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  • 1
    Publication Date: 2019
    Description: 〈span〉〈div〉Abstract〈/div〉The genus 〈span〉Falsolikanella〈/span〉, introduced by Granier (1987), was based on the basal Cretaceous species 〈span〉Likanella campanensis〈/span〉 Azéma and Jaffrezo (1972) and assigned to the tribe Diploporeae (Pia, 1920) emend. Güvenc, 1979 within the green alga order Dasycladales. Later, other species were assigned to 〈span〉Falsolikanella〈/span〉. Sections of the type specimens of 〈span〉Likanella campanensis〈/span〉 are reviewed. They show that in this species, the arrangement of the laterals is not metaspondyl, but typical of the genus 〈span〉Actinoporella〈/span〉 (Gümbel in Alth, 1882) emend Conrad, Praturlon, and Radoičić, 1974, with coronae arising from a single primary lateral. Therefore, the species is assigned to the genus 〈span〉Actinoporella〈/span〉 within the tribe Acetabularieae Decaisne, 1842, family Polyphysaceae Kützing, 1843, and the generic attribution of other species previously assigned to 〈span〉Falsolikanella〈/span〉 is discussed.〈/span〉
    Print ISSN: 0022-3360
    Electronic ISSN: 1937-2337
    Topics: Geosciences
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  • 2
    Publication Date: 1991-09-01
    Description: Calcareous algae are frequent constituents in the shallow-marine limestone intercalations of late Aptian–Maastrichtian strata of the Eastern Desert of Egypt, the Sinai, and southern Jordan. A total of 18 species of green algae (among them 16 dasycladaceans withPraturlonella hammudain. comb. andPraturlonella jordanican. sp., two udoteaceans) and eight species of red algae (among them two gymnocodiaceans, three solenoporaceans, and one squamariacean) are described and compared with algae from several Tethyan occurrences. The stratigraphic distribution is calibrated by 10 assemblage-zones based on the associated foraminiferids and compared with 10 ammonite assemblage-zones.The algal contents vary within the different strata: their total contents and diversities increase from the late Aptian–Albian carbonates to the Cenomanian and decrease to the Turonian–Coniacian; no algae were proved in the Santonian–Campanian. The Maastrichtian occurrences are limited to one outcrop.
    Print ISSN: 0022-3360
    Electronic ISSN: 1937-2337
    Topics: Geosciences
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