白垩纪-古新世巴塔哥尼亚孢子和花粉块:新发现、替代解释和悬而未决的问题

Facundo De Benedetti, María C. Zamaloa, María A. Gandolfo
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引用次数: 0

摘要

有关古植物学样本中孢子和花粉团块的研究很少,而且只有北半球的报告。这些集合体可能源于动物,也可能源于花卉。本文的目的是首次对南半球的孢子和花粉块进行详细研究,并根据它们的形态特征、保存情况以及与推测的活体代表比较,讨论它们可能的起源、植物学亲缘关系和授粉模式。在阿根廷巴塔哥尼亚丘布特省出露的马斯特里赫特-丹尼安拉科洛尼亚地层沉积物中,发现了3个蕨类孢子团块和18个被子植物花粉团块。大多数花粉块是单一的,由未损坏的成分组成,但其中一些花粉块有两种类型的孢子/花粉,外皮已被腐蚀和/或碎裂。这些发现代表了迄今为止南美洲和南半球已知的晚白垩世和早古新世蕨类植物和被子植物菌块的最多样化和最丰富的记录。这些结果表明,有必要对现代类群的授粉情况进行全面的大规模研究,并对古植物学样本进行仔细处理,以减少古植物学解释中已经存在的巨大偏差。化石记录中有关团块的信息极少,这影响了我们对深部时间的散布/授粉的理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Cretaceous-Paleocene Patagonian Spore and Pollen Clumps: New Findings, Alternative Explanations, and Opened Questions

Cretaceous-Paleocene Patagonian Spore and Pollen Clumps: New Findings, Alternative Explanations, and Opened Questions

There are few studies focused on spore and pollen clumps in paleopalynological samples, and these are only reports from the Northern Hemisphere. These aggregates may be of animal or floral origin. The goal of this contribution is to provide the first detailed study of spore and pollen clumps from the Southern Hemisphere, and to discuss their possible origin, botanical affinities, and pollination modes, based on their morphological characteristics, preservation and comparison with putative living representatives. Three fern spore clumps and 18 angiosperm pollen clumps were recognized in Maastrichtian-Danian La Colonia Formation sediments that outcrop at Chubut Province, Patagonia, Argentina. Most clumps are monospecific and composed of undamaged elements but some of them have two types of spore/pollen with corroded and/or fragmented exines. These findings represent the most diverse and abundant record of fern and angiosperm clumps from the Late Cretaceous and early Paleocene so far known from South America and the Southern Hemisphere. These results are indicative of the need for comprehensive large-scale studies on pollination of modern taxa and careful processing of palynological samples to lessen the already large bias in paleopalynological interpretations. The paucity of information on clumps in the fossil record has impaired our comprehension of dispersion/pollination in deep time.

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