Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, KS, USA.
Biodiversity Institute and Museum of Natural History, University of Kansas, Lawrence, KS, USA.
Ann Bot. 2019 Feb 15;123(3):451-460. doi: 10.1093/aob/mcy170.
The asterids (>80 000 extant species) appear in the fossil record with considerable diversity near the Turonian-Coniacian boundary (~90 Ma; Late Cretaceous) and are strongly represented in the earliest diverging lineage, Cornales. These early asterid representatives have so far been reported from western North America and eastern Asia. In this study, we characterize a new cornalean taxon based on charcoalified fruits from the upper Turonian of eastern North America, a separate landmass from western North America at the time, and identify early palaeobiogeographical patterns of Cornales during the Cretaceous.
Fossils were studied and imaged using scanning electron microscopy and micro-computed tomography (micro-CT) scanning. To assess the systematic affinities of the fossils, phylogenetic analyses were conducted using maximum parsimony.
The charcoalified fruits are represented by tri-locular woody endocarps with dorsal apically opening germination valves. Three septa intersect to form a robust central axis. Endocarp ground tissue consists of two zones: an outer endocarp composed of isodiametric sclereids and an inner endocarp containing circum-locular fibres. Central vasculature is absent; however, there are several small vascular bundles scattered within the septa. Phylogenetic analysis places the new taxon within the extinct genus Eydeia.
Thick-walled endocarps with apically opening germination valves, no central vascular bundle and one seed per locule are indicative of the order Cornales. Comparative analysis suggests that the fossils represent a new species, Eydeia jerseyensis sp. nov. This new taxon is the first evidence of Cornales in eastern North America during the Cretaceous and provides insights into the palaeobiogeography and initial diversification of the order.
在化石记录中,以 Asterids(现存超过 80,000 种)为代表的植物在 Turonian-Coniacian 边界附近(约 9000 万年前;白垩纪晚期)多样性显著,并且在最早分化的谱系 Cornales 中占有重要地位。这些早期 Asterids 的代表物种迄今为止仅在北美西部和东亚有报道。在本研究中,我们根据来自北美东部上 Turonian 期的炭化果实描述了一个新的 Cornales 分类群,该地区在当时是与北美西部相分离的陆地,同时确定了 Cornales 在白垩纪的早期古生物地理模式。
通过扫描电子显微镜和微计算机断层扫描(micro-CT)扫描对化石进行研究和成像。为了评估化石的系统亲缘关系,我们使用最大简约法进行了系统发育分析。
炭化果实表现为具有背侧顶部开口的三室木质内果皮,三个隔膜相交形成坚固的中央轴。内果皮的基质组织由两个区域组成:一个由等径的厚壁石细胞组成的外内果皮和一个包含环绕室纤维的内内果皮。中央维管束缺失,但在隔膜内有几个小的血管束。系统发育分析将新分类群置于已灭绝的 Eydeia 属内。
具有顶部开口的萌发阀、无中央维管束和每个室一个种子的厚壁内果皮表明该标本属于 Cornales 目。比较分析表明,这些化石代表了一个新的物种,即 Eydeia jerseyensis sp. nov.。该新分类群是白垩纪北美东部 Cornales 的第一个证据,为该目在古生物地理学和早期多样化方面提供了见解。