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

IF 1.7 3区 地球科学 Q2 PALEONTOLOGY
Maria Tekleva , Mário Miguel Mendes , Jiří Kvaček , Pedro Dinis , Pedro Callapez
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Abstract

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.

在葡萄牙西部托雷斯韦德拉斯卡萨尔多博拉乔下白垩纪岩石中的一种孤立的裂殖蕨类植物孢子囊结构中发现的卡氏孢子的形态学和超微结构
孢子化石为了解蕨类植物的进化史提供了重要信息,包括它们随着时间推移而发生的形态变化和适应性。研究人员对具有由平行或近似平行的肋条(muri)组成的环状雕刻的三叶孢子的形态和超微结构进行了研究。使用光学显微镜、扫描电子显微镜和透射电子显微镜对孢子进行了观察。从托雷斯韦德拉斯(葡萄牙西部卢西坦盆地)附近的 Casal do Borracho 中化石群的沉积物中采集到的单个孢子囊结构中提取了蝉状孢子,该沉积物属于阿尔马格姆地层,被认为是巴利米亚晚期或奥普梯早期(可能比这更早)。该研究将一种裂叶蕨类植物的孢子囊结构和原位蝉状孢子与红豆杉科(Anemiaceae)植物进行了比较。根据孢子的大小和形状、laesura 长度、约 20 条下部窄棱、垂直于孢子两侧的方向以及三组形成 V 形图案的上部棱,本研究中的卡氏孢子被明确归属于化石类群 Cicatricosisporites venustus。孢子的超微结构包括均匀的蝶形外孢子,近端、远端和赤道区域的厚度略有不同。所研究孢子的形态和超微结构与贫血型相符。
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来源期刊
CiteScore
3.50
自引率
21.10%
发文量
149
审稿时长
6 months
期刊介绍: The Review of Palaeobotany and Palynology is an international journal for articles in all fields of palaeobotany and palynology dealing with all groups, ranging from marine palynomorphs to higher land plants. Original contributions and comprehensive review papers should appeal to an international audience. Typical topics include but are not restricted to systematics, evolution, palaeobiology, palaeoecology, biostratigraphy, biochronology, palaeoclimatology, paleogeography, taphonomy, palaeoenvironmental reconstructions, vegetation history, and practical applications of palaeobotany and palynology, e.g. in coal and petroleum geology and archaeology. The journal especially encourages the publication of articles in which palaeobotany and palynology are applied for solving fundamental geological and biological problems as well as innovative and interdisciplinary approaches.
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