Morphology and ultrastructure of cicatricose spores found in an isolated sporangium-bearing structure of a schizaealean fern from the Lower Cretaceous rocks at Casal do Borracho, Torres Vedras, western Portugal

被引:0
|
作者
Tekleva, Maria [1 ]
Mendes, Mario Miguel [2 ,3 ,5 ]
Kvacek, Jiri [4 ]
Dinis, Pedro [2 ,5 ]
Callapez, Pedro [5 ,6 ]
机构
[1] Russian Acad Sci, AA Borissiak Paleontol Inst, Profsoyuznaya 123, Moscow 117647, Russia
[2] Univ Coimbra, MARE Marine & Environm Sci Ctr, Earth Sci Dept, ARNET Aquat Res Network, Rua Silvio Lima,Polo 2, P-3030790 Coimbra, Portugal
[3] Fernando Pessoa Univ, Praca 9 Abril, P-4249004 Porto, Portugal
[4] Natl Museum Prague, Dept Palaeontol, Vaclavske nam 68, Prague 11579, Czech Republic
[5] Univ Coimbra, Space Res Univ Coimbra, CITEUC Ctr Earth & Space Res, Observ Geofis & Astron, P-3040004 Coimbra, Portugal
[6] Univ Alcala, Grp Invest PaleoIber, Alcala De Henares 28805, Spain
关键词
Fossil spores; Ferns; Anemiaceae; Lower Cretaceous; Almargem Formation; Portugal; LUSITANIAN BASIN; ANEMIA SCHIZAEACEAE; POTOMAC GROUP; FLORA; PHYLOGENY; SEDIMENTS; EVOLUTION; MOHRIA;
D O I
10.1016/j.revpalbo.2024.105139
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Fossil spores provide important insights into the evolutionary history of ferns, including their morphological changes and adaptations over time. The morphology and ultrastructure of trilete spores with cicatricose sculpture composed of sets of parallel or near-parallel ribs (muri) have been studied. Observations on the spores were performed using light microscopy, scanning electron microscopy, and transmission electron microscopy. The cicatricose spores were extracted from a single sporangium-bearing structure collected from Casal do Borracho mesofossil flora near Torres Vedras (Lusitanian Basin, western Portugal) from sediments belonging to the Almargem Formation, considered to be of late Barremian or early Aptian age (and possible younger than that). The sporangium-bearing structure of a schizaealean fern and in situ cicatricose spores are compared with the family Anemiaceae. On the basis of spore size and shape, laesura length, with about 20 proximal narrow ribs, oriented perpendicular to the spore sides, and three sets of distal ribs forming V-shaped patterns, the cicatricose spores in the present study are clearly assigned to the fossil-taxon Cicatricosisporites venustus. The spore ultrastructure includes a homogeneous exospore of a blechnoid type with a slight difference in the thickness in the proximal, distal, and equatorial regions. The morphology and ultrastructure of the studied spores are corresponded to Anemia type.
引用
收藏
页数:12
相关论文
共 1 条
  • [1] A new palynoflora from upper Barremian-lower Aptian rocks at Casal do Borracho, Torres Vedras, western Portugal, and its palaeoecological significance
    Mendes, Mario Miguel
    Barron, Eduardo
    Dinis, Pedro
    Rey, Jacques
    Batten, David J.
    CRETACEOUS RESEARCH, 2018, 90 : 363 - 374