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多样的早期矮槲寄生(),始新世波罗的海琥珀生物群的生态关键物种。

Diverse early dwarf mistletoes (), ecological keystones of the Eocene Baltic amber biota.

作者信息

Sadowski Eva-Maria, Seyfullah Leyla J, Wilson Carol A, Calvin Clyde L, Schmidt Alexander R

机构信息

Department of Geobiology, University of Göttingen, Goldschmidtstraße 3, 37077 Göttingen, Germany

Department of Geobiology, University of Göttingen, Goldschmidtstraße 3, 37077 Göttingen, Germany.

出版信息

Am J Bot. 2017 May;104(5):694-718. doi: 10.3732/ajb.1600390. Epub 2017 May 21.

Abstract

PREMISE OF THE STUDY

Extant dwarf mistletoes ( M. Bieb., Viscaceae) are hemiparasites with complex roles in nature. They are one of the most severe pests in northern hemisphere conifer forests, but they also enhance the structural complexity and species diversity of the forests. Here, we describe the first pre-Miocene macrofossils of dwarf mistletoes. The fossils from Eocene Baltic amber provide new insights into the morphological evolution of the lineage and its paleobiogeography.

METHODS

The amber inclusions were investigated with light microscopy and compared with extant Viscaceae and to historic descriptions of lost Baltic amber fossils with affinities to Viscaceae.

KEY RESULTS

Six fossil species of the lineage, comb. nov., comb. nov., sp. nov., sp. nov., comb. nov. and sp. nov., occurred in source forests of Baltic amber, representing the oldest macrofossil evidence of dwarf mistletoes. They share morphological features of their bracts, internodes, fruits, and stomata with extant . Differences from extant dwarf mistletoes, such as the perianth merosity, the nonfusion of squamate bracts and presence of oblanceolate expanded leaves, indicate their affiliation to an ancient lineage of the genus.

CONCLUSIONS

The occurrence of six species of dwarf mistletoes in a single amber deposit suggests was a keystone taxon of the Baltic amber source area. As in extant conifer forests, they probably influenced the structural complexity of the forest, not only leading to more open woodlands but also increasing species diversity, at least at a microhabitat scale.

摘要

研究前提

现存的矮槲寄生(桑寄生科)是半寄生植物,在自然界中具有复杂的作用。它们是北半球针叶林中最严重的害虫之一,但也增加了森林的结构复杂性和物种多样性。在这里,我们描述了矮槲寄生的首个中新世以前的大化石。来自始新世波罗的海琥珀的化石为该谱系的形态演化及其古生物地理学提供了新的见解。

方法

利用光学显微镜对琥珀内含物进行研究,并与现存的桑寄生科植物以及与桑寄生科有亲缘关系的已丢失的波罗的海琥珀化石的历史描述进行比较。

主要结果

该谱系的六个化石物种,新组合,新组合,新物种,新物种,新组合和新物种,出现在波罗的海琥珀的源森林中,代表了矮槲寄生最古老的大化石证据。它们与现存的在苞片、节间、果实和气孔的形态特征上有共同之处。与现存矮槲寄生的不同之处,如花被片基数、鳞状苞片不融合以及倒披针形扩展叶的存在,表明它们属于该属的一个古老谱系。

结论

在单一琥珀矿床中出现六种矮槲寄生表明是波罗的海琥珀源区的关键分类群。与现存针叶林一样,它们可能影响了森林的结构复杂性,不仅导致林地更加开阔,而且至少在微生境尺度上增加了物种多样性。

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