First Appearance Datums ( FAD s) of selected acritarch taxa and correlation between Lower and Middle Ordovician stages
Author(s) -
Servais Thomas,
Molyneux Stewart G.,
Li Jun,
Nowak Hendrik,
Rubinstein Claudia V.,
Vecoli Marco,
Wang Wen Hui,
Yan Kui
Publication year - 2018
Publication title -
lethaia
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.926
H-Index - 57
eISSN - 1502-3931
pISSN - 0024-1164
DOI - 10.1111/let.12248
Subject(s) - gondwana , diachronous , baltica , acritarch , taxon , paleontology , ordovician , biology , stage (stratigraphy) , tectonics , structural basin
First Appearance Datums ( FAD s) of selected, easily recognizable acritarch morphotypes are assessed to determine their potential contribution to correlation between Lower and Middle Ordovician stages and substage divisions along the Gondwanan margin (Perigondwana) and between Perigondwana and other palaeocontinents. The FAD s for 19 genera, species and species groups are recorded throughout their biogeographical ranges. The taxa investigated fall into three groups. Some have FAD s at about the same level throughout their biogeographical ranges and are useful for long‐distance and intercontinental correlation. Among these are Coryphidium , Dactylofusa velifera , Peteinosphaeridium and Rhopaliophora in the upper Tremadocian Stage; Arbusculidium filamentosum , Aureotesta clathrata simplex and Coryphidium bohemicum in the lower–middle Floian Stage; Dicrodiacrodium in the upper Floian Stage; Frankea in the Dapingian–lower Darriwilian stages; and Orthosphaeridium spp., with FAD s in the Dapingian–lower Darriwilian stages of Perigondwanan regions and at about the same level in Baltica. Other taxa, however, have diachronous (or apparently diachronous) FAD s, and this needs to be taken into account when using them for correlation. A second group of genera and species, comprising Striatotheca , the Veryhachium lairdii group and the V. trispinosum group, have a recurring pattern of FAD s in the Tremadocian Stage on Avalonia and in South Gondwana and West Gondwana, but in the Floian Stage of South China and East Gondwana. The third group, consisting of Arkonia , Ampullula , Barakella , Dasydorus , Liliosphaeridium and Sacculidium , have FAD s that are markedly diachronous throughout their biogeographical ranges, although the global FAD s of Arkonia , Ampullula , Liliosphaeridium and Sacculidium are apparently in South China and/or East Gondwana. It is possible that diachronous FAD s are only apparent and an artefact of sampling. Nevertheless, an alternative interpretation, suggested by recurring patterns, is that some as yet undetermined factor controlled a slower biogeographical spread over time, resulting in diachroneity.
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