Gandolfo María A, Hermsen Elizabeth J
L. H. Bailey Hortorium, Plant Biology Section, School of Integrative Plant Science, 412 Mann Library Building, Cornell University, Ithaca, NY 14853, USA.
Department of Environmental and Plant Biology, Porter Hall 315, Ohio University, Athens, OH 45701, USA.
Ann Bot. 2017 Mar 1;119(4):507-516. doi: 10.1093/aob/mcw283.
Radially symmetrical, five-winged fossil fruits from the highly diverse early Eocene Laguna del Hunco flora of Chubut Province, Patagonia, Argentina, are named, described and illustrated. The main goals are to assess the affinities of the fossils and to place them in an evolutionary, palaeoecological and biogeographic context.
Specimens of fossil fruits were collected from the Tufolitas Laguna del Hunco. They were prepared, photographed and compared with similar extant and fossil fruits using published literature. Their structure was also evaluated by comparing them with that of modern Ceratopetalum (Cunoniaceae) fruits through examination of herbarium specimens.
The Laguna del Hunco fossil fruits share the diagnostic features that characterize modern and fossil Ceratopetalum (symmetry, number of fruit wings, presence of a conspicuous floral nectary and overall venation pattern). The pattern of the minor wing (sepal) veins observed in the Patagonian fossil fruits is different from that of modern and previously described fossil Ceratopetalum fruits; therefore, a new fossil species is recognized. An apomorphy (absence of petals) suggests that the fossils belong within crown-group Ceratopetalum .
The Patagonian fossil fruits are the oldest known record for Ceratopetalum . Because the affinities, provenance and age of the fossils are so well established, this new Ceratopetalum fossil species is an excellent candidate for use as a calibration point in divergence dating studies of the family Cunoniaceae. It represents the only record of Ceratopetalum outside Australasia, and further corroborates the biogeographic connection between the Laguna del Hunco flora and ancient and modern floras of the Australasian region.
对来自阿根廷巴塔哥尼亚丘布特省始新世早期高度多样化的拉古纳德尔洪科植物群中呈放射状对称、具五翅的化石果实进行命名、描述和绘图。主要目标是评估这些化石的亲缘关系,并将它们置于进化、古生态和生物地理背景中。
从拉古纳德尔洪科凝灰岩中采集化石果实标本。对其进行处理、拍照,并利用已发表的文献与现存和化石类似果实进行比较。还通过检查标本馆标本,将其结构与现代牛角树属( Cunoniaceae)果实的结构进行比较来评估。
拉古纳德尔洪科化石果实具有现代和化石牛角树属的诊断特征(对称性、果翅数量、明显的花蜜腺存在以及整体脉序模式)。在巴塔哥尼亚化石果实中观察到的小翅(萼片)脉模式与现代和先前描述的化石牛角树属果实不同;因此,识别出一个新的化石物种。一个衍生特征(无花瓣)表明这些化石属于牛角树属冠群。
巴塔哥尼亚化石果实是已知最古老的牛角树属记录。由于这些化石的亲缘关系、来源和年代已得到很好的确立,这个新的牛角树属化石物种是在 Cunoniaceae 科分歧年代测定研究中用作校准点的极佳候选者。它代表了澳大拉西亚以外牛角树属的唯一记录,并进一步证实了拉古纳德尔洪科植物群与澳大拉西亚地区古代和现代植物群之间的生物地理联系。