Jud Nathan A, Gandolfo Maria A, Iglesias Ari, Wilf Peter
L. H. Bailey Hortorium, Plant Biology Section, School of Integrative Plant Science, Cornell University, Ithaca, New York, United States of America.
Universidad Nacional del Comahue, Instituto de Investigaciones en Biodiversidad y Ambiente INIBIOMA-CONICET, San Carlos de Bariloche, Rio Negro, Argentina.
PLoS One. 2017 May 10;12(5):e0176164. doi: 10.1371/journal.pone.0176164. eCollection 2017.
Southern-Hemisphere terrestrial communities from the early Paleocene are poorly known, but recent work on Danian plant fossils from the Salamanca Formation in Chubut Province, Argentina are providing critical data on earliest Paleocene floras. The fossils described here come from a site in the Salamanca Formation dating to ca. 1 million years or less after the end-Cretaceous extinction event; they are the first fossil flowers reported from the Danian of South America, and possible the entire Southern Hemisphere. They are compressions and impressions in flat-laminated light gray shale, and they belong to the family Rhamnaceae (buckthorns). Flowers of Notiantha grandensis gen. et sp. nov. are pentamerous, with distinctly keeled calyx lobes projecting from the hypanthium, clawed and cucullate emarginate petals, antepetalous stamens, and a pentagonal floral disk that fills the hypanthium. Their phylogenetic position was evaluated using a molecular scaffold approach combined with morphological data. Results indicate that the flowers are most like those of extant ziziphoid Rhamnaceae. The associated leaves, assigned to Suessenia grandensis gen. et sp. nov. are simple and ovate, with serrate margins and three acrodromous basal veins. They conform to the distinctive leaves of some extant Rhamnaceae in the ziziphoid and ampelozizyphoid clades. These fossils provide the first unequivocal megafossil evidence of Rhamnaceae in the Southern Hemisphere, demonstrating that Rhamnaceae expanded beyond the tropics by the earliest Paleocene. Given previous reports of rhamnaceous pollen in the late Paleogene and Neogene of Antarctica and southern Australia, this new occurrence increases the possibility of high-latitude dispersal of this family between South America and Australia via Antarctica during the Cenozoic.
人们对古新世早期南半球的陆地群落了解甚少,但最近对阿根廷丘布特省萨拉曼卡组达宁阶植物化石的研究为最早的古新世植物群提供了关键数据。这里描述的化石来自萨拉曼卡组的一个地点,其年代可追溯到白垩纪末大灭绝事件结束后约100万年或更短时间;它们是南美洲达宁阶首次报道的化石花,可能也是整个南半球首次报道的化石花。这些化石是扁平层状浅灰色页岩中的压型化石和印模化石,属于鼠李科(鼠李属植物)。大花诺氏鼠李(Notiantha grandensis)新属新种的花为五基数,萼片明显具龙骨状,从花托伸出,花瓣具爪且兜状微缺,雄蕊与花瓣对生,花盘呈五边形,充满花托。利用分子支架法结合形态学数据评估了它们的系统发育位置。结果表明,这些花与现存的枣族鼠李科植物的花最为相似。与之伴生的叶被归入大花苏氏叶(Suessenia grandensis)新属新种,叶为单叶、卵形,边缘有锯齿,基部有三条离基三出脉。它们与枣族和葡萄叶枣族一些现存鼠李科植物独特的叶相符。这些化石提供了南半球鼠李科明确的大化石证据,表明鼠李科在古新世早期就已扩展到热带以外地区。鉴于此前在南极洲和澳大利亚南部古近纪晚期和新近纪有鼠李科花粉的报道,这一新发现增加了该科在新生代通过南极洲在南美洲和澳大利亚之间进行高纬度扩散的可能性。