Matches in SemOpenAlex for { <https://semopenalex.org/work/W2778141330> ?p ?o ?g. }
- W2778141330 endingPage "47" @default.
- W2778141330 startingPage "20" @default.
- W2778141330 abstract "A 220-m thick carbonate-dominated succession has been deposited in shallow-water, saline lake environments during the early to middle Priabonian (MP17A-MP18 mammal zones) in the Saint-Chaptes Basin (south–east France). The palaeoenvironmental, paleoclimatic and palaeogeographic significance of such saline lake carbonates has been deciphered on the basis of a multi-proxy analyses including: 1) depositional and diagenetic features; 2) biological components (molluscs, benthic foraminifera, characean gyrogonites, spores and pollens); 3) carbon and oxygen stable isotopes; 4) trace elements; and 5) clay mineralogy. Five stages of lacustrine system evolution have been identified: 1) fresh-water closed lake under dry climate (unit U1); 2) fresh to brackish water lacustrine deltaic system with a mixed carbonate-siliciclastic sedimentation under relatively wet climatic conditions (unit U2); 3) salt-water lacustrine carbonate system under humid climatic setting (unit U3); 4) evaporitic lake (unit U4); and 5) closed lake with shallow-water carbonate sedimentation under subtropical to Mediterranean climate with dry seasons (unit U5). Upper Eocene aridification is evidenced to have started as early as the earliest Priabonian (unit U1: MP17A mammal zone). A change from humid to dryer climatic conditions is recorded between units U3 and U4. The early to middle Priabonian saline lake is interpreted as an athalassic (inland) lake that have been transiently connected with neighboring salt lakes influenced by seawater and/or fed with sulfates deriving from recycling of evaporites. Maximum of connection with neighboring saline lakes (Mormoiron Basin, Camargue and Central grabens, Hérault Basin) likely occurred during unit U3 and at the base of unit U5. The most likely sources of salts of these adjacent basins are: 1) Triassic evaporites derived from salt-diapirs (Rhône valley) or from paleo-outcrops located east of the Durance fault or offshore in the Gulf of Lion; or 2) marine incursions from the south, through Paleogene grabens in the Gulf of Lion." @default.
- W2778141330 created "2018-01-05" @default.
- W2778141330 creator A5001616542 @default.
- W2778141330 creator A5001770700 @default.
- W2778141330 creator A5012092566 @default.
- W2778141330 creator A5014878305 @default.
- W2778141330 creator A5019630705 @default.
- W2778141330 creator A5042539038 @default.
- W2778141330 date "2018-05-01" @default.
- W2778141330 modified "2023-10-03" @default.
- W2778141330 title "Reconstruction of a saline, lacustrine carbonate system (Priabonian, St-Chaptes Basin, SE France): Depositional models, paleogeographic and paleoclimatic implications" @default.
- W2778141330 cites W1513073511 @default.
- W2778141330 cites W1561768264 @default.
- W2778141330 cites W1589316101 @default.
- W2778141330 cites W1616863472 @default.
- W2778141330 cites W1623728788 @default.
- W2778141330 cites W1950939513 @default.
- W2778141330 cites W1955429289 @default.
- W2778141330 cites W1964177191 @default.
- W2778141330 cites W1965253289 @default.
- W2778141330 cites W1967764929 @default.
- W2778141330 cites W1967882078 @default.
- W2778141330 cites W1970304739 @default.
- W2778141330 cites W1971657763 @default.
- W2778141330 cites W1977109745 @default.
- W2778141330 cites W1978368649 @default.
- W2778141330 cites W1980012965 @default.
- W2778141330 cites W1980218555 @default.
- W2778141330 cites W1981235841 @default.
- W2778141330 cites W1981792740 @default.
- W2778141330 cites W1989589396 @default.
- W2778141330 cites W1995026670 @default.
- W2778141330 cites W1999316486 @default.
- W2778141330 cites W2000772755 @default.
- W2778141330 cites W2001226697 @default.
- W2778141330 cites W2004786627 @default.
- W2778141330 cites W2005527516 @default.
- W2778141330 cites W2005993109 @default.
- W2778141330 cites W2010202861 @default.
- W2778141330 cites W2011798276 @default.
- W2778141330 cites W2015150069 @default.
- W2778141330 cites W2016586371 @default.
- W2778141330 cites W2017804616 @default.
- W2778141330 cites W2030757691 @default.
- W2778141330 cites W2032972770 @default.
- W2778141330 cites W2035706703 @default.
- W2778141330 cites W2036346462 @default.
- W2778141330 cites W2036482356 @default.
- W2778141330 cites W2038554198 @default.
- W2778141330 cites W2039966849 @default.
- W2778141330 cites W2045554100 @default.
- W2778141330 cites W2046004497 @default.
- W2778141330 cites W2050784296 @default.
- W2778141330 cites W2055645445 @default.
- W2778141330 cites W2063923490 @default.
- W2778141330 cites W2065219432 @default.
- W2778141330 cites W2066026465 @default.
- W2778141330 cites W2066781246 @default.
- W2778141330 cites W2076731456 @default.
- W2778141330 cites W2077087277 @default.
- W2778141330 cites W2080542477 @default.
- W2778141330 cites W2081614809 @default.
- W2778141330 cites W2083153970 @default.
- W2778141330 cites W2087037654 @default.
- W2778141330 cites W2090698941 @default.
- W2778141330 cites W2094137719 @default.
- W2778141330 cites W2094203874 @default.
- W2778141330 cites W2095469249 @default.
- W2778141330 cites W2097596444 @default.
- W2778141330 cites W2098492523 @default.
- W2778141330 cites W2098779621 @default.
- W2778141330 cites W2098832013 @default.
- W2778141330 cites W2100424551 @default.
- W2778141330 cites W2111211903 @default.
- W2778141330 cites W2112397008 @default.
- W2778141330 cites W2114370832 @default.
- W2778141330 cites W2115318620 @default.
- W2778141330 cites W2123753499 @default.
- W2778141330 cites W2127551662 @default.
- W2778141330 cites W2131142087 @default.
- W2778141330 cites W2145365391 @default.
- W2778141330 cites W2158216257 @default.
- W2778141330 cites W2163278707 @default.
- W2778141330 cites W2163874251 @default.
- W2778141330 cites W2165859073 @default.
- W2778141330 cites W2166683934 @default.
- W2778141330 cites W2167970659 @default.
- W2778141330 cites W2168369208 @default.
- W2778141330 cites W2172035340 @default.
- W2778141330 cites W2304166063 @default.
- W2778141330 cites W2323267170 @default.
- W2778141330 cites W2329647001 @default.
- W2778141330 cites W2334603771 @default.
- W2778141330 cites W2350343977 @default.
- W2778141330 cites W2467953918 @default.
- W2778141330 cites W2479300748 @default.
- W2778141330 cites W2736148324 @default.
- W2778141330 cites W2738433541 @default.