2017
DOI: 10.1515/acpa-2017-0015
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Pollen morphology of extant Winteraceae: a study allowing SEM-based affiliation of its fossil representatives

Abstract: ABSTRACT. When applying high-resolution microscopy, the pollen morphology of extant taxa can be used to classify fossil pollen, that is, to address the latter in the established systematic-phylogenetic framework. Here we investigate tetrads and pollen features of 20 different Winteraceae species, most of them belonging to the early-diverging generic lineages Tasmannia, Drimys and Pseudowintera. The tetrads and pollen are grouped into eleven pollen types based on diagnostic features observed by both light and s… Show more

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Cited by 6 publications
(8 citation statements)
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“…Pseudowinterapollis pollen so far has mostly been studied with LM, except for Miocene tetrads from South Africa (cf. Grímsson et al., ). The unique pollen morphology of Winteraceae, however, allows us to confidently place our Greenland material in this family (next section) and in the genus Pseudowinterapollis , albeit not in any of the previously described species.…”
Section: Resultsmentioning
confidence: 99%
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“…Pseudowinterapollis pollen so far has mostly been studied with LM, except for Miocene tetrads from South Africa (cf. Grímsson et al., ). The unique pollen morphology of Winteraceae, however, allows us to confidently place our Greenland material in this family (next section) and in the genus Pseudowinterapollis , albeit not in any of the previously described species.…”
Section: Resultsmentioning
confidence: 99%
“…We also compared our new species to three low‐ to mid‐latitude African–Arabian pollen fossils studied with SEM (Table , Appendix S3), namely Pseudowinterapollis africanensis Grímsson, F.H. Neumann & Zetter from the Miocene of Noordhoek on the Cape Peninsula (Coetzee & Praglowski, ; Grímsson et al., ; Neumann et al., ; Roberts et al., ), Qatanipollis species from the Albian of Israel (Schrank, ; Walker, Brenner, & Walker, ); and Walkeripollis gabonensis J.A.Doyle, Hotton & J.V.Ward from the late Barremian to early Aptian of Gabon, equatorial western Africa (Doyle et al., ). Of these, P. agatdalensis shares the most (overlapping) features with the ~40 Myr younger tetrads from South Africa, whereas the ~50 or 65 Myr older African and Near Eastern fossils differ by a least half of the major traits (Table ; Appendix S3).…”
Section: Resultsmentioning
confidence: 99%
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