Pteridófitas da região noroeste do Estado de São Paulo, Brasil: Dennstaedtiaceae

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Recognition of two morpho-types in eastern South American brackens (Pteridium-Dennstaedtiaceae-Polypodiopsida)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

蕨属的系统发育及谱系地理学研究

蕨属（Pteridium Gled. ex Scop）分布范围极广，几乎遍布于全世界。关于此属的属下分类一直争论不休，主要是因为此属的分布广，形态变异比较大，变异类型之间形态差异不显著，缺乏明确的鉴别性状，或者变异类型之间存在过渡。 本研究利用叶绿体rps4-trnS DNA序列和trnS-G DNA序列构建了世界不同地区蕨属植物的系统关系及中国区域蕨属植物的系统关系，同时构建了世界不同地区蕨属植物的单倍型关系。我们发现，（1）南美洲和澳洲的蕨属植物分化最早;（2）北美洲的蕨属植物遗传变异最丰富，有多条相互独立的进化线（evolutionary lineages）;（3）欧亚大陆和非洲的蕨属植物都与北美洲具有密切关系;（4）大洋洲的蕨属植物同时受南美洲和亚洲蕨属植物的影响;（5）东亚的蕨属植物直接受北美洲蕨属植物的影响，与欧洲和非洲没有直接的关系;（6）非洲和欧洲的蕨属植物关系密切，有着相同的起源。 根据不同地点的蕨属植物的系统关系和单倍型Network关系，我们认为，蕨属植物起源于南美洲，而后向北美洲和澳洲扩散。在北美洲东部和东南部蕨属植物得到繁荣并分别向三个方向扩散与分化。第一个方向是朝北美西部扩散，第二个方向是两次独立扩散到亚洲，第三个方向是扩散到非洲，进而由非洲向欧洲扩散。 根据叶绿体基因所揭示的世界不同地区蕨属植物的发生和发展规律结合前人的研究，我们认为蕨属包含四个物种。Pteridium aquilinum (L.) Kuhn，分布于北美洲、亚洲、非洲和欧洲。该种分布广泛，存在一定的地理分化，可进一步划分8个亚种。Pteridium esculentum (G. Forst.) Cokayne，分布于南美洲，并扩散到澳大利亚，甚至东南亚国家。Pteridium caudatum (L.) Maxon，分布于中美洲和南美洲，是个异源四倍体。Pteridium semihastatum (Wall. ex Ag.) S.B.Andrews，分布于澳洲和东南亚，是个异源四倍体。 通过分子数据和形态分析相结合，作者认为中国蕨属包括两个亚种，即蕨[Pteridium aquilinum (L.) Kuhn subsp.japonicum (Nakai) Á.Löve & D.Löve]和毛轴蕨[Pteridium aquilinum (L.) Kuhn subsp. revolutum (Bl.) X. Q. Chen, stat. nov.]。作者认为，《中国植物志》中记载的食蕨，特有种云南蕨、糙轴蕨、镰羽蕨和长羽蕨并不存在或只是蕨或毛轴蕨的变形，或者毛轴蕨与蕨的杂交个体。 为了今后更进一步研究蕨属植物的系统与进化关系、居群的遗传结构等问题，作者还分离了8个具有多态性的微卫星位点，探讨了微卫星引物开发设计过程中如何提高效率等问题。

The evolutionary history of ferns inferred from 25 low-copy nuclear genes.

UNLABELLED: • PREMISE OF THE STUDY: Understanding fern (monilophyte) phylogeny and its evolutionary timescale is critical for broad investigations of the evolution of land plants, and for providing the point of comparison necessary for studying the evolution of the fern sister group, seed plants. Molecular phylogenetic investigations have revolutionized our understanding of fern phylogeny, however, to date, these studies have relied almost exclusively on plastid data.• METHODS: Here we take a curated phylogenomics approach to infer the first broad fern phylogeny from multiple nuclear loci, by combining broad taxon sampling (73 ferns and 12 outgroup species) with focused character sampling (25 loci comprising 35877 bp), along with rigorous alignment, orthology inference and model selection.• KEY RESULTS: Our phylogeny corroborates some earlier inferences and provides novel insights; in particular, we find strong support for Equisetales as sister to the rest of ferns, Marattiales as sister to leptosporangiate ferns, and Dennstaedtiaceae as sister to the eupolypods. Our divergence-time analyses reveal that divergences among the extant fern orders all occurred prior to ∼200 MYA. Finally, our species-tree inferences are congruent with analyses of concatenated data, but generally with lower support. Those cases where species-tree support values are higher than expected involve relationships that have been supported by smaller plastid datasets, suggesting that deep coalescence may be reducing support from the concatenated nuclear data.• CONCLUSIONS: Our study demonstrates the utility of a curated phylogenomics approach to inferring fern phylogeny, and highlights the need to consider underlying data characteristics, along with data quantity, in phylogenetic studies.

Early - Late Miocene palaeoclimate data and palaefloras of 48 samples from Southern China

Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with the coexistence approach to obtain quantitative palaeoclimate data. Visualization of climate results in maps shows a distinct spatial differentiation in Southern China during the Miocene. Higher seasonalities of temperature and precipitation occur in the north and south parts of Southern China, respectively. During the Miocene, most regions of Southern China and Europe were both warm and humid. Central Eurasia was likely to be an arid center, which gradually spread westward and eastward. Our data provide information about Miocene climate patterns in Southern China and about the evolution of these patterns throughout the Miocene, and is also crucial to unravel and understand the climatic signals of global cooling and tectonic uplift.

Table 2. Percentage of palynomorphs found in each sample through Longling section

The Longling Coal Mine (W. Yunnan) is situated in an area of substantial geotectonic activity. Its Late Pliocene palynoflora is of considerable interest, since the area represents a centre of biodiversity. Eighty-two palynomorphs belonging to 61 families were recovered from the lignite. The palynoflora is dominated by angiosperms (68.3%), with ferns (24.4%), gymnosperms (4.9%) and algae (2.4%). Comparisons indicate that most of the palynoflora was derived from the Montane Humid Evergreen Broad-leaved Forest, with lesser contributions from the Tsuga dumosa Forest and Evergreen Coniferous Broad-leaved Mixed Forest, as well as the Montane Mossy Evergreen Broad-leaved Forest. This indicates that the Late Pliocene climate was cooler than that of the present. In the course of the accumulation of the lignite, the climate underwent five major phases of warming and cooling.