FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2024078927> ?p ?o ?g. }

• W2024078927 endingPage "881" @default.
• W2024078927 startingPage "851" @default.
• W2024078927 abstract "The Murray Supergroup records temperate-water carbonate deposition within a shallow, mesotrophic, Oligo-Miocene inland sea protected from high-energy waves and swells of the open ocean by a granitic archipelago at its southern margin. Rocks are very well preserved and exposed in nearly continuous outcrop along the River Murray in South Australia. Most facies are rich in carbonate silt, contain a background assemblage of gastropods (especially turritellids) and infaunal bivalves, and are packaged on a decimetre-scale defined by firmground and hardground omission surfaces. Bioturbation is pervasive and overprinted, resulting in rare preservation of physical sedimentary structures. Facies are grouped into four associations (large foraminiferan–bryozoan, echinoid–bryozoan, mollusc and clay facies) interpreted to represent shallow-water (<50 m) deposition under progressively higher trophic resource levels (from low mesotrophy to eutrophy), and restricted marine conditions from relatively offshore to nearshore regions. A large-scale shift from high- to low-mesotrophic conditions within lower Miocene strata reflects a change in climate from wet to seasonally dry conditions and highlights the influence terrestrially derived nutrients had upon this shallow, land-locked sea. Overall, low trophic resource levels during periods of seasonally dry climate resulted in a deepening of the euphotic zone, a widespread proliferation of foraminiferan photozoan fauna and a relatively high carbonate productivity. Inshore, heterozoan facies became progressively muddier and restricted towards the shoreline. In contrast, periods of wet climate led to rising trophic resource levels, resulting in a shallowing of the euphotic zone, a decrease in epifaunal and seagrass cover and widespread development of a mostly heterozoan biota dominated by infaunal echinoids. Rates of carbonate production and accumulation were relatively low. The Murray Basin is best described as an epeiric ramp. Wide facies belts developed in a shallow sea on a low-angled slope reaching many hundreds of kilometres in length. Grainy shoal and back-barrier facies were absent. Internally generated waves impinged the sea floor in offshore regions and, because of friction along a wide and shallow sea floor, created a low-energy expanse of waters across the proximal ramp. Storms were the dominating depositional process capable of disrupting the entire sea floor." @default.
• W2024078927 created "2016-06-24" @default.
• W2024078927 creator A5003903190 @default.
• W2024078927 creator A5079681033 @default.
• W2024078927 creator A5081418757 @default.
• W2024078927 creator A5088541432 @default.
• W2024078927 date "2000-08-01" @default.
• W2024078927 modified "2023-10-14" @default.
• W2024078927 title "An epeiric ramp: low-energy, cool-water carbonate facies in a Tertiary inland sea, Murray Basin, South Australia" @default.
• W2024078927 cites W155919060 @default.
• W2024078927 cites W1741338003 @default.
• W2024078927 cites W1967155621 @default.
• W2024078927 cites W1968521098 @default.
• W2024078927 cites W1969099977 @default.
• W2024078927 cites W1971404445 @default.
• W2024078927 cites W1978157185 @default.
• W2024078927 cites W1979563841 @default.
• W2024078927 cites W1980193935 @default.
• W2024078927 cites W1983174468 @default.
• W2024078927 cites W1985350839 @default.
• W2024078927 cites W1986484362 @default.
• W2024078927 cites W1992712824 @default.
• W2024078927 cites W1994374488 @default.
• W2024078927 cites W2000476760 @default.
• W2024078927 cites W2004114920 @default.
• W2024078927 cites W2013864935 @default.
• W2024078927 cites W2016003832 @default.
• W2024078927 cites W2020005783 @default.
• W2024078927 cites W2024654077 @default.
• W2024078927 cites W2029959967 @default.
• W2024078927 cites W2032821463 @default.
• W2024078927 cites W2035110537 @default.
• W2024078927 cites W2040031322 @default.
• W2024078927 cites W2041471080 @default.
• W2024078927 cites W2041635490 @default.
• W2024078927 cites W2042455666 @default.
• W2024078927 cites W2044992791 @default.
• W2024078927 cites W2046994720 @default.
• W2024078927 cites W2049487263 @default.
• W2024078927 cites W2052346014 @default.
• W2024078927 cites W2052834771 @default.
• W2024078927 cites W2057801696 @default.
• W2024078927 cites W2059542863 @default.
• W2024078927 cites W2061084791 @default.
• W2024078927 cites W2062744904 @default.
• W2024078927 cites W2069328966 @default.
• W2024078927 cites W2070635110 @default.
• W2024078927 cites W2088261594 @default.
• W2024078927 cites W2089480007 @default.
• W2024078927 cites W2107294655 @default.
• W2024078927 cites W2126849800 @default.
• W2024078927 cites W2132300109 @default.
• W2024078927 cites W2140152564 @default.
• W2024078927 cites W2165117122 @default.
• W2024078927 cites W2165376925 @default.
• W2024078927 cites W2233134997 @default.
• W2024078927 cites W2303283138 @default.
• W2024078927 cites W2327320150 @default.
• W2024078927 cites W2327706037 @default.
• W2024078927 cites W2334002538 @default.
• W2024078927 cites W94434984 @default.
• W2024078927 doi "https://doi.org/10.1046/j.1365-3091.2000.00328.x" @default.
• W2024078927 hasPublicationYear "2000" @default.
• W2024078927 type Work @default.
• W2024078927 sameAs 2024078927 @default.
• W2024078927 citedByCount "102" @default.
• W2024078927 countsByYear W20240789272012 @default.
• W2024078927 countsByYear W20240789272013 @default.
• W2024078927 countsByYear W20240789272015 @default.
• W2024078927 countsByYear W20240789272016 @default.
• W2024078927 countsByYear W20240789272018 @default.
• W2024078927 countsByYear W20240789272019 @default.
• W2024078927 countsByYear W20240789272020 @default.
• W2024078927 countsByYear W20240789272021 @default.
• W2024078927 countsByYear W20240789272022 @default.
• W2024078927 countsByYear W20240789272023 @default.
• W2024078927 crossrefType "journal-article" @default.
• W2024078927 hasAuthorship W2024078927A5003903190 @default.
• W2024078927 hasAuthorship W2024078927A5079681033 @default.
• W2024078927 hasAuthorship W2024078927A5081418757 @default.
• W2024078927 hasAuthorship W2024078927A5088541432 @default.
• W2024078927 hasConcept C109007969 @default.
• W2024078927 hasConcept C111368507 @default.
• W2024078927 hasConcept C127313418 @default.
• W2024078927 hasConcept C142796444 @default.
• W2024078927 hasConcept C146588470 @default.
• W2024078927 hasConcept C151730666 @default.
• W2024078927 hasConcept C153018869 @default.
• W2024078927 hasConcept C18903297 @default.
• W2024078927 hasConcept C191897082 @default.
• W2024078927 hasConcept C192562407 @default.
• W2024078927 hasConcept C2780659211 @default.
• W2024078927 hasConcept C2780892065 @default.
• W2024078927 hasConcept C2816523 @default.
• W2024078927 hasConcept C77044568 @default.
• W2024078927 hasConcept C86803240 @default.
• W2024078927 hasConcept C86839594 @default.
• W2024078927 hasConceptScore W2024078927C109007969 @default.

• next