FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2152556249> ?p ?o ?g. }

• W2152556249 endingPage "663" @default.
• W2152556249 startingPage "648" @default.
• W2152556249 abstract "Abstract The Lonely Bay Formation, located to the west of Great Slave Lake, Northwest Territories, Canada, is a thick-bedded limestone succession that includes four facies that are characteristic of a Devonian middle-ramp depositional setting. One facies in the Lonely Bay Formation is intensely bioturbated with some burrows filled with calcite and others with dolomite. The calcite-filled burrows are found close to the paleo-shoreline of the Canadian Shield, whereas the dolomite-filled burrows are found in deeper ramp deposits. In the calcite-filled burrows the parent burrows, each surrounded by a diagenetic halo, are readily apparent, whereas the dolomite-filled burrows are largely devoid of original structures. Each burrow type has its own distinctive geochemical suites of rare-earth-elements (REE), trace-elements, and δ18O(PDB) and δ13C(PDB) isotopes. These data indicate that sulfate-reducing bacteria, reducing conditions, and marine organic matter were present in the dolomite-filled burrows. Conversely, geochemical data from the calcite-filled burrows indicate that they remained in suboxic conditions and contained little to no marine organic matter that would have contributed to the formation of early dolomite. For these burrows, continent-derived organic matter may have hindered dolomite formation. The contrast between the two types of burrows clearly shows how the different diagenetic environments influenced the evolution of the carbonate. This study, based on interpretations of various geochemical signatures, highlights the roles that oxygen concentrations and types of organic matter (continental versus marine derived) played in dolomite precipitation." @default.
• W2152556249 created "2016-06-24" @default.
• W2152556249 creator A5055360910 @default.
• W2152556249 creator A5075383401 @default.
• W2152556249 date "2012-10-09" @default.
• W2152556249 modified "2023-10-01" @default.
• W2152556249 title "Petrographic and Geochemical Contrasts Between Calcite- and Dolomite-Filled Burrows In the Middle Devonian Lonely Bay Formation, Northwest Territories, Canada: Implications for Dolomite Formation In Paleozoic Burrows" @default.
• W2152556249 cites W1519145565 @default.
• W2152556249 cites W1525438857 @default.
• W2152556249 cites W1571712783 @default.
• W2152556249 cites W1581560578 @default.
• W2152556249 cites W161518108 @default.
• W2152556249 cites W1981189009 @default.
• W2152556249 cites W1983143813 @default.
• W2152556249 cites W1993898064 @default.
• W2152556249 cites W1995737122 @default.
• W2152556249 cites W1999998990 @default.
• W2152556249 cites W2006124337 @default.
• W2152556249 cites W2008281306 @default.
• W2152556249 cites W2021862772 @default.
• W2152556249 cites W2048523234 @default.
• W2152556249 cites W2050128151 @default.
• W2152556249 cites W2054524404 @default.
• W2152556249 cites W2055324639 @default.
• W2152556249 cites W2060085051 @default.
• W2152556249 cites W2060971146 @default.
• W2152556249 cites W2068527782 @default.
• W2152556249 cites W2077568485 @default.
• W2152556249 cites W2081009732 @default.
• W2152556249 cites W2084208746 @default.
• W2152556249 cites W2085221298 @default.
• W2152556249 cites W2091794361 @default.
• W2152556249 cites W2097386376 @default.
• W2152556249 cites W2110850782 @default.
• W2152556249 cites W2139512662 @default.
• W2152556249 cites W2156215403 @default.
• W2152556249 cites W2166395264 @default.
• W2152556249 cites W2168301466 @default.
• W2152556249 cites W2235226982 @default.
• W2152556249 cites W2909542910 @default.
• W2152556249 cites W2909987637 @default.
• W2152556249 cites W2911204174 @default.
• W2152556249 doi "https://doi.org/10.2110/jsr.2012.57" @default.
• W2152556249 hasPublicationYear "2012" @default.
• W2152556249 type Work @default.
• W2152556249 sameAs 2152556249 @default.
• W2152556249 citedByCount "29" @default.
• W2152556249 countsByYear W21525562492012 @default.
• W2152556249 countsByYear W21525562492013 @default.
• W2152556249 countsByYear W21525562492014 @default.
• W2152556249 countsByYear W21525562492017 @default.
• W2152556249 countsByYear W21525562492018 @default.
• W2152556249 countsByYear W21525562492019 @default.
• W2152556249 countsByYear W21525562492020 @default.
• W2152556249 countsByYear W21525562492021 @default.
• W2152556249 countsByYear W21525562492022 @default.
• W2152556249 countsByYear W21525562492023 @default.
• W2152556249 crossrefType "journal-article" @default.
• W2152556249 hasAuthorship W2152556249A5055360910 @default.
• W2152556249 hasAuthorship W2152556249A5075383401 @default.
• W2152556249 hasConcept C107832698 @default.
• W2152556249 hasConcept C111368507 @default.
• W2152556249 hasConcept C115880899 @default.
• W2152556249 hasConcept C127313418 @default.
• W2152556249 hasConcept C13106087 @default.
• W2152556249 hasConcept C151730666 @default.
• W2152556249 hasConcept C17409809 @default.
• W2152556249 hasConcept C2780181037 @default.
• W2152556249 hasConcept C2780191791 @default.
• W2152556249 hasConcept C59235061 @default.
• W2152556249 hasConceptScore W2152556249C107832698 @default.
• W2152556249 hasConceptScore W2152556249C111368507 @default.
• W2152556249 hasConceptScore W2152556249C115880899 @default.
• W2152556249 hasConceptScore W2152556249C127313418 @default.
• W2152556249 hasConceptScore W2152556249C13106087 @default.
• W2152556249 hasConceptScore W2152556249C151730666 @default.
• W2152556249 hasConceptScore W2152556249C17409809 @default.
• W2152556249 hasConceptScore W2152556249C2780181037 @default.
• W2152556249 hasConceptScore W2152556249C2780191791 @default.
• W2152556249 hasConceptScore W2152556249C59235061 @default.
• W2152556249 hasIssue "9" @default.
• W2152556249 hasLocation W21525562491 @default.
• W2152556249 hasOpenAccess W2152556249 @default.
• W2152556249 hasPrimaryLocation W21525562491 @default.
• W2152556249 hasRelatedWork W1539144340 @default.
• W2152556249 hasRelatedWork W1606027898 @default.
• W2152556249 hasRelatedWork W2051039451 @default.
• W2152556249 hasRelatedWork W2065935458 @default.
• W2152556249 hasRelatedWork W2078170548 @default.
• W2152556249 hasRelatedWork W2085096887 @default.
• W2152556249 hasRelatedWork W2152556249 @default.
• W2152556249 hasRelatedWork W2323142243 @default.
• W2152556249 hasRelatedWork W2327585744 @default.
• W2152556249 hasRelatedWork W3136940746 @default.
• W2152556249 hasVolume "82" @default.
• W2152556249 isParatext "false" @default.
• W2152556249 isRetracted "false" @default.
• W2152556249 magId "2152556249" @default.

• next