Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, KS, 66045, USA.
Biodiversity Institute, University of Kansas, Lawrence, KS, 66045, USA.
New Phytol. 2023 May;238(4):1695-1710. doi: 10.1111/nph.18852. Epub 2023 Mar 21.
The Cycadales are an ancient and charismatic group of seed plants. However, their morphological evolution in deep time is poorly understood. While molecular divergence time analyses estimate a Cretaceous origin for most major living cycad clades, much of the extant diversity is inferred to be a result of Neogene diversifications. This leads to long branches throughout the cycadalean phylogeny that, with few exceptions, have yet to be rectified by unequivocal fossil cycads. We report a permineralized pollen cone from the Campanian Holz Shale located in Silverado Canyon, CA, USA (c. 80 million yr ago). This fossil was studied via serial sectioning, SEM, 3D reconstruction and phylogenetic analyses. Microsporophyll and pollen morphology indicate this cone is assignable to Skyttegaardia, a recently described genus based on disarticulated lignitized microsporophylls from the Early Cretaceous of Denmark. Data from this new species, including a simple cone architecture, anatomical details and vasculature organization, indicate cycadalean affinities for Skyttegaardia. Phylogenetic analyses support this assignment and recover Skyttegaardia as crown-group Cycadales, nested within Zamiaceae. Our findings support a Cretaceous diversification for crown-group Zamiaceae, which included the evolution of morphological divergent extinct taxa with unique traits that have yet to be widely identified in the fossil record.
苏铁目是一类古老而具有魅力的种子植物。然而,它们在深层时间的形态进化仍未被充分理解。尽管分子分歧时间分析估计大多数主要现存苏铁类群起源于白垩纪,但现存的多样性很大程度上被推断为中新世多样化的结果。这导致了苏铁目系统发育中的长枝,除了少数例外,这些长枝尚未被明确的化石苏铁类植物所纠正。我们报道了一个来自美国加利福尼亚州西尔弗拉多峡谷的霍兹页岩(Holz Shale)的晚白垩世(约 8000 万年前)的石化花粉囊。这个化石通过连续切片、SEM、3D 重建和系统发育分析进行了研究。小孢子叶和花粉形态表明,这个花粉囊可归入 Skyttegaardia,这是一个最近基于丹麦早白垩世离散的木质化小孢子叶描述的属。来自这个新物种的数据,包括简单的锥体结构、解剖细节和脉管组织的排列,表明 Skyttegaardia 与苏铁目具有亲缘关系。系统发育分析支持这一分类,并将 Skyttegaardia 归为苏铁目,位于泽米科之中。我们的发现支持了苏铁目在白垩纪的多样化,包括形态上有分歧的灭绝类群的进化,这些类群具有独特的特征,在化石记录中尚未得到广泛识别。