531 hasConceptScore W2118615531C41008148 @default.
• W2118615531 hasIssue "4" @default.
• W2118615531 hasLocation W21186155311 @default.
• W2118615531 hasOpenAccess W2118615531 @default.
• W2118615531 hasPrimaryLocation W21186155311 @default.
• W2118615531 hasRelatedWork W1988881455 @default.
• W2118615531 hasRelatedWork W2029100274 @default.
• W2118615531 hasRelatedWork W2171050805 @default.
• W2118615531 hasRelatedWork W2228586389 @default.
• W2118615531 hasRelatedWork W2256467025 @default.
• W2118615531 hasRelatedWork W2359278653 @default.
• W2118615531 hasRelatedWork W2379719939 @default.
• W2118615531 hasRelatedWork W3087850233 @default.
• W2118615531 hasRelatedWork W4231226515 @default.
• W2118615531 hasRelatedWork W2074932146 @default.
• W2118615531 hasVolume "82" @default.
• W2118615531 isParatext "false" @default.
• W2118615531 isRetracted "false" @default.
• W2118615531 magId "2118615531" @default.
• W2118615531 workType "article" @default.