Matches in SemOpenAlex for { <https://semopenalex.org/work/W3107961896> ?p ?o ?g. }
- W3107961896 endingPage "326" @default.
- W3107961896 startingPage "247" @default.
- W3107961896 abstract "Abstract The Carboniferous Foraminifera are composed of representatives of three classes: Fusulinata, Miliolata and Nodosariata. Despite ample literature on Paleozoic Allogromiata and Textulariata, the real presence of these classes remains questionable during the Carboniferous and they are thus excluded herein. The main biostratigraphical markers belong to the superfamilies Archaediscoidea, Lasiodiscoidea and Bradyinoidea, even if many genera among the archaediscoids still have a controversial nomenclature, as well as do some lasiodiscids and bradyinoids. Secondary biostratigraphical markers belong to Lituotubelloidea (= ‘Tournayelloidea’ of the authors), Endothyroidea and Loeblichioidea (these latter giving rise to the primitive Fusulinida). The Miliolata appear at the Visean/Serpukhovian boundary interval. The typical Carboniferous miliolates are primitive nubeculariins and cornuspirinins. Tubiphytids might be miliolate and cyanobacterium consortia, derived from the nubeculariin Palaeonubecularia . The most primitive nodosariates (syzraniids) appeared in the Moscovian; and gave rise, in the latest Carboniferous, to Protonodosaria , Nodosinelloides and possibly Polarisella , Paravervilleina and the oldest Geinitzinoidea. Palaeobiological data are mainly provided by the genera Bradyina , Tetrataxis and Climacammina . Palaeobiogeographical distributions of Pojarkovella , Janischewskina, Eosigmoilina , Brenckleina , Spireitlina , Hemigordius and Syzrania testify to the successive foraminiferal migrations between the Palaeotethys, Ural and Panthalassan oceans. Two taxa are created: Eoparastaffellidae and Banffellinae." @default.
- W3107961896 created "2020-12-07" @default.
- W3107961896 creator A5022478113 @default.
- W3107961896 creator A5050857807 @default.
- W3107961896 date "2021-03-31" @default.
- W3107961896 modified "2023-10-18" @default.
- W3107961896 title "Carboniferous smaller Foraminifera: convergences and divergences" @default.
- W3107961896 cites W1251475575 @default.
- W3107961896 cites W130268143 @default.
- W3107961896 cites W1495573366 @default.
- W3107961896 cites W1565536200 @default.
- W3107961896 cites W1579438866 @default.
- W3107961896 cites W1585968842 @default.
- W3107961896 cites W1695477525 @default.
- W3107961896 cites W1728449985 @default.
- W3107961896 cites W1788486945 @default.
- W3107961896 cites W1850306293 @default.
- W3107961896 cites W1852660717 @default.
- W3107961896 cites W1911467619 @default.
- W3107961896 cites W1915941302 @default.
- W3107961896 cites W1916730934 @default.
- W3107961896 cites W1964306176 @default.
- W3107961896 cites W1965173604 @default.
- W3107961896 cites W1967049457 @default.
- W3107961896 cites W1967399299 @default.
- W3107961896 cites W1968239232 @default.
- W3107961896 cites W1968506534 @default.
- W3107961896 cites W1969413086 @default.
- W3107961896 cites W1970192301 @default.
- W3107961896 cites W1971129444 @default.
- W3107961896 cites W1971151116 @default.
- W3107961896 cites W1972298334 @default.
- W3107961896 cites W1973069162 @default.
- W3107961896 cites W1975527432 @default.
- W3107961896 cites W1976237764 @default.
- W3107961896 cites W1976611922 @default.
- W3107961896 cites W1978386412 @default.
- W3107961896 cites W1978507158 @default.
- W3107961896 cites W1979548164 @default.
- W3107961896 cites W1980055870 @default.
- W3107961896 cites W1980753654 @default.
- W3107961896 cites W1981295549 @default.
- W3107961896 cites W1982776066 @default.
- W3107961896 cites W1984462444 @default.
- W3107961896 cites W1984531268 @default.
- W3107961896 cites W1986406735 @default.
- W3107961896 cites W1988600902 @default.
- W3107961896 cites W1989042067 @default.
- W3107961896 cites W1991800405 @default.
- W3107961896 cites W1993076539 @default.
- W3107961896 cites W1996629919 @default.
- W3107961896 cites W1999160483 @default.
- W3107961896 cites W1999753429 @default.
- W3107961896 cites W2000150340 @default.
- W3107961896 cites W2001348280 @default.
- W3107961896 cites W2002704004 @default.
- W3107961896 cites W2002742764 @default.
- W3107961896 cites W2003446402 @default.
- W3107961896 cites W2007506474 @default.
- W3107961896 cites W2009320726 @default.
- W3107961896 cites W2010239952 @default.
- W3107961896 cites W2010572609 @default.
- W3107961896 cites W2011417106 @default.
- W3107961896 cites W2012011936 @default.
- W3107961896 cites W2015652291 @default.
- W3107961896 cites W2015699917 @default.
- W3107961896 cites W2015715279 @default.
- W3107961896 cites W2016517593 @default.
- W3107961896 cites W2017630764 @default.
- W3107961896 cites W2017683990 @default.
- W3107961896 cites W2019498134 @default.
- W3107961896 cites W2024417107 @default.
- W3107961896 cites W2024738353 @default.
- W3107961896 cites W2025301696 @default.
- W3107961896 cites W2027728544 @default.
- W3107961896 cites W2028678528 @default.
- W3107961896 cites W2030434502 @default.
- W3107961896 cites W2031163305 @default.
- W3107961896 cites W2034233781 @default.
- W3107961896 cites W2035724014 @default.
- W3107961896 cites W2035911033 @default.
- W3107961896 cites W2037012003 @default.
- W3107961896 cites W2039421030 @default.
- W3107961896 cites W2040325956 @default.
- W3107961896 cites W2040550242 @default.
- W3107961896 cites W2041884264 @default.
- W3107961896 cites W2042575385 @default.
- W3107961896 cites W2045747567 @default.
- W3107961896 cites W2046957555 @default.
- W3107961896 cites W2046992166 @default.
- W3107961896 cites W2052262391 @default.
- W3107961896 cites W2052346014 @default.
- W3107961896 cites W2053759306 @default.
- W3107961896 cites W2054489561 @default.
- W3107961896 cites W2055594708 @default.
- W3107961896 cites W2056709996 @default.
- W3107961896 cites W2057757959 @default.
- W3107961896 cites W2060553931 @default.