北美西北部中新世的北竹属植物和木杖属植物(木杖科)

Botanical Gazette Pub Date : 1991-09-01 DOI:10.1086/337898
S. Manchester, P. Crane, D. Dilcher
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引用次数: 49

摘要

在北半球古新世已经灭绝的trochodenskioldia属,在新近纪首次被记录下来,其依据是来自爱达荷州、华盛顿州和不列颠哥伦比亚南部中新世的果序、果实、相关树枝和叶子。其果序和果实,归属于间冰期野蕨(Nordenskioldia interglacialis)。11月,与古新世的北方野果非常相似,但不同之处在于每个果实的心皮数量更多,并且不太有规律地开裂。叶,木耳(木耳)梳状。在古新世沉积物中,与Nordenskioldia相关的叶片显然是同源的。木耳紫叶与古新世黄叶的不同之处在于沿边缘通常有更突出的齿状突起和更宽的侧主脉分叉。中新世材料保存完好,揭示了古新世标本未保存的特征,特别是木质素化的果实,除了单个成熟种子外,还清楚地显示出流产的胚珠。在中新世间冰期巨齿龙发生的同一地点也记录了巨齿龙的影响。Nordenskioldia的古新世和中新世物种之间,以及Trochodendron的中新世物种与现存物种之间的相似性表明,Trochodendraceae的形态进化在长达4500万年的时间间隔中相对停滞。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Nordenskioldia and Trochodendron (Trochodendraceae) from the Miocene of Northwestern North America
The extinct trochodendraceous genus Nordenskioldia, well represented in the Paleocene of the Northern Hemisphere, is documented for the first time from the Neogene, based upon infructescences, fruits, associated twigs, and foliage from the Miocene of Idaho, Washington, and southern British Columbia. The infructescences and fruits, assigned to Nordenskioldia interglacialis (Hollick) comb. nov., are very similar to Paleocene N. borealis, but differ in ranging to a higher number of carpels per fruit and in being less regularly dehiscent. The leaves, Zizyphoides auriculata (Heer) comb. nov., formerly attributed to Populus and Cocculus, are clearly congeneric with the leaves associated with Nordenskioldia in Paleocene deposits. Zizyphoides auriculata leaves differ from Paleocene Z. flabellum in having generally more prominent dentations along the margin and a broader divergence of the lateral primary veins. Excellent preservation of the Miocene material reveals features not preserved in the Paleocene specimens, and in particular, lignified fruitlets clearly show aborted ovules in addition to the single mature seed. Infructescences of Trochodendron are also documented from the same Miocene localities at which N. interglacialis occurs. The close similarities between Paleocene and Miocene species of Nordenskioldia, and also between the Miocene and extant species of Trochodendron, suggest relative stasis in the morphological evolution of the Trochodendraceae over intervals of up to 45 million years.
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