Megaspores from the Late Triassic‒Early Jurassic of southern Scandinavia: taxonomic and biostratigraphic implications

IF 1.2 4区 地球科学 Q2 GEOLOGY Gff Pub Date : 2021-07-03 DOI:10.1080/11035897.2021.1923060
Jungang Peng, S. Slater, V. Vajda
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引用次数: 3

Abstract

ABSTRACT Here we investigate megaspores from 10 Triassic‒Jurassic localities of southern Sweden and Bornholm, Denmark, based on collections housed in the Swedish Museum of Natural History. We identify and describe 19 megaspore taxa belonging to three stratigraphically constrained assemblages, representing the Rhaetian, Hettangian and Pliensbachian, respectively. Megaspores are abundant and diverse (12 taxa) in the Rhaetian assemblage. Diversity markedly decreases across the Triassic–Jurassic boundary (TJB), with species richness reducing from 12 to two taxa. The Hettangian assemblage is well-preserved but depauperate, and is overwhelmingly dominated by Nathorstisporites hopliticus. A subsequent recovery of lycopsid diversity followed, recorded by an increase in richness to six taxa in the Pliensbachian assemblage. The disappearance of the hygrophilous and diverse heterosporous lycophyte communities across the TJB, suggests a shift to drier conditions in the earliest Jurassic. This is supported by lithological changes from coal-forming environments in the Rhaetian to sandstone-dominated fluvial-estuarine facies in the Hettangian. Throughout this study, we analysed the megaspores using fluorescence microscopy, which revealed detailed morphological features on specimens that were otherwise opaque under visible light. This non-destructive technique is particularly useful for examining opaque megaspores embedded in permanent mounting media, such as epoxy resin, and may provide new insights into historical megaspore collections elsewhere.
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斯堪的纳维亚南部晚三叠世-早侏罗世的大孢子:分类和生物地层学意义
本文以瑞典自然历史博物馆的藏品为基础,研究了瑞典南部和丹麦博恩霍尔姆的10个三叠纪-侏罗纪地区的大孢子。我们鉴定并描述了19个大孢子类群,分别属于3个地层限制组合,分别代表Rhaetian、Hettangian和Pliensbachian。大孢子丰富多样(12个分类群)。三叠系—侏罗系界线(TJB)的多样性明显下降,物种丰富度从12个分类群减少到2个分类群。Hettangian组合保存完好,但发育不良,绝大多数为Nathorstisporites hopliticus。随后,石松多样性恢复,丰富度增加到pliensbachia组合中的6个分类群。整个TJB地区的喜湿性和多样的异孢子石松群落的消失,表明侏罗纪早期向干燥环境的转变。从雷蒂亚成煤环境到河塘期以砂岩为主的河流-河口相的岩性变化支持了这一观点。在整个研究过程中,我们使用荧光显微镜分析了大孢子,揭示了在可见光下不透明的标本的详细形态特征。这种非破坏性技术特别适用于检查嵌入在永久安装介质(如环氧树脂)中的不透明大孢子,并可能为其他地方的历史大孢子收藏提供新的见解。
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来源期刊
Gff
Gff 地学-地质学
CiteScore
2.80
自引率
10.00%
发文量
11
审稿时长
>12 weeks
期刊介绍: GFF is the journal of the Geological Society of Sweden. It is an international scientific journal that publishes papers in English covering the whole field of geology and palaeontology, i.e. petrology, mineralogy, stratigraphy, systematic palaeontology, palaeogeography, historical geology and Quaternary geology. Systematic descriptions of fossils, minerals and rocks are an important part of GFF''s publishing record. Papers on regional or local geology should deal with Balto-Scandian or Northern European geology, or with geologically related areas. Papers on geophysics, geochemistry, biogeochemistry, climatology and hydrology should have a geological context. Descriptions of new methods (analytical, instrumental or numerical), should be relevant to the broad scope of the journal. Review articles are welcome, and may be solicited occasionally. Thematic issues are also possible.
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