期刊论文详细信息
Palaeontologia Electronica
Preliminary investigation of a diverse megafossil floral assemblage from the middle Miocene of southern Mississippi, USA
James E. Starnes1  Brian Axsmith2  Debra Z. Stults2  Daniel McNair3  Mac H. Alford3 
[1] Mississippi Departmental of Environmental Quality;University of South Alabama;University of Southern Mississippi
关键词: Daniel McNair;    Debra Z. Stults;    Brian Axsmith;    Mac H. Alford;    James E. Starnes;    Gulf Coast;    Hattiesburg Formation;    Lemna;    fossil palms;    Salvinia;    Sargentodoxa;    Mississippi;   
DOI  :  10.26879/906
学科分类:地质学
来源: Palaeontologia Electronica
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【 摘 要 】

Our understanding of Miocene floras in eastern North America is hampered by the rarity of megafossil sites. An early report from the middle Miocene Hattiesburg Formation in Mississippi included palms and Ulmus. A later report listed Taxodium, Salix, either Morus or Celtis, and monocot fragments. The floral assemblage described here was recently recovered from along the Bouie River in southern Mississippi. Ferns are represented by complete Salvinia specimens including attached sporocarps, Woodwardia, and Osmunda. Conifers are represented by branchlets of Taxodium. Angiosperms include leaves attributable to the Lauraceae.Platanus is known from leaves, stipules, and fruits. Leaflets of Sambucus are common. Cercis is recognized from leaves with palmate venation and pulvini. Leaves of Quercus sections Lobatae and Quercushave been recovered. The Juglandaceae include fruits of Juglans and two species of Carya. Morus, Populus, and Salix leaves have been recovered. Of particular biogeographical interest is a seed ofSargentodoxa, which is the first record from the southeastern coastal plain of this current Chinese endemic. Monocots include Cyperus and two types of palm, including one with armed petioles. The first vegetative fossils ofLemna from North America have been identified. Because most of the fossils are related to plants still found in the region today, the climate was probably similar to that of the modern central Gulf Coastal Plain. This flora is now one of the most extensively known in the Neogene of southeastern North America and helps to fill a major gap in our understating of Miocene plant evolution.

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