Pollen Grains of Picrodendraceae, Phyllanthaceae, Euphorbiaceae (Former Euphorbiaceae) from Palaeogene Strata of Central Europe and South China 90 ©Geol

Pollen Grains of Picrodendraceae, Phyllanthaceae, Euphorbiaceae (Former Euphorbiaceae) from Palaeogene Strata of Central Europe and South China 90 ©Geol

ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Berichte der Geologischen Bundesanstalt Jahr/Year: 2011 Band/Volume: 85 Autor(en)/Author(s): Hofmann Christa-Charlotte, Zetter Reinhard, Jin JianHua Artikel/Article: Pollen grains of Picrodendraceae, Phyllanthaceae, Euphorbiaceae (former Euphorbiaceae) from Palaeogene strata of Central Europe and South China 90 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Berichte Geol. B.-A., 85 (ISSN 1017-8880) – CBEP 2011, Salzburg, June 5th – 8th Pollen grains of Picrodendraceae, Phyllanthaceae, Euphorbiaceae (former Euphorbiaceae ) from Palaeogene strata of Central Europe and South China. Christa-Ch. Hofmann1, Reinhard Zetter1, Jinhua Jin2 1 University of Vienna, department of Palaeontology, Vienna, Austria 2 School of life Sciences Sun Yat-sen University Guangzhou, China Fossil pollen grains assigned to Picrodendraceae, Phyllanthaceae and Euphorbiaceae have been encountered from sedimentary rocks of Palaeocene and Eocene ages. Fossil stephanoporate, echinate pollen of the Aristogeitonia-type (Picrodendraceae), that have been formerly described as Malvacipollis or Longetia are present in hyperthermal microfloras of Germany (mid-Eocene Stolzenbach) and Austria (lower Eocene Krappfeld, Carinthia) and from the Palaeocene/Eocene boundary rocks of Austria (Salzburg). Mostly all modern similar looking taxa of the Picrodendraceae do occur in the palaeotropics and only very few in the new world. Two fossil stephanoporate, reticulate pollen types that have been formerly described as Retimultiporopollenites spp. occur frequently in mid-Eocene sedimentary rocks of the Changchang Formation (Hainan, South China). They can be affiliated with the extant pantropical genus Phyllanthus (Phyllanthaceae, tribe Phyllantheae), in particular with the taxa P. ruber, P. hainanensis, and P. leptocladus, and might evidence a palaeotropical origin of the Phyllanthaceae. Fossil wood associated with Phyllanthus (Paraphyllanthoxylon hainanensis) from the Changchang basin corroborate the pollen data. A presumable Phyllanthaceae pollen from rocks of Palaeocene/Eocene age is compared with the genus Richeriella, which today has two species growing in Asia (China and Malaysia). Three fossil tricolporate, microreticulate pollen affiliated to the Euphorbiaceae, particularly to Euphorbia, Stillingia and Leucroton are present in the sedimentary rocks at the Palaeocene/Eocene boundary (Salzburg) and the Lower Eocene (Krappfeld, Carinthia) of Austria. Whereas Euphorbia today is a cosmopolitan genus Leucroton today occurs in the Caribbean region and extant Stillingia, a tropical genus, is distributed in the Americas, Madagascar and Malaysia. 90.

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