FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4292689903> ?p ?o ?g. }

• W4292689903 endingPage "485" @default.
• W4292689903 startingPage "457" @default.
• W4292689903 abstract "Lithologic and foraminiferal analysis from the western part of the Valles–San Luis Potosi­ platform reflect a sea-level rise suggesting that the platform was drowned at the Cenomanian-Turonian boundary interval. Benthic and planktic foraminiferal content of the succession was identified to establish the transition from the shallow-water carbonate sedimentation with abundant larger benthic foraminifera, algae, rudists and other molluscs, corals, echinoderms, worms changing to hemipelagic-pelagic sediments containing calcispheres and opportunistic foraminifers (r-strategists), such as whitenellids, hedbergellids, heterohelicids and elongated chambered forms, as well as radiolarians. The El Abra Limestone is dated as the middle-late Cenomanian age (Pseudolituonella reicheliAssemblage Zone) and was deposited on a warm shallow-marine rimmed platform. Peloidal-bioclastic packstone-grainstone is the dominant texture of these rocks. Lithological variations determined by the high detrital influx were followed by a major transgression when wackestone and marly limestone of the lower part of the Soyatal Formation were deposited. The transition to deeper open marine environments is dated as latest Cenomanian/earliest Turonian represented by the Whiteinella archaeocretacea Partial Taxon Range Zone and coincides with a global sea-level rise and the Oceanic Anoxic Event 2 (OAE 2). Deeper overlying deposits of the Helvetoglobotruncana helvetica Total Range Zone (early/middle Turonian) are characterized in the study area by the occurrence of the keeled forms (k strategists). The Cenomanian/Turonian boundary is placed within the Whiteinella archaeocretacea Partial Range Zone in absence of ammonite markers. When theValles-San Luis Potosí platformwas flooded, the carbonate factorywas stressed due to the trophic resource modifications. Production of a larger amount of nutrients led to the extinction of the k-strategist benthic foraminifera; only small benthic foraminifera survived for a short period of time in the newly established mesotrophic conditions. High productivity continued and in the eutrophic episode the calcispheres, r-opportunists, intermediate taxa and the planktic foraminifera with elongate chambers proliferated. Later, complete drowning enabled the recovery of oligotrophic conditions with the occurrence of k-strategist keeled planktic taxa." @default.
• W4292689903 created "2022-08-23" @default.
• W4292689903 creator A5017404224 @default.
• W4292689903 creator A5020802458 @default.
• W4292689903 creator A5026657710 @default.
• W4292689903 creator A5057291592 @default.
• W4292689903 date "2012-01-01" @default.
• W4292689903 modified "2023-10-01" @default.
• W4292689903 title "Biostratigraphy and paleoenvironment of the Cenomanian/Turonian boundary interval based on foraminifera from Valles-San Luis Potosi­ Platform, Mexico" @default.
• W4292689903 doi "https://doi.org/10.47894/mpal.58.6.01" @default.
• W4292689903 hasPublicationYear "2012" @default.
• W4292689903 type Work @default.
• W4292689903 citedByCount "16" @default.
• W4292689903 countsByYear W42926899032015 @default.
• W4292689903 countsByYear W42926899032016 @default.
• W4292689903 countsByYear W42926899032017 @default.
• W4292689903 countsByYear W42926899032019 @default.
• W4292689903 countsByYear W42926899032020 @default.
• W4292689903 countsByYear W42926899032021 @default.
• W4292689903 countsByYear W42926899032022 @default.
• W4292689903 countsByYear W42926899032023 @default.
• W4292689903 crossrefType "journal-article" @default.
• W4292689903 hasAuthorship W4292689903A5017404224 @default.
• W4292689903 hasAuthorship W4292689903A5020802458 @default.
• W4292689903 hasAuthorship W4292689903A5026657710 @default.
• W4292689903 hasAuthorship W4292689903A5057291592 @default.
• W4292689903 hasConcept C109007969 @default.
• W4292689903 hasConcept C111368507 @default.
• W4292689903 hasConcept C12294951 @default.
• W4292689903 hasConcept C127313418 @default.
• W4292689903 hasConcept C146588470 @default.
• W4292689903 hasConcept C151730666 @default.
• W4292689903 hasConcept C19320362 @default.
• W4292689903 hasConcept C27543578 @default.
• W4292689903 hasConcept C2776226903 @default.
• W4292689903 hasConcept C2778609275 @default.
• W4292689903 hasConcept C2779032034 @default.
• W4292689903 hasConcept C2780368712 @default.
• W4292689903 hasConcept C61721801 @default.
• W4292689903 hasConcept C6494504 @default.
• W4292689903 hasConcept C77271252 @default.
• W4292689903 hasConcept C83042747 @default.
• W4292689903 hasConceptScore W4292689903C109007969 @default.
• W4292689903 hasConceptScore W4292689903C111368507 @default.
• W4292689903 hasConceptScore W4292689903C12294951 @default.
• W4292689903 hasConceptScore W4292689903C127313418 @default.
• W4292689903 hasConceptScore W4292689903C146588470 @default.
• W4292689903 hasConceptScore W4292689903C151730666 @default.
• W4292689903 hasConceptScore W4292689903C19320362 @default.
• W4292689903 hasConceptScore W4292689903C27543578 @default.
• W4292689903 hasConceptScore W4292689903C2776226903 @default.
• W4292689903 hasConceptScore W4292689903C2778609275 @default.
• W4292689903 hasConceptScore W4292689903C2779032034 @default.
• W4292689903 hasConceptScore W4292689903C2780368712 @default.
• W4292689903 hasConceptScore W4292689903C61721801 @default.
• W4292689903 hasConceptScore W4292689903C6494504 @default.
• W4292689903 hasConceptScore W4292689903C77271252 @default.
• W4292689903 hasConceptScore W4292689903C83042747 @default.
• W4292689903 hasIssue "6" @default.
• W4292689903 hasLocation W42926899031 @default.
• W4292689903 hasOpenAccess W4292689903 @default.
• W4292689903 hasPrimaryLocation W42926899031 @default.
• W4292689903 hasRelatedWork W1817454131 @default.
• W4292689903 hasRelatedWork W1895033383 @default.
• W4292689903 hasRelatedWork W2060267404 @default.
• W4292689903 hasRelatedWork W2185355962 @default.
• W4292689903 hasRelatedWork W2189391638 @default.
• W4292689903 hasRelatedWork W3097651183 @default.
• W4292689903 hasRelatedWork W4214716469 @default.
• W4292689903 hasRelatedWork W4292689903 @default.
• W4292689903 hasRelatedWork W761170048 @default.
• W4292689903 hasRelatedWork W859527901 @default.
• W4292689903 hasVolume "58" @default.
• W4292689903 isParatext "false" @default.
• W4292689903 isRetracted "false" @default.
• W4292689903 workType "article" @default.