Bera Meghma, Khan Mahasin Ali, Hazra Taposhi, Acharya Krishnendu, Goswami Bapi, Bera Subir
Centre of Advanced Study, Department of Botany, University of Calcutta, 35, B.C. Road, Kolkata, 700019, India; Department of Botany, Vidyanagar College, West Bengal, 743503, India.
Department of Botany, Sidho-Kanho-Birsha University, Ranchi Road, Purulia, 723104, India.
Fungal Biol. 2022 Sep;126(9):576-586. doi: 10.1016/j.funbio.2022.07.003. Epub 2022 Jul 16.
Here, we report the in-situ occurrence of a new fossil-species of Meliolinites (fossil Meliolaceae), Meliolinites bhutanensis sp. nov. on the cuticle fragments of a compressed angiosperm dicot leaf recovered from the middle Siwalik (Formation II: latest Miocene to Pliocene) of Bhutan, eastern Himalaya. This unique foliicolous new fossil fungal species features well-preserved mycelia consisting of superficial, brown to dark brown, septate, thick-walled, branching hyphae with bi-cellular appressoria, unicellular phialides, and a characteristic long, slightly curved hyphal seta. The web-like, brown to dark brown fungal colonies also include globose to sub-globose, dark brown ascomata, and oblong to broadly cylindrical, 5-celled, 4-septate, brown to dark brown, mature ascospores. As almost all features of different stages in the life cycle (ascospores, mature germinating ascospores, superficial lateral hyphae, hyphal seta, hyphopodia, mycelial colony, and ascomata) of this new fossil-species are found, we have proposed the first time a possible life cycle of fossil-species of Meliolaceae. The in-situ evidence of M. bhutanensis on the host leaf cuticle indicates the possible existence of a host-ectoparasite relationship in Bhutan sub-Himalaya's ancient warm and humid tropical evergreen forest during the deposition. So, M. bhutanensis might have thrived generally under warm and humid climate conditions for its growth and development in the Mio-Pliocene time, which is in conformity with our recently published quantitative climatic data by CLAMP (Climate Leaf Analysis Multivariate Program) analysis.
在此,我们报告了一种新的小煤炱属(化石小煤炱科)化石物种——不丹小煤炱(Meliolinites bhutanensis sp. nov.)在从喜马拉雅东部不丹的中锡瓦利克(地层II:最新中新世至上新世)发现的一块压缩被子植物双子叶植物叶片角质层碎片上的原位出现情况。这种独特的叶生新化石真菌物种具有保存完好的菌丝体,由表面的、棕色至深棕色、具隔膜、厚壁、分枝的菌丝组成,带有双细胞附着胞、单细胞瓶梗以及特征性的长且略弯曲的菌丝刚毛。呈网状的、棕色至深棕色的真菌菌落还包括球形至近球形、深棕色的子囊壳,以及长圆形至宽圆柱形、5细胞、4隔膜、棕色至深棕色的成熟子囊孢子。由于发现了该新化石物种生命周期不同阶段(子囊孢子、成熟萌发子囊孢子、表面侧生菌丝、菌丝刚毛、附着枝、菌丝菌落和子囊壳)的几乎所有特征,我们首次提出了小煤炱科化石物种可能的生命周期。不丹小煤炱在寄主叶片角质层上的原位证据表明,在沉积期间,不丹次喜马拉雅地区古老温暖潮湿的热带常绿森林中可能存在寄主 - 外寄生关系。因此,不丹小煤炱在中新世 - 上新世时期可能总体上在温暖潮湿的气候条件下茁壮成长以实现其生长和发育,这与我们最近通过CLAMP(气候叶片分析多变量程序)分析发表的定量气候数据一致。