Hong-Yu Chen , Tao Yang , Ya Li , Dieter Uhl , Lei Han , Jia-Hao Cai , Li Zhang , Yong-Dong Wang , De-Fei Yan
{"title":"A new fossil record of Adiantum (Pteridaceae) from Oligocene of Qaidam Basin, Northwest China and its palaeoenvironmental implications","authors":"Hong-Yu Chen , Tao Yang , Ya Li , Dieter Uhl , Lei Han , Jia-Hao Cai , Li Zhang , Yong-Dong Wang , De-Fei Yan","doi":"10.1016/j.palwor.2024.11.006","DOIUrl":null,"url":null,"abstract":"<div><div><em>Adiantum</em>, a genus of leptosporangiate ferns, belonging to the Pteridaceae, is characterised by marginal sori, reflexed pseudoindusia, and dichotomous venation. As a large and widespread genus, <em>Adiantum</em> includes about 225 extant species and a nearly worldwide distribution, but its fossil record is rather scarce. Here, we describe a new fossil species of <em>Adiantum</em> as <em>A</em>. <em>qaidamense</em> Chen and Yan, n. sp. based on fossil fertile and sterile pinnules from the Oligocene Shangganchaigou Formation in the western Qaidam Basin, Qinghai Province, China. These fossils are mainly characterised by three clearly marginal sori covered by orbicular or oblong pseudoindusia. Both morphological comparisons and cluster analysis indicate that <em>A</em>. <em>qaidamense</em> can be distinguished from previously known species, and <em>A</em>. <em>capillus-junonis</em> seems to be morphologically the most similar extant species. The discovery of <em>A</em>. <em>qaidamense</em> represents an unequivocal macrofossil record of <em>Adiantum</em> in China, and improves our understanding of the palaeogeographic distribution of the genus and the species richness of the Oligocene flora in the western Qaidam Basin. According to the habitats of extant <em>Adiantum</em>, the existence of <em>A</em>. <em>qaidamense</em> probably indicates that there was a flourishing forest growing on probable calcareous soil with abundant water availability during the Oligocene in the western Qaidam Basin.</div></div>","PeriodicalId":48708,"journal":{"name":"Palaeoworld","volume":"34 4","pages":"Article 100898"},"PeriodicalIF":1.7000,"publicationDate":"2024-12-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Palaeoworld","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1871174X24001471","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
引用次数: 0
Abstract
Adiantum, a genus of leptosporangiate ferns, belonging to the Pteridaceae, is characterised by marginal sori, reflexed pseudoindusia, and dichotomous venation. As a large and widespread genus, Adiantum includes about 225 extant species and a nearly worldwide distribution, but its fossil record is rather scarce. Here, we describe a new fossil species of Adiantum as A. qaidamense Chen and Yan, n. sp. based on fossil fertile and sterile pinnules from the Oligocene Shangganchaigou Formation in the western Qaidam Basin, Qinghai Province, China. These fossils are mainly characterised by three clearly marginal sori covered by orbicular or oblong pseudoindusia. Both morphological comparisons and cluster analysis indicate that A. qaidamense can be distinguished from previously known species, and A. capillus-junonis seems to be morphologically the most similar extant species. The discovery of A. qaidamense represents an unequivocal macrofossil record of Adiantum in China, and improves our understanding of the palaeogeographic distribution of the genus and the species richness of the Oligocene flora in the western Qaidam Basin. According to the habitats of extant Adiantum, the existence of A. qaidamense probably indicates that there was a flourishing forest growing on probable calcareous soil with abundant water availability during the Oligocene in the western Qaidam Basin.
期刊介绍:
Palaeoworld is a peer-reviewed quarterly journal dedicated to the study of past life and its environment. We encourage submission of original manuscripts on all aspects of palaeontology and stratigraphy, comparisons of regional and global data in time and space, and results generated by interdisciplinary investigations in related fields. Some issues will be devoted entirely to a special theme whereas others will be composed of contributed articles. Palaeoworld is dedicated to serving a broad spectrum of geoscientists and palaeobiologists as well as serving as a resource for students in fields as diverse as palaeobiology, evolutionary biology, taxonomy and phylogeny, geobiology, historical geology, and palaeoenvironment.
Palaeoworld publishes original articles in the following areas:
•Phylogeny and taxonomic studies of all fossil groups
•Biostratigraphy, chemostratigraphy, chronostratigraphy
•Palaeoecology, palaeoenvironment and global changes throughout Earth history
•Tempo and mode of biological evolution
•Biological events in Earth history (e.g., extinctions, radiations)
•Ecosystem evolution
•Geobiology and molecular palaeobiology
•Palaeontological and stratigraphic methods
•Interdisciplinary studies focusing on fossils and strata