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澳大利亚东冈瓦纳塔斯马尼亚近极地区域早始新世气候最适宜期的非开花植物。

The non-flowering plants of a near-polar forest in East Gondwana, Tasmania, Australia, during the Early Eocene Climatic Optimum.

机构信息

School of Biological Sciences, University of Adelaide, Adelaide, 5005, South Australia, Australia.

出版信息

Am J Bot. 2024 Sep;111(9):e16398. doi: 10.1002/ajb2.16398. Epub 2024 Aug 27.

Abstract

PREMISE

The Cenozoic Macquarie Harbour Formation (MHF) hosts one of the oldest and southernmost post-Cretaceous fossil plant assemblages in Australia. Coinciding with the Early Eocene Climatic Optimum (EECO) and predating the breakup of Australia from Antarctica, it offers critical data to study the diversity and extent of the Austral Polar Forest Biome, and the floristic divergence between Australasia and South America resulting from the Gondwana breakup.

METHODS

The micromorphology and macromorphology of new fossil plant compressions from the MHF were described and systematically analyzed. Previously published non-flowering plant records were reviewed and revised. Macrofossil abundance data were provided. The flora was compared with other early Paleogene assemblages from across the Southern Hemisphere.

RESULTS

Twelve species of non-flowering plants were identified from the macrofossil record. Conifers include Araucariaceae (Araucaria macrophylla, A. readiae, A. timkarikensis sp. nov., and Araucarioides linearis), Podocarpaceae (Acmopyle glabra, Dacrycarpus mucronatus, Podocarpus paralungatikensis sp. nov., and Retrophyllum sp.), and Cupressaceae (Libocedrus microformis). Dacrycarpus linifolius was designated a junior synonym of D. mucronatus. Further components include a cycad (Bowenia johnsonii, Zamiaceae), a pteridosperm (Komlopteris cenozoicus, Umkomasiaceae), and a fern (Lygodium dinmorphyllum, Schizaeaceae).

CONCLUSIONS

The fossil assemblage represents a mixed near-polar forest with a high diversity of conifers. The morphology and preservation of several species indicate adaptations to life at high latitudes. The coexistence of large- and small-leaved conifers implies complex, possibly open forest structures. Comparisons with contemporaneous assemblages from Argentina support a circumpolar biome during the EECO, reaching from southern Australia across Antarctica to southern South America.

摘要

前提

新生代麦夸里港组(MHF)拥有澳大利亚最古老、最南端的新生代后化石植物组合之一。它与早始新世气候最佳期(EECO)同时发生,早于澳大利亚与南极洲分离,为研究澳大利亚极地森林生物群的多样性和范围,以及冈瓦纳分裂导致的澳大利亚-南极洲与南美洲植物区系的分化提供了关键数据。

方法

描述和系统分析了来自 MHF 的新化石植物压缩标本的微观形态和宏观形态。回顾和修订了以前发表的非开花植物记录。提供了大型植物丰度数据。该植物群与南半球其他早古近纪组合进行了比较。

结果

从宏观化石记录中鉴定出 12 种非开花植物。包括南洋杉科(南洋杉属(Araucaria macrophylla、A. readiae、A. timkarikensis sp. nov. 和 Araucarioides linearis)、罗汉松科(罗汉松属(Acmopyle glabra、Dacrycarpus mucronatus、Podocarpus paralungatikensis sp. nov. 和 Retrophyllum sp.)和柏科(贝壳杉属(Libocedrus microformis)。Dacrycarpus linifolius 被指定为 D. mucronatus 的次异名。进一步的组成部分包括苏铁(Bowenia johnsonii,苏铁科)、木贼(Komlopteris cenozoicus,木贼科)和蕨类植物(Lygodium dinmorphyllum,水龙骨科)。

结论

化石组合代表了一个具有高度多样性的针叶树的混合近极地森林。几种物种的形态和保存表明它们适应了高纬度的生活。大、小叶针叶树的共存意味着复杂的、可能是开阔的森林结构。与来自阿根廷的同期组合的比较支持 EECO 期间存在一个环绕极地的生物群,从澳大利亚南部穿过南极洲延伸到南美的南部。

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