印度中部德干高原岩层中最早的鳞片状菖蒲巨型化石及其对古生物地理的影响

Sanchita Kumar , Kaustav Roy , Robert A. Spicer , Mahasin Ali Khan
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引用次数: 0

摘要

本研究描述了两根保存完好的石化棕榈茎,这两根棕榈茎来自印度中部中央邦德干河际岩床最晚的马斯特里赫特期(晚白垩世)至最早的达尼安期(早古新世)沉积物。它们的重要解剖学特征包括:菖蒲类型的总体茎干模式、存在保存完好的纤维血管束(fvbs),其中有两个宽的中木质部血管元件(230 μm-250 μm)和一个韧皮部股、纤维血管束密度均匀、原木质部和中木质部血管元件之间缺乏连续性,以及硬膜纤维部分没有离心分离。这些特征与现存的菖蒲属植物非常相似。过矿化的茎被描述为一个新物种,即 Palmoxylon calamoides Kumar, Roy et Khan sp.这些化石代表了该科最古老的可靠化石记录,支持了它们的冈瓦纳起源,在古新世印度次大陆与欧亚大陆对接之后,它们在追踪从印度到欧洲和其他大陆的迁移路径方面的重要性,以及 "走出印度 "的扩散假说。目前,菖蒲亚科在非洲、亚洲、澳大利亚、欧洲和南美洲均有分布,但该亚科的深部化石记录较少,新生代化石数量也不多,因此有关其起源和扩散的假说难以评估。本研究对该亚科的起源和迁移以及古气候具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Earliest megafossils of scandent calamoid palms from the Deccan Intertrappean Beds of Central India and their paleobiogeographic implications

Two well-preserved petrified palm stems from the latest Maastrichtian (Late Cretaceous) to earliest Danian (Early Paleocene) sediments of the Deccan Intertrappean Beds of Madhya Pradesh, Central India are described. Their significant anatomical characteristics include a Calamus-type general stem pattern, the presence of well-preserved fibrovascular bundles (fvbs) with two wide metaxylem vessel elements (230 μm–250 μm) and one phloem strand, uniform density of fvbs, lack of continuity between protoxylem and metaxylem vessel elements, and an absence of centrifugal differentiation of sclerenchymatous fibrous parts. These features reveal a close resemblance to those of extant genera of scandent Calamoideae. The permineralized stems are described as a new species namely, Palmoxylon calamoides Kumar, Roy et Khan sp. nov. The fossils represent the oldest reliable fossil records of this family, supporting their Gondwanan origin, their importance in tracing their migration pathways from India to Europe and other continents after the docking of the Indian subcontinent with Eurasia during the Paleocene, and an “Out-of-India” dispersal hypothesis. Today the subfamily Calamoideae is disjunctly occurred in Africa, Asia, Australia, Europe, and South America, but the poor deep-time fossil record of this subfamily with a small number of Cenozoic fossils makes hypotheses concerning its origin and dispersal difficult to evaluate. The present study has significant implications for the origin and migration of this subfamily and the paleoclimate.

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